Mountain uplift and erosion have regulated the balance of carbon between Earth's interior
and atmosphere, where prior focus has been placed on the role of silicate mineral …

In the past several decades, field studies have shown that woody plants can access
substantial volumes of water from the pores and fractures of bedrock,–. If, like soil moisture …

Forests are increasingly threatened by climate-change-fuelled cycles of drought, dieback
and wildfires. However, for reasons that remain incompletely understood, some forest stands …

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 …

Soil biota generates carbon that exports vertically to the atmosphere (CO2) and transports
laterally to streams and rivers (dissolved organic and inorganic carbon, DOC and DIC) …

Bedrock vadose zone water storage (ie, rock moisture) dynamics are rarely observed but
potentially key to understanding drought responses. Exploiting a borehole network at a …

Climate influences near-surface biogeochemical processes and thereby determines the
partitioning of carbon dioxide (CO2) in shale, and yet the controls on carbon (C) weathering …

The oxidation of organic carbon in sedimentary bedrock (petrogenic OC, OC petro) is
increasingly recognized as a potential source of CO 2 to the atmosphere. Recent studies …

The evasion of CO2 from inland waters, a major carbon source to the atmosphere, depends
on dissolved inorganic carbon (DIC) concentrations. Our understanding of DIC dynamics …

Dissolved organic and inorganic carbon (DOC and DIC) influence water quality, ecosystem
health, and carbon cycling. Dissolved carbon species are produced by biogeochemical …