Sedimentological, organic petrographic and organic chemical characteristics of Albian and Cenomanian/Turonian black shales from the North Altlantic (Tab. 3, 4) ...
Large parts of the Cretaceous Atlantic Ocean are characterized by the wide-spread deposition of organic-carbon-rich sediments ("black shales“), with a maximum occurrence during Aptian/Albian and Cenomanian/Turonian times. In order to explain the origin of these black shales, changes in the amou...
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ftdatacite:10.1594/pangaea.667191 2024-09-15T18:26:23+00:00 Sedimentological, organic petrographic and organic chemical characteristics of Albian and Cenomanian/Turonian black shales from the North Altlantic (Tab. 3, 4) ... Stein, Ruediger Rullkötter, Jürgen Welte, Dietrich Hugo 1989 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.667191 https://doi.pangaea.de/10.1594/PANGAEA.667191 en eng PANGAEA https://dx.doi.org/10.1007/bf01829328 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Event label Latitude of event Longitude of event Elevation of event DEPTH, sediment/rock Sample code/label Epoch Lithology/composition/facies Carbon, organic, total Hydrogen index, mass HC, per unit mass total organic carbon Maceral Nonaromatic hydrocarbon fraction Comment Drilling/drill rig DSDP/ODP/IODP sample designation Element analyser CHN, LECO Leg41 Leg76 Leg79 Leg93 Glomar Challenger Deep Sea Drilling Project DSDP dataset Supplementary Dataset Dataset 1989 ftdatacite https://doi.org/10.1594/pangaea.66719110.1007/bf01829328 2024-08-01T10:57:37Z Large parts of the Cretaceous Atlantic Ocean are characterized by the wide-spread deposition of organic-carbon-rich sediments ("black shales“), with a maximum occurrence during Aptian/Albian and Cenomanian/Turonian times. In order to explain the origin of these black shales, changes in the amount and type of organic matter in relation to changes in paleogeography, paleoceanic circulation, and paleoclimate have been investigated in detail. The study is mainly based on calculation of accumulation rates of marine and terrigenous organic carbon, organic carbon/sedimentation rate relationships, and estimates of paleoproductivity. Because both the amount and type of organic matter in the black shales change markedly with location and age, different mechanisms must have caused the accumulation of these organic-carbon-rich sediments: (1) Terrigenous organic matter supply was the dominant factor for black shale formation during Hauterivian and Albian times in the Northwest Atlantic.(2) Increased oceanic productivity ... : Supplement to: Stein, Ruediger; Rullkötter, Jürgen; Welte, Dietrich Hugo (1989): Changes in paleoenvironments in the Atlantic Ocean during Cretaceous times: results from black shales studies. Geologische Rundschau, 78(3), 883-901 ... Dataset Northwest Atlantic DataCite |
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Open Polar |
collection |
DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
Event label Latitude of event Longitude of event Elevation of event DEPTH, sediment/rock Sample code/label Epoch Lithology/composition/facies Carbon, organic, total Hydrogen index, mass HC, per unit mass total organic carbon Maceral Nonaromatic hydrocarbon fraction Comment Drilling/drill rig DSDP/ODP/IODP sample designation Element analyser CHN, LECO Leg41 Leg76 Leg79 Leg93 Glomar Challenger Deep Sea Drilling Project DSDP |
spellingShingle |
Event label Latitude of event Longitude of event Elevation of event DEPTH, sediment/rock Sample code/label Epoch Lithology/composition/facies Carbon, organic, total Hydrogen index, mass HC, per unit mass total organic carbon Maceral Nonaromatic hydrocarbon fraction Comment Drilling/drill rig DSDP/ODP/IODP sample designation Element analyser CHN, LECO Leg41 Leg76 Leg79 Leg93 Glomar Challenger Deep Sea Drilling Project DSDP Stein, Ruediger Rullkötter, Jürgen Welte, Dietrich Hugo Sedimentological, organic petrographic and organic chemical characteristics of Albian and Cenomanian/Turonian black shales from the North Altlantic (Tab. 3, 4) ... |
topic_facet |
Event label Latitude of event Longitude of event Elevation of event DEPTH, sediment/rock Sample code/label Epoch Lithology/composition/facies Carbon, organic, total Hydrogen index, mass HC, per unit mass total organic carbon Maceral Nonaromatic hydrocarbon fraction Comment Drilling/drill rig DSDP/ODP/IODP sample designation Element analyser CHN, LECO Leg41 Leg76 Leg79 Leg93 Glomar Challenger Deep Sea Drilling Project DSDP |
description |
Large parts of the Cretaceous Atlantic Ocean are characterized by the wide-spread deposition of organic-carbon-rich sediments ("black shales“), with a maximum occurrence during Aptian/Albian and Cenomanian/Turonian times. In order to explain the origin of these black shales, changes in the amount and type of organic matter in relation to changes in paleogeography, paleoceanic circulation, and paleoclimate have been investigated in detail. The study is mainly based on calculation of accumulation rates of marine and terrigenous organic carbon, organic carbon/sedimentation rate relationships, and estimates of paleoproductivity. Because both the amount and type of organic matter in the black shales change markedly with location and age, different mechanisms must have caused the accumulation of these organic-carbon-rich sediments: (1) Terrigenous organic matter supply was the dominant factor for black shale formation during Hauterivian and Albian times in the Northwest Atlantic.(2) Increased oceanic productivity ... : Supplement to: Stein, Ruediger; Rullkötter, Jürgen; Welte, Dietrich Hugo (1989): Changes in paleoenvironments in the Atlantic Ocean during Cretaceous times: results from black shales studies. Geologische Rundschau, 78(3), 883-901 ... |
format |
Dataset |
author |
Stein, Ruediger Rullkötter, Jürgen Welte, Dietrich Hugo |
author_facet |
Stein, Ruediger Rullkötter, Jürgen Welte, Dietrich Hugo |
author_sort |
Stein, Ruediger |
title |
Sedimentological, organic petrographic and organic chemical characteristics of Albian and Cenomanian/Turonian black shales from the North Altlantic (Tab. 3, 4) ... |
title_short |
Sedimentological, organic petrographic and organic chemical characteristics of Albian and Cenomanian/Turonian black shales from the North Altlantic (Tab. 3, 4) ... |
title_full |
Sedimentological, organic petrographic and organic chemical characteristics of Albian and Cenomanian/Turonian black shales from the North Altlantic (Tab. 3, 4) ... |
title_fullStr |
Sedimentological, organic petrographic and organic chemical characteristics of Albian and Cenomanian/Turonian black shales from the North Altlantic (Tab. 3, 4) ... |
title_full_unstemmed |
Sedimentological, organic petrographic and organic chemical characteristics of Albian and Cenomanian/Turonian black shales from the North Altlantic (Tab. 3, 4) ... |
title_sort |
sedimentological, organic petrographic and organic chemical characteristics of albian and cenomanian/turonian black shales from the north altlantic (tab. 3, 4) ... |
publisher |
PANGAEA |
publishDate |
1989 |
url |
https://dx.doi.org/10.1594/pangaea.667191 https://doi.pangaea.de/10.1594/PANGAEA.667191 |
genre |
Northwest Atlantic |
genre_facet |
Northwest Atlantic |
op_relation |
https://dx.doi.org/10.1007/bf01829328 |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_doi |
https://doi.org/10.1594/pangaea.66719110.1007/bf01829328 |
_version_ |
1810466864334110720 |