Diffusive and Total Oxygen-Uptake of Deep-Sea Sediments in the Eastern South-Atlantic Ocean - In-Situ and Laboratory Measurements

Total O-2 uptake rates were measured by the benthic flux chamber lander ELINOR, and O-2 microprofiles were measured by the profiling lander PROFILUR in the eastern South Atlantic. Diffusive O-2 fluxes through the diffusive boundary layer and the depth distribution of O-2 consumption rates within the...

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Main Authors: GLUD, RN, GUNDERSEN, JK, JØRGENSEN, BB, REVSBECH, NP, SCHULZ, HD
Format: Article in Journal/Newspaper
Language:English
Published: 1994
Subjects:
Online Access:https://pure.au.dk/portal/da/publications/diffusive-and-total-oxygenuptake-of-deepsea-sediments-in-the-eastern-southatlantic-ocean--insitu-and-laboratory-measurements(a85aac2e-ffc8-49da-8c05-df90cb1b9f4a).html
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spelling ftuniaarhuspubl:oai:pure.atira.dk:publications/a85aac2e-ffc8-49da-8c05-df90cb1b9f4a 2023-05-15T18:21:12+02:00 Diffusive and Total Oxygen-Uptake of Deep-Sea Sediments in the Eastern South-Atlantic Ocean - In-Situ and Laboratory Measurements GLUD, RN GUNDERSEN, JK JØRGENSEN, BB REVSBECH, NP SCHULZ, HD 1994-11-01 https://pure.au.dk/portal/da/publications/diffusive-and-total-oxygenuptake-of-deepsea-sediments-in-the-eastern-southatlantic-ocean--insitu-and-laboratory-measurements(a85aac2e-ffc8-49da-8c05-df90cb1b9f4a).html eng eng info:eu-repo/semantics/restrictedAccess GLUD , RN , GUNDERSEN , JK , JØRGENSEN , BB , REVSBECH , NP & SCHULZ , HD 1994 , ' Diffusive and Total Oxygen-Uptake of Deep-Sea Sediments in the Eastern South-Atlantic Ocean - In-Situ and Laboratory Measurements ' , Deep-Sea Research Part I: Oceanographic Research Papers , vol. 41 , no. 11-12 , pp. 1767-1788 . article 1994 ftuniaarhuspubl 2023-04-05T22:56:26Z Total O-2 uptake rates were measured by the benthic flux chamber lander ELINOR, and O-2 microprofiles were measured by the profiling lander PROFILUR in the eastern South Atlantic. Diffusive O-2 fluxes through the diffusive boundary layer and the depth distribution of O-2 consumption rates within the sediment were calculated from the obtained microprofiles. The depth integrated O-2 consumption rate agreed closely with the diffusive O-2 uptake at all stations. Total O-2 uptake was 1.2-4.2 times the diffusive O-2 uptake, and the difference correlated with the abundance of macrofauna in the sediment. Diffusive O-2 uptake and O-2-penetration depths correlated with the organic content of the sediments and exhibited an inverse correlation with water depth. Total and diffusive rates of the in situ O-2 uptake were higher than previously published data for shelf and abyssal sediments in the Atlantic, but were comparable to rates from upwelling areas in the eastern Pacific. Laboratory measurements on recovered sediment cores showed lower O-2 penetration depths and higher diffusive uptake rates than in situ measurements. The differences increased with increasing water depth. We primarily ascribe this compression of O-2 profiles to a transiently increased temperature during recovery and enhanced microbial activity in decompressed sediment cores. Total O-2 uptake rates measured in the laboratory on macrofauna-rich stations were, in contrast, lower than those measured in situ because of underrepresentation and disturbance of the macrofauna. Article in Journal/Newspaper South Atlantic Ocean Aarhus University: Research Pacific
institution Open Polar
collection Aarhus University: Research
op_collection_id ftuniaarhuspubl
language English
description Total O-2 uptake rates were measured by the benthic flux chamber lander ELINOR, and O-2 microprofiles were measured by the profiling lander PROFILUR in the eastern South Atlantic. Diffusive O-2 fluxes through the diffusive boundary layer and the depth distribution of O-2 consumption rates within the sediment were calculated from the obtained microprofiles. The depth integrated O-2 consumption rate agreed closely with the diffusive O-2 uptake at all stations. Total O-2 uptake was 1.2-4.2 times the diffusive O-2 uptake, and the difference correlated with the abundance of macrofauna in the sediment. Diffusive O-2 uptake and O-2-penetration depths correlated with the organic content of the sediments and exhibited an inverse correlation with water depth. Total and diffusive rates of the in situ O-2 uptake were higher than previously published data for shelf and abyssal sediments in the Atlantic, but were comparable to rates from upwelling areas in the eastern Pacific. Laboratory measurements on recovered sediment cores showed lower O-2 penetration depths and higher diffusive uptake rates than in situ measurements. The differences increased with increasing water depth. We primarily ascribe this compression of O-2 profiles to a transiently increased temperature during recovery and enhanced microbial activity in decompressed sediment cores. Total O-2 uptake rates measured in the laboratory on macrofauna-rich stations were, in contrast, lower than those measured in situ because of underrepresentation and disturbance of the macrofauna.
format Article in Journal/Newspaper
author GLUD, RN
GUNDERSEN, JK
JØRGENSEN, BB
REVSBECH, NP
SCHULZ, HD
spellingShingle GLUD, RN
GUNDERSEN, JK
JØRGENSEN, BB
REVSBECH, NP
SCHULZ, HD
Diffusive and Total Oxygen-Uptake of Deep-Sea Sediments in the Eastern South-Atlantic Ocean - In-Situ and Laboratory Measurements
author_facet GLUD, RN
GUNDERSEN, JK
JØRGENSEN, BB
REVSBECH, NP
SCHULZ, HD
author_sort GLUD, RN
title Diffusive and Total Oxygen-Uptake of Deep-Sea Sediments in the Eastern South-Atlantic Ocean - In-Situ and Laboratory Measurements
title_short Diffusive and Total Oxygen-Uptake of Deep-Sea Sediments in the Eastern South-Atlantic Ocean - In-Situ and Laboratory Measurements
title_full Diffusive and Total Oxygen-Uptake of Deep-Sea Sediments in the Eastern South-Atlantic Ocean - In-Situ and Laboratory Measurements
title_fullStr Diffusive and Total Oxygen-Uptake of Deep-Sea Sediments in the Eastern South-Atlantic Ocean - In-Situ and Laboratory Measurements
title_full_unstemmed Diffusive and Total Oxygen-Uptake of Deep-Sea Sediments in the Eastern South-Atlantic Ocean - In-Situ and Laboratory Measurements
title_sort diffusive and total oxygen-uptake of deep-sea sediments in the eastern south-atlantic ocean - in-situ and laboratory measurements
publishDate 1994
url https://pure.au.dk/portal/da/publications/diffusive-and-total-oxygenuptake-of-deepsea-sediments-in-the-eastern-southatlantic-ocean--insitu-and-laboratory-measurements(a85aac2e-ffc8-49da-8c05-df90cb1b9f4a).html
geographic Pacific
geographic_facet Pacific
genre South Atlantic Ocean
genre_facet South Atlantic Ocean
op_source GLUD , RN , GUNDERSEN , JK , JØRGENSEN , BB , REVSBECH , NP & SCHULZ , HD 1994 , ' Diffusive and Total Oxygen-Uptake of Deep-Sea Sediments in the Eastern South-Atlantic Ocean - In-Situ and Laboratory Measurements ' , Deep-Sea Research Part I: Oceanographic Research Papers , vol. 41 , no. 11-12 , pp. 1767-1788 .
op_rights info:eu-repo/semantics/restrictedAccess
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