Stable isotope and Mg/Ca ratios of Paleogene benthic foraminifera in the western North Atlantic
Global cooling and the development of continental-scale Antarctic glaciation occurred in the late middle Eocene to early Oligocene (~38 to 28 million years ago), accompanied by deep-ocean reorganization attributed to gradual Antarctic Circumpolar Current (ACC) development. Our benthic foraminiferal...
Main Authors: | , , , , , , , , |
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Format: | Other/Unknown Material |
Language: | English |
Published: |
PANGAEA
2011
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.771562 https://doi.org/10.1594/PANGAEA.771562 |