Buchumschlag

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...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Hauptverfasser: Taylor, Victoria (VerfasserIn) , Westerhold, T. (VerfasserIn) , Bohaty, Steven M. (VerfasserIn) , Backman, J. (VerfasserIn) , Dunkley Jones, T. (VerfasserIn) , Edgar, K. M. (VerfasserIn) , Egan, K. E. (VerfasserIn) , Lyle, M. (VerfasserIn) , Pälike, H. (VerfasserIn) , Röhl, U. (VerfasserIn) , Zachos, J. (VerfasserIn) , Wilson, Paul (VerfasserIn)
Dokumenttyp: Article (Journal)
Sprache:Englisch
Veröffentlicht: 18 May 2023
In: Paleoceanography and paleoclimatology
Year: 2023, Jahrgang: 38, Heft: 6, Pages: 1-15
ISSN:2572-4525
DOI:10.1029/2022PA004493
Online-Zugang:kostenfrei
kostenfrei
Volltext
Verfasserangaben: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
Beschreibung
Zusammenfassung: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 events are debated. Here we present new records of bulk sediment stable isotope and carbonate composition from a depth transect of sites in the low-latitude Pacific Ocean and one site from the South Atlantic Ocean, together with a new benthic foraminiferal stable isotope record (δ13Cb and δ18Ob) from the Pacific where the sedimentary sequence is most expanded. ...
Beschreibung:Gesehen am 22.11.2023
Beschreibung:Online Resource
ISSN:2572-4525
DOI:10.1029/2022PA004493

Ähnliche Einträge