New Caribbean Locality for the Extinct Great White Shark Carcharodon
NOTES 317 Koopman, K. F., and E. E. Williams. 1951. Fossil Chi- of low relief (< 8 m) and the highlands, a karst plateau roptera collected by H. E. Anthony in Jamaica, rising to roughly 40 m above sea level. The highlands, 1919-1920. Amer. Mus. Nov. 1519:1-29. specifically the Highlands Formation (Brasier and MacPhee, R. D. E. 1984. Quaternary mammal localities Donahue, 1985), are composed of horizontally bedded and Heptaxodontid rodents of Jamaica. Amer. reef limestones of Pliocene age (Watters et al., 1992). Mus. Nov. 2803:1-34. Darby Sink (also known as Darby Cave and Darby’s MacPhee, R. D. E. 1997. Vertebrate paleontology of Cave; 17°38’N, 61°50’W; UTM 299 527) is the largest Jamaican caves. In A. G. Fincham (ed.), Jamaica and best known of a series of distinctive, sheer-walled, Underground: The caves, sinkholes and underground karst collapse features that open from the highlands plateau. Darby Sink is approximately 25 m deep, rivers of the island. 2nd ed. University of West Indies undercut along its northern margin, and large enough Press, Kingston. 447 p. (~ 5400 m2) to support a mesophyllic forest. MacPhee, R. D. E., and C. Flemming. In press. Requiem Carcharodon is represented by a single upper tooth aeternum: The last 500 years of mammalian species (Fig. 1) which we extracted from the eroding Pliocene extinctions. In R. D. E. MacPhee (ed.), Extinctions in limestone wall, some six meters above the floor at the Near Time: Context, Causes, and Consequences. Ple- northern end of Darby Sink. Much of the tooth is miss- num Press, New York.
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