Stable isotope ratios of benthic and planktonic foraminifera from Late Miocene sediments of DSDP Hole 24-238 on the Central Indian Ocean Ridge (Appendix 1)

Tropical Indian Ocean planktonic and benthic foraminifera have 13C/12C ratios which change abruptly within Magnetic Epoch 6 about 6.2 million years ago. All species analyzed in the Late Miocene section of DSDP Site 238 show a shift towards lighter values of delta13C by about 0.8‰. The oxygen isotope...

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Bibliographic Details
Main Authors: Vincent, Edith, Killingley, John S, Berger, Wolfgang H
Format: Dataset
Language:English
Published: PANGAEA 1980
Subjects:
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.682289
https://doi.org/10.1594/PANGAEA.682289