(Table 1) Cd/Ca and Mn/Ca ratios of benthic foraminifera from DSDP Hole 30-289
The late Miocene carbon shift (~6.2 Myr) -a 0.5-1.0 per mil, d13C decrease in benthic and planktonic foraminifera- has been ascribed to changes in global inventory, deep-ocean circulation, and/or productivity. Cadmium, d13C, and nutrients in the ocean are linked; comparison of d13C and Cd/Ca yields...
Main Authors: | , |
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Format: | Dataset |
Language: | English |
Published: |
PANGAEA
1987
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.770015 https://doi.org/10.1594/PANGAEA.770015 |