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Phytolith and Carbon Isotope Evidence for Late Quaternary Vegetation and Climate Change in the Southern Black Hills, South Dakota

Published online by Cambridge University Press:  20 January 2017

Glen G. Fredlund  and
Larry L. Tieszen
Glen G. Fredlund
Affiliation:
Department of Geography, University of Wisconsin, Milwaukee, PO Box 413, Milwaukee, Wisconsin, 53201
Larry L. Tieszen
Affiliation:
Department of Biology, Augustana College, Sioux Falls, South Dakota, 57197
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Abstract

Analyses of phytoliths and carbon isotopes document change in late Quaternary grasslands in the Red Valley of the southern Black Hills. Late Pleistocene grassland composition was equivalent to the C3grass parklands of modern central Alberta. The rise of mixed grassland occurred rapidly between 11,000 and 9000 yr B.P. Early Holocene mixed grasslands included both short and tall C4grasses. A mid-Holocene erosional unconformity (ca. 8000 to 4500 yr B.P.) precludes phytolith or isotope analysis, but suggests lack of vegetation and landscape denudation caused by a drier climatic. Basin-wide stability and soil development followed the erosional episode (ca. 4500 to 3600 yr B.P.). Mesic-adapted C4panicoid grasses increased during this period of soil development. Low-magnitude fluctuation in the C4-dominated mixed grassland occurred throughout the late Holocene (3600 yr B.P. to present). Rise in δ13C values during the last 1000 yr without corresponding change in phytoliths may indicate a decrease in woodlands caused by increased fire frequency.

Type
Original Articles
Information
Quaternary Research , Volume 47 , Issue 2 , March 1997 , pp. 206 - 217
Copyright
University of Washington

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References

Axelrod, D.I., 1985. Rise of the grassland biome, central North America. The Botanical Review 51, 163–201.CrossRefGoogle Scholar
Baker, R.G., Drake, P., 1994. Holocene history of prairie in midwestern United States: Pollen versus plant macrofossils. Ecoscience 1, 333–339.CrossRefGoogle Scholar
Balesdent, J.C., Girardin, C., Mariotti, A., 1993. Site-related δ13 . Ecology 74, 1713–1721.Google Scholar
Barnosky, C.W., Grimm, E.C., Wright, H.E. Jr., 1987. Towards a postglacial history of the northern Great Plains: A review of the paleoecological problems. Annals of Carnegie Museum 56, 259–273.Google Scholar
Boutton, T.W., Archer, S.R., Nordt, L.C., 1994. Climate, CO2 . Nature 372, 625–626.CrossRefGoogle Scholar
Brown, D.A., 1984. Prospects and limits of a phytolith key for grasses in the central United States. Journal of Archaeological Science 11, 345–368.CrossRefGoogle Scholar
Brown, D.A., 1993. Early nineteenth-century grasslands of the midcontinent plains. Annals of the Association of American Geographers 83, 589–612.CrossRefGoogle Scholar
Brown, W.V., 1977. The Kranz syndrome and its subtypes in grass systematics. Memoirs of the Torrey Botanical Club 23, 1–97.Google Scholar
Burke, I.C., Kittel, T.G.F., Lauenroth, W.K., Snook, P., Yonker, C.M., Parton, W.J., 1991. Regional analysis of the central Great Plains: Sensitivity to climate variability. Bioscience 41, 685–692.Google Scholar
Cerling, T.E., 1984. The stable isotope composition of modern soil carbonate and its relationship to climate. Earth and Planetary Science Letters 71, 229–240.CrossRefGoogle Scholar
Cerling, T.E., Quade, J., Wang, Y., Bowman, J.R., 1989. Carbon isotopes in soils and palaeosols as ecology and paleoecology indicators. Nature 341, 138–139.Google Scholar
Collins, D. D., 1969. Macroclimate and the grassland ecosystem. The Grassland Ecosystem: A Preliminary Synthesis 29, 39, Range Science Department Series, No. 2,, Ft. Collins, CO. Google Scholar
Darton, N. H., Paige, S., 1925. Central Black Hills Folio. U.S. Geological Survey Bulletin 219.Google Scholar
Davis, M.B., 1976. Pleistocene biogeography of temperate deciduous forest. Geoscience and Man 13, 13–26.Google Scholar
Downtown, W.J.S., 1975. The occurrence of C4 . Photosynthetica 9, 96–105.Google Scholar
Fredlund, G. G., 1986. Problems in the simultaneous extraction of pollen and phytoliths from clastic sediments. Plant Opal Phytolith Analysis in Archaeology and Paleoecology: Proceedings of the 1984 Phytolith Research Workshop I. Rovner, 102, 111, Occasional Paper No. 1 of the Phytolitharien, North Carolina State University, Raleigh. Google Scholar
Fredlund, G. G., 1993. Paleoenvironmental Interpretations of Stable Carbon. Hydrogen, and Oxygen Isotopes from Opal-Phytoliths Eustis Ash Pit, Nebraska, Current Research in Phytolith Analysis: Applications in Archaeology and Paleoecology, D. PearsallD. Piperno, 46, 69, MASCA Research Papers in Science and Archaeology, University of Pennsylvania Museum. Google Scholar
Fredlund, G. G., Late-Quaternary geomorphic history of lower Highland Creek. Wind Cave National Park South Dakota, Physical Geography. Google Scholar
Fredlund, G.G., 1995. A late Quaternary pollen record from Cheyenne Bottoms, Kansas. Quaternary Research 43, 67–79.Google Scholar
Fredlund, G.G., Tieszen, L.L., 1994. Modern phytolith assemblages from the North American Great Plains. Journal of Biogeography 21, 321–335.CrossRefGoogle Scholar
Fredlund, G.G., Weston, T., Mandel, R., 1985. Palynological evidence for a late prehistoric vegetation change in the southern Black Hills from Cape's Cave (39FA205). Plains Anthropologist 30, 9–23.CrossRefGoogle Scholar
Great Plains Flora Association, 1986. Flora of the Great Plains, University Press of Kansas, Lawrence, Kansas.Google Scholar
Hall, S.A., Valastro, S., 1995. Grassland vegetation in the southern Great Plains during the last glacial maximum. Quaternary Research 44, 237–245.CrossRefGoogle Scholar
Humphrey, J.D., Ferring, C.R., 1994. Stable isotopic evidence for latest Pleistocene and Holocene climate change in north-central Texas. Quaternary Research 41, 200–213.CrossRefGoogle Scholar
Kelly, E.F., Amundson, R.G., Marino, B.D., Deniro, M.J., 1991. Stable isotope ratios of carbon in phytoliths as a quantitative method of monitoring vegetation and climate change. Quaternary Research 35, 222–233.Google Scholar
Kelly, E. F., Yonker, C., Marino, B., 1993. Stable carbon isotope composition of paleosols: An application to Holocene, Climate Change in Continental Isotopic Records, American Geophysical Union. Lohmann, K. C., Swartand, P. K., Savin, S., McKenzie, J., 233, 239, American Geophysical Union Washington, D.C. .Google Scholar
Kuchler, A. W., 1964. Potential natural vegetation of the conterminous United States. .Google Scholar
MacDonald, G.M., 1993. Fossil plant analysis and the reconstruction of plant invasions. Advances in Ecological Research 24, 67–110.Google Scholar
Madole, R.F., 1995. Spatial and temporal patterns of late Quaternary eolian deposition, eastern Colorado, U.S.A. Quaternary Science Reviews 14, 155–177.CrossRefGoogle Scholar
Mandel, R. D., 1992. Soils and Holocene landscape evolution in central and southwestern Kansas: Implications for archaeological research. Soils in Archaeology: Landscape Evolution and Human Occupation Holliday, V. T., 41, 100, Smithsonian Institution Press, Washington, D.C.. Google Scholar
Markgraf, V., Lennon, T., 1986. Paleoenvironmental history of the last 13,000 years of the eastern Powder River Basin, Wyoming and its implications for prehistoric cultural patterns. Plains Anthropologist 31, 1–12.CrossRefGoogle Scholar
Martin, C.W., Johnson, W.C., 1995. Variation in radiocarbon ages of soil organic matter fractions from late Quaternary buried soils. Quaternary Research 43, 232–237.CrossRefGoogle Scholar
McPherson, G.R., Boutton, T.W., Midwood, A.J., 1993. Stable carbon isotope analysis of soil organic matter illustrates vegetation change at the grassland/woodland boundary in southeastern Arizona, USA. Oecologia 93, 95–101.CrossRefGoogle ScholarPubMed
Melillo, J.M., Aber, J.D., Linkins, A.E., Ricca, A., Fry, B., Nadelhoffer, K.J., 1989. Carbon and nitrogen dynamics along the decay continuum: Plant litter to soil organic matter. Plant and Soil 115, 189–198.Google Scholar
Meltzer, D. J., 1995. Modeling the prehistoric response to Altithermal climate on the southern High Plains, Ancient Peoples and Landscapes. Johnson, E., 349, 368, Museum of Texas Tech University Lubbock, Texas. Google Scholar
Metcalfe, C. R., 1960. Anatomy of the Monocotyledons. .Gramineae, I., Clarendon Press, Oxford. Google Scholar
Mulholland, S.C., 1989. Phytolith shape frequencies in North Dakota grasses: A comparison to general patterns. Journal of Archaeological Science 16, 489–511.CrossRefGoogle Scholar
Mulholland, S. C., Rapp Jr., G., 1992. A morphological classification of grass silica-bodies, Phytolith Systematics: Emerging Issues. Rapp, Jr., G, Mulholland, S. C., 65, 90, Plenum, New York. 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
Pentico, E.D., Tieszen, L.L., 1991. Community and soil organic matter stable carbon isotope ratios: Forest-grassland transitions at Wind Cave National Park. Proceedings of South Dakota Academy of Science 70, 69–82.Google Scholar
Phillips, W. S., Shantz, H. L., 1963. Vegetation Change in Northern Great Plains. University of Arizona Agriculture Experiment Station Tucson. Google Scholar
Quade, J., Cerling, T.E., 1995. Expansion of C4 . Palaeogeography, Palaeoclimatology, Palaeoecology 115, 91–116.CrossRefGoogle Scholar
Reider, R. G., 1990. Late Pleistocene and Holocene pedogenic and environmental trends at archaeological sites in plains and mountain areas of Colorado and Wyoming, Archaeological Geology of North America. LascaJ, N. P., Donahue, , 335, 360, Geological Society of America, New York. Google Scholar
Sims, P. L., 1988. Grasslands, North American Terrestrial Vegetation. Barbour, M. G., Billings, W. D., 265, 286, Cambridge University Press, Cambridge. Google Scholar
Teeri, J.A., Stowe, L.G., 1976. Climatic patterns and distribution of C4 . Oecologia 23, 1–12.Google Scholar
Tieszen, L. L., Archer, S., 1990. Isotopic assessment of vegetation change in grassland and woodland systems, Plant Biology of Basin and Range. Osmond, C. B., 293, 321, Springer-Verlag, New York. Google Scholar
Tieszen, L. L., Boutton, T., 1989. Applications of stable isotopic ratios in terrestrial ecosystems, Stable Isotopes in Ecological Research. Rundel, P. W., Ehlerlinger, J. R., Nagy, K. A., Springer-Verlag, New York. Google Scholar
Tieszen, L. L., Reed, B. C., Bliss, N. B., Wylie, B. K., DeJong, D. D., NDVI. C34, Ecological Applications.Google Scholar
Twiss, P.C., Suess, E., Smith, R.M., 1969. Morphological classification of grass phytoliths. Soil Science Society of America 33, 109–115.Google Scholar
Wang, Y., Amundson, R., 1996. Radiocarbon dating of soil organic matter. Quaternary Research 45, 282–288.Google Scholar
Watson, L., Clifford, H.T., Dallwitz, M.J., 1985. The classification of Poaceae: Subfamilies and supertribes. Australian Journal of Botany 33, 433–484.Google Scholar
Wedin, D.A., Tieszen, L.L., Dewy, B., Pastor, J., 1995. Carbon isotope dynamics during grass decomposition and soil organic matter formation. Ecology 76, 1383–1392.Google Scholar
Wright, H. A., Bailey, A. W., 1982. Fire Ecology. Wiley, New York. Google Scholar