a b s t r a c tWe present a database of late-Quaternary plant macrofossil records for northern Eurasia (from 23 to 180 E and 46 to 76 N) comprising 281 localities, over 2300 samples and over 13,000 individual records. Samples are individually radiocarbon dated or are assigned ages via age models fitted to sequences of calibrated radiocarbon dates within a section. Tree species characteristic of modern northern forests (e.g. Picea, Larix, tree-Betula) are recorded at least intermittently from prior to the last glacial maximum (LGM), through the LGM and Lateglacial, to the Holocene, and some records locate trees close to the limits of the Scandinavian ice sheet, supporting the hypothesis that some taxa persisted in northern refugia during the last glacial cycle. Northern trees show differing spatio-temporal patterns across Siberia: deciduous trees were widespread in the Lateglacial, with individuals occurring across much of their contemporary ranges, while evergreen conifers expanded northwards to their range limits in the Holocene.
Significance
Modern humans dispersed into Europe and replaced Neanderthals at least 40,000 years ago. However, the precise timing and climatic context of this dispersal are heavily debated. Therefore, a new project combining paleoenvironmental and archaeological fieldwork has been undertaken at Willendorf II (Austria), a key site for this time period. This project has concluded that modern humans producing Aurignacian stone tools occupied Central Europe about 43,500 years ago in a medium-cold steppe environment with some boreal trees along valleys. This discovery represents the oldest well-documented occurrence of behaviorally modern humans in Europe and demonstrates contemporaneity with Neanderthals in other parts of Europe, showing that behaviorally modern humans and Neanderthals shared this region longer than previously thought.
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