Loading…

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

Deep-sea whale falls create sulfidic habitats 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-f...

Full description

Saved in:
Bibliographic Details
Published in:Marine ecology. Progress series (Halstenbek) 2009-04, Vol.382, p.1-21
Main Authors: Treude, Tina, Smith, Craig R., Wenzhöfer, Frank, Carney, Erin, Bernardino, Angelo F., Hannides, Angelos K., Krüger, Martin, Boetius, Antje
Format: Article
Language:English
Subjects:
Citations: Items that cite this one
Online Access:Get full text
Tags: Add Tag
No Tags, Be the first to tag this record!
Description
Summary:Deep-sea whale falls create sulfidic habitats 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, radiotracer incubations and geochemical analyses. Sediments were studied at different distances (0 to 9 m) from the whale fall. Highest microbial activities and steepest vertical geochemical gradients were found within 0.5 m of the whale fall, revealingex situsulfate reduction andin vitromethanogenesis rates of up to 717 and 99 mmol m–2d–1, respectively. In sediments containing whale biomass, methanogenesis was equivalent to 20 to 30% of sulfate reduction. Duringin vitrosediment 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–1in Years 6 and 7, respectively, of which ~200 mmol d–1were available as free sulfide. Sulfate reduction in bones was much lower, accounting for a total availability of ~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.
ISSN:0171-8630
1616-1599
DOI:10.3354/meps07972