Detailed analysis of the organic carbon content in sediment cores M0002 and M0004

Fuente: PANGAEA
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Autor principal: Stein, Ruediger
Formato: Dataset Open Access
Lenguaje:en
Publicado: PANGAEA 2007
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author Stein, Ruediger
author_facet Stein, Ruediger
collection Datos científicos de ciencias marinas y ambientales
contents During IODP Expedition 302 (Arctic Coring Expedition-ACEX), the first scientific drilling campaign in the permantly ice-covered central Arctic Ocean, a 430 m thick sequence of upper Cretaceaous to Quaternary sediments has been drilled. The lower half of this sequence is composed of organic-carbon-rich (black shale-type) sediments with total organic carbon contents of about 1–14%. Significant amounts of the organic matter preserved in these sediments is of algae-type origin and accumulated under anoxic/euxinic conditions. Here, for the first time detailed data on the source-rock potential of these black shales are presented, indicating that most of the Eocene sediments have a (fair to) good source-rock potential, prone to generate a gas/oil mixture. The source-rock potential of the Campanian and upper Paleocene sediments, on the other hand, is rather low. The presence of oil or gas already generated in situ, however, can be ruled out due to the immaturity of the ACEX sediments.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_552044
institution PANGAEA
language en
publishDate 2007
publisher PANGAEA
record_format pangaea
spellingShingle Detailed analysis of the organic carbon content in sediment cores M0002 and M0004
Stein, Ruediger
302-M0002A; 302-M0004A; 302-M0004B; 302-M0004C; ACEX-M2A; ACEX-M4A; ACEX-M4B; ACEX-M4C; Arctic Coring Expedition, ACEX; Arctic Ocean; CCGS Captain Molly Kool (Vidar Viking); Exp302; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP
During IODP Expedition 302 (Arctic Coring Expedition-ACEX), the first scientific drilling campaign in the permantly ice-covered central Arctic Ocean, a 430 m thick sequence of upper Cretaceaous to Quaternary sediments has been drilled. The lower half of this sequence is composed of organic-carbon-rich (black shale-type) sediments with total organic carbon contents of about 1–14%. Significant amounts of the organic matter preserved in these sediments is of algae-type origin and accumulated under anoxic/euxinic conditions. Here, for the first time detailed data on the source-rock potential of these black shales are presented, indicating that most of the Eocene sediments have a (fair to) good source-rock potential, prone to generate a gas/oil mixture. The source-rock potential of the Campanian and upper Paleocene sediments, on the other hand, is rather low. The presence of oil or gas already generated in situ, however, can be ruled out due to the immaturity of the ACEX sediments.
title Detailed analysis of the organic carbon content in sediment cores M0002 and M0004
topic 302-M0002A; 302-M0004A; 302-M0004B; 302-M0004C; ACEX-M2A; ACEX-M4A; ACEX-M4B; ACEX-M4C; Arctic Coring Expedition, ACEX; Arctic Ocean; CCGS Captain Molly Kool (Vidar Viking); Exp302; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP
url https://doi.org/10.1594/PANGAEA.552044