“…We know this due to several Late Jurassic formations that yielded significant ichthyosaur materials. These are primarily Kimmeridge Clay Formation of England and France (Hulke, 1871; Mansell-Pleydell, 1890; Sauvage, 1911; Delair, 1960, 1986; McGowan, 1976, 1997; Grange et al, 1996; Etches & Clarke, 1999; Moon & Kirton, 2016), the Solnhofen Formation of Germany (Wagner, 1852, 1853; Meyer, 1864; Bauer, 1898; Bardet & Fernández, 2000), the Vaca Muerta Formation of Argentina (Fernández, 1997, 2000, 2007a, 2007b; Gasparini, Spalletti & De La Fuente, 1997, Gasparini et al, 2015), the Agardhfjellet Formation of Svalbard, Norway (Angst et al, 2010; Druckenmiller et al, 2012; Roberts et al, 2014; Delsett et al, 2016, 2017) and a number of formations of the Volgian (Tithonian) age in European Russia (Kabanov, 1959; Efimov, 1998, 1999a, 1999b; Arkhangelsky, 1997, 1998, 2000, 2001a, 2001b; Zverkov, Arkhangelsky & Stenshin, 2015; Zverkov et al, 2015; Zverkov & Efimov, 2019). Still our knowledge of the Late Jurassic ichthyosaurs is non-uniform: some taxa are quite well known owing to relatively complete and well-preserved specimens ( Ophthalmosaurus Seeley, 1874; Grendelius McGowan, 1976; Caypullisaurus Fernández, 1997; Aegirosaurus Bardet & Fernández, 2000; Undorosaurus Efimov, 1999b), whereas others are poorly known from only a small number of largely incomplete and/or poorly preserved specimens (e.g., Nannopterygius Huene, 1922, Brachypterygius Huene, 1922, and Arthropterygius Maxwell, 2010).…”