Parelmoidae Handlirsch 1906

OrderDiaphanopterodea Handlirsch, 1906 Remarks. Commonly among Megasecopteromorpha, and more particularly in Diaphanopterodea, MA shows some degree of connection with RP. It ranges from a connection via a strong cross-vein, shortly after the origin of MA, to a full fusion with R, then continuing along RP, from which MA diverges at some stage. Because Diaphanopterodea also exhibit oblique cross-veins, it can sometimes be difficult to determine whether an oblique structure occurring between RP and MP is the genuine MA or a cross-vein. Unlike previous authors (Carpenter 1963, 1992; Béthoux and Nel 2003), Prokop and Kukalová-Peck (2017) suggested that a full fusion of MA with R / RP occurred in Diaphanoptera Brongniart, 1893, the type-genus of the family from which the names of the order derives. These authors based their interpretation on vein elevation as observed in the specimen MNHN. F. R 51214, holotype of Diaphanoptera munieri Brongniart, 1893. However, our observation reveals that rock compression this particular specimen experienced (like several other Commentry specimens) makes it impossible to derive a solid inference on the elevation of elements attributable to MA. In contrast, the specimen MNHN. F. R 51196 [considered conspecific to the specimen MNHN. F. R 51214 by Béthoux and Nel (2003)] is better preserved in that respect. Our observation revealed that the structure regarded as the base of MA by Béthoux and Nel (2003) and as a cross-vein by Prokop and Kukalová-Peck (2017) is indeed concave, while MA is convex distal to the point where it diverges from RP. This difference in elevation underlies the argument by Prokop and Kukalová-Peck (2017). However, an elevation shift, applying to both MA and CuA, is a general feature of the broader taxon Rostropalaeoptera (Béthoux 2008). Most decisively, in Eukulojidae, whose wings lack cross-venation, the then undisputable bases of MA and CuA are both concave for a short distance before turning convex, after having approached RP and M, respectively (Béthoux 2008: fig. 3). The assumption that MA is fused very early with R / RP in Diaphanoptera is therefore unsubstantiated.

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Publication Details

Journal
Zenodo (CERN European Organization for Nuclear Research)
Published
2024-08-15
DOI
https://doi.org/10.5281/zenodo.13327729
Primary Topic
Complement system in diseases
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article
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article

Parelmoidae Handlirsch 1906

Zenodo (CERN European Organization for Nuclear Research)
Complement system in diseases
article

Parelmoidae Handlirsch 1906

article en

Abstract

OrderDiaphanopterodea Handlirsch, 1906 Remarks. Commonly among Megasecopteromorpha, and more particularly in Diaphanopterodea, MA shows some degree of connection with RP. It ranges from a connection via a strong cross-vein, shortly after the origin of MA, to a full fusion with R, then continuing along RP, from which MA diverges at some stage. Because Diaphanopterodea also exhibit oblique cross-veins, it can sometimes be difficult to determine whether an oblique structure occurring between RP and MP is the genuine MA or a cross-vein. Unlike previous authors (Carpenter 1963, 1992; Béthoux and Nel 2003), Prokop and Kukalová-Peck (2017) suggested that a full fusion of MA with R / RP occurred in Diaphanoptera Brongniart, 1893, the type-genus of the family from which the names of the order derives. These authors based their interpretation on vein elevation as observed in the specimen MNHN. F. R 51214, holotype of Diaphanoptera munieri Brongniart, 1893. However, our observation reveals that rock compression this particular specimen experienced (like several other Commentry specimens) makes it impossible to derive a solid inference on the elevation of elements attributable to MA. In contrast, the specimen MNHN. F. R 51196 [considered conspecific to the specimen MNHN. F. R 51214 by Béthoux and Nel (2003)] is better preserved in that respect. Our observation revealed that the structure regarded as the base of MA by Béthoux and Nel (2003) and as a cross-vein by Prokop and Kukalová-Peck (2017) is indeed concave, while MA is convex distal to the point where it diverges from RP. This difference in elevation underlies the argument by Prokop and Kukalová-Peck (2017). However, an elevation shift, applying to both MA and CuA, is a general feature of the broader taxon Rostropalaeoptera (Béthoux 2008). Most decisively, in Eukulojidae, whose wings lack cross-venation, the then undisputable bases of MA and CuA are both concave for a short distance before turning convex, after having approached RP and M, respectively (Béthoux 2008: fig. 3). The assumption that MA is fused very early with R / RP in Diaphanoptera is therefore unsubstantiated.

Zenodo (CERN European Organization for Nuclear Research)
Centre National de la Recherche Scientifique (FR), South China Normal University (CN), Sorbonne Université (FR), Jiangsu Provincial Institute of Geological Survey (CN), Université Paris 1 Panthéon-Sorbonne (FR), Capital Normal University (CN)
Openalex Percentile: Top 57%
Complement system in diseases
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