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...
Main Authors: | , , |
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Format: | Dataset |
Language: | English |
Published: |
PANGAEA
1980
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.682289 https://doi.org/10.1594/PANGAEA.682289 |