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Journal of Molluscan Studies 2006 72(2):167-177; doi:10.1093/mollus/eyi066
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© The Author 2006. Published by Oxford University Press on behalf of The Malacological Society of London, all rights reserved

GENETIC STRUCTURE OF THE WESTERN NORTH AMERICAN AQUATIC GASTROPOD GENUS TAYLORCONCHA AND DESCRIPTION OF A SECOND SPECIES

ROBERT HERSHLER1, HSIU-PING LIU2, TERRENCE J. FREST3, EDWARD J. JOHANNES3 and WILLIAM H. CLARK4

1Department of Invertebrate Zoology, Smithsonian Institution, P.O. Box 37012, NHB W-305 MRC 163, Washington, D.C. 20013-7012, USA; 2Department of Biological Sciences, University of Denver, Denver, CO 80208, USA; 3DEIXIS Consultants, 2517 NE 65th Street, Seattle, WA 98115-7125, USA; and 4Idaho Power Company, 1221 West Idaho Street, Boise, ID 83702-5610, USA and Orma J. Smith Museum of Natural History, Albertson College of Idaho, Caldwell, ID 83605-4432, USA

Correspondence: R. Hershler; e-mail: hershlerr{at}si.edu

The Bliss Rapids Snail (Taylorconcha serpenticola) is a threatened species that ranges along a short reach of the middle Snake River in southern Idaho. Additional Taylorconcha populations of uncertain taxonomic status have recently been discovered in other portions of the Snake River basin (Owyhee River, lower Snake River). We investigated the phylogenetic relationships and population structure of these snails, together with two outgroups, using cytochrome c oxidase subunit I (COI) of mitochondrial DNA and the first internal transcribed spacer region between the 18S and 5.8S ribosomal DNA. These data show no sharing of haplotypes or genotypes among T. serpenticola and the Owyhee-Lower Snake populations, with both depicted as monophyletic units within the Taylorconcha clade. Both of these datasets and morphological evidence suggest that the Owyhee-Lower Snake populations are a distinct species, which we describe herein (T. insperata new species). Application of an available COI molecular clock suggests that Taylorconcha arose in the late Miocene, when ancestral Snake River drainage was impounded in an extensive lacustrine system (‘Lake Idaho’) in western Idaho. The shallow population structuring of T. insperata suggests that the lower Snake River was only recently colonized subsequent to incision of Hells Canyon, draining of Lake Idaho, and development of a through-going river in the late Neogene. The absence of significant genetic structure in T. serpenticola, which is attributed to the unstable course and flow regime of the middle Snake River during the Quaternary, suggests that this species can be treated as a single management unit.

(Received 14 July 2005; accepted 23 September 2005)


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