Hypotetragona sp., Morey, 1935

Guillam, Elvis, Forel, Marie-Béatrice, Song, Junjun & Crasquin, Sylvie, 2022, Late Devonian-early Carboniferous ostracods (Crustacea) from South China: taxonomy, diversity and implications, European Journal of Taxonomy 804, pp. 1-62 : 20-21

publication ID

https://doi.org/ 10.5852/ejt.2022.804.1689

publication LSID

lsid:zoobank.org:pub:5EEDA63F-8A81-40DF-B5A4-C799498DC523

DOI

https://doi.org/10.5281/zenodo.6363225

persistent identifier

https://treatment.plazi.org/id/03C687C5-6423-FF8C-FD0C-F1544DC4C3BA

treatment provided by

Felipe

scientific name

Hypotetragona sp.
status

 

Hypotetragona sp.

Fig. 6J–M View Fig

Indivisia minata – Song & Gong, 2019: fig. 4t.

Material examined

CHINA • 1 complete carapace (Ad, Fig. 6J View Fig ); Blue Snake section, Tangbagou Formation, sample 19BAI 39; Tournaisian, early Carboniferous; P6M 3865 • 1 complete carapace (A-1, Fig. 6K View Fig ); Blue Snake section, Tangbagou Formation, sample 19BAI 05; Tournaisian, early Carboniferous; P6M 3866 • 1 complete carapace (A-2, Fig. 6L View Fig ); Blue Snake section, Gelaohe Formation, sample 19BAI 60; Famennian, late Devonian; P6M 3867 • 1 complete carapace (A-3, Fig. 6M View Fig ); Blue Snake section, Gelaohe Formation, sample 19BAI 69; Famennian, late Devonian; P6M 3868 • 37 complete carapaces; Blue Snake section, Gelaohe and Tangbagou Formations, samples 19BAI 37, 19BAI 41, 19BAI 44, 19BAI 54, 19BAI 60, 19BAI 68, 19BAI 69; Famennian–Tournaisian, late Devonian–early Carboniferous.

Dimensions

RV: L = 302–846 µm, H = 198–519µm, H/L = 0.57–0.7.

LV: L = 299–834 µm, H = 195–509µm, H/L = 0.56–0.65.

Remarks

The adults of this species are represented by poorly preserved specimens that do not allow for a precise specific attribution. Indivisia minata Wei, 1988 in Song & Gong (2019) from the Famennian, late Devonian, of Blue Snake section, Guizhou, South China ( Song & Gong 2019) differs from Indivisia minata which is stockier, has a more rounded outline, an ADB which is not truncated and a less compressed laterally posterior part in LV. Indivisia minata in Song & Gong (2019) furthermore does not belong to the genus Indivisia Zaspelova, 1954 as shown by the deep sulcus and prominent lobe in the antero–dorsal part of the carapace. It has the typical outline of the family Geisinidae and displays the diagnostic lobes and sulcus of the genus Hypotetragona . It is morphologically similar to Hypotetragona sp. and is considered as conspecific. The specimen shown in Song & Gong (2019) is a steinkern which would explain the absence of ornamentation which is visible in well–preserved juveniles in our material. The size and the H/L ratio of the specimens shown in Song & Gong (2019) are similar to our material. At least 4 ontogenetic stages are present in our material. The ontogenetic development of this species is marked by the outline becoming more rectangular, the sulcus becoming deeper and lobes more developed.

Occurrence

Gelaohe Formation, Blue Snake section, Guizhou, South China, Famennian, late Devonian, ( Song & Gong 2019). Samples 19BAI 05, 19BAI 37, 19BAI 39, 19BAI 41, 19BAI 44, 19BAI 54, 19BAI 60, 19BAI 68, 19BAI 69, Gelaohe and Tangbagou Formations, Blue Snake section, Guizhou, South China, Famennian–Tournaisian, late Devonian–early Carboniferous (this work).

Kingdom

Animalia

Phylum

Arthropoda

Class

Ostracoda

Order

Platycopina

Family

Geisinidae

Genus

Hypotetragona

Loc

Hypotetragona sp.

Guillam, Elvis, Forel, Marie-Béatrice, Song, Junjun & Crasquin, Sylvie 2022
2022
Loc

Indivisia minata

Wei 1988
1988
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