Holocene Expansions of Fagus Silvatica and Abies Alba in Central Europe: Where Are We after Eight Decades of Debate?. Tinner, W. & Lotter, A. 25(5-6):526–549.
Holocene Expansions of Fagus Silvatica and Abies Alba in Central Europe: Where Are We after Eight Decades of Debate? [link]Paper  doi  abstract   bibtex   
During the past eight decades contrasting hypotheses have been put forward to explain the Holocene expansions of Fagus silvatica (beech) and Abies alba (fir) in Central Europe. The hypotheses can be referred to as: (1) climatic change; (2) migrational lag; (3) delay in population increase; (4) human disturbance; and (5) fire disturbance. High-resolution pollen and charcoal records from three sites in lowland Switzerland and southern Germany allow testing the human vs. fire-disturbance hypotheses by means of time-series analysis. Cross-correlations between pairs of pollen as well as between microscopic charcoal and pollen suggest that neither human nor fire disturbance substantially promoted the expansion of Fagus and Abies. We address the remaining hypotheses (climatic change, migrational lag, delay of population increase) by a combined interpretation of our data with independent climatic records and other evidence of past environmental dynamics (e.g. dynamic vegetation modelling) for southern Central Europe. Rapid population expansions in response to cooling and precipitation increase suggest that climatic change was the main forcing factor and that migrational lags were not effective since at least 8200~cal.~yr ago. On the basis of this conclusion we propose an explanatory model for the Holocene expansion of Fagus and Abies in Central Europe: Both trees expanded stepwise across the continent during favourable 8200-type events, which were characterized by changes towards wetter and cooler conditions and corresponded to previously recognized Holocene cold phases in Central Europe as well as in the North Atlantic realm. Asynchronous expansions across continental Europe are explained by analogy to today's precipitation gradients resulting from orographic effects. Response lags of Fagus and Abies to climatic change reached a few decades at most, whereas population expansion in response to climatic change lasted for several centuries, probably as a consequence of intrinsic rates of population increase as well as competition with previously established forest communities. This model is in agreement with recent data from northern Central Europe, where large-scale expansion pulses of Fagus coincided with 8200-type events (e.g. 3800-3400 and 2750-2350~cal. BP). In addition to climatic change, human impact influenced the expansions of Fagus in northern Central Europe. We suggest that Abies expansions across Europe after 5000~cal. BP were inhibited by human and/or fire disturbance.
@article{tinnerHoloceneExpansionsFagus2006,
  title = {Holocene Expansions of {{Fagus}} Silvatica and {{Abies}} Alba in {{Central Europe}}: Where Are We after Eight Decades of Debate?},
  author = {Tinner, W. and Lotter, A.},
  date = {2006-03},
  journaltitle = {Quaternary Science Reviews},
  volume = {25},
  pages = {526--549},
  issn = {0277-3791},
  doi = {10.1016/j.quascirev.2005.03.017},
  url = {https://doi.org/10.1016/j.quascirev.2005.03.017},
  abstract = {During the past eight decades contrasting hypotheses have been put forward to explain the Holocene expansions of Fagus silvatica (beech) and Abies alba (fir) in Central Europe. The hypotheses can be referred to as: (1) climatic change; (2) migrational lag; (3) delay in population increase; (4) human disturbance; and (5) fire disturbance. High-resolution pollen and charcoal records from three sites in lowland Switzerland and southern Germany allow testing the human vs. fire-disturbance hypotheses by means of time-series analysis. Cross-correlations between pairs of pollen as well as between microscopic charcoal and pollen suggest that neither human nor fire disturbance substantially promoted the expansion of Fagus and Abies. We address the remaining hypotheses (climatic change, migrational lag, delay of population increase) by a combined interpretation of our data with independent climatic records and other evidence of past environmental dynamics (e.g. dynamic vegetation modelling) for southern Central Europe. Rapid population expansions in response to cooling and precipitation increase suggest that climatic change was the main forcing factor and that migrational lags were not effective since at least 8200~cal.~yr ago. On the basis of this conclusion we propose an explanatory model for the Holocene expansion of Fagus and Abies in Central Europe: Both trees expanded stepwise across the continent during favourable 8200-type events, which were characterized by changes towards wetter and cooler conditions and corresponded to previously recognized Holocene cold phases in Central Europe as well as in the North Atlantic realm. Asynchronous expansions across continental Europe are explained by analogy to today's precipitation gradients resulting from orographic effects. Response lags of Fagus and Abies to climatic change reached a few decades at most, whereas population expansion in response to climatic change lasted for several centuries, probably as a consequence of intrinsic rates of population increase as well as competition with previously established forest communities. This model is in agreement with recent data from northern Central Europe, where large-scale expansion pulses of Fagus coincided with 8200-type events (e.g. 3800-3400 and 2750-2350~cal. BP). In addition to climatic change, human impact influenced the expansions of Fagus in northern Central Europe. We suggest that Abies expansions across Europe after 5000~cal. BP were inhibited by human and/or fire disturbance.},
  keywords = {*imported-from-citeulike-INRMM,~INRMM-MiD:c-11379088,abies-alba,europe,fagus-sylvatica,migration-history},
  number = {5-6}
}
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