Late Eocene to early Oligocene oxygen and carbon isotope records and biogenic barium accumulation rates in Maud Rise, Kerguelen Plateau and Agulhas Ridge

The late Eocene through early Oligocene (40-33 Ma) represents a transition from a warm-house to icehouse climate mode, with the expansion of Antarctic glaciation shortly after the Eocene/Oligocene (E/O) boundary. Identifying the driving mechanisms for this climatic event remains controversial and de...

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Bibliographic Details
Main Authors: Faria, Gabrielle R, Lazarus, David B, Renaudie, Johan, Stammeier, Jessica, Özen, Volkan, Struck, Ulrich
Format: Dataset
Language:English
Published: PANGAEA
Subjects:
ODP
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.959619