Sinalosia rugosa, Ma & Sun & Hao & Liao, 2002

Ma, Xue-Ping, Sun, Yuan-Lin, Hao, Wei-Cheng & Liao, Wei-Hua, 2002, Rugose corals and brachiopods across the Frasnian- Famennian boundary in central Hunan, South China, Acta Palaeontologica Polonica 47 (2), pp. 373-396 : 386

publication ID

https://doi.org/ 10.5281/zenodo.13304867

persistent identifier

https://treatment.plazi.org/id/03CC87B1-3220-9246-EC14-C978FC0A7826

treatment provided by

Felipe

scientific name

Sinalosia rugosa
status

sp. nov.

Sinalosia rugosa sp. nov.

Figs. 9T–V View Fig , 10A–F View Fig .

Holotype: PUM 00017 View Materials , well−preserved complete specimen; illustrated in Fig. 10A–C View Fig .

Type locality: Southern slope of a small unnamed hill southeast of Daoshitang , Heyi village , Yangqiao Township , Shaodong County, central Hunan Province .

Type horizon: Upper Shetianqiao Formation at a horizon corresponding to uppermost part of bed 22 of the Shetianqiao Formation ( Hou and Wang 1988: 132), late Frasnian (probably Lower Palmatolepis rhenana conodont Zone or younger).

Derivation of the name: It is from well−developed rugae on both valves.

Diagnosis.— Sinalosia characterized by a concavo−convex profile, hinge line about equal to greatest width, ventral valve with cicatrix of attachment very weak to absent, rugae well developed on both valves, and delicate recumbent spines on ventral valve only.

Material.—Over 50 complete and incomplete shells.

Description.—Adult shell generally 2–2.5 cm in width, elliptical in outline, wider than long, concavo−convex in lateral profile, corpus shallow, hinge line about equal to or slightly shorter than greatest width.

Ventral valve moderately convex. Cicatrix of attachment very weak to absent. Interarea well developed; delthyrium small, triangular, closed by pseudodeltidium. Shell surface marked by rugae and alternating weak spines generally lying parallel to surface; hinge spines rare or absent, erect and slightly coarser if present.

Dorsal valve slightly concave, marked by rugae on whole surface; no spines. Interarea low; notothyrium relatively large (nearly equal to delthyrium in size), closed by chilidium, which is penetrated by a bifid cardinal process in some specimens ( Fig. 9T View Fig ).

Dorsal interior with a narrow and low median septum extending to about mid−length of shell; postero−ventrally directed bifid cardinal process high, with a small furrow on top of the cardinal process on each side; sockets short but deep; inner socket ridges well developed, posteriorly connected with the cardinal process. Ventral interiors unknown.

Remarks.—It seems that no similar forms have been recorded yet. This would be the first record of Devonian strophalosioids in China.

Occurrence.—Central Hunan in the Shetianqiao section; late Frasnian.

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