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...

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Bibliographic Details
Main Authors: Katz, Miriam E, Cramer, Benjamin S, Toggweiler, J Robbie, Esmay, Gar, Liu, Chengji, Miller, Kenneth G, Rosenthal, Yair, Wade, Bridget S, Wright, James D
Format: Other/Unknown Material
Language:English
Published: PANGAEA 2011
Subjects:
ODP
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.771562
https://doi.org/10.1594/PANGAEA.771562