UC Berkeley PaleoBios Title Bonnima sp. (Trilobita; Corynexochida) from the Chambless Limestone (Lower Cambrian) of the Marble Mountains, California: First Dorypygidae in a cratonic region of the southern Cordillera Permalink https://escholarship.org/uc/item/8fq03184 Journal PaleoBios, 30(2) ISSN 0031-0298 Author Foster, John R. Publication Date 2011-10-19 DOI 10.5070/P9302021790 Peer reviewed eScholarship.org Powered by the California Digital Library University of California PaleoBios 30(2):45–49, October 19, 2011 © 2011 University of California Museum of Paleontology Bonnima sp. (Trilobita; Corynexochida) from the Chambless Limestone (Lower Cambrian) of the Marble Mountains, California: First Dorypygidae in a cratonic region of the southern Cordillera JOHN R. FOSTER Museum of Western Colorado, P.O. Box 20,000, Grand Junction, CO 81502;
[email protected] A trilobite pygidium, likely referable to the genus Bonnima, is the first evidence of a member of the Corynexochida reported from the Lower Cambrian (Dyeran Stage) Chambless Limestone of the southern Marble Mountains in the Mojave Desert of California. This specimen represents the first occurrence of the family Dorypygidae in the cratonic facies of the Lower Cambrian in the California-western Nevada region, as all of the few previous reports of the family (mostly Bonnia) have been from much thicker, more distal open-shelf deposits far to the northwest in the White- Inyo—Esmeralda County region of California and Nevada. Although still relatively rare, the occurrence of Dorypygidae across a range of environments biofacies realms in this area is typical of their distribution in other regions. INTRODUCTION from 5 cm to 1 m thick, and these beds generally decrease in The Chambless Limestone is a Lower Cambrian unit ex- thickness upward in the formation.