Hostname: page-component-8448b6f56d-cfpbc Total loading time: 0 Render date: 2024-04-23T13:50:51.263Z Has data issue: false hasContentIssue false
  • English
  • Français

Marine reservoir correction for the Pacific coast of central Japan using 14C ages of marine mollusks uplifted during historical earthquakes

Published online by Cambridge University Press:  20 January 2017

Masanobu Shishikura ,
Tomoo Echigo  and
Heitaro Kaneda
Masanobu Shishikura*
Affiliation:
Active Fault Research Center, Geological Survey of Japan/AIST, SiteC7 1-1-1 Higashi, Tsukuba, 305-8567, Japan
Tomoo Echigo
Affiliation:
Department of Geography, University of Tokyo; Research Fellow of the Japan Society for the Promotion of Science, Japan
Heitaro Kaneda
Affiliation:
Active Fault Research Center, Geological Survey of Japan/AIST, SiteC7 1-1-1 Higashi, Tsukuba, 305-8567, Japan
*
⁎Corresponding author. Fax: +81 29 861 3803. E-mail address:m.shishikura@aist.go.jp (M. Shishikura).
Get access Rights & Permissions [Opens in a new window]

Abstract

In this study we utilize marine shell samples from two levels of historically uplifted sessile mollusk assemblages and raised wave-cut benches to evaluate the marine reservoir correction (ΔR) for the Pacific coast of central Japan. Elevation measurements of the uplifted marine shells indicate that the lower assemblage emerged during the 1923 Taisho Kanto earthquake (M7.9), whereas uplift of the upper assemblage is most likely but less confidently ascribed to the 1703 Genroku Kanto earthquake (M8.2). Radiocarbon dating of carefully selected samples from the upper and lower assemblages yielded very similar ΔR values of 82 ± 33 and 77 ± 32 yr, respectively. We regard the former ΔR value as a representative and more reliable value given the uncertainty in correlation of the upper assemblage with the 1703 earthquake. This result is consistent with previously reported ΔR values for the Pacific coast of south-central Japan and areas around the Sea of Japan that are influenced by warm ocean currents. Radiocarbon dating of coseismically uplifted shells can aid in estimating marine reservoir ages in the tectonically active Japan Islands.

Keywords

Pacific OceanCentral Japan14C ageMarine reservoir effectHistorical earthquakeUplifted marine shells
Type
Research Article
Information
Quaternary Research , Volume 67 , Issue 2 , March 2007 , pp. 286 - 291
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.)

Footnotes

1 Present Affiliation: Geology and Environment Geoscience Group, Geo-Research Institute.

References

Hideshima, S., Matsumoto, E., Abe, O., and Kitagawa, H. Northwest pacific marine reservoir correction estimated from annually banded coral from Ishigaki Island, southern Japan. Radiocarbon 43, (2001). 473–476.CrossRefGoogle Scholar
Hughen, K.A., Baillie, M.G.L., Bard, E., Beck, J.W., Bertrand, C.J.H., Blackwell, P.G., Buck, C.E., Burr, G.S., Cutler, K.B., Damon, P.E., Edwards, R.L., Fairbanks, R.G., Friedrich, M., Guilderson, T.P., Kromer, B., McCormac, G., Manning, S., Ramsey, C.B., Reimer, P.J., Reimer, R.W., Remmele, S., Southon, J.R., Stuiver, M., Talamo, S., Taylor, F.W., van der Plicht, J., and Weyhenmeyer, C.E. Marine04 marine radiocarbon age calibration, 0–26 cal kyr BP. Radiocarbon 46, (2004). 1059–1086.Google Scholar
Kishimoto, K., (2000). Combined Bathymetric and Topographic Mesh Data: Japan 250 m grd. GSJ Open-file, 353.Google Scholar
Konishi, K., Tanaka, T., and Sakanoue, M. Secular variation of radiocarbon concentrations in seawater: Sclerochronological approach. Gomez, E.D. Proc. Fourth Int'l. Coral Reef Symp. vol. 1, (1982). Marine Science Center, University of the Philippines, Manila. 181–185.Google Scholar
Kuzmin, Y.V., Burr, G.S., and Jull, A.J.T. Radiocarbon reservoir correction ages in the Peter the Great Gulf, Sea of Japan, and eastern coast of the Kunashir, Southern Kurile (Northwestern Pacific). Radiocarbon 43, (2001). 477–481.CrossRefGoogle Scholar
Kuzmin, Y.V., Burr, G.S., Gorbunov, S.V., and Rakov, V.A. A tale of two seas: reservoir age correction values for the Sakhalin Island (Sea of Japan and Okhotsk Sea). Reservoir Age Variability in the Marine Environment. The 10th International Conference on Accelerator Mass Spectrometry (2005). Google Scholar
Land Survey Department The change of elevation of land caused by the great earthquake of September 1st, 1923. Bulletin Earthquake Research Institute, University of Tokyo vol. 1, (1926). 65–68.Google Scholar
Miura, T., and Kajihara, T. An ecological study of the life histories of two Japanese serpulid worms, Hydroides ezoensis and Pomatoleios kraussii . First International Polychaete Conference. (1984). 338–354.Google Scholar
Miyabe, N. On the vertical earth movements in Kwanto districts. Bulletin of Earthquake Research Institute. University of Tokyo 9, (1931). 1–21.Google Scholar
Nishihata, M., Yamamuro, M., and Kayane, H. Pomatoleios kraussii (Baird) and bench as paleo sea-level indicators on the west and south coast of Miura Peninsula, central Japan (in Japanese with English abstract). Daiyonki Kenkyu (The Quaternary Research) 27, (1988). 31–38.CrossRefGoogle Scholar
Ozawa, S., Hashimoto, M., and Tada, T. Vertical crustal movements in the coastal areas of Japan estimated from tidal observations. Bull. Geogr. Surv. Inst. 43, (1997). 1–21.Google Scholar
Pollitz, F.F., Nyst, M., Nishimura, T., and Thatcher, W. Inference of postseismic deformation mechanisms of the 1923 Kanto earthquake. Journal of Geophysical Research 111, (2006). B05408 http://dx.doi.org/10.1029/2005JB003901Google Scholar
Reimer, P.J., Baillie, M.G.L., Bard, E., Bayliss, A., Beck, J.W., Bertrand, C.J.H., Blackwell, P.G., Buck, C.E., Burr, G.S., Cutler, K.B., Damon, P.E., Edwards, R.L., Fairbanks, R.G., Friedrich, M., Guilderson, T.P., Hogg, A.G., Hughen, K.A., Kromer, B., McCormac, G., Manning, S., Ramsey, C.B., Reimer, R.W., Remmele, S., Southon, J.R., Stuiver, M., Talamo, S., Taylor, F.W., van der Plicht, J., and Weyhenmeyer, C.E. IntCal04 terrestrial radiocarbon age calibration, 0–26 cal kyr BP. Radiocarbon 46, (2004). 1029–1058.Google Scholar
Stuiver, M., and Braziunas, T.F. Modeling atmospheric 14C influences and 14C ages of marine samples to 10,000 BC. Radiocarbon 35, (1993). 137–189.CrossRefGoogle Scholar
Stuiver, M., Reimer, P.J., and Braziunas, T.F. High-precision radiocarbon age calibration for terrestrial and marine samples. Radiocarbon 40, (1998). 1127–1151.CrossRefGoogle Scholar
Tanakadate, H., (1926). Vertical movement of coastal area, associated with the Kanto great earthquake (in Japanese). Chigaku Zasshi (Journal of Geography), 38, 130–135., 188–201., 324–329., 374–390.Google Scholar
Usami, T. Materials for Comprehensive List of Destructive Earthquakes in Japan, 416–2001, -latest edition- (in Japanese). (2003). University Of Tokyo Press, 605p.Google Scholar
Yamasaki, N. Physiographical studies of the great earthquake of Kwanto district, 1923 (in Japanese). Journal of Faculty Science, Imperial University of Tokyo, Sec. 2, (1926). 77–119.Google Scholar
Yoneda, M., Kitagawa, H., van der Plicht, J., Uchida, M., Tanaka, A., Uehiro, T., Shibata, Y., Morita, M., and Ohno, T. Pre-bomb marine reservoir ages in the western north Pacific: preliminary result on Kyoto University collection. Nuclear Instruments and Methods, B 172, (2000). 377–381.CrossRefGoogle Scholar
Yoneda, M., Hirota, M., Uchida, M., Uzawa, K., Tanaka, A., Shibata, Y., and Morita, M. Marine radiocarbon reservoir effect in the western North Pacific observed in archaeological fauna. Radiocarbon 43, (2001). 465–471.Google Scholar
Yoneda, M., Tanaka, A., Shibata, Y., Morita, M., Uzawa, K., Hirota, M., and Uchida, M. Radiocarbon marine reservoir effect in human remains from the Kitakogane site, Hokkaido, Japan. Journal of Archaeological Science 29, (2002). 529–536.CrossRefGoogle Scholar