36 D12. Paleontological Potpourri (Posters)
Friday, 13 April 2018
1:30 PM - 5:30 PM
Room 301 DE/Henley Concourse
FORAMINIFERAL ASSEMBLAGES OF THE SHOREFACE AND INNER SHELF OFF BOGUE BANKS, NORTH CAROLINA
Paper number: 36-1
Program: Technical Sessions
Time: 1:30 PM – 5:30 PM
Authors
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Nina M.E. ShmorhunEast Carolina University, Greenville, NC
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Stephen J. CulverEast Carolina University, Greenville, NC
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David MallinsonEast Carolina University, Greenville, NC
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Kathleen FarrellRaleigh, NC
Abstract
Results indicate slight differences in foraminiferal assemblages for the shoreface and inner shelf cores. The foraminifera are mostly Holocene (56-100%), but up to 7% of shoreface assemblages and 13% of inner shelf assemblages consist of reworked Miocene fossils. Holocene shoreface assemblages contain 86% to 90% Rotaliina, 14% to 31% Miliolina, and 0% Textulariina. In contrast, Holocene inner shelf assemblages have 69% to 100% Rotaliina, 0% to 31% Miliolina, and 0% Textulariina. Within the shoreface samples, Ammonia parkinsoniana, Ammonia tepida, Elphidium mexicanum, and miliolids are more abundant than within inner shelf samples. Planktonic foraminifera are rare. In the shoreface, species diversity (Fisher’s alpha) increases up-core, ranging from 8.238 to 17.442. The results of this study indicate that shoreface and inner shelf environments are not easily distinguished by their sedimentological characteristics. However, there are slight differences in foraminiferal assemblages between the two environments.
Geological Society of America Abstracts with Programs. Vol. 50, No. 3
doi: 10.1130/abs/2018SE-313151
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