Biogeochemistry of a deep-sea whale fall: sulfate reduction, sulfide efflux and methanogenesis


Autoria(s): TREUDE, Tina; SMITH, Craig R.; WENZHOEFER, Frank; CARNEY, Erin; BERNARDINO, Angelo F.; HANNIDES, Angelos K.; KRUEGER, Martin; BOETIUS, Antje
Contribuinte(s)

UNIVERSIDADE DE SÃO PAULO

Data(s)

20/10/2012

20/10/2012

2009

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

http://dx.doi.org/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