Stable isotope ratios of foraminifera from various DSDP/ODP sites
The equator to high southern latitude sea surface and vertical temperature gradients are reconstructed from oxygen isotope values of planktonic and benthic foraminifers for the following five time intervals: late Paleocene, early Eocene, early middle Eocene, late Eocene, and early Oligocene. Paleote...
Main Authors: | , , |
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Format: | Other/Unknown Material |
Language: | English |
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PANGAEA
1994
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Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.729901 https://doi.org/10.1594/PANGAEA.729901 |