Mountain building results in high erosion rates and the interaction of rocks with the
atmosphere, water and life. Carbon transfers that result from increased erosion could control …

Physical and biogeochemical heterogeneity dramatically impacts fluid flow and reactive
solute transport behaviors in geological formations across scales. From micro pores to …

Earth's climate may be stabilized over millennia by solubilization of atmospheric carbon
dioxide (CO2) as minerals weather, but the temperature sensitivity of this thermostat is …

Uplift and erosion modulate the carbon cycle over geologic timescales by exposing minerals
to chemical weathering. However, the erosion sensitivity of mineral weathering remains …

Silicate weathering as an important negative feedback can regulate the Earth's climate over
time, but much debate concerns its response strength to each climatic factor and its …

Globally, inland waters receive a significant but ill‐defined quantity of terrestrial carbon (C).
When summed, the contemporary estimates for the three possible fates of C in inland waters …

Silicate rock weathering maintains a stable and long‐term absorption of CO2. However, the
magnitude, spatial pattern, and evolution characteristics of global silicate rock weathering …

The remarkable complexity of soil and its importance to a wide range of ecosystem services
presents major challenges to the modeling of soil processes. Although major progress in soil …

Groundwater is important for energy and food security, human health and ecosystems. The
time since groundwater was recharged—or groundwater age—can be important for diverse …

The Palaeozoic evolution of land plants revolutionized river geomorphology. However, the
relationships between biotic forcing and channel dynamics are still debated and, as such …