Geochemical investigation of ODP Leg 113 sites
Dissolved organic carbon (DOC) was determined in pore water extracted from pelagic and hemipelagic sediments recovered during Leg 113. DOC concentration varied between 1.82 and 13.6 mg C/L which is one to two orders of magnitude less than previously reported for hemipelagic sediments. It is argued t...
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.726399 2024-09-15T18:36:26+00:00 Geochemical investigation of ODP Leg 113 sites Egeberg, Per Kristian Abdullah, Mohamed I MEDIAN LATITUDE: -64.772429 * MEDIAN LONGITUDE: -24.341806 * SOUTH-BOUND LATITUDE: -70.832000 * WEST-BOUND LONGITUDE: -43.451600 * NORTH-BOUND LATITUDE: -61.810000 * EAST-BOUND LONGITUDE: 3.099900 * DATE/TIME START: 1987-01-16T08:00:00 * DATE/TIME END: 1987-03-07T13:30:00 1990 application/zip, 7 datasets https://doi.pangaea.de/10.1594/PANGAEA.726399 https://doi.org/10.1594/PANGAEA.726399 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.726399 https://doi.org/10.1594/PANGAEA.726399 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess Supplement to: Egeberg, Per Kristian; Abdullah, Mohamed I (1990): The diagenetic factors controlling the dissolved organic carbon (DOC) in pore water from deep sea sediments (ODP Leg 113, Weddell Sea). In: Barker, PF; Kennett, JP; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 113, 169-177, https://doi.org/10.2973/odp.proc.sr.113.167.1990 113-689B 113-690B 113-690C 113-693 113-694B 113-694C 113-695A 113-696A 113-696B 113-697A 113-697B COMPCORE Composite Core DRILL Drilling/drill rig Joides Resolution Leg113 Ocean Drilling Program ODP South Atlantic Ocean Weddell Sea dataset publication series 1990 ftpangaea https://doi.org/10.1594/PANGAEA.72639910.2973/odp.proc.sr.113.167.1990 2024-07-24T02:31:20Z Dissolved organic carbon (DOC) was determined in pore water extracted from pelagic and hemipelagic sediments recovered during Leg 113. DOC concentration varied between 1.82 and 13.6 mg C/L which is one to two orders of magnitude less than previously reported for hemipelagic sediments. It is argued that this difference is related to differences in the intensity of degradation of organic matter. As a first approximation it is found that in reducing sediments, the level of DOC is proportional to the intensity of sulfate reduction. It is suggested that DOC is formed by different mechanisms in oxic and reducing environments. Other/Unknown Material South Atlantic Ocean Weddell Sea PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(-43.451600,3.099900,-61.810000,-70.832000) |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
113-689B 113-690B 113-690C 113-693 113-694B 113-694C 113-695A 113-696A 113-696B 113-697A 113-697B COMPCORE Composite Core DRILL Drilling/drill rig Joides Resolution Leg113 Ocean Drilling Program ODP South Atlantic Ocean Weddell Sea |
spellingShingle |
113-689B 113-690B 113-690C 113-693 113-694B 113-694C 113-695A 113-696A 113-696B 113-697A 113-697B COMPCORE Composite Core DRILL Drilling/drill rig Joides Resolution Leg113 Ocean Drilling Program ODP South Atlantic Ocean Weddell Sea Egeberg, Per Kristian Abdullah, Mohamed I Geochemical investigation of ODP Leg 113 sites |
topic_facet |
113-689B 113-690B 113-690C 113-693 113-694B 113-694C 113-695A 113-696A 113-696B 113-697A 113-697B COMPCORE Composite Core DRILL Drilling/drill rig Joides Resolution Leg113 Ocean Drilling Program ODP South Atlantic Ocean Weddell Sea |
description |
Dissolved organic carbon (DOC) was determined in pore water extracted from pelagic and hemipelagic sediments recovered during Leg 113. DOC concentration varied between 1.82 and 13.6 mg C/L which is one to two orders of magnitude less than previously reported for hemipelagic sediments. It is argued that this difference is related to differences in the intensity of degradation of organic matter. As a first approximation it is found that in reducing sediments, the level of DOC is proportional to the intensity of sulfate reduction. It is suggested that DOC is formed by different mechanisms in oxic and reducing environments. |
format |
Other/Unknown Material |
author |
Egeberg, Per Kristian Abdullah, Mohamed I |
author_facet |
Egeberg, Per Kristian Abdullah, Mohamed I |
author_sort |
Egeberg, Per Kristian |
title |
Geochemical investigation of ODP Leg 113 sites |
title_short |
Geochemical investigation of ODP Leg 113 sites |
title_full |
Geochemical investigation of ODP Leg 113 sites |
title_fullStr |
Geochemical investigation of ODP Leg 113 sites |
title_full_unstemmed |
Geochemical investigation of ODP Leg 113 sites |
title_sort |
geochemical investigation of odp leg 113 sites |
publisher |
PANGAEA |
publishDate |
1990 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.726399 https://doi.org/10.1594/PANGAEA.726399 |
op_coverage |
MEDIAN LATITUDE: -64.772429 * MEDIAN LONGITUDE: -24.341806 * SOUTH-BOUND LATITUDE: -70.832000 * WEST-BOUND LONGITUDE: -43.451600 * NORTH-BOUND LATITUDE: -61.810000 * EAST-BOUND LONGITUDE: 3.099900 * DATE/TIME START: 1987-01-16T08:00:00 * DATE/TIME END: 1987-03-07T13:30:00 |
long_lat |
ENVELOPE(-43.451600,3.099900,-61.810000,-70.832000) |
genre |
South Atlantic Ocean Weddell Sea |
genre_facet |
South Atlantic Ocean Weddell Sea |
op_source |
Supplement to: Egeberg, Per Kristian; Abdullah, Mohamed I (1990): The diagenetic factors controlling the dissolved organic carbon (DOC) in pore water from deep sea sediments (ODP Leg 113, Weddell Sea). In: Barker, PF; Kennett, JP; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 113, 169-177, https://doi.org/10.2973/odp.proc.sr.113.167.1990 |
op_relation |
https://doi.pangaea.de/10.1594/PANGAEA.726399 https://doi.org/10.1594/PANGAEA.726399 |
op_rights |
CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1594/PANGAEA.72639910.2973/odp.proc.sr.113.167.1990 |
_version_ |
1810480098811314176 |