Oxygen-isotope composition of diagenetic calcite in organic-rich rocks: evidence for                          18                         O depletion in marine anaerobic pore water

E. Sass; A. Bein; A. Almogi-Labin

doi:10.1130/0091-7613(1991)019<0839:OICODC>2.3.CO;2

Oxygen-isotope composition of diagenetic calcite in organic-rich rocks: evidence for ¹⁸ O depletion in marine anaerobic pore water

E. Sass
, A. Bein
, A. Almogi-Labin

Fredy & Nadine Herrmann Institute of Earth Sciences

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

134 Scopus citations

Abstract

Upper Cretaceous organic-rich carbonates in Israel contain benthonic foraminifera and varying amounts of early diagenetic infilling of sparry calcite. Relates to light oxygen compositions of the diagenetic calcite to depletion of ¹⁸ O in pore water of normal salinity, a direct consequence of organic matter decomposition in the sulfate-reducing zone. -from Authors

Original language	English
Pages (from-to)	839-842
Number of pages	4
Journal	Geology
Volume	19
Issue number	8
DOIs	https://doi.org/10.1130/0091-7613(1991)019<0839:OICODC>2.3.CO;2
State	Published - 1991

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10.1130/0091-7613(1991)019<0839:OICODC>2.3.CO;2

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title = "Oxygen-isotope composition of diagenetic calcite in organic-rich rocks: evidence for 18 O depletion in marine anaerobic pore water",

abstract = " Upper Cretaceous organic-rich carbonates in Israel contain benthonic foraminifera and varying amounts of early diagenetic infilling of sparry calcite. Relates to light oxygen compositions of the diagenetic calcite to depletion of 18 O in pore water of normal salinity, a direct consequence of organic matter decomposition in the sulfate-reducing zone. -from Authors ",

author = "E. Sass and A. Bein and A. Almogi-Labin",

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doi = "10.1130/0091-7613(1991)019<0839:OICODC>2.3.CO;2",

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PY - 1991

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AB - Upper Cretaceous organic-rich carbonates in Israel contain benthonic foraminifera and varying amounts of early diagenetic infilling of sparry calcite. Relates to light oxygen compositions of the diagenetic calcite to depletion of 18 O in pore water of normal salinity, a direct consequence of organic matter decomposition in the sulfate-reducing zone. -from Authors

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Oxygen-isotope composition of diagenetic calcite in organic-rich rocks: evidence for ¹⁸ O depletion in marine anaerobic pore water

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