Association Genetics of Chemical Wood Properties in Black Poplar (Populus Nigra). Guerra, F. P., Wegrzyn, J. L., Sykes, R., Davis, M. F., Stanton, B. J., & Neale, D. B. 197(1):162–176. Paper doi abstract bibtex [::] Black poplar (Populus nigra) is a potential feedstock for cellulosic ethanol production, although breeding for this specific end use is required. Our goal was to identify associations between single nucleotide polymorphism (SNP) markers within candidate genes encoding cellulose and lignin biosynthetic enzymes, with chemical wood property phenotypic traits, toward the aim of developing genomics-based breeding technologies for bioethanol production. [::] Pyrolysis molecular beam mass spectrometry was used to determine contents of five- and six-carbon sugars, lignin, and syringyl~:~guaiacyl ratio. The association population included 599 clones from 17 half-sib families, which were successfully genotyped using 433 SNPs from 39 candidate genes. Statistical analyses were performed to estimate genetic parameters, linkage disequilibrium (LD), and single marker and haplotype-based associations. [::] A moderate to high heritability was observed for all traits. The LD, across all candidate genes, showed a rapid decay with physical distance. Analysis of single marker-phenotype associations identified six significant marker-trait pairs, whereas nearly 280 haplotypes were associated with phenotypic traits, in both an individual and multiple trait-specific manner. [::] The rapid decay of LD within candidate genes in this population and the genetic associations identified suggest a close relationship between the associated SNPs and the causative polymorphisms underlying the genetic variation of lignocellulosic traits in black poplar.
@article{guerraAssociationGeneticsChemical2013,
title = {Association Genetics of Chemical Wood Properties in Black Poplar ({{Populus}} Nigra)},
author = {Guerra, Fernando P. and Wegrzyn, Jill L. and Sykes, Robert and Davis, Mark F. and Stanton, Brian J. and Neale, David B.},
date = {2013-01},
journaltitle = {New Phytologist},
volume = {197},
pages = {162--176},
issn = {0028-646X},
doi = {10.1111/nph.12003},
url = {https://doi.org/10.1111/nph.12003},
abstract = {[::] Black poplar (Populus nigra) is a potential feedstock for cellulosic ethanol production, although breeding for this specific end use is required. Our goal was to identify associations between single nucleotide polymorphism (SNP) markers within candidate genes encoding cellulose and lignin biosynthetic enzymes, with chemical wood property phenotypic traits, toward the aim of developing genomics-based breeding technologies for bioethanol production. [::] Pyrolysis molecular beam mass spectrometry was used to determine contents of five- and six-carbon sugars, lignin, and syringyl~:~guaiacyl ratio. The association population included 599 clones from 17 half-sib families, which were successfully genotyped using 433 SNPs from 39 candidate genes. Statistical analyses were performed to estimate genetic parameters, linkage disequilibrium (LD), and single marker and haplotype-based associations. [::] A moderate to high heritability was observed for all traits. The LD, across all candidate genes, showed a rapid decay with physical distance. Analysis of single marker-phenotype associations identified six significant marker-trait pairs, whereas nearly 280 haplotypes were associated with phenotypic traits, in both an individual and multiple trait-specific manner. [::] The rapid decay of LD within candidate genes in this population and the genetic associations identified suggest a close relationship between the associated SNPs and the causative polymorphisms underlying the genetic variation of lignocellulosic traits in black poplar.},
keywords = {*imported-from-citeulike-INRMM,~INRMM-MiD:c-13157127,~to-add-doi-URL,association-genetics,bioethanol,cellulose,forest-resources,half-sib-families,lignin,populus-nigra,single-nucleotide-polymorphism},
number = {1}
}
Analysis of Dyes in Textiles from the Chehrabad Salt Mine in Iran. Mouri, C., Aali, A., Zhang, X., & Laursen, R. 2(1):20. Paper doi abstract bibtex This study describes the analysis of dyes from three textile specimens associated with human remains found in the Chehrabad salt mine in northwestern Iran dating to 2000\,±\,400 years BP. They are unique for this part of the world not only because of their age, but because they represent textiles used by common people (salt miners) as opposed to funerary garments of the wealthy. Samples of yarns from these specimens were extracted and analyzed by high performance liquid chromatography with diode array and mass spectrometric detection. The red dye was obtained from madder (specifically Rubia tinctorum L.), and the blue was from an indigo plant, probably woad (Isatis tinctoria L.), both of which are known in Iran. Two yellow, plant-derived, flavonol dyes were found. The first seems to be from a species of tamarisk (Tamarix sp.), whereas the second, found in both yellow and green yarns, is from a so-far unidentified plant. This work represents the first detailed study of these salt mine dyes, and the first evidence for the use of tamarisk as a dyestuff.
@article{mouriAnalysisDyesTextiles2014,
title = {Analysis of Dyes in Textiles from the {{Chehrabad}} Salt Mine in {{Iran}}},
author = {Mouri, Chika and Aali, Abolfazl and Zhang, Xian and Laursen, Richard},
date = {2014},
journaltitle = {Heritage Science},
volume = {2},
pages = {20},
issn = {2050-7445},
doi = {10.1186/s40494-014-0020-3},
url = {https://doi.org/10.1186/s40494-014-0020-3},
abstract = {This study describes the analysis of dyes from three textile specimens associated with human remains found in the Chehrabad salt mine in northwestern Iran dating to 2000\,±\,400 years BP. They are unique for this part of the world not only because of their age, but because they represent textiles used by common people (salt miners) as opposed to funerary garments of the wealthy. Samples of yarns from these specimens were extracted and analyzed by high performance liquid chromatography with diode array and mass spectrometric detection. The red dye was obtained from madder (specifically Rubia tinctorum L.), and the blue was from an indigo plant, probably woad (Isatis tinctoria L.), both of which are known in Iran. Two yellow, plant-derived, flavonol dyes were found. The first seems to be from a species of tamarisk (Tamarix sp.), whereas the second, found in both yellow and green yarns, is from a so-far unidentified plant. This work represents the first detailed study of these salt mine dyes, and the first evidence for the use of tamarisk as a dyestuff.},
keywords = {*imported-from-citeulike-INRMM,~INRMM-MiD:c-13589725,~to-add-doi-URL,forest-resources,iran,secondary-production,tamarix-spp},
number = {1}
}
Reframing Ecosystem Management in the Era of Climate Change: Issues and Knowledge from Forests. Mori, A. S., Spies, T. A., Sudmeier-Rieux, K., & Andrade, A. 165:115–127. Paper doi abstract bibtex We discuss ” ecosystem management (EM)” to face contemporary climate change issues. EM focuses on sustaining ecosystems to meet both ecological and human needs. EM plans have been largely developed independent of concerns about climate change. However, EM is potentially effective for climate change mitigation and adaptation. We provide the principle guidelines based on EM to adaptively tackle the issues. Climate change is one of the significant concerns in land and resource management, creating an urgent need to build social-ecological capacity to address widespread and uncertain environmental changes. Given the diversity and complexity of ecological responses to climate change ” ecosystem management” approaches are needed to provide solutions for meeting both ecological and human needs, while reducing anthropogenic warming and climate-related impacts on society. For instance, ecosystem management can contribute to a reduction in the greenhouse gas emissions through improved land-use and reduced deforestation at a regional scale. Further, conserving and restoring naturally-functioning ecosystems, which is often one of the goals of ecosystem management can significantly contribute to buffering ecological responses to climate extremes such as droughts and wildfires. Moreover, ecosystem management helps build capacity for learning and adaptation at multiple scales. As a result, societies will be better prepared to respond to surprises and uncertainties associated with climate change. In this regard, it is imperative to reframe climate change issues based on the ecosystem approach. Although climate change and ecosystem management plans have largely developed independently, it is now essential for all stakeholders to work together to achieve multiple goals. The ecosystem-based approaches can enable flexible and effective responses to the uncertainties associated with climate change. Reframing ecosystem management helps to face an urgent need for reconsideration and improvement of social-ecological resilience in order to mitigate and adapt to the changing climate. [Excerpt: Conclusion] Novel approaches underpinned by sociology, ecology and climate science are necessary to perform assessments that reflect the many roles that ecosystem management can play in mitigating and adapting to climate change. No single method and focal scale for addressing the effects or causes of climate change exists. Indeed, there are often trade-offs such as those between the goals of building resilience (learning from failure) and reducing vulnerability (minimizing failure) (Adger et al., 2008), suggesting some policies aimed at minimizing exposure to any hazards at the regional scale can potentially conflict with the proactive implementation of adaptive management at the local scale. In this article, we have discussed reframing ecosystem management as an effective way to address the uncertainties of climate change. It is therefore necessary to adopt flexible and robust management strategies that consider various scenarios, rather than adopting a single measure. Similar to climate change, which is intricately connected to other issues beyond physical climatic change, ecological issues are deeply associated with global issues. A number of environmental policies and plans have been historically developed with little consideration of climate instability. Among them, our attempt that integrates different management considerations into the common context lends a strong support for the objectives and approaches of ecosystem management as an effective tool to face climate change uncertainties. [\n] It is important for all stakeholders to work together to identity multiple goals. Ecologists need to address ecosystem processes and functions in the context of possible future conditions; resource managers and policymakers need to build capacity for learning and adaptation; and all stakeholders need to share a recognition that social-ecological systems are interacting not only with each other (social-ecological interdependence) but also with the climate system. In keeping with the view of Moss et al. (2010) that the future climate largely depends on the behaviour of global society, the fates of ecosystems will strongly depend on how human society faces climate change. In particular, there are still important gaps in the combined study of climate and ecosystem science that need to be addressed. At the time of UNFCCC meetings in Copenhagen in 2009, UNEP (2009a) stated that climate information, when coupled with other information such as ecology and socio-economics, should be centralized within policy formulation and decision making process for practical ecosystem management at local and regional scales with reasonable timescales of the next several decades. Bringing different fields together is essential to tackle future complexity. The constructive improvements that come from an ecosystem management strategy, as summarized in Table 2, has the potential to effectively fill the gaps among disciplines and stakeholders.
@article{moriReframingEcosystemManagement2013,
title = {Reframing Ecosystem Management in the Era of Climate Change: Issues and Knowledge from Forests},
author = {Mori, Akira S. and Spies, Thomas A. and Sudmeier-Rieux, Karen and Andrade, Angela},
date = {2013-09},
journaltitle = {Biological Conservation},
volume = {165},
pages = {115--127},
issn = {0006-3207},
doi = {10.1016/j.biocon.2013.05.020},
url = {https://doi.org/10.1016/j.biocon.2013.05.020},
abstract = {We discuss ” ecosystem management (EM)” to face contemporary climate change issues. EM focuses on sustaining ecosystems to meet both ecological and human needs. EM plans have been largely developed independent of concerns about climate change. However, EM is potentially effective for climate change mitigation and adaptation. We provide the principle guidelines based on EM to adaptively tackle the issues. Climate change is one of the significant concerns in land and resource management, creating an urgent need to build social-ecological capacity to address widespread and uncertain environmental changes. Given the diversity and complexity of ecological responses to climate change ” ecosystem management” approaches are needed to provide solutions for meeting both ecological and human needs, while reducing anthropogenic warming and climate-related impacts on society. For instance, ecosystem management can contribute to a reduction in the greenhouse gas emissions through improved land-use and reduced deforestation at a regional scale. Further, conserving and restoring naturally-functioning ecosystems, which is often one of the goals of ecosystem management can significantly contribute to buffering ecological responses to climate extremes such as droughts and wildfires. Moreover, ecosystem management helps build capacity for learning and adaptation at multiple scales. As a result, societies will be better prepared to respond to surprises and uncertainties associated with climate change. In this regard, it is imperative to reframe climate change issues based on the ecosystem approach. Although climate change and ecosystem management plans have largely developed independently, it is now essential for all stakeholders to work together to achieve multiple goals. The ecosystem-based approaches can enable flexible and effective responses to the uncertainties associated with climate change. Reframing ecosystem management helps to face an urgent need for reconsideration and improvement of social-ecological resilience in order to mitigate and adapt to the changing climate.
[Excerpt: Conclusion]
Novel approaches underpinned by sociology, ecology and climate science are necessary to perform assessments that reflect the many roles that ecosystem management can play in mitigating and adapting to climate change. No single method and focal scale for addressing the effects or causes of climate change exists. Indeed, there are often trade-offs such as those between the goals of building resilience (learning from failure) and reducing vulnerability (minimizing failure) (Adger et al., 2008), suggesting some policies aimed at minimizing exposure to any hazards at the regional scale can potentially conflict with the proactive implementation of adaptive management at the local scale. In this article, we have discussed reframing ecosystem management as an effective way to address the uncertainties of climate change. It is therefore necessary to adopt flexible and robust management strategies that consider various scenarios, rather than adopting a single measure. Similar to climate change, which is intricately connected to other issues beyond physical climatic change, ecological issues are deeply associated with global issues. A number of environmental policies and plans have been historically developed with little consideration of climate instability. Among them, our attempt that integrates different management considerations into the common context lends a strong support for the objectives and approaches of ecosystem management as an effective tool to face climate change uncertainties.
[\textbackslash n] It is important for all stakeholders to work together to identity multiple goals. Ecologists need to address ecosystem processes and functions in the context of possible future conditions; resource managers and policymakers need to build capacity for learning and adaptation; and all stakeholders need to share a recognition that social-ecological systems are interacting not only with each other (social-ecological interdependence) but also with the climate system. In keeping with the view of Moss et al. (2010) that the future climate largely depends on the behaviour of global society, the fates of ecosystems will strongly depend on how human society faces climate change. In particular, there are still important gaps in the combined study of climate and ecosystem science that need to be addressed. At the time of UNFCCC meetings in Copenhagen in 2009, UNEP (2009a) stated that climate information, when coupled with other information such as ecology and socio-economics, should be centralized within policy formulation and decision making process for practical ecosystem management at local and regional scales with reasonable timescales of the next several decades. Bringing different fields together is essential to tackle future complexity. The constructive improvements that come from an ecosystem management strategy, as summarized in Table 2, has the potential to effectively fill the gaps among disciplines and stakeholders.},
keywords = {*imported-from-citeulike-INRMM,~INRMM-MiD:c-13912160,~to-add-doi-URL,adaptation,climate-change,climate-extremes,droughts,ecology,ecosystem,forest-resources,incomplete-knowledge,knowledge-integration,mitigation,uncertainty,wildfires}
}
Waterways as Invasion Highways - Impact of Climate Change and Globalization Biological Invasions. Galil, B. S., Nehring, S., & Panov, V. In Biological Invasions, volume 193, of Ecological Studies, pages 59–74. Springer Berlin Heidelberg. Paper doi abstract bibtex The earliest civilizations flourished on the banks of navigable rivers. Indeed, their first monumental hydrological construction projects were concerned with irrigation and transport: around 2200 b.c., the first navigable canal, the Shatt-el-hai, linking the Tigris and Euphrates rivers in Mesopotamia, was excavated; in the 6th century b.c., a canal was built which joined the Nile with the northern Red Sea and, in the 4th century b.c., the Grand Canal in China connected Peking to Hangzhou, a distance of almost 1,000 km.The technological innovations of the 18th century led to an expansion of the network of navigable inland waterways, followed in the 19th century and the early part of the 20th century by the excavation of two interoceanic canals: the Suez Canal, which opened a direct route from the Mediterranean Sea to the Indo-Pacific Ocean, and the Panama Canal, which afforded passage between the Atlantic and Eastern Pacific oceans. Canals connecting rivers over watersheds or seas across narrow land bridges ” dissolve” natural barriers to the dispersal of aquatic organisms, thereby furnishing these with many opportunities for natural dispersal as well as for shipping-mediated transport. The introduction of alien aquatic species has proven to be one of the most profound and damaging anthropogenic deeds - involving both ecological and economic costs. Globalization and climate change are projected to increase aquatic bioinvasions and reduce environmental resistance to invasion of thermophilic biota. Navigable waterways serving as major invasion corridors offer a unique opportunity to study the impact of these processes.
@incollection{galilWaterwaysInvasionHighways2007,
title = {Waterways as Invasion Highways - {{Impact}} of Climate Change and Globalization Biological Invasions},
booktitle = {Biological {{Invasions}}},
author = {Galil, Bella S. and Nehring, Stefan and Panov, Vadim},
editor = {Nentwig, Wolfgang},
date = {2007},
volume = {193},
pages = {59--74},
publisher = {{Springer Berlin Heidelberg}},
location = {{Berlin, Heidelberg}},
doi = {10.1007/978-3-540-36920-2\\_5},
url = {https://doi.org/10.1007/978-3-540-36920-2_5},
abstract = {The earliest civilizations flourished on the banks of navigable rivers. Indeed, their first monumental hydrological construction projects were concerned with irrigation and transport: around 2200 b.c., the first navigable canal, the Shatt-el-hai, linking the Tigris and Euphrates rivers in Mesopotamia, was excavated; in the 6th century b.c., a canal was built which joined the Nile with the northern Red Sea and, in the 4th century b.c., the Grand Canal in China connected Peking to Hangzhou, a distance of almost 1,000 km.The technological innovations of the 18th century led to an expansion of the network of navigable inland waterways, followed in the 19th century and the early part of the 20th century by the excavation of two interoceanic canals: the Suez Canal, which opened a direct route from the Mediterranean Sea to the Indo-Pacific Ocean, and the Panama Canal, which afforded passage between the Atlantic and Eastern Pacific oceans. Canals connecting rivers over watersheds or seas across narrow land bridges ” dissolve” natural barriers to the dispersal of aquatic organisms, thereby furnishing these with many opportunities for natural dispersal as well as for shipping-mediated transport. The introduction of alien aquatic species has proven to be one of the most profound and damaging anthropogenic deeds - involving both ecological and economic costs. Globalization and climate change are projected to increase aquatic bioinvasions and reduce environmental resistance to invasion of thermophilic biota. Navigable waterways serving as major invasion corridors offer a unique opportunity to study the impact of these processes.},
isbn = {978-3-540-77375-7},
keywords = {*imported-from-citeulike-INRMM,~INRMM-MiD:c-11477007,~to-add-doi-URL,alien-species,climate-change,global-change,natural-resources-interactions,water-resources},
series = {Ecological {{Studies}}}
}
Extensive Sharing of Chloroplast Haplotypes among European Birches Indicates Hybridization among Betula Pendula, B. Pubescens and B. Nana. Palme, A. E., Su, Q., Palsson, S., & Lascoux, M. 13(1):167–178. Paper doi abstract bibtex Extensive sharing of chloroplast haplotypes among the silver birch, Betula pendula Roth., the downy birch, B. pubescens Ehrh., and the dwarf birch, B. nana L., was discovered using polymerase chain reaction-restriction fragment length polymporphism markers. The geographical component of the genetic variation was stronger than the species component: the species were not significantly different while 11\,% of the variation could be attributed to differentiation between the two main regions studied, Scandinavia and western Russia. All haplotypes occurring in more than 2\,% of the individuals were shared among the species and the introgression ratios were quite large: 0.79 between B. pubescens and B. pendula and 0.67 between B. pubescens and B. nana. The data also indicate that B. pendula individuals are more similar to sympatric B. pubescens than to B. pendula individuals from nearby forests. However, this trend is not as pronounced when B. pubescens is considered, suggesting that introgression is not symmetrical. The haplotype sharing among the three Betula species is most likely caused by hybridization and subsequent cytoplasmic introgression.
@article{palmeExtensiveSharingChloroplast2004,
title = {Extensive Sharing of Chloroplast Haplotypes among {{European}} Birches Indicates Hybridization among {{Betula}} Pendula, {{B}}. Pubescens and {{B}}. Nana},
author = {Palme, A. E. and Su, Q. and Palsson, S. and Lascoux, M.},
date = {2004-01},
journaltitle = {Molecular Ecology},
volume = {13},
pages = {167--178},
issn = {0962-1083},
doi = {10.1046/j.1365-294x.2003.02034.x},
url = {https://doi.org/10.1046/j.1365-294x.2003.02034.x},
abstract = {Extensive sharing of chloroplast haplotypes among the silver birch, Betula pendula Roth., the downy birch, B. pubescens Ehrh., and the dwarf birch, B. nana L., was discovered using polymerase chain reaction-restriction fragment length polymporphism markers. The geographical component of the genetic variation was stronger than the species component: the species were not significantly different while 11\,\% of the variation could be attributed to differentiation between the two main regions studied, Scandinavia and western Russia. All haplotypes occurring in more than 2\,\% of the individuals were shared among the species and the introgression ratios were quite large: 0.79 between B. pubescens and B. pendula and 0.67 between B. pubescens and B. nana. The data also indicate that B. pendula individuals are more similar to sympatric B. pubescens than to B. pendula individuals from nearby forests. However, this trend is not as pronounced when B. pubescens is considered, suggesting that introgression is not symmetrical. The haplotype sharing among the three Betula species is most likely caused by hybridization and subsequent cytoplasmic introgression.},
keywords = {*imported-from-citeulike-INRMM,~INRMM-MiD:c-13628397,~to-add-doi-URL,betula-nana,betula-pendula,betula-pubescens,europe,forest-resources,hybridisation},
number = {1}
}
Nature vs. Nurture: Managing Relationships between Forests, Agroforestry and Wild Biodiversity. McNeely, J. A. 61-62(1-3):155–165. Paper doi abstract bibtex Many agroforestry systems are found in places that otherwise would be appropriate for natural forests, and often have replaced them. Humans have had a profound influence on forests virtually everywhere they both are found. Thus 'natural' defined as 'without human influence' is a hypothetical construct, though one that has assumed mythological value among many conservationists. Biodiversity is a forest value that does not carry a market price. It is the foundation, however, upon which productive systems depend. The relationship between agroforestry and the wild biodiversity contained in more natural forests is a complicated one, depending on the composition of the agroforestry system itself and the way it is managed. Complex forest gardens are more supportive of biodiversity than monocrop systems, shade coffee more than sun coffee, and systems using native plants tend to be more biologically diverse. Nonnative plants, especially potentially invasive alien species, threaten biodiversity and need to be avoided. The relationship between forests, agroforestry and wild biodiversity can be made most productive through applying adaptive management approaches that incorporate ongoing research and monitoring in order to feed information back into the management system. Maintaining diversity in approaches to management of agroforestry systems will provide humanity with the widest range of options for adapting to changing conditions. Clear government policy frameworks are needed that support alliances among the many interest groups involved in forest biodiversity.
@article{mcneelyNatureVsNurture2004,
title = {Nature vs. Nurture: Managing Relationships between Forests, Agroforestry and Wild Biodiversity},
author = {McNeely, J. A.},
date = {2004},
journaltitle = {Agroforestry Systems},
volume = {61-62},
pages = {155--165},
issn = {1572-9680},
doi = {10.1023/B:AGFO.0000028996.92553.ea},
url = {https://doi.org/10.1023/B:AGFO.0000028996.92553.ea},
abstract = {Many agroforestry systems are found in places that otherwise would be appropriate for natural forests, and often have replaced them. Humans have had a profound influence on forests virtually everywhere they both are found. Thus 'natural' defined as 'without human influence' is a hypothetical construct, though one that has assumed mythological value among many conservationists. Biodiversity is a forest value that does not carry a market price. It is the foundation, however, upon which productive systems depend. The relationship between agroforestry and the wild biodiversity contained in more natural forests is a complicated one, depending on the composition of the agroforestry system itself and the way it is managed. Complex forest gardens are more supportive of biodiversity than monocrop systems, shade coffee more than sun coffee, and systems using native plants tend to be more biologically diverse. Nonnative plants, especially potentially invasive alien species, threaten biodiversity and need to be avoided. The relationship between forests, agroforestry and wild biodiversity can be made most productive through applying adaptive management approaches that incorporate ongoing research and monitoring in order to feed information back into the management system. Maintaining diversity in approaches to management of agroforestry systems will provide humanity with the widest range of options for adapting to changing conditions. Clear government policy frameworks are needed that support alliances among the many interest groups involved in forest biodiversity.},
keywords = {*imported-from-citeulike-INRMM,~INRMM-MiD:c-13938673,~to-add-doi-URL,agroforestry,asia,biodiversity,central-america,europe,forest-management,forest-resources,integration-techniques,mediterranean-region,multi-criteria-decision-analysis,multi-objective-planning,multi-stakeholder-decision-making,multiplicity,north-america,south-america},
number = {1-3}
}
Welcome to Postnormal Times. Sardar, Z. 42(5):435–444. Paper doi abstract bibtex All that was 'normal' has now evaporated; we have entered postnormal times, the in-between period where old orthodoxies are dying, new ones have not yet emerged, and nothing really makes sense. To have any notion of a viable future, we must grasp the significance of this period of transition which is characterised by three c's: complexity, chaos and contradictions. These forces propel and sustain postnormal times leading to uncertainty and different types of ignorance that make decision-making problematic and increase risks to individuals, society and the planet. Postnormal times demands, this paper argues, that we abandon the ideas of 'control and management', and rethink the cherished notions of progress, modernisation and efficiency. The way forward must be based on virtues of humility, modesty and accountability, the indispensible requirement of living with uncertainty, complexity and ignorance. We will have to imagine ourselves out of postnormal times and into a new age of normalcy – with an ethical compass and a broad spectrum of imaginations from the rich diversity of human cultures.
@article{sardarWelcomePostnormalTimes2010,
title = {Welcome to Postnormal Times},
author = {Sardar, Ziauddin},
date = {2010-06},
journaltitle = {Futures},
volume = {42},
pages = {435--444},
issn = {0016-3287},
doi = {10.1016/j.futures.2009.11.028},
url = {https://doi.org/10.1016/j.futures.2009.11.028},
abstract = {All that was 'normal' has now evaporated; we have entered postnormal times, the in-between period where old orthodoxies are dying, new ones have not yet emerged, and nothing really makes sense. To have any notion of a viable future, we must grasp the significance of this period of transition which is characterised by three c's: complexity, chaos and contradictions. These forces propel and sustain postnormal times leading to uncertainty and different types of ignorance that make decision-making problematic and increase risks to individuals, society and the planet. Postnormal times demands, this paper argues, that we abandon the ideas of 'control and management', and rethink the cherished notions of progress, modernisation and efficiency. The way forward must be based on virtues of humility, modesty and accountability, the indispensible requirement of living with uncertainty, complexity and ignorance. We will have to imagine ourselves out of postnormal times and into a new age of normalcy -- with an ethical compass and a broad spectrum of imaginations from the rich diversity of human cultures.},
keywords = {*imported-from-citeulike-INRMM,~INRMM-MiD:c-6230082,~to-add-doi-URL,chaos,complexity,deep-uncertainty,ethics,feedback,mitigation,non-linearity,post-normal-science,science-ethics,science-society-interface,social-system,technocracy,trade-offs,uncertainty,unknown},
number = {5}
}
Evaluating Post-Fire Forest Resilience Using GIS and Multi-Criteria Analysis: An Example from Cape Sounion National Park, Greece. Arianoutsou, M., Koukoulas, S., & Kazanis, D. 47(3):384–397. Paper doi abstract bibtex Forest fires are one of the major causes of ecological disturbance in the mediterranean climate ecosystems of the world. Despite the fact that a lot of resources have been invested in fire prevention and suppression, the number of fires occurring in the Mediterranean Basin in the recent decades has continued to markedly increase. The understanding of the relationship between landscape and fire lies, among others, in the identification of the system's post-fire resilience. In our study, ecological and landscape data are integrated with decision-support techniques in a Geographic Information Systems (GIS) framework to evaluate the risk of losing post-fire resilience in Pinus halepensis forests, using Cape Sounion National Park, Central Greece, as a pilot case. The multi-criteria decision support approach has been used to synthesize both bio-indicators (woody cover, pine density, legume cover and relative species richness and annual colonizers) and geo-indicators (fire history, parent material, and slope inclination) in order to rank the landscape components. Judgments related to the significance of each factor were incorporated within the weights coefficients and then integrated into the multicriteria rule to map the risk index. Sensitivity analysis was very critical for assessing the contribution of each factor and the sensitivity to subjective weight judgments to the final output. The results of this study include a final ranking map of the risk of losing resilience, which is very useful in identifying the risk hotspots , where post-fire management measures should be applied in priority.
@article{arianoutsouEvaluatingPostfireForest2011,
title = {Evaluating Post-Fire Forest Resilience Using {{GIS}} and Multi-Criteria Analysis: An Example from {{Cape Sounion National Park}}, {{Greece}}},
author = {Arianoutsou, Margarita and Koukoulas, Sotirios and Kazanis, Dimitrios},
date = {2011-02},
journaltitle = {Environmental Management},
volume = {47},
pages = {384--397},
issn = {0364-152X},
doi = {10.1007/s00267-011-9614-7},
url = {https://doi.org/10.1007/s00267-011-9614-7},
abstract = {Forest fires are one of the major causes of ecological disturbance in the mediterranean climate ecosystems of the world. Despite the fact that a lot of resources have been invested in fire prevention and suppression, the number of fires occurring in the Mediterranean Basin in the recent decades has continued to markedly increase. The understanding of the relationship between landscape and fire lies, among others, in the identification of the system's post-fire resilience. In our study, ecological and landscape data are integrated with decision-support techniques in a Geographic Information Systems (GIS) framework to evaluate the risk of losing post-fire resilience in Pinus halepensis forests, using Cape Sounion National Park, Central Greece, as a pilot case. The multi-criteria decision support approach has been used to synthesize both bio-indicators (woody cover, pine density, legume cover and relative species richness and annual colonizers) and geo-indicators (fire history, parent material, and slope inclination) in order to rank the landscape components. Judgments related to the significance of each factor were incorporated within the weights coefficients and then integrated into the multicriteria rule to map the risk index. Sensitivity analysis was very critical for assessing the contribution of each factor and the sensitivity to subjective weight judgments to the final output. The results of this study include a final ranking map of the risk of losing resilience, which is very useful in identifying the risk hotspots , where post-fire management measures should be applied in priority.},
keywords = {*imported-from-citeulike-INRMM,~INRMM-MiD:c-8804314,~to-add-doi-URL,array-of-factors,forest-fires,gis,greece,multi-criteria-decision-analysis,multiplicity,postfire-impacts,resilience,wildfires},
number = {3}
}
A Review of the Mechanical Effects of Plant Roots on Concentrated Flow Erosion Rates. Vannoppen, W., Vanmaercke, M., De Baets, S., & Poesen, J. 150:666–678. Paper doi abstract bibtex Living plant roots modify both mechanical and hydrological characteristics of the soil matrix (e.g. soil aggregate stability by root exudates, soil cohesion, infiltration rate, soil moisture content, soil organic matter) and negatively influence the soil erodibility. During the last two decades several studies reported on the effects of plant roots in controlling concentrated flow erosion rates. However a global analysis of the now available data on root effects is still lacking. Yet, a meta-data analysis will contribute to a better understanding of the soil-root interactions as our capability to assess the effectiveness of roots in reducing soil erosion rates due to concentrated flow in different environments remains difficult. The objectives of this study are therefore: i) to provide a state of the art on studies quantifying the effectiveness of roots in reducing soil erosion rates due to concentrated flow; and ii) to explore the overall trends in erosion reduction as a function of the root (length) density, root architecture and soil texture, based on an integrated analysis of published data. We therefore compiled a dataset of measured soil detachment ratios (SDR) for the root density (RD; 822 observations) as well as for the root length density (RLD; 274 observations). A Hill curve model best describes the decrease in SDR as a function of R(L)D. An important finding of our meta-analysis is that RLD is a much more suitable variable to estimate SDR compared to RD as it is linked to root architecture. However, a large proportion of the variability in SDR could not be attributed to RD or RLD, resulting in a low predictive accuracy of these Hill curve models with a model efficiency of 0.11 and 0.17 for RD and RLD respectively. Considering root architecture and soil texture did yield a better predictive model for RLD with a model efficiency of 0.37 for fibrous roots in non-sandy soils while no improvement was found for RD. The unexplained variance is attributed to differences in experimental set-ups and measuring errors which could not be explicitly accounted for due to a lack of additional data. Based on those results, it remains difficult to predict the effects of roots on soil erosion rates. However, by using a Monte Carlo simulation approach, we were able to establish relationships that allow assessing the likely erosion-reducing effects of plant roots, while taking these uncertainties into account. Overall, this study demonstrates that plant roots can be very effective in reducing soil erosion rates due to concentrated flow. [Excerpt: Conclusions] Vegetation can be used to reduce soil degradation by soil erosion processes. This study showed that plant roots can be very effective in controlling soil erosion rates due to concentrated flow. A combination of a well-established vegetation cover together with a dense root system in the topsoil is therefore most effective and recommended to protect the soil against soil erosion processes by water. The erosion-reducing potential of plant roots can be explained by their indirect negative effect on soil erodibility through affecting various soil properties (e.g. aggregate stability, cohesion, organic matter content, infiltration rate and moisture content). However both the environment and management practices have to be taken into account as they influence the effectiveness of plant roots in reducing soil erosion rates. Analysis of a global dataset based on published data showed that the decrease in SDR as a function of RD or RLD could be best described by a Hill curve model. Root architecture and soil texture were further considered as an attempt to improve the models. This resulted in better predictive models for RLD (for fibrous roots in non-sandy soils) while no improvement could be observed for RD. Consequently, it remains difficult to predict the erosion-reducing effects of plant roots on concentrated flow erosion rates as still a large part of the variance remains unexplained. Results of the Monte Carlo analyses ( Fig. 5) present confidence intervals on estimated SDR values for the proposed models that should be used as an estimation of the uncertainty range. As such, the established relationships between root (length) density and the soil detachment ratio allow for meaningful estimations of the mechanical effects of plant roots on concentrated flow erosion rates. The advantage of this approach is that the results of this study can be extrapolated to different environments to examine the likely root effects on erosion rates, as we implicitly take into account the variability in root and soil characteristics. [\n] As tap root systems are less effective in controlling soil erosion compared to fibrous roots, we furthermore prefer the use of RLD as root variable as it indirectly takes into account the root architecture. The influence of soil texture on erosion-reducing potential could not be demonstrated due to a lack of sufficient data on the erosion-reducing potential of plant roots in different soil textures. More empirical studies are needed to examine the role of soil texture on the erosion-reducing potential. Moreover, a more accurate global database is needed to unravel the influence of additional soil, root and environmental variables on the erosion-reducing potential of plant roots and to improve the predictive quality of the models.
@article{vannoppenReviewMechanicalEffects2015,
title = {A Review of the Mechanical Effects of Plant Roots on Concentrated Flow Erosion Rates},
author = {Vannoppen, W. and Vanmaercke, M. and De Baets, S. and Poesen, J.},
date = {2015-11},
journaltitle = {Earth-Science Reviews},
volume = {150},
pages = {666--678},
issn = {0012-8252},
doi = {10.1016/j.earscirev.2015.08.011},
url = {https://doi.org/10.1016/j.earscirev.2015.08.011},
abstract = {Living plant roots modify both mechanical and hydrological characteristics of the soil matrix (e.g. soil aggregate stability by root exudates, soil cohesion, infiltration rate, soil moisture content, soil organic matter) and negatively influence the soil erodibility. During the last two decades several studies reported on the effects of plant roots in controlling concentrated flow erosion rates. However a global analysis of the now available data on root effects is still lacking. Yet, a meta-data analysis will contribute to a better understanding of the soil-root interactions as our capability to assess the effectiveness of roots in reducing soil erosion rates due to concentrated flow in different environments remains difficult. The objectives of this study are therefore: i) to provide a state of the art on studies quantifying the effectiveness of roots in reducing soil erosion rates due to concentrated flow; and ii) to explore the overall trends in erosion reduction as a function of the root (length) density, root architecture and soil texture, based on an integrated analysis of published data. We therefore compiled a dataset of measured soil detachment ratios (SDR) for the root density (RD; 822 observations) as well as for the root length density (RLD; 274 observations). A Hill curve model best describes the decrease in SDR as a function of R(L)D. An important finding of our meta-analysis is that RLD is a much more suitable variable to estimate SDR compared to RD as it is linked to root architecture. However, a large proportion of the variability in SDR could not be attributed to RD or RLD, resulting in a low predictive accuracy of these Hill curve models with a model efficiency of 0.11 and 0.17 for RD and RLD respectively. Considering root architecture and soil texture did yield a better predictive model for RLD with a model efficiency of 0.37 for fibrous roots in non-sandy soils while no improvement was found for RD. The unexplained variance is attributed to differences in experimental set-ups and measuring errors which could not be explicitly accounted for due to a lack of additional data. Based on those results, it remains difficult to predict the effects of roots on soil erosion rates. However, by using a Monte Carlo simulation approach, we were able to establish relationships that allow assessing the likely erosion-reducing effects of plant roots, while taking these uncertainties into account. Overall, this study demonstrates that plant roots can be very effective in reducing soil erosion rates due to concentrated flow.
[Excerpt: Conclusions]
Vegetation can be used to reduce soil degradation by soil erosion processes. This study showed that plant roots can be very effective in controlling soil erosion rates due to concentrated flow. A combination of a well-established vegetation cover together with a dense root system in the topsoil is therefore most effective and recommended to protect the soil against soil erosion processes by water. The erosion-reducing potential of plant roots can be explained by their indirect negative effect on soil erodibility through affecting various soil properties (e.g. aggregate stability, cohesion, organic matter content, infiltration rate and moisture content). However both the environment and management practices have to be taken into account as they influence the effectiveness of plant roots in reducing soil erosion rates. Analysis of a global dataset based on published data showed that the decrease in SDR as a function of RD or RLD could be best described by a Hill curve model. Root architecture and soil texture were further considered as an attempt to improve the models. This resulted in better predictive models for RLD (for fibrous roots in non-sandy soils) while no improvement could be observed for RD. Consequently, it remains difficult to predict the erosion-reducing effects of plant roots on concentrated flow erosion rates as still a large part of the variance remains unexplained. Results of the Monte Carlo analyses ( Fig. 5) present confidence intervals on estimated SDR values for the proposed models that should be used as an estimation of the uncertainty range. As such, the established relationships between root (length) density and the soil detachment ratio allow for meaningful estimations of the mechanical effects of plant roots on concentrated flow erosion rates. The advantage of this approach is that the results of this study can be extrapolated to different environments to examine the likely root effects on erosion rates, as we implicitly take into account the variability in root and soil characteristics.
[\textbackslash n] As tap root systems are less effective in controlling soil erosion compared to fibrous roots, we furthermore prefer the use of RLD as root variable as it indirectly takes into account the root architecture. The influence of soil texture on erosion-reducing potential could not be demonstrated due to a lack of sufficient data on the erosion-reducing potential of plant roots in different soil textures. More empirical studies are needed to examine the role of soil texture on the erosion-reducing potential. Moreover, a more accurate global database is needed to unravel the influence of additional soil, root and environmental variables on the erosion-reducing potential of plant roots and to improve the predictive quality of the models.},
keywords = {*imported-from-citeulike-INRMM,~INRMM-MiD:c-13794980,~to-add-doi-URL,boreal-forests,comparison,eucalyptus-citriodora,forest-resources,macchia,modelling,pinus-tabulaeformis,review,robinia-pseudoacacia,sclerophyllous,soil-erosion,soil-resources,stabilization,uncertainty,vegetation}
}
Social Reference: Aggregating Online Usage of Scientific Literature in CiteULike for Clustering Academic Resources. Jiang, J., He, D., & Ni, C. In Proceedings of the 11th Annual International ACM/IEEE Joint Conference on Digital Libraries, of JCDL '11, pages 401–402. ACM. Paper doi abstract bibtex Citation-based methods have been widely studied and employed for clustering academic resources and mapping science. Although effective, these methods suffer from citation delay. In this study, we extend reference and citation analysis to a broader notion from social perspective. We coin the term "social reference" to refer to the references of literatures in social academic web environment. We propose clustering methods using social reference information from CiteULike. We experiment for journal clustering and author clustering using social reference and compare with citation-based methods. Our experiments indicate: first, social reference implies connections among literatures which are as effective as citation in clustering academic resources; second, in practical settings, social reference-based clustering methods are not as effective as citation-based ones due to the sparseness of social reference data, but they can outperform in clustering new resources that have few citation.
@inproceedings{jiangSocialReferenceAggregating2011,
title = {Social Reference: Aggregating Online Usage of Scientific Literature in {{CiteULike}} for Clustering Academic Resources},
booktitle = {Proceedings of the 11th Annual International {{ACM}}/{{IEEE}} Joint Conference on {{Digital}} Libraries},
author = {Jiang, Jiepu and He, Daqing and Ni, Chaoqun},
date = {2011},
pages = {401--402},
publisher = {{ACM}},
doi = {10.1145/1998076.1998155},
url = {https://doi.org/10.1145/1998076.1998155},
abstract = {Citation-based methods have been widely studied and employed for clustering academic resources and mapping science. Although effective, these methods suffer from citation delay. In this study, we extend reference and citation analysis to a broader notion from social perspective. We coin the term "social reference" to refer to the references of literatures in social academic web environment. We propose clustering methods using social reference information from CiteULike. We experiment for journal clustering and author clustering using social reference and compare with citation-based methods. Our experiments indicate: first, social reference implies connections among literatures which are as effective as citation in clustering academic resources; second, in practical settings, social reference-based clustering methods are not as effective as citation-based ones due to the sparseness of social reference data, but they can outperform in clustering new resources that have few citation.},
isbn = {978-1-4503-0744-4},
keywords = {*imported-from-citeulike-INRMM,~INRMM-MiD:c-10600782,~to-add-doi-URL,citeulike,clustering,metadata,metaknowledge,scientific-communication,scientific-knowledge-sharing,wiki-communication},
series = {{{JCDL}} '11},
venue = {Ottawa, Ontario, Canada}
}
Climatic Discrimination of Mediterranean Broad‐leaved Sclerophyllous and Deciduous Forests in Central Spain. Gavilán, R. & Fernández-González, F. 8(3):377–386. Paper doi abstract bibtex Climatic differences between three types of deciduous (Quercus pyrenaica) and three types of sclerophyllous (Quercus rotundifolia) Mediterranean forests in the Spanish Sistema Central were analyzed by means of Canonical Discriminant Analysis and Jancey's Discriminant Analysis, applied in successive steps to data from 252 meteorological stations. Climatic data included temperature and precipitation records as well as bioclimatic indices. Discriminant analysis was applied to broad-leaved sclerophyllous and deciduous forest communities sampled at each meteorological station using phytosociological methods. Annual and seasonal (summer, spring) water availability are the most important factor controlling the distribution of the two physiognomic forest types; southwestern associations of Quercus pyrenaica and Q. rotundifolia differ from their colder homologues by annual and monthly temperatures; western associations were separated from eastern ones in terms of annual and seasonal precipitation gradients. Discriminant analysis was a good technique to explore climatic gradients not shown by other general ordination or classification methods.
@article{gavilanClimaticDiscriminationMediterranean1997,
title = {Climatic Discrimination of {{Mediterranean}} Broad‐leaved Sclerophyllous and Deciduous Forests in Central {{Spain}}},
author = {Gavilán, Rosario and Fernández-González, Federico},
date = {1997-06},
journaltitle = {Journal of Vegetation Science},
volume = {8},
pages = {377--386},
doi = {10.2307/3237327},
url = {https://doi.org/10.2307/3237327},
abstract = {Climatic differences between three types of deciduous (Quercus pyrenaica) and three types of sclerophyllous (Quercus rotundifolia) Mediterranean forests in the Spanish Sistema Central were analyzed by means of Canonical Discriminant Analysis and Jancey's Discriminant Analysis, applied in successive steps to data from 252 meteorological stations. Climatic data included temperature and precipitation records as well as bioclimatic indices. Discriminant analysis was applied to broad-leaved sclerophyllous and deciduous forest communities sampled at each meteorological station using phytosociological methods. Annual and seasonal (summer, spring) water availability are the most important factor controlling the distribution of the two physiognomic forest types; southwestern associations of Quercus pyrenaica and Q. rotundifolia differ from their colder homologues by annual and monthly temperatures; western associations were separated from eastern ones in terms of annual and seasonal precipitation gradients. Discriminant analysis was a good technique to explore climatic gradients not shown by other general ordination or classification methods.},
keywords = {*imported-from-citeulike-INRMM,~INRMM-MiD:c-13559286,~to-add-doi-URL,broadleaved,forest-classification,forest-resources,forest-types,mediterranean-region,spain},
number = {3}
}
Well below 2 °C: Mitigation Strategies for Avoiding Dangerous to Catastrophic Climate Changes. Xu, Y. & Ramanathan, V. 114(39):10315–10323. Paper doi abstract bibtex The historic Paris Agreement calls for limiting global temperature rise to ” well below 2 °C.” Because of uncertainties in emission scenarios, climate, and carbon cycle feedback, we interpret the Paris Agreement in terms of three climate risk categories and bring in considerations of low-probability (5\,%) high-impact (LPHI) warming in addition to the central (∼50\,% probability) value. The current risk category of dangerous warming is extended to more categories, which are defined by us here as follows: $>$1.5 °C as dangerous; $>$3 °C as catastrophic; and $>$5 °C as unknown, implying beyond catastrophic, including existential threats. With unchecked emissions, the central warming can reach the dangerous level within three decades, with the LPHI warming becoming catastrophic by 2050. We outline a three-lever strategy to limit the central warming below the dangerous level and the LPHI below the catastrophic level, both in the near term ($<$2050) and in the long term (2100): the carbon neutral (CN) lever to achieve zero net emissions of CO2, the super pollutant (SP) lever to mitigate short-lived climate pollutants, and the carbon extraction and sequestration (CES) lever to thin the atmospheric CO2 blanket. Pulling on both CN and SP levers and bending the emissions curve by 2020 can keep the central warming below dangerous levels. To limit the LPHI warming below dangerous levels, the CES lever must be pulled as well to extract as much as 1 trillion tons of CO2 before 2100 to both limit the preindustrial to 2100 cumulative net CO2 emissions to 2.2 trillion tons and bend the warming curve to a cooling trend. [Excerpt: Summary] Basically, for a safe climate, all three levers (CN, SP, and CES) must be deployed as soon as possible. The CN and SP levers must be deployed by 2030 and 2020, respectively; the cumulative CO2 emissions from preindustrial must be limited to 2.2 trillion tons of CO2 (or 0.6 trillion tons of carbon); and the CES lever should extract and sequester as much as 1 trillion tons of CO2 (CES1t), depending on when the CN lever is deployed. If the CN lever is deployed as early as 2020, the required CES is much less than 1 trillion tons. [] We propose that mitigation goals be set in terms of climate risk category instead of a temperature threshold. In this paper, we offer three broad risk categories, but it is likely that a more granular set of categories is required. The temperature threshold has served policy very well; however, given the imminence of dangerous warming within decades, the focus must broaden to include extreme climate changes. Precipitation, flooding, fire, and drought will all become serious sources of concern. The temperature will still occupy our attention because of the heat stress phenomenon and the likelihood of approximately half of the population exposed to deadly heat by 2050 (Box 2). [] We conclude with a commentary on the feasibility of the mitigation options considered thus far. Over 24 technological measures to reduce SLCPs have been detailed previously (39) (details are provided in SI Appendix). These measures include providing clean cook stoves to the poorest three billion of the world's total population and installing particulate filters in all diesel vehicles to reduce global BC emissions by nearly 80\,% and also reduce air pollution-related mortalities by ∼2 million; routine maintenance of gas pipes and banning gas flaring to reduce methane leaks; recovering methane from landfills, water sewage treatment plants, and farm manure; replacing HFCs with other available refrigerants that have negligible greenhouse effects; and installing catalytic converters in vehicles to reduce emissions of ozone precursors. [] CN levers require switching from fossil fuels to renewables such as wind, solar, geothermal and nuclear sources, among others. Also, CO2 emissions from industrial processes should be eliminated. This requires electrification of all end uses and production of electricity from renewables (40). Since many renewables (solar and wind) are intermittent, storage is a crucial issue. Batteries, hydrogen production by renewables, and pumped hydropower are all possible options for storage. While about 50\,% of reductions are possible with scaling up of existing technologies, innovations are required for achieving carbon neutrality in a cost-effective manner (40). Achievement of carbon neutrality also requires societal transformation, governance, and market mechanisms such as cap and trade and carbon pricing (40). The encouraging sign is that 52 cities, 65 businesses, and numerous universities have already embarked on the CN pathway (41). Some of these living laboratories, like California and Stockholm, have shown that the gross domestic product (GDP) can be decoupled from carbon emissions. Their carbon emission per GDP has decreased by 20\,% while bending the carbon emissions curve. The technology development and innovations from these living laboratories should be scaled to the world to greatly accelerate efforts to achieve CN within decades. [] Of the three levers recommended here, the third lever dealing with CES is the most challenging and formidable due to lack of scalable technologies. However, many technologies are being explored, including capturing CO2 in bioenergy power plants (42), biochar production by pyrolysis and storage in soils (43), restoration of soil organic pools (44), chemical weathering of rocks, mineral sequestration, reforestation, and urban forestry, among others. The availability of land and conflict with food production is another important constraint in some of the CES solutions. Major breakthroughs are needed urgently, and in the meantime, the best option is to start on the CN goal by 2020 and mitigate the SPs as soon as possible, since cost-effective technologies are already present to immediately start bending the emission curves.
@article{xuWellMitigationStrategies2017,
title = {Well below 2 °{{C}}: Mitigation Strategies for Avoiding Dangerous to Catastrophic Climate Changes},
author = {Xu, Yangyang and Ramanathan, Veerabhadran},
date = {2017-09},
journaltitle = {Proceedings of the National Academy of Sciences},
volume = {114},
pages = {10315--10323},
issn = {1091-6490},
doi = {10.1073/pnas.1618481114},
url = {https://doi.org/10.1073/pnas.1618481114},
abstract = {The historic Paris Agreement calls for limiting global temperature rise to ” well below 2 °C.” Because of uncertainties in emission scenarios, climate, and carbon cycle feedback, we interpret the Paris Agreement in terms of three climate risk categories and bring in considerations of low-probability (5\,\%) high-impact (LPHI) warming in addition to the central (∼50\,\% probability) value. The current risk category of dangerous warming is extended to more categories, which are defined by us here as follows: {$>$}1.5 °C as dangerous; {$>$}3 °C as catastrophic; and {$>$}5 °C as unknown, implying beyond catastrophic, including existential threats. With unchecked emissions, the central warming can reach the dangerous level within three decades, with the LPHI warming becoming catastrophic by 2050. We outline a three-lever strategy to limit the central warming below the dangerous level and the LPHI below the catastrophic level, both in the near term ({$<$}2050) and in the long term (2100): the carbon neutral (CN) lever to achieve zero net emissions of CO2, the super pollutant (SP) lever to mitigate short-lived climate pollutants, and the carbon extraction and sequestration (CES) lever to thin the atmospheric CO2 blanket. Pulling on both CN and SP levers and bending the emissions curve by 2020 can keep the central warming below dangerous levels. To limit the LPHI warming below dangerous levels, the CES lever must be pulled as well to extract as much as 1 trillion tons of CO2 before 2100 to both limit the preindustrial to 2100 cumulative net CO2 emissions to 2.2 trillion tons and bend the warming curve to a cooling trend.
[Excerpt: Summary] Basically, for a safe climate, all three levers (CN, SP, and CES) must be deployed as soon as possible. The CN and SP levers must be deployed by 2030 and 2020, respectively; the cumulative CO2 emissions from preindustrial must be limited to 2.2 trillion tons of CO2 (or 0.6 trillion tons of carbon); and the CES lever should extract and sequester as much as 1 trillion tons of CO2 (CES1t), depending on when the CN lever is deployed. If the CN lever is deployed as early as 2020, the required CES is much less than 1 trillion tons.
[] We propose that mitigation goals be set in terms of climate risk category instead of a temperature threshold. In this paper, we offer three broad risk categories, but it is likely that a more granular set of categories is required. The temperature threshold has served policy very well; however, given the imminence of dangerous warming within decades, the focus must broaden to include extreme climate changes. Precipitation, flooding, fire, and drought will all become serious sources of concern. The temperature will still occupy our attention because of the heat stress phenomenon and the likelihood of approximately half of the population exposed to deadly heat by 2050 (Box 2).
[] We conclude with a commentary on the feasibility of the mitigation options considered thus far. Over 24 technological measures to reduce SLCPs have been detailed previously (39) (details are provided in SI Appendix). These measures include providing clean cook stoves to the poorest three billion of the world's total population and installing particulate filters in all diesel vehicles to reduce global BC emissions by nearly 80\,\% and also reduce air pollution-related mortalities by ∼2 million; routine maintenance of gas pipes and banning gas flaring to reduce methane leaks; recovering methane from landfills, water sewage treatment plants, and farm manure; replacing HFCs with other available refrigerants that have negligible greenhouse effects; and installing catalytic converters in vehicles to reduce emissions of ozone precursors.
[] CN levers require switching from fossil fuels to renewables such as wind, solar, geothermal and nuclear sources, among others. Also, CO2 emissions from industrial processes should be eliminated. This requires electrification of all end uses and production of electricity from renewables (40). Since many renewables (solar and wind) are intermittent, storage is a crucial issue. Batteries, hydrogen production by renewables, and pumped hydropower are all possible options for storage. While about 50\,\% of reductions are possible with scaling up of existing technologies, innovations are required for achieving carbon neutrality in a cost-effective manner (40). Achievement of carbon neutrality also requires societal transformation, governance, and market mechanisms such as cap and trade and carbon pricing (40). The encouraging sign is that 52 cities, 65 businesses, and numerous universities have already embarked on the CN pathway (41). Some of these living laboratories, like California and Stockholm, have shown that the gross domestic product (GDP) can be decoupled from carbon emissions. Their carbon emission per GDP has decreased by 20\,\% while bending the carbon emissions curve. The technology development and innovations from these living laboratories should be scaled to the world to greatly accelerate efforts to achieve CN within decades.
[] Of the three levers recommended here, the third lever dealing with CES is the most challenging and formidable due to lack of scalable technologies. However, many technologies are being explored, including capturing CO2 in bioenergy power plants (42), biochar production by pyrolysis and storage in soils (43), restoration of soil organic pools (44), chemical weathering of rocks, mineral sequestration, reforestation, and urban forestry, among others. The availability of land and conflict with food production is another important constraint in some of the CES solutions. Major breakthroughs are needed urgently, and in the meantime, the best option is to start on the CN goal by 2020 and mitigate the SPs as soon as possible, since cost-effective technologies are already present to immediately start bending the emission curves.},
keywords = {*imported-from-citeulike-INRMM,~INRMM-MiD:c-14438775,~to-add-doi-URL,adaptation,carbon-capture-and-storage,carbon-emissions,carbon-mitigation,climate-change,global-scale,mitigation,pollution,system-catastrophe},
number = {39}
}
Enhanced Poleward Propagation of Storms under Climate Change. Tamarin-Brodsky, T. & Kaspi, Y. Paper doi abstract bibtex Earth's midlatitudes are dominated by regions of large atmospheric weather variability – often referred to as storm tracks – which influence the distribution of temperature, precipitation and wind in the extratropics. Comprehensive climate models forced by increased greenhouse gas emissions suggest that under global warming the storm tracks shift poleward. While the poleward shift is a robust response across most models, there is currently no consensus on what the underlying dynamical mechanism is. Here we present a new perspective on the poleward shift, which is based on a Lagrangian view of the storm tracks. We show that in addition to a poleward shift in the genesis latitude of the storms, associated with the shift in baroclinicity, the latitudinal displacement of cyclonic storms increases under global warming. This is achieved by applying a storm-tracking algorithm to an ensemble of CMIP5 models. The increased latitudinal propagation in a warmer climate is shown to be a result of stronger upper-level winds and increased atmospheric water vapour. These changes in the propagation characteristics of the storms can have a significant impact on midlatitude climate.
@article{tamarin-brodskyEnhancedPolewardPropagation2017,
title = {Enhanced Poleward Propagation of Storms under Climate Change},
author = {Tamarin-Brodsky, Talia and Kaspi, Yohai},
date = {2017-11},
journaltitle = {Nature Geoscience},
issn = {1752-0894},
doi = {10.1038/s41561-017-0001-8},
url = {https://doi.org/10.1038/s41561-017-0001-8},
abstract = {Earth's midlatitudes are dominated by regions of large atmospheric weather variability -- often referred to as storm tracks -- which influence the distribution of temperature, precipitation and wind in the extratropics. Comprehensive climate models forced by increased greenhouse gas emissions suggest that under global warming the storm tracks shift poleward. While the poleward shift is a robust response across most models, there is currently no consensus on what the underlying dynamical mechanism is. Here we present a new perspective on the poleward shift, which is based on a Lagrangian view of the storm tracks. We show that in addition to a poleward shift in the genesis latitude of the storms, associated with the shift in baroclinicity, the latitudinal displacement of cyclonic storms increases under global warming. This is achieved by applying a storm-tracking algorithm to an ensemble of CMIP5 models. The increased latitudinal propagation in a warmer climate is shown to be a result of stronger upper-level winds and increased atmospheric water vapour. These changes in the propagation characteristics of the storms can have a significant impact on midlatitude climate.},
keywords = {*imported-from-citeulike-INRMM,~INRMM-MiD:c-14476167,~to-add-doi-URL,climate-change,cyclone,global-scale,precipitation,rcp85,storm,wind}
}
The Population Dynamics of Microparasites and Their Invertebrate Hosts. Anderson, R. M. & May, R. M. 291(1054):451–524. Paper doi abstract bibtex We show how directly transmitted microparasites, broadly defined to include viruses, bacteria, protozoans and fungi, may regulate natural populations of invertebrate hosts. The study combines elements of conventional epidemiology (where the host population is assumed constant) with elements of prey-predator studies (which conventionally emphasize how prey and predator populations may be regulated by their interaction). To this end, we construct simple models embodying the essentials of the dynamical interaction between invertebrate hosts and their directly transmitted microparasites. In successive refinements, these models include the effects of recovery and disease-induced mortality, castration or diminished reproduction of infected hosts, vertical transmission, latent periods of infection, stress-related pathogenicity, the interplay between disease and other density-dependent constraints on host population growth, and free-living infective stages. In analysing the dynamical behaviour of these models, we focus on : the possible regulation of the host population by the parasite; the basic reproductive rate of the parasite, and the way in which it affects the dynamics and the evolution of the host-parasite association; and the threshold host density and its implications for endemic or epidemic maintenance of the infection. These are examined in the light of synoptic compilations of field and laboratory data on: birth rates (and disease-induced reduction thereof), natural death rates and disease-induced death rates of hosts; latent periods and efficiencies of vertical transmission of pathogens; the rate of production and lifetime of free-living infective stages; and some characteristics of long-term cycles and of epidemic outbreaks of disease in forest insects. In particular, our models suggest that the baculovirus and microsporidian infections of many temperate forest insects will tend to produce stable cycles in host abundance and in prevalence of infection, with periods in the range 5-12 years. Enough is known about the European larch budmoth and an associated granulosis virus for us to undertake a detailed comparison between theory and data that strongly suggests that the observed 9-10 year cycles are driven by the host-parasite interaction. We also discuss the possible control of invertebrate pest species by pathogens, showing how our models could guide laboratory or field studies, to help estimate whether a given pathogen is capable of regulating the target pest population, and, if so, roughly what quantity is needed to effect a specific level of (local) control. Throughout, the emphasis is on the biological ingredients of the models, and on the biological conclusions to be drawn; mathematical details are given in appendixes.
@article{andersonPopulationDynamicsMicroparasites1981,
title = {The Population Dynamics of Microparasites and Their Invertebrate Hosts},
author = {Anderson, R. M. and May, R. M.},
date = {1981-04},
journaltitle = {Philosophical Transactions of the Royal Society B: Biological Sciences},
volume = {291},
pages = {451--524},
issn = {0962-8436},
doi = {10.1098/rstb.1981.0005},
url = {http://mfkp.org/INRMM/article/14479954},
abstract = {We show how directly transmitted microparasites, broadly defined to include viruses, bacteria, protozoans and fungi, may regulate natural populations of invertebrate hosts. The study combines elements of conventional epidemiology (where the host population is assumed constant) with elements of prey-predator studies (which conventionally emphasize how prey and predator populations may be regulated by their interaction). To this end, we construct simple models embodying the essentials of the dynamical interaction between invertebrate hosts and their directly transmitted microparasites. In successive refinements, these models include the effects of recovery and disease-induced mortality, castration or diminished reproduction of infected hosts, vertical transmission, latent periods of infection, stress-related pathogenicity, the interplay between disease and other density-dependent constraints on host population growth, and free-living infective stages. In analysing the dynamical behaviour of these models, we focus on : the possible regulation of the host population by the parasite; the basic reproductive rate of the parasite, and the way in which it affects the dynamics and the evolution of the host-parasite association; and the threshold host density and its implications for endemic or epidemic maintenance of the infection. These are examined in the light of synoptic compilations of field and laboratory data on: birth rates (and disease-induced reduction thereof), natural death rates and disease-induced death rates of hosts; latent periods and efficiencies of vertical transmission of pathogens; the rate of production and lifetime of free-living infective stages; and some characteristics of long-term cycles and of epidemic outbreaks of disease in forest insects. In particular, our models suggest that the baculovirus and microsporidian infections of many temperate forest insects will tend to produce stable cycles in host abundance and in prevalence of infection, with periods in the range 5-12 years. Enough is known about the European larch budmoth and an associated granulosis virus for us to undertake a detailed comparison between theory and data that strongly suggests that the observed 9-10 year cycles are driven by the host-parasite interaction. We also discuss the possible control of invertebrate pest species by pathogens, showing how our models could guide laboratory or field studies, to help estimate whether a given pathogen is capable of regulating the target pest population, and, if so, roughly what quantity is needed to effect a specific level of (local) control. Throughout, the emphasis is on the biological ingredients of the models, and on the biological conclusions to be drawn; mathematical details are given in appendixes.},
keywords = {*imported-from-citeulike-INRMM,~INRMM-MiD:c-14479954,~to-add-doi-URL,100-ecology-articles,bacteria,dynamic-system,fungi,high-impact-publication,host-parasite,invertebrates,parasite,protozoans,virus},
number = {1054}
}
Flood Plains: Critically Threatened Ecosystems. Tockner, K., Bunn, S. E., Gordon, C., Naiman, R. J., Quinn, G. P., & Stanford, J. A. In Aquatic Ecosystems, pages 45–62. Cambridge University Press. Paper doi abstract bibtex [Excerpt: Introduction] Riparian zones, river-marginal wetland environments and flood plains are key landscape elements with a high diversity of natural functions and services. They are dynamic systems that are shaped by repeated erosion and deposition of sediment, inundation during rising water levels, and complex groundwater-surface water exchange processes (Chapter 3). This dynamic nature makes flood plains among the most biologically productive and diverse ecosystems on earth [...]. Flood plains are also of great cultural and economic importance; most early civilizations arose in fertile flood plains and throughout history people have learned to cultivate and use their rich resources. Flood plains have also served as focal points for urban development and exploitation of their natural functions. [\n] Awareness has been growing during the past decade of the global significance of freshwater biodiversity, of the array of factors that have (or will have) threatened it and the extent to which real damage has already been done [...]. Flood plains in particular have been highly degraded throughout the world by river and flow management and by land-use pressures. Nowadays, they are among the most endangered ecosystems worldwide [...]. Accordingly, flood plains deserve increased attention for their inherent biodiversity, for the goods and services provided to human societies and for their aesthetic and cultural appeal. [\n] This chapter builds upon a recent comprehensive environmental review of riverine flood plains [...]. It starts with a short summary of the distribution and extent of the world's flood plains, followed by an overview of their primary economic, ecological and cultural values. The multifaceted threats that make flood plains one of the most endangered landscape elements worldwide are then discussed. Finally, future trends in floodplain exploitation in developing and developed countries are contrasted, and the ecological consequences of rapid alteration of floodplain ecosystems forecasted. Since flood plains, wetlands and river systems are not always clearly distinguished, general examples of rivers or floodplain wetlands are included in the present review when appropriate. The flood-inundated wetlands and lakes of the humid tropics are treated in more detail later (Chapter 10). [\n] [...] [Flood plain distribution] Flood plains are defined as 'areas of low lying land that are subject to inundation by lateral overflow water from rivers or lakes with which they are associated' [...]. This definition includes fringing flood plains of lakes and rivers, internal deltas and the deltaic flood plains of estuaries. [\n] [...] Based on data from 145 major river corridors around the world, the extent of human impacts on riparian zones is apparent [...]. For example, 11\,% of the riparian area of African rivers (mean population density 24 people km2) is intensively cultivated, compared to 46\,% for North American rivers (mean population density, excluding northern Canada and Alaska, 24 people km2) and 79\,% for European rivers (mean population density 75 people km2). The most impacted riparian corridors with respect to land use are found in Europe and in the densely populated areas of Asia (catchments with population densities $>$200 people km2) [...]. There, 60-99\,% of the entire riparian corridor has been transformed into cropland and/or is urbanized, the latter particularly so in Europe, where the Seine River (France) shows the highest impact of all rivers investigated. [\n] [...] The current situation for European flood plains is critical [...] with 95\,% of the original floodplain area converted to other uses [...]. In 45 European countries, 88\,% of alluvial forests have disappeared from their potential range [...]. Many of the remaining European flood plains are far from pristine and have lost most of their natural functions. For example, of the former 26 000 km2 of floodplain area along the Danube and its major tributaries, about 20 000 km2 are isolated by levees [...]. However, major flood events have highlighted the vast extent of plains still subject to flooding [...]. [\n] [...] [Conclusions] Flood plains are unique and dynamic ecosystems that link rivers with their catchments. They are highly productive environments, supporting a diverse biota, but are also intensively used by humans for agricultural and urban development, resulting in loss of biodiversity and ecological functioning. The priority for flood plains is to conserve those that are still intact and to attempt to rehabilitate those that are degraded. In both cases, protecting or restoring key components of the natural flow regime is essential, while maintaining sustainable use of floodplain resources by local communities, particularly in developing countries. Finding this compromise between conservation and resource use requires a greater understanding of the role of flow relative to other stressors in driving ecological processes in flood plains. Floodplain management and restoration strategies must also take into account climate change models that predict significant changes to flow regimes in most of the world's rivers, especially in temperate and arid regions.
@incollection{tocknerFloodPlainsCritically2008,
title = {Flood Plains: Critically Threatened Ecosystems},
booktitle = {Aquatic {{Ecosystems}}},
author = {Tockner, Klement and Bunn, Stuart E. and Gordon, Christopher and Naiman, Robert J. and Quinn, Gerry P. and Stanford, Jack A.},
editor = {Polunin, Nicholas V. C.},
date = {2008},
pages = {45--62},
publisher = {{Cambridge University Press}},
location = {{Cambridge}},
doi = {10.1017/cbo9780511751790.006},
url = {https://doi.org/10.1017/cbo9780511751790.006},
abstract = {[Excerpt: Introduction]
Riparian zones, river-marginal wetland environments and flood plains are key landscape elements with a high diversity of natural functions and services. They are dynamic systems that are shaped by repeated erosion and deposition of sediment, inundation during rising water levels, and complex groundwater-surface water exchange processes (Chapter 3). This dynamic nature makes flood plains among the most biologically productive and diverse ecosystems on earth [...]. Flood plains are also of great cultural and economic importance; most early civilizations arose in fertile flood plains and throughout history people have learned to cultivate and use their rich resources. Flood plains have also served as focal points for urban development and exploitation of their natural functions.
[\textbackslash n] Awareness has been growing during the past decade of the global significance of freshwater biodiversity, of the array of factors that have (or will have) threatened it and the extent to which real damage has already been done [...]. Flood plains in particular have been highly degraded throughout the world by river and flow management and by land-use pressures. Nowadays, they are among the most endangered ecosystems worldwide [...]. Accordingly, flood plains deserve increased attention for their inherent biodiversity, for the goods and services provided to human societies and for their aesthetic and cultural appeal.
[\textbackslash n] This chapter builds upon a recent comprehensive environmental review of riverine flood plains [...]. It starts with a short summary of the distribution and extent of the world's flood plains, followed by an overview of their primary economic, ecological and cultural values. The multifaceted threats that make flood plains one of the most endangered landscape elements worldwide are then discussed. Finally, future trends in floodplain exploitation in developing and developed countries are contrasted, and the ecological consequences of rapid alteration of floodplain ecosystems forecasted. Since flood plains, wetlands and river systems are not always clearly distinguished, general examples of rivers or floodplain wetlands are included in the present review when appropriate. The flood-inundated wetlands and lakes of the humid tropics are treated in more detail later (Chapter 10).
[\textbackslash n] [...]
[Flood plain distribution]
Flood plains are defined as 'areas of low lying land that are subject to inundation by lateral overflow water from rivers or lakes with which they are associated' [...]. This definition includes fringing flood plains of lakes and rivers, internal deltas and the deltaic flood plains of estuaries. [\textbackslash n] [...]
Based on data from 145 major river corridors around the world, the extent of human impacts on riparian zones is apparent [...]. For example, 11\,\% of the riparian area of African rivers (mean population density 24 people km2) is intensively cultivated, compared to 46\,\% for North American rivers (mean population density, excluding northern Canada and Alaska, 24 people km2) and 79\,\% for European rivers (mean population density 75 people km2). The most impacted riparian corridors with respect to land use are found in Europe and in the densely populated areas of Asia (catchments with population densities {$>$}200 people km2) [...]. There, 60-99\,\% of the entire riparian corridor has been transformed into cropland and/or is urbanized, the latter particularly so in Europe, where the Seine River (France) shows the highest impact of all rivers investigated.
[\textbackslash n] [...]
The current situation for European flood plains is critical [...] with 95\,\% of the original floodplain area converted to other uses [...]. In 45 European countries, 88\,\% of alluvial forests have disappeared from their potential range [...]. Many of the remaining European flood plains are far from pristine and have lost most of their natural functions. For example, of the former 26 000 km2 of floodplain area along the Danube and its major tributaries, about 20 000 km2 are isolated by levees [...]. However, major flood events have highlighted the vast extent of plains still subject to flooding [...].
[\textbackslash n] [...]
[Conclusions]
Flood plains are unique and dynamic ecosystems that link rivers with their catchments. They are highly productive environments, supporting a diverse biota, but are also intensively used by humans for agricultural and urban development, resulting in loss of biodiversity and ecological functioning. The priority for flood plains is to conserve those that are still intact and to attempt to rehabilitate those that are degraded. In both cases, protecting or restoring key components of the natural flow regime is essential, while maintaining sustainable use of floodplain resources by local communities, particularly in developing countries. Finding this compromise between conservation and resource use requires a greater understanding of the role of flow relative to other stressors in driving ecological processes in flood plains. Floodplain management and restoration strategies must also take into account climate change models that predict significant changes to flow regimes in most of the world's rivers, especially in temperate and arid regions.},
isbn = {978-0-511-75179-0},
keywords = {*imported-from-citeulike-INRMM,~INRMM-MiD:c-13938341,~to-add-doi-URL,anthropogenic-changes,arid-climate,climate-change,ecosystem,flood-frequency,flooding-tolerance,floods,forest-resources,river-flow,temperate-climate,vegetation,water-resources}
}
A Data Citation Roadmap for Scientific Publishers. Cousijn, H., Kenall, A., Ganley, E., Harrison, M., Kernohan, D., Murphy, F., Polischuk, P., Martone, M., & Clark, T. Paper doi abstract bibtex This article presents a practical roadmap for scholarly publishers to implement data citation in accordance with the Joint Declaration of Data Citation Principles (JDDCP) [1], a synopsis and harmonization of the recommendations of major science policy bodies. It was developed by the Publishers Early Adopters Expert Group as part of the Data Citation Implementation Pilot (DCIP) project, an initiative of FORCE11.org and the NIH BioCADDIE program. The structure of the roadmap presented here follows the ” life of a paper” workflow and includes the categories Pre-submission, Submission, Production, and Publication. The roadmap is intended to be publisher-agnostic so that all publishers can use this as a starting point when implementing JDDCP-compliant data citation.
@article{cousijnDataCitationRoadmap2017,
title = {A Data Citation Roadmap for Scientific Publishers},
author = {Cousijn, Helena and Kenall, Amye and Ganley, Emma and Harrison, Melissa and Kernohan, David and Murphy, Fiona and Polischuk, Patrick and Martone, Maryann and Clark, Timothy},
date = {2017-01},
journaltitle = {bioRxiv},
pages = {100784+},
doi = {10.1101/100784},
url = {https://doi.org/10.1101/100784},
abstract = {This article presents a practical roadmap for scholarly publishers to implement data citation in accordance with the Joint Declaration of Data Citation Principles (JDDCP) [1], a synopsis and harmonization of the recommendations of major science policy bodies. It was developed by the Publishers Early Adopters Expert Group as part of the Data Citation Implementation Pilot (DCIP) project, an initiative of FORCE11.org and the NIH BioCADDIE program. The structure of the roadmap presented here follows the ” life of a paper” workflow and includes the categories Pre-submission, Submission, Production, and Publication. The roadmap is intended to be publisher-agnostic so that all publishers can use this as a starting point when implementing JDDCP-compliant data citation.},
keywords = {*imported-from-citeulike-INRMM,~INRMM-MiD:c-14270950,~to-add-doi-URL,check-list,citation-metrics,open-data,open-science,research-funding-vs-public-outcome,research-metrics,rewarding-best-research-practices}
}
Soil Degradation and Soil Quality in Western Europe: Current Situation and Future Perspectives. Virto, I., Imaz, M., Fernández-Ugalde, O., Gartzia-Bengoetxea, N., Enrique, A., & Bescansa, P. 7(1):313–365. Paper doi abstract bibtex The extent and causes of chemical, physical and biological degradation of soil, and of soil loss, vary greatly in different countries in Western Europe. The objective of this review paper is to examine these issues and also strategies for soil protection and future perspectives for soil quality evaluation, in light of present legislation aimed at soil protection. Agriculture and forestry are the main causes of many of the above problems, especially physical degradation, erosion and organic matter loss. Land take and soil sealing have increased in recent decades, further enhancing the problems. In agricultural land, conservation farming, organic farming and other soil-friendly practices have been seen to have site-specific effects, depending on the soil characteristics and the particular types of land use and land users. No single soil management strategy is suitable for all regions, soil types and soil uses. Except for soil contamination, specific legislation for soil protection is lacking in Western Europe. The Thematic Strategy for Soil Protection in the European Union has produced valuable information and has encouraged the development of networks and databases. However, soil degradation is addressed only indirectly in environmental policies and through the Common Agricultural Policy of the European Union, which promotes farming practices that support soil conservation. Despite these efforts, there remains a need for soil monitoring networks and decision-support systems aimed at optimization of soil quality in the region. The pressure on European soils will continue in the future, and a clearly defined regulatory framework is needed.
@article{virtoSoilDegradationSoil2014,
title = {Soil Degradation and Soil Quality in {{Western Europe}}: Current Situation and Future Perspectives},
author = {Virto, Iñigo and Imaz, Maŕıa and Fernández-Ugalde, Oihane and Gartzia-Bengoetxea, Nahia and Enrique, Alberto and Bescansa, Paloma},
date = {2014-12},
journaltitle = {Sustainability},
volume = {7},
pages = {313--365},
issn = {2071-1050},
doi = {10.3390/su7010313},
url = {https://doi.org/10.3390/su7010313},
abstract = {The extent and causes of chemical, physical and biological degradation of soil, and of soil loss, vary greatly in different countries in Western Europe. The objective of this review paper is to examine these issues and also strategies for soil protection and future perspectives for soil quality evaluation, in light of present legislation aimed at soil protection. Agriculture and forestry are the main causes of many of the above problems, especially physical degradation, erosion and organic matter loss. Land take and soil sealing have increased in recent decades, further enhancing the problems. In agricultural land, conservation farming, organic farming and other soil-friendly practices have been seen to have site-specific effects, depending on the soil characteristics and the particular types of land use and land users. No single soil management strategy is suitable for all regions, soil types and soil uses. Except for soil contamination, specific legislation for soil protection is lacking in Western Europe. The Thematic Strategy for Soil Protection in the European Union has produced valuable information and has encouraged the development of networks and databases. However, soil degradation is addressed only indirectly in environmental policies and through the Common Agricultural Policy of the European Union, which promotes farming practices that support soil conservation. Despite these efforts, there remains a need for soil monitoring networks and decision-support systems aimed at optimization of soil quality in the region. The pressure on European soils will continue in the future, and a clearly defined regulatory framework is needed.},
keywords = {*imported-from-citeulike-INRMM,~INRMM-MiD:c-13475511,~to-add-doi-URL,mitigation,protection,soil-resources,sustainability,western-europe},
number = {1}
}
Soil Characteristics and Landcover Relationships on Soil Hydraulic Conductivity at a Hillslope Scale: A View towards Local Flood Management. Archer, N. A. L., Bonell, M., Coles, N., MacDonald, A. M., Auton, C. A., & Stevenson, R. 497:208–222. Paper doi abstract bibtex We evaluate woodland/grassland cover and soil types to reduce local flooding. We measured field saturated hydraulic conductivity under grassland and woodland. Established broadleaf woodland had significantly higher infiltration rates than grassland. 1 in 10~year storm events would cause infiltration-excess overland flow on grassland. We suggest deciduous shelterbelts upslope could locally reduce overland flow. There are surprisingly few studies in humid temperate forests which provide reliable evidence that soil permeability is enhanced under forests. This work addresses this research gap through a detailed investigation of permeability on a hillslope in the Eddleston Catchment, Scottish Borders UK, to evaluate the impact of land cover, superficial geology and soil types on permeability using measurements of field saturated hydraulic conductivity (Kfs) supported by detailed topsoil profile descriptions and counting of roots with diameters $>$2~mm. Kfs was measured at depth 0.04-0.15~m using a constant head well permeameter across four paired landcover sites of adjacent tree and intensely grazed grassland. The measured tree types were: 500-year-old mixed woodland; 180-year-old mixed woodland; 45-year-old Pinus sylvestris plantation; and 180-year-old Salix caprea woodland. The respective paired grids of trees and grassland were compared on similar soil texture and topography. This study highlights the significant impact of broadleaf woodland at a hillslope scale on Kfs in comparison to grassland areas: median Kfs values under 180-year-old S. caprea woodland (8~mm~h-1), 180-year-old mixed woodland (119~mm~h-1) and 500-year-old broadleaf woodland (174~mm~h-1) were found to be respectively 8, 6 and 5 times higher than neighbouring grazed grassland areas on the same superficial geology. Further statistical analysis indicates that such Kfs enhancement is associated with the presence of coarse roots ($>$2~mm diameter) creating conduits for preferential flow and a deeper organic layer in the topsoil profile under woodlands. By contrast the P. sylvestris forest had only slightly higher (42~mm~h-1), but not statistically different Kfs values, when compared to adjacent pasture (35~mm~h-1). In the grassland areas, in the absence of course roots, the superficial geology was dominant in accounting for differences in Kfs, with the alluvium floodplain having a significantly lower median Kfs (1~mm~h-1) than surrounding hillslope sites, which had a range of median Kfs from 21 to 39~mm~h-1. The data were used to infer areas of runoff generation by comparing Kfs values with modelled 15~min maximum intensity duration rainfall with a 1 in 10~year return period. Infiltration prevailed in the 180- and 500-year-old mixed and broadleaf woodland, whereas some grassland areas and the floodplain were inferred to generate overland flow. The significantly higher Kfs under broadleaf mature forests suggests that planting broadleaf woodlands on hillslopes in clusters or as shelterbelts within grasslands would provide areas of increased capacity for rainfall infiltration and arrest runoff generation during flood-producing storm events. [Excerpt: Conclusions] Overall this study highlights the significant impact of broadleaf woodland on a hillslope that increases Kfs in comparison to grassland areas. In particular, Kfs under 180 and 500 year old broadleaf forest was found to be respectively 6 and 5 times higher than neighbouring grazed grassland areas on the same superficial geology. This was attributed to the significantly deeper organic layer in the topsoil profile providing greater available water storage and the presence of coarse roots ($>$2 mm diameter) creating conduits for preferential flow. On the other hand, the Kfs under P. sylvestris had only slightly higher Kfs values than the adjacent grassland area, and were statistically not significantly different. This result is surprising considering that root numbers and diameter under P. sylvestris is similar to the 180 year old broadleaf forest. Causal factors may have been due to enhanced illuviation of available organic colloids from pine needles, which could cause soil repellency, ultimately reducing Kfs. The floodplain broadleaf woodland had significantly lower Kfs values than the other woodland area, illustrating the problem of poor soil drainage relating to the gley soils in the floodplain. The coarse roots that did exist within the floodplain woodland were shallow and were spatially less extensive (in clumps), but they did provide some high outlying Kfs values and an associated large mean variance in this parameter. The low median Kfs values at 0.04-0.15 m soil depth under all four measured grassland ranged from median 1 to 39 mm h-1. The highest grassland Kfs values were in head deposits (high gravel content) and the lowest in the alluvium floodplain deposits (higher silt and clay content). The diverse particle size distribution of clay, silt, sand and gravel within the hillslope indicated the significant effect of glaciation and fluvial transport in depositing and sorting which in turn, affected the topsoil Kfs under grassland. Moreover no coarse roots ($>$2 mm diameter) were observed in the soil profiles in the grass areas. Thus at these sites the superficial geology was a more dominant influence on Kfs than biological factors, which were more dominant in broadleaf woodland. Low Kfs values in the floodplain were also observed to be influenced by soil compaction caused by high stocking rates. Of all the soil description parameters (total root numbers, number of roots $>$5 mm, number of roots between 2 and 5 mm, humus depth, stone size, depth of gravel layer), an increase in Kfs was determined by regression analysis to be most associated with total root numbers $>$2 mm diameter. By contrast no statistical relationship between gravel size and Kfs was evident. [\n] Mapping in situ Kfs measurements inferred possible areas of sources and sinks for overland flow during high intensity duration rainfall (the example used was I15max 1 in 10 year rainfall event). A source of overland flow (infiltration-excess and saturation-excess) occurs in most grassland areas and particularly in the floodplain silty soils. Broadleaf woodland areas are likely to act as sinks to overland flow during high intensity rainfall, but at a depth $>$0.15 m sub-surface storm flow is likely to occur. [\n] In terms of NFM, this study suggests that older broadleaf forests on pastoral hillslopes could mitigate local flooding because of the significantly higher infiltration rates and sub-soil Kfs under these forested areas in contrast to the heavily, grazed grasslands. However, as indicated earlier, such deciduous forests occupy only ∼7\,% of woodland in the Scottish Borders ( Anon, 1999) and a paradigm shift in forestation practice in terms of species is thus required.
@article{archerSoilCharacteristicsLandcover2013,
title = {Soil Characteristics and Landcover Relationships on Soil Hydraulic Conductivity at a Hillslope Scale: A View towards Local Flood Management},
author = {Archer, N. A. L. and Bonell, M. and Coles, N. and MacDonald, A. M. and Auton, C. A. and Stevenson, R.},
date = {2013-08},
journaltitle = {Journal of Hydrology},
volume = {497},
pages = {208--222},
issn = {0022-1694},
doi = {10.1016/j.jhydrol.2013.05.043},
url = {https://doi.org/10.1016/j.jhydrol.2013.05.043},
abstract = {We evaluate woodland/grassland cover and soil types to reduce local flooding. We measured field saturated hydraulic conductivity under grassland and woodland. Established broadleaf woodland had significantly higher infiltration rates than grassland. 1 in 10~year storm events would cause infiltration-excess overland flow on grassland. We suggest deciduous shelterbelts upslope could locally reduce overland flow. There are surprisingly few studies in humid temperate forests which provide reliable evidence that soil permeability is enhanced under forests. This work addresses this research gap through a detailed investigation of permeability on a hillslope in the Eddleston Catchment, Scottish Borders UK, to evaluate the impact of land cover, superficial geology and soil types on permeability using measurements of field saturated hydraulic conductivity (Kfs) supported by detailed topsoil profile descriptions and counting of roots with diameters {$>$}2~mm. Kfs was measured at depth 0.04-0.15~m using a constant head well permeameter across four paired landcover sites of adjacent tree and intensely grazed grassland. The measured tree types were: 500-year-old mixed woodland; 180-year-old mixed woodland; 45-year-old Pinus sylvestris plantation; and 180-year-old Salix caprea woodland. The respective paired grids of trees and grassland were compared on similar soil texture and topography. This study highlights the significant impact of broadleaf woodland at a hillslope scale on Kfs in comparison to grassland areas: median Kfs values under 180-year-old S. caprea woodland (8~mm~h-1), 180-year-old mixed woodland (119~mm~h-1) and 500-year-old broadleaf woodland (174~mm~h-1) were found to be respectively 8, 6 and 5 times higher than neighbouring grazed grassland areas on the same superficial geology. Further statistical analysis indicates that such Kfs enhancement is associated with the presence of coarse roots ({$>$}2~mm diameter) creating conduits for preferential flow and a deeper organic layer in the topsoil profile under woodlands. By contrast the P. sylvestris forest had only slightly higher (42~mm~h-1), but not statistically different Kfs values, when compared to adjacent pasture (35~mm~h-1). In the grassland areas, in the absence of course roots, the superficial geology was dominant in accounting for differences in Kfs, with the alluvium floodplain having a significantly lower median Kfs (1~mm~h-1) than surrounding hillslope sites, which had a range of median Kfs from 21 to 39~mm~h-1. The data were used to infer areas of runoff generation by comparing Kfs values with modelled 15~min maximum intensity duration rainfall with a 1 in 10~year return period. Infiltration prevailed in the 180- and 500-year-old mixed and broadleaf woodland, whereas some grassland areas and the floodplain were inferred to generate overland flow. The significantly higher Kfs under broadleaf mature forests suggests that planting broadleaf woodlands on hillslopes in clusters or as shelterbelts within grasslands would provide areas of increased capacity for rainfall infiltration and arrest runoff generation during flood-producing storm events.
[Excerpt: Conclusions]
Overall this study highlights the significant impact of broadleaf woodland on a hillslope that increases Kfs in comparison to grassland areas. In particular, Kfs under 180 and 500 year old broadleaf forest was found to be respectively 6 and 5 times higher than neighbouring grazed grassland areas on the same superficial geology. This was attributed to the significantly deeper organic layer in the topsoil profile providing greater available water storage and the presence of coarse roots ({$>$}2 mm diameter) creating conduits for preferential flow. On the other hand, the Kfs under P. sylvestris had only slightly higher Kfs values than the adjacent grassland area, and were statistically not significantly different. This result is surprising considering that root numbers and diameter under P. sylvestris is similar to the 180 year old broadleaf forest. Causal factors may have been due to enhanced illuviation of available organic colloids from pine needles, which could cause soil repellency, ultimately reducing Kfs. The floodplain broadleaf woodland had significantly lower Kfs values than the other woodland area, illustrating the problem of poor soil drainage relating to the gley soils in the floodplain. The coarse roots that did exist within the floodplain woodland were shallow and were spatially less extensive (in clumps), but they did provide some high outlying Kfs values and an associated large mean variance in this parameter. The low median Kfs values at 0.04-0.15 m soil depth under all four measured grassland ranged from median 1 to 39 mm h-1. The highest grassland Kfs values were in head deposits (high gravel content) and the lowest in the alluvium floodplain deposits (higher silt and clay content). The diverse particle size distribution of clay, silt, sand and gravel within the hillslope indicated the significant effect of glaciation and fluvial transport in depositing and sorting which in turn, affected the topsoil Kfs under grassland. Moreover no coarse roots ({$>$}2 mm diameter) were observed in the soil profiles in the grass areas. Thus at these sites the superficial geology was a more dominant influence on Kfs than biological factors, which were more dominant in broadleaf woodland. Low Kfs values in the floodplain were also observed to be influenced by soil compaction caused by high stocking rates. Of all the soil description parameters (total root numbers, number of roots {$>$}5 mm, number of roots between 2 and 5 mm, humus depth, stone size, depth of gravel layer), an increase in Kfs was determined by regression analysis to be most associated with total root numbers {$>$}2 mm diameter. By contrast no statistical relationship between gravel size and Kfs was evident.
[\textbackslash n] Mapping in situ Kfs measurements inferred possible areas of sources and sinks for overland flow during high intensity duration rainfall (the example used was I15max 1 in 10 year rainfall event). A source of overland flow (infiltration-excess and saturation-excess) occurs in most grassland areas and particularly in the floodplain silty soils. Broadleaf woodland areas are likely to act as sinks to overland flow during high intensity rainfall, but at a depth {$>$}0.15 m sub-surface storm flow is likely to occur.
[\textbackslash n] In terms of NFM, this study suggests that older broadleaf forests on pastoral hillslopes could mitigate local flooding because of the significantly higher infiltration rates and sub-soil Kfs under these forested areas in contrast to the heavily, grazed grasslands. However, as indicated earlier, such deciduous forests occupy only ∼7\,\% of woodland in the Scottish Borders ( Anon, 1999) and a paradigm shift in forestation practice in terms of species is thus required.},
keywords = {*imported-from-citeulike-INRMM,~INRMM-MiD:c-13908859,~to-add-doi-URL,ancient-forests,broadleaved,flood-control,floods,forest-resources,grasslands,land-cover,mature-forests,mitigation,pinus-sylvestris,plantation,runoff,salix-caprea,soil-resources,storm,vegetation,water-resources}
}
Belowground Carbon Trade among Tall Trees in a Temperate Forest. Klein, T., Siegwolf, R. T. W., & Korner, C. 352(6283):342–344. Paper doi abstract bibtex [Editor summary: Carbon trading between adult trees] Competition between individual plants for resources is well known, but sharing of resources may also occur. Klein et al. observed tree-to-tree carbon shuttling between roots of tall trees in a mixed temperate forest in Switzerland (see the Perspective by van der Heijden). By applying stable carbon isotope labeling to individual tree canopies, they show that up to 40\,% of the carbon in the fine roots of one individual may be derived from photosynthetic products of a neighbor. Carbon transfer of this kind, mediated by plant-associated fungi, or mycorrhizae, in the soil, has been reported on a smaller scale in seedlings, but not before in trees. [Abstract] Forest trees compete for light and soil resources, but photoassimilates, once produced in the foliage, are not considered to be exchanged between individuals. Applying stable carbon isotope labeling at the canopy scale, we show that carbon assimilated by 40-meter-tall spruce is traded over to neighboring beech, larch, and pine via overlapping root spheres. Isotope mixing signals indicate that the interspecific, bidirectional transfer, assisted by common ectomycorrhiza networks, accounted for 40\,% of the fine root carbon (about 280 kilograms per hectare per year tree-to-tree transfer). Although competition for resources is commonly considered as the dominant tree-to-tree interaction in forests, trees may interact in more complex ways, including substantial carbon exchange.
@article{kleinBelowgroundCarbonTrade2016,
title = {Belowground Carbon Trade among Tall Trees in a Temperate Forest},
author = {Klein, T. and Siegwolf, R. T. W. and Korner, C.},
date = {2016-04},
journaltitle = {Science},
volume = {352},
pages = {342--344},
issn = {0036-8075},
doi = {10.1126/science.aad6188},
url = {https://doi.org/10.1126/science.aad6188},
abstract = {[Editor summary: Carbon trading between adult trees]
Competition between individual plants for resources is well known, but sharing of resources may also occur. Klein et al. observed tree-to-tree carbon shuttling between roots of tall trees in a mixed temperate forest in Switzerland (see the Perspective by van der Heijden). By applying stable carbon isotope labeling to individual tree canopies, they show that up to 40\,\% of the carbon in the fine roots of one individual may be derived from photosynthetic products of a neighbor. Carbon transfer of this kind, mediated by plant-associated fungi, or mycorrhizae, in the soil, has been reported on a smaller scale in seedlings, but not before in trees.
[Abstract]
Forest trees compete for light and soil resources, but photoassimilates, once produced in the foliage, are not considered to be exchanged between individuals. Applying stable carbon isotope labeling at the canopy scale, we show that carbon assimilated by 40-meter-tall spruce is traded over to neighboring beech, larch, and pine via overlapping root spheres. Isotope mixing signals indicate that the interspecific, bidirectional transfer, assisted by common ectomycorrhiza networks, accounted for 40\,\% of the fine root carbon (about 280 kilograms per hectare per year tree-to-tree transfer). Although competition for resources is commonly considered as the dominant tree-to-tree interaction in forests, trees may interact in more complex ways, including substantial carbon exchange.},
keywords = {*imported-from-citeulike-INRMM,~INRMM-MiD:c-14013061,~to-add-doi-URL,complexity,ecology,forest-resources,mycorrhizal-fungi,networks,organic-carbon,soil-resources,temperate-forests,vegetation},
number = {6283}
}
Improving Generalized Regression Analysis for the Spatial Prediction of Forest Communities. Maggini, R., Lehmann, A., Zimmermann, N. E., & Guisan, A. 33(10):1729–1749. Paper doi abstract bibtex Aim This study used data from temperate forest communities to assess: (1) five different stepwise selection methods with generalized additive models, (2) the effect of weighting absences to ensure a prevalence of 0.5, (3) the effect of limiting absences beyond the environmental envelope defined by presences, (4) four different methods for incorporating spatial autocorrelation, and (5) the effect of integrating an interaction factor defined by a regression tree on the residuals of an initial environmental model. Location State of Vaud, western Switzerland. Methods Generalized additive models (GAMs) were fitted using the grasp package (generalized regression analysis and spatial predictions, http://www.cscf.ch/grasp). Results Model selection based on cross-validation appeared to be the best compromise between model stability and performance (parsimony) among the five methods tested. Weighting absences returned models that perform better than models fitted with the original sample prevalence. This appeared to be mainly due to the impact of very low prevalence values on evaluation statistics. Removing zeroes beyond the range of presences on main environmental gradients changed the set of selected predictors, and potentially their response curve shape. Moreover, removing zeroes slightly improved model performance and stability when compared with the baseline model on the same data set. Incorporating a spatial trend predictor improved model performance and stability significantly. Even better models were obtained when including local spatial autocorrelation. A novel approach to include interactions proved to be an efficient way to account for interactions between all predictors at once. Main conclusions Models and spatial predictions of 18 forest communities were significantly improved by using either: (1) cross-validation as a model selection method, (2) weighted absences, (3) limited absences, (4) predictors accounting for spatial autocorrelation, or (5) a factor variable accounting for interactions between all predictors. The final choice of model strategy should depend on the nature of the available data and the specific study aims. Statistical evaluation is useful in searching for the best modelling practice. However, one should not neglect to consider the shapes and interpretability of response curves, as well as the resulting spatial predictions in the final assessment.
@article{magginiImprovingGeneralizedRegression2006,
title = {Improving Generalized Regression Analysis for the Spatial Prediction of Forest Communities},
author = {Maggini, Ramona and Lehmann, Anthony and Zimmermann, Niklaus E. and Guisan, Antoine},
date = {2006-10},
journaltitle = {Journal of Biogeography},
volume = {33},
pages = {1729--1749},
issn = {0305-0270},
doi = {10.1111/j.1365-2699.2006.01465.x},
url = {http://mfkp.org/INRMM/article/835166},
abstract = {Aim\hspace{0.6em} This study used data from temperate forest communities to assess: (1) five different stepwise selection methods with generalized additive models, (2) the effect of weighting absences to ensure a prevalence of 0.5, (3) the effect of limiting absences beyond the environmental envelope defined by presences, (4) four different methods for incorporating spatial autocorrelation, and (5) the effect of integrating an interaction factor defined by a regression tree on the residuals of an initial environmental model. Location\hspace{0.6em} State of Vaud, western Switzerland. Methods\hspace{0.6em} Generalized additive models (GAMs) were fitted using the grasp package (generalized regression analysis and spatial predictions, http://www.cscf.ch/grasp). Results\hspace{0.6em} Model selection based on cross-validation appeared to be the best compromise between model stability and performance (parsimony) among the five methods tested. Weighting absences returned models that perform better than models fitted with the original sample prevalence. This appeared to be mainly due to the impact of very low prevalence values on evaluation statistics. Removing zeroes beyond the range of presences on main environmental gradients changed the set of selected predictors, and potentially their response curve shape. Moreover, removing zeroes slightly improved model performance and stability when compared with the baseline model on the same data set. Incorporating a spatial trend predictor improved model performance and stability significantly. Even better models were obtained when including local spatial autocorrelation. A novel approach to include interactions proved to be an efficient way to account for interactions between all predictors at once. Main conclusions\hspace{0.6em} Models and spatial predictions of 18 forest communities were significantly improved by using either: (1) cross-validation as a model selection method, (2) weighted absences, (3) limited absences, (4) predictors accounting for spatial autocorrelation, or (5) a factor variable accounting for interactions between all predictors. The final choice of model strategy should depend on the nature of the available data and the specific study aims. Statistical evaluation is useful in searching for the best modelling practice. However, one should not neglect to consider the shapes and interpretability of response curves, as well as the resulting spatial predictions in the final assessment.},
keywords = {*imported-from-citeulike-INRMM,~INRMM-MiD:c-835166,~to-add-doi-URL,bias-correction,bioclimatic-predictors,correlation-analysis,forest-resources,habitat-suitability,statistics,uncertainty,weighting},
number = {10}
}
Assessing Crown Fire Potential in Coniferous Forests of Western North America: A Critique of Current Approaches and Recent Simulation Studies. Cruz, M. G. & Alexander, M. E. 19(4):377+. Paper doi abstract bibtex To control and use wildland fires safely and effectively depends on creditable assessments of fire potential, including the propensity for crowning in conifer forests. Simulation studies that use certain fire modelling systems (i.e. NEXUS, FlamMap, FARSITE, FFE-FVS (Fire and Fuels Extension to the Forest Vegetation Simulator), Fuel Management Analyst (FMAPlus®), BehavePlus) based on separate implementations or direct integration of Rothermel's surface and crown rate of fire spread models with Van Wagner's crown fire transition and propagation models are shown to have a significant underprediction bias when used in assessing potential crown fire behaviour in conifer forests of western North America. The principal sources of this underprediction bias are shown to include: [::(i)] incompatible model linkages; [::(ii)] use of surface and crown fire rate of spread models that have an inherent underprediction bias; and [::(iii)] reduction in crown fire rate of spread based on the use of unsubstantiated crown fraction burned functions. [::The use of uncalibrated custom fuel models] to represent surface fuelbeds is a fourth potential source of bias. [\n] These sources are described and documented in detail based on comparisons with experimental fire and wildfire observations and on separate analyses of model components. The manner in which the two primary canopy fuel inputs influencing crown fire initiation (i.e. foliar moisture content and canopy base height) is handled in these simulation studies and the meaning of Scott and Reinhardt's two crown fire hazard indices are also critically examined. [Excerpt: Summary and concluding remarks] The ready availability of a multitude of fire modelling systems in the US in recent years has led to their widespread use in numerous simulation studies aimed at assessing various fire behaviour characteristics associated with specific fuel complex structures, including the propensity for crown fire initiation and spread (McHugh 2006). The results of these simulations, often aimed at evaluating fuel treatment effectiveness, are in turn utilised in a whole host of applications (e.g. Scott 2003; Fiedler et al. 2004; Skog et al. 2006; Johnson et al. 2007; Finkral and Evans 2008; Huggett et al. 2008; Johnson 2008; Reinhardt et al. 2010) and thus have significant implications for public and wildland firefighter safety, community fire protection, fire management policy-making, and forest management practices. As Cheney (1981) has noted, 'The reality of fire behaviour predictions is that overestimates can be easily readjusted without serious consequences; underestimates of behaviour can be disastrous both to the operations of the fire controller and the credibility of the person making the predictions'. [\n] A critical review of several of these simulation studies, as documented here, has found that the results are often unrealistic for a variety of reasons. It's recognised that the authors of these studies commonly point out the limitations of the models and modelling systems being used through a customary disclaimer concerning the unknowns regarding crown fire behaviour (e.g. Stephens et al. 2009). Nevertheless, the fact that the fuel treatment evaluation studies referenced here are based on modelling systems that utilised model linkages for gauging potential crown fire behaviour that have not previously undergone any form of performance evaluation against independent datasets or any empirical observations should be of concern. There appears, however, to be an aversion within an element of the fire research community to do so (e.g. Scott and Reinhardt 2001; Scott 2006; Stephens et al. 2009). Nevertheless, such testing is now generally regarded as a basic tenet of modern-day model development and evaluation (Jakeman et al. 2006). [\n] Fire modelling systems like NEXUS (Scott and Reinhardt 2001), FFE-FVS (Reinhardt and Crookston 2003), FARSITE (Finney 2004), FMAPlus (Carlton 2005), FlamMap (Finney 2006), and BehavePlus (Andrews et al. 2008) that are based on separate implementations or linkages between Rothermel's (1972, 1991) rate of fire spread models and Van Wagner's (1977, 1993) crown fire transition and propagation models have been shown to have a marked underprediction bias when used to assess potential crown fire behaviour. What has been allowed to evolve is a family of modelling systems composed of independently developed, linked models that were never intended to work together, are sometimes based on very limited data, and may propagate errors beyond acceptable limits. [\n] We have documented here the sources of the bias based on empirical evidence in the form of published experimental fire and wildfire datasets. By analysing model linkages and components, we have described the primary sources of such bias, namely: (1) incompatible model linkages; (2) use of surface and crown fire rate of spread models that have an inherent underprediction bias; and (3) reduction in crown fire rate of spread based on use of unsubstantiated CFB functions. The use of uncalibrated, custom fuel models to represent surface fuelbeds is considered another potential source of bias. [\n] Our analysis has also shown that the crown fire initiation underprediction bias inherent in all of these fire modelling systems could possibly be rectified by modifying the method used to calculate the surface fireline intensity for the purposes of assessing crown fire initiation potential, namely using Nelson's (2003) model to estimate tr in place of Anderson's model (1969). Other modelling systems exist for predicting the likelihood of crown fire initiation and other aspects of crown fire behaviour (Alexander et al. 2006; Cruz et al. 2006b, 2008). Mitsopoulos and Dimitrakopoulos (2007) have, for example, made extensive use of this suite of models in their assessment of crown fire potential in Aleppo pine (Pinus halepensis) forests in Greece. These systems are based on models that have undergone performance evaluations against independent datasets and been shown to be reasonably reliable (Cruz et al. 2003b, 2004, 2006b; Cronan and Jandt 2008). Resolving the underprediction bias associated with predicting active crown fire rate of spread inherent in the Rothermel (1991) model would require substantial changes, including a reassessment of the use of a CFB function, if not complete replacement with a more robust empirically developed model (Cruz et al. 2005) that has been extensively tested (Alexander and Cruz 2006) or a physically based one that has undergone limited testing (Butler et al. 2004). [\n] Alexander (2007) has emphasised that assessments of wildland fire potential involving simulation modelling must be complemented with fire behaviour case study knowledge and by experienced judgment. This review has revealed an overwhelming need for the research users of fire modelling systems to be grounded in the theory and proper application of such tools, including a solid understanding of the assumptions, limitations and accuracy of the underlying models as well as practical knowledge of the subject phenomena (Brown and Davis 1973; Albini 1976; Alexander 2009a, 2009b).
@article{cruzAssessingCrownFire2010,
title = {Assessing Crown Fire Potential in Coniferous Forests of Western {{North America}}: A Critique of Current Approaches and Recent Simulation Studies},
author = {Cruz, Miguel G. and Alexander, Martin E.},
date = {2010},
journaltitle = {International Journal of Wildland Fire},
volume = {19},
pages = {377+},
issn = {1049-8001},
doi = {10.1071/wf08132},
url = {https://doi.org/10.1071/wf08132},
abstract = {To control and use wildland fires safely and effectively depends on creditable assessments of fire potential, including the propensity for crowning in conifer forests. Simulation studies that use certain fire modelling systems (i.e. NEXUS, FlamMap, FARSITE, FFE-FVS (Fire and Fuels Extension to the Forest Vegetation Simulator), Fuel Management Analyst (FMAPlus®), BehavePlus) based on separate implementations or direct integration of Rothermel's surface and crown rate of fire spread models with Van Wagner's crown fire transition and propagation models are shown to have a significant underprediction bias when used in assessing potential crown fire behaviour in conifer forests of western North America. The principal sources of this underprediction bias are shown to include:
[::(i)] incompatible model linkages;
[::(ii)] use of surface and crown fire rate of spread models that have an inherent underprediction bias; and
[::(iii)] reduction in crown fire rate of spread based on the use of unsubstantiated crown fraction burned functions.
[::The use of uncalibrated custom fuel models] to represent surface fuelbeds is a fourth potential source of bias.
[\textbackslash n] These sources are described and documented in detail based on comparisons with experimental fire and wildfire observations and on separate analyses of model components. The manner in which the two primary canopy fuel inputs influencing crown fire initiation (i.e. foliar moisture content and canopy base height) is handled in these simulation studies and the meaning of Scott and Reinhardt's two crown fire hazard indices are also critically examined.
[Excerpt: Summary and concluding remarks]
The ready availability of a multitude of fire modelling systems in the US in recent years has led to their widespread use in numerous simulation studies aimed at assessing various fire behaviour characteristics associated with specific fuel complex structures, including the propensity for crown fire initiation and spread (McHugh 2006). The results of these simulations, often aimed at evaluating fuel treatment effectiveness, are in turn utilised in a whole host of applications (e.g. Scott 2003; Fiedler et al. 2004; Skog et al. 2006; Johnson et al. 2007; Finkral and Evans 2008; Huggett et al. 2008; Johnson 2008; Reinhardt et al. 2010) and thus have significant implications for public and wildland firefighter safety, community fire protection, fire management policy-making, and forest management practices. As Cheney (1981) has noted, 'The reality of fire behaviour predictions is that overestimates can be easily readjusted without serious consequences; underestimates of behaviour can be disastrous both to the operations of the fire controller and the credibility of the person making the predictions'.
[\textbackslash n] A critical review of several of these simulation studies, as documented here, has found that the results are often unrealistic for a variety of reasons. It's recognised that the authors of these studies commonly point out the limitations of the models and modelling systems being used through a customary disclaimer concerning the unknowns regarding crown fire behaviour (e.g. Stephens et al. 2009). Nevertheless, the fact that the fuel treatment evaluation studies referenced here are based on modelling systems that utilised model linkages for gauging potential crown fire behaviour that have not previously undergone any form of performance evaluation against independent datasets or any empirical observations should be of concern. There appears, however, to be an aversion within an element of the fire research community to do so (e.g. Scott and Reinhardt 2001; Scott 2006; Stephens et al. 2009). Nevertheless, such testing is now generally regarded as a basic tenet of modern-day model development and evaluation (Jakeman et al. 2006).
[\textbackslash n] Fire modelling systems like NEXUS (Scott and Reinhardt 2001), FFE-FVS (Reinhardt and Crookston 2003), FARSITE (Finney 2004), FMAPlus (Carlton 2005), FlamMap (Finney 2006), and BehavePlus (Andrews et al. 2008) that are based on separate implementations or linkages between Rothermel's (1972, 1991) rate of fire spread models and Van Wagner's (1977, 1993) crown fire transition and propagation models have been shown to have a marked underprediction bias when used to assess potential crown fire behaviour. What has been allowed to evolve is a family of modelling systems composed of independently developed, linked models that were never intended to work together, are sometimes based on very limited data, and may propagate errors beyond acceptable limits.
[\textbackslash n] We have documented here the sources of the bias based on empirical evidence in the form of published experimental fire and wildfire datasets. By analysing model linkages and components, we have described the primary sources of such bias, namely: (1) incompatible model linkages; (2) use of surface and crown fire rate of spread models that have an inherent underprediction bias; and (3) reduction in crown fire rate of spread based on use of unsubstantiated CFB functions. The use of uncalibrated, custom fuel models to represent surface fuelbeds is considered another potential source of bias.
[\textbackslash n] Our analysis has also shown that the crown fire initiation underprediction bias inherent in all of these fire modelling systems could possibly be rectified by modifying the method used to calculate the surface fireline intensity for the purposes of assessing crown fire initiation potential, namely using Nelson's (2003) model to estimate tr in place of Anderson's model (1969). Other modelling systems exist for predicting the likelihood of crown fire initiation and other aspects of crown fire behaviour (Alexander et al. 2006; Cruz et al. 2006b, 2008). Mitsopoulos and Dimitrakopoulos (2007) have, for example, made extensive use of this suite of models in their assessment of crown fire potential in Aleppo pine (Pinus halepensis) forests in Greece. These systems are based on models that have undergone performance evaluations against independent datasets and been shown to be reasonably reliable (Cruz et al. 2003b, 2004, 2006b; Cronan and Jandt 2008). Resolving the underprediction bias associated with predicting active crown fire rate of spread inherent in the Rothermel (1991) model would require substantial changes, including a reassessment of the use of a CFB function, if not complete replacement with a more robust empirically developed model (Cruz et al. 2005) that has been extensively tested (Alexander and Cruz 2006) or a physically based one that has undergone limited testing (Butler et al. 2004).
[\textbackslash n] Alexander (2007) has emphasised that assessments of wildland fire potential involving simulation modelling must be complemented with fire behaviour case study knowledge and by experienced judgment. This review has revealed an overwhelming need for the research users of fire modelling systems to be grounded in the theory and proper application of such tools, including a solid understanding of the assumptions, limitations and accuracy of the underlying models as well as practical knowledge of the subject phenomena (Brown and Davis 1973; Albini 1976; Alexander 2009a, 2009b).},
keywords = {*imported-from-citeulike-INRMM,~INRMM-MiD:c-13706015,~to-add-doi-URL,canada,comparison,conifers,model-comparison,modelling-uncertainty,prediction-bias,rothermel,simulation,software-uncertainty,uncertainty,united-states,wildfires},
number = {4}
}
Root Exudates Drive Interspecific Facilitation by Enhancing Nodulation and N2 Fixation. Bai, L., Yu-Ying, L., Hua-Mao, W., Fang-Fang, Z., Chun-Jie, L., Xue-Xian, L., Hans, L., & Long, L. 113(23):6496–6501. Paper doi abstract bibtex [Significance] Plant diversity often leads to an increase in ecosystem productivity, but the underpinning mechanisms remain poorly understood. We found that faba bean/maize intercropping enhances productivity, nodulation, and N2 fixation of faba bean through interspecific root interactions. We provide a mechanism explaining how maize promotes N2 fixation of faba bean, where root exudates from maize increase root hair deformation and nodulation in faba bean, double exudation of flavonoids (signaling compounds for rhizobia), and up-regulate the expression of a chalcone-flavanone isomerase gene involved in flavonoid synthesis, and genes mediating nodulation and auxin responses. Our results provide a mechanism for facilitative root-root interactions explaining how species diversity may enhance ecosystem productivity with important implications for developing sustainable agriculture. [Abstract] Plant diversity in experimental systems often enhances ecosystem productivity, but the mechanisms causing this overyielding are only partly understood. Intercropping faba beans (Vicia faba L.) and maize (Zea mays L.) result in overyielding and also, enhanced nodulation by faba beans. By using permeable and impermeable root barriers in a 2-y field experiment, we show that root-root interactions between faba bean and maize significantly increase both nodulation and symbiotic N2 fixation in intercropped faba bean. Furthermore, root exudates from maize promote faba bean nodulation, whereas root exudates from wheat and barley do not. Thus, a decline of soil nitrate concentrations caused by intercropped cereals is not the sole mechanism for maize promoting faba bean nodulation. Intercropped maize also caused a twofold increase in exudation of flavonoids (signaling compounds for rhizobia) in the systems. Roots of faba bean treated with maize root exudates exhibited an immediate 11-fold increase in the expression of chalcone-flavanone isomerase (involved in flavonoid synthesis) gene together with a significantly increased expression of genes mediating nodulation and auxin response. After 35 d, faba beans treated with maize root exudate continued to show up-regulation of key nodulation genes, such as early nodulin 93 (ENOD93), and promoted nitrogen fixation. Our results reveal a mechanism for how intercropped maize promotes nitrogen fixation of faba bean, where maize root exudates promote flavonoid synthesis in faba bean, increase nodulation, and stimulate nitrogen fixation after enhanced gene expression. These results indicate facilitative root-root interactions and provide a mechanism for a positive relationship between species diversity and ecosystem productivity.
@article{baiRootExudatesDrive2016,
title = {Root Exudates Drive Interspecific Facilitation by Enhancing Nodulation and {{N2}} Fixation},
author = {Bai, Li and Yu-Ying, Li and Hua-Mao, Wu and Fang-Fang, Zhang and Chun-Jie, Li and Xue-Xian, Li and Hans, Lambers and Long, Li},
date = {2016-06},
journaltitle = {Proceedings of the National Academy of Sciences},
volume = {113},
pages = {6496--6501},
issn = {1091-6490},
doi = {10.1073/pnas.1523580113},
url = {http://mfkp.org/INRMM/article/14062242},
abstract = {[Significance]
Plant diversity often leads to an increase in ecosystem productivity, but the underpinning mechanisms remain poorly understood. We found that faba bean/maize intercropping enhances productivity, nodulation, and N2 fixation of faba bean through interspecific root interactions. We provide a mechanism explaining how maize promotes N2 fixation of faba bean, where root exudates from maize increase root hair deformation and nodulation in faba bean, double exudation of flavonoids (signaling compounds for rhizobia), and up-regulate the expression of a chalcone-flavanone isomerase gene involved in flavonoid synthesis, and genes mediating nodulation and auxin responses. Our results provide a mechanism for facilitative root-root interactions explaining how species diversity may enhance ecosystem productivity with important implications for developing sustainable agriculture.
[Abstract]
Plant diversity in experimental systems often enhances ecosystem productivity, but the mechanisms causing this overyielding are only partly understood. Intercropping faba beans (Vicia faba L.) and maize (Zea mays L.) result in overyielding and also, enhanced nodulation by faba beans. By using permeable and impermeable root barriers in a 2-y field experiment, we show that root-root interactions between faba bean and maize significantly increase both nodulation and symbiotic N2 fixation in intercropped faba bean. Furthermore, root exudates from maize promote faba bean nodulation, whereas root exudates from wheat and barley do not. Thus, a decline of soil nitrate concentrations caused by intercropped cereals is not the sole mechanism for maize promoting faba bean nodulation. Intercropped maize also caused a twofold increase in exudation of flavonoids (signaling compounds for rhizobia) in the systems. Roots of faba bean treated with maize root exudates exhibited an immediate 11-fold increase in the expression of chalcone-flavanone isomerase (involved in flavonoid synthesis) gene together with a significantly increased expression of genes mediating nodulation and auxin response. After 35 d, faba beans treated with maize root exudate continued to show up-regulation of key nodulation genes, such as early nodulin 93 (ENOD93), and promoted nitrogen fixation. Our results reveal a mechanism for how intercropped maize promotes nitrogen fixation of faba bean, where maize root exudates promote flavonoid synthesis in faba bean, increase nodulation, and stimulate nitrogen fixation after enhanced gene expression. These results indicate facilitative root-root interactions and provide a mechanism for a positive relationship between species diversity and ecosystem productivity.},
keywords = {*imported-from-citeulike-INRMM,~INRMM-MiD:c-14062242,~to-add-doi-URL,agricultural-resources,biodiversity,diversity,ecosystem,nitrogen,soil-resources,species-association,sustainability,vegetation,vicia-faba,zea-mays},
number = {23}
}
Observational Evidence for Cloud Cover Enhancement over Western European Forests. Teuling, A. J., Taylor, C. M., Meirink, J. F., Melsen, L. A., Miralles, D. G., van Heerwaarden, C. C., Vautard, R., Stegehuis, A. I., Nabuurs, G., & de Arellano, J. V. 8:14065+. Paper doi abstract bibtex Forests impact regional hydrology and climate directly by regulating water and heat fluxes. Indirect effects through cloud formation and precipitation can be important in facilitating continental-scale moisture recycling but are poorly understood at regional scales. In particular, the impact of temperate forest on clouds is largely unknown. Here we provide observational evidence for a strong increase in cloud cover over large forest regions in western Europe based on analysis of 10 years of 15\,min resolution data from geostationary satellites. In addition, we show that widespread windthrow by cyclone Klaus in the Landes forest led to a significant decrease in local cloud cover in subsequent years. Strong cloud development along the downwind edges of larger forest areas are consistent with a forest-breeze mesoscale circulation. Our results highlight the need to include impacts on cloud formation when evaluating the water and climate services of temperate forests, in particular around densely populated areas.
@article{teulingObservationalEvidenceCloud2017,
title = {Observational Evidence for Cloud Cover Enhancement over Western {{European}} Forests},
author = {Teuling, Adriaan J. and Taylor, Christopher M. and Meirink, Jan F. and Melsen, Lieke A. and Miralles, Diego G. and van Heerwaarden, Chiel C. and Vautard, Robert and Stegehuis, Annemiek I. and Nabuurs, Gert-Jan and de Arellano, Jordi V.},
date = {2017-01},
journaltitle = {Nature Communications},
volume = {8},
pages = {14065+},
issn = {2041-1723},
doi = {10.1038/ncomms14065},
url = {http://mfkp.org/INRMM/article/14257971},
abstract = {Forests impact regional hydrology and climate directly by regulating water and heat fluxes. Indirect effects through cloud formation and precipitation can be important in facilitating continental-scale moisture recycling but are poorly understood at regional scales. In particular, the impact of temperate forest on clouds is largely unknown. Here we provide observational evidence for a strong increase in cloud cover over large forest regions in western Europe based on analysis of 10 years of 15\,min resolution data from geostationary satellites. In addition, we show that widespread windthrow by cyclone Klaus in the Landes forest led to a significant decrease in local cloud cover in subsequent years. Strong cloud development along the downwind edges of larger forest areas are consistent with a forest-breeze mesoscale circulation. Our results highlight the need to include impacts on cloud formation when evaluating the water and climate services of temperate forests, in particular around densely populated areas.},
keywords = {*imported-from-citeulike-INRMM,~INRMM-MiD:c-14257971,~to-add-doi-URL,climate,climate-projections,cloud-formation,cloudiness,cross-disciplinary-perspective,ecosystem-services,europe,featured-publication,feedback,forest-breeze,forest-resources,modelling-uncertainty,temperate-forests},
options = {useprefix=true}
}
Extreme Terseness: Some Languages Are More Agile than Others. Taylor, S. 2675:334–336. Paper doi abstract bibtex While XP principles are independent of the languages in which software is developed, we can distinguish properties of programming languages that affect the agility of development. Some languages are inherently more agile than others, and the experience of developing software in these languages reflects this. A family of languages descended from the mathematics notation developed at Harvard in the 1950s by Iverson [1] shares properties of extreme terseness and abstractive power with weak data typing. The history of software development in these languages foreshadows some of the characteristics of XP projects. To these linguistic communities, XP offers the prospect of rehabilitating styles of software development that fell into disrepute with the rise of software engineering. Conversely, these languages offer XP practitioners the possibility of radical condensation of the conversation between developer and customer.
@article{taylorExtremeTersenessLanguages2003,
title = {Extreme Terseness: Some Languages Are More Agile than Others},
author = {Taylor, Stephen},
editor = {Marchesi, Michele and Succi, Giancarlo},
date = {2003-06},
journaltitle = {Lecture Notes in Computer Science},
volume = {2675},
pages = {334--336},
issn = {0302-9743},
doi = {10.1007/3-540-44870-5_44},
url = {https://doi.org/10.1007/3-540-44870-5_44},
abstract = {While XP principles are independent of the languages in which software is developed, we can distinguish properties of programming languages that affect the agility of development. Some languages are inherently more agile than others, and the experience of developing software in these languages reflects this. A family of languages descended from the mathematics notation developed at Harvard in the 1950s by Iverson [1] shares properties of extreme terseness and abstractive power with weak data typing. The history of software development in these languages foreshadows some of the characteristics of XP projects. To these linguistic communities, XP offers the prospect of rehabilitating styles of software development that fell into disrepute with the rise of software engineering. Conversely, these languages offer XP practitioners the possibility of radical condensation of the conversation between developer and customer.},
keywords = {*imported-from-citeulike-INRMM,~INRMM-MiD:c-9337607,~to-add-doi-URL,agile-programming,array-programming,mathematical-reasoning,notation,notation-as-a-tool-of-thought,software-engineering,terseness},
series = {Lecture {{Notes}} in {{Computer Science}}}
}
A New Global Burned Area Product for Climate Assessment of Fire Impacts. Chuvieco, E., Yue, C., Heil, A., Mouillot, F., Alonso-Canas, I., Padilla, M., Pereira, J. M., Oom, D., & Tansey, K. 25(5):619–629. Paper doi abstract bibtex [Aim] This paper presents a new global burned area (BA) product developed within the framework of the European Space Agency's Climate Change Initiative (CCI) programme, along with a first assessment of its potentials for atmospheric and carbon cycle modelling. [Innovation] Methods are presented for generating a new global BA product, along with a comparison with existing BA products, in terms of BA extension, fire size and shapes and emissions derived from biomass burnings. [Main conclusions] Three years of the global BA product were produced, accounting for a total BA of between 360 and 380 Mha year-1. General omission and commission errors for BA were 0.76 and 0.64, but they decreased to 0.51 and 0.52, respectively, for sites with more than 10\,% BA. Intercomparison with other existing BA datasets found similar spatial and temporal trends, mainly with the BA included in the Global Fire Emissions Database (GFED4), although regional differences were found (particularly in the 2006 fires of eastern Europe). The simulated carbon emissions from biomass burning averaged 2.1 Pg C year-1.
@article{chuviecoNewGlobalBurned2016,
title = {A New Global Burned Area Product for Climate Assessment of Fire Impacts},
author = {Chuvieco, Emilio and Yue, Chao and Heil, Angelika and Mouillot, Florent and Alonso-Canas, Itziar and Padilla, Marc and Pereira, Jose M. and Oom, Duarte and Tansey, Kevin},
date = {2016-05},
journaltitle = {Global Ecology and Biogeography},
volume = {25},
pages = {619--629},
issn = {1466-822X},
doi = {10.1111/geb.12440},
url = {https://doi.org/10.1111/geb.12440},
abstract = {[Aim] This paper presents a new global burned area (BA) product developed within the framework of the European Space Agency's Climate Change Initiative (CCI) programme, along with a first assessment of its potentials for atmospheric and carbon cycle modelling.
[Innovation] Methods are presented for generating a new global BA product, along with a comparison with existing BA products, in terms of BA extension, fire size and shapes and emissions derived from biomass burnings.
[Main conclusions] Three years of the global BA product were produced, accounting for a total BA of between 360 and 380 Mha year-1. General omission and commission errors for BA were 0.76 and 0.64, but they decreased to 0.51 and 0.52, respectively, for sites with more than 10\,\% BA. Intercomparison with other existing BA datasets found similar spatial and temporal trends, mainly with the BA included in the Global Fire Emissions Database (GFED4), although regional differences were found (particularly in the 2006 fires of eastern Europe). The simulated carbon emissions from biomass burning averaged 2.1 Pg C year-1.},
keywords = {*imported-from-citeulike-INRMM,~INRMM-MiD:c-14257088,~to-add-doi-URL,burnt-area,carbon-emissions,climate-change,fire-emissions,global-scale,wildfires},
number = {5}
}
HISDAC-US, Historical Settlement Data Compilation for the Conterminous United States over 200 Years. Leyk, S. & Uhl, J. H. 5:180175+. Paper doi abstract bibtex Human settlement plays a key role in understanding social processes such as urbanization and interactions between human and environmental systems but not much is known about the landscape evolution before the era of operational remote sensing technology. In this study, housing and property databases are used to create new gridded settlement layers describing human settlement processes at fine spatial and temporal resolution in the conterminous United States between 1810 and 2015. The main products are a raster composite layer representing the year of first settlement, and a raster time series of built-up intensity representing the sum of building areas in a pixel. Several accompanying uncertainty surfaces are provided to ensure the user is informed about inherent spatial, temporal and thematic uncertainty in the data. A validation study using high quality reference data confirms high levels of accuracy of the resulting data products. These settlement data will be of great interest in disciplines in which the long-term evolution of human settlement represents crucial information to explore novel research questions.
@article{leykHISDACUSHistoricalSettlement2018,
title = {{{HISDAC}}-{{US}}, Historical Settlement Data Compilation for the Conterminous {{United States}} over 200 Years},
author = {Leyk, Stefan and Uhl, Johannes H.},
date = {2018-09},
journaltitle = {Scientific Data},
volume = {5},
pages = {180175+},
issn = {2052-4463},
doi = {10.1038/sdata.2018.175},
url = {https://doi.org/10.1038/sdata.2018.175},
abstract = {Human settlement plays a key role in understanding social processes such as urbanization and interactions between human and environmental systems but not much is known about the landscape evolution before the era of operational remote sensing technology. In this study, housing and property databases are used to create new gridded settlement layers describing human settlement processes at fine spatial and temporal resolution in the conterminous United States between 1810 and 2015. The main products are a raster composite layer representing the year of first settlement, and a raster time series of built-up intensity representing the sum of building areas in a pixel. Several accompanying uncertainty surfaces are provided to ensure the user is informed about inherent spatial, temporal and thematic uncertainty in the data. A validation study using high quality reference data confirms high levels of accuracy of the resulting data products. These settlement data will be of great interest in disciplines in which the long-term evolution of human settlement represents crucial information to explore novel research questions.},
keywords = {*imported-from-citeulike-INRMM,~INRMM-MiD:c-14633453,~to-add-doi-URL,data-integration,historical-perspective,human-settlement,integrated-modelling,integration-techniques,open-data,time-series,uncertainty,united-states}
}
Italian Scientists Vilified in Wake of Olive-Tree Deaths. Abbott, A. Paper doi abstract bibtex [Excerpt] [...] plant scientists at various institutes in Bari, the capital of the Puglia region, [southern Italy, ...] have been subject to a police investigation about whether they are responsible for the introduction of the bacterium, Xylella fastidiosa, into Puglia, or for allowing its subsequent spread. Police have called in several researchers involved in Xylella research for questioning and confiscated computers and documents from scientific institutes. ” We'd just like to be left to do our work without this suspicion and this stress,” says Donato Boscia, head of the Bari unit of the CNR Institute for Sustainable Plant Protection (IPSP), whom police questioned in April. [...] Xylella is endemic in parts of the Americas, including Costa Rica, Brazil and California, but was not previously found in Europe. That changed in October 2013, when scientists at the IPSP and the University of Bari identified the bacterium as the cause of an unusual disease outbreak in olive trees. The outbreak immediately became subject to European Union (EU) regulations to limit its spread, and regional scientists began a systematic effort to understand the disease and contain it: the scientists went on to show that the bacterium was being carried by the spittlebug insect. [::Ornamental plants] From the start, farmers and environmentalists in Italy objected to containment measures, which involved uprooting trees and spraying the groves with pesticides. But trouble for the Puglian scientists began in April 2014, when individuals told police that they suspected that the epidemic was caused by bacteria that scientists had brought in from California for a European training course on Xylella at the Mediterranean Agronomic Institute of Bari (IAMB) in 2010. [\n] Scientists say that this suggestion is ludicrous because the Puglia strain is different from the strains used at the workshop; the widely accepted theory is that the infection was imported with ornamental plants from Costa Rica, where the endemic Xylella strain matches the Puglia strain. [\n] However, the complaints spawned a much broader investigation by public prosecutors, including what role scientists may have had in the epidemic. [...] The prosecutors declined Nature's request for comment. But in March, one of them [...] implied in an interview [...] that they are looking into theories that the bacterium may have been deliberately introduced into the area, or became entrenched because agricultural scientists failed to monitor the region properly, either deliberately or through neglect. [...The prosecutor expressed concern] about the possible corrupting influence of businesses, such as solar-energy companies, which might stand to gain from the clearing of olive groves. [...] [\n] Puglian scientists have had to contend with public criticism too. Several popular blogs devoted to the Xylella emergency have cast doubt on scientists' ways of working and their results – saying, for example, that a remedy exists but is being suppressed [... and] that Xylella had not been proved to be the source of the outbreak and that the deaths were instead due to a fungus that could be eliminated without destroying trees. An expert panel of the European Food Safety Authority debunked these suggestions in a report published in April. [...] [\n] On 27 May, the regional government announced a €2-million (US\$2.2-million) fund for projects that might aid the diagnosis, epidemiology and monitoring of the bacterium. It said that a 'containment area' in the province of Lecce – where the bacterium is now endemic, making complete eradication impossible – will be used as an open-air Xylella laboratory. National and European research agencies have also promised money, says Boscia. ” The outdoor laboratory would be perfect for all of us – and also allow critics to put their own theories to the test.”
@article{abbottItalianScientistsVilified2015,
title = {Italian Scientists Vilified in Wake of Olive-Tree Deaths},
author = {Abbott, Alison},
date = {2015-06},
journaltitle = {Nature},
issn = {1476-4687},
doi = {10.1038/nature.2015.17651},
url = {https://doi.org/10.1038/nature.2015.17651},
abstract = {[Excerpt] [...] plant scientists at various institutes in Bari, the capital of the Puglia region, [southern Italy, ...] have been subject to a police investigation about whether they are responsible for the introduction of the bacterium, Xylella fastidiosa, into Puglia, or for allowing its subsequent spread. Police have called in several researchers involved in Xylella research for questioning and confiscated computers and documents from scientific institutes. ” We'd just like to be left to do our work without this suspicion and this stress,” says Donato Boscia, head of the Bari unit of the CNR Institute for Sustainable Plant Protection (IPSP), whom police questioned in April. [...]
Xylella is endemic in parts of the Americas, including Costa Rica, Brazil and California, but was not previously found in Europe. That changed in October 2013, when scientists at the IPSP and the University of Bari identified the bacterium as the cause of an unusual disease outbreak in olive trees. The outbreak immediately became subject to European Union (EU) regulations to limit its spread, and regional scientists began a systematic effort to understand the disease and contain it: the scientists went on to show that the bacterium was being carried by the spittlebug insect.
[::Ornamental plants]
From the start, farmers and environmentalists in Italy objected to containment measures, which involved uprooting trees and spraying the groves with pesticides. But trouble for the Puglian scientists began in April 2014, when individuals told police that they suspected that the epidemic was caused by bacteria that scientists had brought in from California for a European training course on Xylella at the Mediterranean Agronomic Institute of Bari (IAMB) in 2010.
[\textbackslash n] Scientists say that this suggestion is ludicrous because the Puglia strain is different from the strains used at the workshop; the widely accepted theory is that the infection was imported with ornamental plants from Costa Rica, where the endemic Xylella strain matches the Puglia strain.
[\textbackslash n] However, the complaints spawned a much broader investigation by public prosecutors, including what role scientists may have had in the epidemic. [...] The prosecutors declined Nature's request for comment. But in March, one of them [...] implied in an interview [...] that they are looking into theories that the bacterium may have been deliberately introduced into the area, or became entrenched because agricultural scientists failed to monitor the region properly, either deliberately or through neglect. [...The prosecutor expressed concern] about the possible corrupting influence of businesses, such as solar-energy companies, which might stand to gain from the clearing of olive groves. [...]
[\textbackslash n] Puglian scientists have had to contend with public criticism too. Several popular blogs devoted to the Xylella emergency have cast doubt on scientists' ways of working and their results -- saying, for example, that a remedy exists but is being suppressed [... and] that Xylella had not been proved to be the source of the outbreak and that the deaths were instead due to a fungus that could be eliminated without destroying trees. An expert panel of the European Food Safety Authority debunked these suggestions in a report published in April. [...]
[\textbackslash n] On 27 May, the regional government announced a €2-million (US\$2.2-million) fund for projects that might aid the diagnosis, epidemiology and monitoring of the bacterium. It said that a 'containment area' in the province of Lecce -- where the bacterium is now endemic, making complete eradication impossible -- will be used as an open-air Xylella laboratory. National and European research agencies have also promised money, says Boscia. ” The outdoor laboratory would be perfect for all of us -- and also allow critics to put their own theories to the test.”},
keywords = {*imported-from-citeulike-INRMM,~INRMM-MiD:c-13636189,~to-add-doi-URL,agricultural-resources,complexity,disturbances,forest-resources,multi-stakeholder-decision-making,olea-europaea,plant-pests,science-based-decision-making,science-ethics,science-policy-interface,science-society-interface,scientific-communication,solar-energy,uncertainty,xylella-fastidiosa}
}
Wildfire Smoke Exposure: A Guide for the Nurse Practitioner. Forsberg, N. T., Longo, B. M., Baxter, K., & Boutté, M. 8(2):98–106. Paper doi abstract bibtex Wildfires produce enormous quantities of finely sized air pollution. Exposure to wildfire smoke is associated with increased incidence of cardio-respiratory health effects, especially in children, persons with chronic disease, and the elderly. This article discusses exposure to particle air pollution, toxicological mechanisms, timing of clinical presentations, and treatment guidelines for use by the nurse practitioner during smoke events.
@article{forsbergWildfireSmokeExposure2012,
title = {Wildfire Smoke Exposure: A Guide for the Nurse Practitioner},
author = {Forsberg, Nicole T. and Longo, Bernadette M. and Baxter, Kimberly and Boutté, Marie},
date = {2012-02},
journaltitle = {The Journal for Nurse Practitioners},
volume = {8},
pages = {98--106},
issn = {1555-4155},
doi = {10.1016/j.nurpra.2011.07.001},
url = {https://doi.org/10.1016/j.nurpra.2011.07.001},
abstract = {Wildfires produce enormous quantities of finely sized air pollution. Exposure to wildfire smoke is associated with increased incidence of cardio-respiratory health effects, especially in children, persons with chronic disease, and the elderly. This article discusses exposure to particle air pollution, toxicological mechanisms, timing of clinical presentations, and treatment guidelines for use by the nurse practitioner during smoke events.},
keywords = {*imported-from-citeulike-INRMM,~INRMM-MiD:c-14617565,~to-add-doi-URL,adaptation,air-pollution,check-list,fire-emissions,guidelines,human-health,mortality,particulate-matter,smoke,wildfires},
number = {2}
}
What Can Machine Learning Do? Workforce Implications. Brynjolfsson, E. & Mitchell, T. 358(6370):1530–1534. Paper doi abstract bibtex Digital computers have transformed work in almost every sector of the economy over the past several decades (1). We are now at the beginning of an even larger and more rapid transformation due to recent advances in machine learning (ML), which is capable of accelerating the pace of automation itself. However, although it is clear that ML is a ” general purpose technology,” like the steam engine and electricity, which spawns a plethora of additional innovations and capabilities (2), there is no widely shared agreement on the tasks where ML systems excel, and thus little agreement on the specific expected impacts on the workforce and on the economy more broadly. We discuss what we see to be key implications for the workforce, drawing on our rubric of what the current generation of ML systems can and cannot do [see the supplementary materials (SM)]. Although parts of many jobs may be ” suitable for ML” (SML), other tasks within these same jobs do not fit the criteria for ML well; hence, effects on employment are more complex than the simple replacement and substitution story emphasized by some. Although economic effects of ML are relatively limited today, and we are not facing the imminent ” end of work” as is sometimes proclaimed, the implications for the economy and the workforce going forward are profound.
@article{brynjolfssonWhatCanMachine2017,
title = {What Can Machine Learning Do? {{Workforce}} Implications},
author = {Brynjolfsson, Erik and Mitchell, Tom},
date = {2017-12},
journaltitle = {Science},
volume = {358},
pages = {1530--1534},
issn = {0036-8075},
doi = {10.1126/science.aap8062},
url = {https://doi.org/10.1126/science.aap8062},
abstract = {Digital computers have transformed work in almost every sector of the economy over the past several decades (1). We are now at the beginning of an even larger and more rapid transformation due to recent advances in machine learning (ML), which is capable of accelerating the pace of automation itself. However, although it is clear that ML is a ” general purpose technology,” like the steam engine and electricity, which spawns a plethora of additional innovations and capabilities (2), there is no widely shared agreement on the tasks where ML systems excel, and thus little agreement on the specific expected impacts on the workforce and on the economy more broadly. We discuss what we see to be key implications for the workforce, drawing on our rubric of what the current generation of ML systems can and cannot do [see the supplementary materials (SM)]. Although parts of many jobs may be ” suitable for ML” (SML), other tasks within these same jobs do not fit the criteria for ML well; hence, effects on employment are more complex than the simple replacement and substitution story emphasized by some. Although economic effects of ML are relatively limited today, and we are not facing the imminent ” end of work” as is sometimes proclaimed, the implications for the economy and the workforce going forward are profound.},
keywords = {*imported-from-citeulike-INRMM,~INRMM-MiD:c-14507143,~to-add-doi-URL,artificial-intelligence,artificial-neural-networks,automation,computational-science,ethics,human-behaviour,human-centered-automation,human-machine-interface,machine-learning,science-ethics},
number = {6370}
}
Soil Erosion Assessment - Mind the Gap. Kim, J., Ivanov, V. Y., & Fatichi, S. 43(24):2016GL071480+. Paper doi abstract bibtex Accurate assessment of erosion rates remains an elusive problem because soil loss is strongly nonunique with respect to the main drivers. In addressing the mechanistic causes of erosion responses, we discriminate between macroscale effects of external factors – long studied and referred to as ” geomorphic external variability”, and microscale effects, introduced as ” geomorphic internal variability.” The latter source of erosion variations represents the knowledge gap, an overlooked but vital element of geomorphic response, significantly impacting the low predictability skill of deterministic models at field-catchment scales. This is corroborated with experiments using a comprehensive physical model that dynamically updates the soil mass and particle composition. As complete knowledge of microscale conditions for arbitrary location and time is infeasible, we propose that new predictive frameworks of soil erosion should embed stochastic components in deterministic assessments of external and internal types of geomorphic variability.
@article{kimSoilErosionAssessment2016,
title = {Soil Erosion Assessment - {{Mind}} the Gap},
author = {Kim, Jongho and Ivanov, Valeriy Y. and Fatichi, Simone},
date = {2016-12},
journaltitle = {Geophys. Res. Lett.},
volume = {43},
pages = {2016GL071480+},
issn = {0094-8276},
doi = {10.1002/2016gl071480},
url = {http://mfkp.org/INRMM/article/14257841},
abstract = {Accurate assessment of erosion rates remains an elusive problem because soil loss is strongly nonunique with respect to the main drivers. In addressing the mechanistic causes of erosion responses, we discriminate between macroscale effects of external factors -- long studied and referred to as ” geomorphic external variability”, and microscale effects, introduced as ” geomorphic internal variability.” The latter source of erosion variations represents the knowledge gap, an overlooked but vital element of geomorphic response, significantly impacting the low predictability skill of deterministic models at field-catchment scales. This is corroborated with experiments using a comprehensive physical model that dynamically updates the soil mass and particle composition. As complete knowledge of microscale conditions for arbitrary location and time is infeasible, we propose that new predictive frameworks of soil erosion should embed stochastic components in deterministic assessments of external and internal types of geomorphic variability.},
keywords = {*imported-from-citeulike-INRMM,~INRMM-MiD:c-14257841,~to-add-doi-URL,erodibility,local-scale,modelling-uncertainty,soil-erosion,soil-resources,uncertainty},
number = {24}
}
Influence of Landscape Structure on Patterns of Forest Fires in Boreal Forest Landscapes in Sweden. Hellberg, E., Niklasson, M., & Granström, A. 34(2):332–338. Paper doi abstract bibtex To analyze the effect of landscape structure (viz. amount of wetlands) on the past forest fire regime in boreal Sweden, we reconstructed detailed fire histories by cross-dating fire scars in living and dead Scots pine (Pinus sylvestris L.) in two different landscape types: mire-free landscapes with a low proportion (1\,%-2\,%) of mires and mire-rich landscapes with a high proportion (21\,%-33\,%) of mires. Two localities were selected and at each one, adjacent mire-free and mire-rich areas of 256-601 ha were sampled. Over the studied 650-year period, the two landscape types differed primarily in the fire intervals and sizes of fires. In the mire-rich landscapes, fires had frequently stopped against mire elements. The net effect was significantly longer fire intervals in the mire-rich than in the mire-free landscape (on average, 32 versus 56 years). The mire-rich areas also had a tail of very long fire intervals lacking in the mire-free areas (maximal interval 292 years). We conclude that mires can have a profound effect on both spatial and temporal patterns of forest fires in the boreal forest, but only when they are effective fuel breaks (i.e., they are wet enough) at the time the fires burn and if they truly dissect the nonmire portion of the forest landscape.
@article{hellbergInfluenceLandscapeStructure2004,
title = {Influence of Landscape Structure on Patterns of Forest Fires in Boreal Forest Landscapes in {{Sweden}}},
author = {Hellberg, Erik and Niklasson, Mats and Granström, Anders},
date = {2004-02},
journaltitle = {Canadian Journal of Forest Research},
volume = {34},
pages = {332--338},
issn = {1208-6037},
doi = {10.1139/x03-175},
url = {http://mfkp.org/INRMM/article/14426179},
abstract = {To analyze the effect of landscape structure (viz. amount of wetlands) on the past forest fire regime in boreal Sweden, we reconstructed detailed fire histories by cross-dating fire scars in living and dead Scots pine (Pinus sylvestris L.) in two different landscape types: mire-free landscapes with a low proportion (1\,\%-2\,\%) of mires and mire-rich landscapes with a high proportion (21\,\%-33\,\%) of mires. Two localities were selected and at each one, adjacent mire-free and mire-rich areas of 256-601 ha were sampled. Over the studied 650-year period, the two landscape types differed primarily in the fire intervals and sizes of fires. In the mire-rich landscapes, fires had frequently stopped against mire elements. The net effect was significantly longer fire intervals in the mire-rich than in the mire-free landscape (on average, 32 versus 56 years). The mire-rich areas also had a tail of very long fire intervals lacking in the mire-free areas (maximal interval 292 years). We conclude that mires can have a profound effect on both spatial and temporal patterns of forest fires in the boreal forest, but only when they are effective fuel breaks (i.e., they are wet enough) at the time the fires burn and if they truly dissect the nonmire portion of the forest landscape.},
keywords = {*imported-from-citeulike-INRMM,~INRMM-MiD:c-14426179,~to-add-doi-URL,boreal-forests,fire-frequency,forest-fires,forest-resources,mires,spatial-pattern,water-resources,wetlands,wildfires},
number = {2}
}
Pest Categorisation of Melampsora Medusae. Jeger, M., Bragard, C., Caffier, D., Candresse, T., Chatzivassiliou, E., Dehnen-Schmutz, K., Gilioli, G., Grégoire, J., Jaques Miret, J. A., MacLeod, A., Navajas Navarro, M., Niere, B., Parnell, S., Potting, R., Rafoss, T., Rossi, V., Urek, G., Van Bruggen, A., Van der Werf, W., West, J., Winter, S., Boberg, J., Gonthier, P., & Pautasso, M. 16(7):e05354+. Paper doi abstract bibtex Following a request from the European Commission, the EFSA Plant Health Panel performed a pest categorisation of Melampsora medusae, a well-defined and distinguishable fungal species of the family Melampsoraceae. The pathogen is regulated in Annex IAI of Council Directive 2000/29/EC as a harmful organism whose introduction into the EU is banned. M. medusae is a heteroecious rust fungus with Populus spp. as primary telial hosts and various conifers (Larix, Pinus, Pseudotsuga, Abies, Picea and Tsuga spp.) as secondary aecial hosts. M. medusae is native to North America and has spread to South America, Africa, Asia, Oceania, as well as the EU, where M. medusae f. sp. deltoidae has been reported with a restricted distribution and low impacts from Belgium, south-west France and southern Portugal. The pest could spread to other EU countries, via dissemination of spores, movement of host plants for planting and cut branches. Climate is assumed not to be a limiting factor for the establishment of the pathogen in the EU. M. medusae is the most widespread and important Melampsora rust in North America. In western Canada, extensive damage has been reported to conifers and Populus spp. in nurseries and plantations as well as in woodlands. M. medusae is damaging in both Australia and New Zealand. The pest could have economic and environmental impacts in the EU if aggressive isolates of M. medusae were introduced into the EU. Import prohibition of host plants for planting is an available measure to reduce the risk of further introductions. Some resistant Populus cultivars are available. Moreover, increasing the genetic diversity of poplar plantations can prevent disease impacts. The main uncertainty concerns the factors explaining the low pathogenicity of the populations of M. medusae present in the EU. The criteria assessed by the Panel for consideration as a potential quarantine pest are met (the pest is present, but with a restricted distribution, and is officially under control). Given that plants for planting are not the main pathway of spread, not all criteria for consideration as a regulated non-quarantine pest are met. [Excerpt: Conclusions] [...] [::Identity of the pest] The identity of the pest as a species is clear. [] [...] [] The recent change in name from Ceratocystis fagacearum to Bretziella fagacearum may take time for acceptance by the scientific community. [...] [::Absence/presence of the pest in the EU territory] M. medusae is present, although not widespread, in the EU (and only represented by M. medusae f. sp. deltoidae). It is reported as present with few occurrences both in Belgium and France, and present with a restricted distribution in South Portugal. [...] [::Regulatory status] M. medusae is regulated by Council Directive 2000/29/EC (Annex IAI) as a harmful organism whose introduction into, and spread within, all Member States shall be banned. [] [...] [::Pest potential for entry, establishment and spread in the EU territory] Entry: the pest could enter the EU via host plants for planting and cut branches. [] Establishment: hosts and favourable climatic conditions are widespread in the risk assessment area. [] Spread: hosts and favourable climatic conditions are widespread in the risk assessment area. [] [...] [] Plants for planting are not the main means of spread, as the pathogen can also spread via cut branches and aerial dissemination of spores. [] [...] [] There is uncertainty about which factors are limiting the spread of M. medusae in the EU MS which have reported the pathogen (overwintering problems, host alternation or ecological constraints). [] There is uncertainty about the level of susceptibility of the native P. alba and P. tremula. [...] [::Potential for consequences in the EU territory] The introduction into the EU of aggressive isolates of M. medusae (of both the already present M. medusae f. sp. deltoidae and the not known to occur M. medusae f. sp. tremuloides) would have economic and environmental impacts in woodlands, poplar plantations and nurseries. [] [...] [] The introduction into the EU of aggressive isolates of M. medusae (of both the already present M. medusae f. sp. deltoidae and the not known to occur M. medusae f. sp. tremuloides) would have an impact on the intended use of plants for planting. [] [...] [] It is unclear if low pathogenicity of populations of either f. sp. of M. medusae may be due to their reduced life cycle characteristics. [...] [::Available measures] Import prohibition of host plants for planting is an available measure to reduce the risk of introduction. [] Some resistant Populus cultivars are available. Moreover, increasing host genetic diversity can prevent disease impacts. [] [...] [] Production of plants for planting in pest free areas and places of production can prevent pest presence on plants for planting. [] [...] [] The effectiveness of pest free areas for the production of clean nursery stock is uncertain, due to the long-distance dispersal potential of the rust. [...] [::Conclusion on pest categorisation] The criteria assessed by the Panel for consideration as a potential quarantine pest are met. The pathogen is present in the EU but with a restricted distribution and is under official control. [] [...] [] The criterion on plants for planting as the main pathway of spread is not met. [...] [::Aspects of assessment to focus on/scenarios to address in future if appropriate] The main knowledge gap concerns the factors responsible for the low aggressiveness of the populations of M. medusae present in Europe. [...]
@article{jegerPestCategorisationMelampsora2018,
title = {Pest Categorisation of {{Melampsora}} Medusae},
author = {Jeger, Michael and Bragard, Claude and Caffier, David and Candresse, Thierry and Chatzivassiliou, Elisavet and Dehnen-Schmutz, Katharina and Gilioli, Gianni and Grégoire, Jean-Claude and Jaques Miret, Josep A. and MacLeod, Alan and Navajas Navarro, Maria and Niere, Björn and Parnell, Stephen and Potting, Roel and Rafoss, Trond and Rossi, Vittorio and Urek, Gregor and Van Bruggen, Ariena and Van der Werf, Wopke and West, Jonathan and Winter, Stephan and Boberg, Johanna and Gonthier, Paolo and Pautasso, Marco},
date = {2018-07},
journaltitle = {EFSA Journal},
volume = {16},
pages = {e05354+},
issn = {1831-4732},
doi = {10.2903/j.efsa.2018.5354},
url = {https://doi.org/10.2903/j.efsa.2018.5354},
abstract = {Following a request from the European Commission, the EFSA Plant Health Panel performed a pest categorisation of Melampsora medusae, a well-defined and distinguishable fungal species of the family Melampsoraceae. The pathogen is regulated in Annex IAI of Council Directive 2000/29/EC as a harmful organism whose introduction into the EU is banned. M. medusae is a heteroecious rust fungus with Populus spp. as primary telial hosts and various conifers (Larix, Pinus, Pseudotsuga, Abies, Picea and Tsuga spp.) as secondary aecial hosts. M. medusae is native to North America and has spread to South America, Africa, Asia, Oceania, as well as the EU, where M. medusae f. sp. deltoidae has been reported with a restricted distribution and low impacts from Belgium, south-west France and southern Portugal. The pest could spread to other EU countries, via dissemination of spores, movement of host plants for planting and cut branches. Climate is assumed not to be a limiting factor for the establishment of the pathogen in the EU. M. medusae is the most widespread and important Melampsora rust in North America. In western Canada, extensive damage has been reported to conifers and Populus spp. in nurseries and plantations as well as in woodlands. M. medusae is damaging in both Australia and New Zealand. The pest could have economic and environmental impacts in the EU if aggressive isolates of M. medusae were introduced into the EU. Import prohibition of host plants for planting is an available measure to reduce the risk of further introductions. Some resistant Populus cultivars are available. Moreover, increasing the genetic diversity of poplar plantations can prevent disease impacts. The main uncertainty concerns the factors explaining the low pathogenicity of the populations of M. medusae present in the EU. The criteria assessed by the Panel for consideration as a potential quarantine pest are met (the pest is present, but with a restricted distribution, and is officially under control). Given that plants for planting are not the main pathway of spread, not all criteria for consideration as a regulated non-quarantine pest are met.
[Excerpt: Conclusions] [...] [::Identity of the pest] The identity of the pest as a species is clear. [] [...] [] The recent change in name from Ceratocystis fagacearum to Bretziella fagacearum may take time for acceptance by the scientific community. [...]
[::Absence/presence of the pest in the EU territory] M. medusae is present, although not widespread, in the EU (and only represented by M. medusae f. sp. deltoidae). It is reported as present with few occurrences both in Belgium and France, and present with a restricted distribution in South Portugal. [...]
[::Regulatory status] M. medusae is regulated by Council Directive 2000/29/EC (Annex IAI) as a harmful organism whose introduction into, and spread within, all Member States shall be banned. [] [...]
[::Pest potential for entry, establishment and spread in the EU territory] Entry: the pest could enter the EU via host plants for planting and cut branches.
[] Establishment: hosts and favourable climatic conditions are widespread in the risk assessment area.
[] Spread: hosts and favourable climatic conditions are widespread in the risk assessment area. [] [...]
[] Plants for planting are not the main means of spread, as the pathogen can also spread via cut branches and aerial dissemination of spores. [] [...]
[] There is uncertainty about which factors are limiting the spread of M. medusae in the EU MS which have reported the pathogen (overwintering problems, host alternation or ecological constraints).
[] There is uncertainty about the level of susceptibility of the native P. alba and P. tremula. [...]
[::Potential for consequences in the EU territory] The introduction into the EU of aggressive isolates of M. medusae (of both the already present M. medusae f. sp. deltoidae and the not known to occur M. medusae f. sp. tremuloides) would have economic and environmental impacts in woodlands, poplar plantations and nurseries. [] [...] [] The introduction into the EU of aggressive isolates of M. medusae (of both the already present M. medusae f. sp. deltoidae and the not known to occur M. medusae f. sp. tremuloides) would have an impact on the intended use of plants for planting. [] [...] [] It is unclear if low pathogenicity of populations of either f. sp. of M. medusae may be due to their reduced life cycle characteristics. [...]
[::Available measures] Import prohibition of host plants for planting is an available measure to reduce the risk of introduction.
[] Some resistant Populus cultivars are available. Moreover, increasing host genetic diversity can prevent disease impacts. [] [...]
[] Production of plants for planting in pest free areas and places of production can prevent pest presence on plants for planting. [] [...]
[] The effectiveness of pest free areas for the production of clean nursery stock is uncertain, due to the long-distance dispersal potential of the rust. [...]
[::Conclusion on pest categorisation] The criteria assessed by the Panel for consideration as a potential quarantine pest are met. The pathogen is present in the EU but with a restricted distribution and is under official control. [] [...]
[] The criterion on plants for planting as the main pathway of spread is not met. [...]
[::Aspects of assessment to focus on/scenarios to address in future if appropriate] The main knowledge gap concerns the factors responsible for the low aggressiveness of the populations of M. medusae present in Europe. [...]},
keywords = {*imported-from-citeulike-INRMM,~INRMM-MiD:c-14636135,~to-add-doi-URL,abies-spp,disturbances,efsa,efsa-scientific-opinion,europe,forest-pests,forest-resources,fungal-diseases,fungi,larix-spp,melampsora-medusae,picea-spp,pinus-spp,plant-pests,populus-spp,pseudotsuga-spp,tsuga-spp},
number = {7}
}
The Use of Terrestrial LiDAR Technology in Forest Science: Application Fields, Benefits and Challenges. Dassot, M., Constant, T., & Fournier, M. 68(5):959–974. Paper doi abstract bibtex [Introduction] The use of terrestrial LiDAR (light detection and ranging) scanners in forest environments is being studied extensively at present due to the high potential of this technology to acquire three-dimensional data on standing trees rapidly and accurately. This article aims to establish the state-of-the-art in this emerging area. [Objectives] Terrestrial LiDAR has been applied to forest inventory measurements (plot cartography, species recognition, diameter at breast height, tree height, stem density, basal area and plot-level wood volume estimates) and canopy characterisation (virtual projections, gap fraction and three-dimensional foliage distribution). These techniques have been extended to stand value and wood quality assessment. Terrestrial LiDAR also provides new support for ecological applications such as the assessment of the physical properties of leaves, transpiration processes and microhabitat diversity. [Results] Since 2003, both the capabilities of the devices and data processing technology have improved significantly, with encouraging results. Nevertheless, measurement patterns and device specifications must be selected carefully according to the objectives of the study. Moreover, automated and reliable programmes are still required to process data to make these methodologies applicable specifically to the forest sciences and to fill the gap between time-consuming manual methods and wide-scale remote sensing such as airborne LiDAR scanning. [Excerpt: Conclusions] The aim of this article was to establish the state-of-the-art of the current applications of T-LiDAR technology in forest science, as well as to determine its applicability for its intended use. It appears that T-LiDAR instruments have the potential to enhance forest measurements and to overcome metrological difficulties by describing the under-canopy structure faster and in greater detail than time-consuming manual techniques. T-LiDAR scanning also provides information inaccessible to large-scale airborne LiDAR measurements. Its potential implications in the fields of forest inventories, commercial wood management and forest ecology are many. Two aspects need to be improved to make this technology specifically applicable to forestry. The first concerns the T-LiDAR devices themselves, particularly in terms of acquisition time, signal-to-noise ratio, and cost. The second concerns the development of cheap and easy-to-use software that would make it possible to automatically extract information from incomplete data. T-LiDAR has also been used within the field of forest ecology over the past few years. These studies concerned very specific applications, but demonstrated the potential of this technology to provide a good background for ecological questions such as microhabitat distribution and the assessment of the ecological processes that occur in the forest environment. Despite the maturity of these devices, some progress remains to be made in the analysis of the 3D cloud to enhance the extraction of relevant information. There is no doubt that the evolution of devices and computing science will make T-LiDAR technology an important source of information for describing natural environments in the future.
@article{dassotUseTerrestrialLiDAR2011,
title = {The Use of Terrestrial {{LiDAR}} Technology in Forest Science: Application Fields, Benefits and Challenges},
author = {Dassot, Mathieu and Constant, Thiéry and Fournier, Meriem},
date = {2011},
journaltitle = {Annals of Forest Science},
volume = {68},
pages = {959--974},
issn = {1297-966X},
doi = {10.1007/s13595-011-0102-2},
url = {http://mfkp.org/INRMM/article/13704459},
abstract = {[Introduction] The use of terrestrial LiDAR (light detection and ranging) scanners in forest environments is being studied extensively at present due to the high potential of this technology to acquire three-dimensional data on standing trees rapidly and accurately. This article aims to establish the state-of-the-art in this emerging area.
[Objectives] Terrestrial LiDAR has been applied to forest inventory measurements (plot cartography, species recognition, diameter at breast height, tree height, stem density, basal area and plot-level wood volume estimates) and canopy characterisation (virtual projections, gap fraction and three-dimensional foliage distribution). These techniques have been extended to stand value and wood quality assessment. Terrestrial LiDAR also provides new support for ecological applications such as the assessment of the physical properties of leaves, transpiration processes and microhabitat diversity.
[Results] Since 2003, both the capabilities of the devices and data processing technology have improved significantly, with encouraging results. Nevertheless, measurement patterns and device specifications must be selected carefully according to the objectives of the study. Moreover, automated and reliable programmes are still required to process data to make these methodologies applicable specifically to the forest sciences and to fill the gap between time-consuming manual methods and wide-scale remote sensing such as airborne LiDAR scanning.
[Excerpt: Conclusions] The aim of this article was to establish the state-of-the-art of the current applications of T-LiDAR technology in forest science, as well as to determine its applicability for its intended use. It appears that T-LiDAR instruments have the potential to enhance forest measurements and to overcome metrological difficulties by describing the under-canopy structure faster and in greater detail than time-consuming manual techniques. T-LiDAR scanning also provides information inaccessible to large-scale airborne LiDAR measurements. Its potential implications in the fields of forest inventories, commercial wood management and forest ecology are many. Two aspects need to be improved to make this technology specifically applicable to forestry. The first concerns the T-LiDAR devices themselves, particularly in terms of acquisition time, signal-to-noise ratio, and cost. The second concerns the development of cheap and easy-to-use software that would make it possible to automatically extract information from incomplete data. T-LiDAR has also been used within the field of forest ecology over the past few years. These studies concerned very specific applications, but demonstrated the potential of this technology to provide a good background for ecological questions such as microhabitat distribution and the assessment of the ecological processes that occur in the forest environment. Despite the maturity of these devices, some progress remains to be made in the analysis of the 3D cloud to enhance the extraction of relevant information. There is no doubt that the evolution of devices and computing science will make T-LiDAR technology an important source of information for describing natural environments in the future.},
keywords = {*imported-from-citeulike-INRMM,~INRMM-MiD:c-13704459,~to-add-doi-URL,data,ecology,field-measurements,forest-resources,inventories,lidar,remote-sensing,terrestrial-lidar,wide-scale},
number = {5}
}
Phenolic Profile in the Quality Control of Walnut (Juglans Regia L.) Leaves. Amaral, J. S., Seabra, R. M., Andrade, P. B., Valentão, P., Pereira, J. A., & Ferreres, F. 88(3):373–379. Paper doi abstract bibtex Qualitative and quantitative determinations of phenolic compounds were carried out on walnut leaves samples from six different cultivars, with the same agricultural, geographical and climatic conditions. The evolution of major phenolic compounds amounts was monitored from May to September. Two extractive procedures were assayed and best results were obtained using acidified water and a solid phase extraction column purification step. Qualitative analysis was performed by HPLC-DAD/MS and, in all samples, seven phenolic compounds were identified (3-caffeoylquinic, 3-p-coumaroylquinic and 4-p-coumaroylquinic acids, quercetin 3-galactoside, quercetin 3-arabinoside, quercetin 3-xyloside, quercetin 3-rhamnoside) and two other partially identified phenolics (quercetin 3-pentoside and kaempferol 3-pentoside derivatives) were also detected. Quantification of phenolic compounds was performed by HPLC-DAD, which revealed that quercetin 3-galactoside was always the major compound while 4-p-coumaroylquinic acid was the minor one. The highest content of phenolics was found in May and July.
@article{amaralPhenolicProfileQuality2004,
title = {Phenolic Profile in the Quality Control of Walnut ({{Juglans}} Regia {{L}}.) Leaves},
author = {Amaral, Joana S. and Seabra, Rosa M. and Andrade, Paula B. and Valentão, Patŕıcia and Pereira, José A. and Ferreres, Federico},
date = {2004},
journaltitle = {Food Chemistry},
volume = {88},
pages = {373--379},
doi = {10.1016/j.foodchem.2004.01.055},
url = {https://doi.org/10.1016/j.foodchem.2004.01.055},
abstract = {Qualitative and quantitative determinations of phenolic compounds were carried out on walnut leaves samples from six different cultivars, with the same agricultural, geographical and climatic conditions. The evolution of major phenolic compounds amounts was monitored from May to September. Two extractive procedures were assayed and best results were obtained using acidified water and a solid phase extraction column purification step. Qualitative analysis was performed by HPLC-DAD/MS and, in all samples, seven phenolic compounds were identified (3-caffeoylquinic, 3-p-coumaroylquinic and 4-p-coumaroylquinic acids, quercetin 3-galactoside, quercetin 3-arabinoside, quercetin 3-xyloside, quercetin 3-rhamnoside) and two other partially identified phenolics (quercetin 3-pentoside and kaempferol 3-pentoside derivatives) were also detected. Quantification of phenolic compounds was performed by HPLC-DAD, which revealed that quercetin 3-galactoside was always the major compound while 4-p-coumaroylquinic acid was the minor one. The highest content of phenolics was found in May and July.},
keywords = {*imported-from-citeulike-INRMM,~INRMM-MiD:c-13576805,~to-add-doi-URL,juglans-regia,phenolic-compounds,walnut-leaf},
number = {3}
}
Escaping RGBland: Selecting Colors for Statistical Graphics. Zeileis, A., Hornik, K., & Murrell, P. 53(9):3259–3270. Paper doi abstract bibtex Statistical graphics are often augmented by the use of color coding information contained in some variable. When this involves the shading of areas (and not only points or lines) – e.g.,~as in bar plots, pie charts, mosaic displays or heatmaps – it is important that the colors are perceptually based and do not introduce optical illusions or systematic bias. Based on the perceptually-based Hue-Chroma-Luminance (HCL) color space suitable color palettes are derived for coding categorical data (qualitative palettes) and numerical variables (sequential and diverging palettes).
@article{zeileisEscapingRGBlandSelecting2009,
title = {Escaping {{RGBland}}: Selecting Colors for Statistical Graphics},
author = {Zeileis, Achim and Hornik, Kurt and Murrell, Paul},
date = {2009-07},
journaltitle = {Computational Statistics \& Data Analysis},
volume = {53},
pages = {3259--3270},
issn = {0167-9473},
doi = {10.1016/j.csda.2008.11.033},
url = {https://doi.org/10.1126/science.1229881},
abstract = {Statistical graphics are often augmented by the use of color coding information contained in some variable. When this involves the shading of areas (and not only points or lines) -- e.g.,~as in bar plots, pie charts, mosaic displays or heatmaps -- it is important that the colors are perceptually based and do not introduce optical illusions or systematic bias. Based on the perceptually-based Hue-Chroma-Luminance (HCL) color space suitable color palettes are derived for coding categorical data (qualitative palettes) and numerical variables (sequential and diverging palettes).},
keywords = {*imported-from-citeulike-INRMM,~INRMM-MiD:c-5094127,~to-add-doi-URL,cognitive-structure,scientific-communication,semantics,technology-mediated-communication,visual-notation,visualization},
number = {9}
}
Dalby Söderskog Revisited: Long-Term Vegetation Changes in a South Swedish Deciduous Forest. von Oheimb, G. & Brunet, J. 31(2):229–242. Paper doi abstract bibtex In this study, we report on 67 years of secondary succession in the temperate deciduous forest Dalby Söderskog, southern Sweden. In 2002 vegetation analyses were conducted in 74 systematically distributed plots and the results compared with similar investigations during the years 1935, 1969 and 1976. Additionally, a floristic survey of the forest was made and compared with inventories of the years 1925, 1935 and 1970. From 1970 to 2002, overall species richness of the forest continued to decline, but at a lower rate than before. In 2002, for the first time, shade-tolerant forest species constituted the largest group. In the upper tree layer Fraxinus excelsior became the most important species, at the expense of Quercus robur and Ulmus glabra. In the herb layer, no changes in total or mean species richness were exhibited at plot scale between 1976 and 2002. In contrast to the lack of quantitative changes in species richness, we observed major changes in species composition at the plot level. In particular, the former dominant species Mercurialis perennis had declined markedly. After release from a historical regime of livestock grazing and irregular cuttings, the predicted steady-state community dominated by Ulmus and Mercurialis only prevailed for a few decades before unexpected external events, in this particular case Dutch elm disease and invasion by the slug Arion lusitanicus, initiated a successional change. We conclude that unexpected diseases or pests or rare climatic extremes can play a decisive role in forest dynamics and strongly interact with more gradual autogenic changes of forest structure and composition. [Excerpt: Changes in the tree and shrub layer] A similar long-term decline in regeneration of Quercus spp., such as observed in Dalby Söderskog, has been reported from a wide range of forest reserves in Europe and North America ( Glitzenstein et al., 1986, Emborg et al., 1996, Vera, 2000, Cowell and Jackson, 2002, Harcombe et al., 2002, Runkle et al., 2005 and von Oheimb et al., 2005). The present Quercus canopy trees are relicts of the more open stand structure of former times and do not regenerate under a closed canopy ( Table 2). In the absence of management, Lindquist, 1938 and Malmer et al., 1978 and Diekmann (1994) suggest that Ulmus would be the dominating tree species on moist eutric cambisols due to its characteristics as a shade-bearing, late-successional species, with the advanced regeneration exhibiting a higher shade-tolerance and the canopy trees having a higher competitive vigour than the early- to mid-successional species Fraxinus. Leemans (1992) used the forest succession model FORSKA to simulate species composition and stand structure of Dalby Söderskog. Starting the simulation run in 1920, the author found that species composition stabilized after 100 years as a forest of Ulmus, with scattered individuals of Fraxinus and Quercus. Fagus remained limited to the patches which initially had a high Fagus abundance. [\n] However, Diekmann (1994) suggested the Dutch elm disease (DED) had the potential to reverse these future trends. DED is a response of Ulmus spp. to infection by the fungus Ophiostoma novo-ulmi, which is spread by Scolytus beetles ( Röhrig, 1996). A particularly aggressive strain of DED was first recorded in Sk˚ane in 1979. In 1986, Dalby Söderskog was not yet visibly damaged ( Persson, 1987), but DED started to spread in the reserve during the following years. In order to reduce damage, 10-70 Ulmus trees were cut per year in Dalby Söderskog between 1988 and 1997 (pers. comm., 2002, County Board of Sk˚ane). By 2002, a considerable proportion of the Ulmus canopy trees had been killed or infected by DED (personal observation). [\n] In an unmanaged Ulmus glabra population in Lady Park Wood (western Britain), which has been recorded since 1945 and which has been subjected to DED since 1972, Peterken and Mountford (1998) found that about 65\,% of the individuals present 40 years ago have been killed by DED. However, the population increased 1.4 times during this period. In particular on moist sites of the forest, seedling regeneration was the main survival mechanism and a few individuals survived by producing basal sprouts. While Ulmus recruitment from seedlings was infrequent before the onset of DED in Lady Park Wood, new saplings established soon after the canopy had been opened up. Peterken and Mountford (1998) suggest that, unless DED abates, Ulmus seems likely to persist as a fast turnover population of poles that never reaches the forest canopy. In a population of Ulmus americana in Michigan most of the larger trees were killed by DED, but the species remained dominant in the understorey ( Richardson and Cares, 1976). Based on the vegetation data of the plots, the impact of DED seems to result in similar changes of the Ulmus population in Dalby Söderskog. [\n] [...] [Conclusions] Considering seven decades of vegetation changes in Dalby Söderskog, our results highlight the role of unpredictable historical events that strongly influence the process of autogenic succession. In most places, disturbance after windstorms, fire, pathogen outbreaks or other unpredictable large-scale disturbance will prevent the persistence of stable late-successional forest communities (Pontailler et al., 1997 and McLachlan et al., 2000). Long-term studies are essential in separating the effects of autogenic processes, extreme events, and more gradual changes in the environment upon community structure (Mountford et al., 1999, Runkle, 2000, Woods, 2000 and Harcombe et al., 2002). [\n] After release from a historical regime of livestock grazing and irregular cuttings, the predicted steady-state community in Dalby Söderskog dominated by Ulmus and Mercurialis perennis only prevailed for a few decades before unexpected external events, in this particular case Dutch elm disease and invasion by the slug Arion lusitanicus, initiated a successional change which will be interesting to follow. When walking through the forest in 2006, large numbers of juvenile Fraxinus and Fagus can be seen in gaps, but young Ulmus trees are also common, and in several places Quercus saplings can be observed. The last tree inventory was in 1970 and a new survey which includes regeneration will be of particular importance in an analysis of the changing structure of the forest.
@article{vonoheimbDalbySoderskogRevisited2007,
title = {Dalby {{Söderskog}} Revisited: Long-Term Vegetation Changes in a South {{Swedish}} Deciduous Forest},
author = {von Oheimb, Goddert and Brunet, Jörg},
date = {2007-03},
journaltitle = {Acta Oecologica},
volume = {31},
pages = {229--242},
issn = {1146-609X},
doi = {10.1016/j.actao.2006.12.001},
url = {https://doi.org/10.1016/j.actao.2006.12.001},
abstract = {In this study, we report on 67 years of secondary succession in the temperate deciduous forest Dalby Söderskog, southern Sweden. In 2002 vegetation analyses were conducted in 74 systematically distributed plots and the results compared with similar investigations during the years 1935, 1969 and 1976. Additionally, a floristic survey of the forest was made and compared with inventories of the years 1925, 1935 and 1970. From 1970 to 2002, overall species richness of the forest continued to decline, but at a lower rate than before. In 2002, for the first time, shade-tolerant forest species constituted the largest group. In the upper tree layer Fraxinus excelsior became the most important species, at the expense of Quercus robur and Ulmus glabra. In the herb layer, no changes in total or mean species richness were exhibited at plot scale between 1976 and 2002. In contrast to the lack of quantitative changes in species richness, we observed major changes in species composition at the plot level. In particular, the former dominant species Mercurialis perennis had declined markedly. After release from a historical regime of livestock grazing and irregular cuttings, the predicted steady-state community dominated by Ulmus and Mercurialis only prevailed for a few decades before unexpected external events, in this particular case Dutch elm disease and invasion by the slug Arion lusitanicus, initiated a successional change. We conclude that unexpected diseases or pests or rare climatic extremes can play a decisive role in forest dynamics and strongly interact with more gradual autogenic changes of forest structure and composition.
[Excerpt: Changes in the tree and shrub layer]
A similar long-term decline in regeneration of Quercus spp., such as observed in Dalby Söderskog, has been reported from a wide range of forest reserves in Europe and North America ( Glitzenstein et al., 1986, Emborg et al., 1996, Vera, 2000, Cowell and Jackson, 2002, Harcombe et al., 2002, Runkle et al., 2005 and von Oheimb et al., 2005). The present Quercus canopy trees are relicts of the more open stand structure of former times and do not regenerate under a closed canopy ( Table 2). In the absence of management, Lindquist, 1938 and Malmer et al., 1978 and Diekmann (1994) suggest that Ulmus would be the dominating tree species on moist eutric cambisols due to its characteristics as a shade-bearing, late-successional species, with the advanced regeneration exhibiting a higher shade-tolerance and the canopy trees having a higher competitive vigour than the early- to mid-successional species Fraxinus. Leemans (1992) used the forest succession model FORSKA to simulate species composition and stand structure of Dalby Söderskog. Starting the simulation run in 1920, the author found that species composition stabilized after 100 years as a forest of Ulmus, with scattered individuals of Fraxinus and Quercus. Fagus remained limited to the patches which initially had a high Fagus abundance.
[\textbackslash n] However, Diekmann (1994) suggested the Dutch elm disease (DED) had the potential to reverse these future trends. DED is a response of Ulmus spp. to infection by the fungus Ophiostoma novo-ulmi, which is spread by Scolytus beetles ( Röhrig, 1996). A particularly aggressive strain of DED was first recorded in Sk˚ane in 1979. In 1986, Dalby Söderskog was not yet visibly damaged ( Persson, 1987), but DED started to spread in the reserve during the following years. In order to reduce damage, 10-70 Ulmus trees were cut per year in Dalby Söderskog between 1988 and 1997 (pers. comm., 2002, County Board of Sk˚ane). By 2002, a considerable proportion of the Ulmus canopy trees had been killed or infected by DED (personal observation).
[\textbackslash n] In an unmanaged Ulmus glabra population in Lady Park Wood (western Britain), which has been recorded since 1945 and which has been subjected to DED since 1972, Peterken and Mountford (1998) found that about 65\,\% of the individuals present 40 years ago have been killed by DED. However, the population increased 1.4 times during this period. In particular on moist sites of the forest, seedling regeneration was the main survival mechanism and a few individuals survived by producing basal sprouts. While Ulmus recruitment from seedlings was infrequent before the onset of DED in Lady Park Wood, new saplings established soon after the canopy had been opened up. Peterken and Mountford (1998) suggest that, unless DED abates, Ulmus seems likely to persist as a fast turnover population of poles that never reaches the forest canopy. In a population of Ulmus americana in Michigan most of the larger trees were killed by DED, but the species remained dominant in the understorey ( Richardson and Cares, 1976). Based on the vegetation data of the plots, the impact of DED seems to result in similar changes of the Ulmus population in Dalby Söderskog. [\textbackslash n] [...]
[Conclusions]
Considering seven decades of vegetation changes in Dalby Söderskog, our results highlight the role of unpredictable historical events that strongly influence the process of autogenic succession. In most places, disturbance after windstorms, fire, pathogen outbreaks or other unpredictable large-scale disturbance will prevent the persistence of stable late-successional forest communities (Pontailler et al., 1997 and McLachlan et al., 2000). Long-term studies are essential in separating the effects of autogenic processes, extreme events, and more gradual changes in the environment upon community structure (Mountford et al., 1999, Runkle, 2000, Woods, 2000 and Harcombe et al., 2002).
[\textbackslash n] After release from a historical regime of livestock grazing and irregular cuttings, the predicted steady-state community in Dalby Söderskog dominated by Ulmus and Mercurialis perennis only prevailed for a few decades before unexpected external events, in this particular case Dutch elm disease and invasion by the slug Arion lusitanicus, initiated a successional change which will be interesting to follow. When walking through the forest in 2006, large numbers of juvenile Fraxinus and Fagus can be seen in gaps, but young Ulmus trees are also common, and in several places Quercus saplings can be observed. The last tree inventory was in 1970 and a new survey which includes regeneration will be of particular importance in an analysis of the changing structure of the forest.},
keywords = {*imported-from-citeulike-INRMM,~INRMM-MiD:c-13713915,~to-add-doi-URL,arion-lusitanicus,corylus-avellana,crataegus-spp,disturbances,dutch-elm-disease,forest-pests,forest-resources,forest-succession,fraxinus-excelsior,ground-vegetation,mercurialis-perennis,plant-pests,quercus-robur,sweden,ulmus-glabra},
number = {2},
options = {useprefix=true}
}
Mechanisms of Carbon Storage in Mountainous Headwater Rivers. Wohl, E., Dwire, K., Sutfin, N., Polvi, L., & Bazan, R. 3:1263+. Paper doi abstract bibtex Published research emphasizes rapid downstream export of terrestrial carbon from mountainous headwater rivers, but little work focuses on mechanisms that create carbon storage along these rivers, or on the volume of carbon storage. Here we estimate organic carbon stored in diverse valley types of headwater rivers in Rocky Mountain National Park, CO, USA. We show that low-gradient, broad valley bottoms with old-growth forest or active beaver colonies store the great majority of above- and below-ground carbon. These laterally unconfined valley segments constitute $<$25\,% of total river length, but store ̃75\,% of the carbon. Floodplain sediment and coarse wood dominate carbon storage. Our estimates of riverine carbon storage represent a previously undocumented but important carbon sink. Our results indicate that: not all mountainous rivers rapidly export carbon; not all valley segments are equally important in carbon storage; and historical changes in riverine complexity have likely reduced carbon storage.
@article{wohlMechanismsCarbonStorage2012,
title = {Mechanisms of Carbon Storage in Mountainous Headwater Rivers},
author = {Wohl, Ellen and Dwire, Kathleen and Sutfin, Nicholas and Polvi, Lina and Bazan, Roberto},
date = {2012-12},
journaltitle = {Nature Communications},
volume = {3},
pages = {1263+},
issn = {2041-1723},
doi = {10.1038/ncomms2274},
url = {https://doi.org/10.1038/ncomms2274},
abstract = {Published research emphasizes rapid downstream export of terrestrial carbon from mountainous headwater rivers, but little work focuses on mechanisms that create carbon storage along these rivers, or on the volume of carbon storage. Here we estimate organic carbon stored in diverse valley types of headwater rivers in Rocky Mountain National Park, CO, USA. We show that low-gradient, broad valley bottoms with old-growth forest or active beaver colonies store the great majority of above- and below-ground carbon. These laterally unconfined valley segments constitute {$<$}25\,\% of total river length, but store ̃75\,\% of the carbon. Floodplain sediment and coarse wood dominate carbon storage. Our estimates of riverine carbon storage represent a previously undocumented but important carbon sink. Our results indicate that: not all mountainous rivers rapidly export carbon; not all valley segments are equally important in carbon storage; and historical changes in riverine complexity have likely reduced carbon storage.},
keywords = {*imported-from-citeulike-INRMM,~INRMM-MiD:c-13886685,~to-add-doi-URL,carbon-stock,forest-resources,mountainous-areas,slope,spatial-prioritization,water-resources}
}
Modelling Long-Term Fire Occurrence Factors in Spain by Accounting for Local Variations with Geographically Weighted Regression. Mart́ınez-Fernández, J., Chuvieco, E., & Koutsias, N. 13(2):311–327. Paper doi abstract bibtex Humans are responsible for most forest fires in Europe, but anthropogenic factors behind these events are still poorly understood. We tried to identify the driving factors of human-caused fire occurrence in Spain by applying two different statistical approaches. Firstly, assuming stationary processes for the whole country, we created models based on multiple linear regression and binary logistic regression to find factors associated with fire density and fire presence, respectively. Secondly, we used geographically weighted regression (GWR) to better understand and explore the local and regional variations of those factors behind human-caused fire occurrence. [] The number of human-caused fires occurring within a 25-yr period (1983-2007) was computed for each of the 7638 Spanish mainland municipalities, creating a binary variable (fire/no fire) to develop logistic models, and a continuous variable (fire density) to build standard linear regression models. A total of 383 657 fires were registered in the study dataset. The binary logistic model, which estimates the probability of having/not having a fire, successfully classified 76.4\,% of the total observations, while the ordinary least squares (OLS) regression model explained 53\,% of the variation of the fire density patterns (adjusted R2 = 0.53). Both approaches confirmed, in addition to forest and climatic variables, the importance of variables related with agrarian activities, land abandonment, rural population exodus and developmental processes as underlying factors of fire occurrence. [] For the GWR approach, the explanatory power of the GW linear model for fire density using an adaptive bandwidth increased from 53\,% to 67\,%, while for the GW logistic model the correctly classified observations improved only slightly, from 76.4\,% to 78.4\,%, but significantly according to the corrected Akaike Information Criterion (AICc), from 3451.19 to 3321.19. The results from GWR indicated a significant spatial variation in the local parameter estimates for all the variables and an important reduction of the autocorrelation in the residuals of the GW linear model. Despite the fitting improvement of local models, GW regression, more than an alternative to "global" or traditional regression modelling, seems to be a valuable complement to explore the non-stationary relationships between the response variable and the explanatory variables. The synergy of global and local modelling provides insights into fire management and policy and helps further our understanding of the fire problem over large areas while at the same time recognizing its local character.
@article{martinez-fernandezModellingLongtermFire2013,
title = {Modelling Long-Term Fire Occurrence Factors in {{Spain}} by Accounting for Local Variations with Geographically Weighted Regression},
author = {Mart́ınez-Fernández, J. and Chuvieco, E. and Koutsias, N.},
date = {2013-02},
journaltitle = {Natural Hazards and Earth System Science},
volume = {13},
pages = {311--327},
issn = {1684-9981},
doi = {10.5194/nhess-13-311-2013},
url = {http://mfkp.org/INRMM/article/14257121},
abstract = {Humans are responsible for most forest fires in Europe, but anthropogenic factors behind these events are still poorly understood. We tried to identify the driving factors of human-caused fire occurrence in Spain by applying two different statistical approaches. Firstly, assuming stationary processes for the whole country, we created models based on multiple linear regression and binary logistic regression to find factors associated with fire density and fire presence, respectively. Secondly, we used geographically weighted regression (GWR) to better understand and explore the local and regional variations of those factors behind human-caused fire occurrence.
[] The number of human-caused fires occurring within a 25-yr period (1983-2007) was computed for each of the 7638 Spanish mainland municipalities, creating a binary variable (fire/no fire) to develop logistic models, and a continuous variable (fire density) to build standard linear regression models. A total of 383 657 fires were registered in the study dataset. The binary logistic model, which estimates the probability of having/not having a fire, successfully classified 76.4\,\% of the total observations, while the ordinary least squares (OLS) regression model explained 53\,\% of the variation of the fire density patterns (adjusted R2 = 0.53). Both approaches confirmed, in addition to forest and climatic variables, the importance of variables related with agrarian activities, land abandonment, rural population exodus and developmental processes as underlying factors of fire occurrence.
[] For the GWR approach, the explanatory power of the GW linear model for fire density using an adaptive bandwidth increased from 53\,\% to 67\,\%, while for the GW logistic model the correctly classified observations improved only slightly, from 76.4\,\% to 78.4\,\%, but significantly according to the corrected Akaike Information Criterion (AICc), from 3451.19 to 3321.19. The results from GWR indicated a significant spatial variation in the local parameter estimates for all the variables and an important reduction of the autocorrelation in the residuals of the GW linear model. Despite the fitting improvement of local models, GW regression, more than an alternative to "global" or traditional regression modelling, seems to be a valuable complement to explore the non-stationary relationships between the response variable and the explanatory variables. The synergy of global and local modelling provides insights into fire management and policy and helps further our understanding of the fire problem over large areas while at the same time recognizing its local character.},
keywords = {*imported-from-citeulike-INRMM,~INRMM-MiD:c-14257121,~to-add-doi-URL,anthropogenic-impacts,forest-fires,spain,spatial-analysis,spatial-pattern,wildfires},
number = {2}
}
Modelling the Potential Distribution of Betula Utilis in the Himalaya. Bobrowski, M., Gerlitz, L., & Schickhoff, U. 11:69–83. Paper doi abstract bibtex [Highlights] [::] We modelled for the first time potential distribution of Betula utilis in the Himalayan mountains on a broad scale. [::] Two temperature and three precipitation variables are useful for predicting the current potential distribution of B. utilis. [::] We applied Generalized Linear Models and evaluated model performance using a multi-faceted approach. [::] Comparison between the current predictions and the distribution range decribed in the vegetation map of Schweinfurth (1957). [::] New starting point for modelling treeline dynamics and treeline shifts in the Himalaya under novel climate conditions. [Abstract] Developing sustainable adaptation pathways under climate change conditions in mountain regions requires accurate predictions of treeline shifts and future distribution ranges of treeline species. Here, we model for the first time the potential distribution of Betula utilis, a principal Himalayan treeline species, to provide a basis for the analysis of future range shifts. Our target species Betula utilis is widespread at alpine treelines in the Himalayan mountains, the distribution range extends across the Himalayan mountain range. Our objective is to model the potential distribution of B. utilis in relation to current climate conditions. We generated a dataset of 590 occurrence records and used 24 variables for ecological niche modelling. We calibrated Generalized Linear Models using the Akaike Information Criterion (AIC) and evaluated model performance using threshold-independent (AUC, Area Under the Curve) and threshold-dependent (TSS, True Skill Statistics) characteristics as well as visual assessments of projected distribution maps. We found two temperature-related (Mean Temperature of the Wettest Quarter, Temperature Annual Range) and three precipitation-related variables (Precipitation of the Coldest Quarter, Average Precipitation of March, April and May and Precipitation Seasonality) to be useful for predicting the potential distribution of B. utilis. All models had high predictive power (AUC ≥ 0.98 and TSS ≥ 0.89). The projected suitable area in the Himalayan mountains varies considerably, with most extensive distribution in the western and central Himalayan region. A substantial difference between potential and real distribution in the eastern Himalaya points to decreasing competitiveness of B. utilis under more oceanic conditions in the eastern part of the mountain system. A comparison between the vegetation map of Schweinfurth (1957) and our current predictions suggests that B. utilis does not reach the upper elevational limit in vast areas of its potential distribution range due to anthropogenically caused treeline depressions. This study underlines the significance of accuracies of current environmental niche models for species distribution modelling under climate change scenarios. Analysing and understanding the environmental factors driving the current distribution of B. utilis is crucial for the prediction of future range shifts of B. utilis and other treeline species, and for deriving appropriate climate change adaptation strategies.
@article{bobrowskiModellingPotentialDistribution2017,
title = {Modelling the Potential Distribution of {{Betula}} Utilis in the {{Himalaya}}},
author = {Bobrowski, Maria and Gerlitz, Lars and Schickhoff, Udo},
date = {2017-07},
journaltitle = {Global Ecology and Conservation},
volume = {11},
pages = {69--83},
issn = {2351-9894},
doi = {10.1016/j.gecco.2017.04.003},
url = {http://mfkp.org/INRMM/article/14385050},
abstract = {[Highlights] [::] We modelled for the first time potential distribution of Betula utilis in the Himalayan mountains on a broad scale. [::] Two temperature and three precipitation variables are useful for predicting the current potential distribution of B. utilis. [::] We applied Generalized Linear Models and evaluated model performance using a multi-faceted approach. [::] Comparison between the current predictions and the distribution range decribed in the vegetation map of Schweinfurth (1957). [::] New starting point for modelling treeline dynamics and treeline shifts in the Himalaya under novel climate conditions.
[Abstract] Developing sustainable adaptation pathways under climate change conditions in mountain regions requires accurate predictions of treeline shifts and future distribution ranges of treeline species. Here, we model for the first time the potential distribution of Betula utilis, a principal Himalayan treeline species, to provide a basis for the analysis of future range shifts. Our target species Betula utilis is widespread at alpine treelines in the Himalayan mountains, the distribution range extends across the Himalayan mountain range. Our objective is to model the potential distribution of B. utilis in relation to current climate conditions. We generated a dataset of 590 occurrence records and used 24 variables for ecological niche modelling. We calibrated Generalized Linear Models using the Akaike Information Criterion (AIC) and evaluated model performance using threshold-independent (AUC, Area Under the Curve) and threshold-dependent (TSS, True Skill Statistics) characteristics as well as visual assessments of projected distribution maps. We found two temperature-related (Mean Temperature of the Wettest Quarter, Temperature Annual Range) and three precipitation-related variables (Precipitation of the Coldest Quarter, Average Precipitation of March, April and May and Precipitation Seasonality) to be useful for predicting the potential distribution of B. utilis. All models had high predictive power (AUC ≥ 0.98 and TSS ≥ 0.89). The projected suitable area in the Himalayan mountains varies considerably, with most extensive distribution in the western and central Himalayan region. A substantial difference between potential and real distribution in the eastern Himalaya points to decreasing competitiveness of B. utilis under more oceanic conditions in the eastern part of the mountain system. A comparison between the vegetation map of Schweinfurth (1957) and our current predictions suggests that B. utilis does not reach the upper elevational limit in vast areas of its potential distribution range due to anthropogenically caused treeline depressions. This study underlines the significance of accuracies of current environmental niche models for species distribution modelling under climate change scenarios. Analysing and understanding the environmental factors driving the current distribution of B. utilis is crucial for the prediction of future range shifts of B. utilis and other treeline species, and for deriving appropriate climate change adaptation strategies.},
keywords = {*imported-from-citeulike-INRMM,~INRMM-MiD:c-14385050,~to-add-doi-URL,betula-utilis,bioclimatic-predictors,chelsa-climate,forest-resources,habitat-suitability,himalayan-region,precipitation,temperature}
}
Has Land Use Pushed Terrestrial Biodiversity beyond the Planetary Boundary? A Global Assessment. Newbold, T., Hudson, L. N., Arnell, A. P., Contu, S., De Palma, A., Ferrier, S., Hill, S. L. L., Hoskins, A. J., Lysenko, I., Phillips, H. R. P., Burton, V. J., Chng, C. W. T., Emerson, S., Gao, D., Pask-Hale, G., Hutton, J., Jung, M., Sanchez-Ortiz, K., Simmons, B. I., Whitmee, S., Zhang, H., Scharlemann, J. P. W., & Purvis, A. 353(6296):288–291. Paper doi abstract bibtex [Crossing ” safe” limits for biodiversity loss] The planetary boundaries framework attempts to set limits for biodiversity loss within which ecological function is relatively unaffected. Newbold et al. present a quantitative global analysis of the extent to which the proposed planetary boundary has been crossed (see the Perspective by Oliver). Using over 2 million records for nearly 40,000 terrestrial species, they modeled the response of biodiversity to land use and related pressures and then estimated, at a spatial resolution of ∼1 km2, the extent and spatial patterns of changes in local biodiversity. Across 65\,% of the terrestrial surface, land use and related pressures have caused biotic intactness to decline beyond 10\,%, the proposed ” safe” planetary boundary. Changes have been most pronounced in grassland biomes and biodiversity hotspots. [Abstract] Land use and related pressures have reduced local terrestrial biodiversity, but it is unclear how the magnitude of change relates to the recently proposed planetary boundary ( ” safe limit”). We estimate that land use and related pressures have already reduced local biodiversity intactness – the average proportion of natural biodiversity remaining in local ecosystems – beyond its recently proposed planetary boundary across 58.1\,% of the world's land surface, where 71.4\,% of the human population live. Biodiversity intactness within most biomes (especially grassland biomes), most biodiversity hotspots, and even some wilderness areas is inferred to be beyond the boundary. Such widespread transgression of safe limits suggests that biodiversity loss, if unchecked, will undermine efforts toward long-term sustainable development.
@article{newboldHasLandUse2016,
title = {Has Land Use Pushed Terrestrial Biodiversity beyond the Planetary Boundary? {{A}} Global Assessment},
author = {Newbold, T. and Hudson, L. N. and Arnell, A. P. and Contu, S. and De Palma, A. and Ferrier, S. and Hill, S. L. L. and Hoskins, A. J. and Lysenko, I. and Phillips, H. R. P. and Burton, V. J. and Chng, C. W. T. and Emerson, S. and Gao, D. and Pask-Hale, G. and Hutton, J. and Jung, M. and Sanchez-Ortiz, K. and Simmons, B. I. and Whitmee, S. and Zhang, H. and Scharlemann, J. P. W. and Purvis, A.},
date = {2016-07},
journaltitle = {Science},
volume = {353},
pages = {288--291},
issn = {0036-8075},
doi = {10.1126/science.aaf2201},
url = {https://doi.org/10.1126/science.aaf2201},
abstract = {[Crossing ” safe” limits for biodiversity loss]
The planetary boundaries framework attempts to set limits for biodiversity loss within which ecological function is relatively unaffected. Newbold et al. present a quantitative global analysis of the extent to which the proposed planetary boundary has been crossed (see the Perspective by Oliver). Using over 2 million records for nearly 40,000 terrestrial species, they modeled the response of biodiversity to land use and related pressures and then estimated, at a spatial resolution of ∼1 km2, the extent and spatial patterns of changes in local biodiversity. Across 65\,\% of the terrestrial surface, land use and related pressures have caused biotic intactness to decline beyond 10\,\%, the proposed ” safe” planetary boundary. Changes have been most pronounced in grassland biomes and biodiversity hotspots.
[Abstract]
Land use and related pressures have reduced local terrestrial biodiversity, but it is unclear how the magnitude of change relates to the recently proposed planetary boundary ( ” safe limit”). We estimate that land use and related pressures have already reduced local biodiversity intactness -- the average proportion of natural biodiversity remaining in local ecosystems -- beyond its recently proposed planetary boundary across 58.1\,\% of the world's land surface, where 71.4\,\% of the human population live. Biodiversity intactness within most biomes (especially grassland biomes), most biodiversity hotspots, and even some wilderness areas is inferred to be beyond the boundary. Such widespread transgression of safe limits suggests that biodiversity loss, if unchecked, will undermine efforts toward long-term sustainable development.},
keywords = {*imported-from-citeulike-INRMM,~INRMM-MiD:c-14097161,~to-add-doi-URL,anthropocene,anthropogenic-changes,biodiversity,ecology,global-change,global-scale,grasslands,homeostasis,hotspot,land-use,species-richness,tipping-point},
number = {6296}
}
Plants and Habitats of European Cities. Kelcey, J. G. & Müller, N., editors . Paper doi abstract bibtex Plants and Habitats of European Cities contains details of sixteen cities in the European peninsula from Almeria to St. Petersburg and from Sofia to London. The chapters start with a description of the natural features and history of the cities and then consider how urbanization has affected the environment (for example, pollution, the heat island effect and climatic changes). The recorded botanical history of the city is followed by an account of the flora, which is mainly concerned with flowering plants and ferns. Where there is sufficient information the chapters include summary descriptions of the algae, bryophytes, lichens and fungi. The plant communities and species composition of the major natural and semi-natural habitats are described and followed by accounts of the species found in more typical urban habitats. These include housing areas of different types and densities, industrial zones, unused and previously developed land, parks, cemeteries, allotments and similar habitats, transport routes (for example railway land and road verges) and various aquatic habitats including rivers and flooded mineral workings. Plants and Habitats of European Cities is another important step towards the full understanding of the natural history of European cities. It is unique in describing, for the first time in a single volume, the flora and plant communities that occur in some of the major European cities. The authors are leading experts on urban botany and of the flora of the cities about which they have written. The book has been written and edited to be accessible to a wide range of interests and expertise including academic botanists and ecologists, landscape architects, planners, urban designers, ordinary people with an interest in natural history in general and botany in particular, undergraduates and other students not only in Europe but throughout the world. About the Editors: John G. Kelcey is not an academic but a practitioner. After graduating in Botany and Geology from the University of Manchester, Britain, he was appointed the ecologist of Milton Keynes Development Corporation a new town for 250,000 people, which was promoted by the British Government. Subsequently he became an ecological consultant and advisor and carried out ecological assessments of major development projects including housing schemes, commercial and retail developments, mainly in urban areas. During this time he was a member of nine professional institutions and several learned societies in Europe. Norbert Müller is a vegetation ecologist and Professor in the University of Applied Sciences Erfurt, Germany, holding the chair of the Department Landscape Management and Restoration Ecology. Within his main research fields, urban biodiversity and conservation biology, he studied flora and vegetation of several large cities in Asia, Europe, North America and South Africa. He is responsible for URBIO - a worldwide scientific network with the aim of promoting urban biodiversity through a continuing dialogue with the Convention on Biological Diversity.
@collection{kelceyPlantsHabitatsEuropean2011,
title = {Plants and {{Habitats}} of {{European Cities}}},
editor = {Kelcey, John G. and Müller, Norbert},
date = {2011},
publisher = {{Springer-Verlag}},
location = {{New York}},
doi = {10.1007/978-0-387-89684-7},
url = {http://mfkp.org/INRMM/article/13577957},
abstract = {Plants and Habitats of European Cities contains details of sixteen cities in the European peninsula from Almeria to St. Petersburg and from Sofia to London. The chapters start with a description of the natural features and history of the cities and then consider how urbanization has affected the environment (for example, pollution, the heat island effect and climatic changes). The recorded botanical history of the city is followed by an account of the flora, which is mainly concerned with flowering plants and ferns. Where there is sufficient information the chapters include summary descriptions of the algae, bryophytes, lichens and fungi. The plant communities and species composition of the major natural and semi-natural habitats are described and followed by accounts of the species found in more typical urban habitats. These include housing areas of different types and densities, industrial zones, unused and previously developed land, parks, cemeteries, allotments and similar habitats, transport routes (for example railway land and road verges) and various aquatic habitats including rivers and flooded mineral workings. Plants and Habitats of European Cities is another important step towards the full understanding of the natural history of European cities. It is unique in describing, for the first time in a single volume, the flora and plant communities that occur in some of the major European cities. The authors are leading experts on urban botany and of the flora of the cities about which they have written. The book has been written and edited to be accessible to a wide range of interests and expertise including academic botanists and ecologists, landscape architects, planners, urban designers, ordinary people with an interest in natural history in general and botany in particular, undergraduates and other students not only in Europe but throughout the world. About the Editors: John G. Kelcey is not an academic but a practitioner. After graduating in Botany and Geology from the University of Manchester, Britain, he was appointed the ecologist of Milton Keynes Development Corporation a new town for 250,000 people, which was promoted by the British Government. Subsequently he became an ecological consultant and advisor and carried out ecological assessments of major development projects including housing schemes, commercial and retail developments, mainly in urban areas. During this time he was a member of nine professional institutions and several learned societies in Europe. Norbert Müller is a vegetation ecologist and Professor in the University of Applied Sciences Erfurt, Germany, holding the chair of the Department Landscape Management and Restoration Ecology. Within his main research fields, urban biodiversity and conservation biology, he studied flora and vegetation of several large cities in Asia, Europe, North America and South Africa. He is responsible for URBIO - a worldwide scientific network with the aim of promoting urban biodiversity through a continuing dialogue with the Convention on Biological Diversity.},
isbn = {978-0-387-89684-7},
keywords = {*imported-from-citeulike-INRMM,~INRMM-MiD:c-13577957,~to-add-doi-URL,europe,forest-resources,urban-areas,urban-habitats,vegetation-composition,vegetation-types}
}
Pricing Biodiversity and Ecosystem Services: The Never-Ending Story. Gatto, M. & De Leo, G. A. 50(4):347–355. Paper doi abstract bibtex [Excerpt from the Conclusions] An impressive literature is available on environmental impact assessment and multiattribute analysis that documents the experience gained through 30 years of study and application. Nevertheless, these studies seem to be confined to the area of urban planning and are almost completely ignored by present-day economists as well as by many ecologists. Somewhere between the assignment of a zero value to biodiversity (the old-fashioned but still used practice, in which environmental impacts are viewed as externalities to be discarded from the balance sheet) and the assignment of an infinite value (as advocated by some radical environmentalists), lie more sensible methods to assign value to biodiversity than the price tag techniques suggested by the new wave of environmental economists. Rather than collapsing every measure of social and environmental value onto a monetary axis, environmental impact assessment and multiattribute analysis allow for explicit consideration of intangible nonmonctary values along with classical economic assessment, which, of course, remains important. It is, in fact, possible to assess ecosystem values and the ecological impact of human activity without using prices. Concepts such as Odum's eMergy (1996) and Rees' ecological footprint (Wackernagel and Rees 1996), although perceived by some as naive, may aid both ecologists and economists in addressing this important need. To summarize our viewpoint, economists should recognize that cost – benefit analysis is only part of the decision-making process and that it lies at the same level as other considerations. Ecologists should accept that monetary valuation of biodiversity and ecosystem services is possible (and even helpful) for part of its value, typically its use value. We contend that the realistic substitute for markets, when they fail, is a transparent decision-making process, not old-style cost – benefit analysis. The idea that, if one could get the price right, the best and most effective decisions at both the individual and public levels would automatically follow is, for many scientists, a sort of Panglossian obsession. In reality, there is no simple solution to complex problems. We fear that putting an a priori monetary value on biodiversity and ecosystem services will prevent humans from valuing the environment other than as a commodity to be exploited, thus reinvigorating the old economic paradigm that assumes a perfect substitution between natural and human-made capital (Ehrenfeld 1988). As Rees (1998) wrote, "for all its theoretical attractiveness, ascribing money values to nature's services is only a partial solution to the present dilemma and, if relied on exclusively, may actually be counterproductive" (p. 52).
@article{gattoPricingBiodiversityEcosystem2000,
title = {Pricing Biodiversity and Ecosystem Services: The Never-Ending Story},
author = {Gatto, Marino and De Leo, Giulio A.},
date = {2000},
journaltitle = {BioScience},
volume = {50},
pages = {347--355},
issn = {0006-3568},
doi = {10.1641/0006-3568(2000)050[0347:PBAEST]2.3.CO;2},
url = {https://doi.org/10.1641/0006-3568(2000)050[0347:PBAEST]2.3.CO;2},
abstract = {[Excerpt from the Conclusions] An impressive literature is available on environmental impact assessment and multiattribute analysis that documents the experience gained through 30 years of study and application. Nevertheless, these studies seem to be confined to the area of urban planning and are almost completely ignored by present-day economists as well as by many ecologists. Somewhere between the assignment of a zero value to biodiversity (the old-fashioned but still used practice, in which environmental impacts are viewed as externalities to be discarded from the balance sheet) and the assignment of an infinite value (as advocated by some radical environmentalists), lie more sensible methods to assign value to biodiversity than the price tag techniques suggested by the new wave of environmental economists. Rather than collapsing every measure of social and environmental value onto a monetary axis, environmental impact assessment and multiattribute analysis allow for explicit consideration of intangible nonmonctary values along with classical economic assessment, which, of course, remains important. It is, in fact, possible to assess ecosystem values and the ecological impact of human activity without using prices. Concepts such as Odum's eMergy (1996) and Rees' ecological footprint (Wackernagel and Rees 1996), although perceived by some as naive, may aid both ecologists and economists in addressing this important need. To summarize our viewpoint, economists should recognize that cost -- benefit analysis is only part of the decision-making process and that it lies at the same level as other considerations. Ecologists should accept that monetary valuation of biodiversity and ecosystem services is possible (and even helpful) for part of its value, typically its use value. We contend that the realistic substitute for markets, when they fail, is a transparent decision-making process, not old-style cost -- benefit analysis. The idea that, if one could get the price right, the best and most effective decisions at both the individual and public levels would automatically follow is, for many scientists, a sort of Panglossian obsession. In reality, there is no simple solution to complex problems. We fear that putting an a priori monetary value on biodiversity and ecosystem services will prevent humans from valuing the environment other than as a commodity to be exploited, thus reinvigorating the old economic paradigm that assumes a perfect substitution between natural and human-made capital (Ehrenfeld 1988). As Rees (1998) wrote, "for all its theoretical attractiveness, ascribing money values to nature's services is only a partial solution to the present dilemma and, if relied on exclusively, may actually be counterproductive" (p. 52).},
keywords = {*imported-from-citeulike-INRMM,~INRMM-MiD:c-12608523,~to-add-doi-URL,bias-toward-primacy-of-theory-over-reality,biodiversity,complexity,cost-benefit-analysis,costs,ecosystem-services,multi-criteria-decision-analysis,multi-objective-planning,nonmarket-impacts,pricing,risk-assessment,trade-offs},
number = {4}
}
Projections of Climate Change Indices of Temperature and Precipitation from an Ensemble of Bias-Adjusted High-Resolution EURO-CORDEX Regional Climate Models. Dosio, A. 121(10):2015JD024411-5511. Paper doi abstract bibtex Statistical bias-adjustment of climate models' outputs is being increasingly used for assessing the impact of climate change on several sectors. It is known that these techniques may alter the mean climate signal of the adjusted variable; however, the effect on the projected occurrence of climate extremes is less commonly investigated. Here the outputs of an ensemble of high-resolution (0.11°) regional climate models (RCM) from the Coordinated Regional-climate Downscaling Experiment for Europe (EURO-CORDEX) have been bias adjusted, and a number of climate indices from the Expert Team on Climate Change Detection and Indices have been calculated for the present (1981-2010) and future (2071-2100) climate. Indices include absolute-thresholds indices, percentile-based indices, and indices based on the duration of an event. Results show that absolute-threshold indices are largely affected by bias adjustment, as they depend strongly on both the present mean climate value (usually largely biased in the original RCMs) and its shift under climate change. The change of percentile-based indices is less affected by bias adjustment, as that of indices based on the duration of an event (e.g., consecutive dry days or heat waves) although the present climate value can differ between original and bias-adjusted results. Indices like R95ptot (the total amount of precipitation larger than the 95th reference percentile) are largely affected by bias adjustment, although, when analyzing an ensemble of RCMs, the differences are usually smaller than, or comparable to, the intermodel variability.
@article{dosioProjectionsClimateChange2016,
title = {Projections of Climate Change Indices of Temperature and Precipitation from an Ensemble of Bias-Adjusted High-Resolution {{EURO}}-{{CORDEX}} Regional Climate Models},
author = {Dosio, Alessandro},
date = {2016-05},
journaltitle = {J. Geophys. Res. Atmos.},
volume = {121},
pages = {2015JD024411-5511},
issn = {2169-897X},
doi = {10.1002/2015jd024411},
url = {http://mfkp.org/INRMM/article/14053888},
abstract = {Statistical bias-adjustment of climate models' outputs is being increasingly used for assessing the impact of climate change on several sectors. It is known that these techniques may alter the mean climate signal of the adjusted variable; however, the effect on the projected occurrence of climate extremes is less commonly investigated. Here the outputs of an ensemble of high-resolution (0.11°) regional climate models (RCM) from the Coordinated Regional-climate Downscaling Experiment for Europe (EURO-CORDEX) have been bias adjusted, and a number of climate indices from the Expert Team on Climate Change Detection and Indices have been calculated for the present (1981-2010) and future (2071-2100) climate. Indices include absolute-thresholds indices, percentile-based indices, and indices based on the duration of an event. Results show that absolute-threshold indices are largely affected by bias adjustment, as they depend strongly on both the present mean climate value (usually largely biased in the original RCMs) and its shift under climate change. The change of percentile-based indices is less affected by bias adjustment, as that of indices based on the duration of an event (e.g., consecutive dry days or heat waves) although the present climate value can differ between original and bias-adjusted results. Indices like R95ptot (the total amount of precipitation larger than the 95th reference percentile) are largely affected by bias adjustment, although, when analyzing an ensemble of RCMs, the differences are usually smaller than, or comparable to, the intermodel variability.},
keywords = {*imported-from-citeulike-INRMM,~INRMM-MiD:c-14053888,~to-add-doi-URL,bias-correction,climate-change,ipcc,ipcc-scenarios,precipitation,temperature},
number = {10}
}
Population Viability Risk Management (PVRM) for in Situ Management of Endangered Tree Species - A Case Study on a Taxus Baccata L. Population. Dhar, A., Ruprecht, H., & Vacik, H. 255(7):2835–2845. Paper doi abstract bibtex Population viability risk management (PVRM) provides a framework for explicitly including qualitative information about the possible outcomes of a management decision with regard to the viability of an endangered population in conservation management. Multi-criteria decision-making (MCDM) techniques enables managers to select the most preferred choice of action in a context where several criteria apply simultaneously. In that context a combined approach of the PVRM concept and a MCDM technique is presented for the development, evaluation and finally ranking of the in situ conservation strategies. We discuss the concept based on a case study for the maintenance of a gene conservation forest of an English yew population (Taxus baccata L.) in Styria, Austria. As part of the PVRM the analytic hierarchy process (AHP) is used to evaluate six conservation strategies with regard to the viability of the yew population. The viability of the population is evaluated based on the results of an analysis of the current environmental, social and economical state and a characterization of the ecological parameters of its population. The most significant risk factors (illegal cutting, browsing by game, tree competition, light availability and genetic sustainability) are structured and prioritised according to their impact on the viability of the yew population applying the AHP. Effects of the six conservation strategies on the viability of the yew population are determined through a qualitative assessment of the probability of a decrease of the population along with four different environmental scenarios. In this context strategy IV combining selective thinning, protection measures, game control with public relation activities seems to be the most effective alternative. The benefits of the combined approach of the PVRM concept with the AHP for the rational analysis of conservation strategies for this endangered tree species are discussed.
@article{dharPopulationViabilityRisk2008,
title = {Population Viability Risk Management ({{PVRM}}) for in Situ Management of Endangered Tree Species - {{A}} Case Study on a {{Taxus}} Baccata {{L}}. Population},
author = {Dhar, Amalesh and Ruprecht, Herwig and Vacik, Harald},
date = {2008},
journaltitle = {Forest Ecology and Management},
volume = {255},
pages = {2835--2845},
issn = {0378-1127},
doi = {10.1016/j.foreco.2008.01.059},
url = {https://doi.org/10.1016/j.foreco.2008.01.059},
abstract = {Population viability risk management (PVRM) provides a framework for explicitly including qualitative information about the possible outcomes of a management decision with regard to the viability of an endangered population in conservation management. Multi-criteria decision-making (MCDM) techniques enables managers to select the most preferred choice of action in a context where several criteria apply simultaneously. In that context a combined approach of the PVRM concept and a MCDM technique is presented for the development, evaluation and finally ranking of the in situ conservation strategies. We discuss the concept based on a case study for the maintenance of a gene conservation forest of an English yew population (Taxus baccata L.) in Styria, Austria. As part of the PVRM the analytic hierarchy process (AHP) is used to evaluate six conservation strategies with regard to the viability of the yew population. The viability of the population is evaluated based on the results of an analysis of the current environmental, social and economical state and a characterization of the ecological parameters of its population. The most significant risk factors (illegal cutting, browsing by game, tree competition, light availability and genetic sustainability) are structured and prioritised according to their impact on the viability of the yew population applying the AHP. Effects of the six conservation strategies on the viability of the yew population are determined through a qualitative assessment of the probability of a decrease of the population along with four different environmental scenarios. In this context strategy IV combining selective thinning, protection measures, game control with public relation activities seems to be the most effective alternative. The benefits of the combined approach of the PVRM concept with the AHP for the rational analysis of conservation strategies for this endangered tree species are discussed.},
keywords = {*imported-from-citeulike-INRMM,~INRMM-MiD:c-13507586,~to-add-doi-URL,population-viability-risk-management,taxus-baccata},
number = {7}
}
Pest Categorisation of Stegophora~Ulmea. Jeger, M., Bragard, C., Caffier, D., Candresse, T., Chatzivassiliou, E., Dehnen-Schmutz, K., Gilioli, G., Gregoire, J., Jaques Miret, J. A., MacLeod, A., Navajas Navarro, M., Niere, B., Parnell, S., Potting, R., Rafoss, T., Rossi, V., Urek, G., Van Bruggen, A., Van der Werf, W., West, J., Winter, S., Boberg, J., Gonthier, P., & Pautasso, M. 15(12):e05105+. Paper doi abstract bibtex Following a request from the European Commission, the EFSA Panel on Plant Health (PLH) performed a pest categorisation of Stegophora ulmea, a well-defined and distinguishable fungal species of the family Sydowiellaceae. S. ulmea causes a tree disease known as black spot of elm (Ulmus spp.). The pathogen is reported from North America (native range) and Asia (Far-East Russia and China), but not from the EU. S. ulmea is regulated in Council Directive 2000/29/EC (Annex IIAI) as a harmful organism whose introduction into the EU is banned on plants of Ulmus L. and Zelkova L., intended for planting, other than seeds. The pathogen has been occasionally intercepted on imported bonsai plants (and then destroyed) in the Netherlands and the UK. It could enter the EU and spread within it via plants for planting (including bonsai) and cut branches. Hosts and favourable climatic conditions are common in the EU. The European native elm species Ulmus glabra and Ulmus laevis were found to be more susceptible to the disease than North American elm species, but information is lacking on Ulmus minor. The disease is rarely fatal, but S. ulmea can cause considerable damage, particularly in wet summers. Reduction of inoculum by the removal of leaf debris and avoiding overhead watering in nurseries can reduce the risk of spread of the pathogen. The main knowledge gaps concern (i) the distribution of the pest in Asian countries, (ii) the relative role of the means of entry/spread and (iii) the potential consequences in mature tree plantations and native woodland. The criteria assessed by the Panel for consideration as potential quarantine pest are met. For regulated non-quarantine pests, the criterion on the pest presence in the EU is not met. [Excerpt: Conclusions] [...] [::Identity of the pest] The identity of the pest as a species is clear. [...] [::Absence/presence of the pest in the EU territory] The pest is not reported to be present in the EU. [...] There is a doubtful and unconfirmed record of the fungus in Romania. Interceptions in the Netherlands and UK were followed by eradication. [...] [::Regulatory status] S. ulmea is regulated by Council Directive 2000/29/EC (Annex IIA) on plants of Ulmus and Zelkova, intended for planting, other than seeds. [...] [::Pest potential for entry, establishment and spread in the EU territory] Entry: the pest could enter the EU via the plants for planting pathway, as well as on bonsai plants and cut foliage [] Establishment: hosts and favourable climatic conditions are widespread in the risk assessment (RA) area [] Spread: the pest would be able to spread following establishment mainly on infected plants for planting and bonsai plants. [...] [] There is a lack of data on the trade of Ulmus spp. and Zelkova spp. bonsai plants within the EU [...] [::Potential for consequences in the EU territory] The pest introduction could have impacts especially in nurseries and on amenity trees. [...] [] The introduction of the pest could have an impact on the intended use of plants for planting. [...] [] There is uncertainty about the level of impact of the disease, which has rarely been described in detail, particularly in native woodland and planted forests. The consequences for U. minor are uncertain, given the lack of information on its susceptibility. [...] [::Available measures] Reduction of inoculum by the removal and appropriate disposal of leaf debris and avoiding overhead watering in nurseries can reduce the risk of spread of the pathogen. Breeding for host resistance/tolerance may reduce the level of impacts. [...] [] Key uncertainties: The relative importance of overwintering in buds compared to primary infection in spring. [...] [::Conclusion on pest categorisation] The criteria assessed by the Panel for consideration as potential quarantine pest are met. [...] [] The criterion on the pest presence in the EU is not met. [...] [::Aspects of assessment to focus on/scenarios to address in future if appropriate] The main knowledge gaps concern (i) the distribution of the pest in Asian countries, (ii) the relative role of the means of entry/spread (plants for planting other than bonsai plants, bonsai plants and cut foliage), and (iii) the potential consequences in mature tree plantations and native woodland. However, the present categorisation has explored most if not all of the available data on these knowledge gaps [...]
@article{jegerPestCategorisationStegophora2017,
title = {Pest Categorisation of {{Stegophora}}~Ulmea},
author = {Jeger, Michael and Bragard, Claude and Caffier, David and Candresse, Thierry and Chatzivassiliou, Elisavet and Dehnen-Schmutz, Katharina and Gilioli, Gianni and Gregoire, Jean-Claude and Jaques Miret, Josep A. and MacLeod, Alan and Navajas Navarro, Maria and Niere, Björn and Parnell, Stephen and Potting, Roel and Rafoss, Trond and Rossi, Vittorio and Urek, Gregor and Van Bruggen, Ariena and Van der Werf, Wopke and West, Jonathan and Winter, Stephan and Boberg, Johanna and Gonthier, Paolo and Pautasso, Marco},
date = {2017-12},
journaltitle = {EFSA Journal},
volume = {15},
pages = {e05105+},
issn = {1831-4732},
doi = {10.2903/j.efsa.2017.5105},
url = {https://doi.org/10.2903/j.efsa.2017.5105},
abstract = {Following a request from the European Commission, the EFSA Panel on Plant Health (PLH) performed a pest categorisation of Stegophora ulmea, a well-defined and distinguishable fungal species of the family Sydowiellaceae. S. ulmea causes a tree disease known as black spot of elm (Ulmus spp.). The pathogen is reported from North America (native range) and Asia (Far-East Russia and China), but not from the EU. S. ulmea is regulated in Council Directive 2000/29/EC (Annex IIAI) as a harmful organism whose introduction into the EU is banned on plants of Ulmus L. and Zelkova L., intended for planting, other than seeds. The pathogen has been occasionally intercepted on imported bonsai plants (and then destroyed) in the Netherlands and the UK. It could enter the EU and spread within it via plants for planting (including bonsai) and cut branches. Hosts and favourable climatic conditions are common in the EU. The European native elm species Ulmus glabra and Ulmus laevis were found to be more susceptible to the disease than North American elm species, but information is lacking on Ulmus minor. The disease is rarely fatal, but S. ulmea can cause considerable damage, particularly in wet summers. Reduction of inoculum by the removal of leaf debris and avoiding overhead watering in nurseries can reduce the risk of spread of the pathogen. The main knowledge gaps concern (i) the distribution of the pest in Asian countries, (ii) the relative role of the means of entry/spread and (iii) the potential consequences in mature tree plantations and native woodland. The criteria assessed by the Panel for consideration as potential quarantine pest are met. For regulated non-quarantine pests, the criterion on the pest presence in the EU is not met.
[Excerpt: Conclusions] [...] [::Identity of the pest] The identity of the pest as a species is clear. [...]
[::Absence/presence of the pest in the EU territory] The pest is not reported to be present in the EU. [...] There is a doubtful and unconfirmed record of the fungus in Romania. Interceptions in the Netherlands and UK were followed by eradication. [...]
[::Regulatory status] S. ulmea is regulated by Council Directive 2000/29/EC (Annex IIA) on plants of Ulmus and Zelkova, intended for planting, other than seeds. [...]
[::Pest potential for entry, establishment and spread in the EU territory] Entry: the pest could enter the EU via the plants for planting pathway, as well as on bonsai plants and cut foliage
[] Establishment: hosts and favourable climatic conditions are widespread in the risk assessment (RA) area
[] Spread: the pest would be able to spread following establishment mainly on infected plants for planting and bonsai plants. [...]
[] There is a lack of data on the trade of Ulmus spp. and Zelkova spp. bonsai plants within the EU [...]
[::Potential for consequences in the EU territory] The pest introduction could have impacts especially in nurseries and on amenity trees. [...]
[] The introduction of the pest could have an impact on the intended use of plants for planting. [...]
[] There is uncertainty about the level of impact of the disease, which has rarely been described in detail, particularly in native woodland and planted forests. The consequences for U. minor are uncertain, given the lack of information on its susceptibility. [...]
[::Available measures] Reduction of inoculum by the removal and appropriate disposal of leaf debris and avoiding overhead watering in nurseries can reduce the risk of spread of the pathogen. Breeding for host resistance/tolerance may reduce the level of impacts. [...]
[] Key uncertainties: The relative importance of overwintering in buds compared to primary infection in spring. [...]
[::Conclusion on pest categorisation] The criteria assessed by the Panel for consideration as potential quarantine pest are met. [...] [] The criterion on the pest presence in the EU is not met. [...]
[::Aspects of assessment to focus on/scenarios to address in future if appropriate] The main knowledge gaps concern (i) the distribution of the pest in Asian countries, (ii) the relative role of the means of entry/spread (plants for planting other than bonsai plants, bonsai plants and cut foliage), and (iii) the potential consequences in mature tree plantations and native woodland.
However, the present categorisation has explored most if not all of the available data on these knowledge gaps [...]},
keywords = {*imported-from-citeulike-INRMM,~INRMM-MiD:c-14506369,~to-add-doi-URL,disturbances,efsa,efsa-scientific-opinion,europe,forest-pests,plant-pests,stegophora-ulmea,ulmus-glabra,ulmus-laevis,ulmus-spp,zelkova-spp},
number = {12}
}
Vegetation and Fire History of the Euganean Hills (Colli Euganei) as Recorded by Lateglacial and Holocene Sedimentary Series from Lago Della Costa (Northeastern Italy). Kaltenrieder, P., Procacci, G., Vannière, B., & Tinner, W. 20(5):679–695. Paper doi abstract bibtex We reconstruct the vegetational and fire history of the Colli Euganei and northeastern Po Plain from c . 16 500 cal. BP to the present using AMS-dated sedimentary pollen, microscopic and macroscopic charcoal records. Our study site, Lago della Costa, is the only natural water basin with an undisturbed late-Quaternary sediment accumulation in the northeastern Po Plain. Mixed coniferous-deciduous forests occurred since at latest 14 500 cal. BP. Gradual expansion of e.g. Alnus glutinosa and Carpinus betulus is documented after c. 11 000 cal. BP. A further expansion of Abies alba and Alnus at 9200 cal. BP coincided with a population buildup of these species in the Insubrian region c. 200 km northwest of our site. A further increase of Alnus about 6400 cal. BP was accompanied by an expansion of Castanea sativa and Juglans regia as well as meadow and field plants. This vegetational change was contemporaneous with a huge increase of regional and local fire activity. Our data suggest that fire disturbance favoured strong and moderate re-sprouters, e.g. Alnus, Carpinus and Castanea, whereas fire-sensitive taxa, e.g. Tilia and Abies were disadvantaged. The close link between crops, weeds and fire activity suggests human impact as the main source of changes in Neolithic vegetation and fire regime. To our knowledge these are the oldest palaeobotanical data suggesting the cultivation of Castanea and Juglans in Europe and elsewhere. Our pollen and charcoal records document the subsequent cultivation of Castanea, Juglans, Olea and Cerealia t. during the Bronze Age (4150 – 2750 cal. BP). Subsequently, intensification of land use continued during the Iron and Roman Age and Medieval times. In contrast with other northern Italian sites vegetation around our site was always rather open with a substantial proportion covered by grassland. We explain this peculiarity of the site by its location near river banks and floodlands.
@article{kaltenriederVegetationFireHistory2010,
title = {Vegetation and Fire History of the {{Euganean Hills}} ({{Colli Euganei}}) as Recorded by {{Lateglacial}} and {{Holocene}} Sedimentary Series from {{Lago}} Della {{Costa}} (Northeastern {{Italy}})},
author = {Kaltenrieder, P. and Procacci, G. and Vannière, B. and Tinner, W.},
date = {2010-08},
journaltitle = {The Holocene},
volume = {20},
pages = {679--695},
issn = {1477-0911},
doi = {10.1177/0959683609358911},
url = {https://doi.org/10.1177/0959683609358911},
abstract = {We reconstruct the vegetational and fire history of the Colli Euganei and northeastern Po Plain from c . 16 500 cal. BP to the present using AMS-dated sedimentary pollen, microscopic and macroscopic charcoal records. Our study site, Lago della Costa, is the only natural water basin with an undisturbed late-Quaternary sediment accumulation in the northeastern Po Plain. Mixed coniferous-deciduous forests occurred since at latest 14 500 cal. BP. Gradual expansion of e.g. Alnus glutinosa and Carpinus betulus is documented after c. 11 000 cal. BP. A further expansion of Abies alba and Alnus at 9200 cal. BP coincided with a population buildup of these species in the Insubrian region c. 200 km northwest of our site. A further increase of Alnus about 6400 cal. BP was accompanied by an expansion of Castanea sativa and Juglans regia as well as meadow and field plants. This vegetational change was contemporaneous with a huge increase of regional and local fire activity. Our data suggest that fire disturbance favoured strong and moderate re-sprouters, e.g. Alnus, Carpinus and Castanea, whereas fire-sensitive taxa, e.g. Tilia and Abies were disadvantaged. The close link between crops, weeds and fire activity suggests human impact as the main source of changes in Neolithic vegetation and fire regime. To our knowledge these are the oldest palaeobotanical data suggesting the cultivation of Castanea and Juglans in Europe and elsewhere. Our pollen and charcoal records document the subsequent cultivation of Castanea, Juglans, Olea and Cerealia t. during the Bronze Age (4150 -- 2750 cal. BP). Subsequently, intensification of land use continued during the Iron and Roman Age and Medieval times. In contrast with other northern Italian sites vegetation around our site was always rather open with a substantial proportion covered by grassland. We explain this peculiarity of the site by its location near river banks and floodlands.},
keywords = {*imported-from-citeulike-INRMM,~INRMM-MiD:c-13593940,~to-add-doi-URL,castanea-spp,charcoal,colli-euganei,juglans-spp,paleoecology,po-plain,pollen},
number = {5}
}
The Potential for Eucalyptus as a Wood Fuel in the UK. Leslie, A. D., Mencuccini, M., & Perks, M. 89(1):176–182. Paper doi abstract bibtex Considerable potential exists in the UK for utilising woody biomass, grown under short rotation forestry management systems, to produce electricity or heat. There are benefits to using biomass in generating heat and power the main environmental benefit being from substituting for fossil fuel combustion and consequent carbon emissions. Woody biomass production in short rotation forestry involves growing single stemmed trees rather than coppice over rotations of between 10 and 15~years. Eucalypts are particularly suited to such biomass production as they exhibit relatively high wood density, have suitable chemical characteristics, exhibit low moisture content and can be easily harvested all year around using conventional machinery if single-stemmed growth form is maintained. The UK has a climate that is not well suited to the majority of eucalypts. However, there is a small number of eucalypt species that can withstand the stresses caused by frozen ground and desiccating winds or sub-zero temperatures that can occur. These species are from more southern latitudes and high altitude areas of Australia. However, even the most cold resistant species can be damaged by UK winter climate extremes and therefore careful matching of species to site environmental constraints is critical. Informed decision making is made problematic by the small area and limited distribution of current planting, although it is clear that particularly cold areas and for most species, sites with poor drainage should be generally avoided. This article provides a discussion of the potential of, and constraints to, using eucalypts for biomass in the UK and provides a tentative list of recommended species, their potential growth rates and their advantages and disadvantages. ⺠Eucalyptus in plantations has potential in the UK as a source of woody biomass. ⺠Fast early growth enables high productivity over short rotations. ⺠Unseasonal frosts and unusually cold winters pose a risk. ⺠It is not clear whether climate change will benefit or hinder use of eucalypts for biomass in the UK. [Excerpt: Conclusions] The interest in using biomass as a source of energy has provided a catalyst for the re-examination of the potential role of eucalypts in short rotation forestry in Britain. Their high productivity can provide substantial yields of biomass, reduce greenhouse gas emissions from fossil fuel consumption and can also reduce operational fossil fuel use by replacement of more energy intensive forms of land use. Existing trials and small plantations of eucalypts have shown that there are a limited range of species of eucalypts that can survive and thrive in the relatively low temperatures prevalent in the UK. The limited distribution and extent of plantings make detailed matching of species to site currently imperfect. A sensible approach is, therefore, to attempt to identify species and provenances that will perform well over a wide range of sites and avoid areas that are particularly cold, have low rainfall and for most species, have poor drainage.
@article{lesliePotentialEucalyptusWood2012,
title = {The Potential for {{Eucalyptus}} as a Wood Fuel in the {{UK}}},
author = {Leslie, A. D. and Mencuccini, M. and Perks, M.},
date = {2012-01},
journaltitle = {Applied Energy},
volume = {89},
pages = {176--182},
issn = {0306-2619},
doi = {10.1016/j.apenergy.2011.07.037},
url = {https://doi.org/10.1016/j.apenergy.2011.07.037},
abstract = {Considerable potential exists in the UK for utilising woody biomass, grown under short rotation forestry management systems, to produce electricity or heat. There are benefits to using biomass in generating heat and power the main environmental benefit being from substituting for fossil fuel combustion and consequent carbon emissions. Woody biomass production in short rotation forestry involves growing single stemmed trees rather than coppice over rotations of between 10 and 15~years. Eucalypts are particularly suited to such biomass production as they exhibit relatively high wood density, have suitable chemical characteristics, exhibit low moisture content and can be easily harvested all year around using conventional machinery if single-stemmed growth form is maintained. The UK has a climate that is not well suited to the majority of eucalypts. However, there is a small number of eucalypt species that can withstand the stresses caused by frozen ground and desiccating winds or sub-zero temperatures that can occur. These species are from more southern latitudes and high altitude areas of Australia. However, even the most cold resistant species can be damaged by UK winter climate extremes and therefore careful matching of species to site environmental constraints is critical. Informed decision making is made problematic by the small area and limited distribution of current planting, although it is clear that particularly cold areas and for most species, sites with poor drainage should be generally avoided. This article provides a discussion of the potential of, and constraints to, using eucalypts for biomass in the UK and provides a tentative list of recommended species, their potential growth rates and their advantages and disadvantages. ⺠Eucalyptus in plantations has potential in the UK as a source of woody biomass. ⺠Fast early growth enables high productivity over short rotations. ⺠Unseasonal frosts and unusually cold winters pose a risk. ⺠It is not clear whether climate change will benefit or hinder use of eucalypts for biomass in the UK.
[Excerpt: Conclusions]
The interest in using biomass as a source of energy has provided a catalyst for the re-examination of the potential role of eucalypts in short rotation forestry in Britain. Their high productivity can provide substantial yields of biomass, reduce greenhouse gas emissions from fossil fuel consumption and can also reduce operational fossil fuel use by replacement of more energy intensive forms of land use. Existing trials and small plantations of eucalypts have shown that there are a limited range of species of eucalypts that can survive and thrive in the relatively low temperatures prevalent in the UK. The limited distribution and extent of plantings make detailed matching of species to site currently imperfect. A sensible approach is, therefore, to attempt to identify species and provenances that will perform well over a wide range of sites and avoid areas that are particularly cold, have low rainfall and for most species, have poor drainage.},
keywords = {*imported-from-citeulike-INRMM,~INRMM-MiD:c-13780667,~to-add-doi-URL,eucalyptus-spp,forest-resources,fuelwood,short-rotation-forestry,united-kingdom},
number = {1}
}
Fungal Endophytes in Mediterranean Oak Forests: A Lesson from Discula Quercina. Moricca, S. & Ragazzi, A. 98(4):380–386. Paper doi abstract bibtex Fungal endophytes that colonize forest trees are widespread, but they are less well known than endophytes infecting grasses. The few studies on endophytes in trees mainly concern the tropical areas and the northernmost latitudes, while similar investigations in the Mediterranean region have so far been scarce and incidental. Endophytes are studied mostly in economically important forests suffering from diseases, such as oak forests. One common endophyte that has received some study on oak is the mitosporic Discula quercina. This paper, after first addressing some basic problems on tree endophytes, examines the ecology of D. quercina in Mediterranean oak stands. D. quercina is usually viewed as a symptomless colonizer of healthy Quercus cerris, infecting new leaves early in the growing season, in an unstable equilibrium between transient mutualism/neutralism and latent pathogenesis. It is postulated here that climatic factors can change the endophytic nature of D. quercina, turning it into a weak pathogen or an opportunistic invader of senescing and indeed healthy trees. It is argued more generally that stochastic events can cause the lifestyle of an endophyte to switch from beneficial/neutral to pathogenic, transforming the tree-endophyte interaction, an interaction that depends in part on the matching genomes of the tree and endophyte, and on the environmental context.
@article{moriccaFungalEndophytesMediterranean2008,
title = {Fungal Endophytes in {{Mediterranean}} Oak Forests: A Lesson from {{Discula}} Quercina},
author = {Moricca, S. and Ragazzi, A.},
date = {2008-04},
journaltitle = {Phytopathology},
volume = {98},
pages = {380--386},
issn = {0031-949X},
doi = {10.1094/phyto-98-4-0380},
url = {https://doi.org/10.1094/phyto-98-4-0380},
abstract = {Fungal endophytes that colonize forest trees are widespread, but they are less well known than endophytes infecting grasses. The few studies on endophytes in trees mainly concern the tropical areas and the northernmost latitudes, while similar investigations in the Mediterranean region have so far been scarce and incidental. Endophytes are studied mostly in economically important forests suffering from diseases, such as oak forests. One common endophyte that has received some study on oak is the mitosporic Discula quercina. This paper, after first addressing some basic problems on tree endophytes, examines the ecology of D. quercina in Mediterranean oak stands. D. quercina is usually viewed as a symptomless colonizer of healthy Quercus cerris, infecting new leaves early in the growing season, in an unstable equilibrium between transient mutualism/neutralism and latent pathogenesis. It is postulated here that climatic factors can change the endophytic nature of D. quercina, turning it into a weak pathogen or an opportunistic invader of senescing and indeed healthy trees. It is argued more generally that stochastic events can cause the lifestyle of an endophyte to switch from beneficial/neutral to pathogenic, transforming the tree-endophyte interaction, an interaction that depends in part on the matching genomes of the tree and endophyte, and on the environmental context.},
keywords = {*imported-from-citeulike-INRMM,~INRMM-MiD:c-8971667,~to-add-doi-URL,droughts,fitness,forest-pests,forest-resources,fungal-diseases,opportunistic-plant-pests,parasitism,quercus-cerris,symbiosis},
number = {4}
}
Wildfire-Related Debris Flow from a Hazards Perspective. Cannon, S. H. & Gartner, J. E. In Debris-Flow Hazards and Related Phenomena, of Springer Praxis Books, pages 363–385. Springer Berlin Heidelberg. Paper doi abstract bibtex [Excerpt: Introduction] Wildland fire can have profound effects on the hydrologic response of a watershed. Consumption of the rainfall-intercepting canopy and of the soil-mantling litter and duff, intensive drying of the soil, combustion of soil-binding organic matter, and the enhancement or formation of water-repellent soils can change the infiltration characteristics and erodibility of the soil, leading to decreased rainfall infiltration, subsequent significantly increased overland flow and runoff in channels, and movement of soil (e.g., Swanson, 1981; Spittler, 1995; Doerr et al., 2000; Martin and Moody, 2001; Moody and Martin, 2001b; Wondzell and King, 2003). Unit-area peak discharges measured following wildfire have shown between 1.45- and 870-fold increases over pre-fire rates (Moody and Martin, 2001a). Removal of obstructions by wildfire through consumption of vegetation can also enhance the erosive power of overland flow, resulting in accelerated erosion of material from hillslopes (Meyer, 2002). Increased runoff can erode significant volumes of material from channels, either by bank failure or channel bed erosion. Over longer time periods, decreased rates of evapotranspiration caused by vegetation mortality and decay of root structure may result in increased soil moisture and the loss of soil cohesion (Klock and Helvey, 1976; Swanson, 1981; Schmidt et al., 2001). Rainfall on burned watersheds thus has a high potential to transport and deposit large volumes of sediment both within and down-channel from the burned area. [\n] Debris flows can be one of the most hazardous consequences of rainfall on burned hillslopes (e.g., Parrett, 1987; Morton, 1989; Meyer and Wells, 1997; Cannon, 2001) (Fig. 15.1A,B). They pose a hazard distinct from other sediment-laden flows because of their unique destructive power. Debris flows can occur with little warning, can exert great impulsive loads on objects in their paths, and even small debris flows can strip vegetation, block drainage ways, damage structures by impact and erosion, and endanger human life. The deaths of sixteen people during the Christmas Day 2003 storm that impacted recently-burned hillslopes in southern California highlight the most drastic consequences of post-wildfire debris flows (Los Angeles Times, 2003). In addition to the lives lost, US\$9.5 million were spent to remove the 4.1 million cubic meters of material deposited in debris retention basins following this event. Understanding the processes that result in fire-related debris flows, the conditions under which they occur, and their size and frequency of occurrence are critical elements in effective post-fire hazard assessments. [\n] The objective of this chapter is to provide an overview of the current understanding of post-wildfire debris-flow processes and their occurrence. [\n] [...] [Summary and conclusions] Data compiled from studies of debris-flow processes following wildfires throughout the western U.S. can answer some of the questions fundamental to post-fire hazard assessments - what, where, why, when, how big, and how often? Not all elements of all questions have satisfactory answers, but what follows is what can be gleaned from the preceding pages. [::What and why?] Fire-related debris flows have been found to initiate through two primary processes: runoff-dominated erosion by surface overland flow, and infiltration-triggered failure of a discrete landslide mass. Runoff-dominated processes are by far the most prevalent (76\,% of a sample of 210 basins), and occur in response to decreased infiltration and attendant increased runoff and erosion brought about by the immediate effects of the fires. Infiltration-triggered landslide activity is frequently attributed to both increased soil moisture brought about by vegetation-mortality-induced reduced transpiration rates, and root decay associated with decreases in soil cohesion. [::Where?] Debris flows that initiate through runoff-dominated erosion have been documented throughout the intermountain west and southern California. Basins underlain with sedimentary and metamorphic rock types with more than about 65\,% of their areas burned at a combination of high and moderate severities, and with areas and average gradients that fall above the threshold shown in Fig. 15.9 are those most likely to produce this type of debris flow. [\n] [...] [::When?] Runoff-initiated debris flows are produced in response to storms that occur up to two years after the fire, and often in response to the first significant rainfall of the storm season. They occur most frequently in response to storms with average intensities greater than about 4 mm/hr and between 30 minutes and 24 hours in duration. However, debris flows have occurred within a storm after as little as 6 minutes of rainfall at intensities of 95 mm/hr. [\n] [...] [\n] Debris flows generated through mobilization of landslides can occur during the first rainy season immediately after the fire, and up to about 10 years after the fire. These events generally occur in response to prolonged rainfall events, and in some cases, considerably more material is contributed to the debris flows from hillslope runoff and channel erosion than from the landslide scars. [...] [::How big?] Reported peak discharge estimates for runoff-initiated debris-flow events vary between 2 and 240 m3/s and reported volumes range from as little as 600 m3 to 300,000 m3. [...] [::How often?] Basins with thin colluvial covers and minimal channel-fill deposits generally produce debris flows only in response to the first significant rainfall of the season. Basins with thick channel-fill deposits, and those mantled with thick accumulations of talus, frequently produce numerous debris flows throughout the rainy season. [\n] In the absence of similar data in other settings throughout the world, the relations developed here may be appropriate for preliminary hazard assessments. However, we would expect that local conditions strongly affect debris-flow occurrence, and collection and analysis of site-specific data can only help but to improve such assessments. [\n] [...]
@incollection{cannonWildfirerelatedDebrisFlow2005,
title = {Wildfire-Related Debris Flow from a Hazards Perspective},
booktitle = {Debris-Flow {{Hazards}} and {{Related Phenomena}}},
author = {Cannon, Susan H. and Gartner, Joseph E.},
date = {2005},
pages = {363--385},
publisher = {{Springer Berlin Heidelberg}},
doi = {10.1007/3-540-27129-5\\_15},
url = {http://mfkp.org/INRMM/article/14110940},
abstract = {[Excerpt: Introduction] Wildland fire can have profound effects on the hydrologic response of a watershed. Consumption of the rainfall-intercepting canopy and of the soil-mantling litter and duff, intensive drying of the soil, combustion of soil-binding organic matter, and the enhancement or formation of water-repellent soils can change the infiltration characteristics and erodibility of the soil, leading to decreased rainfall infiltration, subsequent significantly increased overland flow and runoff in channels, and movement of soil (e.g., Swanson, 1981; Spittler, 1995; Doerr et al., 2000; Martin and Moody, 2001; Moody and Martin, 2001b; Wondzell and King, 2003). Unit-area peak discharges measured following wildfire have shown between 1.45- and 870-fold increases over pre-fire rates (Moody and Martin, 2001a). Removal of obstructions by wildfire through consumption of vegetation can also enhance the erosive power of overland flow, resulting in accelerated erosion of material from hillslopes (Meyer, 2002). Increased runoff can erode significant volumes of material from channels, either by bank failure or channel bed erosion. Over longer time periods, decreased rates of evapotranspiration caused by vegetation mortality and decay of root structure may result in increased soil moisture and the loss of soil cohesion (Klock and Helvey, 1976; Swanson, 1981; Schmidt et al., 2001). Rainfall on burned watersheds thus has a high potential to transport and deposit large volumes of sediment both within and down-channel from the burned area.
[\textbackslash n] Debris flows can be one of the most hazardous consequences of rainfall on burned hillslopes (e.g., Parrett, 1987; Morton, 1989; Meyer and Wells, 1997; Cannon, 2001) (Fig. 15.1A,B). They pose a hazard distinct from other sediment-laden flows because of their unique destructive power. Debris flows can occur with little warning, can exert great impulsive loads on objects in their paths, and even small debris flows can strip vegetation, block drainage ways, damage structures by impact and erosion, and endanger human life. The deaths of sixteen people during the Christmas Day 2003 storm that impacted recently-burned hillslopes in southern California highlight the most drastic consequences of post-wildfire debris flows (Los Angeles Times, 2003). In addition to the lives lost, US\$9.5 million were spent to remove the 4.1 million cubic meters of material deposited in debris retention basins following this event. Understanding the processes that result in fire-related debris flows, the conditions under which they occur, and their size and frequency of occurrence are critical elements in effective post-fire hazard assessments.
[\textbackslash n] The objective of this chapter is to provide an overview of the current understanding of post-wildfire debris-flow processes and their occurrence.
[\textbackslash n] [...]
[Summary and conclusions] Data compiled from studies of debris-flow processes following wildfires throughout the western U.S. can answer some of the questions fundamental to post-fire hazard assessments - what, where, why, when, how big, and how often? Not all elements of all questions have satisfactory answers, but what follows is what can be gleaned from the preceding pages.
[::What and why?] Fire-related debris flows have been found to initiate through two primary processes: runoff-dominated erosion by surface overland flow, and infiltration-triggered failure of a discrete landslide mass. Runoff-dominated processes are by far the most prevalent (76\,\% of a sample of 210 basins), and occur in response to decreased infiltration and attendant increased runoff and erosion brought about by the immediate effects of the fires. Infiltration-triggered landslide activity is frequently attributed to both increased soil moisture brought about by vegetation-mortality-induced reduced transpiration rates, and root decay associated with decreases in soil cohesion.
[::Where?] Debris flows that initiate through runoff-dominated erosion have been documented throughout the intermountain west and southern California. Basins underlain with sedimentary and metamorphic rock types with more than about 65\,\% of their areas burned at a combination of high and moderate severities, and with areas and average gradients that fall above the threshold shown in Fig. 15.9 are those most likely to produce this type of debris flow. [\textbackslash n] [...]
[::When?] Runoff-initiated debris flows are produced in response to storms that occur up to two years after the fire, and often in response to the first significant rainfall of the storm season. They occur most frequently in response to storms with average intensities greater than about 4 mm/hr and between 30 minutes and 24 hours in duration. However, debris flows have occurred within a storm after as little as 6 minutes of rainfall at intensities of 95 mm/hr. [\textbackslash n] [...] [\textbackslash n] Debris flows generated through mobilization of landslides can occur during the first rainy season immediately after the fire, and up to about 10 years after the fire. These events generally occur in response to prolonged rainfall events, and in some cases, considerably more material is contributed to the debris flows from hillslope runoff and channel erosion than from the landslide scars. [...]
[::How big?] Reported peak discharge estimates for runoff-initiated debris-flow events vary between 2 and 240 m3/s and reported volumes range from as little as 600 m3 to 300,000 m3. [...]
[::How often?] Basins with thin colluvial covers and minimal channel-fill deposits generally produce debris flows only in response to the first significant rainfall of the season. Basins with thick channel-fill deposits, and those mantled with thick accumulations of talus, frequently produce numerous debris flows throughout the rainy season.
[\textbackslash n] In the absence of similar data in other settings throughout the world, the relations developed here may be appropriate for preliminary hazard assessments. However, we would expect that local conditions strongly affect debris-flow occurrence, and collection and analysis of site-specific data can only help but to improve such assessments.
[\textbackslash n] [...]},
isbn = {978-3-540-27129-1},
keywords = {*imported-from-citeulike-INRMM,~INRMM-MiD:c-14110940,~to-add-doi-URL,burnt-area,debris-flows,erodibility,forest-resources,hydrology,landslides,natural-hazards,postfire-impacts,precipitation,runoff,sediment-transport,soil-erosion,soil-hydrophobicity,soil-moisture,soil-resources,water-resources,wildfires},
series = {Springer {{Praxis Books}}}
}
Global Urban Signatures of Phenotypic Change in Animal and Plant Populations. Alberti, M., Correa, C., Marzluff, J. M., Hendry, A. P., Palkovacs, E. P., Gotanda, K. M., Hunt, V. M., Apgar, T. M., & Zhou, Y. Paper doi abstract bibtex [Significance] Ecoevolutionary feedbacks on contemporary timescales were hypothesized over half a century ago, but only recently has evidence begun to emerge. The role that human activity plays in such dynamics is still unclear. Through a metaanalysis of $>$1,600 phenotypic changes in species across regions and ecosystem types, we examine the evidence that the rate of phenotypic change has an urban signature. Our findings indicate greater phenotypic change in urbanizing systems compared with natural and nonurban anthropogenic systems. By explicitly linking urban development to trait changes that might affect ecosystem function, we provide insights into the potential ecoevolutionary implications for maintaining ecosystem function and the sustainability of human well-being. [Abstract] Humans challenge the phenotypic, genetic, and cultural makeup of species by affecting the fitness landscapes on which they evolve. Recent studies show that cities might play a major role in contemporary evolution by accelerating phenotypic changes in wildlife, including animals, plants, fungi, and other organisms. Many studies of ecoevolutionary change have focused on anthropogenic drivers, but none of these studies has specifically examined the role that urbanization plays in ecoevolution or explicitly examined its mechanisms. This paper presents evidence on the mechanisms linking urban development patterns to rapid evolutionary changes for species that play important functional roles in communities and ecosystems. Through a metaanalysis of experimental and observational studies reporting more than 1,600 phenotypic changes in species across multiple regions, we ask whether we can discriminate an urban signature of phenotypic change beyond the established natural baselines and other anthropogenic signals. We then assess the relative impact of five types of urban disturbances including habitat modifications, biotic interactions, habitat heterogeneity, novel disturbances, and social interactions. Our study shows a clear urban signal; rates of phenotypic change are greater in urbanizing systems compared with natural and nonurban anthropogenic systems. By explicitly linking urban development to traits that affect ecosystem function, we can map potential ecoevolutionary implications of emerging patterns of urban agglomerations and uncover insights for maintaining key ecosystem functions upon which the sustainability of human well-being depends.
@article{albertiGlobalUrbanSignatures2017,
title = {Global Urban Signatures of Phenotypic Change in Animal and Plant Populations},
author = {Alberti, Marina and Correa, Cristian and Marzluff, John M. and Hendry, Andrew P. and Palkovacs, Eric P. and Gotanda, Kiyoko M. and Hunt, Victoria M. and Apgar, Travis M. and Zhou, Yuyu},
date = {2017-01},
journaltitle = {Proceedings of the National Academy of Sciences},
pages = {201606034+},
issn = {1091-6490},
doi = {10.1073/pnas.1606034114},
url = {https://doi.org/10.1073/pnas.1606034114},
abstract = {[Significance]
Ecoevolutionary feedbacks on contemporary timescales were hypothesized over half a century ago, but only recently has evidence begun to emerge. The role that human activity plays in such dynamics is still unclear. Through a metaanalysis of {$>$}1,600 phenotypic changes in species across regions and ecosystem types, we examine the evidence that the rate of phenotypic change has an urban signature. Our findings indicate greater phenotypic change in urbanizing systems compared with natural and nonurban anthropogenic systems. By explicitly linking urban development to trait changes that might affect ecosystem function, we provide insights into the potential ecoevolutionary implications for maintaining ecosystem function and the sustainability of human well-being.
[Abstract]
Humans challenge the phenotypic, genetic, and cultural makeup of species by affecting the fitness landscapes on which they evolve. Recent studies show that cities might play a major role in contemporary evolution by accelerating phenotypic changes in wildlife, including animals, plants, fungi, and other organisms. Many studies of ecoevolutionary change have focused on anthropogenic drivers, but none of these studies has specifically examined the role that urbanization plays in ecoevolution or explicitly examined its mechanisms. This paper presents evidence on the mechanisms linking urban development patterns to rapid evolutionary changes for species that play important functional roles in communities and ecosystems. Through a metaanalysis of experimental and observational studies reporting more than 1,600 phenotypic changes in species across multiple regions, we ask whether we can discriminate an urban signature of phenotypic change beyond the established natural baselines and other anthropogenic signals. We then assess the relative impact of five types of urban disturbances including habitat modifications, biotic interactions, habitat heterogeneity, novel disturbances, and social interactions. Our study shows a clear urban signal; rates of phenotypic change are greater in urbanizing systems compared with natural and nonurban anthropogenic systems. By explicitly linking urban development to traits that affect ecosystem function, we can map potential ecoevolutionary implications of emerging patterns of urban agglomerations and uncover insights for maintaining key ecosystem functions upon which the sustainability of human well-being depends.},
keywords = {*imported-from-citeulike-INRMM,~INRMM-MiD:c-14246966,~to-add-doi-URL,anthropocene,anthropogenic-changes,anthropogenic-impacts,ecosystem,ecosystem-functions,evolution,genetic-variability,meta-analysis,phenotypes-vs-genotypes,sustainability,urban-areas}
}
How to Hasten Open Access. Swan, A., Cockerill, M., & Sipp, D. 495(7442):442–443. Paper doi abstract bibtex Three advocates for a universally free scholarly literature give their prescriptions for the movement's next push, from findability to translations.
@article{swanHowHastenOpen2013,
title = {How to Hasten Open Access},
author = {Swan, Alma and Cockerill, Matthew and Sipp, Douglas},
date = {2013-03},
journaltitle = {Nature},
volume = {495},
pages = {442--443},
issn = {0028-0836},
doi = {10.1038/495442a},
url = {https://doi.org/10.1038/495442a},
abstract = {Three advocates for a universally free scholarly literature give their prescriptions for the movement's next push, from findability to translations.},
keywords = {*imported-from-citeulike-INRMM,~INRMM-MiD:c-12216944,~to-add-doi-URL,european-commission,free-scientific-knowledge,knowledge-freedom,open-access,open-access-embargo,science-policy-interface,scientific-knowledge-sharing,united-states},
number = {7442}
}