Biogeochemical investigation of sediments at the Hakon Mosby Mud Volcano (Barents Sea) ...

We have investigated if in a cold seep methane or sulfide is used for chemosynthetic primary production and if significant amounts of the sulfide produced by anaerobic oxidation of methane are oxidized geochemically and hence are not available for chemosynthetic production. Geochemically controlled...

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Main Authors: Lichtschlag, Anna, Felden, Janine, Brüchert, Volker, Boetius, Antje, de Beer, Dirk
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2009
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.715022
https://doi.pangaea.de/10.1594/PANGAEA.715022
id ftdatacite:10.1594/pangaea.715022
record_format openpolar
spelling ftdatacite:10.1594/pangaea.715022 2024-09-15T17:57:51+00:00 Biogeochemical investigation of sediments at the Hakon Mosby Mud Volcano (Barents Sea) ... Lichtschlag, Anna Felden, Janine Brüchert, Volker Boetius, Antje de Beer, Dirk 2009 application/zip https://dx.doi.org/10.1594/pangaea.715022 https://doi.pangaea.de/10.1594/PANGAEA.715022 en eng PANGAEA https://dx.doi.org/10.4319/lo.2010.55.2.0931 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Push corer Microsensor profiler MultiCorer VICKING Pourquoi Pas ? 2005 Hotspot Ecosystem Research on the Margins of European Seas HERMES article Collection Supplementary Publication Series of Datasets 2009 ftdatacite https://doi.org/10.1594/pangaea.71502210.4319/lo.2010.55.2.0931 2024-08-01T10:58:30Z We have investigated if in a cold seep methane or sulfide is used for chemosynthetic primary production and if significant amounts of the sulfide produced by anaerobic oxidation of methane are oxidized geochemically and hence are not available for chemosynthetic production. Geochemically controlled redox reactions and biological turnover were compared in different habitats of the Håkon Mosby Mud Volcano. The center of the mud volcano is characterized by the highest fluid flow, and most primary production by the microbial community depends on oxidation of methane. The small amount of sulfide produced is oxidized geochemically with oxygen or is precipitated with dissolved iron. In the medium flow peripheral Beggiatoa habitat sulfide is largely oxidized biologically. The oxygen and nitrate supply is high enough that Beggiatoa can oxidize the sulfide completely, and chemical sulfide oxidation or precipitation is not important. An internally stored nitrate reservoir with average concentrations of 110 mmol L-1 ... : Supplement to: Lichtschlag, Anna; Felden, Janine; Brüchert, Volker; Boetius, Antje; de Beer, Dirk (2010): Geochemical processes and chemosynthetic primary production in different thiotrophic mats of the Hakon Mosby Mud Volcano (Barents Sea). Limnology and Oceanography, 55(2), 931-949 ... Article in Journal/Newspaper Barents Sea DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Push corer
Microsensor profiler
MultiCorer
VICKING
Pourquoi Pas ? 2005
Hotspot Ecosystem Research on the Margins of European Seas HERMES
spellingShingle Push corer
Microsensor profiler
MultiCorer
VICKING
Pourquoi Pas ? 2005
Hotspot Ecosystem Research on the Margins of European Seas HERMES
Lichtschlag, Anna
Felden, Janine
Brüchert, Volker
Boetius, Antje
de Beer, Dirk
Biogeochemical investigation of sediments at the Hakon Mosby Mud Volcano (Barents Sea) ...
topic_facet Push corer
Microsensor profiler
MultiCorer
VICKING
Pourquoi Pas ? 2005
Hotspot Ecosystem Research on the Margins of European Seas HERMES
description We have investigated if in a cold seep methane or sulfide is used for chemosynthetic primary production and if significant amounts of the sulfide produced by anaerobic oxidation of methane are oxidized geochemically and hence are not available for chemosynthetic production. Geochemically controlled redox reactions and biological turnover were compared in different habitats of the Håkon Mosby Mud Volcano. The center of the mud volcano is characterized by the highest fluid flow, and most primary production by the microbial community depends on oxidation of methane. The small amount of sulfide produced is oxidized geochemically with oxygen or is precipitated with dissolved iron. In the medium flow peripheral Beggiatoa habitat sulfide is largely oxidized biologically. The oxygen and nitrate supply is high enough that Beggiatoa can oxidize the sulfide completely, and chemical sulfide oxidation or precipitation is not important. An internally stored nitrate reservoir with average concentrations of 110 mmol L-1 ... : Supplement to: Lichtschlag, Anna; Felden, Janine; Brüchert, Volker; Boetius, Antje; de Beer, Dirk (2010): Geochemical processes and chemosynthetic primary production in different thiotrophic mats of the Hakon Mosby Mud Volcano (Barents Sea). Limnology and Oceanography, 55(2), 931-949 ...
format Article in Journal/Newspaper
author Lichtschlag, Anna
Felden, Janine
Brüchert, Volker
Boetius, Antje
de Beer, Dirk
author_facet Lichtschlag, Anna
Felden, Janine
Brüchert, Volker
Boetius, Antje
de Beer, Dirk
author_sort Lichtschlag, Anna
title Biogeochemical investigation of sediments at the Hakon Mosby Mud Volcano (Barents Sea) ...
title_short Biogeochemical investigation of sediments at the Hakon Mosby Mud Volcano (Barents Sea) ...
title_full Biogeochemical investigation of sediments at the Hakon Mosby Mud Volcano (Barents Sea) ...
title_fullStr Biogeochemical investigation of sediments at the Hakon Mosby Mud Volcano (Barents Sea) ...
title_full_unstemmed Biogeochemical investigation of sediments at the Hakon Mosby Mud Volcano (Barents Sea) ...
title_sort biogeochemical investigation of sediments at the hakon mosby mud volcano (barents sea) ...
publisher PANGAEA
publishDate 2009
url https://dx.doi.org/10.1594/pangaea.715022
https://doi.pangaea.de/10.1594/PANGAEA.715022
genre Barents Sea
genre_facet Barents Sea
op_relation https://dx.doi.org/10.4319/lo.2010.55.2.0931
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.71502210.4319/lo.2010.55.2.0931
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