Middle to late Miocene oxygen isotope stratigraphy of ODP site 1085 (SE Atlantic): new constrains on Miocene climate variability and sea-level fluctuations
The middle Miocene delta18O increase represents a fundamental change in earth's climate system due to a major expansion and permanent establishment of the East Antarctic Ice Sheet accompanied by some effect of deepwater cooling. The long-term cooling trend in the middle to late Miocene was supe...
Main Authors: | , , |
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Format: | Dataset |
Language: | English |
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PANGAEA
2005
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.694041 https://doi.org/10.1594/PANGAEA.694041 |