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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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 |
_version_ |
1766131864597168128 |