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Surface-Exposure Chronology Using in Situ Cosmogenic 3He in Antarctic Quartz Sandstone Boulders

Published online by Cambridge University Press:  20 January 2017

Abstract

In situ-produced cosmogenic helium (3Hec) provides a new tool for constraining histories of Quaternary geomorphic surfaces. Before general application of the technique, however, the systematics and production rates of 3Hec must be well understood. In a companion study, 3He and 10Be data from sandstone and granite boulders in the Dry Valleys region of Antarctica have been used to constrain the ages of an important moraine sequence formed by the Taylor Glacier. Data from these deposits also provide information about the systematics of 3He in quartz that has important implications for geochronology based on 3Hec. In contrast to previous results from olivine and clinopyroxene, crushing quartz in vacuo releases helium with high 3He/4He ratios (up to 148 × Ra, where Ra is the atmospheric 3He/4He ratio), indicating that crushing cannot be used to determine the isotopic composition of trapped (i.e., noncosmogenic) helium in quartz. Analysis of 3He in different size fractions of the same samples indicates significant 3 He loss not predicted by existing 3He diffusion data for quartz. The origin of the discrepancy is not clear, but loss from these samples is not as significant as suggested by the limited data of previous studies.

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Articles
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University of Washington

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References

Andrews, J. N. (1985). The isotopic composition of radiogenic helium and its use to study groundwater movement in confined aquifers. Chemical Geology 49, 339351.Google Scholar
Bard, E. Hamelin, B. Fairbanks, R. G., and Zindler, A. (1990). Calibration of the 14-C timescale over the past 30,000 years using mass-spectrometric U-Th ages from Barbados corals. Nature 345, 405410.Google Scholar
Bierman, P., and Gillespie, A. (1991). Range fires: A significant factor in exposure-age determination and geomorphic surface evaluation. Geology 19, 641644.Google Scholar
Bockheim, J. G. (1982). Properties of a chronosequence of ultraxerous soils in the Trans-Antarctic Mountains. Geoderma 28, 239255.CrossRefGoogle Scholar
Bogard, D. D., and Cressy, P. J. (1973). Spallation production of 3-He, 21-Ne, 38-Ar from target elements in the Bruderheim chondrite. Geochimica et Cosmochimica Acta 37, 527546.CrossRefGoogle Scholar
Brook, E. J. Kurz, M. D. Denton, G. H., and Ackert, R. P. Jr. (1993). Chronology of Taylor Glacier advances in Arena Valley, Antarctica, using in situ cosmogenic 3He and 10Be. Quaternary Research 39, 1123.CrossRefGoogle Scholar
Brown, E. Edmond, J, M. Raisbeck, G. M. Yiou, F. Kurz, M., and Brook, E. J. (1991). Examination of surface exposure ages of Antarctic moraines using in situ produced 10-Be and 26-A1. Geochimica et Cosmochimica Acta 55(8), 22692284.CrossRefGoogle Scholar
Caruso, L., and Simmons, G. (1985). Uranium and microcracks in a 1,000-meter core, Redstone, New Hampshire. Contributions to Mineralogy and Petrology 90, 117.Google Scholar
Cerling, T. E. (1990). Dating geomorphological surfaces using cos-mogenic 3He. Quaternary Research 33, 148156.Google Scholar
Craig, H., and Poreda, R. J. (1986). Cosmogenic 3He in terrestrial rocks: The summit lavas of Maui. Proceedings of the National Academy of Science 83, 19701974.Google Scholar
Denton, G. H. Bockheim, J. G. Wilson, S. C., and Stuiver, M. (1989). Late Wisconsin and early Holocene glacial history, inner Ross Em-bayment, Antarctica. Quaternary Research 31, 151182.CrossRefGoogle Scholar
Dorn, R. Turrin, B. D. Jull, A. J. T. Linick, T. W., and Donahue, D. J, (1987). Radiocarbon and cation ratio ages from rock varnish on Tioga and Tahoe moraine boulders of Pine Creek, Eastern Sierra Nevada, California, and the paleoclimatic implications. Quaternary Research 28, 3849.Google Scholar
Emery, K. O. (1944). Brush fires and exfoliation. American Journal of Science 242, 506508.Google Scholar
Eugster, O. (1988). Cosmic-ray production rates for 3He, 21Ne, 38Ar, 83Kx, and 126Xe in chondrites based on 81Kr-Kr exposure ages. Geochimica et Cosmochimica Acta 52(6), 16491662.Google Scholar
Friedman, I. E., and Weed, R. (1987). Microbial trace fossil formation, biogenous, and abiotic weathering in the Antarctic cold desert. Science 236, 703705.CrossRefGoogle Scholar
Giletti, B. J., and Kulp, J. L. (1955). Radon leakage from radioactive minerals. American Mineralogist 40, 481496.Google Scholar
Graf, T. Kohl, C. P. Marti, K., and Nishiizumi, K. (1991). Cosmic-ray produced neon in Antarctic rocks. Geophysical Research Letters 18(2), 203206.Google Scholar
Kurz, M. D. (1986a). Cosmogenic helium in a terrestrial igneous rock. Nature 320(6061), 435439.Google Scholar
Kurz, M. D. (1986b). In situ production of terrestrial cosmogenic helium and some applications to geochronology. Geochimica et Cosmochimica Acta 50, 28552862.Google Scholar
Kurz, M. D. (1987). Erratum: Correction to Kurz (1986b). Geochimica et Cosmochimica Acta 51, 1019.Google Scholar
Kurz, M. D. Colodner, D. Trull, T. W. Moore, R. B., and O’Brien, K. (1990). Cosmic ray exposure dating with in situ produced cosmogenic 3He: Results from young lava flows. Earth and Planetary Science Letters 97, 177189.Google Scholar
Kurz, M. D. Gurney, J. J. Jenkins, W. J., and Lott, D. E. (1987). Helium isotope variability within single diamonds from the Orapa kim-berlite pipe. Earth and Planetary Science Letters 6, 5768.Google Scholar
Kurz, M. D. Brook, E. J., and Ackert, R. P. Surface exposure dating of Antarctic glacial deposits. Antarctic Journal of the United States, in press.Google Scholar
Lal, D. (1987). Production of 3He in terrestrial rocks. Chemical Geology (Isotope Geoscience Section) 66, 8998.Google Scholar
Lal, D. (1991). Cosmic ray labeling of erosion surfaces: In situ nuclide production rates and erosion models. Earth and Planetary Science Letters 104, 424439.Google Scholar
Lal, D., and Peters, B. (1967). Cosmic ray produced radioactivity on the earth. In “Handbuch der Physic,” pp. 551612. Springer-Verlag, New York.Google Scholar
Light, E. S. Merker, M. Verschell, H. J. Mendell, R. B., and Korff, S. A. (1973). Time dependent worldwide distribution of atmospheric neutrons and of their products. Journal of Geophysical Research 78(16), 27412762.CrossRefGoogle Scholar
Lingenfelter, R. E. (1963). Production of carbon-14 by cosmic ray neutrons. Reviews of Geophysics 1(1), 3555.Google Scholar
Mabuchi, H. Y. Gensho, Y. Wada, Y., and Hamaguchi, H. (1971). Phosphorous-32 induced by cosmic rays in laboratory chemicals. Geochemical Journal 4, 105110.Google Scholar
Mamyrin, B. A., and Tolstikhin, I. N. (1984). “Helium Isotopes in Nature.” Elsevier, New York.Google Scholar
Marchant, D. (1990). “Surficial Geology and Stratigraphy in Arena Valley, Antarctica: Implications for Antarctic Tertiary Glacial History.” Unpublished MS dissertation, University of Maine at Orono.Google Scholar
Matz, D. M. Pinet, P. R., and Hayes, M. O. (1972). Stratigraphy and petrology of the Beacon Supergroup, Southern Victoria Land. In “Antarctica Geology and Geophysics” (Adie, R. J., Ed.), pp. 353358. Universitetsforlaget, Oslo.Google Scholar
McElroy, and Rose, (1987). “Geology of the Beacon Heights Area: Southern Victoria Land, Antarctica.” New Zealand Geological Sur-vey Miscellaneous Series Map 15. DSIR, Wellington, New Zealand.Google Scholar
McKay, C. P., and Friedman, E. I. (1985). The cryptoendolithic microbial environment in the Antarctic cold desert: Temperature variations in nature. Polar Biology 4, 1925.Google Scholar
Merker, M. Light, E. S. Verschell, H. J. Mendell, R. B., and Korff, S. A. (1973). Time dependent worldwide distribution of atmospheric neutrons and their products. 1. Fast neutron observations. Journal of Geophysical Research 78(16), 27272740.Google Scholar
Morrison, P., and Pine, J. (1955). Radiogenic origin of the helium isotopes in rocks. Annals of the New York Academy of Sciences 62, 7192.Google Scholar
Nishiizumi, K. Klein, J. Middleton, R., and Craig, H. (1990). Cos-mogenic 10-Be, 26-A1, and 3-He in olivine from Maui lavas. Earth and Planetary Science Letters 98, 263266.Google Scholar
Nishiizumi, K. Winterer, E. L. Kohl, C. P. Klein, J. Middleton, R. Lal, D., and Arnold, J. R. (1989). Cosmic ray production rates of 10Be and 26 Al in quartz from glacially polished rocks. Journal of Geophysical Research 94(B12), 1790717915.Google Scholar
Pomerantz, M. A., and Agarwal, S. P. (1962). Spatial distribution of cosmic ray intensity and geomagnetic theory. Philosophical Magazine!, 15031511.Google Scholar
Rose, D. C Fenton, K. B. Katzman, J., and Simpson, J. A. (1956). Latitude effect of the cosmic ray nucleon and meson components at sea level from the arctic to the antarctic. Canadian Journal of Physics 34, 968984.Google Scholar
Staudacher, T., and Allegre, C. J. (1991). Cosmogenic neon in ultrama-fic nodules from Asia and in quartzite from Antarctica. Earth and Planetary Science Letters 106, 87102.Google Scholar
Tarling, D. H. (1983). “Paleomagnetism: Principles and applications in geology, geophysics, and archaeology.” Chapman and Hall, New York.Google Scholar
Trull, T. W. Kurz, M. D., and Jenkins, W. J. (1991). Diffusion of cosmogenic 3-He in olivine and quartz: Implications for surface exposure dating. Earth and Planetary Science Letters 103, 241256.CrossRefGoogle Scholar
Wetherill, G. W. (1954). Variations in the isotopic abundances of neon and argon extracted from radioactive minerals. Physical Review 96(1), 679683.Google Scholar
Yokoyama, Y. Reyss, J., and Guichard, F. (1977). Production of radionuclides by cosmic rays at mountain altitudes. Earth and Planetary Science Letters 36, 4456.CrossRefGoogle Scholar