31 Undergraduate Research II (Posters)
Friday, 29 March 2019
8:00 AM - 12:00 PM
Carolina Ballroom
BRIDGING A BIOGEOGRAPHIC GAP BY STUDYING PLIO-PLEISTOCENE EXTINCTION EPISODES THROUGH MOLLUSCAN ASSEMBLAGES OF GEORGIA AND NORTHERN FLORIDA
Paper number: 31-16
Program: Theme Sessions
Time: 8:00 AM – 12:00 PM
Authors
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Christy VisaggiGeorgia State University, Atlanta, GA
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Roger W. PortellUniversity of Florida, Gainesville, FL
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Lisa DuongGeorgia State University, Atlanta, GA
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Katherine C. HewittNational Science Foundation, Alexandria, GA
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Lacey J. DavisGeorgia State University, Atlanta, GA
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Leonardo Maduro-SalvarreyGeorgia State University, Atlanta, GA
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Eduardo MorontaGeorgia State University, Atlanta, GA
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Matthew J. ToroGeorgia State University, Atlanta, GA
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Amy J. ReberGeorgia State University, Atlanta, GA
Abstract
Plio-Pleistocene fossils from Georgia were studied primarily from museum collections from various institutions in the region (e.g., Fernbank Science Center, Georgia Southern University, Florida Museum of Natural History). Ongoing data-mining and study of borrowed collections has yielded a new database of Plio-Pleistocene fossils for over 12,500 specimens recorded from Georgia. Top genera for bivalves include Mulinia, Donax, Anadara, Pleuromeris, Abra, Mercenaria, and Ervilia. Top genera for gastropods include Neverita, Crepidula, Terebra, Oliva, Natica, Nassarius, Busycon, Anachis, and Acteocina.
Specimens analyzed from the Plio-Pleistocene Nashua Formation of northern Florida include bulk samples of quarry spoils collected in September 2018. Three locations at a quarry were sampled and specimens sieved, sorted, and identified by students in a paleontology class at Georgia State University. Data collection is still in process, but so far, nearly 2,000 specimens have been studied. To date, 47 bivalve and 26 gastropod genera have been identified. Samples are dominated by Mulinia for bivalves; gastropods are well-represented by Oliva, Conus, and Crepidula. Future work will analyze these results in the context of extinction patterns in the region.
Geological Society of America Abstracts with Programs. Vol. 51, No. 3
doi: 10.1130/abs/2019SE-326743
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