Guangxi Natural History Museum, Zoology collectionsRecent molecular divergence estimates (e.g., Jones et al., 2013) place the origin of Lepidosauria in the Early Triassic (~240-250 million years ago [Ma]) and that of Squamata in the Early Jurassic (~193 Ma). However, most lepidosaurs are small and this limits both the potential for their skeletons to be preserved after death, and the chances of recovering their fossils. As a result, the earliest stages of lepidosaurian history and diversification are poorly documented. The lepidosaurian stem is represented by a small number of Triassic and Jurassic genera, most of which represent survivors of earlier originating lineages. These stem-taxa are grouped with lepidosaurs into a more inclusive clade, Lepidosauromorpha. The position of the marine Sauropterygia (nothosaurs, plesiosaurs, placodonts, pliosaurs) and Ichthyosauria in relation to Lepidosauromorpha or Archosauromorpha remains unresolved (e.g., Jiang et al., 2014;Motani et al., 2015), and these taxa are covered in Chapter 8 by Reisz, Müller, Sobral, Scheyer & Neenan. Currently, the first recorded crown-group lepidosaurs are all rhynchocephalians, dating from the Middle Triassic onward (Jones et al., 2013). The first uncontentious squamate fossils are from the Middle Jurassic (e.g., Evans, 1994Evans, , 1998Evans & Jones, 2010), but these are both rare and mostly fragmentary. The squamate record improves substantially from the Cretaceous onward, with the first records of specialised marine lizards (Mosasauria) and the first unambiguous snakes in the mid-Cretaceous, and the first amphisbaenians in the Palaeocene.