It is commonly believed that trees were absent in Scandinavia during the last glaciation and first recolonized the Scandinavian Peninsula with the retreat of its ice sheet some 9000 years ago. Here, we show the presence of a rare mitochondrial DNA haplotype of spruce that appears unique to Scandinavia and with its highest frequency to the west—an area believed to sustain ice-free refugia during most of the last ice age. We further show the survival of DNA from this haplotype in lake sediments and pollen of Trøndelag in central Norway dating back ~10,300 years and chloroplast DNA of pine and spruce in lake sediments adjacent to the ice-free Andøya refugium in northwestern Norway as early as ~22,000 and 17,700 years ago, respectively. Our fin...
Andøya on the NW coast of Norway is a key site for understanding the Last Glacial Maximum (LGM) in n...
Tundra plant communities in the northern high latitudes are expected to undergo large distributional...
The phylogeographic structure and postglacial history of balsam fir (Abies balsamea), a transcontine...
It is commonly believed that trees were absent in Scandinavia during the last glaciation and first r...
The survival of boreal trees in ice-free cryptic refugia’s at high latitudes during the Last Glacial...
Contrasting theories exist regarding how Norway spruce (Picea abies) recolonized Fennoscandia after ...
During the climate oscillations of the Pleistocene an ice sheet formed covering Fennoscandia. Tradit...
Recent studies applying innovative technologies, such as genetic analysis and carbon dating, contrad...
Abstract Background At the last glacial maximum, Fennoscandia was covered by an ice sheet while the ...
This dataset includes two raw Illumina NextSeq 500 libraries (paired-end sequenced) and the associat...
survival of Pinus and Picea in northern Scandinavia. Their methodology does not exclude contaminatio...
Paleorecords offer key information for evaluating model simulations of species migration in response...
Andøya on the NW coast of Norway is a key site for understanding the Last Glacial Maximum (LGM) in n...
Aim We used combined palaeobotanical and genetic data to assess whether Norway spruce (Picea abies)...
Andøya on the NW coast of Norway is a key site for understanding the Last Glacial Maximum (LGM) in n...
Tundra plant communities in the northern high latitudes are expected to undergo large distributional...
The phylogeographic structure and postglacial history of balsam fir (Abies balsamea), a transcontine...
It is commonly believed that trees were absent in Scandinavia during the last glaciation and first r...
The survival of boreal trees in ice-free cryptic refugia’s at high latitudes during the Last Glacial...
Contrasting theories exist regarding how Norway spruce (Picea abies) recolonized Fennoscandia after ...
During the climate oscillations of the Pleistocene an ice sheet formed covering Fennoscandia. Tradit...
Recent studies applying innovative technologies, such as genetic analysis and carbon dating, contrad...
Abstract Background At the last glacial maximum, Fennoscandia was covered by an ice sheet while the ...
This dataset includes two raw Illumina NextSeq 500 libraries (paired-end sequenced) and the associat...
survival of Pinus and Picea in northern Scandinavia. Their methodology does not exclude contaminatio...
Paleorecords offer key information for evaluating model simulations of species migration in response...
Andøya on the NW coast of Norway is a key site for understanding the Last Glacial Maximum (LGM) in n...
Aim We used combined palaeobotanical and genetic data to assess whether Norway spruce (Picea abies)...
Andøya on the NW coast of Norway is a key site for understanding the Last Glacial Maximum (LGM) in n...
Tundra plant communities in the northern high latitudes are expected to undergo large distributional...
The phylogeographic structure and postglacial history of balsam fir (Abies balsamea), a transcontine...