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 …

Microplastic (MP) pollution is of great environmental concern. MPs have been found all over
the Earth, including in the poles, which is indicative for the important threat they constitute …

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 …

Freshwater discharge from glaciers is increasing across the Arctic in response to
anthropogenic climate change, which raises questions about the potential downstream …

The secular trend of seawater strontium isotope ratio (87 Sr/86 Sr) reflects changes in the
relative contributions of continental versus mantle reservoirs to ocean composition, and …

Current understanding of the long-term carbon cycle posits that Earth's climate is stabilized
by a negative feedback involving CO 2 consumption by chemical weathering of silicate …

Water plays a critical role in erosion and sediment transport and this relationship is most
evident in the hyperarid Atacama Desert of Northern Chile, a region characterized by …

Climatic and non‐climatic factors affect the chemical weathering of silicate rocks, which in
turn affects the CO2 concentration in the atmosphere on a long‐term scale. However, the …

Carbonate rocks are a peculiarity of the Earth relative to other planets in the solar system.
Large terrestrial areas are covered by carbonate lithology, which actively reacts with …

Sedimentary rocks can release carbon dioxide (CO2) during the weathering of rock organic
carbon and sulfide minerals. This sedimentary carbon could act as a feedback on Earth's …