Several recent studies (Estes et al., 1988; Schwenk, 1988; Cooper, 1997; Lee, 1998; Lee and Caldwell, 2000) have suggested that snakes are related to anguimorph lizards and, in particular, are nested within varanoids. However, there are characters that contradict this arrangement. ror instance, the teeth of all varanoid lizards exhibit a distinctive infolding of dentine and enamel near the base of the tooth crown. This results in a characteristic appearance, with regular vertical grooves and ridges around the entire circumference of the tooth base (Bullet, 1942). The occurrence of this has previously been interpreted as a derived character uniting varanoid lizards as a monophyletic group, to the exclusion of other squamates such as snakes (Pregill et al., 1986; Estes et al., 1988; Lee, 1998). It characterizes all extant varanoid lizards (Varanus, Lanthanotus, and Heloderma) and extinct terrestrial forms such as Estesia, Until recently, plicidentine has not been observed in nonvaranoid lizards, apart from a weak development in some extinct anguids and necrosaurids, which are closely related to varanoids (Estes et al., 1988). It is also absent in amphisbaenians and has been regarded as absent in all primitive living snakes (e.g., Estes et al., 1988). However, an enigmatic Eocene snake (Archaeophis) and some advanced snakes (caenophidians) possess externally fluted or grooved teeth, which are superficially similar to those of varanoids (Janensch, 1906; Bogert, 1943; Klauber, 1956; Vaeth et al., 1985). Nevertheless, despite these occurrences, the apparent absence of plicidentine in more basal snakes (scolecophidians and anilioids) has led to the widespread assumption that it is primitively absent in snakes. Here, we describe jaw fragments of two species of primitive snakes (from the extinct family Madtsoiidae) that clearly exhibit varanoid-like plicidentine. These observations, together with other recent studies of primitive snakes (see later), suggest that plicidentine