Southeastern Section - 60th Annual Meeting (23–25 March 2011)

Paper No. 5
Presentation Time: 1:30 PM-5:30 PM

A MORPHOLOGICAL AND PHYLOGENETIC EXAMINATION OF THE MIOCENE AND PLIOCENE BIVALVE GENUS CHESAPECTEN


SCLAFANI, Judith A., Department of Geology, College of William and Mary, PO Box 8795, Williamsburg, VA 23187, LOCKWOOD, Rowan, Department of Geology, The College of William and Mary, P.O. Box 8795, Williamsburg, VA 23187 and WARD, Lauck, Virginia Museum of Natural History, 21 Starling Avenue, Martinsville, VA 24112, jasclafani@email.wm.edu

The scallop genus Chesapecten, characterized by its strong ribbing and large size, originated in the early Miocene and was extinct by the late Pliocene. It was highly abundant in the mid Atlantic region of the U.S. and was an important component of marine ecosystems. The genus is comprised of nine species and is widely thought to represent an example of gradual evolution. The limited geographic and stratigraphic ranges of each species make them important indicators for the coastal plain deposits in which they are found. However, because of high variability within species and hybridization between species, they are sometimes difficult to identify based solely on morphology.

This study aims to more quantitatively define the species of Chesapecten using: (1) a morphological assessment of late Miocene and early Pliocene species and (2) a phylogeny of the entire genus. Specimens for the morphological assessment were collected from Cobham Wharf (Surry County, Virginia) and included all three species present at that location (C. middlesexensis, C. jeffersonius, C. madisonius), while those used for the phylogeny were obtained from the collections at the Virginia Museum of Natural History and included all nine defined species. A portion of the cliff at Cobham Wharf was bulk-sampled at half-meter increments, yielding seven total samples with about 12 specimens each. Approximately 12 museum specimens were chosen from three locations for each species, yielding roughly 36 specimens per species.

Analyses involved collecting 10 morphologic landmarks defining shell shape from each field specimen and approximately 60 phylogenetic characters describing shell shape and ornamentation from each museum specimen. Landmark data were Procrustes transformed to eliminate variation based on size, rotation, and location. From this, principal components analysis was used to produce a morphospace. Phylogenetic data were used to reconstruct a parsimony-based phylogeny and bootstrapping allowed us to assess overall robustness of tree topology. Preliminary results indicate that, based on landmark configurations alone, there is no statistically significant difference among the seven samples collected from the field, but that variability within species, especially C. middlesexensis, might vary significantly.