Results 191 to 200 of about 122,416 (319)
Impact‐Generated Mixing, Melting and Vaporization of the Early Earth's Crust
Abstract Earth's primary accretion was followed by a protracted flux of interplanetary collisions by leftover planetesimals. The effects of the largest collisions—with bodies possibly exceeding 1,000 km diameter—would have been devastating for terrestrial near‐surface environments.
S. Marchi +3 more
wiley +1 more source
Crustal constraints on the surface expression of mantle upwelling in a back-arc passive margin setting. [PDF]
Hwang JY, Chang SJ, Sohn YJ, Kim KH.
europepmc +1 more source
Seasonality in Marine Organic Carbon Export and Sequestration Pathways
Abstract The ocean's biological carbon pump transports organic carbon from the surface to depth via three main pathways: the gravitational sinking of particles, active transport by vertically migrating zooplankton, and mixing and advection of suspended and dissolved organic carbon.
Renjian Li +3 more
wiley +1 more source
Revisiting the scale of mantle plume-induced hot spot swells. [PDF]
Liu L +5 more
europepmc +1 more source
Bilateral heterogeneity in an upwelling mantle via double subduction of oceanic lithosphere
Dao Van Nghiem
openalex +2 more sources
R.R. Stanichnaya, S.V. Stanichny
openaire +1 more source
Abstract The biological carbon pump sequesters carbon through passive fluxes of biologically derived carbon, and by active vertical movement of marine organisms. Trophic coupling between pelagic and benthic communities increases the efficiency of the biological carbon pump as less carbon is lost to remineralization.
Daniel Ottmann +6 more
wiley +1 more source
Microbial diagenesis of dissolved organic matter from the ocean's surface to abyssal depths: a case study in the Humboldt upwelling system. [PDF]
Engel A +6 more
europepmc +1 more source

