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 importance of carbonate weathering carbon sinks (CCSs) is almost equal to that of
vegetation photosynthesis in the global carbon cycle. However, CCSs have become …

Rivers integrate processes occurring throughout their watersheds and are therefore
sentinels of change across broad spatial scales. River chemistry also regulates ecosystem …

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 largest negative inorganic carbon isotope excursion in Earth's history, namely the
Ediacaran Shuram Excursion (SE), closely followed by early animal radiation, has been …

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 …

INTRODUCTION Oxidative weathering of pyrite, the most abundant sulfide mineral in Earth's
crust, is coupled to the biogeochemical cycles of sulfur, oxygen, carbon, and iron. Pyrite …

Global climate is thought to be modulated by the supply of minerals to Earth's surface.
Whereas silicate weathering removes carbon dioxide (CO2) from the atmosphere …

The Neoproterozoic era witnessed a succession of biological innovations that culminated in
diverse animal body plans and behaviours during the Ediacaran–Cambrian radiations …

The 540s, 1450s, and 1600s represent three of the five coldest decades in the Common Era
(CE). In each of these cases, the cause of these cold pulses has been attributed to large …