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The sample yielded a conventional 14C age of 380 ± 60 Radiocarbon Years BP with a ∆ 13C of -29.6 relative to PDB-1 (Beta Analytic sample #Beta-86999, November 1995). That carbon was analyzed with extended counting to enhance precision. After mechanical and chemical pre-treatment, less than one gram of suitable carbon remained. Why the Audubon’s shearwater was exclusively favored in these feasts is not known.” The charcoal and bone samples were collected from a 2-m- wide flowstone ledge on the eastern side of the chamber, and the charcoal was submitted to Beta Analytic for radiocarbon analysis (sample #Beta-86999, November 1995). Stream Drama CD R18, a playlist by ~Angel~ from desktop or your mobile device. Stream R18 Drama Cd Favs, a playlist by oshirumarimaru from desktop or your mobile device. Kaye (1959: 166) further suggested, based upon the location and character- istic of the deposit, “the bird bones constitute a midden built with the refuse of many feasts, probably during Indian occu- pancy of the cave, and that the charcoal represents scattered ashes from the fires. This identification is consistent with bird bones collected during the 1995 sampling.
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The abundance of charcoal fragments within the cave, it seems to the writer, cannot be ascribed to natural causes.” Kaye (1959) reported these bones to be exclusively those of Audubon’s shearwater (Puffinus lherminieri). Kaye (1959: 166) first described this deposit: “Bones of what must be literally thousands of birds are contained in the floor deposit of the chamber and all of them are more or less inti- mately mixed with small charcoal fragments. The sample site itself consists of a 2.5 to 7.5 cm layer of mixed charcoal, bird bone, and silt, atop a 15 cm bed of yellowish silt. This chamber is located in complete darkness several hundred meters, and around several bends, from the nearest entrance. The sample area is located in the distal end of a 40 m long by 5 m wide chamber. Charcoal fragments and bird bone samples were collected from a mixed charcoal and bone deposit in a back chamber of Cueva Negra, Isla de Mona, Puerto Rico on August 1995 for identification and radiocarbon dating. This time period encompasses the first contact between Taino population and Europeans, and the subsequent removal of the last of the Taino from the island to Puerto Rico in 1578. Radiocarbon dating yielded a conventional 14C age of 380 ☖0 Radiocarbon Years before present.Ĭonsidering the standard deviation in the 14C data, the range in pos- sible calendar dates is from 1480 to 1655 AD. FRANK Department of Geology and Geophysics, University of Minnesota, Minneapolis, MN 55455 USA Charcoal fragments were collected from a mixed charcoal and bone deposit from a chamber in Cueva Negra, Isla de Mona Puerto Rico. A RADIOCARBON DATE OF 380 ☖0 BP FOR A TAINO SITE, CUEVA NEGRA, ISLA DE MONA, PUERTO RICO EDWARD F. Journal of Cave and Karst Studies 60(2): 101-102. Frank-A Radiocarbon Date of 380 ☖0BP for a Taino Site, Cueva Negra, Isla de Mona, Puerto Rico.
Frank Journal of Cave and Karst Studies, August 1998