Results 231 to 240 of about 82,783 (326)
Microbial Community Dynamics in Early Tufa Biofilms
Microbial succession shapes the early development of tufa biofilms in karst freshwater systems, with prokaryotic communities stabilizing rapidly and microeukaryotes contributing to extracellular polymeric substance production and carbonate entrapment. Site‐specific hydrodynamics and organic inputs drive community specialization, ultimately influencing ...
Andrea Čačković +3 more
wiley +1 more source
Average physical structure of cratonic lithosphere, from thermodynamic inversion of global surface-wave data. [PDF]
Xu Y, Lebedev S, Fullea J.
europepmc +1 more source
Globally Mapping the Nitrogen Stable Isotope Ratios of Terrestrial Vegetation From 1984 to 2022
Abstract Nitrogen cycles control the structure, function, and composition of ecosystems globally. Despite their importance, our understanding of long‐term changes in global nitrogen cycles remains limited. The foliar nitrogen stable isotope ratio (δ15N) serves as a valuable metric for assessing changes in nitrogen cycling and potentially in plant ...
Jinyan Yang +12 more
wiley +1 more source
Intraplate deformation of Gondwana terranes and implications for the Wilson Cycle. [PDF]
Fonseca A, De Grave J.
europepmc +1 more source
Abstract The High Arctic Large Igneous Province (HALIP) formed in the circum‐Arctic during the Cretaceous. The timing and duration of emplacement of these mafic magmas are important for understanding the climatic and environmental effects, yet many uncertainties remain. The dating methods used vary greatly between different regions.
A. M. R. Sartell +4 more
wiley +1 more source
Seismic and gravity constraints on plate flexure and mantle rheology along the whole Hawaiian-Emperor seamount chain. [PDF]
Watts AB +5 more
europepmc +1 more source
Toward Reconstructing Mantle Convection Using a Minimum‐Continent‐Motion Reference Frame
Abstract Studying geodynamic processes at the plate‐mantle interface requires knowledge of how plates move over and subduct into the mantle. The absolute motion of plates relative to the mantle since ∼120 Ma is classically estimated using hotspot tracks.
S. D. M. Wagenaar +2 more
wiley +1 more source
Terrane accretion explains thin and hot ocean-continent back-arcs. [PDF]
Erdős Z +3 more
europepmc +1 more source

