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The Middle Triassic of the Tethyan domain contains heavily bioturbated carbonates known as vermicular limestones. In the Tatricum domain in the Tatra Mountains, Western Carpathians, these were deposited on a restricted carbonate ramp below the fair-weather wave base. Sedimentological and geochemical evidence points to a hypersaline depositional environment. The vermicular limestones contain an impoverished...
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