Chemistry of organic matter of glacial and Cretaceous sediments from the Prydz Bay ...
Organic matter in Miocene glacial sediments in Hole 739C on the Antarctic Shelf represents erosional recycled continental material. Various indications of maturity in bulk organic matter, kerogens, and extracts imply that an exposed section of mature organic carbon-rich material was present during t...
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ftdatacite:10.1594/pangaea.758521 2024-09-15T17:41:12+00:00 Chemistry of organic matter of glacial and Cretaceous sediments from the Prydz Bay ... McDonald, Thomas J Kennicutt, Mahlon C Rafalska, Janina K Fox, Richard G 1991 application/zip https://dx.doi.org/10.1594/pangaea.758521 https://doi.pangaea.de/10.1594/PANGAEA.758521 en eng PANGAEA https://dx.doi.org/10.2973/odp.proc.sr.119.176.1991 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Drilling/drill rig Leg119 Joides Resolution Ocean Drilling Program ODP article Collection Supplementary Publication Series of Datasets 1991 ftdatacite https://doi.org/10.1594/pangaea.75852110.2973/odp.proc.sr.119.176.1991 2024-08-01T10:51:52Z Organic matter in Miocene glacial sediments in Hole 739C on the Antarctic Shelf represents erosional recycled continental material. Various indications of maturity in bulk organic matter, kerogens, and extracts imply that an exposed section of mature organic carbon-rich material was present during the Miocene. Based on biomarker, n-alkane, and kerogen analysis, a massive diamictite of early Eocene/Oligocene age at Hole 739C contains immature organic matter. Visual and pyrolysis analyses of the kerogens suggest a predominance of terrestrial organic matter in all samples from Hole 739C. A reversal of thermal maturities, i.e., more-mature overlying less-mature sections, may be related to redeposition generated from glacial erosion.Siliciclastic fluviatile sediments of Lower Cretaceous age from Hole 741A were analyzed. The organic matter from this hole contains immature aliphatic and aromatic biomarkers as well as a suite of odd carbon number-dominated nalkanes. Visual examination and pyrolysis analysis of the ... : Supplement to: McDonald, Thomas J; Kennicutt, Mahlon C; Rafalska, Janina K; Fox, Richard G (1991): Source and maturity of organic matter in glacial and cretaceous sediments from Prydz Bay, Antarctica, Holes 739C and 741A. In: Barron, J; Larsen, B; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 119, 401-405 ... Article in Journal/Newspaper Antarc* Antarctic Antarctica Prydz Bay DataCite |
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ftdatacite |
language |
English |
topic |
Drilling/drill rig Leg119 Joides Resolution Ocean Drilling Program ODP |
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Drilling/drill rig Leg119 Joides Resolution Ocean Drilling Program ODP McDonald, Thomas J Kennicutt, Mahlon C Rafalska, Janina K Fox, Richard G Chemistry of organic matter of glacial and Cretaceous sediments from the Prydz Bay ... |
topic_facet |
Drilling/drill rig Leg119 Joides Resolution Ocean Drilling Program ODP |
description |
Organic matter in Miocene glacial sediments in Hole 739C on the Antarctic Shelf represents erosional recycled continental material. Various indications of maturity in bulk organic matter, kerogens, and extracts imply that an exposed section of mature organic carbon-rich material was present during the Miocene. Based on biomarker, n-alkane, and kerogen analysis, a massive diamictite of early Eocene/Oligocene age at Hole 739C contains immature organic matter. Visual and pyrolysis analyses of the kerogens suggest a predominance of terrestrial organic matter in all samples from Hole 739C. A reversal of thermal maturities, i.e., more-mature overlying less-mature sections, may be related to redeposition generated from glacial erosion.Siliciclastic fluviatile sediments of Lower Cretaceous age from Hole 741A were analyzed. The organic matter from this hole contains immature aliphatic and aromatic biomarkers as well as a suite of odd carbon number-dominated nalkanes. Visual examination and pyrolysis analysis of the ... : Supplement to: McDonald, Thomas J; Kennicutt, Mahlon C; Rafalska, Janina K; Fox, Richard G (1991): Source and maturity of organic matter in glacial and cretaceous sediments from Prydz Bay, Antarctica, Holes 739C and 741A. In: Barron, J; Larsen, B; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 119, 401-405 ... |
format |
Article in Journal/Newspaper |
author |
McDonald, Thomas J Kennicutt, Mahlon C Rafalska, Janina K Fox, Richard G |
author_facet |
McDonald, Thomas J Kennicutt, Mahlon C Rafalska, Janina K Fox, Richard G |
author_sort |
McDonald, Thomas J |
title |
Chemistry of organic matter of glacial and Cretaceous sediments from the Prydz Bay ... |
title_short |
Chemistry of organic matter of glacial and Cretaceous sediments from the Prydz Bay ... |
title_full |
Chemistry of organic matter of glacial and Cretaceous sediments from the Prydz Bay ... |
title_fullStr |
Chemistry of organic matter of glacial and Cretaceous sediments from the Prydz Bay ... |
title_full_unstemmed |
Chemistry of organic matter of glacial and Cretaceous sediments from the Prydz Bay ... |
title_sort |
chemistry of organic matter of glacial and cretaceous sediments from the prydz bay ... |
publisher |
PANGAEA |
publishDate |
1991 |
url |
https://dx.doi.org/10.1594/pangaea.758521 https://doi.pangaea.de/10.1594/PANGAEA.758521 |
genre |
Antarc* Antarctic Antarctica Prydz Bay |
genre_facet |
Antarc* Antarctic Antarctica Prydz Bay |
op_relation |
https://dx.doi.org/10.2973/odp.proc.sr.119.176.1991 |
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.75852110.2973/odp.proc.sr.119.176.1991 |
_version_ |
1810487347213500416 |