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Episodes of late Holocene aridity recorded by stalagmites from Devil's icebox Cave, Central Missouri, USA

Published online by Cambridge University Press:  20 January 2017

Rhawn F. Denniston ,
Michelle DuPree ,
Jeffrey A. Dorale ,
Yemane Asmerom ,
Victor J. Polyak  and
Scott J. Carpenter
Rhawn F. Denniston*
Affiliation:
Department of Geology, Cornell College, Mount Vernon, IA 52314, USA
Michelle DuPree
Affiliation:
Department of Geology, Cornell College, Mount Vernon, IA 52314, USA
Jeffrey A. Dorale
Affiliation:
Department of Geoscience, University of Iowa, Iowa City, IA 52242, USA
Yemane Asmerom
Affiliation:
Department of Earth and Planetary Sciences, University of New Mexico, Albuquerque, NM 87131, USA
Victor J. Polyak
Affiliation:
Department of Earth and Planetary Sciences, University of New Mexico, Albuquerque, NM 87131, USA
Scott J. Carpenter
Affiliation:
Department of Geoscience, University of Iowa, Iowa City, IA 52242, USA
*
*Corresponding author. Fax: +1 319 895 5667.E-mail address:RDenniston@CornellCollege.edu (R.F. Dennison)
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Abstract

Two stalagmites from Devil's Icebox Cave, central Missouri, display similar δ13C and δ18O values and trends during the late Holocene. Positive δ13C excursions at 3.5–2.6 ka and 1.2–0.9 ka are interpreted to reflect drier conditions. These elevated stalagmite δ13C values could have plausibly been driven by increasing C4 plant abundances over the cave or an increased contribution of bedrock carbon, both of which could reflect decreased effective moisture. A lack of corresponding oxygen isotopic anomalies during these intervals suggests that neither mean annual temperature nor the seasonality of precipitation changed concomitantly with dryness. Both of the δ13C excursions identified in our stalagmite record are roughly coincident with dry intervals from a number of sites located across the Great Plains.

Keywords

SpeleothemPrairieLate HoloceneDrynessCarbonOxygenIsotope
Type
Research Article
Information
Quaternary Research , Volume 68 , Issue 1 , July 2007 , pp. 45 - 52
Copyright
University of Washington

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Footnotes

1 Current address: Department of Geology, Ball State University, Muncie, IN 47306, USA

References

Arbogast, A.F. (1996). Stratigraphic evidence for late-Holocene Aeolian sand mobilization and soil formation in south-central Kansas, U.S..Journal of Arid Environments, 34, 403–411.CrossRefGoogle Scholar
Baker, A., Ito, E., Smart, P.L., McEwan, R.F.(1997). Elevated and variable values of 13C in speleothems in a British cave system.Chemical Geology, 136, 263–270.CrossRefGoogle Scholar
Baker, R.G., González, L.A., Raymo, M., Bettis, E.A. III, Reagan, M.K., Dorale, J.A.(1998). Comparison of multiple proxy records of Holocene environments in the midwestern United States.Geology, 26, 1131–1134.Google Scholar
Baker, R.G., Fredlund, G.G., Mandel, R.D., Bettis, E.A. III(2000). Holocene environments of the central Great Plains: multi-proxy evidence from alluvial sequences, southeastern Nebraska.Quaternary International, 67, 75–88.CrossRefGoogle Scholar
Banner, J.L., Kaufman, J.(1994). The isotopic record of ocean chemistry and diagenesis preserved in non-luminescent brachiopods from Mississippian carbonate rocks, Illinois and Missouri.Geological Society of America Bulletin, 106, 1074–1082.2.3.CO;2>CrossRefGoogle Scholar
Bartlein, P.J., Whitlock, C.(1993). Paleoclimatic interpretation of the Elk Lake record.Bradbury, J.P., Dean, W.E. Elk Lake, Minnesota; Evidence for Rapid Climate Change in the North-Central United States Geological Society of America, Boulder, CO.275–293.Google Scholar
Bond, G., Kromer, B., Beer, J., Muscheler, R., Evans, M.N., Showers, W., Hoffman, S., Lotti-Bond, R., Hajdas, I., Bonani, G.(2001). Persistent solar influence on North Atlantic climate during the Holocene.Science, 294, 2130–2136.CrossRefGoogle ScholarPubMed
Broecker, W.S., Peng, T.H.(1982). Tracers in the Sea. Eldigio Press, Palisades, New York.690 ppGoogle Scholar
Cerling, T.E. (1984). The stable isotopic composition of modern soil carbonate and its relationship to climate.Earth and Planetary Science Letters, 71, 229–240.CrossRefGoogle Scholar
Chen, J., Edwards, L., Wasserburg, W.(1986). 238U, 234U, and 232Th in seawater.Earth and Planetary Science Letters, 80, 241–251.Google Scholar
Clarke, M.L., Rendell, H.M.(2003). Late Holocene dune accretion and episodes of persistent drought in the Great Plains of Northeastern Colorado.Quaternary Science Reviews, 22, 1051–1058.Google Scholar
Cook, E.R., Woodhouse, C.A., Eakin, C.M., Meko, D.M., Stahle, D.W(2004). Long-term aridity changes in the western United States.Science, 306, 1015–1018.Google Scholar
Cramer, B.S, Saltzman, M.R, Day, J.E, Witzke, B.J in press. Lithological expression of global positive carbon isotope excursions in Epeiric sea settings: carbonate production, organic carbon burial, and oceanography during the late Famennian, Special Paper-Geological Association of Canada..Google Scholar
Daniels, J.M., Knox, J.C.(2005). Alluvial stratigraphic evidence for channel incision during the Medieval Warm Period, Central Great Plains, USA.Holocene, 15, 736–747.CrossRefGoogle Scholar
Dansgaard, W. (1964). Stable isotopes in precipitation.Tellus, 16, 436–468.Google Scholar
Denniston, R.F., González, L.A., Asmerom, Y., Baker, R.G., Reagan, M.K., Bettis, E.A. III(1999). Evidence for increased cool season moisture during the middle Holocene.Geology, 27, 815–818.Google Scholar
Dorale, J.A., González, L.A., Reagan, M.K., Pickett, D.A., Murrell, M.T., Baker, R.G.(1992). A high-resolution record of Holocene climate change in speleothem calcite from Cold Water Cave, northeast Iowa.Science, 258, 1626–1630.Google Scholar
Dorale, J.A., Edwards, R.L., Ito, E., Gonzalez, L.A.(1998). Climate and vegetation history of the mid-continent from 75 to 25 ka: a speleothem record from Crevice Cave, Missouri, USA.Science, 282, 1871–1874.CrossRefGoogle Scholar
Dorale, J.A., Edwards, R.L., Onac, B.P.(2002). Stable isotopes as environmental indicators in speleothems.Yuan, D.-X. Karst Processes and the Carbon Cycle.Geological Publishing House, Beijing.107–120.Google Scholar
Dorale, J.A., Edwards, R.L., Alexander, C.A Jr., Shen, C.-C., Richards, D.A., Cheng, H.(2004). Uranium-series dating of speleothems: current techniques, limits and applications.Sasowsky, I.D., Mylroie, J.E. Studies of Cave Sediments: Physical and Chemical Records of Paleoclimate Kluwer Academic/Plenum Publishers, NY.177–197.Google Scholar
Forman, S.L., Oglesby, R., Markgraf, V., Stafford, T.(1995). Paleoclimatic significance of Late Quaternary Eolian deposition on the Piedmont and High Plains, Central United States.Global and Planetary Change, 11, 35–55.Google Scholar
Fritz, S.C., Metcalfe, S.E., Dean, W.(2001). Holocene climate patterns in the Americas from paleolimnological records.Markgraf, V. Interhemispheric Climate Linkages Academic Press, San Diego, CA.163–241.Google Scholar
Frumkin, A., Ford, D.C., Schwarcz, H.P.(2000). Paleoclimate and vegetation of the last glacial cycles in Jerusalem from a speleothem record.Global Biogeochemical Cycles, 14, 863–870.CrossRefGoogle Scholar
Gat, J.R. (1980). The isotopes of hydrogen and oxygen in precipitation.Fritz, P., Fontes, J. Handbook of Environmental Isotope Geochemistry Elsevier, New York.21–44.Google Scholar
Grimm, E.C., Clark, J.S.(1998). Holocene vegetation and climate change in the northern Great Plains: evidence from pollen and charcoal studies.Geological Society of America Annual Meeting Abstracts with Programs, v., p.Google Scholar
Hall, S.A., Lintz, C.(1984). Buried trees, water table fluctuations, and 3000 years of changing climate in west-central Oklahoma.Quaternary Research, 22, 129–133.Google Scholar
Hendy, C.H. (1971). The isotopic geochemistry of speleothems—I. The calculation of the effects of different modes of formation on the isotopic composition of speleothems and their applicability as palaeoclimatic indicators.Geochimica et Cosmochimica Acta, 35, 801–824.CrossRefGoogle Scholar
Hsieh, Y.-P. (1993). Radiocarbon signatures of turnover rates in active soil organic carbon pools.Soil Science Society of America Journal, 57, 1020–1022.Google Scholar
Madole, R.F. (1994). Stratigraphic evidence of desertification in the west-central Great Plains within the past 1000 yr.Geology, 22, 483–486.Google Scholar
Mason, J.A., Swinhart, J.B., Goble, R.J., Loope, D.B.(2004). Late Holocene dune activity linked to hydrological drought, Nebraska Sand Hills, USA.Holocene, 14, 209–217.Google Scholar
Miao, X., Mason, J., Swinehart, J.B., Loope, D.B., Hanson, P.R., Goble, R.J., Liu, X.(2007). A 10,000 year record of dune activity, dust storms, and  severe drought in the central Great Plains.Geology, 35, 119–122.CrossRefGoogle Scholar
Mickler, P.J., Stern, L.A., Banner, J.L.(2006). Large kinetic isotope effects in modern speleothems.Geological Society of America Bulletin, 118, 65–81.Google Scholar
Quade, J. (2004). Isotopic records from ground-water and cave speleothem calcite in North America.Gillespie, A.R., Porter, S.C., Atwater, B.F. The Quaternary Period in the United States Developments in Quaternary Science, vol. 1, Elsevier, 205–220.Google Scholar
Quade, J., Cerling, T.E., Bowman, J.R.(1989). Systematic variation in the carbon and oxyge isotopic composition of Holocene soil carbonate along elevation transects in the southern Great Basin, USA.Geological Society of America, 101, 464–475.2.3.CO;2>CrossRefGoogle Scholar
Schubert, S.D., Suzrez, M.J., Pegion, P.J., Koster, R.D., Bacmeister, J.T.(2004). On the cause of the 1930s Dust Bowl.Science, 303, 1855–1859.Google Scholar
Simpkins, W.W. (1995). Isotopic composition of precipitation in central Iowa.Journal of Hydrology, 172, 185–207.Google Scholar
Stokes, S., Swinehart, J.B.(1997). Middle- and late-Holocene dune reactivation in the Nebraska Sand Hills, USA.Holocene, 7, 263–272.Google Scholar
Stokes, S., Rich, J., Swinehart, J., Loope, D.B.(1999). Holocene timing of megabarchan dune construction in the Nebraska Sand Hills.Geological Society of America Fall Meeting Abstracts with Program, 31, 231 Google Scholar
Stuiver, M., Reimer, P.J.(1993). Extended 14C database and revised CALIB radiocarbon calibration program.Radiocarbon, 35, 215–230.Google Scholar
Swinehart, J.B. (1998). Holocene climate variability in the central Great Plains; the record from Eolian and lake/marsh sediments.Geological Society of America Fall Meeting Abstracts with Program, 30, 250 Google Scholar
Swinehart, J., Nicholson, B., Loope, D., Nicklen, B.(2000). Latest Wisconsin and Holocene climatic fluctuations in a Nebraska Sand Hills peatland inferred from suspended sand content and plant macrofossils.Geological Society of America Fall Meeting Abstracts with Program, 32, 95 Google Scholar
Teeri, J.A., Stowe, L.G.(1976). Climatic patterns and the distribution of C4 grasses in North America.Oecologia, 23, 1–12.Google Scholar
Tieszen, L.L., Boutton, T., Rundel, P.W., Ehlerlinger, J.R., Nagy, K.A.(1989). Stable Isotopes in Ecological Research. Springer-Verlag, New York.167–195.Google Scholar