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Geochemical proxies of North American freshwater routing during the Younger Dryas cold event

The Younger Dryas cold interval represents a time when much of the Northern Hemisphere cooled from ≈12.9 to 11.5 kiloyears B.P. The cause of this event, which has long been viewed as the canonical example of abrupt climate change, was initially attributed to the routing of freshwater to the St. Lawr...

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Detalhes bibliográficos
Main Authors: Carlson, Anders E., Clark, Peter U., Haley, Brian A., Klinkhammer, Gary P., Simmons, Kathleen, Brook, Edward J., Meissner, Katrin J.
Formato: Artigo
Idioma:Inglês
Publicado em: National Academy of Sciences 2007
Assuntos:
Acesso em linha:https://ncbi.nlm.nih.gov/pmc/articles/PMC1871824/
https://ncbi.nlm.nih.gov/pubmed/17420461
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.0611313104
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