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USGS Open-File Report 94-588

Pliocene vegetation and climate in Arctic Russia

Robert S. Thompson
U.S. Geological Survey, Denver, CO
Tundra vegetation occurs today along the Russian Arctic coast under extremely cold climates. During the early and middle Pliocene conditions were quite different, and forests grew along the Arctic coast of Russia, as well as in northernmost Alaska and Canada. Palynological and plant macrofossil data from the Far Northeast of Russia indicate that Larix, Picea, Pinus pumila, Alnaster, and tree-Betula lived near the coast. Pollen spectra of this age contain only very low levels of Artemisia, Chenopods, tundra herbs and other indicators of open vegetation (Giterman et al., 1982; Fradkina, 1991). Forest cover decreased and Arctic vegetation increased across northern Asia between approximately 3.5 Ma and 2.5 Ma (Fradkina, 1991; Volkova, 1991), suggesting pronounced cooling occurred through this time. Shrub-Betula, Alnaster, moss, and Poaceae increased in importance during this transition, as Larix, Picea, Pinus, and other tree species declined. At the Krestovka section on the Kolyma River in the Russian Far Northeast, Giterman et al. (1982) interpreted palynological data as indicating a late Pliocene sequence of open forest being replaced by treeless vegetation (steppe-tundra?), which in turn was replaced by open larch forest. They also report ice-wedge pseudomorphs in the late Pliocene sediments, indicating the initiation of permafrost. Early Pleistocene sediments from this site contain a complex array of permafrost features, suggesting increasingly cold conditions through the Pliocene-Pleistocene transition.

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