Cordulibellula inopinata, Sroka & Howells & Nel, 2023
publication ID |
https://doi.org/ 10.4202/app.01072.2023 |
persistent identifier |
https://treatment.plazi.org/id/03B487A7-0860-FFE9-FCD2-FC0840A1FC86 |
treatment provided by |
Felipe |
scientific name |
Cordulibellula inopinata |
status |
sp. nov. |
Cordulibellula inopinata sp. nov.
Figs. 1 View Fig , 2 View Fig .
Zoobank LSID: urn:lsid:zoobank.org:act:B664998B-1919-451F-8BF3-80AF942020B5
Etymology: From Latin inopinata , unexpected; referring to the unexpected find of a “relict” “libelluloid” related to Mesozoic taxa in the middle Eocene.
Type material: Holotype FHPR 11611, part and counterpart of an isolated hind wing, partly folded and deformed.
Type locality: Lake Uinta , near Bonanza, Utah, USA .
Type horizon: Upper Parachute Creek Member, Green River Formation; middle Eocene.
Diagnosis.—Hind wing characters only. Straight gaff (= basal CuA before its branching); CuAa with at least three posterior branches; an obliquely elongate anal loop subdivided into one large and two smaller cells; MP and MAa clearly undulating; a well-defined Rspl; a zigzagged Mspl.
Description.—Preserved part of wing 29.2 mm long, ca. 6.0 mm wide, estimated length of wing 32.0 mm; distance between nodus (N) and pterostigma (Pt) 13.6 mm between pterostigma and wing apex 2.8 mm; pterostigma 3.3 mm long, 0.8 mm wide, parallel sided (distal side not more oblique than basal side), covering two long cells; pterostig- mal brace aligned with basal side and weakly oblique; 11 postnodal crossveins, not aligned with the eight postsubnodal crossveins; an important “libellulid” gap in basal part of postsubnodal space; “cordulegastrid” gap present; five visible antenodal crossveins of first and second rows nearly aligned, probably nine originally, primary antenodals not preserved; arculus only partly preserved (posterior part); discoidal triangle free, isosceles, with base located close to arculus, separated by less than 1/2 length of arculus, basal side of discoidal triangle (t) 1.7 mm long, anterior side 2.8 mm long, distal side (Mab) 2.8 mm long; hypertriangle likely with two crossveins, with MA distinctly curved; subdiscoidal space free, distinctly closed by an oblique PsA incompletely preserved; only CuP in submedian space; median space free; anal loop (al) transversely elongate, 4.8 mm long, max. 1.0 mm wide, narrow obliquely elongate, with a midrib and divided into one large and two smaller cells; basal CuA before its branching long but straight; CuAa with at least three posterior branches, probably more; MP basally weakly zigzagged and distally undulated; MAa distally undulated too; posdiscoidal area rather broad, with two rows of cells basally near the discoidal triangle and a zigzagged Mspl, one row of cells between MAa and Mspl; RP3/4 poorly preserved; IR2 weakly zigzagged, parallel with RP 2 in its main part, but diverging distally; two Bqs crossveins; base of RP2 aligned with subnodus; lestid oblique crossvein one cell distad subnodus; one row of cells between RP1 and RP2 up to 3.5 mm basad pterostigma; a strongly zigzagged IR1; a well-defined Rspl weakly curved anteriorly, with one row of cells between it and IR2.
Stratigraphic and geographic range.—Upper Parachute Creek Member, Green River Formation, middle Eocene; Lake Uinta.
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