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Burning peat and reworking loess contribute to the formation and evolution of a large Carolina-bay basin

Published online by Cambridge University Press:  20 January 2017

Antonio B. Rodriguez ,
Matthew N. Waters  and
Michael F. Piehler
Antonio B. Rodriguez*
Affiliation:
Institute of Marine Sciences, University of North Carolina at Chapel Hill, Morehead City, NC 28557, USA
Matthew N. Waters
Affiliation:
Department of Biology, Valdosta State University, Valdosta, GA 31698, USA
Michael F. Piehler
Affiliation:
Institute of Marine Sciences, University of North Carolina at Chapel Hill, Morehead City, NC 28557, USA
*
*Corresponding author. Fax: + 1 252 726 2426. E-mail address:abrodrig@email.unc.edu (A.B. Rodriguez).
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Abstract

Carolina bays are nearly ubiquitous along ~ 1300 km of the North American Atlantic Coastal Plain, but relatively few bays have been examined in detail, making their formation and evolution a topic of controversy. The Lake Mattamuskeet basin, eastern North Carolina, USA, is a conglomeration of multiple Carolina bays that form a > 162 km2 lake. The eastern shoreline of the lake is made up of a 2.9-km-wide plain of parabolic ridges that recorded rapid shoreface progradation. The lower shoreface deposit contains abundant charcoal beds and laminae dated 6465–6863 cal yr BP, corresponding with initiation of a lacustrine environment in the eastern part of the lake. A core from the western part of the lake sampled a 1541–1633 cal yr BP charcoal bed at the base of the lacustrine unit, indicating formation of this part of the basin postdates the eastern basin. Lake Mattamuskeet has no relationship to the Younger Dryas or a linked impact event because rim accretion significantly postdates 12,000 cal yr BP. The shoreline progradation, and association of charcoal beds with the oldest lake sediment in both main parts of the basin, suggest that fire and subsequent hydrodynamic processes were associated with initial formation of these Carolina bays.

Keywords

Carolina bayLoessYounger DryasClimate changeFireEolianPeat

Information

Type
Original Articles
Information
Quaternary Research , Volume 77 , Issue 1 , January 2012 , pp. 171 - 181
Copyright
University of Washington

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References

Ashton, A.D., Murray, A.B., Littlewood, R., Lewis, D.A., Hong, P., (2009). Fetch-limited self-organization of elongate water bodies. Geology 37, 187–190.Google Scholar
Barefoot, D.W., (1995). Touring the Backroads of North Carolina's Upper Coast. John F. Blair Publishing, Winston-Salem.Google Scholar
Bliley, D.J., Burney, D.A., (1988). Late Pleistocene climatic factors in the genesis of a Carolina bay. Southeastern Geology 29, 83–101.Google Scholar
Bliley, D.J., Pettry, D.E., (1979). Carolina bays of the eastern shore of Virginia. Soil Science Society of America Journal 43, 558–564.Google Scholar
Brill, A. L., (1996). The Suffolk Scarp: a Pleistocene barrier island in Beaufort and Pamlico Counties. Unpublished Master's thesis, Duke University.Google Scholar
Brooks, M.J., Taylor, B.E., Grant, J.A., (1996). Carolina bay geoarchaeology and Holocene landscape evolution on the upper coastal plain of South Carolina. Geoarchaeology 11, 481–504.Google Scholar
Carver, R.E., Brook, G.A., (1989). Late Pleistocene paleowind directions, Atlantic Coastal Plain, U.S.A.. Palaeogeography, Palaeoclimatology, Palaeoecology 74, 205–216.CrossRefGoogle Scholar
Cohen, A.D., (1979). Peat Deposits of the Albemarle"Pamlico Peninsula. pp. 49 North Carolina Energy Institute, Raleigh.Google Scholar
Culver, S.J., Grand Pre, C.A., Mallinson, D.J., Riggs, S.R., Corbett, D.R., Foley, J., Hale, M., Metger, L., Ricardo, J., Rosenberger, J., Smith, C.G., Smith, C.W., Snyder, S.W., Twamley, D., (2007). Late Holocene barrier island collapse: Outer Banks, North Carolina, USA. The Sedimentary Record 5, 4–8.Google Scholar
Firestone, R.B., West, A., Kennett, J.P., Becker, L., Bunch, T.E., Revay, Z.S., Schultz, P.H., Belgya, T., Kennett, D.J., Erlandson, J.M., Dickenson, O.J., Goodyear, A.C., Harris, R.S., Howard, G.A., Kloosterman, J.B., Lechler, P., Mayewski, P.A., Montgomery, J., Poreda, R., Darrah, T., Que Hee, S.S., Smith, A.R., Stich, A., Topping, W., Wittke, J.H., Wolbach, W.S., (2007a). Evidence for an extraterrestrial impact event 12,900 years ago that led to megafaunal extinctions and the onset of the Younger Dryas cooling. Proceedings of the National Academy of Sciences 104, 16016–16021.Google Scholar
Firestone, R.B., West, A., Revay, Z., Belgya, T., Smith, A., Que Hee, S., (2007b). Evidence for a massive extraterrestrial airburst over North America 12.9 ka ago. Eos (Transactions, American Geophysical Union) 88, Abstract PP41A-01.Google Scholar
Fisher, T.G., Loope, W.L., Pierce, W., Jol, H.M., (2007). Big lake records preserved in a little lake's sediment: an example from Silver Lake, Michigan, USA. Journal of Paleolimnology 37, 365–382.Google Scholar
Forman, S.L., Oglesby, R., Markgraf, V., (1995). Paleoclimatic significance of Late Quaternary eolian deposition on the Piedmont and High Plains, Central United States. Global and Planetary Change 11, 35–55.CrossRefGoogle Scholar
Forrest, L.C., (2000). Lake Mattamuskeet: New Holland and Hyde County. Arcadia Publishing, Charleston.Google Scholar
Foss, J.E., Fanning, D.S., Miller, F.P., Wagner, D.P., (1978). Loess deposits of the eastern shore of Maryland. Soil Science Society of America Journal 42, 329–333.CrossRefGoogle Scholar
Gaiser, E.E., Taylor, B.E., Brooks, M.J., (2001). Establishment of wetlands on the southeastern Atlantic Coastal Plain: paleolimnological evidence of a mid-Holocene hydrologic threshold from a South Carolina pond. Journal of Paleolimnology 26, 373–391.CrossRefGoogle Scholar
Gamble, E.E., Daniels, R.B., Wheeler, W.H., (1977). Primary and secondary rims of Carolina bays. Southeastern Geology 18, 199–212.Google Scholar
Goman, M., Leigh, D.S., (2004). Wet early to middle Holocene conditions on the upper coastal plain of North Carolina. Quaternary Research 61, 256–264.Google Scholar
Grant, J.A., Brooks, M.J., Taylor, B.E., (1998). New constraints on the evolution of Carolina bays from ground penetrating radar. Geomorphology 22, 325–345.CrossRefGoogle Scholar
Heiri, O., Lotter, A.F., Lemcke, G., (2001). Loss on ignition as a method for estimating organic and carbonate content in sediments: reproducibility and comparability of resuts. Journal of Paleolimnology 25, 101–110.Google Scholar
Horton, B.P., Peltier, W.R., Culver, S.J., Drummond, R., Engelhart, S.E., Kemp, A.C., Mallinson, D., Thieler, E.R., Riggs, S.R., Ames, D.V., Thomson, K.H., (2009). Holocene sea-level changes along the North Carolina coastline and their implications for glacial isostatic adjustment models. Quaternary Science Reviews 28, 1725–1736.Google Scholar
Ingram, R.L., (1987). Peat Deposits of North Carolina. North Carolina Geological Survey, Bulletin 88, Raleigh.Google Scholar
Ivester, A.H., Brooks, M.J., Taylor, B.E., (2007). Sedimentology and ages of Carolina bay sand rims. Geological Society of America Abstracts with Programs 39, 5.Google Scholar
Johnson, D., (1942). The Origin of the Carolina Bays. Columbia University Press, New York.Google Scholar
Kaczorowski, R.T., (1977). The Carolina bays and their relationship to modern oriented lakes (abs.). Geological Society of America Bulletin 9, 151–152.Google Scholar
Kennett, D.J., Kennett, J.P., West, A., Mercer, C., Que Hee, S.S., Bement, L., Bunch, T.E., Sellers, M., Wolbach, W.S., (2009a). Nanodiamonds in the Younger Dryas boundary sediment layer. Science 323, 94.CrossRefGoogle ScholarPubMed
Kennett, D.J., Kennett, J.P., West, A., West, G.J., Bunch, T.E., Culleton, B.J., Erlandson, J.M., Que Hee, S.S., Johnson, J.R., Mercer, C., Shen, F., Sellers, M., Stafford jr., T.W., Stich, A., Weaver, J.C., Wittke, J.H., Wolbach, W.S., (2009b). Shock-synthesized hexagonal diamonds in Younger Dryas boundary sediments. Proceedings of the National Academy of Sciences 106, 12623–12628.Google Scholar
LeGrand, H.E., (1953). Streamlining of the Carolina bays. The Journal of Geology 61, 263–274.Google Scholar
Mallinson, D., Burdette, K., Mahan, S., Brook, G., (2008). Optically stimulated luminescence age controls on late Pleistocene and Holocene coastal lithosomes, North Carolina, USA. Quaternary Research 69, 97–109.CrossRefGoogle Scholar
Markewich, H.W., Markewich, W., (1994). An overview of Pleistocene and Holocene inland dunes in Georgia and the Carolinas – morphology, distribution, age, and paleoclimate. U.S. Geological Survey Bulletin 2069, 1–32.Google Scholar
Mason, J.A., (2001). Transport direction of Peoria Loess in Nebraska and implications for loess sources on the central Great Plains. Quaternary Research 56, 79–86.CrossRefGoogle Scholar
Mason, J.A., Jacobs, P.M., Hanson, P.R., Miao, X., Goble, R.J., (2003). Sources and paleoclimatic significance of Holocene Bignell Loess, central Great Plains, USA. Quaternary Research 60, 330–339.Google Scholar
May, J.H., Warne, A.G., (1999). Hydrologic and geochemical factors required for the development of Carolina bays along the Atlantic and Gulf of Mexico coastal plain, USA. Environmental and Engineering Geosience 5, 261–270.CrossRefGoogle Scholar
Miao, X., Mason, J.A., Swinehart, J.B., Loope, D.B., Hanson, P.R., Goble, R.J., Liu, X., (2007). A 10,000 year record of dune activity, dust storms, and severe drought in the central Great Plains. Geology 35, 119–122.Google Scholar
Moorhead, K.K., Brinson, M.M., (1995). Response of wetlands to rising sea level in the lower coastal plain of North Carolina. Ecological Applications 5, 261–271.Google Scholar
Neal, A., (2004). Ground-penetrating radar and its use in sedimentology: principles, problems and progress. Earth-Science Reviews 66, 261–330.CrossRefGoogle Scholar
Otvos, E.G., (2004). Prospects for interregional correlations using Wisconsin and Holocene aridity episodes, northern Gulf of Mexico coastal plain. Quaternary Research 61, 105–118.Google Scholar
Pinter, N., Ishman, S.E., (2008). Impacts, mega-tsunami, and other extraordinary claims. GSA Today 18, 37–38.Google Scholar
Price, W.A., (1968). Carolina bays. Fairbridge, R.W., Encyclopedia of Geomorphology. Reinhold Book Corporation, New York. 102–108.Google Scholar
Prouty, W.F., (1952). Carolina bays and their origin. Bulletin of the Geological Society of America 63, 167–224.Google Scholar
Riggs, S.R., York, L.L., Wehmiller, J.F., Snyder, S.W., (1992). Depositional patterns resulting from high-frequency Quaternary sea-level fluctuations in northeastern North Carolina. Fletcher, C.H., Wehmiller, J.F., Quaternary Coasts of the United States: Marine and Lacustrine Systems. SEPM Special Publication, SEPM. 141–153.Google Scholar
Savage jr., H., (1982). The Mysterious Carolina Bays. University of South Carolina Press, Columbia.Google Scholar
Simonson, R.W., (1982). Loess in soils of Delaware, Maryland, and northeastern Virginia. Soil Science 133, 167–178.Google Scholar
Siple, G.E., (1960). Some geologic and hydrologic factors affecting limestone terrains of Tertiary Age in South Carolina. Southeastern Geology 2, 1–11.Google Scholar
Smalley, I., (1995). Making the material: the formation of silt-sized primary mineral particles for loess deposits. Quaternary Science Reviews 14, 645–651.Google Scholar
Stahle, D.W., Cleaveland, M.K., Hehr, J.G., (1988). North Carolina climate changes reconstructed from tree rings: A.D. 372 to 1985. Science 240, 1517–1519.Google Scholar
Stolt, M.H., Rabenhorst, M.C., (1987a). Carolina bays on the eastern shore of Maryland: II. Distribution and origin. Soil Science Society of America Journal 51, 399–405.Google Scholar
Stolt, M.H., Rabenhorst, M.C., (1987b). Carolina bays on the eastern shore of Maryland: I. Soil characterization and classification. Soil Science Society of America Journal 51, 394–398.Google Scholar
Stuiver, M., Reimer, P.J., (1993). Extended 14C database and revised CALIB radiocarbon calibration program. Radiocarbon 35, 215–230.Google Scholar
Surovell, T.A., Holliday, V.T., Gingerich, J.A.M., Ketron, C., Haynes jr., C.V., Hilman, I., Wagner, D.P., Johnson, E., Claeys, P., (2009). An independent evaluation of the Younger Dryas extraterrestrial impact hypothesis. Proceedings of the National Academy of Sciences 106, 18155–18158.Google Scholar
Thom, B.G., (1970). Carolina bays in Horry and Marion counties, South Carolina. Geological Society of America Bulletin 81, 783–814.Google Scholar
Waters, M.N., Piehler, M.F., Rodriguez, A.B., Smoak, J.M., Bianchi, T.S., (2009). Shallow lake trophic status linked to late Holocene climate and human impacts. Journal of Paleolimnology 42, 51–64.CrossRefGoogle Scholar
Waters, M.N., Piehler, M.F., Smoak, J., Martens, C., (2010). The development and persistence of alternative ecosystem states in a large, shallow lake. Freshwater Biology 55, 1249–1261.Google Scholar
Wehmiller, J.F., Simmons, K.R., Cheng, H., Edwards, R.L., Martin-McNaughten, J., York, L.L., Krantz, D.E., Shen, C.C., (2004). Uranium-series coral age from the US Atlantic Coastal Plain – the "80 ka problem" revisited. Quaternary International 120, 3–14.CrossRefGoogle Scholar
Whalley, W.B., Marshal, J.R., Smith, B.J., (1982). Origin of desert loess from some experimental observations. Science 300, 433–435.Google Scholar
Whitehead, D.R., (1972). Developmental and environmental history of the Dismal Swamp. Ecological Monographs 42, 301–315.Google Scholar
Whitehead, D.R., (1981). Late-Pleistocene vegetational changes in northeastern North Carolina. Ecological Monographs 51, 451–471.Google Scholar