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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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| Autori principali: | , , , , , , |
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| Natura: | Artigo |
| Lingua: | Inglês |
| Pubblicazione: |
National Academy of Sciences
2007
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| Soggetti: | |
| Accesso online: | 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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