Stable oxygen and carbon isotope data for the Mid-Pleistocene Transition (MPT)
To investigate potential changes in the North Atlantic intermediate water-mass configuration across the Mid-Pleistocene Transition (MPT; approx. 550-1200 ka) we utilize d18O and d13C records obtained on the deep thermocline-dwelling foraminifera Globorotalia crassaformis and benthic Cibicidoides wue...
Main Authors: | , , |
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Format: | Other/Unknown Material |
Language: | English |
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PANGAEA
2022
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Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.947028 https://doi.org/10.1594/PANGAEA.947028 |