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Lower Cambrian coeloscleritophorans (Ninella, Siphogonuchites) from Xinjiang and Shaanxi, China

Published online by Cambridge University Press:  01 May 2009

S. Conway Morris  and
A. J. Chapman
S. Conway Morris
Affiliation:
Department of Earth Sciences, University of Cambridge, Cambridge CB2 3EQ, UK
A. J. Chapman
Affiliation:
Department of Earth Sciences, University of Cambridge, Cambridge CB2 3EQ, UK
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Abstract

Ninella tarimensis from the Lower Cambrian Yurtus Formation of western Xinjiang, China, is shown to be a relative of the halkieriids and siphogonuchitids. These are known principally from dispersed sclerites, presumably secreted by slug-like organisms that were an abundant component of the Cambrian benthos. The sclerites of N. tarimensis are relatively small, strongly recurved and usually possess an upper surface ornamented with transverse sculpture. The lower surface is more or less smooth and is joined to the upper surface via steep faces that may be grooved. The apertural region is quadrate in outline and bears a circular foramen. Ninella is fairly widespread and is known from elsewhere in China (Guizhou and Shaanxi Provinces) and from Kazakhstan. A brief description of the siphogonuchitid scleritome is also presented, based on dispersed sclerites and shells from the Lower Cambrian of Shaanxi Province, China. Formal synonymy of the sciotaxa Siphogonuchites, Dabashanites, Lopochites, and Maikhanella as Siphogonuchites is proposed.

Type
Articles
Information
Geological Magazine , Volume 133 , Issue 1 , January 1996 , pp. 33 - 51
Copyright
Copyright © Cambridge University Press 1996

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