18 
Janet A. Roth and Joshua Laerm 
ments; ChM.PV2357-2358, ChM.PV2452, three lower cheek tooth frag- 
ments; HS.E-33A, HS.A-82, two right ulnae; HS.E-27, distal epiphyses of 
two radii, ChM.PV2321, right tibia; ChM.PV2413, left tibia and portion 
of shaft; ChM.PV2329, right pelvic fragment, including acetabulum; 
ChM.PV2322, right astragalus; ChM.PV2745, calcaneal fragment; 
ChM.PV2372, 2328, ChM.PV2444, three metapodial fragments; 
ChM.PV2326, fragment of proximal part of metapodial; ChM.GPV1978, 
metapodial; HS.E-25, two phalanges; ChM.PV2323-2325, ChM.PV2443, 
four phalanges; UGV1 15, LM 1 or LM 2 ; UGV1 16, RP 3 or RP 4 ; UGV1 17, 
RM 1 , UGV118, LP 2 ; UGV119, RP 3 or RP 4 ; UGV124, buccal section of 
LM 1 ; UGV125, RP 3 or RP 4 ; UGV126, lingual section of RM 1 UGV127, 
LP 3 or LP 4 ; UGV134, LM 1 or LM 2 ; UGV113, RM 3 ; UGV114, LP 2 ; 
UGV120, RM, or RM,; UGV121, LM, UGV122, LM 1 , or LM 2 ; 
UGV123, LM 3 ; UGV122, LM, or LM 2 ; UGV123, LM 3 ; UGV128, LM, 
or LM 2 ; UGV129, LP 3 or LP 4 ; UGV130, RM, or RM 2 ; UGV160, 
glenoid region of scapula. 
Remarks. — The possibility that some of the equid remains are of Re- 
cent origin must be considered since E. caballus is a modern inhabitant of 
Edisto Island and permineralization is known to take place at a com- 
paratively rapid rate on the island (O’Kelley 1976). Although the anti- 
quity of the Equus material cannot be proven absolutely at this time, 
three factors indicate that at least most of the remains are Pleistocene. 
First, the very dark color and strong permineralization of some of the 
fossils is comparable to that of material from species that definitely 
became extinct during the Pleistocene. Second, the relative abundance of 
horse material in the fauna would suggest numerous individuals occur- 
ring over a long period of time. Finally, Equus is an expected member of 
the Pleistocene fauna at Edisto Island. 
Family Tapiridae 
Tapirus Brisson sp. indet. — tapir 
Material . — ChM.PV2362, symphyseal fragment of mandible with 
fragmentary root of RI 2 ; ChM.PV2363, right upper molar fragment; 
ChM.PV2364, deciduous RM 1 ; ChM.PV2365, upper molar fragment; 
HS.E-68, carpal element; HS.Q, right upper molar fragment; HS.R, right 
molar; UGV150, LM,; from the private collection of W. M. Wagner, left 
mandible with P 3 -M 3 present. 
Remarks.— The incomplete nature of most of the specimens prevents 
specific determination. 
Order Artiodactyla 
Family Tayassuidae 
Mylohyus cf. M. fossilis (Leidy) — long nosed peccary 
Material. — ChM.PV2414, symphyseal mandibular fragment with 
roots of RI,, RI 2 , RC, LI,, IC; ChM.PV2499, LM,; from the private 
