Post-eruption colonization and community succession of hydrothermal microbial mats

Abstract:

T-RFLP fingerprint cluster analysis and qPCR of microbial mat communities from hydrothermal vent habitats among recent post-eruption sites exhibit similar communities containing Epsilonproteobacteria that are phylogenetically similar and capable of hydrogen-oxidation (e.g., Nitratiruptor, Caminibacter, Nautilia, Thioreductor, and/or Lebetimonas). This community is the first (Group I) of three community types that represent different stages in the transition from vapor-dominated to brine-dominated water-rock interactions (i.e., vent effluent geochemistry). We have now observed this similar transition from four hydrothermal regions from across the Pacific Ocean. The second type of mat community (Group II) that has been observed is characterized by the presence of another group of Epsilonproteobacteria; however, these are mostly sulfur-oxidizing phylotypes (e.g., Sulfurimonas, Sulfurovum, and/or Sulfuricurvum). Finally, once the transition from sulfur to iron is complete, then the third type (Group III) cluster together by the presence of Zetaproteobacteria, which are known to use iron-oxidation. Each of these community types are dominated by groups of microorganisms characterized by cultured isolates, all of which are strict chemolithoautotrophs capable of carbon fixation and are hypothesized as both ecosystem engineers and primary producers in these energy-rich ecosystems. We also consider the thermodynamic implications towards carbon fixation for each of the three groups of mat communities.