Sedimentology and geochemistry of core GIK23258-2 in the Barents Sea
At the western continental margin of the Barents Sea, 75°N, hemipelagic sediments provide a record of Holocene climate change with a time resolution of 10-70 years. Planktic foraminifera counts reveal a very early Holocene thermal optimum 10.7-7.7 kyr BP, with summer sea surface temperatures (SST) o...
Main Authors: | , , , , , , |
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Format: | Other/Unknown Material |
Language: | English |
Published: |
PANGAEA
2003
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.727691 https://doi.org/10.1594/PANGAEA.727691 |