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A Late Permian Chinese gastropod species, possibly larval, in the Middle Pennsylvanian of New Mexico

Published online by Cambridge University Press:  14 July 2015

Barry S. Kues ,
Roger L. Batten ,
Douglas H. Erwin  and
Pan Hua-Zhang
Barry S. Kues
Affiliation:
1Department of Earth and Planetary Sciences, MSC 03 2040, University of New Mexico, Albuquerque 87131-0001
Roger L. Batten
Affiliation:
277 East Missouri, #76, Phoenix, Arizona 85012
Douglas H. Erwin
Affiliation:
3Department of Paleobiology, MRC-121, National Museum of Natural History, Washington, D.C. 20560
Pan Hua-Zhang
Affiliation:
4Nanjing Institute of Geology and Palaeontology, Academica Sinica, Nanjing, People's Republic of China 210008
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Extract

Kues and Batten (2001, p. 30, fig. 6.17–6.20) described several distinctive, minute, low-spired gastropod specimens from the Desmoinesian (Middle Pennsylvanian) Flechado Formation of north-central New Mexico, assigning them questionably to Lunulazona Sadlick and Nielsen, 1963 because of the strongly developed collabral elements similar to those of that genus. These shells, consisting of three or four inflated whorls, are at most 1 mm in height and the later whorls bear conspicuous, sharp, widely spaced collabral ribs that bend strongly across a wide, slightly flattened band interpreted as a peripheral selenizone. While recognizing these specimens as a distinct, unnamed taxon, Kues and Batten (2001) believed that they likely represent juveniles of an as yet unrecognized larger species of gastropod with a different mature morphology.

Type
Paleontological Notes
Information
Journal of Paleontology , Volume 78 , Issue 2 , March 2004 , pp. 420 - 423
Copyright
Copyright © The Paleontological Society 

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