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...

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Bibliographic Details
Main Authors: Westerhold, Thomas, Bickert, Torsten, Röhl, Ursula
Format: Dataset
Language:English
Published: PANGAEA 2005
Subjects:
ODP
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.694041
https://doi.org/10.1594/PANGAEA.694041