Moderately halophilic and euryhaline bacteria are routinely found in cool to warm hydrothermal vent and nearby cold, deep-sea environments. To elucidate the diversity of these microorganisms - with the goal of determining which among them constitute ecotypes specifically associated with hydrothermal vent and subseafloor habitats - PCR primers were designed to detect natural populations of euryhaline Gammaproteobacteria belonging to the cosmopolitan genera Halomonas and Marinobacter. The distribution patterns of 16S rRNA gene sequence data revealed that Halomonas group 2A comprised a subseafloor population at Axial Seamount on the Juan de Fuca Ridge. Complementary biogeographic and physiological data suggested that other Halomonas clades include members that are cold adapted (Halomonas group 2B) or associated with massive sulfide deposits (Halomonas group 2C). Similarly, a monophyletic Marinobacter clade may represent Fe(2+) -oxidizing facultative chemoautotrophs based on the phylogenetic data presented here and previously reported phenotypic characterizations. The biogeographic distributions of Halomonas and Marinobacter isolates and clones reveal that these are cosmopolitan genera, commonly found in the deep sea and in hydrothermal vent settings. As such, they are good candidates for further laboratory investigations into the biogeochemical processes in these environments.
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http://dx.doi.org/10.1111/j.1574-6941.2010.00984.x | DOI Listing |
FEBS J
January 2025
'The Protein Factory 2.0', Dipartimento di Biotecnologie e Scienze della Vita, Università degli Studi dell'Insubria, Varese, Italy.
The sequestration of carbon dioxide using carbonic anhydrase (CA) is one of the most effective methods for mitigating global warming. The burning of fossil fuels releases large quantities of flue gas; because of its high temperature and of the alkaline conditions required for CaCO precipitation in the mineralization process, thermo-alkali-stable CAs are needed. In this context, Manyumwa et al.
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January 2025
Dipartimento Scienze e Tecnologie Biologiche, Chimiche e Farmaceutiche, University of Palermo, Viale delle Scienze, 90128 Palermo, Italy.
Marine hydrothermal ecosystems represent extreme environments connected to submarine volcanic areas characterized by vents, having high temperatures and particular chemical compositions. The hydrothermal marine system of Panarea, located in one of the seven small islands belonging to the Aeolian Archipelago (southern Tyrrhenian Sea), is characterized by a range of vents exhibiting diverse physical and chemical conditions. We aimed to analyze the microbial community of a peculiar hot spring belonging to the Panarea hydrothermal field, known as "Black Point" (BP), in two separate sampling expeditions (May and August).
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January 2025
Department of Science Education, National Taipei University of Education, 134 Section 2, Heping East Road, Taipei City 106, Taiwan.
The shallow-sea hydrothermal vent at Guishan Islet, located off the coast of Taiwan, serves as a remarkable natural site for studying microbial ecology in extreme environments. In April 2019, we investigated the composition of prokaryotic picoplankton communities, their gene expression profiles, and the dissolved inorganic carbon uptake efficiency. Our results revealed that the chemolithotrophs spp.
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December 2024
Division of Biochemistry, Faculty of Pharmaceutical Sciences, Tohoku Medical and Pharmaceutical University, Sendai 981-8558, Japan.
We propose a hypothesis for the simultaneous emergence of bacteria, archaea, viruses, and mobile elements by sequential and concrete biochemical pathways. The emergence process can be considered analogous to crystallization, where genetic and biochemical systems stabilize as organisms evolve from their common ancestor, the LUCA, which was a non-free-living pool of single operon type genomes including double-stranded (ds) DNA at an ancient submarine alkaline vent. Each dsDNA operon was transcribed by different systems in σ, TFIIB, or TBP genomes.
View Article and Find Full Text PDFSci Rep
January 2025
Department of Geology, School of Natural Sciences, Trinity College Dublin, Dublin, Ireland.
Massive injection of C depleted carbon to the ocean and atmosphere coincided with major environmental upheaval multiple times in the geological record. For several events, the source of carbon has been attributed to explosive venting of gas produced when magmatic sills intruded organic-rich sediment. The concept mostly derives from studies of a few ancient sedimentary basins with numerous hydrothermal vent complexes (HTVCs) where craters appear to have formed across large areas of the seafloor at the same time, but good examples remain rare in strata younger than the Early Eocene.
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