“…For instance, most taxa (sensu Schoch, 2019) are of early Permian age and reveal a remarkable diversity that suggests a much earlier diversification sometime in the Carboniferous (Schoch and Milner, 2014). Upper Carboniferous deposits in the Czech Republic (Nýřany, Broumov), Germany (Stützerbach in the Thuringian forest), France (Montceau-les-Mines in Sâone et Loire), and the United States (Linton and Five Points in Ohio, Mazon Creek in Illinois, Hamilton Quarry and Garnett in Kansas) have yielded a diverse record of dissorophoid material that documents the presence of most major clades within the group: the micromelerpetids Limnogyrinus elegans Fritsch, 1881 and Nyranerpeton amilneri Werneburg, 2012 (Werneburg, 1994(Werneburg, , 2012Schoch and Witzmann, 2018); the branchiosaurids Branchiosaurus and Apateon (Boy, 1987;Werneburg, 2012); the trematopids Actiobates peabodyi Eaton, 1973, Anconastes vesperus Berman et al, 1987, Fedexia striegeli Berman et al, 2010, Mordex calliprepes Steen, 1938, and Mattauschia laticeps (Fritsch, 1881) (Berman et al, 1987(Berman et al, , 2010Werneburg, 2012;Milner, 2019;Gee and Reisz, 2020a); and the amphibamiforms Platyrhinops lyelli (Wyman, 1858) (Hook and Baird, 1984;Clack and Milner, 2010), Amphibamus grandiceps (Watson, 1940;Milner, 1982), and Eoscopus lockardi Daly, 1994. As recently outlined (Schoch, 2019), major phylogenetic questions remain regarding the Dissorophoidea that range from their early diversification, to the position of branchiosaurids and lissamphibians, to the early evolution of olsoniform and amphibamiform branches (Boy, 1981;Anderson et al, 2008a, b;Schoch, 2012Schoch, , 2013Maddin et al, 2013). It is clear that in addition to applying new preparation techniques to existing material, the discovery of new specimens will play an important role in resolving these uncerta...…”