71Somali Boidae and Pythonidae
in the Palaeogene [Cenozoic era] of both Old and New World, but fossil nds of the
living genus Eryx have never been reported from pre-Miocene times» perhaps with
the only exception of a skull of Crythiosaurus from the Mongolian Oligocene (Pal-
aeogene period), originally described as an amphisbaenid. True Eryx are known to
have been widely distributed in the Mediterranean and Black Sea areas between the
end of the lower Miocene and the late Pliocene (Neogene period). Messinian (late
Miocene) remnants, probably belonging to Eryx, have been described from near Alba
(Piedmont) by CAVALLO et al. (1993). The available fossil remains suggest that most
representatives of Eryx inhabiting Europe in the past were similar to the recent Asi-
atic members of the genus, except for one or two taxa from S Spain (Eryx primitivus
Szyndlar & Schleich 1994, middle Pliocene; Eryx aff. primitivus, middle/late Pliocene)
belonging to the Afro-Arabian complex, displaying primitive conditions in their cau-
dal osteology and probably representing an early offshoot of a hypothetical ancestral
stock leading to the extant species of Eryx. According to HOLMAN (1998), E. jaculus
is only known from the Pleistocene (Quaternary period) of Europe [Greece: Chios Is.
(Middle Pleistocene) and Kos Is. (“Upper Quaternary”)]. For fossil erycine snakes see
also KLUGE (1993a) and RODRÍGUEZ-ROBLES et al. (1999).
Description. Size small to rather large: greatest adult total length from about
40 cm, e.g. in E. elegans (Gray 1849), to a little more than 1 m as in E. johnii and E
tataricus, according to SEUFER (2001). Head not or scarcely distinct from the neck;
body cylindrical, stout; tail short, thick, conical or terminating in a sharp point, not
or, very slightly prehensile. Eye small or very small, with vertical pupil. No labial
pits. Head covered with small, irregular, smooth scales (except on the snout); dor-
sals small, numerous, smooth or keeled; subcaudals entire, sometimes some of them
divided; anal single, only exceptionally divided. Mental groove present or absent. No
chin shields. Hemipenis extending to ventral 8 to 14 when retracted, feebly or not
bilobate, without papillae, ounced and calyculate, the sulcus spermaticus forked or
undivided. Skull and muscles: prefrontals widely separated; nasals broad posteriorly,
clearly longer than frontals; palatine mobile, strongly toothed, its choanal process
reduced; retractor arcus palatini present (palatine scarcely mobile, weakly toothed,
its choanal process large, and no retractor arcus palatini in the North American
Erycinae Lichanura and Charina). Maxillary and mandibular teeth numerous, solid,
ungrooved, arranged in an anonodont and scaphiodont set (only the rst tooth some-
times a little shorter than the second). ALEXANDER & GANS (1966) found in E. colubri-
nus (n = 2), E. conicus (Schneider 1801) (n = 1) and E. jaculus (n = 2) the following
combined data: 168(?)-188 (ventral) and 254-278 (dorsal) body scale rows, ca 18-28
(ventral) and ca 18-28 (dorsal) caudal scale rows, 174-190 body vertebrae, 19-29 tail
vertebrae; the dermal-vertebral ratios of the three species turned out to be: body (ven-
tral 1:1; dorsal 1.4:1), caudal (ventral 1:1; dorsal 1.0-1.1:1).
Biology (see also Eryx colubrinus, Biology). Terrestrial, fossorial or semifos-
sorial, predominantly crepuscular and nocturnal snakes inhabiting arid and sub-
arid regions, usually not strictly linked to sand substrata, notwithstanding their
common name; they are able to disappear very quickly into the sand where they
creep just beneath the surface. According to VAN WOERKOM (1987: 49) «a furrow
along the middle of the back and, sometimes, strongly keeled scales prevent the
sand from sliding off their backs and showing their presence». Sand boas may be
found above the ground during the night or at twilight, hiding by day under stones,
in soil crevices, in burrows or under the sand; occasionally they are active on the