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Chronology and Ecology of Late Pleistocene Megafauna in the Northern Willamette Valley, Oregon

Published online by Cambridge University Press:  20 January 2017

Daniel M. Gilmour ,
Virginia L. Butler ,
Jim E. O'Connor ,
Edward Byrd Davis ,
Brendan J. Culleton ,
Douglas J. Kennett  and
Gregory Hodgins
Daniel M. Gilmour*
Affiliation:
Willamette Cultural Resources Associates, Ltd., 623 SE Mill Street, Portland, OR 97214, USA Department of Anthropology, Portland State University, P.O. Box 751, Portland, OR 97202, USA
Virginia L. Butler
Affiliation:
Department of Anthropology, Portland State University, P.O. Box 751, Portland, OR 97202, USA
Jim E. O'Connor
Affiliation:
U.S. Geological Survey, 2130 SW 5th Avenue, Portland, OR 97201, USA
Edward Byrd Davis
Affiliation:
Museum of Natural and Cultural History, University of Oregon, 1680 E. 15th Ave., Eugene, OR 97403, USA Department of Geological Sciences, 1272 University of Oregon, Eugene, OR 97403, USA
Brendan J. Culleton
Affiliation:
Department of Anthropology, Pennsylvania State University, 409 Carpenter Building, University Park, PA 16802, USA
Douglas J. Kennett
Affiliation:
Department of Anthropology, Pennsylvania State University, 409 Carpenter Building, University Park, PA 16802, USA
Gregory Hodgins
Affiliation:
NSF-Arizona AMS Facility, Department of Physics, University of Arizona, Physics Building, 1118 East Fourth St., P.O. Box 210081, Tucson, AZ 85721, USA School of Anthropology, University of Arizona, USA
*
*Corresponding author. E-mail addresses:danny@willamettecra.com (D.M. Gilmour), virginia@pdx.edu (V.L. Butler), oconnor@usgs.gov (J.E. O'Connor), edavis@uoregon.edu (E.B. Davis), bjc23@psu.edu (B.J. Culleton), djk23@psu.edu (D.J. Kennett), ghodgins@physics.arizona.edu (G. Hodgins).
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Abstract

Since the mid-19th century, western Oregon's Willamette Valley has been a source of remains from a wide variety of extinct megafauna. Few of these have been previously described or dated, but new chronologic and isotopic analyses in conjunction with updated evaluations of stratigraphic context provide substantial new information on the species present, timing of losses, and paleoenvironmental conditions. Using subfossil material from the northern valley, we use AMS radiocarbon dating, stable isotope (δ13C and δ15N) analyses, and taxonomic dietary specialization and habitat preferences to reconstruct environments and to develop a local chronology of events that we then compare with continental and regional archaeological and paleoenvironmental data. Analysis of twelve bone specimens demonstrates the presence of bison, mammoth, horse, sloth, and mastodon from ~ 15,000–13,000 cal yr BP. The latest ages coincide with changing regional climate corresponding to the onset of the Younger Dryas. It is suggested that cooling conditions led to increased forest cover, and along with river aggradation, reduced the area of preferred habitat for the larger bodied herbivores, which contributed to the demise of local megafauna. Archaeological evidence for megafauna–human interactions in the Pacific Northwest is scarce, limiting our ability to address the human role in causing extinction.

Keywords

Megafaunal extinctionsPleistocenePacific NorthwestStable isotopesYounger DryasOverkill
Type
Research Article
Information
Quaternary Research , Volume 83 , Issue 1 , January 2015 , pp. 127 - 136
Copyright
University of Washington

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References

Addington, Y.S. (2006). Mastodon: The Tualatin Connection.. Tualatin Historical Society, Tualatin. (On file).Google Scholar
Alley, R.B. (2000). The Younger Dryas cold interval as viewed from central Greenland.. Quaternary Science Reviews 19, 213–226.CrossRefGoogle Scholar
Alley, R.B. (2004). GISP2 Ice Core Temperature and Accumulation Data. IGBP PAGES/World Data Center for Paleoclimatology Data Contribution Series #2004-013.. NOAA/NGDC Paleoclimatology Program, Boulder.Google Scholar
Ambrose, S.H. (1990). Preparation and characterization of bone and tooth collagen for isotopic analysis.. Journal of Archaeological Science 17, 431–451.Google Scholar
Barnosky, C.W. (1985). Late-Quaternary vegetation history near Battle Ground Lake, Southern Puget Trough, Washington.. Geological Society of America Bulletin 96, 263–271.2.0.CO;2>CrossRefGoogle Scholar
Barnosky, A.D., Koch, P.L., Feranec, R.S., Wing, S.L., and Shabel, A.B. (2004). Assessing the causes of Late Pleistocene extinctions on the continents.. Science 306, 70–75.Google Scholar
Barton, B.R., and Cearley, S.J. (2008). Paleontological investigations at the Pratum-Rutschman/Qualey Mammoth Site, Marion County, Oregon.. Current Research in the Pleistocene 25, 161–163.Google Scholar
Beck, C.T., and Jones, G.T. (1997). The Terminal Pleistocene/Early Holocene archaeology of the Great Basin.. Journal of World Prehistory 11, 161–236.CrossRefGoogle Scholar
Beck, C.T., and Jones, G.T. (2010). Clovis and Western Stemmed: population migration and the meeting of two technologies in the Intermountain West.. American Antiquity 75, 81–116.CrossRefGoogle Scholar
Bocherens, H. (2003). Isotopic biogeochemistry and the paleoecology of the mammoth steppe fauna.. In: Reumer, J. (Ed.), Advances in Mammoth Research, Proceedings of the 2nd International Mammoth Conference, Rotterdam. DEINSEA. 9, 57–76.Google Scholar
Boulanger, M.T., and Lyman, R.L. (2014). Northeastern North American Pleistocene megafauna chronologically overlapped minimally with Paleoindians.. Quaternary Science Reviews 85, 35–46.CrossRefGoogle Scholar
Bradshaw, C.J.A., Cooper, A., Turney, C.S.M., and Brook, B.W. (2012). Robust estimates of extinction time in the geological record.. Quaternary Science Reviews 33, 14–19.Google Scholar
Bronk Ramsey, C. (2010). OxCal v4.2.3. Oxford Radiocarbon Accelerator Unit, Oxford.Google Scholar
Brown, T.A., Nelson, D.E., Vogel, J.S., and Southon, J.R. (1988). Improved collagen extraction by modified Longin method.. Radiocarbon 30, 171–177.CrossRefGoogle Scholar
Cannon, M.D., and Meltzer, D.J. (2004). Early Paleoindian foraging: examining the faunal evidence for large mammal specialization and regional variability in prey choice.. Quaternary Science Reviews 23, 1955–1987.Google Scholar
Cearley, S.J. (2008). Paleontology, Geography and Biochemistry of the Pratum Mammoth, Western Oregon. Unpublished Bachelor of Science thesis. Department of Geology, Central Washington University,, Ellensburg..Google Scholar
Connolly, T.J. (1994). Paleo point occurrences in the Willamette Valley, Oregon.. In: Baxter, P.W. (Ed.), Contributions to the Archaeology of Oregon 1989–1994 Occasional Papers. 5. Association of Oregon Archaeologists, Eugene.81–88.Google Scholar
Connolly, T.J. (2003a). Human hair from Terminal Pleistocene peat deposits in the Willamette Valley.. Current Archaeological Happenings in Oregon 28(3/4), 9–15.Google Scholar
Connolly, T.J. (2003b). Letter Report re: Exploratory Archaeological Probing for the Oregon Highway 214 Sidewalk Construction, City of Woodburn, Marion County, Oregon.. State Historic Preservation Office, Salem.(On file).Google Scholar
Cressman, L.S. (1947). Further information on projectile points from Oregon.. American Antiquity 13, 177–179.Google Scholar
Cressman, L.S., and Laughlin, W.S. (1941). A probable association of mammoth and artifacts in the Willamette Valley, Oregon.. American Antiquity 6, 339–342.CrossRefGoogle Scholar
DeNiro, M.J. (1985). Postmortem preservation and alteration of in vivo bone collagen isotope ratios in relation to palaeodietary reconstruction.. Nature 317, 806–809.Google Scholar
Drucker, D.G., and Bocherens, H. (2009). Carbon stable isotopes of mammal bones as tracers of canopy development and habitat use in temperate and boreal contexts.. In: Creighton, J.D., Roney, P.J. (Eds.), Forest Canopies: Forest Production, Ecosystem Health, and Climate Conditions. Nova Science Publishers, Hauppauge, NY., 103–109.Google Scholar
Gannett, M.W., and Caldwell, R.R. (1998). Geologic framework of the Willamette Lowland aquifer system, Oregon and Washington.. Professional Papers, 1424-A U.S. Department of the Interior, U.S. Geological Survey, Denver.Google Scholar
Gilbert, M.T., Jenkins, D.L., Gotherstrom, A., Naveran, N., Sanchez, J.J., Hofreiter, M., Thomsen, P.F., Binladen, J., Higham, T.F.G., Yohe II, R.M., Parr, R., Cummings, L.S., and Willerslev, E. (2008). DNA from pre-Clovis human coprolites in Oregon, North America.. Science 320, 786–789.Google Scholar
Gilmour, D.M. (2011). Chronology and Ecology of Late Pleistocene Megafauna in the Northern Willamette Valley, Oregon. Unpublished Master of Arts thesis. Department of Anthropology, Portland State University,, Portland..Google Scholar
Glenn, J.L. (1965). Late Quaternary Sedimentation and Geological History of the North Willamette Valley, Oregon. Unpublished doctoral dissertation. Department of Geology, Oregon State University,, Corvallis..Google Scholar
Goebel, T., Waters, M.R., and O'Rourke, D.H. (2008). The late Pleistocene dispersal of modern humans in the Americas.. Science 319, 1497–1502.CrossRefGoogle ScholarPubMed
Goldberg, P., Berna, F., and Macphail, R.I. (2009). Comment on “DNA from Pre-Clovis Human Coprolites in Oregon, North America”.. Science 325, 148c.Google Scholar
Grayson, D.K. (2007). Deciphering North American Pleistocene extinctions.. Journal of Anthropological Research 63, 185–213.Google Scholar
Grayson, D.K. (2011). The Great Basin: A Natural Prehistory.. University of California Press, Berkeley.CrossRefGoogle Scholar
Grootes, P.M., Stuiver, M., White, J.W.C., Johnsen, S., and Jouzel, J. (1993). Comparison of oxygen isotope records from the GISP2 and GRIP Greenland ice cores.. Nature 366, 552–554.Google Scholar
Grund, B.S., Surovell, T.A., and Lyons, S.K. (2012). Range sizes and shifts of North American Pleistocene mammals are not consistent with a climatic explanation for extinction.. World Archaeology 44, 43–55.CrossRefGoogle Scholar
Hay, O.P. (1927). The Pleistocene of the Western Region of North America and Its Vertebrated Animals.. Carnegie Institution of Washington, Washington D.C..Google Scholar
Haynes, G. (1991). Mammoths, Mastodonts, and Elephants.. Cambridge University Press, New York.Google Scholar
Haynes, G. (2009). American Megafaunal Extinctions at the End of the Pleistocene.. Springer, New York.Google Scholar
Haynes, G. (2007). Comment on "Redefining the Age of Clovis: Implications for the Peopling of the Americas".. Science 317, 320.Google Scholar
Jenkins, D.L. (2012). Clovis age Western stemmed projectile points and human coprolites at the Paisley Caves.. Science 337, 223–228.Google Scholar
Jones, G.T., Beck, C.T., Jones, E.E., and Hughes, R.E. (2003). Archaeology Lithic Source Use and Paleoarchaic Foraging Territories in the Great Basin.. American Antiquity 68, 5–38.Google Scholar
Koch, P.L., and Barnosky, A.D. (2006). Late Quaternary extinctions: state of the debate.. Annual Review of Ecology, Evolution, and Systematics 37, 215–250.Google Scholar
Koch, P.L., Hoppe, K.A., and Webb, D.S. (1998). The isotopic ecology of Late Pleistocene mammals in North America: part 1 – Florida.. Chemical Geology 152, 119–138.Google Scholar
Longin, R. (1971). New method of collagen extraction for radiocarbon dating.. Nature 230, 241–242.CrossRefGoogle ScholarPubMed
Lorenzen, E.D. (2011). Species-specific responses of Late Quaternary megafauna to climate and humans.. Nature 479, 359–364.CrossRefGoogle ScholarPubMed
Lyman, R.L. (2013). Paleoindian exploitation of mammals in eastern Washington State.. American Antiquity 78, 227–247.CrossRefGoogle Scholar
Lysek, C.A. (1999). Amateur paleontologist uncovers Oregon mammoths.. Mammoth Trumpet 14, 2 14–16.Google Scholar
MacFadden, B.J. (1992). Fossil Horses: Systematics, Paleobiology, and Evolution of the Family Equidae.. Cambridge University Press, New York.Google Scholar
MacFadden, B.J., Cerling, T.E., Harris, J.M., and Prado, J. (1999). Ancient latitudinal gradients of C3/C4 grasses interpreted from stable isotopes of New World Pleistocene horse (Equus) teeth.. Global Ecology and Biogeography 8, 137–149.Google Scholar
Marcott, S.A., Fountain, A.G., O'Connor, J.E., Sniffen, P.J., and Dethier, D.P. (2009). A latest Pleistocene and Holocene glacial history and paleoclimate reconstruction at Three Sisters and Broken Top Volcanoes, Oregon, U.S.A.. Quaternary Research 71, 181–189.Google Scholar
Martin, P.S. (1967). Prehistoric overkill.. In: Martin, P.S., Wright, H.E. (Eds.), Pleistocene Extinctions: The Search for a Cause. Yale University Press, New Haven., pp. 75–120.Google Scholar
Martin, P.S. (1973). The discovery of America.. Science 179, 969–974.Google Scholar
McCornack, E.C. (1914). A study of Oregon Pleistocene.. University of Oregon Bulletin, New Series 12, 2 2–16.Google Scholar
McCornack, E.C. (1920). Contributions to the Pleistocene history of Oregon.. University of Oregon Leaflet Series, Geology Bulletin 6, 1–22.Google Scholar
McDonald, J.N. (1981). North American Bison: Their Classification and Evolution.. University of California Press, Berkeley.Google Scholar
McDonald, H.G., and Pelikan, S. (2006). Mammoths and mylodonts: exotic species from two different continents in North American Pleistocene faunas.. Quaternary International 142–143, 229–241.Google Scholar
McDonald, H., Agenbroad, L.D., and Haden, C.M. (2004). Late Pleistocene mylodont sloth Paramylodon harlani (Mammalia: Xenarthra) from Arizona.. The Southwestern Naturalist 49, 229–238.Google Scholar
Meltzer, D.J. (2004). Peopling of North America.. In: Gillespie, A., Porter, S.C., Atwater, B. (Eds.), The Quaternary Period in the United States. Elsevier Science, New York., pp. 539–563.Google Scholar
Meltzer, D.J., and Bar-Yosef, O. (2012). Looking for the Younger Dryas.. In: Eren, M.I. (Ed.), Hunter–Gatherer Behavior: Human Response During the Younger Dryas. Left Coast Press, Walnut Creek., pp. 249–267.Google Scholar
Meltzer, D.J., and Holliday, V.T. (2010). Would North American Paleoindians have noticed Younger Dryas age climate changes?.. Journal of World Prehistory 23, 1–41.Google Scholar
Minervini, J.M., O'Connor, J.E., and Wells, R.E. (2003). Maps showing inundation depths, ice-rafted erratics, and sedimentary facies of Late Pleistocene Missoula floods in the Willamette Valley, Oregon.. Open-File Reports, 03-408 U.S. Department of the Interior, U.S. Geological Survey, Denver.Google Scholar
Newsom, L.A., and Mihlbachler, M.C. (2006). Mastodon (Mammut americanum) diet and foraging patterns based on dung material from the Page/Ladson Site (8JE581), Jefferson County, Florida.. In: Webb, S.D. (Ed.), The First Floridians and Last Mastodons: the Page-Ladson Site in the Aucilla River. Springer, Dordrecht. pp. 263–333.Google Scholar
O'Connor, J.E., and Benito, G. (2009). Late Pleistocene Missoula Floods: 15,000–20,000 calendar years before present from radiocarbon dating.. Geological Society of America Abstracts with Programs 41, 169.Google Scholar
O'Connor, J., Sarna-Wojcicki, A., Wozniak, K.C., Polette, D.J., and Fleck, R.J. (2001). Origin, extent, and thickness of Quaternary geologic units in the Willamette Valley, Oregon.. Professional Papers, 1620 U.S. Department of the Interior, U.S. Geological Survey, Denver.Google Scholar
Perkins, H.C. (1842). Notice of fossil bones from Oregon Territory in a letter to Dr. C.T. Jackson.. American Journal of Science and Arts 42, 136–140.Google Scholar
Personius, S.F., Kelsey, H.M., and Grabau, P.C. (1993). Evidence for regional stream aggradation in the central Oregon Coast Range during the Pleistocene–Holocene transition.. Quaternary Research 40, 297–308.Google Scholar
Poinar, H., Fiedel, S., King, C.E., Devault, A.M., Bos, K., Kuch, M., and Debruyne, R. (2009). Comment on “DNA from Pre-Clovis Human Coprolites in Oregon, North America”.. Science 25, 148a.Google Scholar
Rasmussen, M. (2014). The genome of a Late Pleistocene human from a Clovis burial site in western Montana.. Nature 506, 225–229.Google Scholar
Reese, J., and Fagan, J.L. (1997). An Early-Holocene archaeological site in Oregon's Willamette Valley.. Current Research in the Pleistocene 14, 77–78.Google Scholar
Reimer, P.J. (2013). IntCal13 and Marine13 radiocarbon age calibration curves 0–50,000 years cal BP.. Radiocarbon 55, 1869–1887.CrossRefGoogle Scholar
Rivals, F., Solounias, N., and Mihlbachler, M.C. (2007). Evidence for geographic variation in the diets of Late Pleistocene and Early Holocene bison in North America, and differences from the diets of recent bison.. Quaternary Research 68, 338–346.Google Scholar
Scott, E. (2006). Extinct horses and their relatives.. In: Jefferson, G.T., Lindsey, L. (Eds.), Fossil Treasures of the Anza-Borrego Desert: The Last Seven Million Years. Sunbelt, San Diego., 253–271.Google Scholar
Simpson, G.G. (1942). The Beginnings of vertebrate paleontology in North America.. Proceedings of the American Philosophical Society 81, 130–188.Google Scholar
Stafford jr., T.W., Brendel, K., and Duhamel, R.C. (1988). Radiocarbon, 13C and 15N analysis of fossil bone: removal of humates with XAD-2 Resin.. Geochimica et Cosmochimica Acta 52, 2257–2267.Google Scholar
Stafford jr., T.W., Hare, P.E., Currie, L.A., Jull, A.J.T., and Donahue, D. (1991). Accelerator radiocarbon dating at the molecular level.. Journal of Archaeological Science 18, 35–72.Google Scholar
Stenger, A.T. (2002). Temporal association of paleontological and archaeological resources in Woodburn, ca. 12,000 BP: a preliminary report.. Current Archaeological Happenings in Oregon 27(3/4), 12–17.Google Scholar
Stuiver, M., and Grootes, P.M. (2000). GISP2 oxygen isotope ratios.. Quaternary Research 53, 277–284.CrossRefGoogle Scholar
Stuiver, M., and Polach, H.A. (1977). Discussion: reporting of 14C data.. Radiocarbon 19, 355–363.Google Scholar
Vacco, D.A., Clark, P.U., Mix, A.C., Cheng, H., and Edwards, R.L. (2005). A speleothem record of Younger Dryas cooling, Klamath Mountains, Oregon, USA.. Quaternary Research 60, 249–256.Google Scholar
van Klinken, G.J. (1999). Bone collagen quality indicators for palaeodietary and radiocarbon measurements.. Journal of Archaeological Science 26, 687–695.Google Scholar
Waitt, R.B. (1980). About 40 Last-glacial Lake Missoula jökulhlaups through southern Washington.. Journal of Geology 88, 653–679.Google Scholar
Waitt, R.B. (1985). Case for periodic, colossal jökulhlaups from Pleistocene Glacial Lake Missoula.. Geological Society of America Bulletin 96, 1271–1286.Google Scholar
Walsh, M.K., Whitlock, C., and Bartlein, P.J. (2008). 14,300-year-long record of fire–vegetation–climate linkages at Battle Ground Lake, southwestern Washington.. Quaternary Research 70, 251–264.Google Scholar
Wampler, P.J. (2004). Contrasting Styles of Geomorphic Response to Climatic, Anthropogenic, and Fluvial Changes Across Modern to Millennial Time Scales, Clackamas River, Oregon. Unpublished doctoral dissertation. Department of Geology, Oregon State University, , Corvallis. .Google Scholar
Ward, G.K., and Wilson, S.R. (1978). Procedures for comparing and combining radiocarbon age-determinations: a critique.. Archaeometry 20, 19–31.Google Scholar
Waters, M.R., and Stafford jr., T.W. (2007). Redefining the Age of Clovis: implications for the peopling of the Americas.. Science 315, 1122–1126.Google Scholar
Waters, M.R., Stafford jr., T.W., McDonald, H.G., Gustafson, C., Rasmussen, M., Cappellini, E., Olsen, J.V., Szklarczyk, D., Jensen, L.J., Gilbert, M.T.P. Gilbert, and Willerslev, E. (2011). Pre-Clovis mastodon hunting 13,800 years ago at the Manis Site, Washington.. Science 334, 351–353.Google Scholar
Webb, D.S. (1992). A brief history of New World Proboscidea with emphasis on their adaptations and interactions with man.. In: Fox, J.W., Smith, C.B., Wilkins, K.T.(Eds.), Proboscidean and Paleoindian Interactions. Baylor University Press, Waco. pp. 15–34.Google Scholar
Wilkes, C. (1844). Narrative of the United States Exploring Expedition During the Years 1838, 1839, 1840, 1841, 1842, volume 4.. C. Sherman, Philadelphia.Google Scholar
Yamhill River Pleistocene Project, (2010). The Yamhill River Pleistocene Project. http://www.yamhillriverpleistocene.com/ (Accessed October 1, 2010).Google Scholar
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