Bairdia davehornei Forel, 2013

Forel, Marie-Béatrice, Crasquin, Sylvie, Hips, Kinga, Kershaw, Steve, Collin, Pierre-Yves & Haas, János, 2013, Biodiversity evolution through the Permian-Triassic boundary event: Ostracods from the Bükk Mountains, Hungary, Acta Palaeontologica Polonica 58 (1), pp. 195-219 : 203

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/8F15E272-D36B-4E73-83B8-C38A29D47A91

taxon LSID

lsid:zoobank.org:act:8F15E272-D36B-4E73-83B8-C38A29D47A91

treatment provided by

Felipe

scientific name

Bairdia davehornei Forel
status

sp. nov.

Bairdia davehornei Forel sp. nov.

Figs. 6Q–U View Fig , 8 View Fig .

Etymology: Dedicated to Professor David J. Horne (Queen Mary University, London).

Type material: Holotype: one complete carapace, Fig. 6Q View Fig , UPMC P6M2777 , sample 08BAN61 . Paratype: one complete carapace, Fig. 6R View Fig , UPMC P6M2778 , sample 08BAN62 .

Type locality: Bálvány North section, Bükk Mountains, Hungary .

Type horizon: Level 7, Gerennavár Limestone Formation , Changhsingian, Upper Permian .

Material.—32 complete and 2 broken carapaces, samples 08BAN47, 61 and 62 (see Fig. 2B), levels 1, 7, 8, Nagyvisnyó and Gerennavár Limestone Formations, Bálvány North section, Hungary, Changhsingian to Griesbachian, Upper Permian–Lower Triassic.

Diagnosis.—A species of Bairdia with an elongated carapace (L/H = 2) with a truncated AVB, regularly arched dorsal parts, and a rounded PB with the maximum of curvature at lower 1/3rd of H. Dimensions.—L 290–560 µm; H 141–275 µm (see Fig. 8 View Fig ).

Description.—Carapace elongated (L = 2H), DB, PDB, and ADB regularly arched at LV; DB, PDB, and ADB quite straight at RV; AB with small radius of curvature, with maximum of curvature located above mid−H; AVB truncated; VB concave, particularly at RV; PB rounded with large radius of curvature, maximum of curvature located at the lower 1/3 of H; typical bairdian beak visible only on some specimens; LV overlaps RV slightly all around the carapace with maximum at DB; Hmax located near mid−L. Internal features unknown. Discussion.— Bairdia davehornei sp. nov. could be compared to Bairdia fangnianqiaoi Crasquin, 2010 from the Griesbachian Meishan section ( China; Crasquin et al. 2010a). The latter species has a more slender PB and a more elongated carapace in lateral view. Cryptobairdia heshanenis Chen, 2002 (Wuchiapingian of Matan and Pinding section, China; Shi and Chen 2002) is also close to Bairdia davehornei sp. nov. but has a more distinct flattened and a larger AB. Bairdia davehornei sp. nov. differs from Bairdia ? kemerensis from the Griesbachian of Turkey (Crasquin−Soleau et al. 2004b) in its shorter DB and smaller AB.

Stratigraphic and geographic range.—Bálvány North section, levels 1 to 8, samples 08BAN47, 61 and 62 (see Fig. 2B), Nagyvisnyó and Gerennavár Limestone Formations, Changhsingian–Griesbachian, Upper Permian–Lower Triassic.

Kingdom

Animalia

Phylum

Arthropoda

Class

Ostracoda

Order

Podocopida

Family

Bairdiidae

Genus

Bairdia

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