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Vegetation history in central Kentucky and Tennessee (USA) during the last glacial and deglacial periods

Published online by Cambridge University Press:  20 January 2017

Yao Liu ,
Jennifer J. Andersen ,
John W. Williams  and
Stephen T. Jackson
Yao Liu
Affiliation:
Department of Botany, University of Wyoming, Laramie, WY 82071, USA Program in Ecology, University of Wyoming, Laramie, WY 82071, USA
Jennifer J. Andersen
Affiliation:
Department of Botany, University of Wyoming, Laramie, WY 82071, USA
John W. Williams
Affiliation:
Department of Geography & Nelson Center for Climatic Research, University of Wisconsin, Madison, WI 53706, USA
Stephen T. Jackson*
Affiliation:
Department of Botany, University of Wyoming, Laramie, WY 82071, USA Program in Ecology, University of Wyoming, Laramie, WY 82071, USA
*
*Corresponding author at: DOI Southwest Climate Science Center, 1955 E. Sixth St., Tucson, AZ 85719, USA. E-mail address:[email protected] (S.T. Jackson).
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Abstract

Knowledge about vegetation dynamics during the last glacial and deglacial periods in southeastern North America is under-constrained owing to low site density and problematic chronologies. New pollen records from two classic sites, Anderson Pond, TN, and Jackson Pond, KY, supported by AMS 14C age models, span 25.2–13.7 ka and 31.0–15.4 ka, respectively. A transition from Pinus dominance to Picea dominance is recorded at Jackson Pond ca. 26.2 ka, ~ coincident with Heinrich Event H2. Anderson and Jackson Ponds record a transition from conifer to deciduous-tree dominance ~ 15.9 and 15.4 ka, respectively, marking the development of no-analog vegetation characterized by moderate to high abundances of Picea, Quercus, Carya, Ulmus, Fraxinus, Ostrya/Carpinus, Cyperaceae, and Poaceae, and preceding by ~ 2000 yr the advent of similar no-analog vegetation in glaciated terrain to the north. No-analog vegetation developed as a time-transgressive, south-to-north pattern, mediated by climatic warming. Sporormiella abundances are consistently low throughout the Jackson and Anderson Pond records, suggesting that megafaunal abundances and effects on vegetation varied regionally or possibly that the Sporormiella signal was not well-expressed at these sites. Additional records with well-constrained chronologies are necessary to assess patterns and mechanisms of vegetation dynamics during the last glacial and deglacial periods.

Keywords

Pollen recordsAnderson PondTNJackson PondKYNo-analog vegetationGlacial and deglacial periodsSoutheastern North America
Type
Research Article
Information
Quaternary Research , Volume 79 , Issue 2 , March 2013 , pp. 189 - 198
Copyright
University of Washington

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References

Aario, L. Waldgrenzen und subresenten Pollenspectren in Petsamo Lappland. Annales Acadamie Scientiarium Fennicae A 54, (1940). 1–120.Google Scholar
Blaauw, M. Methods and code for ‘classical’ age-modeling of radiocarbon sequences. Quaternary Geochronology 5, (2010). 512–518.CrossRefGoogle Scholar
Blaauw, M., and Christen, J.A. Flexible paleoclimate age-depth models using an autoregressive gamma process. Bayesian Analysis 6, (2011). 457–474.Google Scholar
Blois, J.L., Williams, J.W., Grimm, E.C., Jackson, S.T., and Graham, R.W. A methodological framework for assessing and reducing temporal uncertainty in paleovegetation mapping from late-Quaternary pollen records. Quaternary Science Reviews 30, (2011). 1926–1939.Google Scholar
Bromwich, D.H., Toracinta, E.R., Wei, H., Oglesby, R.J., Fastook, J.L., and Hughes, T.J. Polar MM5 simulations of the winter climate of the Laurentide Ice Sheet at the LGM. Journal of Climate 17, (2004). 3415–3433.Google Scholar
Bromwich, D.H., Toracinta, E.R., Oglesby, R.J., Fastook, J.L., and Hughes, T.J. LGM summer climate on the southern margin of the Laurentide Ice Sheet: wet or dry?. Journal of Climate 18, (2005). 3317–3338.Google Scholar
Delcourt, H.R., (1978). Late Quaternary vegetation history of the Eastern Highland Rim and adjacent Cumberland Plateau of Tennessee. Ph.D. Thesis, University of Minnesota, Minneapolis.Google Scholar
Delcourt, H.R. Late Quaternary vegetation history of the eastern Highland Rim and adjacent Cumberland Plateau of Tennessee. Ecological Monographs 49, (1979). 255–280.Google Scholar
Dyke, A.S., Moore, A., and Robertson, L. Deglaciation of North America. Open File Report 1574, 2 sheets. (2003). Geological Survey of Canada, Ottawa.Google Scholar
Etienne, D., Wilhelm, B., Sabatier, P., Reyss, J.-L., and Arnaud, F. Influence of sample location and livestock numbers on Sporormiella concentrations and accumulation rates in surface sediments of Lake Allos, French Alps. Journal of Paleolimnology (2012). http://dx.doi.org/10.1007/s10933-012-9646-xGoogle Scholar
Fenneman, N.M. Physiography of Eastern United States. (1938). McGraw-Hill, New York.Google Scholar
Gill, J.L., Williams, J.W., Jackson, S.T., Lininger, K.B., and Robinson, G.S. Pleistocene megafaunal collapse, novel plant communities, and enhanced fire regimes in North America. Science 326, (2009). 1100–1103.Google Scholar
Gill, J.L., Williams, J.W., Donnelly, J.P., Jackson, S.T., and Schellinger, G.C. Climatic and megaherbivore controls on late-glacial vegetation dynamics: a new, high-resolution, multi-proxy record from Silver Lake, Ohio. Quaternary Science Reviews 34, (2012). 66–80.Google Scholar
Gonzales, L.M., and Grimm, E.C. Synchronization of late-glacial vegetation changes at Crystal Lake, Illinois, USA with the North Atlantic Event Stratigraphy. Quaternary Research 72, (2009). 234–245.Google Scholar
Gonzales, L.M., Williams, J.W., and Grimm, E.C. Expanded response-surfaces: a new method to reconstruct paleoclimates from fossil pollen assemblages that lack modern analogues. Quaternary Science Reviews 28, (2009). 3315–3332.Google Scholar
Goring, S., Williams, J.W., Blois, J.L., Jackson, S.T., Paciorek, C.J., Booth, R.K., Marlon, J.R., Blaauw, M., and Christen, J.A. Deposition times in the northeastern United States during the Holocene: establishing valid priors for Bayesian age models. Quaternary Science Reviews 48, (2012). 54–60.Google Scholar
Grimm, E.C. CONISS: a FORTRAN 77 program for stratigraphically constrained cluster analysis by the method of incremental sum of squares. Computers & Geosciences 13, (1987). 13–35.Google Scholar
Grimm, E.C., Watts, W.A., Jacobson, G.L. Jr., Hansen, B.C.S., Almquist, H.R., and Dieffenbacher-Krall, A.C. Evidence for warm wet Heinrich events in Florida. Quaternary Science Reviews 25, (2006). 2197–2211.Google Scholar
Grimm, E.C., Maher, L.J. Jr., and Nelson, D.M. The magnitude of error in conventional bulk-sediment radiocarbon dates from central North America. Quaternary Research 72, (2009). 301–308.Google Scholar
Hussey, T.C., (1993). A 20,000-year record of vegetation and climate at Clear Pond, Northeastern South Carolina. M.S. thesis, University of Maine, Orono.Google Scholar
Jackson, S.T. Techniques for analysing unconsolidated lake sediments. Jones, T., and Rowe, N. Fossil Plants and Spores: Modern Techniques. (1999). Geological Society of London, London. 274–278.Google Scholar
Jackson, S.T., and Smith, S.J. Pollen dispersal and representation on an isolated, forested plateau. New Phytologist 128, (1994). 181–193.Google Scholar
Jackson, S.T., and Weng, C. Late Quaternary extinction of a tree species in eastern North America. Proceedings of the National Academy of Sciences 96, (1999). 13847–13852.Google Scholar
Jackson, S.T., and Whitehead, D.R. Pollen and macrofossils from Wisconsinan interstadial sediments in northeastern Georgia. Quaternary Research 39, (1993). 99–106.Google Scholar
Jackson, S.T., and Williams, J.W. Modern analogs in Quaternary paleoecology: here today, gone yesterday, gone tomorrow?. Annual Review of Earth and Planetary Sciences 32, (2004). 495–537.CrossRefGoogle Scholar
Jackson, S.T., Overpeck, J.T., Webb, T. III, Keattch, S.E., and Anderson, K.H. Mapped plant macrofossil and pollen records of Late Quaternary vegetation change in eastern North America. Quaternary Science Reviews 16, (1997). 1–70.Google Scholar
Jackson, S.T., Webb, R.S., Anderson, K.H., Overpeck, J.T., Webb, T. III, Williams, J., and Hansen, B.C.S. Vegetation and environment in unglaciated eastern North America during the last glacial maximum. Quaternary Science Reviews 19, (2000). 489–508.Google Scholar
Jones, R.A., (2011). Transitions in the Ozarks: a paleoecological record of the last deglaciation at Cupola Pond, MO, USA. M.S. thesis, University of Wyoming, .Google Scholar
Liu, Y., Brewer, S., Booth, R.K., Minckley, T.A., and Jackson, S.T. Temporal density of pollen sampling affects age determination of the mid-Holocene hemlock (Tsuga) decline. Quaternary Science Reviews 45, (2012). 54–59.Google Scholar
MacDonald, G.M., Beukens, R.P., and Kieser, W.E. Radiocarbon dating of limnic sediments: a comparative analysis and discussion. Ecology 72, (1991). 1150–1155.CrossRefGoogle Scholar
Magri, D., Vendramin, G.G., Comps, B., Dupanloup, I., Geburek, T., Gömöry, D., Latałowa, M., Thomas Litt, T., Ladislav Paule, L., Roure, J.M., Tantau, I., van der Knaap, W.O., Rémy, J., Petit, R.J., and de Beaulieu, J.-L. A new scenario for the Quaternary history of European beech populations: palaeobotanical evidence and genetic consequences. New Phytologist 171, (2006). 199–221.Google Scholar
McLachlan, J.S., Clark, J.S., and Manos, P.S. Molecular indicators of tree migration capacity under rapid climate change. Ecology 86, (2005). 2088–2098.Google Scholar
Miller, P.A., Giesecke, T., Hickler, T., Bradshaw, R.H.W., Smith, B., Seppä, H., Valdes, P.J., and Sykes, M.T. Exploring climatic and biotic controls on Holocene vegetation change in Fennoscandia. Journal of Ecology 96, (2008). 247–259.Google Scholar
Nelson, D.M., Hu, F.S., Grimm, E.C., Curry, B.B., and Slate, J.E. The influence of aridity and fire on Holocene prairie communities in the eastern Prairie Peninsula. Ecology 87, (2006). 2523–2536.Google Scholar
Olsson, I.U. Radiometric dating. Berglund, B.E. Handbook of Holocene Palaeoecology and Palaeohydrology. (1986). John Wiley & Sons, Chichester, England. 273–312.Google Scholar
Overpeck, J.T., Webb, R.S., Webb, T. III Mapping eastern North American vegetation changes of the past 18 ka: no-analogs and the future. Geology 20, (1992). 1071–1074.Google Scholar
Parker, N.E., and Williams, J.W. Influences of climate, cattle density, and lake morphology on Sporormiella abundances in modern lake sediments in the US Great Plains. The Holocene 22, (2011). 475–483.Google Scholar
Raper, D., and Bush, M. A test of Sporormiella representation as a predictor of megaherbivore presence and abundance. Quaternary Research 71, (2009). 490–496.Google Scholar
Rasmussen, S.O., Andersen, K.K., Svensson, A.M., Steffensen, J.P., Vinther, B.M., Clausen, H.B., Siggaard-Andersen, M.-L., Johnsen, S.J., Larsen, L.B., Dahl-Jensen, D., Bigler, M., Röthlisberger, R., Fischer, H., Goto-Azuma, K., Hansson, M.E., and Ruth, U. A new Greenland ice core chronology for the Last glacial termination. Journal of Geophysical Research 111, (2006). D06102 Google Scholar
Reimer, P.J., Baillie, M.G.L., Bard, E., Bayliss, A., Beck, J.W., Blackwell, P.G., Ramsey, C.B., Buck, C.E., Burr, G.S., Edwards, R.L., Friedrich, M., Grootes, P.M., Guilderson, T.P., Hajdas, I., Heaton, T.J., Hogg, A.G., Hughen, K.A., Kaiser, K.F., Kromer, B., McCormac, F.G., Manning, S.W., Reimer, R.W., Richards, D.A., Southon, J.R., Talamo, S., Turney, C.S.M., van der Plicht, J., and Weyhenmeyer, C.E. IntCal90 and Marine09 radiocarbon age calibration curves, 0–50,000 years cal BP. Radiocarbon 51, (2009). 1111–1150.Google Scholar
Smith, E.N., (1984). Late-Quaternary vegetational history at Cupola Pond, Ozark National Scenic Riverways, southeastern Missouri. Thesis. The University of Tennessee, Knoxville, Tennessee, USA.. 115 pp.Google Scholar
Stewart, J.R., and Lister, A.M. Cryptic northern refugia and the origins of the modern biota. Trends in Ecology & Evolution 16, (2001). 608–613.Google Scholar
Stoner, J.S., Channell, J.E.T., Hillaire-Marcel, C., and Kissel, C. Geomagnetic paleointensity and environmental record from Labrador Sea core MD95-2024: global marine sediment and ice core chronostratigraphy for the last 110 kyr. Earth and Planetary Science Letters 183, (2000). 161–177.Google Scholar
Watts, W.A. The full-glacial vegetation of northwestern Georgia. Ecology 51, (1970). 17–33.CrossRefGoogle Scholar
Watts, W.A. Late-Quaternary vegetation history at White Pond on the inner Coastal Plain of South Carolina. Quaternary Research 13, (1980). 187–199.Google Scholar
Watts, W.A., and Hansen, B.C.S. Pre-Holocene and Holocene pollen records of vegetation history from the Florida peninsula and their climatic implications. Palaeogeography, Palaeoclimatolology, Palaeoecology 109, (1994). 163–176.Google Scholar
Watts, W.A., and Stuiver, M. Late Wisconsin climate of northern Florida and the origin of species-rich deciduous forest. Science 210, (1980). 325–327.Google Scholar
Webb, R.S., Webb, T. III Rates of sediment accumulation in pollen cores from small lakes and mires of eastern North America. Quaternary Research 30, (1988). 284–297.Google Scholar
Whitehead, D.R. Late-Pleistocene vegetational changes in northeastern North Carolina. Ecological Monographs 51, (1981). 451–471.Google Scholar
Whitehead, D.R., and Sheehan, M.C. Holocene vegetational changes in the Tombigbee River Valley, eastern Mississippi. American Midland Naturalist 113, (1985). 122–137.Google Scholar
Whitmore, J., Gajewski, K., Sawada, M., Williams, J.W., Shuman, B., Bartlein, P.J., Minckley, T., Viau, A.E., Webb, T. III, Shafer, S.L., Anderson, P.M., and Brubaker, L.B. Modern pollen data from North America and Greenland for multi-scale paleoenvironmental applications. Quaternary Science Reviews 24, (2005). 1828–1848.Google Scholar
Wilkins, G.R., (1985). Late-Quaternary vegetation history at Jackson Pond, Larue County, Kentucky. Thesis. The University of Tennessee, Knoxville, Tennessee, USA.Google Scholar
Wilkins, G.R., Delcourt, P.A., Delcourt, H.R., Harrison, F.W., and Turner, M.R. Paleoecology of central Kentucky since the last glacial maximum. Quaternary Research 36, (1991). 224–239.Google Scholar
Williams, J.W., and Jackson, S.T. Novel climates, no-analog communities, and ecological surprises. Frontiers in Ecology and the Environment 5, (2007). 475–482.Google Scholar
Williams, J.W., and Shuman, B.N. Obtaining accurate and precise environmental reconstructions from the modern analog technique and North American surface pollen dataset. Quaternary Science Reviews 27, (2008). 669–687.Google Scholar
Williams, J.W., Shuman, B.N., Webb, T. III Dissimilarity analyses of late-Quaternary vegetation and climate in eastern North America. Ecology 82, (2001). 3346–3362.Google Scholar
Williams, J.W., Shuman, B.N., Webb, T. III, Bartlein, P.J., and Leduc, P.L. Late Quaternary vegetation dynamics in North America: scaling from taxa to biomes. Ecological Monographs 74, (2004). 309–334.Google Scholar
Williams, J.W., Blois, J.L., and Shuman, B.N. Extrinsic and intrinsic forcing of abrupt ecological change: case studies from the late Quaternary. Journal of Ecology 99, (2011). 664–677.Google Scholar
Wright, H.E. Jr., Mann, D.H., and Glaser, P.H. Piston corers for peat and lake sediments. Ecology 65, (1984). 657–659.Google Scholar
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