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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Bibliografski detalji
Glavni autori: Bromley, Gordon R. M., Putnam, Aaron E., Rademaker, Kurt M., Lowell, Thomas V., Schaefer, Joerg M., Hall, Brenda, Winckler, Gisela, Birkel, Sean D., Borns, Harold W.
Format: Artigo
Jezik:Inglês
Izdano: National Academy of Sciences 2014
Teme:
Physical Sciences
Online pristup: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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