Results 61 to 70 of about 363 (122)
Abstract Oxygen deficient zones (ODZs) are key areas of nitrogen loss, a process dependent on organic matter. Understanding the sources of organic matter in the ODZ is necessary to predict how biogeochemical cycles will respond to ocean changes. Size fractionated (5–20, 20–53, 53–180, 180–500, >500 μm) particulate organic C and N (POM) concentration ...
Clara A. Fuchsman, Jacob A. Cram
wiley +1 more source
Hot desert surface soils are characterized by extremely low water activities for large parts of any annual cycle. It is widely assumed that microbial processes in such soils are very limited.
Carlos León-Sobrino +3 more
doaj +1 more source
Abstract Relative to their limited areal extent, riparian ecosystems are disproportionately important in regulating inorganic solute export from agricultural landscapes. We investigated spatial patterns of solute concentrations in surface and ground waters of stream corridors to infer the dominant hydrologic transport and biogeochemical pathways that ...
Caitlin M. Mayernik +8 more
wiley +1 more source
Trait‐Based Life History Strategies Shape Bacterial Niche Breadth
This study investigates bacterial niche breadth through a large‐scale soil survey and over 2000 bacterial genomes. It identifies key life‐history traits—growth, competition, stress tolerance, resource acquisition, and dispersal—that correlate with niche breadth.
Ziheng Peng +8 more
wiley +1 more source
Background Corals are known for their symbiotic relationships, yet there is limited evidence of chemoautotrophic associations. This is despite some corals occurring near cold seeps where chemosymbiotic fauna abound including mussels that host sulfur ...
Samuel A. Vohsen +7 more
doaj +1 more source
Chemolithoautotrophic production mediating the cycling of the greenhouse gases N2O and CH4 in an upwelling ecosystem [PDF]
The high availability of electron donors occurring in coastal upwelling ecosystems with marked oxyclines favours chemoautotrophy, in turn leading to high N2O and CH4 cycling associated with aerobic NH4+ (AAO) and CH4 oxidation (AMO).
M. E. Alcaman +4 more
doaj
Rapid warming of the Arctic is accelerating permafrost (frozen ground) thaw and releasing previously frozen organic matter into streams and rivers. At an abruptly thawing permafrost site in Siberia (Duvanny Yar), we show that permafrost thaw streams and their outflow waters to the Kolyma River release greenhouse gases to the atmosphere.
Kirsi H. Keskitalo +9 more
wiley +1 more source
Dark carbon fixation in stream carbon cycling
Abstract Headwater streams are often characterized by turbulence, organic matter inputs from terrestrial systems, net heterotrophy, and the microbial loop supplying carbon and energy for consumers. However, ecological models overlook dark carbon fixation (DCF), the light‐independent inorganic carbon uptake, mainly based on chemosynthesis, using energy ...
Fausto Machado‐Silva +5 more
wiley +1 more source
Summary Viruses are the most abundant life forms in the world's oceans and they are key drivers of biogeochemical cycles, but their impact on the microbial assemblages inhabiting hydrothermal vent ecosystems is still largely unknown.
Rastelli E +8 more
openaire +5 more sources
Bacterial chemoautotrophic reoxidation in sub-Arctic sediments: a seasonal study in Kobbefjord, Greenland [PDF]
Anoxic mineralization of organic matter releases dissolved inorganic carbon and produces reduced mineralization products. The reoxidation of these reduced compounds is essential for biogeochemical cycling in sediments and is mainly performed by ...
Boschker, Henricus T.S. +15 more
core +1 more source

