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Stable Isotopes in Pocket Gopher Teeth as Evidence of a Late Matuyama Climate Shift in the Southern Rocky Mountains

Published online by Cambridge University Press:  20 January 2017

Karel L. Rogers  and
Yang Wang
Karel L. Rogers
Affiliation:
Biology Department, 218 Padnos, Grand Valley State University, Allendale, Michigan, 49401-9403, E-mail: rogersk@gvsu.edu
Yang Wang
Affiliation:
Department of Geological Sciences, 108 Carraway Building, Florida State University, Tallahassee, Florida, 32306-4100
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Abstract

Previous work in the San Luis Valley of south-central Colorado and northern New Mexico at the Hansen Bluff and SAM Cave localities has allowed reconstruction of the paleoclimate in the region during the interval from ∼0.6 myr to ∼2.6 myr. Surface exposures at Hansen Bluff have been correlated to deep-sea oxygen isotope core stages 18–23 and one of the glacial periods contained therein to the oldest “Nebraskan” till in southwestern Iowa. Deposits in SAM Cave correlate to Hansen Bluff on the basis of paleomagnetics, climate interpretation, and microtine rodent biochronology. In this paper, carbon and oxygen stable isotope data of herbivorous rodent teeth are used as indicators of change in the predominance of C3, C4, and CAM plants and of changes in temperature and precipitation. Taken together with other previously analyzed data from these localities, the evidence indicates a shift in the severity of glacial events that is mainly related to the hydrologic characteristics of the climate. This shift may have been caused by broad regional uplift that may have been instrumental in shifting global climate cycles from the 41,000-yr Matuyama cycles to the Brunhes 100,000-yr-dominated cycles.

Keywords

stable isotopesenamelPleistocenepaleoclimateColorado Plateauregional upliftBrunhesMatuyama
Type
Research Article
Information
Quaternary Research , Volume 57 , Issue 2 , March 2002 , pp. 200 - 207
Copyright
University of Washington

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References

Barnosky, A.D What causes “disharmonious” mammal assemblages?. Saunders, J.J, Styles, B.W, and Baryshnikov, G.F Quaternary Paleozoology in the Northern Hemisphere. (1998). 173–186.Google Scholar
Bell, C.J, and Barnosky, A.D The Microtine rodents from the Pit Locality in Porcupine Cave, Park County, Colorado. Annals of the Carnegie Museum 69, (2000). 93–134.CrossRefGoogle Scholar
Berggren, W.A, Hilgen, F.J, Langereis, C.G, Kent, D.V, Obradovich, J.D, Raffi, I, Raymo, M.E, and Shackleton, N.J Late Neogene chronology: New perspectives in high-resolution stratigraphy. Geological Society of America Bulletin 107, (1995). 1272–1287.2.3.CO;2>CrossRefGoogle Scholar
Cerling, T.E, Wang, Y, and Quade, J Expansion of C4 ecosystems as an indicator of global ecological change in the late Miocene. Nature 361, (1993). 344–345.CrossRefGoogle Scholar
Davis, M.B, and Shaw, R.G Range shifts and adaptive responses to Quaternary climate change. Science 292, (2001). 673–679.CrossRefGoogle ScholarPubMed
Hoffmeister, D.F Mammals of Arizona. (1986). University of Arizona Press, Tucson.Google Scholar
Kukla, G.J Pleistodene land–sea correlations I. Europe. Earth Science Reviews 13, (1977). 307–374.CrossRefGoogle Scholar
MacFadden, B.J Middle Pleistocene climate change recorded in fossil mammal teeth from Tarija, Bolivia, and upper limit of the Ensenadan Land-Mammal Age. Quaternary Research 54, (2000). 121–131.CrossRefGoogle Scholar
McCrea, J.M On the isotopic chemistry of carbonates and a paleotemperature scale. Journal of Chemical Physics 18, (1950). 849–857.CrossRefGoogle Scholar
Peizhen, Z, Molnar, P, and Downs, W.R Increased sedimentation rates and grain sizes 2–4 Myr ago due to the influence of climate change on erosion rates. Nature 410, (2001). 891–897.Google Scholar
Pisias, N.G, and Moore, T.C The evolution of Pleistocene climate: A time series approach. Earth and Planetary Science Letters 52, (1981). 450–458.CrossRefGoogle Scholar
Raymo, M.E, Ruddiman, W.F, Backman, J, Clement, B.M, and Matinson, D.G Late Pliocene variation in Northern Hemisphere ice sheets and North Atlantic deep water circulation. Paleoceanography 4, (1989). 413–446.Google Scholar
Rogers, K.L, Repenning, C.A, Forester, R.M, Larson, E.E, Hall, S.A, Smith, G.R, Anderson, E, and Brown, T.J Middle Pleistocene (Late Irvingtonian: Nebraskan) climatic changes in south-central Colorado. National Geographic Research 1, (1985). 535–563.Google Scholar
Rogers, K.L, Larson, E.E, Smith, G, Katzman, D, Smith, G.R, Cerling, T, Wang, Y, Baker, R.G, Lohmann, K.C, Repenning, C.A, Patterson, P, and Mackie, G Pliocene and Pleistocene geologic and climatic evolution in the San Luis Valley of south-central Colorado. Palaeogragraphy, Palaeoclimatology, and Palaeoecology 94, (1992). 55–86.CrossRefGoogle Scholar
Rogers, K.L, Repenning, C.A, Luiszer, F.G, and Benson, R.D Geologic hisotry, stratigraphy, and paleontology of SAM Cave, north-central New Mexico. New Mexico Geology 22, (2000). 89–100.CrossRefGoogle Scholar
Ruddiman, W.F, and Kutzbach, J.E Forcing of late Cenozoic Northern Hemisphere climate by plateau uplift in southern Asia and the American West. Journal of Geophysical Research 94, (1989). 409–418.Google Scholar
Ruddiman, W.F, and Raymo, M.E Northern Hemisphere climate regimes during the past 3 Ma: Possible tectonic connections. Philosophical Transaction of the Royal Society of London B 318, (1988). 414–430.Google Scholar
Ruddiman, W.F, Raymo, M, and McIntyre, A Matuyama 41,000-year cycles: North Atlantic Ocean and Northern Hemisphere ice sheets. Earth and Planetary Science Letters 80, (1986). 117–129.Google Scholar
Sancetta, C, and Silvestri, S Pliocene–Pleistocene evolution of the North Pacific ocean–atmosphere system, interpreted from fossil diatoms. Paleoceanography 1, (1986). 163–180.Google Scholar
Shackleton, N.J, and Opdyke, N.D Oxygen-isotope and paleomagnetic stratigraphy of Pacific Core V28-239 late Pliocene to latest Pleistocene. Geological Society of America Memoir 145, (1976). 449–464.Google Scholar
Shackleton, N.J, Backman, J, Zimmerman, H, Kent, D.V, Hall, M.A, Roberts, D.G, Schnitker, D, and Baldauf, J Oxygen isotope calibration of the onset of ice-rafting and history of glaciation in the North Atlantic region. Nature 307, (1984). 620–623.CrossRefGoogle Scholar
Teeri, J.A, and Stowe, L.G Climatic patterns and the distribution of C4 grasses in North America. Oecologia 23, (1976). 1–12.CrossRefGoogle ScholarPubMed
Wang, T, and Cerling, T.E A model of fossil tooth and bone diagenesis: Implications for paleodiet reconstruction from stable isotopes. Palaeogragraphy, Palaeoclimatology, and Palaeoecology 107, (1994). 281–289.CrossRefGoogle Scholar
Wood, D.L, and Barnosky, A.D Middle Pleistocene climate change in the Colorado Rocky Mountains indicated by fossil mammals from Porcupine Cave. Quaternary Research 41, (1994). 366–375.Google Scholar
Zachos, J, Pagani, M, Sloan, L, Thomas, E, and Billups, K Trends, rhythms, and aberrations in global climate 65 Myr to present. Science 292, (2001). 686–693.CrossRefGoogle Scholar