Abstract
Our primary objective was to develop an understanding of the geomorphic evolution of Whiteoak Bottoms (WOB), a peatland along the Nantahala River in the Southern Blue Ridge Mountains (SBRM) of western North Carolina. Radiocarbon dates directly above basal fluvial sediments returned ages of 14,000 to 15,000 cal yr BP. These ages indicate WOB is the oldest dated peatland in the SBRM and that such wetlands have persisted throughout the Holocene. Below the relatively flat surface of the wetland, paleochannels, similar to those of the modern channel, were found; suggesting a persistence of similar channel morphology since the terminal Pleistocene. The wetland’s stratigraphy reveals a consistent pattern with basal fluvial cobbles being overlain by sandy channel-fill grading up into peat. Two different distinct inorganic deposits separate the lower organic deposits from the sapric peat deposits at the surface. Interestingly, we estimate more than 56% of the organic matter preserved by the wetland accumulated during the first 6,000 years of development. Overall, WOB has accumulated approximately 424 Mg/ha of carbon during the past 15,000 years. Maintenance of this wetland initially depended on the Nantahala River; however, today it is ground water and beavers that allows for the persistence of this rare landscape.
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References
Autin WJ (1992) Use of alloformations for definition of Holocene meander belts in the middle Amite River, southeastern Louisiana. Geological Society of America Bulletin 104:233–241
Bendix J, Hupp CR (2000) Hydrological and geomorphological impacts on riparian plant communities. Hydrological Processes 14:2977–2990
Clark KL, Gholz HL, Castro MS (2004) Carbon dynamics along a chronosequence of slash pine plantations in north Florida. Ecological Applications 14:1154–1171
Delcourt PA, Delcourt HR (1984) Late Quaternary paleoclimates and biotic responses in eastern North America and the western North Atlantic Ocean. Palaeogeography, Palaeoclimatology, Palaeoecology 48:263–284
Delcourt HR, Delcourt PA (2004) Prehistoric Native Americans and ecological change: human ecosystems in eastern North America since the Pleistocene. Cambridge University Press, Cambridge
Eaton LS, Morgan BA, Kochel RC, Howard AD (2003) Quaternary deposits and landscape evolution of the central Blue Ridge of Virginia. Geomorphology 56:139–154
Gaddy LL (1981) The bogs of the southwestern mountains of North Carolina. Department of Environment and Natural Resources, Office of Natural Resource Planning and Conservation, North Carolina Natural Heritage Program. Raleigh, NC.
Gee GW, Bauder JW (1986) Particle size analysis. In: Klute A (ed) Methods of soil analysis: part I, physical and mineralogical methods, 2nd edn. American Society of Agronomy - Soil Science Society of America, Madison, pp 383–411
Goman M, Leigh DS (2004) Wet Early to Middle Holocene conditions on the upper Coastal Plain of North Carolina, USA. Quaternary Research 61:256–264
Heiri O, Lotter AF, Lemcke G (2001) Loss on ignition as a method for estimating organic and carbonate content in sediments: reproducibility and comparability of results. Journal of Paleolimnology 25:101–110
Hupp CR, Osterkamp WR (1996) Riparian vegetation and fluvial geomorphic processes. Geomorphology 14:277–295
Johnson LC, Damman AWH (1991) Species-controlled sphagnum decay on a South Swedish raised bog. Oikos 61:234–242
Kneller M, Peteet D (1999) Late-Glacial to Early Holocene climate changes from a Central Appalachian pollen and macrofossil record. Quaternary Research 51:133–147
LaMoreaux HK, Brook GA, Knox JA (2009) Late Pleistocene and Holocene environments of the Southeastern United States from the stratigraphy and pollen content of a peat deposit on the Georgia Coastal Plain. Palaeogeography, Palaeoclimatology, Palaeoecology 280:300–312
Leigh DS (2006) Terminal Pleistocene braided to meandering transition in rivers of the Southeastern USA. Catena 66:155–160
Leigh DS (2008) Late Quaternary climates and river channels of the Atlantic Coastal Plain, Southeastern USA. Geomorphology 101:90–108
Leigh DS (2010) Morphology and channel evolution of small streams in the southern Blue Ridge Mountains of Western North Carolina. Southeastern Geographer 50:397–421
Leigh DS, Webb PA (2006) Holocene erosion, sedimentation, and stratigraphy at Raven Fork, Southern Blue Ridge Mountains, USA. Geomorphology 78:161–177
Liang F (2008) Monsoonal climate change during the Holocene: speleothem evidence from Southwestern China, Northern India, and the Southeastern USA. Dissertation, University of Georgia
Liu J, Liu S, Loveland TR (2006) Temporal evolution of carbon budgets of the Appalachian forests in the U.S. from 1972 to 2000. Forest Ecology and Management 222:191–201
Lizee TR, Manooch CS, Young RS (1998) Saprolite-controlled, wetland geomorphology: an example from Flat Laurel Gap in the North Carolina Blue Ridge. Geological Society of America Abstracts with Programs 30:139
Miller JO, Galbraith JM, Daniels WL (2004) Soil organic carbon content in frigid Southern Appalachian Mountain soils. Soil Science Society of America Journal 68:194–203
Moorhead KK, Moynihan RE, Simpson SL (2000) Soil characteristics of four Southern Appalachian fens in North Carolina, USA. Wetlands 20:560–564
Murdock NA (1994) Rare and endangered plants and animals of Southern Appalachian wetlands. Water, Air, and Soil Pollution 77:385–405
Naiman RJ, Johnston CA, Kelley JC (1988) Alteration of North American streams by beaver. BioScience 38:753–762
North American Commission on Stratigraphic Nomenclature (2005) North American stratigraphic code. American Association of Petroleum Geologists Bulletin 89:1547–1591
Osterkamp WR, Hupp CR (1984) Geomorphic and vegetative characteristics along three northern Virginia streams. Geological Society of America Bulletin 95:1093–1101
Pittillo DJ (1994) Vegetation of three high elevation southern Appalachian bogs and implications of their vegetational history. Water, Air, and Soil Pollution 77:333–348
Powers MC (1953) A new roundness scale for sedimentary particles. Journal of Sedimentary Research 23:117–119
PRISM Climate Group (1895–2009) http://gisdev.nacse.org/prism/nn/. Accessed June 22, 2010.
Robinson GRJ, Lesure FG, Marlowe JII, Foley NK, Clark SH (1992) Bedrock geology and mineral resources of the Knoxville 1 degree by 2 degrees quadrangle, Tennessee, North Carolina, and South Carolina, United States Geological Society
Schafale MP, Weakley AS (1990) Classification of the natural communities of North Carolina, third approximation. Department of Environment and Natural Resources, Office of Natural Resource Planning and Conservation, North Carolina Natural Heritage Program. Raleigh, NC
Schwartzman, E (2010) An inventory of the natural areas of Macon County, North Carolina. Department of Environment and Natural Resources, Office of Natural Resource Planning and Conservation, North Carolina Natural Heritage Program. Raleigh, NC
SERCC (12/1/1942 to 12/31/2007) Climate data for Coweeta Exp Stn, North Carolina. http://www.sercc.com/cgi-bin/sercc/cliMAIN.pl?nc2102. Accessed March 20, 2009.
Shafer DS (1986) Flat Laurel Gap bog, Pisgah Ridge, North Carolina: Late Holocene development of a high-elevation heath bald. Castanea 51:1–10
Shafer DS (1988) Late Quaternary landscape evolution at Flat Laurel Gap, Blue Ridge Mountains, North Carolina. Quaternary Research 30:7–11
Soil Survey Division Staff (1993) Soil survey manual. U.S. Government Printing Office, Washington, DC
Tanner BR, Kinner D, Barbour S, Young R (2010) Radiocarbon dates reveal a high elevation, early Holocene wetland deposit in the Southern Appalachian Mountains. Geological Society of America Abstracts with Programs 42:188
Vitt DH, Wieder RK (2009) The structure and function of bryophyte-dominated peatlands. In: Goffinet B, Shaw AJ (eds) Bryophyte biology. Cambridge University Press, Cambridge, pp 357–391
Walter RC, Merritts DJ (2008) Natural streams and the legacy of water-powered mills. Science 319:299–304
Warren RJ, Pittillo DJ, Rossell IM (2004) Vascular flora of a Southern Appalachian fen and floodplain complex. Castanea 69:116–124
Weakley AS, Schafale MP (1994) Non-alluvial wetlands of the Southern Blue Ridge — Diversity in a threatened ecosystem. Water, Air, and Soil Pollution 77:359–383
Weishampel P, Kolka R, King JY (2009) Carbon pools and productivity in a 1-km2 heterogeneous forest and peatland mosaic in Minnesota, USA. Forest Ecology and Management 257:747–754
Acknowledgments
We thank all of the field and lab assistants that helped obtaining our data. Funding in support of this research came from the National Science Foundation (DEB-0823293) in support of the Coweeta LTER program. The U.S.D.A. Forest Service granted permission to conduct this research, for which we are grateful.
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McDonald, J.M., Leigh, D.S. Terminal Pleistocene through Holocene Evolution of Whiteoak Bottoms, a Southern Blue Ridge Mountains Peatland. Wetlands 31, 783–797 (2011). https://doi.org/10.1007/s13157-011-0195-2
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DOI: https://doi.org/10.1007/s13157-011-0195-2