Vegetation Changes Associated with the Younger Dryas from the Sediments of Silver Lake, Summit County, Ohio, USA
As the climate was warming during the last deglaciation, a millennium-long return to near-glacial conditions—called the Younger Dryas (YD) stadial—occurred about 12.9 to 11.7 ka ago. Prior studies have characterized the vegetation and climatic impacts of the YD stadial in the US upper Midwest from a...
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Veröffentlicht in: | The Ohio journal of science 2020-12, Vol.120 (2), p.30-38 |
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Sprache: | eng |
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