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 …

The carbon cycle of the coastal ocean is a dynamic component of the global carbon budget.
But the diverse sources and sinks of carbon and their complex interactions in these waters …

For the estimation of global karst carbon sink, a few conventional methods usually require
the parameters that are difficult to measure, resulting in the big cost. Moreover, under the …

Chemical weathering is an integral part of both the rock and carbon cycles and is being
affected by changes in land use, particularly as a result of agricultural practices such as …

The nine editions of Stable Isotope Geochemistry have appeared over a time span of nearly
50 years. The first edition (1973) appeared as a slim book of 135 pages. Due to the rapid …

The oxidation of organic carbon contained within sedimentary rocks (“petrogenic” carbon, or
hereafter OCpetro) emits nearly as much CO2 as is released by volcanism, thereby playing …

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 …

The biogeochemical sulfur cycle is intimately linked to the cycles of carbon, iron, and
oxygen, and plays an important role in global climate via weathering reactions and aerosols …

The observed stability of Earth's climate over millions of years is thought to depend on the
rate of carbon dioxide (CO2) release from the solid Earth being balanced by the rate of CO2 …

The long-term cooling, decline in the partial pressure of carbon dioxide, and the
establishment of permanent polar ice sheets during the Neogene period, have frequently …