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Modern animals are classified into between 30 and 35 phyla: all major modern phyla were present at the beginning of the Cambrian, along with a great variety of now-extinct phyla recorded in the Burgess Shale (Cambrian) in Canada.
Class Anthozoa likely appeared in the Precambrian, though the fossil record is sparse and inconclusive. Several soft-bodied Vendian animals are now thought to be early Anthozoa. Sequence analyses also supports the theory that Anthozoa are the first branch of the Phylum Cnidaria (Bridge et al.1992). Only a few CaCO3-secreting corals or coral-like organisms are known from the early Cambrian (e.g., Sorauf and Savarese 1995), and the Cothoniida, are known from the middle Cambrian.nthozoans do not have a medusa stage in their development as do other cnidarians. Rather, they release sperm and eggs that form a planula that attaches to a surface on which they grow. A coral head contains thousands of genetically identical polyps, each typically a few millimeters in diameter.