Late Pleistocene proxy records of sediment core GeoB3388-1 from the eastern subtropical Pacific

Paleoceanographic evidence from midlatitudes bearing on the long-term development of Pacific Ocean surface circulation through the middle and late Pleistocene is scant because of a lack of marine paleorecords exceeding the last four or five glacial cycles. Here we compare benthic and planktonic fora...

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Bibliographic Details
Main Authors: Mohtadi, Mahyar, Hebbeln, Dierk, Nunez-Ricardo, Samuel, Lange, Carina Beatriz
Format: Dataset
Language:English
Published: PANGAEA 2006
Subjects:
SL
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.686213
https://doi.org/10.1594/PANGAEA.686213