Nature Geoscience, Published online: 17 June 2026; doi:10.1038/s41561-026-02018-w
Heat flux across the core–mantle boundary is laterally variable, and heat may flow into the core beneath hot piles of dense material such as large low-shear-wave-velocity provinces, according to mantle thermochemical convection models…
Source: Nature Geoscience | Springer Nature Limited
Nature Geoscience | Springer Nature Limited
- Negative core–mantle boundary heat flux beneath low-shear-wave-velocity provinces
- Enhanced marine burial of terrestrial organic carbon through the Palaeocene–Eocene Thermal Maximum
- Vigorous mantle convection triggered the Cretaceous Pacific large igneous provinces
- Observed stratospheric mean age decrease consistent with circulation acceleration
- The pace of stratospheric circulation
- Major contribution of anaplerosis to inorganic carbon fixation in the dark ocean
- Tracking hydrogen migration in iron under Earth’s core conditions
- Large CO<sub>2</sub> seeps and hydrate field on the seafloor offshore Mayotte Island
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