Stable carbon and oxygen isotope ratios of Planulina wuellerstorfi from sediments of the Vema Channel

Oxygen- and carbon-isotopic analyses have been performed on the benthic foraminifer Planulina wuellerstorfi in seven Late Quaternary cores from the Vema Channel-Rio Grande Rise region. The cores are distributed over the water-depth interval of 2340 to 3939 m, which includes the present transition fr...

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Bibliographic Details
Main Authors: Curry, William B, Lohmann, G P
Format: Dataset
Language:English
Published: PANGAEA 1982
Subjects:
PC
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.726254
https://doi.org/10.1594/PANGAEA.726254