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Climate in Southwestern Ontario, Canada, between AD 1610 and 1885 Inferred from Oxygen and Hydrogen Isotopic Measurements of Wood Cellulose from Trees in Different Hydrologic Settings

Published online by Cambridge University Press:  20 January 2017

William M. Buhay  and
Thomas W.D. Edwards
William M. Buhay
Affiliation:
Department of Earth Sciences and Waterloo Center for Groundwater Research, University of Waterloo, Waterloo, Ontario, Canada N2L 3G1
Thomas W.D. Edwards
Affiliation:
Department of Earth Sciences and Waterloo Center for Groundwater Research, University of Waterloo, Waterloo, Ontario, Canada N2L 3G1
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Abstract

Oxygen and hydrogen isotopes were measured in wood cellulose and cellulose-nitrate from trees that grew in different hydrologic settings in southwestern Ontario, Canada. An isotope model that accounts for isotopic fractionations associated with photosynthesis in plants was applied to the stable isotope data to infer past meteoric water isotopic composition and seasonal air moisture variations. The model-inferred climate data was rationalized in terms of the trees' hydrologic environment and weather characteristics of the Great Lakes region. The result is an account of summer and winter conditions in southwestern Ontario for 275 years (1610 to 1885) prior to instrumental climate records. Conditions between 1610 and 1750 are inferred to have been cooler and drier than present. This was followed by a warm-moist climate interval between 1750 and 1885 during which there was an increase in winter precipitation. Cool-dry conditions were recorded instrumentally in this region at the end of the nineteenth century.

Type
Research Article
Information
Quaternary Research , Volume 44 , Issue 3 , November 1995 , pp. 438 - 446
Copyright
University of Washington

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References

Ball, T. (1985). A dramatic change in the general circulation on the west coast of Hudson Bay in 1760 AD: Synoptic evidence based on historic records. Syllogeus 37 , 219–228.Google Scholar
Ball, T, (1992). Climatic change, droughts and their social impact: Central Canada, 1811-20, a classic example. In “The Year Without a Summer” (Harrington, C. R., Ed.), pp. 185–195. Canadian Museum of Nature, Ottawa.Google Scholar
Baron, W. A., and Gordon, G. A. (1985). A reconstruction of New England climate using historical materials, 1620–1980. Syllogeus 55 , 229–246.Google Scholar
Bergeron, Y., and Archambault, S. (1993). Decreasing frequency of forest fires in the southern boreal zone of Québec and its relation to global warming since the end of the “Little Ice Age.” The Holocene 3 , 255–259.Google Scholar
Bishop, C. T. J. (1992). Historical variation of water levels in Lakes Erie and Michigan-Huron. Journal of Great Lakes Research 16 , 406–425.Google Scholar
Bryson, R. A., and Hare, F. K. (1974). “Climates of North America.” Elsevier, New York.Google Scholar
Buhay, W. M. (1994). “Stable Isotope (δ18O, δ2C and δl3C) Dendroclimatological Studies in the Waterloo Region of Southern Ontario, Canada, Between AD 1610 and 1990.” Ph.D. dissertation, University of Waterloo.Google Scholar
Burk, R. L., and Stuiver, M. (1981). Oxygen isotope ratios in trees reflect mean annual temperature and humidity. Science 211 , 1417–1419.Google ScholarPubMed
Campbell, I. D., and McAndrews, J. H. (1991). Cluster analysis of late Holocene pollen trends in Ontario. Canadian Journal of Botany 69 , 1719–1730.Google Scholar
Campbell, I. D., and McAndrews, J. H. (1993). Forest disequilibrium caused by rapid Little Ice Age cooling. Nature 366 , 336–338.Google Scholar
Catchpole, A. J. W. (1992). River ice and sea ice in the Hudson Bay Region during the second decade of the nineteenth century, In “The Year Without a Summer” (Harrington, C. R., Ed.), pp. 233–244, Canadian Museum of Nature, Ottawa.Google Scholar
Clague, J. J. Mathewes, R. W. Buhay, W. M., and Edwards, T. W. D. (1992). Early Holocene climate at Castle Peak, southern Coast Mountains, British Columbia, Canada. Palaeogeography, Palaeoclimatology, Palaeoecology 95, 153–167.Google Scholar
Coleman, M. L. Shepherd, T. J. Durham, J. E. Rouse, J. E., and Moore, G. R. (1982). Reduction of water with zinc for hydrogen isotope analysis. Analytical Chemistry 54 , 993–995.Google Scholar
DeNiro, M. J. (1981). The effects of different methods of preparing cellulose nitrate on the determination of the D/H ratios of non-exchangeable hydrogen of cellulose. Earth and Planetary Science Letters 54 , 1845–1854.Google Scholar
DeNiro, M. J., and Cooper, L. W. (1989). Post-photosynthetic modification of oxygen isotope ratios of carbohydrates in the potato: Implications for paleoclimatic reconstruction based on isotopic analysis of wood cellulose. Geochimica et Cosmockimica Acta 53 , 2573–2580.Google Scholar
Edwards, T. W. D. (1990). New contributions to isotope dendroclimatology from studies of plants. Geochimica et Cosmockimica Acta 54 , 1843–1844.Google Scholar
Edwards, T. W. D. (1993). Interpreting past climate from stable isotopes in continental organic matter. In “Climate Change in Continental Isotopic Records” (Swart, P. K. Lohmann, K. C. McKenzie, J., and Savin, S., Eds.), pp. 333–341. American Geophysical Union Monograph 78.Google Scholar
Edwards, T. W. D. Aravena, R. Fritz, P., and Morgan, A. V. (1985). Interpreting paleoclimate from 1S0 and 2H in plant cellulose: Comparison with evidence from fossil insects and relict permafrost in southwestern Ontario. Canadian Journal of Earth Sciences 22, 1720–1726.Google Scholar
Edwards, T. W. D., and Buhay, W. M. (in press). Paleoclimatic significance of oxygen and hydrogen isotope correlations in tree-rings. Palaeogeography, Palaeoclimatology, Palaeoecology. Google Scholar
Edwards, T. W. D., Buhay, W. M. Elgood, R. J., and Jiang, H. B. (1994). An improved nickel-tube pyrolysis method for oxygen isotope analysis of organic matter and water, Chemical Geology 114 , 179–183.Google Scholar
Edwards, T. W. D., and Fritz, P. (1986). Assessing meteoric water composition and relative humidity from lsO and 2H in wood cellulose: Paleoclimatic implications for southern Ontario, Canada. Applied Geochemistry 1 , 715–723.Google Scholar
Egbert, R. L. (1990). A paleoclimate classification system with U.S. western interior examples. The Mountain Geologist 27 , 99–106.Google Scholar
Eichenlaub, V. L. (1979). “Weather and Climate of the Great Lakes Region.” University of Notre Dame Press, Notre Dame, IN.Google Scholar
Epstein, S., and Krishnamurthy, R. V. (1989). Environmental information in the isotopic record in trees. Philosophical Transactions of the Royal Society of London A330, 427–439.Google Scholar
Epstein, S., and Yapp, C. J. (1976). Climatic implications of the D/H ratio of hydrogen in C-H groups in tree cellulose. Earth and Planetary Science Letters 30 , 252–261.Google Scholar
Fritz, P., and Fontes, J. Ch. (1980). Introduction. In “Handbook of Environmental Isotope Geochemistry,” (Fritz, and Fontes, J. Ch., Eds.), Vol. 1 pp. 1–19. Elsevier, New York.Google Scholar
Geiger, M. (1971). The snowbelt of southwestern Ontario. In “Waterloo County Area Selected Geographical Essays” (McLellan, A., Ed.), pp. 175. Department of Geography, University of Waterloo.Google Scholar
Green, J. W. (1963). Wood cellulose. In “Methods in Carbohydrate Chemistry” (Whistler, R. L., Ed.), pp. 9–20. Academic Press, New York.Google Scholar
Kelly, P. E. Cook, E. R., and Larson, D. W. (1994). A 1397-year tree-ring chronology of Thuja occidentalis from cliff faces of the Niagara Escarpment, southern Ontario, Canada. Canadian Journal of Forest Research 24 , 1049–1057.Google Scholar
Lahey, J. F. Bryson, R. A. Wahl, E. W., and Henderson, V. D. (1950). “Atlas of 500 mb Characteristics for the Northern Hemisphere.” University of Wisconsin Press, Madison.Google Scholar
Lamb, H. H. (1992). First essay at reconstructing the general atmospheric circulation in 1816 and the early nineteenth century. In “The Year Without a Summer” (Harrington, C. R., Ed.), pp. 355–357. Canadian Museum of Nature, Ottawa.Google Scholar
Lawrence, J. R., and White, I. W. C. (1984). Precipitation amounts during the growing season from the D/H ratios of Eastern White Pine. Nature 311 , 558–560.Google Scholar
Lipp, J. Trimbom, P. Graff, W., and Becker, B. (1993). Climatic significance of D/H ratios in the cellulose of late wood in tree-rings from spruce (L., Picea abies). In “Isotope Techniques in the Study of Past and Current Environmental Changes in the Hydrosphere and Atmosphere,” (IAEA-SM-329/ 44/0), pp. 395–406. Vienna, Austria.Google Scholar
Newell, J. P. (1992). The climate of the Labrador Sea in the spring and summer of 1816, and comparisons with modem analogues. In “The Year Without a Summer” (Harrington, C. R., Ed.), pp. 245–254. Canadian Museum of Nature, Ottawa.Google Scholar
Petterssen, P., and Calabrese, P. (1959). On some weather influences due to warming of the air by the Great Lakes in winter. Journal of Meteorology 16 , 646–652.Google Scholar
Phillips, D. W, (1988). Climate change in the Great Lakes Region. In “Proceedings of the First US-Canada Symposium on the Impacts of Climate Change in the Great Lakes Basin.” Illinois State Water Survey, Chicago, Illinois.Google Scholar
Phillips, D. W, (1990). “The Climates of Canada.” Environment Canada Government Document.Google Scholar
Quinn, F. H. (1981). Secular changes in annual and seasonal Great Lakes precipitation. Water Resources Research 17 , 1619–1624.Google Scholar
Ramesh, R. Bhattacharya, S. K., and Gopalan, K. (1986). Climatic correlations in the stable isotope records of silver fir (Abies pindrow) trees from Kashmir, India. Earth and Planetary Science Letters 79 , 66–74.Google Scholar
Richards, T. L. (1964) Meteorological aspects of ice cover on the Great Lakes. Monthly Weather Review 92 , 297–304.Google Scholar
Scott, P. A. Fayle, D. C. F., Bentley, C. V., and Hansell, R. I. C. (1988). Large-scale changes in atmospheric circulation interpreted from patterns of tree growth at Churchill, Manitoba, Canada. Arctic and Alpine Research 20 , 199–211.Google Scholar
Wilson, C. (1985). Daily weather maps for Canada, summers 1816 to 1818—A pilot study. Syllogeus 55 , 191–218.Google Scholar
Wilson, C. (1992). Climate in Canada, 1809-20: Three approaches to the Hudson’s Bay company Archives as an historical database. In “The Year Without a Summer” (Harrington, C. R., Ed.), pp. 162–184. Canadian Museum of Nature, Ottawa.Google Scholar
Yakir, D. (1992). Variations in the natural abundance of oxygen-18 and deuterium in plant carbohydrates. Plant, Cell and Environment 15 , 1005–1020.Google Scholar
Yapp, C. J., and 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, 333–350.Google Scholar
Yapp, C. J., and Epstein, S. (1982). A re-examination of cellulose carbon bound hydrogen 5D measurements and some factors affecting plant-water D/H relationships. Geochimica et Cosmockimica Acta 46 , 955–965.Google Scholar
Yapp, C. J., and Epstein, S. (1985). Seasonal contributions to the climatic variations recorded in tree ring deuterium/hydrogen data. Journal of Geophysical Research 90 , 3747–3752.Google Scholar