Paleoceanographic significance of high-resolution carbon isotope records across the Cenomanian-Turonian boundary in the Western Interior and New Jersey coastal plain, USA

Andrew R. Bowman; Timothy J. Bralower

doi:10.1016/j.margeo.2005.02.010

Paleoceanographic significance of high-resolution carbon isotope records across the Cenomanian-Turonian boundary in the Western Interior and New Jersey coastal plain, USA

Andrew R. Bowman, Timothy J. Bralower

Geosciences

Research output: Contribution to journal › Article › peer-review

77 Scopus citations

Abstract

Carbon isotope measurements have been made on bulk carbonate and organic matter in three sections across the Cenomanian-Turonian boundary. The stratigraphy records the positive carbon isotopic excursion that is associated with the major oceanic anoxic event (OAE2). Comparison of TOC and isotopic data in sections from a range of different environments suggests that the positive excursion is a response to increased burial of organic matter in the deep ocean. The lack of coupled negative shifts in δ¹³C_org and δ¹³C_carb records at the onset of OAE2 does not support a causal role for volcanism or methane hydrate dissociation.

Original language	English (US)
Pages (from-to)	305-321
Number of pages	17
Journal	Marine Geology
Volume	217
Issue number	3-4
DOIs	https://doi.org/10.1016/j.margeo.2005.02.010
State	Published - Jun 15 2005

All Science Journal Classification (ASJC) codes

Oceanography
Geology
Geochemistry and Petrology

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10.1016/j.margeo.2005.02.010

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@article{a15dda6f55c04a1cb2f9b4713a3ef866,

title = "Paleoceanographic significance of high-resolution carbon isotope records across the Cenomanian-Turonian boundary in the Western Interior and New Jersey coastal plain, USA",

abstract = "Carbon isotope measurements have been made on bulk carbonate and organic matter in three sections across the Cenomanian-Turonian boundary. The stratigraphy records the positive carbon isotopic excursion that is associated with the major oceanic anoxic event (OAE2). Comparison of TOC and isotopic data in sections from a range of different environments suggests that the positive excursion is a response to increased burial of organic matter in the deep ocean. The lack of coupled negative shifts in δ13Corg and δ13Ccarb records at the onset of OAE2 does not support a causal role for volcanism or methane hydrate dissociation.",

author = "Bowman, \{Andrew R.\} and Bralower, \{Timothy J.\}",

note = "Funding Information: We thank Jason Eleson, Jim, Bergen and Dave Watkins for field assistance and Howard Mendlovitz, Isabel Monta{\~n}ez, and Jim Wright for help with stable isotope analysis. We are grateful to Hugh Jenkyns for sharing unpublished data and to Elisabetta Erba for her thorough review of an earlier manuscript. Research funded by NSF OCE 0084032 Biocomplexity: The Evolution and the Radiation of Eucarytoic Phytoplankton Taxa (EREUPT).",

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doi = "10.1016/j.margeo.2005.02.010",

language = "English (US)",

volume = "217",

pages = "305--321",

journal = "Marine Geology",

issn = "0025-3227",

publisher = "Elsevier B.V.",

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T1 - Paleoceanographic significance of high-resolution carbon isotope records across the Cenomanian-Turonian boundary in the Western Interior and New Jersey coastal plain, USA

AU - Bowman, Andrew R.

AU - Bralower, Timothy J.

N1 - Funding Information: We thank Jason Eleson, Jim, Bergen and Dave Watkins for field assistance and Howard Mendlovitz, Isabel Montañez, and Jim Wright for help with stable isotope analysis. We are grateful to Hugh Jenkyns for sharing unpublished data and to Elisabetta Erba for her thorough review of an earlier manuscript. Research funded by NSF OCE 0084032 Biocomplexity: The Evolution and the Radiation of Eucarytoic Phytoplankton Taxa (EREUPT).

PY - 2005/6/15

Y1 - 2005/6/15

N2 - Carbon isotope measurements have been made on bulk carbonate and organic matter in three sections across the Cenomanian-Turonian boundary. The stratigraphy records the positive carbon isotopic excursion that is associated with the major oceanic anoxic event (OAE2). Comparison of TOC and isotopic data in sections from a range of different environments suggests that the positive excursion is a response to increased burial of organic matter in the deep ocean. The lack of coupled negative shifts in δ13Corg and δ13Ccarb records at the onset of OAE2 does not support a causal role for volcanism or methane hydrate dissociation.

AB - Carbon isotope measurements have been made on bulk carbonate and organic matter in three sections across the Cenomanian-Turonian boundary. The stratigraphy records the positive carbon isotopic excursion that is associated with the major oceanic anoxic event (OAE2). Comparison of TOC and isotopic data in sections from a range of different environments suggests that the positive excursion is a response to increased burial of organic matter in the deep ocean. The lack of coupled negative shifts in δ13Corg and δ13Ccarb records at the onset of OAE2 does not support a causal role for volcanism or methane hydrate dissociation.

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U2 - 10.1016/j.margeo.2005.02.010

DO - 10.1016/j.margeo.2005.02.010

M3 - Article

AN - SCOPUS:20144379654

SN - 0025-3227

VL - 217

SP - 305

EP - 321

JO - Marine Geology

JF - Marine Geology

IS - 3-4

ER -

Paleoceanographic significance of high-resolution carbon isotope records across the Cenomanian-Turonian boundary in the Western Interior and New Jersey coastal plain, USA

Abstract

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