Benthic foraminiferal and bulk sediment stable isotope records, and carbonate content records from the eastern equatorial Pacific, and a reconstruction of the calcite compensation depth, across the EO

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Auteurs principaux: Taylor, Victoria E, Westerhold, Thomas, Bohaty, Steven M, Backman, Jan, Dunkley Jones, Tom, Egan, Katie, Edgar, Kirsty M, Lyle, Mitchell W, Pälike, Heiko, Röhl, Ursula, Zachos, James C, Wilson, Paul A
Format: Dataset Open Access
Langue:en
Publié: PANGAEA 2023
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author Taylor, Victoria E
Westerhold, Thomas
Bohaty, Steven M
Backman, Jan
Dunkley Jones, Tom
Egan, Katie
Edgar, Kirsty M
Lyle, Mitchell W
Pälike, Heiko
Röhl, Ursula
Zachos, James C
Wilson, Paul A
author_facet Taylor, Victoria E
Westerhold, Thomas
Bohaty, Steven M
Backman, Jan
Dunkley Jones, Tom
Egan, Katie
Edgar, Kirsty M
Lyle, Mitchell W
Pälike, Heiko
Röhl, Ursula
Zachos, James C
Wilson, Paul A
collection Datos científicos de ciencias marinas y ambientales
contents 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 (EOT; ~34 Ma), suggesting a strong relationship between calcium carbonate (CaCO3) cycling and Antarctic glaciation. To further investigate the linkages between these two events, detailed records of deep-sea carbonate content, and bulk sediment and benthic foraminiferal stable isotope records are needed. This dataset contains bulk sediment stable isotope and carbonate content records from eight sites in the eastern equatorial Pacific (ODP Leg 199 and IODP Expedition 320). These records were used to reconstruct the depth of the calcite compensation depth (CCD) across the Eocene-Oligocene Transition. The projected depth of the CCD is included in this dataset. In addition, this dataset contains a monospecific epifaunal benthic foraminiferal stable isotope stratigraphy from IODP Expedition 320 Site U1334, in the eastern equatorial Pacific, across the Eocene-Oligocene Transition.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_956848
institution PANGAEA
language en
publishDate 2023
publisher PANGAEA
record_format pangaea
spellingShingle Benthic foraminiferal and bulk sediment stable isotope records, and carbonate content records from the eastern equatorial Pacific, and a reconstruction of the calcite compensation depth, across the EO
Taylor, Victoria E
Westerhold, Thomas
Bohaty, Steven M
Backman, Jan
Dunkley Jones, Tom
Egan, Katie
Edgar, Kirsty M
Lyle, Mitchell W
Pälike, Heiko
Röhl, Ursula
Zachos, James C
Wilson, Paul A
CCD; Eocene-Oligocene Transition; IODP Exp. 320; ODP Leg 199
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 (EOT; ~34 Ma), suggesting a strong relationship between calcium carbonate (CaCO3) cycling and Antarctic glaciation. To further investigate the linkages between these two events, detailed records of deep-sea carbonate content, and bulk sediment and benthic foraminiferal stable isotope records are needed. This dataset contains bulk sediment stable isotope and carbonate content records from eight sites in the eastern equatorial Pacific (ODP Leg 199 and IODP Expedition 320). These records were used to reconstruct the depth of the calcite compensation depth (CCD) across the Eocene-Oligocene Transition. The projected depth of the CCD is included in this dataset. In addition, this dataset contains a monospecific epifaunal benthic foraminiferal stable isotope stratigraphy from IODP Expedition 320 Site U1334, in the eastern equatorial Pacific, across the Eocene-Oligocene Transition.
title Benthic foraminiferal and bulk sediment stable isotope records, and carbonate content records from the eastern equatorial Pacific, and a reconstruction of the calcite compensation depth, across the EO
topic CCD; Eocene-Oligocene Transition; IODP Exp. 320; ODP Leg 199
url https://doi.org/10.1594/PANGAEA.956848