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The archaeal phylum Bathyarchaeota, which is composed of a large number of diverse lineages, is widespread and abundant in marine sediments. Environmental factors that control the distribution, abundance and evolution of this largely diversified archaeal phylum are currently unclear. In this study, a new pair of specific primers that target the major marine subgroups of bathyarchaeotal 16S rRNA genes was designed and evaluated to investigate the distribution and abundance of Bathyarchaeota in marine sediments. The abundance of Bathyarchaeota along two sediment cores from the deep-sea sediments of South China Sea (SCS, each from the Dongsha and Shenhu area) was determined. A strong correlation was found between the bathyarchaeotal abundance and the content of total organic carbon (TOC), suggesting an important role of Bathyarchaeota in organic matter remineralisation in the sediments of SCS. Furthermore, diversity analysis revealed that subgroups Bathy-2, Bathy-8 and Bathy-10 were dominant bathyarchaeotal members of the deep-sea sediments in the SCS. Bathy-8 was found predominantly within the reducing and deeper sediment layers, while Bathy-10 occurred preferentially in the oxidizing and shallower sediment layers. Our study lays a foundation for the further understanding of the ecological functions and niche differentiation of the important but not well-understood sedimentary archaeal group.
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http://dx.doi.org/10.1111/1758-2229.12539 | DOI Listing |
Environ Microbiol Rep
October 2025
Department of Biology, Marine Biology Section, University of Copenhagen, Helsingør, Denmark.
Due to climate change, sea ice more commonly retreats over the shelf breaks in the Arctic Ocean, impacting sea ice-pelagic-benthic coupling in the deeper basins. Nitrogen fixation (the reduction of dinitrogen gas to bioavailable ammonia by microorganisms called diazotrophs) is reported from Arctic shelf sediments but is unknown from the Arctic deep sea. We sampled five locations of deep-sea (900-1500 m) surface sediments in the central ice-covered Arctic Ocean to measure potential nitrogen fixation through long-term (> 280 days) stable-isotope (N) incubations and to study diazotroph community composition through amplicon sequencing of the functional marker gene nifH.
View Article and Find Full Text PDFRev Sci Instrum
September 2025
Key Laboratory of Ocean Energy Utilization and Energy Conservation of Ministry of Education, Dalian University of Technology, Dalian 116024, People's Republic of China.
Metastable hydrates are widely distributed in shallow deep-sea sediments, posing significant risks to the long-term stability of offshore foundation structures. Unveiling the weakening mechanisms at the hydrate-bearing sediment-structure interface is crucial for establishing a theoretical framework for the safe design of deep-sea structures. A high-pressure (up to 12.
View Article and Find Full Text PDFMycobiology
August 2025
Departamento de Botánica, Instituto de Biología, Universidad Nacional Autónoma de México, Mexico City, Mexico.
Microorganisms from hydrothermal vents fields in the Pescadero Basin represent a promising source for biotechnological applications due to their adaptation to extreme environments. The hydrocarbon seeps in the Pescadero Basin provide a natural precedent for native fungi capable of biodegrading crude oil. In this study, the ability of eight fungal isolates from hydrothermal vent sediments in the Pescadero Basin to bioconvert extra-heavy crude oil (EHCO) was evaluated.
View Article and Find Full Text PDFMicroorganisms
August 2025
LAMIR Institute, Graduate Program in Geology, Universidade Federal do Paraná, Curitiba 81531-980, Paraná, Brazil.
Extreme environments, such as hypersaline habitats, hot springs, deep-sea hydrothermal vents, glaciers, and permafrost, provide diverse ecological niches for studying microbial evolution. However, knowledge of microbial communities in extreme environments at high southern latitudes remains limited, aside from Antarctica. Laguna Timone is a hypersaline crater lake located in a Pleistocene maar of the Pali Aike Volcanic Field, southern Patagonia; the lake was formed during basaltic eruptions in a periglacial setting.
View Article and Find Full Text PDFWater Res
August 2025
Key Laboratory of Marine Mineral Resources, Ministry of Natural Resources, Guangzhou Marine Geological Survey, China Geological Survey, Guangzhou, 511458, China; National Engineering Research Center for Gas Hydrate Exploration and Development, Guangzhou 511458, China. Electronic address: dengyinan@1
Microplastics (MPs) have penetrated even the most remote deep-sea sediments, yet their vertical distribution and depositional pathways remain unclear. This study analyzed sediment cores (0-20 cm) from 11 Philippine Sea stations, finding MPs in all layers with an average abundance of 218.4 ± 303.
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