An Advancement in Removing Extraneous Color From Wood for Low-Magnification Reflected-Light Image Analysis of Conifer Tree Rings

Authors

  • Paul R. Sheppard
  • Alex Wiedenhoeft

Keywords:

Wood color, dendrochronology, image analysis, summer precipitation, New Mexico

Abstract

This paper describes the removal of extraneous color from increment cores of conifers prior to reflected-light image analysis of tree rings. Ponderosa pine in central New Mexico was chosen for study. Peroxide bleaching was used as a pretreatment to remove extraneous color and still yield usable wood for image analysis. The cores were bleached in 3% peroxide raised to pH 12 and heated to 60° C, and then they were soaked in 95% ethanol and rinsed in water. The cores were dried slowly to avoid checking or cracking. This treatment removed heartwood color while leaving the wood reasonably sound. Wood reflectance and latewood width were measured using reflected-light image analysis. For dendroclimatic modeling, best-subsets regression was used to determine the strongest predictive model, which was May-September rainfall using latewood reflectance and latewood width. The ability to dendroclimatically model and reconstruct summer precipitation is contingent on having latewood reflectance (density) measurements, and reconstructing summer precipitation in the Southwest will enhance paleoclimatology of the region. Image analysis with reflected white light is thus closer to being more widely applicable in dendrochronology.

References

Adams, D. K., and A. C. Comrie. 1997. The North American monsoon. Bull. Am. Meteorol. Soc.78(10):2197-2213.nAndrews, D. H., and R. P. Singh. 1979. Peroxide bleaching. Pages 211-253 in R. P. Singh, ed. The bleaching of pulp, 3rd ed., revised. TAPPI Press, Atlanta, GA.nBerg, W. K., D. M. Anderson, and J. J. Bates. 2000. Satellite observations of a Pacific moisture surge associated with flooding in Las Vegas. Geophys. Res. Lett.27(16): 2553-2556.nBlasing, T. J., D. N. Duvick, and D. C. West. 1981. Dendroclimatic calibration and verification using regionally averaged and single station precipitation data. Tree-Ring Bull.41:37-43.nBlasing, T. J., A. M. Solomon, and D. N. Duvick. 1984. Response functions revisited. Tree-Ring Bull.44:1-15.nBowyer, J. L., R. Shmulsky, and J. G. Haygreen. 2003. Forest products and wood science: An introduction, 4th ed. Iowa State Press, Ames, IA. 554 pp.nBradfield, M. 1971. The changing pattern of Hopi agriculture. Occasional Paper Number 30. Royal Anthropological Institute of Great Britain and Ireland, London, UK. 66 pp.nBriffa, K. R., P. D. Jones, and F. H. Schweingruber. 1988. Summer temperature patterns over Europe: A reconstruction from 1750 A.D. based on maximum latewood density indices of conifers. Quat. Res.30:36-52.nBurns, R. M., and B. H. Honkala, tech. coords. 1990. Silvics of North America, volume 1, Conifers. USDA Forest Service Agriculture Handbook 654, Washington, DC.nCleaveland, M. K. 1986. Climatic response of densitometric properties in semiarid site tree rings. Tree-Ring Bull.46:13-29.nConkey, L. E. 1988. Decline in old-growth red spruce in western Maine: An analysis of wood density and climate. Can. J. For. Res.18(8):1063-1068.nCook, E. R., and K. Peters. 1981. The smoothing spline: A new approach to standardizing forest interior tree-ring width series for dendroclimatic studies. Tree-Ring Bull.41:45-53.nCox, J. R. 1988. Seasonal burning and mowing impacts on Sporobolus wrightii grasslands. J. Range Manag.41(1):12-15.nD'Arrigo, R. D., and G. C. Jacoby. 1991. A 1000-year record of winter precipitation from northwestern New Mexico, USA: A reconstruction from tree-rings and its relation to El Niño and the Southern Oscillation. Holocene1(2):95-101.nDouglass, A. E. 1920. Evidence of climatic effects in the annual rings of trees. Ecology1(1):24-32.nDouglass, A. E. 1941. Crossdating in dendrochronology. J. For.39(10):825-831.nDraper, N., and H. Smith. 1981. Applied regression analysis, 2nd ed. Wiley, New York, NY. 709 pp.nEakin, H., and J. Conley. 2002. Climate variability and the vulnerability of ranching in southeastern Arizona: A pilot study. Clim. Res.21(3):271-281.nFritts, H. C. 1976. Tree rings and climate. Academic Press, New York, NY. 567 pp.nFritts, H. C., J. E. Mosimann, and C. P. Bottorff. 1969. A revised computer program for standardizing tree-ring series. Tree-Ring Bull.29(1-2):15-20.nGrissino-Mayer, H. D. 1993. An updated list of species used in tree-ring research. Tree-Ring Bull.53:17-43.nGrissino-Mayer, H. D. 1996. A 2129-year reconstruction of precipitation for northwestern New Mexico, USA. Pages 191-204 in J. S. Dean, D. M. Meko, and T. W. Swetnam, eds. Tree rings, environment, and humanity. Radiocarbon, Tucson, AZ.nJ. S. Dean. 2001. Evaluating crossdating accuracy: A manual and tutorial for the computer program COFECHA. Tree-Ring Res.57(2):205-221.nJ. S. Dean., and H. C. Fritts. 1997. The International Tree-Ring Data Bank: An enhanced global database serving the global scientific community. Holocene7(2):235-238.nJ. S. Dean., and T. W. Swetnam. 2000. Century-scale climate forcing of fire regimes in the American Southwest. Holocene10(2):213-220.nJ. S. Dean., T. W. Swetnam., and R. K. Adams. 1997. The rare old-aged conifers of El Malpais-their role in understanding climatic change in the American Southwest. Pages 155-161 in K. Mabery, ed. Natural history of El Malpais National Monument. New Mexico Bureau of Mines and Mineral Resources Bulletin 156, Albuquerque, NM.nHaston, L., and J. Michaelsen. 1994. Long-term central coastal California precipitation variability and relationships to El Niño-Southern Oscillation. J. Clim.7(9): 1373-1387.nHidalgo, H. C., J. A. Dracup, G. M. MacDonald, and J. A. King. 2001. Comparison of tree species sensitivity to high and low extreme hydroclimatic events. Phys. Geogr.22(2):115-134.nHolmes, R. L. 1983. Computer-assisted quality control in tree-ring dating and measurement. Tree-Ring Bull.43: 69-78.nHughes, M. K., X. Wu, X. Shao, and G. M. Garfin. 1994. A preliminary reconstruction of rainfall in north-central China since A.D. 1600 from tree-ring density and width. Quat. Res.42(1):88-99.nJacoby, G. C., I. S. Ivanciu, and L. D. Ulan. 1988. A 263-year record of summer temperature for northern Quebec reconstructed from tree-ring data and evidence of a major climatic shift in the early 1800's. Palaeogeogr. Palaeoclim. Palaeoecol.64(1-2):69-78.nJagels, R., and F. W. Telewski. 1990. Computer-aided image analysis of tree rings. Pages 76-93 in E. R. Cook and L. A. Kairiukstis, eds. Methods of dendrochronology: Applications in the environmental sciences. International Institute for Applied Systems Analysis, Kluwer Academic Publishers, Boston, MA.nJurwitz, L. R. 1953. Arizona's two-season rainfall pattern. Weatherwise6:96-99.nLaanterä, M., J. J. Lindberg, A. Sneck, and K. Soljamo. 1993. Degradation of the polymer structure of wood by wetting and drying. Viscoelasticity and morphology of the composite cell structure. J. Macromolec. Sci. Pure Appl. Chem.A30(9-10):715-726.nLiverman, D. 1999. Climate change and the borderlands: An introduction and assessment. Borderlines7:1-4.nMantanis, G. I., R. A. Young, and R. M. Rowell. 1994a. Swelling of wood: Part 1. Swelling in water. Wood Sci. Technol.28(2):119-134.nMantanis, G. I., R. A. Young, and R. M. Rowell. 1994b. Swelling of wood: Part 2. Swelling in organic liquids. Holzforschung48(6): 480-490.nMcCarroll, D., E. Pettigrew, A. Luckman, F. Guibal, and J. L. Edouard. 2002. Blue reflectance provides a surrogate for latewood density of high-latitude tree rings. Arct. Antarct. Alpine Res.34(4):450-453.nMcMillin, C. W. 1982. Application of automatic imageanalysis to wood science. Wood Sci.14(3):97-105.nMeko, D. M., and C. H. Baisan. 2001. Pilot study of late wood-width of conifers as an indicator of variability of summer rainfall in the North American monsoon. Internat. J. Climatol.21(6):697-708.nMerideth, R. W. 2001. A primer on climatic variability and change in the Southwest. Institute for the Study of Planet Earth, University of Arizona, Tucson, AZ. 28 pp.nMichaelsen, J. 1987. Cross-validation in statistical climate models. J. Clim. Appl. Meteorol.26(11):1589-1600.nNi, F. B., T. Cavazos, M. K. Hughes, A. C. Comrie, and G. Funkhouser. 2002. Cool-season precipitation in the southwestern USA since AD 1000: Comparison of linear and nonlinear techniques for reconstruction. Internat. J. Climatol.22(13):1645-1662.nOstrom, C. W. 1990. Time series analysis regression techniques. Sage Publications, Newbury Park, CA. 85 pp.nParker, M. L., and W. E. S. Henoch. 1971. The use of Engelmann spruce latewood density for dendrochronological purposes. Can. J. For. Res.1(2):90-98.nPhipps, R. L. 1985. Collecting, preparing, crossdating, and measuring tree increment cores. US Geological Survey Water Resources Investigations Report 85-4148. 48 pp.nRigling, A., P. O. Waldner, T. Forster, O. U. Bräker, and A. Pouttu. 2001. Ecological interpretation of tree-ring width and intra-annual density fluctuations in Pinus sylvestris on dry sites in the central Alps and Siberia. Can. J. For. Res.31(1):18-31.nRobinson, W. J., and R. Evans. 1980. A microcomputerbased tree-ring measuring system. Tree-Ring Bull.40: 59-64.nRowell, R. M., R. Pettersen, J. S. Han, J. S. Rowell, and M. Tshabalala. 2005. Cell wall chemistry. Pages 35-74 in R. Rowell, ed. Handbook of wood chemistry and wood composites. CRC Press, Boca Raton, FL.nSchulman, E. 1956. Dendroclimatic changes in semiarid America. University of Arizona Press, Tucson, AZ. 142 pp.nSheppard, P. R. 1999. Overcoming extraneous wood color variation during low-magnification reflected-light image analysis of conifer tree rings. Wood Fiber Sci.31(2): 106-115.nSheppard, P. R., and L. O. White. 1995. Tree-ring responses to the 1978 earthquake at Stephens Pass, northeastern California. Geology23(2):109-112.nSheppard, P. R., and L. J. Graumlich. 1996. A reflected-light video imaging system for tree-ring analysis of conifers. Pages 879-889 in J. S. Dean, D. M. Meko, and T. W. Swetnam, eds. Tree rings, environment, and humanity. Radiocarbon, Tucson, AZ.nSheppard, P. R., and S. Y. Singavarapu. 2006. Solving the "magnification irony" in reflected-light image analysis of conifer tree rings using a microscope. J. Imag. Sci. Tech.50(3):304-308.nSheppard, P. R., L. J. Graumlich, and L. E. Conkey. 1996. Reflected-light image analysis of conifer rings for reconstructing climate. Holocene6(1):62-68.nSheppard, P. R., A. C. Comrie, K. Angersbach, G. D. Packin, and M. K. Hughes. 2002. The climate of the US Southwest. Clim. Res.21(3):239-258.nSokal R. R., and F. J. Rohlf. 1981. Biometry. WH Freeman and Co., San Francisco, CA. 859 pp.nSwetnam, T. W., M. A. Thompson, and E. K. Sutherland. 1985. Using dendrochronology to measure radial growth of defoliated trees. USDA Forest Service Agricultural Handbook 639. 39 pp.nTelewski, F. W., and G. C. Jacoby. 1987. Current status of x-ray densitometry. Pages 630-646 in G. C. Jacoby, and J. W. Hornbeck, comps. Proc. International Symposium on Ecological Aspects of Tree-ring Analysis. US Department of Energy, Publication CONF-8608144, Washington, DC.nUSFS. 1983. Black stain root disease. US Forest Service Forest Disease Management Notes 84, Portland, OR. 1 p.nUSFS FPL. 1966. Difference between heartwood and sapwood. United States Forest Service Forest Products Laboratory Research Note FPL-147, Madison, WI. 2 pp.nWilks, D. S. 1997. Resampling hypothesis tests for autocorrelated fields. J. Clim.10(1):65-82.nWright, H. A., and A. W. Bailey. 1982. Fire ecology: United States and southern Canada. John Wiley and Sons, New York, NY. 501 pp.nYamaguchi, D. K., and F. C. Brunstein. 1991. Special sanding films and sandpapers for surfacing narrow-ring increment cores. Tree-Ring Bull.51:43-46.n

Downloads

Published

2007-06-05

Issue

Section

Research Contributions