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Volcanic origin for Younger Dryas geochemical anomalies ca. 12,900 cal B.P.
The Younger Dryas (YD) abrupt cooling event ca. 12.9 ± 0.1 ka is associated with substantial meltwater input into the North Atlantic Ocean, reversing deglacial warming. One controversial and prevailing hypothesis is that a bolide impact or airburst is responsible for these environmental changes. Her...
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| Publicado no: | Sci Adv |
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| Main Authors: | , , , , |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
American Association for the Advancement of Science
2020
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| Assuntos: | |
| Acesso em linha: | https://ncbi.nlm.nih.gov/pmc/articles/PMC7399481/ https://ncbi.nlm.nih.gov/pubmed/32789166 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1126/sciadv.aax8587 |
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