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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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 |
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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 |
_version_ |
1810434044725297152 |