Palynofacies investigation of Callovian sediments of DSDP Hole 79-534A

During the extension of Deep Sea Drilling Project (DSDP) Leg 76 a new and previously unpenetrated lithological unit composed mainly of claystones was cored above basalt basement at Site 534 in the Blake-Bahama Basin. The Callovian part of the new unit contains interbedded 'black shales' wh...

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Main Author: Tyson, Richard V
Format: Dataset
Language:English
Published: PANGAEA 1984
Subjects:
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.746749
https://doi.org/10.1594/PANGAEA.746749
id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.746749
record_format openpolar
spelling ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.746749 2023-05-15T17:33:22+02:00 Palynofacies investigation of Callovian sediments of DSDP Hole 79-534A Tyson, Richard V LATITUDE: 28.343300 * LONGITUDE: -75.381700 * DATE/TIME START: 1980-10-21T00:00:00 * DATE/TIME END: 1980-10-21T00:00:00 1984-10-22 application/zip, 3 datasets https://doi.pangaea.de/10.1594/PANGAEA.746749 https://doi.org/10.1594/PANGAEA.746749 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.746749 https://doi.org/10.1594/PANGAEA.746749 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY Supplement to: Tyson, Richard V (1984): Palynofacies investigation of Callovian (Middle Jurassic) sediments from DSDP Site 534, Blake-Bahama Basin, Western Central Atlantic. Marine and Petroleum Geology, 1(1), 3-13, https://doi.org/10.1016/0264-8172(84)90116-8 76-534A Deep Sea Drilling Project DRILL Drilling/drill rig DSDP Glomar Challenger Leg76 North Atlantic/BASIN Dataset 1984 ftpangaea https://doi.org/10.1594/PANGAEA.746749 https://doi.org/10.1016/0264-8172(84)90116-8 2023-01-20T07:31:57Z During the extension of Deep Sea Drilling Project (DSDP) Leg 76 a new and previously unpenetrated lithological unit composed mainly of claystones was cored above basalt basement at Site 534 in the Blake-Bahama Basin. The Callovian part of the new unit contains interbedded 'black shales' which were hitherto unexpected in this part of the section. This Paper presents a brief palynological examination of lithofacies-kerogen relationships in these sediments and shows that their organic content is almost entirely a function of the re-deposition of terrestial and marine organic matter versus the ambient redox conditions of the depositional environment. Allochthonous organic matter inputs are highest in the interbedded turbidites and decline progressively toward the pelagic black shales in which marine organic matter is comparatively well preserved. The significance of various kerogen and palynomorph indices are discussed. The study emphasizes the absolute necessity for sedimentologically-aware sampling in all palynological and geochemical work on lithologically heterogeneous sequences. Dataset North Atlantic PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(-75.381700,-75.381700,28.343300,28.343300)
institution Open Polar
collection PANGAEA - Data Publisher for Earth & Environmental Science
op_collection_id ftpangaea
language English
topic 76-534A
Deep Sea Drilling Project
DRILL
Drilling/drill rig
DSDP
Glomar Challenger
Leg76
North Atlantic/BASIN
spellingShingle 76-534A
Deep Sea Drilling Project
DRILL
Drilling/drill rig
DSDP
Glomar Challenger
Leg76
North Atlantic/BASIN
Tyson, Richard V
Palynofacies investigation of Callovian sediments of DSDP Hole 79-534A
topic_facet 76-534A
Deep Sea Drilling Project
DRILL
Drilling/drill rig
DSDP
Glomar Challenger
Leg76
North Atlantic/BASIN
description During the extension of Deep Sea Drilling Project (DSDP) Leg 76 a new and previously unpenetrated lithological unit composed mainly of claystones was cored above basalt basement at Site 534 in the Blake-Bahama Basin. The Callovian part of the new unit contains interbedded 'black shales' which were hitherto unexpected in this part of the section. This Paper presents a brief palynological examination of lithofacies-kerogen relationships in these sediments and shows that their organic content is almost entirely a function of the re-deposition of terrestial and marine organic matter versus the ambient redox conditions of the depositional environment. Allochthonous organic matter inputs are highest in the interbedded turbidites and decline progressively toward the pelagic black shales in which marine organic matter is comparatively well preserved. The significance of various kerogen and palynomorph indices are discussed. The study emphasizes the absolute necessity for sedimentologically-aware sampling in all palynological and geochemical work on lithologically heterogeneous sequences.
format Dataset
author Tyson, Richard V
author_facet Tyson, Richard V
author_sort Tyson, Richard V
title Palynofacies investigation of Callovian sediments of DSDP Hole 79-534A
title_short Palynofacies investigation of Callovian sediments of DSDP Hole 79-534A
title_full Palynofacies investigation of Callovian sediments of DSDP Hole 79-534A
title_fullStr Palynofacies investigation of Callovian sediments of DSDP Hole 79-534A
title_full_unstemmed Palynofacies investigation of Callovian sediments of DSDP Hole 79-534A
title_sort palynofacies investigation of callovian sediments of dsdp hole 79-534a
publisher PANGAEA
publishDate 1984
url https://doi.pangaea.de/10.1594/PANGAEA.746749
https://doi.org/10.1594/PANGAEA.746749
op_coverage LATITUDE: 28.343300 * LONGITUDE: -75.381700 * DATE/TIME START: 1980-10-21T00:00:00 * DATE/TIME END: 1980-10-21T00:00:00
long_lat ENVELOPE(-75.381700,-75.381700,28.343300,28.343300)
genre North Atlantic
genre_facet North Atlantic
op_source Supplement to: Tyson, Richard V (1984): Palynofacies investigation of Callovian (Middle Jurassic) sediments from DSDP Site 534, Blake-Bahama Basin, Western Central Atlantic. Marine and Petroleum Geology, 1(1), 3-13, https://doi.org/10.1016/0264-8172(84)90116-8
op_relation https://doi.pangaea.de/10.1594/PANGAEA.746749
https://doi.org/10.1594/PANGAEA.746749
op_rights CC-BY-3.0: Creative Commons Attribution 3.0 Unported
Access constraints: unrestricted
info:eu-repo/semantics/openAccess
op_rightsnorm CC-BY
op_doi https://doi.org/10.1594/PANGAEA.746749
https://doi.org/10.1016/0264-8172(84)90116-8
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