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Environmental change recorded in sediments from the Marmes rockshelter archaeological site, southeastern Washington state, USA

Published online by Cambridge University Press:  20 January 2017

Gary Huckleberry  and
Cynthia Fadem
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Abstract

The Marmes Rockshelter archaeological site in southeastern Washington state contains a > 11 kyr stratigraphic record that was excavated in the 1960s but only recently analyzed in detail. We present the results of physical, chemical, and isotopic analyses of archived Marmes sediments from rockshelter, hillslope, and floodplain locations. Multiple lines of evidence including éboulis production, soil chemistry, and δ13C and δ18O signatures in soil organic matter and calcium carbonate suggest that relatively cool, moist conditions 10,600 to 9700 14C yr BP were followed by relatively warm and dry conditions as early as 9000 14C yr BP. Warm and dry conditions extended to the late Holocene, followed by a return to cooler and moister climate. The limited range of δ13C and δ18O values in Marmes paleosols suggests that the magnitude of moisture and temperature shifts was locally buffered in the lower Snake River Canyon but adequate to generate significant changes in sedimentation and soil formation, possibly due to nonlinear geological and pedological processes. These buffered canyon environments were well suited for establishing residential bases associated with foraging and logistical collecting strategies and may have minimized the influence of climate changes in food resource abundance.

Keywords

ArchaeologyStratigraphyStable isotopesClimate changeHuman ecologyColumbia Plateau
Type
Research Article
Information
Quaternary Research , Volume 67 , Issue 1 , January 2007 , pp. 21 - 32
Copyright
University of Washington

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Footnotes

1 Current address: 3577 E. Nugget Canyon Place, Tucson, AZ 85718, USA.
2 Current address: Department of Earth and Planetary Sciences, Washington University, Campus Box 1169, 1 Brookings Dr., St. Louis, MO 63130-4862, USA

References

Alley, R.B., Marotske, J., Nordhaus, W.D., Overpeck, J.T., Peteet, D.M., Pielke, R.A. Jr., Pierrehumbert, R.T., Rhines, P.B., Stocker, T.F., Talley, L.D., and Wallace, J.M. Abrupt climate change. Science 299, (2003). 2005–2010.Google Scholar
Ames, K.M. Early Holocene forager mobility strategies on the southern Columbia Plateau. Willig, J.A., Aikens, C.M., and Fagan, J.L. Early Human Occupation in Far Western North America: The Clovis–Archaic interface. (1988). Nevada State Museum Anthropological Papers 21, Carson City. 325–360.Google Scholar
Ames, K.M., Dumond, D.E., Galm, J.R., and Minor, R. Prehistory of the southern Plateau. Walker, D.E. Jr. Handbook of North American Indians, Vol 12: Plateau. (1998). Smithsonian Institution Press, Washington, DC. 103–119.Google Scholar
Anderson, R.S. Near-surface thermal profiles in alpine bedrock: implications for the frost weathering of rock. Arctic and Alpine Research 30, (1998). 362–372.Google Scholar
Benson, L., Kashgarian, M., Rye, R., Lund, S., Paillet, F., Smoot, J., Kester, C., Mensing, S., Meko, D., and Lindstrom, S. Holocene multidecadal and multicentennial droughts affecting northern California and Nevada. Quaternary Science Reviews 21, (2002). 659–682.Google Scholar
Bohn, H., McNeal, B., and O'Connor, G. Soil Chemistry. 2nd ed (1985). John Wiley Sons, New York.Google Scholar
Boutton, T.W. Stable carbon isotope ratios of soil organic matter and their use as indicators of vegetation and climate change. Boutton, T.W., and Yamasaki, S. Mass Spectrometry of Soils. (1996). Marcel Dekker, Inc., New York City. 47–82.Google Scholar
Broughton, J., and O'Connell, J.F. On evolutionary ecology, selectionist archaeology, and behavioral archaeology. American Antiquity 64, (1999). 153–165.CrossRefGoogle Scholar
Butler, V.L., and Campbell, S.K. Resource intensification and resource depression in the Pacific Northwest of North America: a zooarchaeological review. Journal of World Prehistory 18, (2004). 327–405.Google Scholar
Cerling, T. The stable isotopic composition of modern soil carbonate and its relationship to climate. Earth and Planetary Science Letters 71, (1984). 229–240.Google Scholar
Cerling, T.E. Development of grasslands and savannas in East Africa during the Neogene. Palaeogeography. Palaeoclimatology, Palaeoecology (Global and Planetary Change Section) 97, (1992). 241–247.Google Scholar
Cerling, T., and Quade, J. Stable carbon and oxygen isotopes in soil carbonates. Climate change in continental records. Geophysical Monograph 78, (1993). 217–231.Google Scholar
Chatters, J. Population growth, climatic cooling, and the development of collector strategies on the southern Plateau, western North America. Journal of World Prehistory 9, (1995). 341–400.Google Scholar
Chatters, J. Environment. Walker, D.E. Jr. Handbook of North American Indians, vol 12: Plateau. (1998). Smithsonian Institution Press, Washington, DC. 29–48.Google Scholar
COHMAP Climatic changes of the last 18,000 years: observations and model simulations. Science 241, (1988). 1043–1052.Google Scholar
Davis, L., (2001). The Coevolution of Early Hunter-Gatherer Culture and Riparian Ecosystems in the Southern Columbia River Plateau. Ph.D. dissertation, University of Alberta, Edmonton.Google Scholar
Davis, L.G., and Schweger, C.E. Geoarchaeological context of late Pleistocene and early Holocene occupation at the Cooper's Ferry site, western Idaho, USA. Geoarchaeology: An International Journal 19, (2004). 685–704.CrossRefGoogle Scholar
Davis, L., Muehlenbachs, K., Schweger, C.E., and Rutter, N.W. Differential response of vegetation to postglacial climate in the Lower Salmon River Canyon, Idaho. Palaeogeography, Palaeoclimatology, Palaeoecology 185, (2002). 339–354.CrossRefGoogle Scholar
Fadem, C., (2004). The Pleistocene-Holocene Transition in Southeastern Washington: An Examination of Sediment and Paleosol Isotope Geochemistry from the Marmes Site (45FR50).. Unpublished M.A. thesis, Department of Anthropology, Washington State University, Pullman.Google Scholar
Farrand, W. Rockshelter and cave sediments. Stein, J.K., and Farrand, W.R. Archaeological Sediments in Context. (1985). Center for the Study of Early Man, Orono, ME. 21–39.Google Scholar
Fryxell, R. Through a mirror darkly. The Record. (1963). Washington State Univ. Library, Pullman. 1–18.Google Scholar
Fryxell, R. Regional patterns of sedimentation recorded by cave and rock-shelter stratigraphy in the Columbia Plateau, Washington. Geological Society of America Special Paper 76, (1964). 272 (abstract) Google Scholar
Fryxell, R., and Daugherty, R.D. Interim Report: Archaeological Salvage in the Lower Monumental Reservoir, Washington. Laboratory of Anthropology Report of Investigations No. 21. (1962). Washington State University, Pullman.Google Scholar
Fryxell, R., and Daugherty, R.D. Late Glacial and Post-Glacial Geological and Archaeological Chronology of the Columbia Plateau, Washington. Laboratory of Anthropology Report of Investigations No. 23. (1963). Washington State University, Pullman.Google Scholar
Fryxell, R., and Keel, B.C. Emergency Salvage Excavations for the Recovery of Early Human Remains and Related Scientific Materials from the Marmes Rockshelter Archaeological Site, Southeastern Washington. Final Report to the Army Corps of Engineers. (1969). Laboratory of Anthropology, Washington State University, Walla Walla, WA.Google Scholar
Fryxell, R., Bielicki, T., Daugherty, R.D., Gustafson, C.E., Irwin, H.T., Keel, B.C., Krantz, G.S., (1968). Human skeletal material and artifacts from sediments of Pinedale (Wisconsin) glacial age in southeastern Washington, United States. Proceedings VIIIth International Congress of Anthropological and Ethnological Sciences, Volume 3, : Ethnology and Archaeology, pp. 186–191.Google Scholar
Gustafson, C., (1972). Faunal Remains from the Marmes Rockshelter and Related Archaeological Sites in the Columbia Basin.. Unpublished Ph.D. dissertation, Department of Zoology. Washington State University, Pullman.Google Scholar
Gustafson, C., and Wegner, R. Faunal remains. Hicks, B.A. Marmes Rockshelter: A Final Report on 11,000 Years of Cultural Uses. (2004). Washington State Univ. Press, Pullman. 253–317.Google Scholar
Hicks, B.A. Interpretations. Hicks, B.A. Marmes Rockshelter: A Final Report on 11,000 Years of Cultural Uses. (2004). Washington State Univ. Press, Pullman. 389–421.Google Scholar
Holliday, V.T. Stratigraphy and Paleoenvironment of Late Quaternary Valley Fills on the Southern High Plains. (1995). Geological Society of America Memoir 186, Boulder, CO.Google Scholar
Huckleberry, G., Lenz, B., Galm, J., and Gough, S. Recent geoarchaeological discoveries in central Washington. Swanson, T. Western Cordillera and Adjacent Areas. (2003). Geological Society of America Field Guide 4, Boulder, CO. 237–249.Google Scholar
Huckleberry, G., Gustafson, C., and Gibson, S. Stratigraphy and site formation processes. Hicks, B.A. Marmes Rockshelter: A Final Report on 11,000 Years of Cultural Uses. (2004). Washington State Univ. Press, Pullman. 77–121.Google Scholar
Kaufman, D.S. et al. Holocene thermal maximum in the western Arctic (0–180°W). Quaternary Science Reviews 23, (2004). 529–560.Google Scholar
Karlstrom, E.T. Description and genesis of buried sand-filled soil wedges near Flagstaff, Arizona. Physical Geography 22, (2001). 167–186.Google Scholar
Leonardy, F.C., and Rice, D.G. A proposed culture typology for the Lower Snake River region, southeastern Washington. Northwest Anthropological Research Notes 4, (1970). 1–29.Google Scholar
Lyman, R.L. On the analysis and interpretation of species list data in zooarchaeology. Journal of Ethnobiology 6, (1986). 67–81.Google Scholar
Lyman, R.L. Influences of mid-Holocene Altithermal climates on mammalian faunas and human subsistence in eastern Washington. Journal of Ethnobiology 12, (1992). 37–62.Google Scholar
Lyman, R.L. Late-Quaternary diminution and abundance of prehistoric bison (Bison sp.) in eastern Washington state, USA. Quaternary Research 62, (2004). 76–85.Google Scholar
Lyman, R.L., and Wolverton, S. The late prehistoric-early historic game sink in the northwestern United States. Conservation Biology 16, (2002). 73–85.Google Scholar
Madsen, D.B. Late Quaternary Paleoecology in the Bonneville Basin. Bulletin 130. (2000). Utah Geological Survey, Salt Lake City.Google Scholar
Marshall, A.G., (1971). An Alluvial Chronology of the Lower Palouse River Canyon and Its Relation to Local Archaeological Sites.. Unpublished M.A. thesis, Department of Anthropology, Washington State University, Pullman.Google Scholar
McFadden, L.D., Weldon, R.J. II Rates and processes of soil development on Quaternary terraces in Cajon Pass, California. Geological Society of America Bulletin 98, (1987). 280–293.Google Scholar
Mears, B. Jr. Periglacial wedges and the late Pleistocene environment of Wyoming's intermountain basins. Quaternary Research 15, (1981). 171–198.Google Scholar
Mehringer, P.J. Jr. Columbia River Basin Ecosystems: Late Quaternary Environments. US. (1996). Forest Service and Bureau of Land Management, Walla Walla, WA. (http://www.icbemp.gov/science)Google Scholar
Muhs, D. Intrinsic thresholds in soil systems. Physical Geography 5, (1984). 99–110.Google Scholar
Nordt, L.C. Stable carbon and oxygen isotopes in soils. Goldberg, P., Holliday, T., and Ferring, R.C. Earth Sciences and Archaeology. (2001). Plenum Publishers, New York. 419–448.Google Scholar
Nordt, L.C., Wilding, L.P., and Hallmark, C.T. Stable carbon isotope composition of pedogenic carbonates and their use in studying pedogenesis. Boutton, T.W., and Yamasaki, S. Mass Spectrometry of Soils. (1996). Marcel Dekker, Inc., New York City. 133–154.Google Scholar
Peterson, F.F., (1961). Solodized Solonetz Soils Occurring on the Uplands of the Palouse Loess.. Unpublished Ph.D. Dissertation, Department of Crop and Soil Science, Washington State University, Pullman.Google Scholar
Péwé, T.L. The periglacial environment in North America during Wisconsin time. Porter, S.C., Wright, H.E. Jr. Late Quaternary Environments of the United States, vol 1: The Late Pleistocene. (1983). University of Minnesota Press, Minneapolis. 157–189.Google Scholar
Rhode, D. The role of paleoecology in the development of Great Basin archaeology, and vice-versa. Beck, C. Models for the Millennium: Great Basin Anthropology Today. (1999). University of Utah Press, Salt Lake City. 29–49.Google Scholar
Richards, L.A. Diagnosis and Improvement of Saline and Alkali Soils. U.S. Department of Agriculture Handbook 60. (1954). U.S. Government Printing Office, Washington D.C.Google Scholar
Rowe, K.C., Heske, E.J., Brown, P.W., Paige, K.N., (2004). Surviving the ice: Northern refugia and post-glacial colonization. Proceedings of the National Academy of Sciences, 101 10,355–10,359.Google Scholar
Sheppard, J.C., Wigand, P.E., Gustafson, C.E., and Rubin, M. A reevaluation of the Marmes rockshelter radiocarbon chronology. American Antiquity 52, (1987). 118–125.Google Scholar
Stetler, L.D., and Gaylord, D.R. Evaluating eolian–climatic interactions using a regional climate model from Hanford, Washington (USA). Geomorphology 17, (1996). 99–113.Google Scholar
Thackray, G.D., Lundeen, K.A., and Borgert, J.A. Latest Pleistocene alpine glacier advances in the Sawtooth Mountains, Idaho, USA: reflections of midlatitude moisture transport at the close of the last glaciation. Geology 32, (2004). 225–228.Google Scholar
Thompson, R., Whitlock, C., Bartlein, P.J., Harrison, S.P., and Spaulding, W.G. Climatic changes in the western United States since 18,000 yr B.P.. Wright, H.E., Kutzbach, J.E., Webb, T. III, Ruddiman, W.F., Street-Perrott, F.A., and Bartlein, P.J. Global Climates Since the Last Glacial Maximum. (1993). University of Minnesota Press, Minneapolis. 468–513.Google Scholar
Walder, J., and Hallet, B. A theoretical model of the fracture of rock during freezing. Geological Society of America Bulletin 96, (1985). 336–346.Google Scholar
Whitlock, C., and Bartlein, P.J. Vegetation and climate change in northwest America during the past 125 k yr. Nature 38, (1997). 57–61.Google Scholar
Wigand, P.E., and Hicks, B.A. Environmental overview. Hicks, B.A. Marmes Rockshelter: A Final Report on 11,000 Years of Cultural Use. (2004). Washington State Univ. Press, Pullman. 43–64.Google Scholar
Wigand, P.E., and Rhode, D. Great Basin vegetation history and aquatic systems: the last 150,000 years. Hershler, R., Madsen, D.B., and Currey, D.R. Great Basin Aquatic Systems History, Smithsonian Contributions to the Earth Sciences 33. (2002). Smithsonian Institution Press, Washington D.C. 309–368.Google Scholar