(Table 2) C-14 age data from ODP Hole 145-883

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...

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Bibliographic Details
Main Authors: Sarnthein, Michael, Kiefer, Thorsten, Grootes, Pieter Meiert, Elderfield, Henry, Erlenkeuser, Helmut
Format: Dataset
Language:English
Published: PANGAEA 2006
Subjects:
145-883
Accelerator mass spectrometry (AMS)
Age
comment
dated
dated material
dated standard deviation
Calculated
Calendar age
COMPCORE
Composite Core
DEPTH
sediment/rock
Joides Resolution
Leg145
North Pacific Ocean
Ocean Drilling Program
ODP
Reservoir effect/correction
Sample
optional label/labor no
North Atlantic
Subarctic
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.723920
https://doi.org/10.1594/PANGAEA.723920
Description
Summary: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.

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