The deep subseafloor biosphere supports a diverse population of prokaryotes belonging to the Bacteria and Archaea. Most of the taxonomic groups identified by molecular methods contain mainly uncultured phylotypes. Despite this several cultured strains have been isolated from this habitat, but they probably do not represent the majority of the population. Evidence is starting to suggest that some of the activities measured, such as sulphate reduction and methanogenesis, reflected in geochemical profiles, are carried out by a small subset of the community detected by molecular methods. It is further possible that heterotrophy may be the most important mode of metabolism in subsurface sediments and heterotrophic microorganisms could dominate the uncultured prokaryotic population. Although, heterotrophy is limited by the increasing recalcitrance of organic matter with depth, this may be counteracted by thermal activation of buried organic matter providing additional substrates at depth.
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http://dx.doi.org/10.1111/j.1574-6941.2008.00566.x | DOI Listing |
Mar Environ Res
December 2024
Institut National de Recherche Halieutique (INRH), Casablanca 20100, Morocco. Electronic address:
The recent decline in the health status of deep-sea habitats around the world has pushed the need to document and map their distribution to preserve them in their marine ecosystems. This work describes deep-water coral habitats (133-729 m) and their associated communities, based on nine ROV video transects. These transects cover a 171 km sub-seafloor profile within a predefined 5560 km area along the North Atlantic coast of Morocco, surveyed in 2020 as part of a coral habitat mapping study under the FAO-NANSEN programme.
View Article and Find Full Text PDFMicroorganisms
October 2024
State Key Laboratory of Pharmaceutical Biotechnology, Nanjing University, Nanjing 210023, China.
Fungi inhabiting deep subseafloor sediments have been shown to possess anaerobic methane (CH) production capabilities under atmospheric conditions. However, their ability to produce CH under in situ conditions with high hydrostatic pressure (HHP) remains unclear. Here, 20R-7-F01, isolated from ~2 km below the seafloor, was cultured in Seawater Medium (SM) in culture bottles fitted with sterile syringes for pressure equilibration.
View Article and Find Full Text PDFJ Am Chem Soc
November 2024
Department of Physics, Hong Kong University of Science and Technology, Hong Kong 999077, China.
How life started on Earth is an unsolved mystery. There are various hypotheses for the location ranging from outer space to the seafloor, subseafloor, or potentially deeper. Here, we applied extensive ab initio molecular dynamics simulations to study chemical reactions between NH, HO, H, and CO at pressures () and temperatures () approximating the conditions of Earth's upper mantle (i.
View Article and Find Full Text PDFIt was once believed that only microbes and viruses inhabited the subseafloor crust beneath hydrothermal vents. Yet, on the seafloor, animals like the giant tubeworm Riftia pachyptila thrive. Their larvae are thought to disperse in the water column, despite never being observed there.
View Article and Find Full Text PDFAppl Environ Microbiol
October 2024
State Key Laboratory of Pharmaceutical Biotechnology, Nanjing University, Nanjing, Jiangsu, China.
Unlabelled: Deep-sea sediments harbor abundant microbial communities extending vertically up to ~2.5 km below the seafloor. Despite their prevalence, the reasons for their large community sizes and low energy fluxes remain unclear.
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