WARMINGS IN THE FAR NORTHWESTERN PACIFIC PROMOTED PRE-CLOVIS IMMIGRATION TO AMERICA DURING HEINRICH EVENT 1

Sarnthein M.; Kiefer T.; Elderfield H.; Grootes P.M.; Erlenkeuser H.

dc.contributor.author	Sarnthein M.
dc.contributor.author	Kiefer T.
dc.contributor.author	Elderfield H.
dc.contributor.author	Grootes P.M.
dc.contributor.author	Erlenkeuser H.
dc.date.accessioned	2024-12-28T06:16:15Z
dc.date.available	2024-12-28T06:16:15Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13732298
dc.identifier.citation	Geology, 2006, 34, 3, 141-144
dc.identifier.issn	0091-7613
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/47150
dc.description.abstract	Well-dated multidecadal-to centennial-scale sediment records from the subarctic northwest Pacific show that the early deglacial 18.5-15.0 ka was marked by 3 pronounced short-term warmings of ~5 °C. They lasted 500-1500 yr each and were coeval with early to late stages of cold Heinrich event 1 in the North Atlantic. These regional climate windows may have promoted a pre-Clovis emigration of people from the cold-arid monsoon climate in East Asia to the climatically more favorable, then-emerged Beringian and Aleutian shelf regions and the Americas, as suggested by archeological findings. © 2006 Geological Society of America.
dc.subject	HEINRICH I STADIAL
dc.subject	PALEOCEANOGRAPHY
dc.subject	PRE-CLOVIS IMMIGRATION
dc.subject	SEA-SURFACE WARMING
dc.subject	SUBARCTIC NORTH PACIFIC
dc.title	WARMINGS IN THE FAR NORTHWESTERN PACIFIC PROMOTED PRE-CLOVIS IMMIGRATION TO AMERICA DURING HEINRICH EVENT 1
dc.type	Статья
dc.identifier.doi	10.1130/G22200.1