Stable oxygen and carbon isotope ratios of Pliocene benthic foraminifera in the Atlantic Ocean
Large changes in benthic foraminiferal delta180 and delta13C occurred during the Pliocene (between 3.0 and 2.0 Ma) at Hole 665A. Oxygen isotopic compositions increased to maximum values at 2.4 Ma, correlating with an 18O enrichment observed at Hole 552A and other locations (Shackleton et al., 1984)....
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Format: | Other/Unknown Material |
Language: | English |
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PANGAEA
1989
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Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.696223 https://doi.org/10.1594/PANGAEA.696223 |