Sphenothallus from the Lower Silurian of China

Author:

Yi Wang,Shou-Gang Hao,Xu Chen,Jia-Yu Rong,Guo-Xiang Li,Jianbo Liu,Honghe Xu

Abstract

The genus Sphenothallus was erected by Hall (1847, p. 261), who originally considered it a land plant. Sphenothallus was later classified as a marine invertebrate. Moore and Harrington (1956, p. F65) regarded Sphenothallus as a hydrozoan or scyphozoan. Van Iten et al. (1992, p. 139) supported Moore and Harrington's idea, and argued that it displays a close relationship to conularids (also see Li, 2000, p. 91). However, Mason and Yochelson (1985, p. 93–94) suggested that Sphenothallus is an annelid or “worm” (also see Fauchald et al., 1986, p. 64; Feldmann et al., 1986, p. 344–345; Choi, 1990, p. 403; Bartels et al., 1998, p. 114–117). The exact phylogenetic affinity of Sphenothallus is still debated.

Publisher

Cambridge University Press (CUP)

Subject

Paleontology

Reference28 articles.

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2. Account of some new or little-known species of fossils, mostly from the Paleozoic rocks of New York;Ruedemann;New York State Museum Bulletin,1916

3. Fossil worms from the Devonian of North America (Sphenothallus) and Burma (“Vermes”) previously identified as phyllocarid arthropods

4. The discovery of a sessile Conularia;Ruedemann;New York State Geological Survey Annual Report,1896

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