Hydrocarbon gases in ODP Leg 104 samples

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Autori principali: Kvenvolden, Keith A, Golan-Bac, Margaret, McDonald, Thomas J, Pflaum, Ronald C, Brooks, James M
Natura: Dataset Open Access
Lingua:en
Pubblicazione: PANGAEA 1989
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author Kvenvolden, Keith A
Golan-Bac, Margaret
McDonald, Thomas J
Pflaum, Ronald C
Brooks, James M
author_facet Kvenvolden, Keith A
Golan-Bac, Margaret
McDonald, Thomas J
Pflaum, Ronald C
Brooks, James M
collection Datos científicos de ciencias marinas y ambientales
contents Geochemical studies at three ODP Leg 104 sites on the Wring Plateau help define the distribution of hydrocarbon gases in sediment of this prominent feature of the Norwegian continental margin. Low levels of hydrocarbon gas were encountered in sediment of the outer part of the plateau, but sediment of the inner part of the plateau is very gassy. The molecular composition of inner plateau gases (>99.9% methane) and the carbon isotopic composition of the methane (avg. = -76 per mil relative to the PDB standard) clearly show that the gas is biogenic. Heavier hydrocarbon gases accompany this methane, and their presence is probably a result of both chemical and microbial low-temperature diagenesis. Although these heavier hydrocarbons were not detected in sediment of the outer part of the plateau during shipboard analyses, subsequent shore-based analyses showed that these compounds are present at very low concentrations. Methane in the gassy sediment of the inner part of the plateau may be present as gas hydrates, judging from sedimentological and inorganic geochemical considerations, but no discernible gas hydrates were recovered during drilling.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_736715
institution PANGAEA
language en
publishDate 1989
publisher PANGAEA
record_format pangaea
spellingShingle Hydrocarbon gases in ODP Leg 104 samples
Kvenvolden, Keith A
Golan-Bac, Margaret
McDonald, Thomas J
Pflaum, Ronald C
Brooks, James M
104-642; 104-643A; 104-644; 104-644A; COMPCORE; Composite Core; DRILL; Drilling/drill rig; Joides Resolution; Leg104; Norwegian Sea; Ocean Drilling Program; ODP
Geochemical studies at three ODP Leg 104 sites on the Wring Plateau help define the distribution of hydrocarbon gases in sediment of this prominent feature of the Norwegian continental margin. Low levels of hydrocarbon gas were encountered in sediment of the outer part of the plateau, but sediment of the inner part of the plateau is very gassy. The molecular composition of inner plateau gases (>99.9% methane) and the carbon isotopic composition of the methane (avg. = -76 per mil relative to the PDB standard) clearly show that the gas is biogenic. Heavier hydrocarbon gases accompany this methane, and their presence is probably a result of both chemical and microbial low-temperature diagenesis. Although these heavier hydrocarbons were not detected in sediment of the outer part of the plateau during shipboard analyses, subsequent shore-based analyses showed that these compounds are present at very low concentrations. Methane in the gassy sediment of the inner part of the plateau may be present as gas hydrates, judging from sedimentological and inorganic geochemical considerations, but no discernible gas hydrates were recovered during drilling.
title Hydrocarbon gases in ODP Leg 104 samples
topic 104-642; 104-643A; 104-644; 104-644A; COMPCORE; Composite Core; DRILL; Drilling/drill rig; Joides Resolution; Leg104; Norwegian Sea; Ocean Drilling Program; ODP
url https://doi.org/10.1594/PANGAEA.736715