Oxidative weathering of pyrite consumes O2, generates dissolved sulfate (SO42−) and acidifies carbonates to release CO2 to the ocean-atmosphere system. Mountain belts are hotspots of chemical weatheri...

Meteoric water circulation is more prevalent along active fault zones, but its maximum depth is controlled by the fault's deformation style Variations in topography, orographic precipitation, and...

The burial of terrestrially derived organic carbon in coastal marine sediments greatly increased during the Palaeocene–Eocene Thermal Maximum, probably helping to draw down a large portion of carbon r...

Permafrost thaw on the Qinghai–Tibet Plateau increases rock-weathering rates while reducing river CO2 emissions, suggesting geological carbon fluxes may eventually outpace thaw-driven emissions.

Meltwaters from mountain glaciers and ice sheets contain essential micronutrients like zinc, cobalt, nickel, cadmium, and copper, which can fertilize nutrient-limited ecosystems but also raise metal t...

We propose that one of the largest known bioconstructions (the Monte Zenone bioherm) in the Southern Alps, northern Italy, and its growth on a tilted and drowned platform block of the Norian Dolomia ...

Modern pyrite burial in seafloor sediments exceeds pyrite oxidation on land, indicating that the sulfur cycle is out of balance, and acts to increase atmospheric oxygen levels, according to a diagenet...

Modern pyrite burial in seafloor sediments exceeds pyrite oxidation on land, indicating that the sulfur cycle is out of balance, and acts to increase atmospheric oxygen levels, according to a diagenet...