Results 21 to 30 of about 3,897 (205)

Microbial turnover times in the deep seabed studied by amino acid racemization modelling

open access: yesScientific Reports, 2017
The study of active microbial populations in deep, energy-limited marine sediments has extended our knowledge of the limits of life on Earth. Typically, microbial activity in the deep biosphere is calculated by transport-reaction modelling of pore water ...
Stefan Braun   +8 more
doaj   +1 more source

Metapangenomic investigation provides insight into niche differentiation of methanogenic populations from the subsurface serpentinizing environment, Samail Ophiolite, Oman

open access: yesFrontiers in Microbiology, 2023
Serpentinization reactions produce highly reduced waters that have hyperalkaline pH and that can have high concentrations of H2 and CH4. Putatively autotrophic methanogenic archaea have been identified in the subsurface waters of the Samail Ophiolite ...
Patrick H. Thieringer   +3 more
doaj   +1 more source

From Plant to Paddy—How Rice Root Iron Plaque Can Affect the Paddy Field Iron Cycling

open access: yesSoil Systems, 2020
Iron plaque on rice roots represents a sink and source of iron in paddy fields. However, the extent of iron plaque in impacting paddy field iron cycling is not yet fully deciphered.
Markus Maisch   +3 more
doaj   +1 more source

Integrating microbiology into the Drigg Post-closure radiological safety assessment [PDF]

open access: yes, 2001
BNFL owns and operates the UK.s principal solid Low Level Radioactive Waste disposal site at Drigg in Cumbria, north west England. Drigg has been receiving waste since 1959 with approximately 900,000 m3 of waste disposed of to date.
Small, J.   +3 more
core   +4 more sources

N2O formation by nitrite-induced (chemo)denitrification in coastal marine sediment

open access: yesScientific Reports, 2019
Nitrous oxide (N2O) is a potent greenhouse gas that also contributes to stratospheric ozone depletion. Besides microbial denitrification, abiotic nitrite reduction by Fe(II) (chemodenitrification) has the potential to be an important source of N2O. Here,
Julia M. Otte   +5 more
doaj   +1 more source

Time Zero for Net Zero: A Coal Mine Baseline for Decarbonising Heat

open access: yesEarth Science, Systems and Society, 2022
Mine water geothermal energy could provide sustainable heating, cooling and storage to assist in the decarbonisation of heat and achieving Net Zero carbon emissions.
Alison A. Monaghan   +25 more
doaj   +1 more source

Applications of Fourier-transform Infrared Spectroscopy in Geomicrobiology

open access: yes, 2019
Fourier-transform infrared (FTIR) spectroscopy is a technique that measures the molecular-level vibrations in a material, such as a bacterial biofilm, to get a better understanding of the chemistry of the system.
Gorzsás, András,   +1 more
core   +1 more source

Iron mineral dissolution releases iron and associated organic carbon during permafrost thaw

open access: yesNature Communications, 2020
Iron minerals trap carbon in permafrost, preventing microbial degradation and release to the atmosphere as CO2, but the stability of this carbon as permafrost thaws is unclear.
Monique S. Patzner   +10 more
doaj   +1 more source

Statistical trends in culture methods of endolithic bacteria extracted from Quartz, K-Feldspar (Jurassic) and Calcite (Quaternary) in semi-arid areas in Colombia

open access: yesGeologica Acta, 2022
Microbial endolithic communities are ubiquitous in many deserts around the globe. They have been found in many different lithologies, including quartz, plagioclase and calcite.
Julian Andreas Corzo-Acosta   +1 more
doaj   +1 more source

CANT-HYD: A Curated Database of Phylogeny-Derived Hidden Markov Models for Annotation of Marker Genes Involved in Hydrocarbon Degradation

open access: yesFrontiers in Microbiology, 2022
Many pathways for hydrocarbon degradation have been discovered, yet there are no dedicated tools to identify and predict the hydrocarbon degradation potential of microbial genomes and metagenomes.
Varada Khot   +11 more
doaj   +1 more source

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