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An analysis and comparison of observed Pleistocene South Carolina (USA) shoreline elevations with predicted elevations derived from Marine Oxygen Isotope Stages

Published online by Cambridge University Press:  20 January 2017

William Richardson Doar III  and
Christopher George St. Clement Kendall
William Richardson Doar III*
Affiliation:
South Carolina Geological Survey, Department of Natural Resources, 5 Geology Road, Columbia, SC 29210, USA Department of Earth and Ocean Sciences, University of South Carolina, 701 Sumter Street, EWS 617, Columbia, SC 29208, USA
Christopher George St. Clement Kendall
Affiliation:
Department of Earth and Ocean Sciences, University of South Carolina, 701 Sumter Street, EWS 617, Columbia, SC 29208, USA
*
*Corresponding author.E-mail addresses:wdoar@yahoo.com (W.R. Doar), kendall@geol.sc.edu (C.G.S.C. Kendall).
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Abstract

Geological maps of South Carolina, covering >6800 km2, confirm the existence of eight preserved Pleistocene shorelines above current sea level: Marietta (+ 42.6 m), Wicomico (+ 27.4 m), Penholoway (+ 21.3 m), Ladson (+ 17.4 m), Ten Mile Hill (+ 10.7 m), Pamlico (+ 6.7 m), Princess Anne (+ 5.2 m), and Silver Bluff (+ 3 m). Current geochronologic data suggest that these eight shorelines correlate with Marine Oxygen Isotope Stages (MIS) as follows: Marietta—older than MIS 77; Wicomico—MIS 55–45; Penholoway—MIS 19 or 17; Ladson—MIS 11; Ten Mile Hill—MIS 7; Pamlico—MIS 5; Princess Anne—MIS 5; and Silver Bluff—MIS 5 or 3. Except for the MIS 5e Pamlico, and possibly the MIS 11 Ladson, the South Carolina elevations are higher than predicted by isotope proxy-based reconstructions. The <4 m of total relief from the Pamlico to the Silver Bluff shoreline in South Carolina, for which other reconstructions suggest an expected relief of ~ 80 m, illustrates the lack of match. Our results suggest that processes affecting either post-depositional changes in shoreline elevations or the creation of proxy sea-level estimates must be considered before using paleo sea-level position on continental margins.

Keywords

Pleistocene stratigraphySea-level reconstructionsIsostatic adjustmentMarine Oxygen Isotope StagesGeologic mappingShorelines
Type
Articles
Information
Quaternary Research , Volume 82 , Issue 1 , July 2014 , pp. 164 - 174
Copyright
University of Washington

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