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Archive · collection · 1989

Age determination and sea surface temperature reconstruction for the Southern Ocean

Listed in PANGAEA and DataCite — shown once because both records carry DOI 10.1594/pangaea.727006

The isotopic and micropaleontological deglacial records of three deep-sea cores from 44°S to 55°S have been dated by accelerator mass spectrometry.

Description

The available records did not allow accurate dating of the initiation of the deglaciation. By 13,000 years B.P., sea surface temperatures reached values similar to the present values.

A cool oscillation abruptly interrupted this warm phase between 12,000 and 11,000 years B.P. Initiation of this cooling therefore preceded the northern hemisphere Younger Dryas by approximately 1000 years. Complete warming was reached by 10,000 years B.P., more or less synchronous with the northeast Atlantic Ocean.

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Inferred from text
Mass spectrometry 75%
Provenance · 2 source records, 8 field assertions
SourceKeyLast seenRaw
PANGAEAoai:pangaea.de:doi:10.1594/PANGAEA.72700614 d agoJSON v1
DataCite10.1594/pangaea.72700614 d agoJSON v1
FieldAssertionExtractorEvidence
access_levelsource · PANGAEAconnector:pangaea@1.0.0
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concepts[modality].local:modality:mass-spectrometryenrichment · PANGAEAkeyword-concept-rules@1.0.0title+description (75%)
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licensesource · PANGAEAconnector:pangaea@1.0.0/metadata/dc/rights
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