Clavofabella? lanshella Guillam & Forel, 2022

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 : 11-12

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.6363209

persistent identifier

https://treatment.plazi.org/id/9B24EB32-22A9-4A92-99D8-6C5F7B6744D0

taxon LSID

lsid:zoobank.org:act:9B24EB32-22A9-4A92-99D8-6C5F7B6744D0

treatment provided by

Felipe

scientific name

Clavofabella? lanshella Guillam & Forel
status

sp. nov.

Clavofabella? lanshella Guillam & Forel sp. nov.

urn:lsid:zoobank.org:act:9B24EB32-22A9-4A92-99D8-6C5F7B6744D0

Fig. 5F–L View Fig

Diagnosis

A new species questionably attributed to Clavofabella with elongate outline and laterally compressed spinose free margin at LV.

Etymology

The specific epithet refers to the Latinization of the Chinese ‘ lan she ’, which means ‘blue snake’ in reference to the name given to the section.

Material examined

Holotype

CHINA • 1 complete carapace ( Fig. 5F–G View Fig ); Blue Snake section , Gelaohe Formation, sample 19BAI 68; Famennian, late Devonian; P6M 3842 .

Paratype

CHINA • 1 complete carapace ( Fig. 5H View Fig ); Blue Snake section , Gelaohe Formation, sample 19BAI 68; Famennian, late Devonian; P6M 3843 .

Other material

CHINA • 1 complete carapace (A-1, Fig. 5I View Fig ); Blue Snake section , Gelaohe Formation, sample 19BAI 68; P6M 3844 1 complete carapace (A-2, Fig. 5J View Fig ); Blue Snake section , Gelaohe Formation, sample 19BAI 68; P6M 3845 1 complete carapace (A-3, Fig. 5L View Fig ); Blue Snake section , Gelaohe Formation, sample 19BAI 68; P6M 3846 20 complete carapaces; Blue Snake section , Gelaohe Formation, samples 19BAI 63, 19BAI 67, 19BAI 68, 19BAI 74. All from the Famennian, late Devonian.

Dimensions

See Fig. 4A View Fig .

Description

Carapace large, preplete, ovoid/rectangular (adults) to inverted triangular (young juveniles) in lateral view, lenticular with laterally compressed anterior and posterior margins in dorsal view. Lmax slightly above mid-H, Hmax in front of mid-L, Wmax around mid-H and slightly in front of mid-L. RV overlaps LV all around, with maximum along free margin. Hinge line slightly sinuous with gentle concavity immediately posterior to ACA, slightly invaginated all along its length. Obtuse cardinal angles, ACA about 145°, PCA about 130°. Surface coarsely reticulate with round reticulae. LV with a spinose free margin that could indicate the presence of a velar structure. Pit relatively large (H about 32% of Hmax, L about 14% of Lmax), ovoid, elongated dorso-ventrally, located slightly in front of mid-L, slightly above mid-H, at Wmax.

Remarks

This species is doubtfully attributed to the genus Clavofabella Martinsson, 1955 described from the Late Wenlock (Silurian) of Gotland, Sweden ( Martinsson 1955) because of RV overlapping LV, surface reticulated, sulcal pit and spinose free margin that could indicate the presence of a velar structure and that points to heteromorphs after Moore (1961). However, the tubercles in all known species belonging to Clavofabella are short and rounded and are absent at DB where the dolon is located in heteromorphs. In our material, these structures are spines rather than tubercles and are located along the entire free margin and are larger than those described from all known species belonging to this genus. Clavofabella? lanshella sp. nov. also differs from all other species of this genus by its laterally compressed morphology, more elongate lateral outline, larger sulcal pit, coarse reticulation and straighter DB. The H/L scatter plot of Clavofabella? lanshella sp. nov. ( Fig. 4A View Fig ) allows to discriminate four ontogenetic stages (A-3 to Ad). The ontogenetic development of this species is marked by the elongation of the carapace, increasing compression of the free margin, enlargement of the pit and growth of spines along free margin.

Occurrence

Samples 19BAI 63, 19BAI 67, 19BAI 68, 19BAI 74, Gelaohe Formation, Blue Snake section, Famennian, late Devonian (this work).

Kingdom

Animalia

Phylum

Arthropoda

Class

Ostracoda

SubClass

Podocopa

Order

Palaeocopida

SubOrder

Beyrichiocopina

SuperFamily

Primitiopsoidea

Family

Paraparchitidae

Genus

Clavofabella

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