Norway spruce postglacial recolonization of Fennoscandia. Nota, K., Klaminder, J., Milesi, P., Bindler, R., Nobile, A., van Steijn, T., Bertilsson, S., Svensson, B., Hirota, S. K., Matsuo, A., Gunnarsson, U., Seppä, H., Väliranta, M. M., Wohlfarth, B., Suyama, Y., & Parducci, L. Nature Communications, 13(1):1333, March, 2022. Publisher: Nature Publishing Group![Norway spruce postglacial recolonization of Fennoscandia [link]](https://bibbase.org/img/filetypes/link.svg "link")
Paper doi abstract bibtex Contrasting theories exist regarding how Norway spruce (Picea abies) recolonized Fennoscandia after the last glaciation and both early Holocene establishments from western microrefugia and late Holocene colonization from the east have been postulated. Here, we show that Norway spruce was present in southern Fennoscandia as early as 14.7 ± 0.1 cal. kyr BP and that the millennia-old clonal spruce trees present today in central Sweden likely arrived with an early Holocene migration from the east. Our findings are based on ancient sedimentary DNA from multiple European sites (N = 15) combined with nuclear and mitochondrial DNA analysis of ancient clonal (N = 135) and contemporary spruce forest trees (N = 129) from central Sweden. Our other findings imply that Norway spruce was present shortly after deglaciation at the margins of the Scandinavian Ice Sheet, and support previously disputed finds of pollen in southern Sweden claiming spruce establishment during the Lateglacial.
@article{nota_norway_2022,
title = {Norway spruce postglacial recolonization of {Fennoscandia}},
volume = {13},
copyright = {2022 The Author(s)},
issn = {2041-1723},
url = {https://www.nature.com/articles/s41467-022-28976-4},
doi = {10.1038/s41467-022-28976-4},
abstract = {Contrasting theories exist regarding how Norway spruce (Picea abies) recolonized Fennoscandia after the last glaciation and both early Holocene establishments from western microrefugia and late Holocene colonization from the east have been postulated. Here, we show that Norway spruce was present in southern Fennoscandia as early as 14.7 ± 0.1 cal. kyr BP and that the millennia-old clonal spruce trees present today in central Sweden likely arrived with an early Holocene migration from the east. Our findings are based on ancient sedimentary DNA from multiple European sites (N = 15) combined with nuclear and mitochondrial DNA analysis of ancient clonal (N = 135) and contemporary spruce forest trees (N = 129) from central Sweden. Our other findings imply that Norway spruce was present shortly after deglaciation at the margins of the Scandinavian Ice Sheet, and support previously disputed finds of pollen in southern Sweden claiming spruce establishment during the Lateglacial.},
language = {en},
number = {1},
urldate = {2024-03-27},
journal = {Nature Communications},
author = {Nota, Kevin and Klaminder, Jonatan and Milesi, Pascal and Bindler, Richard and Nobile, Alessandro and van Steijn, Tamara and Bertilsson, Stefan and Svensson, Brita and Hirota, Shun K. and Matsuo, Ayumi and Gunnarsson, Urban and Seppä, Heikki and Väliranta, Minna M. and Wohlfarth, Barbara and Suyama, Yoshihisa and Parducci, Laura},
month = mar,
year = {2022},
note = {Publisher: Nature Publishing Group},
keywords = {Ecological genetics, Plant evolution},
pages = {1333},
}
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