Abstract Beringia, including Alaska and North-Eastern Siberia, has long been a focal point for biogeographical research in a wide range of plant and animal taxa. Whether boreal forest refugia existed in Beringia during the Last Glacial Maximum (LGM) is a major but unanswered question in Quaternary science. We analysed DNA sequence data from Amanita muscaria using phylogenetic and coalescent methods to test whether this boreal-temperate ectomycorrhizal fungus was present in Alaska during the LGM. Our data indicates that there are at least two endemic groups showing no detectable migration from or to populations that survived the LGM in Southern refugia. One of these occurs in the boreal forests of Interior Alaska, while the other group is en...
International audienceAbstract During the last glacial–interglacial cycle, Arctic biotas experienced...
Previous phylogeographical and palaeontological studies on the biota of northern North America have ...
During the last glacial–interglacial cycle, Arctic biotas experienced substantial climatic changes, ...
Paleorecords offer key information for evaluating model simulations of species migration in response...
Although a recent study of white spruce using chloroplast DNA uncovered the presence of a glacial re...
Although a recent study of white spruce using chloroplast DNA uncovered the presence of a glacial re...
Paleorecords offer key information for evaluating model simulations of species migration in response...
Evidence has been accumulating that suggests some arcto-boreal plant taxa persisted through the Last...
Aim Beringia, far north-eastern Siberia and north-western North America, was largely unglaciated dur...
Paleoenvironmental reconstructions help us to track vegetation responses to climatic changes, and ca...
Evidence is accumulating that some arcto-boreal plant taxa persisted through the Last Glacial Maximu...
Evidence is accumulating that some arcto-boreal plant taxa persisted through the Last Glacial Maximu...
Evidence is accumulating that some arcto-boreal plant taxa persisted through the Last Glacial Maximu...
During the last glacial–interglacial cycle, Arctic biotas experienced substantial climatic changes, ...
Thesis (M.S.) University of Alaska Fairbanks, 2002Periodic glacial advances during the Pleistocene f...
International audienceAbstract During the last glacial–interglacial cycle, Arctic biotas experienced...
Previous phylogeographical and palaeontological studies on the biota of northern North America have ...
During the last glacial–interglacial cycle, Arctic biotas experienced substantial climatic changes, ...
Paleorecords offer key information for evaluating model simulations of species migration in response...
Although a recent study of white spruce using chloroplast DNA uncovered the presence of a glacial re...
Although a recent study of white spruce using chloroplast DNA uncovered the presence of a glacial re...
Paleorecords offer key information for evaluating model simulations of species migration in response...
Evidence has been accumulating that suggests some arcto-boreal plant taxa persisted through the Last...
Aim Beringia, far north-eastern Siberia and north-western North America, was largely unglaciated dur...
Paleoenvironmental reconstructions help us to track vegetation responses to climatic changes, and ca...
Evidence is accumulating that some arcto-boreal plant taxa persisted through the Last Glacial Maximu...
Evidence is accumulating that some arcto-boreal plant taxa persisted through the Last Glacial Maximu...
Evidence is accumulating that some arcto-boreal plant taxa persisted through the Last Glacial Maximu...
During the last glacial–interglacial cycle, Arctic biotas experienced substantial climatic changes, ...
Thesis (M.S.) University of Alaska Fairbanks, 2002Periodic glacial advances during the Pleistocene f...
International audienceAbstract During the last glacial–interglacial cycle, Arctic biotas experienced...
Previous phylogeographical and palaeontological studies on the biota of northern North America have ...
During the last glacial–interglacial cycle, Arctic biotas experienced substantial climatic changes, ...