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Grassland Vegetation in the Southern Great Plains during the Last Glacial Maximum

Published online by Cambridge University Press:  20 January 2017

Stephen A. Hall  and
Salvatore Valastro Jr.
Stephen A. Hall
Affiliation:
Department of Geography, University of Texas at Austin, Austin, Texas 78712
Salvatore Valastro Jr.
Affiliation:
Radiocarbon Laboratory, J. J. Pickle Research Campus, University of Texas at Austin, Austin, Texas 78758
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Abstract

New pollen records from White Lake in the Southern High Plains and from Friesenhahn Cave on the southeastern Edwards Plateau of Texas indicate that the glacial-age vegetation of the southern Great Plains was a grassland. The High Plains was a treeless Artemisia grassland and the Edwards Plateau, at the south edge of the Great Plains, was a grassland with pinyon pines and deciduous trees in canyons and riparian habitats. The glacial-age grasslands differ from modern shortgrass and tallgrass prairies and may have no modern analog. The dominance of prairie vegetation during the last glacial maximum is compatible with late Pleistocene mammalian faunas and late-glacial grassland pollen records from the region. Earlier interpretations of a pine-spruce forest on the High Plains were based on pollen assemblages that are here shown to have been altered by postdepositional deterioration, resulting in differential preservation of conifer pollen grains. Accordingly, the "Tahoka Pluvial" and other "climatic episodes" defined by High Plains pollen records are abandoned.

Type
Research Article
Information
Quaternary Research , Volume 44 , Issue 2 , September 1995 , pp. 237 - 245
Copyright
University of Washington

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References

Ashbaugh, K. M., and Metcalf, A. L. (1986). Fossil molluscan faunas from four spring-related deposits in the northern Chihuahuan Desert, southern New Mexico and westernmost Texas. New Mexico Bureau of Mines & Mineral Resources, Socorro, Circular 200, 25 pp.Google Scholar
Blum, M. D. Toomey, R. S. III, and Valastro, S. Jr. (1994). Fluvial response to Late Quaternary climatic and environmental change, Edwards Plateau, Texas. Palaeogeography, Palaeoclimatology, Palaeoecology 108 , 1–21.Google Scholar
Blum, M. D., and Valastro, S. Jr. (1989). Response of the Pedemales River of central Texas to late Holocene climatic change. Annals of the Association of American Geographers 79 , 435–456.Google Scholar
Blum, M. D., and Valastro, S. Jr. (1992). Quaternary stratigraphy and geoarchaeology of the Colorado and Concho Rivers, West Texas. Geoarchaeology 7 , 419–148.Google Scholar
Bryant, V. M. Jr. (1977). A 16,000 year pollen record of vegetational change in central Texas. Palynology 1 , 143–156.Google Scholar
Bryant, V. M. Jr., and Hall, S. A. (1993). Archaeological palynology in the United States: A critique. American Antiquity 58 , 277–286.Google Scholar
Bryant, V. M. Jr., and Holloway, R. G. (1985). A late-Quatemary paleoenvironmental record of Texas: An overview of the pollen evidence. In “Pollen Records of Late-Quatemary North American Sediments” (Bryant, V. M. Jr. and Holloway, R. G., Eds.), pp. 39–70. American Association of Strati-graphic Palynologists Foundation, Dallas.Google Scholar
Bryant, V. M. Jr., and Schoenwetter, J. (1987). Pollen records from Lubbock Lake. In “Lubbock Lake; Late Quaternary Studies on the Southern High Plains” (Johnson, E., Ed.), pp. 36–40. Texas A & M University Press, College Station.Google Scholar
Camper, H. A. (1991). “Pollen Analysis of Patschke Bog.” M.S. thesis, Texas A & M University, College Station.Google Scholar
Dalquest, W. W., and Schultz, G. E. (1992). “Ice Age Mammals of Northwestern Texas.” Midwestern State University Press, Wichita Falls, TX.Google Scholar
Drake, R. J. (1975). Fossil nonmarine mollusks of the 1961-63 Llano Estacado paleoecology study. In “Late Pleistocene Environments of the Southern High Plains” (Wendorf, F. and Hester, J. J., Eds.), pp. 201–245. Publication of the Fort Burgwin Research Center, No. 9, Ranchos de Taos, NM.Google Scholar
Evans, G. L. (1961). The Friesenhahn Cave. Texas Memorial Museum Bulletin 2 , 1–22. [University of Texas, Austin].Google Scholar
Evans, G. L., and Meade, G. E. (1945). Quaternary of the Texas High Plains. Austin, University of Texas, Austin, Publication 4401, pp. 485–507.Google Scholar
Frye, R. G. Brown, K. L., and McMahan, C. A. (1984). The Vegetation Types of Texas. Scale 1:1,000,000. Texas Parks and Wildlife Department, Austin.Google Scholar
Graham, R. W. (1976). “Pleistocene and Holocene Mammals, Taphonomy, and Paleoecology of the Friesenhahn Cave Local Fauna, Bexar County, Texas.” Ph.D. dissertation, University of Texas at Austin.Google Scholar
Graham, R. W. (1987). Late Quaternary mammalian faunas and paleoenvironments of the southwestern Plains of the United States. In “Late Quaternary Mammalian Biogeography and Environments of the Great Plains and Prairies” (Graham, R. W. Semketi, H. A. Jr., and Graham, M. A., Eds.), pp. 24–86. Scientific Papers, Vol. 22, Illinois State Museum, Springfield.Google Scholar
Graham, R. W., and Lundeiius, E. L. Jr. (1984). Coevolutionary disequilibrium and Pleistocene extinctions. In “Quaternary Extinctions: A Prehistoric Revolution” (Martin, P. S. and Klein, R. G., Eds.), pp. 223–249. University of Arizona Press, Tucson.Google Scholar
Graham, R. W., and Meade, J. I. (1987). Environmental fluctuations and evolution of mammalian faunas during the last glaciation in North America. In “North America and Adjacent Oceans During the Last Deglaciation” (Ruddiman, W. F. and Wright, H. E. Jr., Eds.), pp. 371–402. The Geology of North America, Vol. K-3, Geological Society of America, Boulder, CO.Google Scholar
Guthrie, R. D. (1990). “Frozen Fauna of the Mammoth Steppe: The Story of Blue Babe.” University of Chicago Press, Chicago.Google Scholar
Hafsten, U. (1961). Pleistocene development of vegetation and climate in the southern High Plains as evidenced by pollen analysis. In “Paleoecology of the Llano Estacado” (Wendorf, F. Ed.), pp. 59–91. Fort Burgwin Research Center, Publication No. 1, Museum of New Mexico Press, Santa Fe.Google Scholar
Hafsten, U (1964). A standard pollen diagram for the southern High Plains, USA, covering the period back to the early Wisconsin glaciation. International Quaternary Congress, VI, Report 2, pp. 407–420, Warsaw.Google Scholar
Hall, S. A. (1981). Deteriorated pollen grains and the interpretation of Quaternary pollen diagrams. Review of Palaeobotany and Palynology 32 , 193–206.Google Scholar
Hall, S. A. (1990). Pollen deposition and vegetation in the southern Rocky Mountains and southwest Plains, USA. Grana 29 , 47–61.Google Scholar
Hall, S. A. (1991). Late glacial grassland at the Aubrey Clovis site, North Texas. [Geological Society of America] Abstracts with Programs 23(4), 29.Google Scholar
Hall, S. A. (1992). Comparative pollen influx at a nine-trap array in the Grand Prairie of northern Texas. Texas Journal of Science 44 , 469–474.Google Scholar
Hall, S. A. (1994). Modem pollen influx in tallgrass and shortgrass prairies, southern Great Plains, USA. Grana 33 , 321–326.Google Scholar
Hansen, B. S., and Cushing, E. J. (1973). Identification of pine pollen of late Quaternary age from the Chuska Mountains, New Mexico. Geological Society of America Bulletin 84 , 1181–1200.Google Scholar
Harbour, J. (1975). General stratigraphy. In “Late Pleistocene Environments of the Southern High Plains” (Wendorf, F., and Hester, J. J., Eds.), pp. 33–56. Publication of the Fort Burgwin Research Center, No. 9, Ranchos de Taos, New Mexico.Google Scholar
Harris, A. H. (1977). Biotic environments of the Paleoindian. The Museum Journal 17 , 1–12, [West Texas Museum Association, Texas Tech University, Lubbock].Google Scholar
Hibbard, C. W. (1960). An interpretation of Pliocene and Pleistocene climates in North America. Michigan Academy of Science Annual Report 62 , 5–30.Google Scholar
Holliday, V. T. (1985). Archaeological geology of the Lubbock Lake Site, southern High Plains of Texas. Geological Society of America Bulletin 96 , 1483–1492.Google Scholar
Holliday, V. T. (1987). A reexamination of Late-Pleistocene boreal forest reconstructions for the southern High Plains. Quaternary Research 28 , 238–244.Google Scholar
Holliday, V. T. Johnson, E. Hall, S. A., and Bryant, V. M. (1985). Reevaluation of the Lubbock Subpluvial. Current Research in the Pleistocene 2 , 119–121.Google Scholar
Lundelius, E. L. Jr. (1967). Late-Pleistocene and Holocene faunal history of central Texas. In “Pleistocene Extinctions: The Search for a Cause” (Martin, P. S. and Wright, H. E. Jr., Eds.), pp. 287–319. Yale University Press, New Haven.Google Scholar
McMahan, C. A. Frye, R. G., and Brown, K. L. (1984). “The Vegetation Types of Texas, Including Cropland.” Texas Parks and Wildlife Department, Austin.Google Scholar
Metcalf, A. L. (1984). Land snails (Gastropoda: Pulmonata) from Cimarron County, Oklahoma. Texas Journal of Science 36 , 53–64.Google Scholar
Miller, B. B. (1975). A sequence of radiocarbon-dated Wisconsinan nonmarine molluscan faunas from southwestern Kansas-northwestern Oklahoma. In “Studies on Cenozoic Paleontology and Stratigraphy in Honor of Claude W. Hibbard” (Smith, G. R. and Friedland, N. E., Eds.), pp. 9–18. Papers on Paleontology No. 12, University of Michigan Museum of Paleontology, Ann Arbor.Google Scholar
Neck, R. W. (1987). Changing Holocene snail faunas and environments along the Eastern Caprock Escarpment of Texas. Quaternary Research 27 , 312–322.Google Scholar
Neck, R. W. (1990). Ecological analysis of the living molluscs of the Texas Panhandle. American Malacological Bulletin 8 , 9–18.Google Scholar
Oldfield, F. (1975). Pollen analytical results, part II. In “Late Pleistocene Environments of the Southern High Plains” (Wendorf, F. and Hester, J. J., Eds.), pp. 121–146. Publication of the Fort Burgwin Research Center, No. 9, Ranchos de Taos, NM.Google Scholar
Oldfield, F., and Schoenwetter, J. (1964). Late Quaternary environments and early man on the southern High Plains. Antiquity 38 , 226–229.Google Scholar
Oldfield, F., and Schoenwetter, J. (1975). Discussion of the pollen analytical evidence. In “Late Pleistocene Environments of the Southern High Plains” (Wendorf, F. and Hester, J. J., Eds.), pp. 149–177. Publication of the Fort Burgwin Research Center, No. 9, Ranchos de Taos, NM.Google Scholar
Potzger, J. E., and Tharp, B. C. (1947). Pollen profile from a Texas bog. Ecology 28 , 274–280.Google Scholar
Powell, A. M. (1988). “Trees and Shrubs of Trans-Pecos Texas, Including Big Bend and Guadalupe Mountains National Parks.” Big Bend Natural History Association, Big Bend National Park, TX.Google Scholar
Reeves, C. C. Jr. (1976). Quaternary stratigraphy and geologic history of southern High Plains, Texas and New Mexico. In “Quaternary Stratigraphy of North America” (Mahaney, W.C., Ed.), pp. 213–234. Dowden, Hutchinson, and Ross, Stroudsburg, PA.Google Scholar
Rowley, J. R., and Prijanto, B. (1977). Selective destruction of the exine of pollen grains. Geophytology 7 , 1–23.Google Scholar
Shaw, R. B. Volman, K. C., and Smeins, F. (1980). Modern pollen rain and vegetation on the Edwards Plateau, Texas. Palynology 4 , 205–213.Google Scholar
Slaughter, B. H. (1975). Ecological interpretation of the Brown Sand Wedge local fauna. In “Late Pleistocene Environments of the Southern High Plains” (Wendorf, F. and Hester, J. J., Eds.), pp. 179–192. J’ublication of the Fort Burgwin Research Center, No. 9, Ranchos de Taos, NM.Google Scholar
Stanley, R. G., and Linskens, H. F. (1974). “Pollen: Biology, Biochemistry, Management.” Springer-Verlag, New York.Google Scholar
Toomey, R. S. III (1989). Hall’s Cave. In “Geomorphology, Quaternary Stratigraphy, and Paleoecology of Central Texas” (Hall, S. A. and Gustav-son, T. C., Eds.), pp. C1–C19. 7th Annual Meeting, South Central Cell, Friends of the Pleistocene, Central Texas Guidebook.Google Scholar
Toomey, R. S. III (1993). “Late Pleistocene and Holocene Faunal and Environmental Changes at Hall’s Cave, Kerr County, Texas.” Ph.D. dissertation, University of Texas at Austin.Google Scholar
Toomey, R. S. III Blum, M. D., and Valastro, S. Jr. (1993). Late Quaternary climates and environments of the Edwards Plateau, Texas. Global and Planetary Change 7 , 299–320.Google Scholar
Van Auken, O. W. (1988). Woody vegetation of the southeastern escarpment and plateau. In “Edwards Plateau Vegetation: Plant Ecological Studies in Central Texas” (Amos, B. B. and Gehlbach, F. R., Eds.), pp. 43–55. Baylor University Press, Waco, TX.Google Scholar
Van Auken, O. W. Ford, A. L., and Stein, A. (1979). A comparison of some woody upland and riparian plant communities of the southern Edwards Plateau. Southwestern Naturalist 24 , 165–180.Google Scholar
Van Devender, T. R. (1986). Pleistocene climates and endemism in the Chihuahuan Desert flora. In “Second Symposium on Resources of the Chihuahuan Desert Region, United States and Mexico” (Barlow, J. C. Powell, A. M., and Timmermann, B. N., Eds.), pp. 1–19. Chihuahuan Desert Research Institute, Alpine, TX.Google Scholar
Wendorf, F. (1961a). An interpretation of late Pleistocene environments of the Llano Estacado. In “Paleoecology of the Llano Estacado” (Wendorf, F., Ed.), pp. 115–133. Fort Burgwin Research Center, Publication No. 1, Museum of New Mexico Press, Santa Fe.Google Scholar
Wendorf, F. (1961b). Invertebrate collections. In “Paleoecology of the Llano Estacado” (Wendorf, F., Ed.), pp. 105–114. Fort Burgwin Research Center, Publication No. 1, Museum of New Mexico Press, Santa Fe.Google Scholar
Wendorf, F. (1975). Summary and conclusions. In “Late Pleistocene Environments of the Southern High Plains” (Wendorf, F. and Hester, J. J., Eds.), pp. 257–278. Publication of the Fort Burgwin Research Center, No. 9, Ranchos de Taos, New Mexico.Google Scholar
White, S. E., and Valastro, S. Jr. (1984). Pleistocene glaciation of Volcano Ajusco, central Mexico, and comparison with the standard Mexican glacial sequence. Quaternary Research 21 , 21–35.Google Scholar
Wilson, L. R. (1966). Palynology of the Domebo Site. In “Domebo: A Paleo- Indian Mammoth Kill in the Prairie-Plains” (Leonhardy, F. C., Ed.), pp. 44–50. Contributions of the Museum of the Great Plains, No. 1, Lawton, OK.Google Scholar