The Cenomanian- Turonian Oceanic Anoxic Event, II. Palaeoceanographic controls on organic-matter production and preservation.

M. A. Arthur; S. O. Schlanger; H. C. Jenkyns

The Cenomanian- Turonian Oceanic Anoxic Event, II. Palaeoceanographic controls on organic-matter production and preservation.

M. A. Arthur, S. O. Schlanger, H. C. Jenkyns

Geosciences

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

313 Scopus citations

Abstract

The OAE coincided with a maximum sea level highstand. Sea level, which may be responding to some volcano-tectonic event, is the common link and ultimately the driving force for ^orgC deposition in globally distributed basins under different climatic and ocean circulation regimes. -from Authors

Original language	English (US)
Pages (from-to)	401-420
Number of pages	20
Journal	Unknown Journal
State	Published - 1987

All Science Journal Classification (ASJC) codes

General Environmental Science
General Earth and Planetary Sciences

Cite this

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title = "The Cenomanian- Turonian Oceanic Anoxic Event, II. Palaeoceanographic controls on organic-matter production and preservation.",

abstract = "The OAE coincided with a maximum sea level highstand. Sea level, which may be responding to some volcano-tectonic event, is the common link and ultimately the driving force for orgC deposition in globally distributed basins under different climatic and ocean circulation regimes. -from Authors",

author = "Arthur, {M. A.} and Schlanger, {S. O.} and Jenkyns, {H. C.}",

year = "1987",

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pages = "401--420",

journal = "Unknown Journal",

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AU - Arthur, M. A.

AU - Schlanger, S. O.

AU - Jenkyns, H. C.

PY - 1987

Y1 - 1987

N2 - The OAE coincided with a maximum sea level highstand. Sea level, which may be responding to some volcano-tectonic event, is the common link and ultimately the driving force for orgC deposition in globally distributed basins under different climatic and ocean circulation regimes. -from Authors

AB - The OAE coincided with a maximum sea level highstand. Sea level, which may be responding to some volcano-tectonic event, is the common link and ultimately the driving force for orgC deposition in globally distributed basins under different climatic and ocean circulation regimes. -from Authors

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M3 - Article

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JO - Unknown Journal

JF - Unknown Journal

ER -

The Cenomanian- Turonian Oceanic Anoxic Event, II. Palaeoceanographic controls on organic-matter production and preservation.

Abstract

All Science Journal Classification (ASJC) codes

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