Stable oxygen isotope ratios of marine barite from Cenozoic sediments
We report new data on oxygen isotopes in marine sulfate (delta18O[SO4]), measured in marine barite (BaSO4), over the Cenozoic. The delta18O[SO4] varies by 6x over the Cenozoic, with major peaks 3, 15, 30 and 55 Ma. The delta18O[SO4] does not co-vary with the delta18O[SO4], emphasizing that different...
Main Authors: | , |
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Format: | Dataset |
Language: | English |
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PANGAEA
2006
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.707885 https://doi.org/10.1594/PANGAEA.707885 |