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...

Full description

Bibliographic Details
Main Authors: Stein, Ruediger, Littke, Ralf, Stax, Rainer, Welte, Dietrich Hugo
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 1989
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.744883
https://doi.pangaea.de/10.1594/PANGAEA.744883
id ftdatacite:10.1594/pangaea.744883
record_format openpolar
spelling 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
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Drilling/drill rig
Composite Core
Leg105
Joides Resolution
Ocean Drilling Program ODP
spellingShingle 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