Bairdia anisongae Forel, 2013
publication ID |
https://doi.org/ 10.4202/app.2011.0126 |
publication LSID |
lsid:zoobank.org:pub:15268E3E-5628-419C-B76F-6710BA70723E |
persistent identifier |
https://treatment.plazi.org/id/1F5EDEB9-0409-4F62-ACC7-D79F99B92DFA |
taxon LSID |
lsid:zoobank.org:act:1F5EDEB9-0409-4F62-ACC7-D79F99B92DFA |
treatment provided by |
Felipe |
scientific name |
Bairdia anisongae Forel |
status |
sp. nov. |
Bairdia anisongae Forel sp. nov.
Figs. 6N–P View Fig , 7 View Fig .
Etymology: Dedicated to Dr. Anisong Chitnarin (Suranaree University of Technology, Nakhon Ratchasima, Thailand).
Type material: Holotype: one complete carapace, Fig. 6N View Fig , UPMC P6M2774 , sample 08BAN55 . Paratype: one complete carapace, Fig. 6O View Fig , UPMC P6M2775 , sample 08BAN62 .
Type locality: Bálvány North section, Bükk Mountains, Hungary .
Type horizon: Level 4, Nagyvisnyó Limestone Formation , Changhsingian, Upper Permian .
Material.—Three complete and four broken carapaces, samples 08BAN47, 55 and 62 (see Fig. 2B), levels 1, 4, 8, Nagyvisnyó and Gerennavár Limestone Formations, Bálvány North section, Hungary, Changhsingian to Griesbachian, Upper Permian–Lower Triassic.
Diagnosis.—A species of Bairdia with straight PDB, DB, and ADB, with narrow AB and almost parallel AVB and PDB.
Dimensions.—L 210–325 µm; H 120–200 µm (see Fig. 7 View Fig ).
Description.—Carapace quite high (H/L 0.57–0.63), with straight DB, PDB, and ADB at both valves; DB steeply inclined backwards; AB with small radius of curvature and maximum of convexity located high (above mid−H); AVB
http://dx.doi.org/10.4202/app.2011.0126
straight and long, almost parallel to PDB; VB long and quite straight at both valves; PB with small radius of curvature with maximum of convexity located low (lower than 1/5 th of H); PDB straight and long at both valves; Hmax located a little in front of mid−L; LV overlaps RV very faintly all around the carapace with a maximum at DB, carapace biconvex and thin in dorsal view. Internal features unknown.
Discussion.— Bairdia anisongae sp. nov. shows the same angularity between dorsal parts (PDB/DB/ADB) as Bairdia wushunbaoi Crasquin, 2010 and Bairdia paussi Crasquin, 2010 both from Changhsingian of Meishan section (Crasquin et al. 2010a). In B. wushunbaoi the AB is narrower and its maximum of curvature is located higher. B. paussi has a more elongated carapace with a less strongly inclined DB. Bairdia anisongae sp. nov. differs from B. wailiensis Crasquin−Soleau, 2006 from the Lower Triassic of Guangxi (Crasquin−Soleau et al. 2006) (see Fig. 5J–M View Fig ) in its more distinct dorsal parts, its more tapering PB and the smaller radius of curvature of AB.
Stratigraphic and geographic range.—Bálvány North section, levels 1 to 8, samples 08BAN47, 55 and 62 (see Fig. 2B), Nagyvisnyó and Gerennavár Limestone Formations, Changhsingian to Griesbachian, Upper Permian to Lower Triassic.
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