125 Paleontology: The Role of Collections in Diversity, Databases, and Museums (Posters)
Monday, 2 November 2015
9:00 AM - 6:30 PM
Exhibit Hall
GEOGRAPHIC AND TEMPORAL COMPARISONS OF BIVALVE DIVERSITY IN THE PLIO-PLEISTOCENE OF VIRGINIA AND THE CAROLINAS
Paper number: 125-5
Program: Technical Sessions
Time: 9:00 AM – 6:30 PM
Authors
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Patricia KelleyUniversity of North Carolina Wilmington, Wilmington, NC
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Samuel H. NeelyUniversity of North Carolina Wilmington, Wilmington, NC
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Robert J. ErdieUniversity of North Carolina Wilmington, Wilmington, NC
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Conor C. MacNairUniversity of North Carolina Wilmington, Wilmington, NC
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William D. OakesUniversity of North Carolina Wilmington, Wilmington, NC
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Caleb A. QuintoUniversity of North Carolina Wilmington, Wilmington, NC
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Hannah R. VanDerkinUniversity of North Carolina Wilmington, Wilmington, NC
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Gregory P. DietlPaleontological Research Institution, Ithaca, NY
Abstract
Tearcoat Branch and Morgarts Beach samples were dominated by Mulinia; dominance was ~0.60 in contrast to 0.26 and 0.22 for Kirby Pond and Moore House samples. As predicted, when rarefied to the same size (1180 specimens), the South Carolina samples were much richer (24 and 28 genera) than the Virginia samples (13 and 16 genera). The disparity in richness between north and south remained when rarefaction omitted the dominant genus. Compared to the North Carolina Duplin, South Carolina samples were significantly less rich than at the Lumber River and Robeson Farm but similar to Natural Well, especially when Mulinia was omitted. We did not find the expected drop in diversity from the Pliocene to Pleistocene. South Carolina Duplin samples were less rich than the Waccamaw samples but richness overlapped (95% confidence intervals) with the James City at Lee Creek when rarefied without the dominant genus. Confidence intervals overlapped for most lower Waccamaw and Duplin sites studied. Yorktown samples were less rich than all others. Lack of richness decline may be related to taphonomy, environment, or taxonomic level of study.