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Climate in the Great Lakes Region Between 14,000 and 4000 Years Ago from Isotopic Composition of Conifer Wood

  • Steven W Leavitt (a1), Irina P Panyushkina (a1), Todd Lange (a2), Alex Wiedenhoeft (a3), Li Cheng (a1), R Douglas Hunter (a4), John Hughes (a5), Frank Pranschke (a6), Allan F Schneider (a7), Joseph Moran (a8) and Ron Stieglitz (a8)...

Abstract

The isotopic composition of ancient wood has the potential to provide information about past environments. We analyzed the δ13C, δ18O, and δ2H of cellulose of conifer trees from several cross-sections at each of 9 sites around the Great Lakes region ranging from ∼4000 to 14,000 cal BP. Isotopic values of Picea, Pinus, and Thuja species seem interchangeable for δ18O and δ2H comparisons, but Thuja appears distinctly different from the other 2 in its δ13C composition. Isotopic results suggest that the 2 sites of near-Younger Dryas age experienced the coldest conditions, although the Gribben Basin site near the Laurentide ice sheet was relatively dry, whereas the Liverpool site 500 km south was moister. The spatial isotopic variability of 3 of the 4 sites of Two Creeks age shows evidence of an elevation effect, perhaps related to sites farther inland from the Lake Michigan shoreline experiencing warmer daytime growing season temperatures. Thus, despite floristic similarity across sites (wood samples at 7 of the sites being Picea), the isotopes appear to reflect environmental differences that might not be readily evident from a purely floristic interpretation of macrofossil or pollen identification.

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Copyright

Corresponding author

Corresponding author. Email: sleavitt@u.arizona.edu

References

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Becker, B, Kromer, B, Trimborn, P. 1991. A stable-isotope tree-ring timescale of the late Glacial-Holocene boundary. Nature 353:647–9.
Booth, RK, Jackson, ST, Thompson, TA. 2002. Paleoecology of a northern Michigan Lake and the relationship among climate, vegetation, and Great Lakes water levels. Quaternary Research 57:120–30.
Bryson, RA, Baerreis, DA, Wendland, WM. 1970. The character of late-glacial and post-glacial climatic changes. In: Dort, WJ, Jones, JK, editors. Pleistocene and Recent Environments of the Central Great Plains. Lawrence: University of Kansas Press. p 5374.
Edwards, TWD, Fritz, P. 1986. Assessing meteoric water composition and relative humidity from 18O and 2H in wood cellulose: paleoclimatic implications for southern Ontario, Canada. Applied Geochemistry 1:715–23.
Farquhar, GD, O'Leary, MH, Baxter, JA. 1982. On the relationship between carbon isotope discrimination and intercellular carbon dioxide concentration in leaves. Australian Journal of Plant Physiology 9:121–37.
Friedman, I, Smith, GI. 1970. Deuterium content of snow cores from Sierra Nevada area. Science 169:467–70.
Friedrich, M, Kromer, B, Spurk, M, Hoffman, J, Kauser, KF. 1999. Paleo-environment and radiocarbon calibration as derived from Lateglacial/Early Holocene tree-ring chronologies. Quaternary International 61:2739.
Gray, J, Thompson, P. 1976. Climatic information from 18O/16O ratios of cellulose in tree rings. Nature 262: 481–2.
Hemming, DL, Switsur, VR, Waterhouse, JS, Heaton, THE, Carter, AHC. 1998. Climate variation and the stable carbon isotope composition of tree ring cellulose: an intercomparison of Quercus robur, Fagus sylvatica and Pinus silvestris . Tellus 50B:2533.
Hunter, RD, Panyushkina, IP, Leavitt, SW, Wiedenhoeft, AC, Zawiskie, J. 2006. A mid-Holocene submerged conifer forest in the southern Lake Huron Basin. Quaternary Research 66:6777.
Kaiser, KF. 1994. Two Creeks Interstade dated through dendrochronology and AMS. Quaternary Research 42(3):288–98.
Kendall, C, Coplen, TB. 2002. Distribution of oxygen-18 and deuterium in river waters across the United States. Hydrological Processes 15:1363–93.
Kerwin, M, Overpeck, JT, Webb, RS, DeVernal, A, Rind, DH, Healy, RJ. 1999. The role of oceanic forcing in mid-Holocene Northern Hemisphere climatic change. Paleoceanography 14:200–10.
Leavitt, SW. 2002. Prospects for reconstruction of seasonal environment from tree-ring d13C: Baseline findings from the Great Lakes area, U.S.A. Chemical Geology 192(1–2):4758.
Leavitt, SW. Forthcoming. Regional expression of the 1988 U.S. Midwest drought in seasonal d13C of tree rings. Journal of Geophysical ResearchAtmospheres .
Leavitt, SW, Long, A. 1984. Sampling strategy for stable carbon isotope analysis of tree rings in pine. Nature 311:145–7.
Leavitt, SW, Long, A. 1986. Stable-carbon isotope variability in tree foliage and wood. Ecology 67:1002–10.
Leavitt, SW, Long, A. 1988. Intertree variability of d13C in tree rings. In: Rundel, PW, Ehleringer, JR, Nagy, KA, editors. Stable Isotopes in Ecological Research . Chapter 7. New York: Springer-Verlag. p 95104.
Leavitt, SW, Long, A. 1989. Drought indicated in carbon-13/carbon-12 ratios of southwestern tree rings. Water Resources Bulletin 25:341–7.
Leavitt, SW, Kalin, RM. 1992. A new tree-ring width, d13C and 14C investigation of the Two Creeks site. Radiocarbon 34(3):792–7.
Leavitt, SW, Newberry, T. 1992. Systematics of stable-carbon isotopic differences between gymnosperm and angiosperm trees. Plant Physiology (Life Sci. Adv.) 11: 257–62.
Leavitt, SW, Danzer, SR. 1993. Method for batch processing small wood samples to holocellulose for stable-carbon isotope analysis. Analytical Chemistry 65:87–9.
Leavitt, SW, Wright, WE, Long, A. 2002. Spatial expression of ENSO, drought and summer monsoon in seasonal d13C of ponderosa pine tree rings in southern Arizona and New Mexico. Journal of Geophysical Research 107(D18):4349. doi:10.1029/2001JD001312.
Lipp, J, Trimborn, P, Fritz, P, Moser, H, Becker, B, Frenzel, B. 1991. Stable isotopes in tree ring cellulose and climatic change. Tellus 43B:322–30.
Lowell, TV, Larson, GJ, Hughes, JD, Denton, GH. 1999. Age verification of the Lake Gribben forest bed and the Younger Dryas advance of the Laurentide ice sheet. Canadian Journal of Earth Science 36:383–93.
Mayr, C, Frenzel, B, Friedrich, M, Spurk, M, Stichler, W, Trimborn, P. 2003. Stable carbon- and hydrogen-isotope ratios of subfossil oaks in southern Germany: Methodology and application to a composite record for the Holocene. The Holocene 13:393402.
Moran, JM, Stieglitz, RD, Quigley, DP. 1988. Glacial geology, road construction in northeast Wisconsin reveals clues to Earth's natural history. Earth Science (winter):1618.
Pranschke, F, Schabica, CW. 1993. The remains of an 8200-year-old forest on the floor of southern Lake Michigan [final Report to the National Geographic Society]. Grant #4748-92.
Pregitzer, KS, Reed, DD, Bornhorst, TJ, Foster, DR, Mroz, GD, McLachlin, JS, Laks, PE, Stokke, DD, Martin, PE, Brown, SE. 2000. A buried spruce forest provides evidence at the stand and landscape scale for the effects of environment on vegetation at the Pleistocene/Holocene boundary. Journal of Ecology 88:4553.
Ramesh, R, Bhattacharya, SK, Gopalan, K. 1985. Dendro-chronological implications of isotope coherence in trees from Kashmir Valley, India. Nature 317:802–4.
Reimer, PJ, Baillie, MGL, Bard, E, Bayliss, A, Beck, JW, Bertrand, CJH, Blackwell, PG, Buck, CE, Burr, GS, Cutler, KB, Damon, PE, Edwards, RL, Fairbanks, RG, Friedrich, M, Guilderson, TP, Hogg, AG, Hughen, KA, Kromer, B, McCormac, FG, Manning, SW, Ramsey, CB, Reimer, RW, Remmele, S, Southon, JR, Stuiver, M, Talamo, S, Taylor, FW, van der Plicht, J, Weyhenmeyer, CE. 2004. IntCal04 terrestrial radiocarbon age calibration, 26–0 kyr BP. Radiocarbon 46(3):1029–58.
Roden, JS, Lin, G, Ehleringer, JR. 1999. A mechanistic model for interpretation of hydrogen and oxygen isotope ratios in tree ring cellulose. Geochimica et Cosmochimica Acta 64:2135.
Saurer, M, Siegenthaler, U. 1989. 13C/12C ratios in tree are sensitive to relative humidity. Dendrochronologia 7: 913.
Saurer, M, Borella, S, Leuenberger, M. 1997. d18O of tree rings of beech (Fagus silvatica) as a record of d18O of the growing season precipitation. Tellus 49B:8092.
Schneider, AF, Hansel, AK. 1990. Evidence for post-Two Creeks age of the type Calumet shoreline of glacial Lake Chicago. Geological Society of America Special Paper 251. p 18.
Shane, LCK, Anderson, KH. 1993. Intensity, gradients and reversals in late glacial environmental change in east-central North America. Quaternary Science Reviews 12:397–20.
Smith, HJ, Fischer, H, Mastroianni, D, Deck, B, Wahlen, M. 1999. Dual modes of the carbon cycle since the last glacial maximum. Nature 400:248–50.
Sternberg, LSL. 1989. Oxygen and hydrogen isotope measurements in plant cellulose analysis. In: Linskens, HF, Jackson, JF, editors. Plant Fibres. Modern Methods of Plant Analysis. Volume 10. New York: Springer-Verlag. p 8999.
Stuiver, M, Braziunas, TF. 1987. Tree cellulose 13C/12C isotope ratios and climate change. Nature 328:5860.
Stuiver, M, Reimer, PJ. 1993. Extended 14C database and revised CALIB radiocarbon calibration program (Version 5.0). Radiocarbon 35(1):215–30.
Stuiver, M, Reimer, PJ, Braziunas, TF. 1998. High-precision radiocarbon age calibration for terrestrial and marine samples. Radiocarbon 40(3):1127–51.
Thwaites, FT. 1958. The Green Bay forest bed locality [unpublished manuscript]. 3 p.
Winkler, MG, Swain, AM, Kutzbach, JE. 1986. Middle-Holocene dry period in the northern midwestern United States: lake levels and pollen stratigraphy. Quaternary Research 25:235–50.
Yakir, D, DeNiro, MJ. 1990. Oxygen and hydrogen isotope fractionation during cellulose metabolism in Lemna gibba L. Plant Physiology 93:325–32.
Yapp, CJ, Epstein, S. 1977. Climatic implications of D/H ratios of meteoric water over North America (9500–22,000 B.P.) as inferred from ancient wood cellulose C-H hydrogen. Earth and Planetary Science Letters 34:333–50.
Yapp, CJ, Epstein, S. 1982. Climatic significance of the hydrogen isotope ratios in tree cellulose. Nature 297: 636–9.
Yu, Z. 2000. Ecosystem response to Lateglacial and early Holocene climate oscillations in the Great Lakes region of North America. Quaternary Science Reviews 19:1723–47.

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