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...
Main Authors: | , |
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Format: | Dataset |
Language: | English |
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PANGAEA
1982
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Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.726254 https://doi.org/10.1594/PANGAEA.726254 |