“…Unfortunately, the holotype specimen CORD-PZ 82, described as a "Fragmenta alae Hymenopterorum" by Kurtz (1921), has not been located in Rösler et al, 1981;Martins-Neto, 1996;Beckly, 1998 ;Huguet et al, 2002;Prokop et al, 2023 Petromantis rieki Pinto (Fig. Tillyard, 1928;Fraser, 1957;Nel et al, 2012; Wieland, 1925;Tillyard, 1925Tillyard, , 1926Carpenter, 1992 Marquat, 1991;Storozhenko, 1998;Aristov et al, 2006 Dysmorphoptiloides acostai Pinto (1994Pinto ( , 1996Pinto ( , 1999 The consensus for the Bajo de Véliz Formation age ranges from the latest Carboniferous to the earliest Permian (Gutiérrez, 2006;Césari & Chiesa, 2017). Pinto (1995) argued a Late Carboniferous age on the basis that many insect genera and/or species at the Bajo de Véliz belonged to families exclusively found in Carboniferous strata from the USA, France, and Russia (Pinto & Ornellas, 1978, 1980Pinto & Hünicken, 1980;Pinto & Adami-Rodrigues, 1997).…”