Stable isotope analysis on planktic foraminifera in sediment cores from the eastern Mediterranean sapropel formation
During the late Pleistocene, sapropels (layers of organic-carbon rich sediment) formed throughout the entire Eastern Mediterranean Basin in close association with glacial/interglacial transitions. The current theory for the mechanism of sapropel formation involves a density stratification of the wat...
Main Authors: | , |
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Format: | Dataset |
Language: | English |
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PANGAEA
1984
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.727247 https://doi.org/10.1594/PANGAEA.727247 |