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Younger Dryas deglaciation of Scotland driven by warming summers
The Younger Dryas Stadial (YDS; ∼12,900–11,600 y ago) in the Northern Hemisphere is classically defined by abrupt cooling and renewed glaciation during the last glacial–interglacial transition. Although this event involved a global reorganization of atmospheric and oceanic circulation [Denton GH, Al...
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| Hauptverfasser: | , , , , , , , , |
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| Format: | Artigo |
| Sprache: | Inglês |
| Veröffentlicht: |
National Academy of Sciences
2014
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| Schlagworte: | |
| Online Zugang: | https://ncbi.nlm.nih.gov/pmc/articles/PMC4035952/ https://ncbi.nlm.nih.gov/pubmed/24733909 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1321122111 |
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