Stable oxygen isotope record of benthic foraminifera from the tropical Atlantic
Benthic foraminiferal oxygen isotope ratios from two sediment cores recovered at 426 and 1299 m water depth in the eastern and western tropical Atlantic show that a slowdown of the thermohaline circulation (THC) during Heinrich event H1 and the Younger Dryas was accompanied by rapid and intense warm...
Main Authors: | , , , , , |
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Format: | Dataset |
Language: | English |
Published: |
PANGAEA
2004
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.737914 https://doi.org/10.1594/PANGAEA.737914 |