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Meandrina sp. Time Place In Our Region
Description In the Coyote Mountains of eastern San Diego County fossil remains of these coral are usually discovered as fragmentary coral heads. However, occasionally small complete patches of fossil reef are found, still attached to the ancient bedrock of the sea floor. Species related to these two species of fossil corals occur today only in the Caribbean Sea. For example, Melandrina bowersi is an extinct species, but Melandrina labyrinthiformis, found today in the Caribbean, looks very similar to it. In the same way, Dichocoenia merriami is an extinct species, but has many similarities to D. stokesi which occurs in the Caribbean. How can we explain this phenomenon? During the late Miocene and early Pliocene, the eastern part of the Pacific Ocean, the Gulf of Mexico and the Caribbean Sea were all linked together to form one continuous marine environment, since the land barrier of the Isthmus of Panama did not yet exist. This means that marine invertebrates such as corals, which have larval forms that occur in the plankton and move with ocean currents, could easily spread from off the coast of California to the Caribbean Sea. With elevation of the Isthmus in the mid-Pliocene the brain corals became extinct in the Pacific while surviving in the Caribbean. Suggested Reading
Text: Margaret Dykens and Lynett Gillette Search | Site Index | Home | Museum Guide (PDF) © San Diego Natural History Museum |
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