(Table 2) Organic residue at DSDP Hole 76-534A ...
The kind, sedimentation rate, and diagenesis of organic particles delivered to the North Atlantic seafloor during the Middle Jurassic-Early Cretaceous were responsible for the presence of carbonaceous sediments in Hole 534A. Organic-rich black clays formed from the rapid supply of organic matter; th...
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ftdatacite:10.1594/pangaea.809985 2024-09-15T18:22:32+00:00 (Table 2) Organic residue at DSDP Hole 76-534A ... Habib, Daniel 1983 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.809985 https://doi.pangaea.de/10.1594/PANGAEA.809985 en eng PANGAEA https://dx.doi.org/10.2973/dsdp.proc.76.139.1983 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Sample code/label Organic matter - Comment Drilling/drill rig DSDP/ODP/IODP sample designation Leg76 Glomar Challenger Deep Sea Drilling Project DSDP dataset Supplementary Dataset Dataset 1983 ftdatacite https://doi.org/10.1594/pangaea.80998510.2973/dsdp.proc.76.139.1983 2024-08-01T10:51:52Z The kind, sedimentation rate, and diagenesis of organic particles delivered to the North Atlantic seafloor during the Middle Jurassic-Early Cretaceous were responsible for the presence of carbonaceous sediments in Hole 534A. Organic-rich black clays formed from the rapid supply of organic matter; this organic matter was composed of either abundant, well-preserved, and poorly sorted particles of land plants deposited in clays and silty clays within terrigenous turbiditic sequences (tracheal facies) or abundant amorphous debris (xenomorphic facies) generated through the digestive tracts of marine zooplankton and sedimented as fecal pellets. Evidence for the fecal-pellet origin of xenomorphic debris is illustrated. Black clays were also produced in sediments containing less organic matter as a result of the black color of carbonized particles composing all or most of the residues (micrinitic facies). Slowly sedimented hematitic Aptian clays contain very little carbonized, organic debris that survived diagenetic ... : Supplement to: Habib, Daniel (1983): Sedimentation-rate-dependent distribution of organic matter in the North Atlantic Jurassic-Cretaceous. In: Sheridan, RE; Gradstein, FM; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 76, 781-794 ... Dataset North Atlantic DataCite |
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English |
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Sample code/label Organic matter - Comment Drilling/drill rig DSDP/ODP/IODP sample designation Leg76 Glomar Challenger Deep Sea Drilling Project DSDP |
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Sample code/label Organic matter - Comment Drilling/drill rig DSDP/ODP/IODP sample designation Leg76 Glomar Challenger Deep Sea Drilling Project DSDP Habib, Daniel (Table 2) Organic residue at DSDP Hole 76-534A ... |
topic_facet |
Sample code/label Organic matter - Comment Drilling/drill rig DSDP/ODP/IODP sample designation Leg76 Glomar Challenger Deep Sea Drilling Project DSDP |
description |
The kind, sedimentation rate, and diagenesis of organic particles delivered to the North Atlantic seafloor during the Middle Jurassic-Early Cretaceous were responsible for the presence of carbonaceous sediments in Hole 534A. Organic-rich black clays formed from the rapid supply of organic matter; this organic matter was composed of either abundant, well-preserved, and poorly sorted particles of land plants deposited in clays and silty clays within terrigenous turbiditic sequences (tracheal facies) or abundant amorphous debris (xenomorphic facies) generated through the digestive tracts of marine zooplankton and sedimented as fecal pellets. Evidence for the fecal-pellet origin of xenomorphic debris is illustrated. Black clays were also produced in sediments containing less organic matter as a result of the black color of carbonized particles composing all or most of the residues (micrinitic facies). Slowly sedimented hematitic Aptian clays contain very little carbonized, organic debris that survived diagenetic ... : Supplement to: Habib, Daniel (1983): Sedimentation-rate-dependent distribution of organic matter in the North Atlantic Jurassic-Cretaceous. In: Sheridan, RE; Gradstein, FM; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 76, 781-794 ... |
format |
Dataset |
author |
Habib, Daniel |
author_facet |
Habib, Daniel |
author_sort |
Habib, Daniel |
title |
(Table 2) Organic residue at DSDP Hole 76-534A ... |
title_short |
(Table 2) Organic residue at DSDP Hole 76-534A ... |
title_full |
(Table 2) Organic residue at DSDP Hole 76-534A ... |
title_fullStr |
(Table 2) Organic residue at DSDP Hole 76-534A ... |
title_full_unstemmed |
(Table 2) Organic residue at DSDP Hole 76-534A ... |
title_sort |
(table 2) organic residue at dsdp hole 76-534a ... |
publisher |
PANGAEA |
publishDate |
1983 |
url |
https://dx.doi.org/10.1594/pangaea.809985 https://doi.pangaea.de/10.1594/PANGAEA.809985 |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_relation |
https://dx.doi.org/10.2973/dsdp.proc.76.139.1983 |
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.80998510.2973/dsdp.proc.76.139.1983 |
_version_ |
1810462395783446528 |