Carbonate geochemistry theories

Carbonate geochemistry studies the chemical processes involving carbonate minerals, primarily composed of carbon and oxygen, like limestone and marble. These processes play a key role in the carbon cycle, influencing climate and ecosystems. Carbonates can form through biological activity (like shell-building organisms) or chemical reactions in water. Changes in pH and temperature can affect how carbonates dissolve or precipitate, impacting water quality and the stability of sediments. Understanding these processes helps scientists predict environmental changes, such as ocean acidification, and assess geological formations relevant for resources like oil and gas.