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 links between the weathering of silicate minerals, the global carbon cycle and climate
change are complex and involve a whole range of often inter-related tectonic, climatic …

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 …

Revision of the GEOCARB model (Berner, 1991, 1994) for paleolevels of atmospheric CO~
2~, has been made with emphasis on factors affecting CO~ 2~ uptake by continental …

The Miocene Climatic Optimum (MCO) from~ 17 to 14 million years ago (Ma) represents an
enigmatic reversal in Cenozoic cooling. A synthesis of marine paleotemperature records …

The term" carbon cycle" is normally thought to mean those processes that govern the
present-day transfer of carbon between life, the atmosphere, and the oceans. This book …

This paper describes the ways in which the major rock-forming primary minerals (olivine,
pyroxenes, amphiboles, feldspars, micas and chlorites) break down during weathering, the …

Монография обобщает результаты оригинальных исследований автора, а также
обширные опубликованные материалы о применении лишайников в мониторинге …

Because there remains a lack of knowledge about the spatially explicit distribution of
chemical weathering rates at the global scale, a model that considers prominent first-order …

CO2-consumption by chemical weathering of silicates and resulting silicate/carbonate
weathering ratios influences long-term climate changes. However, little is known of the …