(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...

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Bibliographic Details
Main Authors: Delaney, Margaret Lois, Boyle, Edward A
Format: Dataset
Language:English
Published: PANGAEA 1987
Subjects:
AGE
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.770015
https://doi.org/10.1594/PANGAEA.770015