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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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Bibliografski detalji
Izdano u:Sci Adv
Glavni autori: Sun, N., Brandon, A. D., Forman, S. L., Waters, M. R., Befus, K. S.
Format: Artigo
Jezik:Inglês
Izdano: American Association for the Advancement of Science 2020
Teme:
Online pristup: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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