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...
Main Authors: | , , , |
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Format: | Dataset |
Language: | English |
Published: |
PANGAEA
2006
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.686213 https://doi.org/10.1594/PANGAEA.686213 |