Biogeochemistry of a deep-sea whale fall: sulfate reduction, sulfide efflux and methanogenesis
Contribuinte(s) |
UNIVERSIDADE DE SÃO PAULO |
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Data(s) |
20/10/2012
20/10/2012
2009
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Resumo |
Deep-sea whale falls create sulfidic habits Supporting chemoautotrophic communities, but microbial processes underlying the formation Of Such habitats remain poorly evaluated. Microbial degradation processes (sulfate reduction, methanogenesis) and biogeochemical gradients were studied in a whale-fall habitat created by a 30 t whale carcass deployed at 1675 m depth for 6 to 7 yr on the California margin. A variety of measurements were conducted including photomosaicking, microsensor measurements, radio-tracer incubations and geochemical analyses. Sediments were Studied at different distances (0 to 9 in) from the whale fall. Highest microbial activities and steepest vertical geochemical gradients were found within 0.5 m of the whale fall, revealing ex situ sulfate reduction and in vitro methanogenesis rates of up to 717 and 99 mmol m(-2) d(-1), respectively. In sediments containing whale biomass, methanogenesis was equivalent to 20 to 30%, of sulfate reduction. During in vitro sediment studies, sulfide and methane were produced within days to weeks after addition of whale biomass, indicating that chemosynthesis is promoted at early stages of the whale fall. Total sulfide production from sediments within 0.5 m of the whale fall was 2.1 +/- 3 and 1.5 +/- 2.1 mol d(-1) in Years 6 and 7, respectively, of which similar to 200 mmol d(-1) were available as free sulfide. Sulfate reduction in bones was much lower, accounting for a total availability of similar to 10 mmol sulfide d(-1). Over periods of at least 7 yr, whale falls can create sulfidic conditions similar to other chemosynthetic habitats Such as cold seeps and hydrothermal vents. National Undersea Research Center Alaska, NOAA National Undersea Research Center Alaska, NOAA USA National Science Foundation (NSF) U. S. National Science Foundation (NSF) Biological Oceanography Program Biological Oceanography Program[OCE 0096422] Max Planck Society, the University of Hawaii at Manao Max Planck Society, the University of Hawaii at Manao Monterey Bay Aquarium Research Institute Monterey Bay Aquarium Research Institute School of Ocean and Earth Science and Technology, University of Hawaii at Manoa[7748] School of Ocean and Earth Science and Technology, University of Hawaii at Manoa |
Identificador |
MARINE ECOLOGY-PROGRESS SERIES, v. 382, p. 1-21, 2009 0171-8630 http://producao.usp.br/handle/BDPI/32081 10.3354/meps07972 |
Idioma(s) |
eng |
Publicador |
INTER-RESEARCH |
Relação |
Marine Ecology-progress Series |
Direitos |
restrictedAccess Copyright INTER-RESEARCH |
Palavras-Chave | #Chemosynthesis #Organic carbon input #Microbial degradation #Sediment #Bone #Cold seep #Hydrothermal vent #DIFFUSIVE BOUNDARY-LAYERS #SANTA-CATALINA BASIN #ANAEROBIC OXIDATION #COMMUNITY STRUCTURE #METHANE PRODUCTION #HYDROTHERMAL VENT #OXYGEN-UPTAKE #CONTINENTAL-MARGIN #NORTHEAST PACIFIC #MARINE-SEDIMENTS #Ecology #Marine & Freshwater Biology #Oceanography |
Tipo |
article original article publishedVersion |