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14C Concentrations of Single-Year Tree Rings from About 22,000 Years Ago Obtained Using A Highly Accurate Measuring Method

Published online by Cambridge University Press:  18 July 2016

Toshiyuki Gandou
Affiliation:
Department of Physics, Yamagata University, 1-4-12 Kojirakawa, Yamagata 990-8560, Japan
Hirohisa Sakurai*
Affiliation:
Department of Physics, Yamagata University, 1-4-12 Kojirakawa, Yamagata 990-8560, Japan
Wataru Katoh
Affiliation:
Department of Physics, Yamagata University, 1-4-12 Kojirakawa, Yamagata 990-8560, Japan
Yousuke Takahashi
Affiliation:
Department of Physics, Yamagata University, 1-4-12 Kojirakawa, Yamagata 990-8560, Japan
Syuichi Gunji
Affiliation:
Department of Physics, Yamagata University, 1-4-12 Kojirakawa, Yamagata 990-8560, Japan
Fuyuki Tokanai
Affiliation:
Department of Physics, Yamagata University, 1-4-12 Kojirakawa, Yamagata 990-8560, Japan
Hiroyuki Matsuzaki
Affiliation:
Research Center for Nuclear Science and Technology, The University of Tokyo, Tokyo 113-0032, Japan
*
Corresponding author. Email: sakurai@ksprite.kj.yamagata-u.ac.jp.
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Abstract

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We have measured the radiocarbon concentrations in single-yr tree rings of old wood by accelerated mass spectrometry (AMS) using a multicathode. The 14C concentrations of 10 single-yr tree rings were measured in 100 tree rings at intervals of 10. For each single-yr tree-ring sample, typically 80 measurements of the 14C concentrations were carried out using multicathodes. The sample standard deviations indicated that there are other fluctuations of typically 1.5%, in addition to the fluctuation of the Poisson counting statistics which is typically 3% for each measurement. The average 14C date of the tree rings was 22,130 ± 306 BP for all 624 data of single-yr tree-ring samples measured by the multicathodes. From the calibration data of Lake Suigetsu, the calendar dates of these 100 tree rings were located between 25,400 cal BP and 26,150 cal BP. The 14C dates changed between 21,979 BP and 22,272 BP, with an error of approximately 50 BP, corresponding to a precision of approximately 0.5%. There was a step with a change of approximately 144 BP for each 10 yr in the time profile.

Type
Part II
Copyright
Copyright © The Arizona Board of Regents on behalf of the University of Arizona 

References

Beck, JW, Richards, DA, Edwards, RL, Silverman, BW, Smart, PL, Donahue, DL, Hererra-Osterheld, S, Burr, GS, Calsoyas, L, Jull, AJT, Biddulph, D. 2001. Extremely large variations of atmospheric 14C concentration during the Last Glacial Period. Science 292: 2453–58.Google Scholar
Beer, J. 2000a. Long-term indirect indices of solar variability. Space Science Reviews 100:115.Google Scholar
Beer, J, Mende, W, Stellmacher, R. 2000b. The role of the sun in climate forcing. Quaternary Science Reviews 19:403–15.Google Scholar
Endo, K, Sakurai, H, Sekiguchi, H, Gunji, S, Kato, A, Furusawa, S, Inui, E, Suzuki, A, Hamano, M. 2000. 14C measurement of synthesized benzene from old tree rings. IEEE Transactions on Nuclear Science 47(6):302–5.CrossRefGoogle Scholar
Guo, Z, Liu, K, Lu, X, Ma, H, Li, K, Yuan, S, Wu, X. 2000. The use of AMS radiocarbon dating for Xia-Shang-Zhou chronology. Nuclear Instruments and Methods in Physics Research B 172:724–31.CrossRefGoogle Scholar
Kitagawa, H, van der Plicht, J. 1998. Atmospheric radiocarbon calibration to 45,000 yr BP. Science 279:1187–90.Google Scholar
Kocharov, GE, Ostryakov, VM, Peristykh, AN, Vasil'ev, VA. 1995. Radiocarbon content variations and Maunder Minimum of solar activity. Solar Physics 159: 381–91.Google Scholar
Oeschger, H, Siegenthaler, U, Gugelmann, A, Schotterer, U. 1975. A box diffusion model to study the carbon dioxide exchange in nature. Tellus 27:168–92Google Scholar
Peristykh, A, Damon, PE. 1998. Modulation of atmospheric 14C concentration by the solar wind and irradiance components of the Hale and Schwabe solar cycles. Solar Physics 177:343–55.Google Scholar
Sakurai, H, Sawaki, Y, Matsumoto, T, Aoki, T, Kato, W, Gandou, T, Gunji, S, Tokanai, F. 2003. Characteristics of high-purity Teflon vial for 14C measurement in old tree rings. Nuclear Instruments and Methods in Physics Research A 505:454–7.Google Scholar
Sakurai, H, Gandou, T, Kato, W, Sawaki, Y, Matsumoto, T, Aoki, T, Matsuzaki, H, Gunji, S, Tokanai, F. Forthcoming. AMS measurement of C-14 concentration in a single-year ring of a 2500-year-old tree. Nuclear Instruments and Methods in Physics Research B. Google Scholar
Stuiver, M, Braziunas, F. 1993. Sun, ocean, climate and atmospheric 14CO2 . The Holocene 3:289305 Google Scholar
Stuiver, M, Braziunas, F. 1998. Anthropogenic and solar components of hemispheric 14C. Geophysical Research Letters 25(3):329–32.Google Scholar
Suzuki, A, Sakurai, H, Endo, K, Noma, M, Gunji, S, Inui, E, Hamano, M. 1999. Pulse-height distribution of β rays in 14C Measurement with liquid scintillation counting system Quantulus. IEEE Transactions on Nuclear Science 46(3):302–5Google Scholar
Tuniz, C, Bird, JR, Fink, D, Herzog, GF. 1998. Accelerator Mass Spectrometry. Boca Raton: CRC Press. 300 p.Google Scholar