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Evidence for multiple, episodic, mid-Holocene Hypsithermal recorded in two soil profiles along an alluvial floodplain catena, southeastern Tennessee, USA

Published online by Cambridge University Press:  20 January 2017

Steven G. Driese ,
Zheng-Hua Li  and
Larry D. McKay
Steven G. Driese*
Affiliation:
Department of Geology, One Bear Place #97354, Baylor University, Waco, TX 76798-7354, USA
Zheng-Hua Li
Affiliation:
Department of Earth and Planetary Sciences, University of Tennessee, Knoxville, TN 37996-1410, USA
Larry D. McKay
Affiliation:
Department of Earth and Planetary Sciences, University of Tennessee, Knoxville, TN 37996-1410, USA
*
*Corresponding author. Fax: +1 254 710 2673.E-mail address:Steven_Driese@baylor.edu (S.G. Driese).
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Abstract

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Floodplain soil–paleosol successions are valuable archives for reconstructing Pleistocene–Holocene climate changes but have been relatively unstudied in the southern Appalachian region. Two soil profiles on a small floodplain in southeastern Tennessee, USA were described and sampled in detail using both pedological and geological approaches, including stable carbon isotope analysis of soil organic matter (SOM). Correlation between the 2 profiles was constrained by uncalibrated AMS14C ages of bulk humates, and using SOM δ13C values, both mobile and immobile elements. Four distinct 2.5–4‰ shifts towards less negative δ13C values for SOM suggest ∼ 300-yr cyclicity and transient warmer and drier climate events, with either water-stressed C3vegetation or as much as 35% C4plants present during the mid-Holocene. These postulated multi-episodic drier climate conditions have never before been documented in the southern Appalachian region and are tentatively correlated with mid-Holocene warming and drying in the eastern US, the nearly time-equivalent mid-Holocene events documented in Texas, the US High Plains and in the Gulf of Mexico. High rates of floodplain sediment accumulation (0.5–3 mm/yr), high clay content and maintenance of poorly drained soil conditions favor preservation of high-resolution climate archives in floodplain deposits by inhibiting oxidation and translocation of organic C.

Keywords

PaleoclimateMid-Holocene soilsStable carbon isotopesSoutheastern USFloodplains
Type
Original Articles
Information
Quaternary Research , Volume 69 , Issue 2 , March 2008 , pp. 276 - 291
Copyright
Elsevier Inc.

References

Accoe, F., Boeckx, P., Van Cleemput, O., Hofman, G., Zhang, Y., Li, R.-H., Guanxiong, C., (2002). Evolution of the δ13C signature related to total carbon contents and carbon decomposition rate constants in a soil profile under grassland. Rapid Communications in Mass Spectrometry 16, 2184–2189.CrossRefGoogle Scholar
Aslan, A., Autin, W.J., (1998). Holocene flood-plain soil formation in the southern lower Mississippi Valley: implications for interpreting alluvial paleosols. Geological Society of America Bulletin 110, 433–449.Google Scholar
Aslan, A., Autin, W.J., (1999). Evolution of the Holocene Mississippi River floodplain, Ferriday, Louisiana: insights on the origin of fine-grained floodplains. Journal of Sediementary Research 69, 800–815.Google Scholar
Birkeland, P.W., (1999). Topography—soil relations with time in different climatic settings. Soils and Geomorphology 3rd ed. Oxford University Press, New York., 230–267.Google Scholar
Blake, G.R., Hartge, K.H., (1986). Bulk density. Klute, A., 2nd ed. Methods of Soil Analysis, Part I. Physical and Mineralogical Methods. Soil Science Society of America Agronomy Monograph vol. 9, Soil Science Society of America, Madison, WI., 363–375.Google Scholar
Blokhuis, W.A., Kooistra, M.J., Wilding, L.P., (1990). Micromorphology of cracking clayey soils (Vertisols). Douglas, L.A., Soil Micromorphology: a Basic and Applied Science. Developments in Soil Science 19, Elsevier Pub. Co., New York., 123–148.Google Scholar
Boutton, T.W., (1996). Stable carbon isotope ratios of soil organic matter and their use as indicators of vegetation and climate change. Boutton, T.W., Yamasaki, S., Mass Spectrometry of Soils. Dekker, New York., 47–82.Google Scholar
Boutton, T.W., Nordt, L.C., Archer, S.R., Midwood, A.J., Casar, I., (1993). Stable carbon isotope ratios of soil organic matter and their potential use as indicators of paleoclimate. Isotope Techniques in the Study of Past and Current Environmental Changes in the Hydrosphere and the Atmosphere. International Atomic Energy Agency, Vienna 445–459.Google Scholar
Brewer, R., (1976). Fabric and Mineral Analysis of Soils. 2nd edition Krieger Pub. Co., New York., .Google Scholar
Bullock, P., Fédoroff, N., Jungerius, A., Stoops, G., Tursina, T., (1985). Handbook of Soil Thin Section Description. Waine Research Publications, Albrighton, UK., .Google Scholar
Cerling, T.E., Ehleringer, J.L., (2000). Welcome to the C4 world. Gastaldo, R.A., DiMichele, W.A., Phanerozoic Terrestrial Ecosystems, A Short Course. The Paleontological Society Papers 6, The Paleontological Society, New Haven, CT., 273–286.Google Scholar
Delcourt, H.R., (1979). Late Quaternary vegetation history of the eastern Highland Rim and adjacent Cumberland Plateau of Tennessee. Ecological Monographs 49, 255–280.CrossRefGoogle Scholar
Driese, S.G., Mora, C.I., Stiles, C.A., Joeckel, R.M., Nordt, L.C., (2000). Mass-balance reconstruction of a modern Vertisol: implications for interpreting the geochemistry and burial alteration of paleo-Vertisols. Geoderma 95, 179–204.CrossRefGoogle Scholar
Driese, S.G., Jacobs, J.R., Nordt, L.C., (2003). Comparison of modern and ancient Vertisols developed on limestone in terms of their geochemistry and parent material. Sedimentary Geology 157, 49–69.Google Scholar
Driese, S.G., Li, Z.-H., Horn, S.P., (2005). Late Pleistocene to Holocene paleoclimate and paleogeomorphic history interpreted from 23,000 14C yr B.P. paleosol and floodplain soils, southeastern West Virginia, USA. Quaternary Research 63, 136–149.CrossRefGoogle Scholar
Dwyer, T.R., Mullins, H.T., Good, S.C., (1996). Paleoclimatic implications of Holocene lake-level fluctuations, Owasco Lake, New York. Geology 24, 519–522.Google Scholar
Fitzpatrick, E.A., (1993). Soil Microscopy and Micromorphology. New York, John Wiley and Sons., .Google Scholar
Goman, M., Leigh, D.S., (2004). Wet early to middle Holocene conditions on the upper Coastal Plain of North Carolina, USA. Quaternary Research 61, 256–264.Google Scholar
Harrison, S.P., Kutzbach, J.E., Liu, Z., Bartlein, P.J., Otto-Bliesner, B., Muhs, D., Prentice, I.C., Thompson, R.S., (2003). Mid-Holocene climates of the Americas: a dynamical response to changed seasonality. Climate Dynamics 20, 663–688.Google Scholar
Hurt, G.W., Whited, P.M., Pringle, R.F., (1998). Field Indicators of Hydric Soils in the United States. Natural Resources Conservation Service, Version 4.0 US Department of Agriculture, .Google Scholar
Jackson, B.W., (1982). Soil Survey of Hamilton County, Tennessee. U.S. Department of Agriculture, Natural Resources Conservation Service.Google Scholar
Johnson, W.C., Willey, K.L., Macpherson, G.L., (2007). Carbon isotope variation in modern soils of the tallgrass prairie: analogues for the interpretation of isotopic records derived from paleosols. Quaternary International 162–163, 3–20.Google Scholar
Leigh, D.S., Feeney, T.P., (1995). Paleochannels indicating wet climate and lack of response to lower sea level, southeast Georgia. Geology 23, 687–690.Google Scholar
Lund, S., Curry, W.B., (2004). Late Holocene variability in Florida Current surface density: patterns and possible causes. Paleoceanography 19, 4, PA4001. doi: 10.1029/2004PA001008.Google Scholar
Luther, E.T., (1979). Geology of Hamilton County, Tennessee. Bulletin 79, Tennessee Division of Geology, Nashville., .Google Scholar
Meltzer, D.J., (1999). Human responses to Middle Holocene (Altithermal) climates on the North American Great Plains. Quaternary Research 52, 404–416.Google Scholar
Nordt, L.C., Boutton, T.W., Hallmark, C.T., Waters, M.R., (1994). Late Quaternary vegetation and climate change in Central Texas based on the isotopic composition of organic carbon. Quaternary Research 41, 109–120.CrossRefGoogle Scholar
Nordt, L.C., Boutton, T.W., Jacob, J.S., Mandel, R.D., (2002). C4 plant productivity and climate-CO2 variations in south-central Texas during the Quaternary. Quaternary Research 58, 182–188.Google Scholar
Nordt, L., Wilding, L., Lynn, W.L., Crawford, C., (2004). Vertisol genesis in a humid climate in the coastal plain of Texas. Geoderma 122, 83–102.CrossRefGoogle Scholar
PiPujol, M.O., Buurman, P., (1994). The distinction between ground-water gley and surface-water gley phenomena in tertiary paleosols of the Ebro basin, northeast Spain. Palaeogeography, Palaeoclimatology, Palaeoecology 110, 103–113.Google Scholar
Poore, R.Z., Dowsett, H.J., Verardo, S., Quinn, T.M., (2003). Millennial- to century-scale variability in Gulf of Mexico Holocene climate records. Paleoceanography 18, 2, 26–1:26–11.CrossRefGoogle Scholar
Poore, R.Z., Quinn, T.M., Verardo, S., (2004). Century-scale movement of the Atlantic Intertropical Convergence Zone linked to solar variability. Geophysical Research Letters 31, L12214, .Google Scholar
Richey, J.N., Poore, R.Z., Flower, B.P., Quinn, T.M., (2007). 1400 yr multiproxy record of climate variability from the northern Gulf of Mexico. Geology 35, 423–426.Google Scholar
Singer, M.J., Janitzky, P., (1986). Field and laboratory procedures used in a soil chronosequence study. US Geological Survey Bulletin 1648, 49 p.Google Scholar
Soil Survey Staff, , Soil Survey Laboratory Information Manual: Soil Survey Investigations Report 42, US Government Printing Office, Washington, D.C., Version 3.0.Google Scholar
Soil Survey Staff, , (1998). Keys to Soil Taxonomy. 8th edition US Government Printing Office, Washington, D.C.., .Google Scholar
Stichler, W., (1995). Interlaboratory Comparison of New Materials for Carbon and Oxygen Isotope Ratio Measurements. Reference and Intercomparison Materials for Stable Isotopes of Light Elements. International Atomic Agency, Vienna, Austria., 67–74.,IAEA TECDOC-825.Google Scholar
Stoops, G., (2003). Guidelines for Analysis and Description of Soil and Regolith Thin Sections. Madison, WI, Soil Science Society of America., .Google Scholar
Vepraskas, M.J., Wilding, L.P., (1983a). Aquic moisture regimes in soils with and without low chroma colors. Soil Science Society of America Journal 47, 280–285.CrossRefGoogle Scholar
Vepraskas, M.J., Wilding, L.P., (1983b). Albic neoskeletans in argillic horizons as indices of seasonal saturation and iron reduction. Soil Science Society of America Journal 47, 1202–1208.Google Scholar
Vepraskas, M.J., (1992). Redoximorphic Features for Identifying Aquic Conditions. Technical Bulletin 301, North Carolina Agricultural Research Service, Raleigh, NC., .Google Scholar
Vepraskas, M.J., (2001). Morphological features of seasonally reduced soils. Richardson, J.L., Vepraskas, M.J., Wetland Soils: Genesis, Hydrology, Landscapes, and Classification. Lewis Publishers, New York., 163–182.Google Scholar
Vepraskas, M.J., Guertal, W.R., (1992). Morphological indicators of soil wetness. Kimble, J.M., Proceedings of the Eighth International Soil Correlation Meeting: Characterization, Classification, and Utilization of Wet Soils. USDA Soil Conservation Service, Lincoln, Nebraska., 307–312.Google Scholar
Vepraskas, M.J., Wilding, L.P., Drees, L.R., (1994). Aquic conditions for soil taxonomy: concepts, soil morphology and micromorphology. Ringrose-Voase, A.J., Humphreys, G.S., Soil Micromorphology: Studies in Management and Genesis. Developments in Soil Science 22. Elsevier Pub. Co., New York., 117–131.Google Scholar
Wang, H., Follmer, L.R., Liu, J.C., (2000a). Isotope evidence of paleo-El Niño-Southern Oscillation cycles in loess–paleosol record in the central United States. Geology 28, 771–774.Google Scholar
Wang, Y., Amundson, R., Niu, X., (2000b). Seasonal and altitudinal variation in decomposition of soil organic matter inferred from radiocarbon measurements of soil CO2 flux. Global Biogeochemical Cycles 14, 199–211.CrossRefGoogle Scholar
Webb, R.S., Anderson, K.H., Webb, T., (1993). Pollen response-surface estimates of Late Quaternary changes in the moisture balance of the northeastern United States. Quaternary Research 40, 213–227.CrossRefGoogle Scholar
Wilding, L.P., Tessier, D., (1988). Genesis of Vertisols: shrink–swell phenomena. Wilding, L.P., Puentes, R., Vertisols: Their Distribution, Properties, Classification and Management. Texas A & M University Printing Center, College Station, TX., 55–81.Google Scholar
Yu, Z., Ito, E., (1999). Possible solar forcing of century-scale drought frequency in the northern Great Plains. Geology 27, 263–266.Google Scholar