Abstract

ABSTRACT During recent oceanographic cruises to Pacific hydrothermal vent sites (9°N and the Guaymas Basin), the rapid microbial formation of filamentous sulfur mats by a new chemoautotrophic, hydrogen sulfide-oxidizing bacterium was documented in both in situ and shipboard experiments. Observations suggest that formation of these sulfur mats may be a factor in the initial colonization of hydrothermal surfaces by macrofaunal Alvinella worms. This novel metabolic capability, previously shown to be carried out by a coastal strain in H 2 S continuous-flow reactors, may be an important, heretofore unconsidered, source of microbial organic matter production at deep-sea hydrothermal vents.

Keywords

Hydrothermal ventSulfurHydrothermal circulationMicrobial matChemosynthesisSulfur cycleSulfideOrganic matterEnvironmental chemistryOceanographyEcologyBacteriaBiologyChemistryGeologyCyanobacteriaPaleontology

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Publication Info

Year
1999
Type
article
Volume
65
Issue
5
Pages
2253-2255
Citations
129
Access
Closed

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Craig D. Taylor, Carl O. Wirsen, Françoise Gaill (1999). Rapid Microbial Production of Filamentous Sulfur Mats at Hydrothermal Vents. Applied and Environmental Microbiology , 65 (5) , 2253-2255. https://doi.org/10.1128/aem.65.5.2253-2255.1999

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DOI
10.1128/aem.65.5.2253-2255.1999