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As millions of years passed, evolution turned the ocean into a factory for carbonates. Creatures like corals, clams, and microscopic plankton (coccolithophores) learned to extract minerals from the seawater to grow shells and skeletons.
Warm Water: Most carbonate-producing organisms thrive in tropical to subtropical climates (30 degrees north or south of the equator).Shallow Depth: Photosynthetic organisms, such as green algae and symbiotic corals, require light, limiting major production to the photic zone (usually less than 100 meters deep).Clear Water: High turbidity from clay or silt clogs the feeding mechanisms of carbonate producers and blocks sunlight.Salinity: Most carbonate producers require normal marine salinity; extreme fluctuations can kill the "factory." Depositional Models and Facies origin of carbonate sedimentary rocks pdf extra quality
