Organic geochemistry of Cretaceous black shales from the Galicia Margin

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Hauptverfasser: Meyers, Philip A, Dunham, Keith W, Ho, Eileen S
Format: Dataset Open Access
Sprache:en
Veröffentlicht: PANGAEA 1987
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author Meyers, Philip A
Dunham, Keith W
Ho, Eileen S
author_facet Meyers, Philip A
Dunham, Keith W
Ho, Eileen S
collection Datos científicos de ciencias marinas y ambientales
contents Organic-carbon-rich "black shales" from three different Cretaceous episodes sampled during Ocean Drilling Program Leg 103 have been studied by organic geochemical methods. Rock-Eval analysis, carbon isotope data, and lipid biomarkers show organic matter to contain varying proportions of marine and continental materials. In Hauterivian-Barremian organic-carbon-rich turbiditic marlstones, major amounts of land-derived organic matter are found. Aptian-Albian black-colored shales are interspersed within green claystones, from which they differ by containing more marine organic matter. An abbreviated layer of black shale from the Cenomanian-Turonian boundary is dominated by well-preserved marine organic matter. Downslope transport and rapid reburial within a predominantly oxygenated deepwater setting created most of these examples of black shales, except for the Cenomanian-Turonian deposits in which deepwater anoxia may have been involved.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_757260
institution PANGAEA
language en
publishDate 1987
publisher PANGAEA
record_format pangaea
spellingShingle Organic geochemistry of Cretaceous black shales from the Galicia Margin
Meyers, Philip A
Dunham, Keith W
Ho, Eileen S
103-638B; 103-641A; 103-641C; DRILL; Drilling/drill rig; Joides Resolution; Leg103; North Atlantic Ocean; Ocean Drilling Program; ODP
Organic-carbon-rich "black shales" from three different Cretaceous episodes sampled during Ocean Drilling Program Leg 103 have been studied by organic geochemical methods. Rock-Eval analysis, carbon isotope data, and lipid biomarkers show organic matter to contain varying proportions of marine and continental materials. In Hauterivian-Barremian organic-carbon-rich turbiditic marlstones, major amounts of land-derived organic matter are found. Aptian-Albian black-colored shales are interspersed within green claystones, from which they differ by containing more marine organic matter. An abbreviated layer of black shale from the Cenomanian-Turonian boundary is dominated by well-preserved marine organic matter. Downslope transport and rapid reburial within a predominantly oxygenated deepwater setting created most of these examples of black shales, except for the Cenomanian-Turonian deposits in which deepwater anoxia may have been involved.
title Organic geochemistry of Cretaceous black shales from the Galicia Margin
topic 103-638B; 103-641A; 103-641C; DRILL; Drilling/drill rig; Joides Resolution; Leg103; North Atlantic Ocean; Ocean Drilling Program; ODP
url https://doi.org/10.1594/PANGAEA.757260