Transient shoaling, over-deepening and settling of the calcite compensation depth at the eocene-oligocene transition

The major Cenozoic shift from a shallow (∼3-4 km) to deep (∼4.5 km) calcite compensation depth (CCD) occurred at the Eocene-Oligocene Transition (∼34 Ma), suggesting a strong relationship between calcium carbonate (CaCO3) cycling and Antarctic glaciation. However, the linkages between these two even...

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Main Authors: Taylor, Victoria (Author) , Westerhold, T. (Author) , Bohaty, Steven M. (Author) , Backman, J. (Author) , Dunkley Jones, T. (Author) , Edgar, K. M. (Author) , Egan, K. E. (Author) , Lyle, M. (Author) , Pälike, H. (Author) , Röhl, U. (Author) , Zachos, J. (Author) , Wilson, Paul (Author)
Format: Article (Journal)
Language:English
Published: 18 May 2023
In: Paleoceanography and paleoclimatology
Year: 2023, Volume: 38, Issue: 6, Pages: 1-15
ISSN:2572-4525
DOI:10.1029/2022PA004493
Online Access:Verlag, kostenfrei, Volltext: https://doi.org/10.1029/2022PA004493
Verlag, kostenfrei, Volltext: https://onlinelibrary.wiley.com/doi/abs/10.1029/2022PA004493
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Author Notes:V.E. Taylor, T. Westerhold, S.M. Bohaty, J. Backman, T. Dunkley Jones, K.M. Edgar, K.E. Egan, M. Lyle, H. Pälike, U. Röhl, J. Zachos, and P.A. Wilson

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