The Kulau Limestone is part of Gondwana Megasequnce. The Kulau limestone contain mostly dominated by Fusulinid, Crinoid, and Bryzoa part of the permian in age.
Fusulinids were elements of warm-water photozoan fauna during the Permian and are absent from cold-water carbonates composed of heterozoan facies ( James, 1997)
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