“…There are only large, poorly calcified areas on the latero-ventral sides in modern representatives -the branchiostegites (Ng et al, 2008). The molting lines in these regions are clearly visible on the flanks or in ventral view in fossils ascribed to Homolodromioidea (e.g., Schweitzer and Feldmann, 2008;Klompmaker et al, 2011Klompmaker et al, , 2012Klompmaker et al, , 2016Klompmaker et al, , 2020Starzyk, 2013Starzyk, , 2015a, but they are rarely illustrated.…”