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...

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Bibliographic Details
Main Authors: Rühlemann, Carsten, Mulitza, Stefan, Lohmann, Gerrit, Paul, André, Prange, Matthias, Wefer, Gerold
Format: Dataset
Language:English
Published: PANGAEA 2004
Subjects:
SL
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.737914
https://doi.org/10.1594/PANGAEA.737914