Carbon chemistry of ODP Leg 105 sites ...
The quantity and quality of organic carbon of Eocene to Holocene sediments from ODP Sites 645, 646, and 647 were investigated to reconstruct depositional environments. Results were based on organic-carbon and nitrogen determinations, Rock-Eval pyrolysis, and kerogen microscopy.The sediments at Site...
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ftdatacite:10.1594/pangaea.744883 2024-09-30T14:32:38+00:00 Carbon chemistry of ODP Leg 105 sites ... Stein, Ruediger Littke, Ralf Stax, Rainer Welte, Dietrich Hugo 1989 application/zip https://dx.doi.org/10.1594/pangaea.744883 https://doi.pangaea.de/10.1594/PANGAEA.744883 en eng PANGAEA https://dx.doi.org/10.2973/odp.proc.sr.105.154.1989 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Drilling/drill rig Composite Core Leg105 Joides Resolution Ocean Drilling Program ODP Collection Supplementary Publication Series of Datasets article 1989 ftdatacite https://doi.org/10.1594/pangaea.74488310.2973/odp.proc.sr.105.154.1989 2024-09-02T08:36:09Z The quantity and quality of organic carbon of Eocene to Holocene sediments from ODP Sites 645, 646, and 647 were investigated to reconstruct depositional environments. Results were based on organic-carbon and nitrogen determinations, Rock-Eval pyrolysis, and kerogen microscopy.The sediments at Site 645 in Baffin Bay are characterized by relatively high organic-carbon values, most of which range from 0.5% to almost 3%, with maximum values in the middle Miocene. Distinct maxima of organic-carbon accumulation rates occur between 18 and 12.5 Ma and between 3.4 and 0 Ma. At Sites 646 and 647 in the Labrador Sea, organic-carbon contents vary between 0.1% and 0.75%. Cyclic 'Milankovitch-type' changes in organic-carbon deposition imply climate-controlled mechanisms that cause these fluctuations.The composition of organic matter at Site 645 is dominated by terrigenous components throughout the entire sediment sequence. An increased content of marine organic carbon was recorded only in the late-middle Miocene. At ... : Supplement to: Stein, Ruediger; Littke, Ralf; Stax, Rainer; Welte, Dietrich Hugo (1989): Quantity, provenance, and maturity of organic matter at ODP Sites 645, 646, and 647: implications for reconstruction of paleoenvironments in Baffin Bay and Labrador Sea during Tertiary and Quaternary time. In: Srivastava, SP; Arthur, M; Clement, B; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 105, 185-208 ... Article in Journal/Newspaper Baffin Bay Baffin Bay Baffin Labrador Sea DataCite Baffin Bay |
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English |
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Drilling/drill rig Composite Core Leg105 Joides Resolution Ocean Drilling Program ODP |
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Drilling/drill rig Composite Core Leg105 Joides Resolution Ocean Drilling Program ODP Stein, Ruediger Littke, Ralf Stax, Rainer Welte, Dietrich Hugo Carbon chemistry of ODP Leg 105 sites ... |
topic_facet |
Drilling/drill rig Composite Core Leg105 Joides Resolution Ocean Drilling Program ODP |
description |
The quantity and quality of organic carbon of Eocene to Holocene sediments from ODP Sites 645, 646, and 647 were investigated to reconstruct depositional environments. Results were based on organic-carbon and nitrogen determinations, Rock-Eval pyrolysis, and kerogen microscopy.The sediments at Site 645 in Baffin Bay are characterized by relatively high organic-carbon values, most of which range from 0.5% to almost 3%, with maximum values in the middle Miocene. Distinct maxima of organic-carbon accumulation rates occur between 18 and 12.5 Ma and between 3.4 and 0 Ma. At Sites 646 and 647 in the Labrador Sea, organic-carbon contents vary between 0.1% and 0.75%. Cyclic 'Milankovitch-type' changes in organic-carbon deposition imply climate-controlled mechanisms that cause these fluctuations.The composition of organic matter at Site 645 is dominated by terrigenous components throughout the entire sediment sequence. An increased content of marine organic carbon was recorded only in the late-middle Miocene. At ... : Supplement to: Stein, Ruediger; Littke, Ralf; Stax, Rainer; Welte, Dietrich Hugo (1989): Quantity, provenance, and maturity of organic matter at ODP Sites 645, 646, and 647: implications for reconstruction of paleoenvironments in Baffin Bay and Labrador Sea during Tertiary and Quaternary time. In: Srivastava, SP; Arthur, M; Clement, B; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 105, 185-208 ... |
format |
Article in Journal/Newspaper |
author |
Stein, Ruediger Littke, Ralf Stax, Rainer Welte, Dietrich Hugo |
author_facet |
Stein, Ruediger Littke, Ralf Stax, Rainer Welte, Dietrich Hugo |
author_sort |
Stein, Ruediger |
title |
Carbon chemistry of ODP Leg 105 sites ... |
title_short |
Carbon chemistry of ODP Leg 105 sites ... |
title_full |
Carbon chemistry of ODP Leg 105 sites ... |
title_fullStr |
Carbon chemistry of ODP Leg 105 sites ... |
title_full_unstemmed |
Carbon chemistry of ODP Leg 105 sites ... |
title_sort |
carbon chemistry of odp leg 105 sites ... |
publisher |
PANGAEA |
publishDate |
1989 |
url |
https://dx.doi.org/10.1594/pangaea.744883 https://doi.pangaea.de/10.1594/PANGAEA.744883 |
geographic |
Baffin Bay |
geographic_facet |
Baffin Bay |
genre |
Baffin Bay Baffin Bay Baffin Labrador Sea |
genre_facet |
Baffin Bay Baffin Bay Baffin Labrador Sea |
op_relation |
https://dx.doi.org/10.2973/odp.proc.sr.105.154.1989 |
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.74488310.2973/odp.proc.sr.105.154.1989 |
_version_ |
1811636741971378176 |