Guangxidella bransoni ( Müller, 1956 )

Leu, Marc, Bucher, Hugo, Vennemann, Torsten, Bagherpour, Borhan, Ji, Cheng, Brosse, Morgane & Goudemand, Nicolas, 2022, A Unitary Association-based conodont biozonation of the Smithian-Spathian boundary (Early Triassic) and associated biotic crisis from South China, Swiss Journal of Palaeontology (19) 141 (1), pp. 1-61 : 47-49

publication ID

https://doi.org/ 10.1186/s13358-022-00259-x

DOI

https://doi.org/10.5281/zenodo.13128060

persistent identifier

https://treatment.plazi.org/id/038B1D1D-6447-FF81-FCA1-EDFBD20AFD67

treatment provided by

Felipe

scientific name

Guangxidella bransoni ( Müller, 1956 )
status

 

Guangxidella bransoni ( Müller, 1956)

Figs. 15E View Fig ; 16E View Fig .

*1956 Neoprioniodus bransoni n. sp.; Müller, p. 829, pl. 95, figs. 19–21.

1956 Neoprioniodus bicuspidatus n. sp.; Müller, p. 828, pl. 95, figs. 16, 17.

1979 Neospathodus bicuspidatus (Müller) ; Solien, p. 302, pl. 3, figs. 2, 3.

1989 Ozarkodina gigantea n. sp.; Tang, p. 409, pl. 31, figs. 10, 14.

1991 Guangxidella typica n. sp.; Zhang & Yang, p. 33, pl. 1, figs. 1a, b, 2a, b.

2009 Guangxidella bransoni (Müller) ; Orchard & Zonneveld, p. 780, fig. 15, parts 26–28.

2014 Guangxidella bransoni (Müller) ; Maekawa & Igo in Shigeta et al., p. 211, figs. 152.16–152.18, 153–159, 160.1–160.4

2018 Guangxidella bransoni (Müller) ; Maekawa in Maekawa et al., p. 24, figs. 14.7–14.10.

Number of specimens:>30

Description. Te segminate P1 element has variably discrete, laterally compressed denticles whose height decreases to the anterior and a very large, variably reclined, terminal cusp. Te basal margin is up-arched and the basal cavity is flat, cordiform and asymmetrical.

Remarks. Gu. bicuspidatus was differentiated from Gu. bransoni on the basis of its closer spaced denticles, the one in front of the cusp being almost as high as the latter ( Müller, 1956). Yet, given the broad range of intraspecific variation present in large collections such as those illustrated by Shigeta et al. (2014), it is in our opinion no longer tenable to keep both species separated. Although both taxa are defined in the same paper by Müller (1956) and the definition of Gu. bicuspidatus appears before that of Gu. bransoni , we have decided to name them bransoni because the etymology of bicuspidatus refers to a 2-cusp element, which is not typical of the revised species. Furthermore, Müller’s holotype of Gu. bicuspidatus is broken, whereas his holotype of Gu. bransoni is better preserved (not broken), better illustrated (also in aboral view) and corresponds better to the revised type.

(See figure on next page.)

Occurrence. USA: Dinner Springs Canyon, Lower Triassic Meekoceras beds, Crittenden Ranch, Elko County, Nevada ( Müller, 1956); Taynes Formation ( Parachirognathus Zone , Utah, ( Solien 1979). British Columbia, Canada ( Orchard & Zonneveld, 2009). Taho Formation, Novispathodus ex. gr. waageni Zone ) Southwest Japan ( Maekawa et al., 2018). Nanpanjiang basin: Bac Tuy Formation, Owenites beds within the Novispathodus ex. gr. waageni Zone , North-eastern Vietnam ( Shigeta et al., 2014). Luolou Formation, Neospathodus waageni Zone , Guangxi, China ( Zhang & Yang, 1991).

V

Royal British Columbia Museum - Herbarium

GBIF Dataset (for parent article) Darwin Core Archive (for parent article) View in SIBiLS Plain XML RDF