The first Permian Diaphanopterodea (Insecta, Megasecopteromorpha) from China Author Yang, Nan https://orcid.org/0009-0000-2687-3916 College of Life Sciences, Capital Normal University, 105 Xisanhuanbeilu, Haidian District, Beijing, China Author Cui, Yingying https://orcid.org/0009-0008-2544-2821 College of Life Sciences, South China Normal University, Guangzhou, China Author Xu, Ziqiang 0000-0002-2682-2550 College of Life Sciences, Capital Normal University, 105 Xisanhuanbeilu, Haidian District, Beijing, China Author Xu, Yanqi Geological Survey of Jiangsu Province, Jiangsu, China Author Ren, Dong 0000-0001-8660-0901 College of Life Sciences, Capital Normal University, 105 Xisanhuanbeilu, Haidian District, Beijing, China Author Béthoux, Olivier 0000-0002-3178-8967 CR 2 P (Centre de Recherche en Paléontologie – Paris), MNHN – CNRS – Sorbonne Université, Paris, France text Fossil Record 2024 2024-08-15 27 2 247 258 journal article 10.3897/fr.27.e128892 E93DEB3D-DFFF-4BE5-8B06-E79DB3F271F7 Family Parelmoidae Rohdendorf, 1962 Type genus. Parelmoa Carpenter, 1947 . Included genera. Diapha Kukalová-Peck, 1974 ; Elmodiapha Kukalová-Peck, 1974 ; Paradiapha Kukalová-Peck, 1974 ; Permelmoa Prokop & Nel, 2011 ; Permodiapha Kukalová-Peck, 1974 ; Permuralia Sinichenkova & Kukalová-Peck, 1997 ; Protodiapha Kukalová-Peck, 1974 ; Pseudelmoa Carpenter, 1947 ; Stenodiapha Kukalová-Peck, 1974 ; Sinoelmoa gen. nov. Commented diagnosis. ScP long, ending beyond the first fork of RP (plesiomorphy within Diaphanopterodea ); near wing base, shortly after its origin, CuA fused for some distance with, or running closely along, R + M (apomorphy; as currently documented, shared with all Diaphanopterodea except Sinodiaphidae , in which CuA is connected with M by a short cross-vein, and Diaphanopteridae , in which the connection of CuA and M is very brief); first cross-vein in the CuA – CuP area very short and oblique, with CuA displaying a clear inflexion at the point of connection with this cross-vein [also present in Diaphanopteridae , Carrizodiaphanoptera and, to some extent, Elmoidae (Fig. 3 ); possibly an apomorphy of the entire Diaphanopterodea – except for Sinodiaphidae , in which this state is primarily absent –, and with presumed secondary losses in various families, such as Martynoviidae ]; MP branched (plesiomorphy within Diaphanopterodea ); CuP with 1–3 distal branches (plesiomorphy within Diaphanopterodea ); developed anal area (putative apomorphy for the family). Remarks. The combination of (i) an overall rich venation, (ii) a long fusion of CuA with R + M (or, CuA running very close to R + M for some distance), and (iii) a cua-cup cross-vein very short, is generally used to identify members of the Parelmoidae . The Pennsylvanian Diaphanopteridae differ from this family only by lacking character state (ii) (see Béthoux and Nel 2003 ). Given the polarity of several character states listed as diagnostic of the family, it is not excluded that this taxonomic concept might represent a paraphyletic entity, to include other Diaphanopterodea families, such as Elmoidae . Carpenter (1992) considered the six genera and 10 species reported from the Obora locality (Permian, Cisuralian, Sakmarian), and originally assigned to the Elmoidae or Parelmoidae ( Kukalová-Peck 1974 ) , as of uncertain Parelmoidael affinities. Addressing aspects of species delimitation, and the systematics of these species, is made difficult by post-depositional deformations this material endured. Nevertheless, wing venation character states they display tend to indicate a placement to the family Parelmoidae as delimited above, in particular the well-developed anal area. Also, despite deformation, this comparatively large sample allows appreciating variation in character states variability (in other words, how the extent of variability varies within families), likely to differ among (and within) the closely related families Diaphanopteridae , Parelmoidae and Elmoidae (see below and Kukalová-Peck and Sinichenkova 1992 ). Notably, a distal fork of CuP is common in the Obora material, with some specimens displaying an early fork, and even a 3 - branched CuP. The relation between RP and MA is also very variable across the corresponding species, ranging from a complete lack of fusion to a long one. In contrast, species of the genus Parelmoa Carpenter, 1947 (Fig. 2 A – D ) show more stable venational features (CuP simple; MA and RP connected by a short cross-vein). Among other Parelmoidae , the monotypic genera Pseudelmoa Carpenter 1947 (Fig. 2 E ) and Permuralia Sinichenkova & Kukalová-Peck, 1997 (Fig. 2 F ) remain similar to Parelmoa spp. in most of their venational features. Also, Elmoa trisecta Tillyard, 1937 ( Elmoidae ; Fig. 3 ) shows rather stable venational features, with a consistent occurrence of a (i) distally forked CuP and (ii) a MA distinct from RP , with a cross-vein connecting the two veins shortly after the origin of the latter. The Obora material is therefore unusual in several respects. Instead of attempting to finely resolve relationships between the corresponding taxa, whose variability in many aspects cannot be properly appreciated, we believe it is more sensible to use the Parelmoidae as a broad taxonomic concept, possibly paraphyletic (i. e., a grade), to include the Obora material.