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• W1513819451 abstract "Plant macrofossils together with other proxy data enable the reconstruction of Eurasian vegetation history during the Quaternary, indicating that the climatic impact on vegetation in high latitudes is not just restricted to global temperature fluctuations but also depends decisively on the oceanic influence on climate. It is shown that Arctic climate in Eurasia during both cold and warm stages was much more continental than today, resulting in tundra-steppe or forest-tundra vegetation. Increased oceanic influence during the Holocene in the major Beringian refugium of Arctic vegetation may have resulted from neotectonic subsidence and the transgression of the East Siberian Arctic shelves." @default.
• W1513819451 created "2016-06-24" @default.
• W1513819451 creator A5039993233 @default.
• W1513819451 date "2007-01-01" @default.
• W1513819451 modified "2023-09-23" @default.
• W1513819451 title "PLANT MACROFOSSIL RECORDS | Arctic Eurasia" @default.
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• W1513819451 doi "https://doi.org/10.1016/b0-44-452747-8/00219-2" @default.
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