Brachyopoidea
publication ID |
https://doi.org/ 10.5194/fr-24-33-2021 |
DOI |
https://doi.org/10.5281/zenodo.12110328 |
persistent identifier |
https://treatment.plazi.org/id/6D66DD4E-6730-FFFB-FF23-F9D2740DFEBB |
treatment provided by |
Felipe |
scientific name |
Brachyopoidea |
status |
|
Brachyopoidea indet.
Reference material
KS37-8 ( Fig. 3m –p View Figure 3 ), intercentrum.
Formation/age
Phu Kradung Formation (Upper Jurassic).
Locality and sediment
KS37-8 was collected at the Khao Wong locality in Khao Wong District , Kalasin Province. Sediments in this locality are grey to green siltstones .
Description
KS37-8 is a wedge-shaped intercentrum with the dorsal edge much shorter than the ventral edge. The parapophyses are close to the posterodorsal margin on the lateral surface. Both anterior and posterior surfaces are concave and show a marked circular notochordal canal, which is visible as a circular pit. The pleurocentra are reduced or absent. This intercentrum KS37-8 probably belongs to Brachyopoidea since it is the only Stereospondyli superfamily retrieved beyond the Triassic ( Buffetaut et al., 1994b). Furthermore, the wedge-shaped morphology of KS37-8 resembles the intercentra of the Brachyopoidea ( Shishkin, 1991; Warren et al., 1997; Warren and Dammiani, 1999; Warren et al., 2011), which are similar to the intercentra discovered from the Indochina block ( TF 3144) and Sibumasu blocks ( TF 3328 and TF 3329) of Thailand ( Buffetaut et al., 1994a, c). However, the intercentrum is not sufficiently diagnostic for identification at the family level.
TF |
Department of Mineral Resources |
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