Previous studies on enamel microstructure in Ornithischia have focused on derived lineages of this clade based on species
from the northern hemisphere. Here we describe the enamel microstructure of Manidens condorensis from the late Early
Jurassic of Argentina that belongs to Heterodontosauridae (interpreted as the basal-most clade of Ornithischia). Enamel
microstructure in the cheek teeth lacks a basal unit layer, presents incipient divergent crystallite as the dominant enamel
type and parallel crystallite enamel type (with or without incrementing lines). Enamel of maxillary and dentary teeth
differs from each other in enamel distribution (asymmetric vs. symmetric), structure (presence vs. absence of tubules, and
less vs. more abundant parallel crystallite enamel with incrementing lines) and ordering (regular ordering of enamel types
vs. in patches). The enamel microstructure of Manidens is the simplest of all known Ornithischia, and is more similar to
that of the sauropodomorph Plateosaurus than to the one reported for the basal theropod Coelophysis. Similarities within
Ornithischia are present with pachycephalosaurids and, to a lesser extent, with ankylosaurs. Phylogenetic optimization of
enamel characters in Ornithischia allows the inference of new ancestral states for the internal nodes of the major lineages
and to highlight evolutionary transformations: (i) absence of a basal unit layer and presence of parallel crystallite and
incipient divergent columnar enamel as the ancestral state for Ornithischia; (ii) the shared presence of incipient divergent
columnar units or poorly developed divergent columnar enamel in Pachycephalosauridae and Thyreophora represents a
retention of the plesiomorphic ornithischian condition; (iii) the wavy enamel of Dryomorpha evolved from the ancestral
incipient divergent columnar units present in Ornithopoda and; (iv) enamel thickness and asymmetry has independently
evolved at least four times in Ornithischia.
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