GLACIOEUSTATIC SEA LEVEL, GAS HYDRATE STABILITY, AND A LATE PLEISTOCENE SHELF-EDGE DELTA IN THE NORTHEAST GULF OF MEXICO: ENVIRONMENTAL FACTORS CONTROLLING SHELF-MARGIN STABILITY AND THE PROBABLE RECORD OF PRE-CLOVIS MAN IN NORTH AMERICA
Of importance from a paleo-anthropological perspective, is the period during which the Lagniappe delta establishes attractive coastal environments at the shelf-edge, i.e., shortly before and during the last glacial maximum. This is a time for testing outer continental shelf habitats for evidence of pre-Clovis populations in North America. The oldest Clovis corrected radiocarbon dates are about 13 ka BP. Possible pre-Clovis artifacts have been reported in the U.S. and elsewhere in the Americas.
Drowned anthropogenic shell middens are observed along the Louisiana coast. Middens in bays and lakes have been detected by side-scan sonar and divers. We suggest that shell middens are the most easily identified targets for studying early humans in drowned deltaic paleo-environments of the outer continental shelf that have not been disrupted by hydrate dissociation. Stable shelf-edge delta systems of the Gulf of Mexico, like the Lagniappe, provide optimal settings in which to search for evidence of early man.