Abstract

The reptilian clade Squamata is defined primarily by osteological synapomorphies, few of which are entirely unambiguous. Studies of developing squamate eggs have revealed a uniquely specialized feature not known to occur in any other amniotes. This feature-the yolk cleft/isolated yolk mass complex-lines the ventral hemisphere of the egg. During its formation, extraembryonic mesoderm penetrates the yolk and an exocoelom (the yolk cleft [YC]) forms in association with it, cutting off a thin segment of yolk (the "isolated yolk mass" [IYM]) from the main body of the yolk. The YC-IYM complex has been observed and described in more than 65 squamate species in 12 families. In viviparous species, it contributes to the "omphaloplacenta," a type of yolk sac placenta unique to squamates. The only squamates known to lack the IYM are a few highly placentotrophic skinks with minuscule eggs, viviparous species in which it clearly has been lost. Given its absence in mammals, chelonians, crocodylians, and birds, the YC-IYM complex warrants recognition as a developmental synapomorphy of the squamate clade. As in extant viviparous lizards and snakes, the YC-IYM complex presumably contributed to the placenta of extinct viviparous squamates.

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