Maceral distribution, stratigraphic position and vitrinite reflectance at DSDP Hole 81-555 ...

Twenty-four sediment samples from late Paleocene to early Eocene were studied for maceral content, vitrinite reflectance, and spectral fluorescence in order to determine some parameters of the origin and diagenetic history of their organic fraction. The sediments had been obtained at Site 555 of DSD...

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Main Authors: Lund, Jane, Riegel, Walter
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 1984
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.806668
https://doi.pangaea.de/10.1594/PANGAEA.806668
id ftdatacite:10.1594/pangaea.806668
record_format openpolar
spelling ftdatacite:10.1594/pangaea.806668 2024-09-15T18:23:35+00:00 Maceral distribution, stratigraphic position and vitrinite reflectance at DSDP Hole 81-555 ... Lund, Jane Riegel, Walter 1984 application/zip https://dx.doi.org/10.1594/pangaea.806668 https://doi.pangaea.de/10.1594/PANGAEA.806668 en eng PANGAEA https://dx.doi.org/10.2973/dsdp.proc.81.118.1984 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Drilling/drill rig Leg81 Glomar Challenger Deep Sea Drilling Project DSDP article Collection Supplementary Publication Series of Datasets 1984 ftdatacite https://doi.org/10.1594/pangaea.80666810.2973/dsdp.proc.81.118.1984 2024-08-01T10:51:31Z Twenty-four sediment samples from late Paleocene to early Eocene were studied for maceral content, vitrinite reflectance, and spectral fluorescence in order to determine some parameters of the origin and diagenetic history of their organic fraction. The sediments had been obtained at Site 555 of DSDP Leg 81 in the northeastern North Atlantic. The bulk of the microscopically visible fraction is made up of humic materials; inertinites follow as a distant second; and liptinites are exceedingly rare. No unequivocal evidence of marine organic matter was found. Humic materials are highly decomposed, showing signs of aerobic (frequency of sclerotinites) as well as anaerobic (abundance of and intimate association with framboidal pyrite) microbial degradation. Vitrinite reflectance values vary between 0.26 and 0.35 Ro and show a slight increase with depth. These values, indicative of a low-rank lignite stage of coalification, contrast somewhat with the sporinite fluorescence spectra, which show the configuration ... : Supplement to: Lund, Jane; Riegel, Walter (1984): Petrography of degraded plant fragments from Paleocene-Eocene sediments of Deep Sea Drilling Project Leg 81, Site 555, Rockall Plateau. In: Roberts, DG; Schnittker, D; et al. (eds.), Initial Reports of the Deep Sea Drilling Project, Washington (U.S. Govt. Printing Office), 81, 623-629 ... Article in Journal/Newspaper North Atlantic DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Drilling/drill rig
Leg81
Glomar Challenger
Deep Sea Drilling Project DSDP
spellingShingle Drilling/drill rig
Leg81
Glomar Challenger
Deep Sea Drilling Project DSDP
Lund, Jane
Riegel, Walter
Maceral distribution, stratigraphic position and vitrinite reflectance at DSDP Hole 81-555 ...
topic_facet Drilling/drill rig
Leg81
Glomar Challenger
Deep Sea Drilling Project DSDP
description Twenty-four sediment samples from late Paleocene to early Eocene were studied for maceral content, vitrinite reflectance, and spectral fluorescence in order to determine some parameters of the origin and diagenetic history of their organic fraction. The sediments had been obtained at Site 555 of DSDP Leg 81 in the northeastern North Atlantic. The bulk of the microscopically visible fraction is made up of humic materials; inertinites follow as a distant second; and liptinites are exceedingly rare. No unequivocal evidence of marine organic matter was found. Humic materials are highly decomposed, showing signs of aerobic (frequency of sclerotinites) as well as anaerobic (abundance of and intimate association with framboidal pyrite) microbial degradation. Vitrinite reflectance values vary between 0.26 and 0.35 Ro and show a slight increase with depth. These values, indicative of a low-rank lignite stage of coalification, contrast somewhat with the sporinite fluorescence spectra, which show the configuration ... : Supplement to: Lund, Jane; Riegel, Walter (1984): Petrography of degraded plant fragments from Paleocene-Eocene sediments of Deep Sea Drilling Project Leg 81, Site 555, Rockall Plateau. In: Roberts, DG; Schnittker, D; et al. (eds.), Initial Reports of the Deep Sea Drilling Project, Washington (U.S. Govt. Printing Office), 81, 623-629 ...
format Article in Journal/Newspaper
author Lund, Jane
Riegel, Walter
author_facet Lund, Jane
Riegel, Walter
author_sort Lund, Jane
title Maceral distribution, stratigraphic position and vitrinite reflectance at DSDP Hole 81-555 ...
title_short Maceral distribution, stratigraphic position and vitrinite reflectance at DSDP Hole 81-555 ...
title_full Maceral distribution, stratigraphic position and vitrinite reflectance at DSDP Hole 81-555 ...
title_fullStr Maceral distribution, stratigraphic position and vitrinite reflectance at DSDP Hole 81-555 ...
title_full_unstemmed Maceral distribution, stratigraphic position and vitrinite reflectance at DSDP Hole 81-555 ...
title_sort maceral distribution, stratigraphic position and vitrinite reflectance at dsdp hole 81-555 ...
publisher PANGAEA
publishDate 1984
url https://dx.doi.org/10.1594/pangaea.806668
https://doi.pangaea.de/10.1594/PANGAEA.806668
genre North Atlantic
genre_facet North Atlantic
op_relation https://dx.doi.org/10.2973/dsdp.proc.81.118.1984
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.80666810.2973/dsdp.proc.81.118.1984
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