Shelf ecosystems along the U.S. Atlantic coastal plain prior to and during the Paleocene‐Eocene thermal maximum: Insights Into the stratigraphic architecture
Shelf ecosystems along the U.S. Atlantic coastal plain prior to and during the Paleocene‐Eocene thermal maximum: Insights Into the stratigraphic architecture
The Paleocene-Eocene Thermal Maximum (PETM) is the most pronounced global warming event of the early Paleogene related to atmospheric CO
2 increases. It is characterized by negative δ
18O and δ
13C excursions recorded in sedimentary archives and a transient disruption of the marine biosphere. Sites from the U.S. Atlantic Coastal Plain show an additional small, but distinct δ
13C excursion below the onset of the PETM, coined the “pre-onset excursion” (POE), mimicking the PETM-forced environmental perturbations. This study focuses on the South Dover Bridge core in Maryland, where the Paleocene-Eocene transition is stratigraphically constrained by calcareous nannoplankton and stable isotope data, and in which the POE is well-expressed. The site was situated in a middle neritic marine shelf setting near a major outflow of the paleo-Potomac River system. We generated high-resolution benthic foraminiferal assemblage, stable isotope, trace-metal, grain-size and clay mineralogy data. The resulting stratigraphic subdivision of this Paleocene-Eocene transition is placed within a depth transect across the paleoshelf, highlighting that the PETM sequence is relatively expanded. The geochemical records provide detailed insights into the paleoenvironment, developing from a well-oxygenated water column in latest Paleocene to a PETM-ecosystem under severe biotic stress-conditions, with shifts in food supply and temperature, and under dysoxic bottom waters in a more river-dominated setting. Environmental changes started in the latest Paleocene and culminated atthe onset of the PETM, hinting to an intensifying trigger rather than to an instantaneous event at the Paleocene-Eocene boundary toppling the global system.
Paleocene-Eocene Thermal Maximum (PETM), South Dover Bridge, benthic foraminifera, pre-onset excursion (POE), shelf ecosystem, stratigraphy
Doubrawa, Monika
8b83ffaf-8029-407b-bbcd-3a18cfe09fc6
Stassen, Peter
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Robinson, Marci M.
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Babila, Tali L.
a59f9473-d145-4d43-92c0-ea682f29fdcc
Zachos, James C.
c262d59f-aadc-4e09-b844-098db9a0e3c5
Speijer, Robert P.
00c09937-bce3-4673-9de2-ef9c2d9bcb0d
Doubrawa, Monika
8b83ffaf-8029-407b-bbcd-3a18cfe09fc6
Stassen, Peter
f2860860-6c1b-4bb9-ac6c-13da42517a91
Robinson, Marci M.
0979ef67-cd77-417c-a8bb-28dd8c6dafa0
Babila, Tali L.
a59f9473-d145-4d43-92c0-ea682f29fdcc
Zachos, James C.
c262d59f-aadc-4e09-b844-098db9a0e3c5
Speijer, Robert P.
00c09937-bce3-4673-9de2-ef9c2d9bcb0d
Doubrawa, Monika, Stassen, Peter, Robinson, Marci M., Babila, Tali L., Zachos, James C. and Speijer, Robert P.
(2022)
Shelf ecosystems along the U.S. Atlantic coastal plain prior to and during the Paleocene‐Eocene thermal maximum: Insights Into the stratigraphic architecture.
Paleoceanography and Paleoclimatology, 37 (10), [e2022PA004475].
(doi:10.1029/2022PA004475).
Abstract
The Paleocene-Eocene Thermal Maximum (PETM) is the most pronounced global warming event of the early Paleogene related to atmospheric CO
2 increases. It is characterized by negative δ
18O and δ
13C excursions recorded in sedimentary archives and a transient disruption of the marine biosphere. Sites from the U.S. Atlantic Coastal Plain show an additional small, but distinct δ
13C excursion below the onset of the PETM, coined the “pre-onset excursion” (POE), mimicking the PETM-forced environmental perturbations. This study focuses on the South Dover Bridge core in Maryland, where the Paleocene-Eocene transition is stratigraphically constrained by calcareous nannoplankton and stable isotope data, and in which the POE is well-expressed. The site was situated in a middle neritic marine shelf setting near a major outflow of the paleo-Potomac River system. We generated high-resolution benthic foraminiferal assemblage, stable isotope, trace-metal, grain-size and clay mineralogy data. The resulting stratigraphic subdivision of this Paleocene-Eocene transition is placed within a depth transect across the paleoshelf, highlighting that the PETM sequence is relatively expanded. The geochemical records provide detailed insights into the paleoenvironment, developing from a well-oxygenated water column in latest Paleocene to a PETM-ecosystem under severe biotic stress-conditions, with shifts in food supply and temperature, and under dysoxic bottom waters in a more river-dominated setting. Environmental changes started in the latest Paleocene and culminated atthe onset of the PETM, hinting to an intensifying trigger rather than to an instantaneous event at the Paleocene-Eocene boundary toppling the global system.
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Paleoceanog and Paleoclimatol - 2022 - Doubrawa_Accepted Version
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Paleoceanog and Paleoclimatol - 2022 - Doubrawa - Shelf Ecosystems Along the U S Atlantic Coastal Plain Prior to and
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Accepted/In Press date: 21 September 2022
e-pub ahead of print date: 3 October 2022
Keywords:
Paleocene-Eocene Thermal Maximum (PETM), South Dover Bridge, benthic foraminifera, pre-onset excursion (POE), shelf ecosystem, stratigraphy
Identifiers
Local EPrints ID: 474543
URI: http://eprints.soton.ac.uk/id/eprint/474543
ISSN: 2572-4525
PURE UUID: d57080dd-b2a5-4af1-9bff-b0e89696a668
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Date deposited: 24 Feb 2023 17:32
Last modified: 17 Mar 2024 03:52
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Contributors
Author:
Monika Doubrawa
Author:
Peter Stassen
Author:
Marci M. Robinson
Author:
Tali L. Babila
Author:
James C. Zachos
Author:
Robert P. Speijer
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