Planktonic foraminiferal abundances and stable isotope ratios in middle Miocene sediments of the North Atlantic and the southwestern Pacific

A three-fold expansion of the Antarctic ice sheet at 13.60, 12.82, and 11.60 Ma has been inferred from delta18O maxima analyzed in planktonic and benthic foraminiferal tests, although accompanying changes in sea surface temperature have not been detailed. We present estimated changes in middle Mioce...

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Bibliographic Details
Main Authors: Ohta, Satoshi, Kaiho, Kunio, Takei, Tomohiro
Format: Dataset
Language:English
Published: PANGAEA 2003
Subjects:
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.695369
https://doi.org/10.1594/PANGAEA.695369