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Intertidal deposition occurs in areas between the high and low tide marks, where the rocks are periodically exposed and submerged by the tides. Supratidal deposition takes place above the normal tidal range, where rocks are exposed to the atmosphere and occasional seawater splashes during storm surges. Subtidal deposition occurs within the normal tidal range, where rocks are constantly submerged.

Carbonate rocks formed through intertidal and supratidal deposition may display the following features: 1. Algal laminations or microbial mats: These formations indicate the presence of organisms that thrive in the intertidal or supratidal zone. 2. Mudcracks: As rocks are exposed to sunlight and air during low tide, the sediments can dry out and form mudcracks. 3. Salinity-related minerals: Evaporation in these environments can cause the precipitation of evaporite minerals such as gypsum and anhydrite. 4. Fossils or traces of organisms: The presence of fossils or traces of organisms that thrive in the intertidal or supratidal zone, such as crustaceans, gastropods, or bivalves. 5. Dolomite or dedolomite: These minerals can precipitate in an environment with fluctuating salinity levels.

Carbonate rocks formed through subtidal deposition may display the following features: 1. Fossils of marine organisms: Subtidal environments usually contain a variety of marine life, including corals, echinoderms, and foraminifera, which can leave their remains in the rock. 2. Cross-bedding, ripples, or dunes: These sedimentary structures indicate the influence of currents, waves, or other water movement in a subtidal environment. 3. In-situ corals or reefs: The presence of in-situ corals or reef structures in the rock indicates a subtidal environment where the organisms could grow undisturbed. 4. Lime mud, peloids, or ooids: These small sedimentary grains or aggregates may form in a subtidal environment due to the precipitation of calcium carbonate in the water column or the action of waves and currents. By distinguishing the features associated with intertidal or supratidal deposition and those related to subtidal deposition in carbonate rocks, it becomes possible to determine the depositional environment in which these rocks were formed.