Constarium
← Search

Data · dataset · 2006

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

Listed in DataCite

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.

Description

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.

Links

Topics

Inferred from text
Tabular 65%
Provenance · 1 source records, 7 field assertions
SourceKeyLast seenRaw
DataCite10.1594/pangaea.72392012 d agoJSON v1
FieldAssertionExtractorEvidence
access_levelsource · DataCiteconnector:datacite@1.0.0/data/attributes/rightsList
concepts[modality].local:modality:tabularenrichment · DataCitekeyword-concept-rules@1.0.0title+description (65%)
descriptionsource · DataCiteconnector:datacite@1.0.0/data/attributes/descriptions
licensesource · DataCiteconnector:datacite@1.0.0/data/attributes/rightsList
publication_datesource · DataCiteconnector:datacite@1.0.0/data/attributes/dates
spatialsource · DataCiteconnector:datacite@1.0.0
titlesource · DataCiteconnector:datacite@1.0.0/data/attributes/titles/0/title