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The Antarctic Ice Sheet (AIS) underwent dramatic changes over the Holocene, impacting global sea levels. This Review discusses these pre-industrial Holocene changes and their drivers, as well as their relevance for current and future perturbations to the AIS. See Jones et al.
Image: Richard. S. Jones. Cover design: Carl Conway.
An article in Geochemistry, Geophysics, Geosystems finds that chlorite- and serpentine-rich assemblages are most likely to control the frictional properties at subduction zone plate interfaces.
An article in Nature Climate Change reports that emigration will reduce by 10–35% in the lowest income groups, exposing them to subsequent climate impacts.
The Antarctic Ice Sheet (AIS) underwent dramatic changes over the Holocene, impacting global sea levels. In this Review, Jones et al. discuss changes in this ice sheet during the pre-industrial Holocene. The drivers behind these past changes are explored, as well as their relevance for current and future changes in the AIS.
Black carbon is produced by wildfire and fossil fuel burning, and persists in the environment over centuries to millennia. This Review describes black carbon sources and budgets, discusses its transport along the land-to-ocean continuum and highlights its enigmatic cycling in the ocean.
Phase transitions in the mantle transition zone could affect material and heat exchange between the upper and lower mantle. This Review discusses how compositional heterogeneity affects mantle convection based on seismic observations, plausible mantle compositions and model predictions.