Literature DB >> 22009262

Microbial eukaryote life in the new hypersaline deep-sea basin Thetis.

Alexandra Stock1, Hans-Werner Breiner, Maria Pachiadaki, Virginia Edgcomb, Sabine Filker, Violetta La Cono, Michail M Yakimov, Thorsten Stoeck.   

Abstract

Only recently, a novel anoxic hypersaline (thalassic) basin in the eastern Mediterranean was discovered at a depth of 3,258 m. The halite-saturated brine of this polyextreme basin revealed one of the highest salt concentrations ever reported for such an environment (salinity of 348‰). Using a eukaryote-specific probe and fluorescence in situ hybridization, we counted 0.6 × 10(4) protists per liter of anoxic brine. SSU rRNA sequence analyses, based on amplification of environmental cDNA identified fungi as the most diverse taxonomic group of eukaryotes in the brine, making deep-sea brines sources of unknown fungal diversity and hotspots for the discovery of novel metabolic pathways and for secondary metabolites. The second most diverse phylotypes are ciliates and stramenopiles (each 20%). The occurrence of closely related ciliate sequences exclusively in other Mediterranean brine basins suggests specific adaptations of the respective organisms to such habitats. Betadiversity-analyses confirm that microeukaryote communities in the brine and the interface are notably different. Several distinct morphotypes in brine samples suggest that the rRNA sequences detected in Thetis brine can be linked to indigenous polyextremophile protists. This contradicts previous assumptions that such extremely high salt concentrations are anathema to eukaryotic life. The upper salinity limits for eukaryotic life remain unidentified.

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Year:  2011        PMID: 22009262     DOI: 10.1007/s00792-011-0401-4

Source DB:  PubMed          Journal:  Extremophiles        ISSN: 1431-0651            Impact factor:   2.395


  46 in total

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1.  Unveiling microbial activities along the halocline of Thetis, a deep-sea hypersaline anoxic basin.

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7.  Environmental selection of protistan plankton communities in hypersaline anoxic deep-sea basins, Eastern Mediterranean Sea.

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