Biogeochemistry of a low-activity cold seep in the Larsen B area, western Weddell Sea, Antarctica
- 1Max Planck Institute for Marine Microbiology, Bremen, Germany
- 2Institute for Environmental Geosciences, University of Basel, Basel, Switzerland
- 3MARUM – Center for Marine Environmental Sciences and Department of Geosciences, Univ. of Bremen, Bremen, Germany
- 4Alfred Wegener Institute for Polar and Marine Research, Bremerhaven, Germany
- 5Universidad de Magallanes, Punta Arenas, Chile
- 6German Aerospace Centre, Bonn, Germany
Abstract. First videographic indication of an Antarctic cold seep ecosystem was recently obtained from the collapsed Larsen B ice shelf, western Weddell Sea (Domack et al., 2005). Within the framework of the R/V Polarstern expedition ANTXXIII-8, we revisited this area for geochemical, microbiological and further videographical examinations. During two dives with ROV Cherokee (MARUM, Bremen), several bivalve shell agglomerations of the seep-associated, chemosynthetic clam Calyptogena sp. were found in the trough of the Crane and Evans glacier. The absence of living clam specimens indicates that the flux of sulphide and hence the seepage activity is diminished at present. This impression was further substantiated by our geochemical observations. Concentrations of thermogenic methane were moderately elevated with 2 μM in surface sediments of a clam patch, increasing up to 9 μM at a sediment depth of about 1 m in the bottom sections of the sediment cores. This correlated with a moderate decrease in sulphate from about 28 mM at the surface down to 23.4 mM, an increase in sulphide to up to 1.43 mM and elevated rates of the anaerobic oxidation of methane (AOM) of up to 600 pmol cm−3 d−1 at about 1 m below the seafloor. Molecular analyses indicate that methanotrophic archaea related to ANME-3 are the most likely candidates mediating AOM in sediments of the Larsen B seep.