Throughout Earth's history, CO2 is thought to have exerted a fundamental control on
environmental change. Here we review and revise CO2 reconstructions from boron isotopes …

Mountain building in the Andes, the longest continental mountain range on Earth, started in
the Late Cretaceous but was highly diachronous. Reconstructing the timing of surface uplift …

Mountain belts modulate denudation flux and hydrologic processes and are thus
fundamental to nutrient cycling on Earth's surface. We used europium anomalies in detrital …

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 …

How well do deep-sea sedimentary archives track erosion in upland sources, driven by
climatic change or tectonic forcing? Located on the western edge of South Asian monsoon …

During evolution of the South Sandwich subduction zone, which has consumed South
American Plate oceanic lithosphere, somehow continental crust of both the South American …

Sea level and deep-sea temperature variations are key indicators of global climate changes.
For continuous records over millions of years, deep-sea carbonate microfossil–based δ18O …

Earth's plate-tectonic activity regulates the carbon cycle and, hence, climate, via volcanic
outgassing and silicate-rock weathering. Mountain building, arc–continent collisions and …

Significant advances in understanding and predicting freshwater algal bloom dynamics
have emerged in response to both increased occurrence and financial burden of nuisance …

Clay adsorption is a critical process responsible for the mobilization and cycling of
potassium (K) on Earth's surface. Recent studies emphasized the potential of using stable K …