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The post-spinel transition in mantle composition, which occurs at 660-km depth in Earth’s mantle, takes place over a pressure range equivalent to 250 m in depth, according to multi-anvil experiments for realistic mantle compositions and temperatures.
A redistribution of marine calcifiers along with a reduction in weathering led to increased seafloor carbonate deposition during the late Neogene, according to a global compilation of carbonate mass accumulation rate records from sediment cores.
Steady-state chemical differentiation between Earth’s mantle and crust was reached 3.5 billion years ago, following vigorous crustal recycling, according to mass balance modelling of molybdenum isotopes measured in mantle-derived volcanic rocks.
Depleted mantle is a volumetrically dominant component of the Azores plume and possibly of oceanic basalt sources more generally, according to neodymium isotope compositions of olivine-hosted melt inclusions from lavas of the Azores mantle plume.
Seismicity induced by wastewater injections is widespread in Oklahoma, probably because its basement is susceptible to the reactivation of basement-rooted faults, according to three-dimensional seismic analyses, rock-mechanics experiments and field surveys.
The Havre Tough back-arc basin, New Zealand, formed rapidly and in two phases: initial, limited seafloor spreading was followed by a transition to arc magmatism, as shown by geophysical data and modelling.
The structure of the lithosphere and its impact on mantle flow significantly influence the impact of Earth’s interior dynamics on surface topography, suggest statistical analyses of Earth’s topography.
Glaciers in the Andes have lost about 23 Gt of mass per year between 2000 and 2018, with the fastest loss in Patagonia, according to time series of digital elevation models that are based on ASTER stereo images.
Some lake basins in the polar regions of Titan may be craters from nitrogen vapour explosions due to past warming, according to analysis of their morphology in comparison to terrestrial explosion craters from magma–water interaction.
The northern temperate carbon sink is estimated to increase by 0.64 PgC each year for each increase in atmospheric CO2 concentrations by 100 ppm, suggests an analysis of data from field experiments at 7 sites constraints.
Evaporite dissolution coupled with pyrite burial can lead to biogeochemical feedbacks that explain the enigmatic Neoproterozoic carbon isotope record, according to numerical model simulations.
Vigorous mixing between the protolunar disk and Earth followed by processes in the cooling disk may explain the enrichment in light isotopes of tin on the Moon relative to Earth, as found by analysis of lunar rocks and geochemical calculations.
Archaean granitic rocks formed by melting of silica-enriched subducted basaltic crust through interaction with seawater, according to heavy silicon isotopes measured in Archaean samples.
Granitic continental crust in the Archaean formed from a basaltic source that was enriched in silica due to interaction with the early oceans before melting, according to silicon isotope analyses on rocks from the Kaapvaal craton.
Inclusion of sponge spicules and radiolarians increases the global ocean biological sink of silicon by 28%, with 95% of that increase attributed to sponges, according to examination of sediments from 17 marine cores.
The European mega-heatwaves in 2003 and 2010 were intensified by torrents of hot air that were transported in from desiccated regions upwind, suggests an analysis of observations and reanalysis data together with a Lagrangian heat-tracking framework.