Results 211 to 220 of about 38,380 (249)
Abstract Microbial communities are strongly controlled by local nutrient availability, frequently resulting from mineral weathering and erosion. On Earth, basaltic rocks in habitable alkaline lacustrine environments are often initially colonised by ‘pioneer’ communities that induce the precipitation of fine‐scale microbial carbonate ‘coatings’; on Mars,
Keyron Hickman‐Lewis +6 more
wiley +1 more source
Lamination-Controlled Lithofacies Differentiation and Shale Oil Enrichment: A Case Study of the Qingshankou Formation, Songliao Basin. [PDF]
Yao Q +9 more
europepmc +1 more source
Abstract The Mars 2020 mission has explored depositional environments recorded in a fan‐shaped deposit on the western side of Jezero crater. Kodiak butte is an isolated outcrop of sedimentary rock ∼1 km south of the western fan scarp and may be an erosional remnant of said fan.
O. A. Kanine +4 more
wiley +1 more source
Reassessment of Miocene putative coprolites from Poland suggests a biogenic origin and probable squamate (reptilian) producers. [PDF]
Brachaniec T +6 more
europepmc +1 more source
Influence of Floodplain Subsurface Composition on Peatland Stream Channel Mobility
Abstract Peatlands are important for the earth's carbon cycle, globally storing the equivalent of two‐thirds of the atmospheric carbon reservoir. The capacity of peatlands to preserve organic matter is influenced by stream‐channel mobility and sediment reworking; however, the nature of these processes is poorly constrained.
J. M. Nelson +3 more
wiley +1 more source
Environmental evolution of a coastal lake in the Larsemann Hills, East Antarctica during the Holocene: a multi-proxy perspective. [PDF]
Joju GS +12 more
europepmc +1 more source
Abstract African rainforests store large quantities of carbon within below‐ground reservoirs, yet these stocks are threatened by land use and climate disturbances. Previous studies revealed that the peatlands of the Cuvette Centrale in the Congo Basin accumulated less organic carbon (OC) between 7,500 and 2,000 yrs BP (so‐called “Ghost Interval ...
M. P. Engelhardt +8 more
wiley +1 more source
Rapid acceleration of ice-cover loss from Northern Hemisphere lakes above critical air temperature thresholds. [PDF]
Zhou J +6 more
europepmc +1 more source
Abstract Detrital zircon U–Pb geochronology from Triassic–Jurassic basins in the New England Orogen (NEO) constrains sediment provenance and episodic continental arc evolution along the eastern Gondwanan margin. Dominant zircon clusters at 270–230 Ma and 340–300 Ma in these basins were likely sourced from contemporaneous magmatism in the NEO ...
Yanxiong Zhang +2 more
wiley +1 more source
Microbial N<sub>2</sub>O Reduction in Sulfidic Waters: Implications for Proterozoic Oceans. [PDF]
Buessecker S +8 more
europepmc +1 more source

