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

Michael Allan Arthur, S. O. Schlanger, H. C. Jenkyns

Research output: Contribution to journalArticle

272 Citations (Scopus)

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 languageEnglish (US)
Pages (from-to)401-420
Number of pages20
JournalUnknown Journal
StatePublished - Jan 1 1987

Fingerprint

Turonian
sea level
organic matter
highstand
volcano
tectonics
basin
ocean circulation

All Science Journal Classification (ASJC) codes

  • Environmental Science(all)
  • Earth and Planetary Sciences(all)

Cite this

@article{d2c1299091934ac68ff85608beddfa04,
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, {Michael Allan} and Schlanger, {S. O.} and Jenkyns, {H. C.}",
year = "1987",
month = "1",
day = "1",
language = "English (US)",
pages = "401--420",
journal = "[No source information available]",
issn = "0042-1215",

}

The Cenomanian- Turonian Oceanic Anoxic Event, II. Palaeoceanographic controls on organic-matter production and preservation. / Arthur, Michael Allan; Schlanger, S. O.; Jenkyns, H. C.

In: Unknown Journal, 01.01.1987, p. 401-420.

Research output: Contribution to journalArticle

TY - JOUR

T1 - The Cenomanian- Turonian Oceanic Anoxic Event, II. Palaeoceanographic controls on organic-matter production and preservation.

AU - Arthur, Michael Allan

AU - Schlanger, S. O.

AU - Jenkyns, H. C.

PY - 1987/1/1

Y1 - 1987/1/1

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

UR - http://www.scopus.com/inward/record.url?scp=0023510987&partnerID=8YFLogxK

UR - http://www.scopus.com/inward/citedby.url?scp=0023510987&partnerID=8YFLogxK

M3 - Article

SP - 401

EP - 420

JO - [No source information available]

JF - [No source information available]

SN - 0042-1215

ER -