Hostname: page-component-586b7cd67f-g8jcs Total loading time: 0 Render date: 2024-11-25T20:59:59.529Z Has data issue: false hasContentIssue false

A Test of “Annual Resolution” in Stalagmites Using Tree Rings

Published online by Cambridge University Press:  20 January 2017

Julio L. Betancourt*
Affiliation:
U.S. Geological Survey, Desert Laboratory, 1675 W. Anklam Road, Tucson, Arizona, 85745, E-mail: [email protected]
Henri D. Grissino-Mayer
Affiliation:
Department of Geography, The University of Tennessee, Knoxville, Tennessee, 37996
Matthew W. Salzer
Affiliation:
Laboratory of Tree-Ring Research, The University of Arizona, Tucson, Arizona, 85721
Thomas W. Swetnam
Affiliation:
Laboratory of Tree-Ring Research, The University of Arizona, Tucson, Arizona, 85721
*
1To whom correspondence should be addressed. Telephone: (520) 670-6821 ext. 109.

Abstract

So-called annual banding has been identified in a number of speleothems in which the number of bands approximates the time interval between successive U-series dates. The apparent annual resolution of speleothem records, however, remains largely untested. Here we statistically compare variations in band thickness from a late Holocene stalagmite in Carlsbad Cavern, Southern New Mexico, USA, with three independent tree-ring chronologies form the same region. We found no correspondence. Although there may be various explanations for the discordance, this limited exercise suggests that banded stalagmites should be held to the same rigorous standards in chronology building and climatic inference as annually resolved tree rings, corals, and ice cores.

Type
Short Paper
Copyright
University of Washington

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Baumgartner, T. R., Michaelsen, J., Thompson, L. G., Shen, G. T., Soutar, A., and Casey, R. E. (1989). The recording of interannual climatic change by high-resolution natural systems: Tree-rings, coral bands, glacial ice layers, and marine varves.. In Aspects of Climatic Variability in the Pacific and the Western AmericasD. H. Peterson, Ed., Am. Geophys. Union, Geophysical Monographs55, 1–15.Google Scholar
Cook, E.R. Temperature histories in tree rings and corals. Climate Dynamics 11, (1995). 211 222.CrossRefGoogle Scholar
Cook, E. R, and Kairiukstis, L. A. 1990, Methods of Dendrochronology: Applications in the Environmental Sciences, Kluwer Academic, Boston.Google Scholar
Dean, J.S. Demography, environment, and subsistence stress. Tainter, J.A., and Tainter, B.B. Evolving Complexity and Environmental Risk in the Prehistoric Southwest. (1996). Addison-Wesley, Reading. 25 56.Google Scholar
Dean, J.S., Euler, R.C., Gumerman, G.J., Plog, F., Hevly, R.H., and Karlstrom, T.N.V. Human behavior, demography, and paleoenvironment on the Colorado Plateaus. American Antiquity 50, (1985). 537 554.Google Scholar
Denniston, R.F., González, L.A., Sharma, R., and Reagan, M.K. Speleothem evidence for changes in Indian summer monsoon precipitation over the last ∼2300 years. Quaternary Research 53, (2000). 196 202.CrossRefGoogle Scholar
Dorale, J.A., Edwards, R.L., Ito, E., and González, L.A. Climate and vegetation history of the mid-continent from 75 to 25 ka: A speleothem record from Crevice Cave, Missouri, U.S.A. Science 282, (1998). 1871 1874.Google Scholar
Fritts, H.C. Reconstructing Large-Scale Climatic Patterns from Tree-Ring Data. (1991). Univ. of Arizona Press, Tucson.Google Scholar
Grissino-Mayer, H. D. (1996). A 2129-year reconstruction of precipitation for northwestern New Mexico, USA.. In Tree Rings, Environment, and HumanityJ. S. Dean, D. M. Meko, and T. W. Swetnam, Eds., Radiocarbon1996, Department of Geosciences, Univ. of Arizona, Tucson: pp. 191204.Google Scholar
Grissino-Mayer, H. D, Baisan, C. H, and Swetnam, T. W. 1997, A 1,373-Year Reconstruction of Annual Precipitation for the Southern Rio Grande Basin. Fort Bliss, TX: Unpublished Final Report to the Legacy Program, Directorate of Environment, Natural Resources Division.Google Scholar
Holmes, R.L. Computer-assisted quality control in tree-ring dating and measurement. Tree-Ring Bulletin 43, (1983). 69 78.Google Scholar
McDermott, F., Mattey, D.P., and Hawkesworth, C. Centennial-scale Holocene climate variability revealed by a high-resolution speleothem δ18O record from SW Ireland. Science 294, (2001). 1328 1330.CrossRefGoogle ScholarPubMed
Musgrove, M.L., Banner, J.L., Mack, L.E., Combs, D.M., James, E.W., Cheng, H., and Edwards, R.L. Geochronology of late Pleistocene to Holocene speleothems from central Texas: Implications for regional paleoclimates. Geological Society of America Bulletin 113, (2001). 1532 1543.Google Scholar
Polyak, V.J., and Asmerom, Y. Late Holocene climate and cultural changes in the southwestern United States. Science 294, (2001). 148 151.CrossRefGoogle ScholarPubMed
Proctor, C.J., Baker, A., Barnes, W.L., and Gilmour, M.A. A thousand-year speleothem proxy record of North Atlantic climate from Scotland. Climate Dynamics 16, (2000). 815 820.Google Scholar
Qian, W., and Shu, Y. Little Ice Age climate near Beijng, China, inferred from historical and stalagmite records. Quaternary Research 57, (2002). 109 119.Google Scholar
Salzer, M. W. 2000, Dendroclimatology in the San Francisco Peaks Region of Northern Arizona, USA. Unpublished Ph.D. dissertation, Department of Geosciences, Univ. of Arizona, Tucson.Google Scholar
Salzer, M. W. (In press), Reconstructed temperature and precipitation on a millennial timescale from tree-rings in the San Francisco Peaks area of northern Arizona, Climatic Change.Google Scholar
Wang, Y.J., Cheng, H., Edward, R.L., An, Z.S., Wu, J.Y., Schen, C.-C., and Dorale, J.A. A high-resolution absolute-dated late Pleistocene monsoon record from Hulu Cave, China. Science 294, (2001). 2245 2248.CrossRefGoogle ScholarPubMed