“…Both specimens of N. ignaciobritoi come from the upper part of the Jiufotang Formation (see Wu et al, 2018), while the holotype of N. luei comes from the lowermost part of the Jiufotang Formation. This stratigraphic distribution might be suggestive of an anagenetic link between the two species, similar to the case of Pteranodon longiceps (from the upper Smoky Hill Chalk) and Pteranodon sternbergi (from the lower Smoky Hill Chalk) according to Bennett (1994), but see taxonomic controversies (Kellner, 2010, 2017; Martin-Silverstone et al, 2017; Acorn et al, 2017). The same has been speculated as a possible explanation for the occurrence of multiple species of Anhanguera (Pinheiro & Rodrigues, 2017), Thalassodromeus and Tupuxuara (Pêgas, Costa & Kellner, 2018) in the Romualdo Formation.…”