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...
Main Authors: | , , |
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Format: | Dataset |
Language: | English |
Published: |
PANGAEA
2003
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.695369 https://doi.org/10.1594/PANGAEA.695369 |