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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Bibliographic Details
Main Authors: Curry, William B, Miller, Kenneth G
Format: Other/Unknown Material
Language:English
Published: PANGAEA 1989
Subjects:
ODP
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.696223
https://doi.org/10.1594/PANGAEA.696223