The "Warm Water Model" is the standard for understanding ancient carbonates. In tropical, shallow, agitated waters, CO₂ is degassed, and evaporation is high. This environment favors the precipitation of aragonite and high-magnesium calcite (HMC), which are metastable polymorphs of calcium carbonate.
Carbonate sediments are highly unstable chemically. The transformation of loose sediment into rock (lithification) occurs through diagenetic pathways driven by pore-water chemistry. origin of carbonate sedimentary rocks pdf extra quality
Carbonate sediments are generated within the depositional basin rather than transported into it. The source of this sediment is termed the "Carbonate Factory." Three primary factories dominate the geologic record. The Origin of Carbonate Sedimentary Rocks: A Story