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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Detalhes bibliográficos
Main Authors: 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.
Formato: Artigo
Idioma:Inglês
Publicado em: National Academy of Sciences 2014
Assuntos:
Physical Sciences
Acesso em linha: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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