Hostname: page-component-586b7cd67f-gb8f7 Total loading time: 0 Render date: 2024-11-23T03:02:03.635Z Has data issue: false hasContentIssue false
  • English
  • Français

Radiocarbon Age Offset Between Shell and Plant Pairs in the Holocene Sediments Under Hakata Bay, Western Japan

Published online by Cambridge University Press:  28 April 2017

Toshimichi Nakanishi ,
Wan Hong ,
Shoichi Shimoyama ,
Shin’ichi Sato ,
Gyujun Park  and
Jong-Geol Lee
Toshimichi Nakanishi
Affiliation:
AIG Collaborative Research Institute for International Study on Eruptive History and Informatics, Fukuoka University, Nanakuma 8-19-1, Jonan-ku, Fukuoka 814-0180, Japan
Wan Hong*
Affiliation:
Geologic Environment Division, Korea Institute of Geoscience & Mineral Resources, Gajeong-dong 30, Yuseong-gu, Daejeon 305-350, Republic of Korea
Shoichi Shimoyama
Affiliation:
Institute of Lowland and Marine Research, Saga University, Honjyo 1, Saga 840-8502, Japan
Shin’ichi Sato
Affiliation:
Faculty of Science, Shizuoka University, Ohya 836, Suruga-ku, Shizuoka 422-8529, Japan
Gyujun Park
Affiliation:
Geologic Environment Division, Korea Institute of Geoscience & Mineral Resources, Gajeong-dong 30, Yuseong-gu, Daejeon 305-350, Republic of Korea
Jong-Geol Lee
Affiliation:
Geologic Environment Division, Korea Institute of Geoscience & Mineral Resources, Gajeong-dong 30, Yuseong-gu, Daejeon 305-350, Republic of Korea
*
*Corresponding author. Email: [email protected].
Get access Rights & Permissions [Opens in a new window]

Abstract

To measure chronological changes in the marine reservoir effect in western Japan, 47 marine shells and 35 terrestrial plants from the same horizons in two cores of Holocene sediments were radiocarbon dated by the KIGAM AMS facility. These cores were obtained from the central and northern parts of Hakata Bay using a Geoslicer device. This drilling tool provided us continuous coverage and many samples. In order to determine the species effects on the marine reservoir effect, both filter feeders and a deposit feeder were selected for study. Based on the analysis of lithology, mollusk assemblage, and 14C dating, two sedimentary units were determined: the upper bay floor sediment and lower estuarine sediment. Reservoir ages of 280±150 yr (n=17) and 340±140 yr (n=18) were obtained from the central and northern parts of Hakata Bay during 2000 to 10,000 cal BP, respectively. Based on these results, it is clear that a paleoenvironmental change occurred here as a result of sea-level rise during the deglacial period.

Keywords

reservoir effectbay sedimentHoloceneAMS radiocarbon datingHakata Bay
Type
14C as a Tracer of Past or Present Continental Environment
Information
Radiocarbon , Volume 59 , Special Issue 2: Proceedings of the 22nd International Radiocarbon Conference (Part 1 of 2) , April 2017 , pp. 423 - 434
Copyright
© 2017 by the Arizona Board of Regents on behalf of the University of Arizona 

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

Selected Papers from the 2015 Radiocarbon Conference, Dakar, Senegal, 16–20 November 2015

References

Haraguchi, T, Nakata, T, Shimazaki, K, Imaizumi, T, Kojima, K, Ishimaru, T. 1998. A new sampling method of unconsolidated sediments by long geo-slicer, a pile-type soil sampler. Journal of the Japan Society Engineering Geology 39:306–314. In Japanese with English abstract.Google Scholar
Hideshima, S, Matsumoto, E, Abe, O, Kitagawa, H. 2001. Northwest Pacific marine reservoir correction estimated from annually banded coral from Ishigaki Island, southwest Japan. Radiocarbon 43(2A):473–476.Google Scholar
Hong, W, Park, JH, Kim, KJ, Woo, HJ, Kim, JK, Choi, HK, Kim, GD. 2010a. Establishment of chemical preparation methods and development of an automated reduction system for AMS sample preparation at KIGAM. Radiocarbon 52(3):1277–1287.Google Scholar
Hong, W, Park, JH, Sung, KS, Woo, HJ, Kim, JK, Choi, HW, Kim, GD. 2010b. A new1MV AMS facility at KIGAM. Radiocarbon 52(2):243–251.Google Scholar
Hori, K, Saito, Y. 2007. An early Holocene sea-level jump and delta initiation. Geophysical Research Letters 34:L18401.CrossRefGoogle Scholar
Ichihara, T, Takatsuka, K, Shimoyama, S. 1996. Ichnostratigraphy’ – the use of ichnofacies in stratigraphy. Journal of the Geological Society of Japan 102:685–699. In Japanese with English abstract.Google Scholar
Jull, AJT, Burr, GS, Hodgins, GWL. 2013. Radiocarbon dating, reservoir effects, and calibration. Quaternary International 299:64–71.Google Scholar
Kong, GS, Lee, CW. 2005. The sea. Journal of the Korean Society of Oceanography 10(2):124–128. In Korean with English abstract.Google Scholar
Konishi, K, Tanaka, T, Sakanoue, M. 1982. Secular variation of radiocarbon concentration in seawater: sclerochronological approach. In: Proceedings of the Fourth International Coral Reef Symposium. Berkeley: Marine Sciences Center. p 181–185.Google Scholar
Kuzmin, YV, Burr, GS, Jull, AJT. 2001. Radiocarbon reservoir correction ages in the Peter the Great Gulf, Sea of Japan, and eastern coast of the Kunashir, Southern Kuriles (Northwestern Pacific). Radiocarbon 43(2):477–481.Google Scholar
Kuzmin, YV, Burr, GS, Gorbunov, SV, Rakov, VA, Razjigaeva, NG. 2007. A tale of two seas: Reservoir age correction values (R, ΔR) for the Sakhalin Island (Sea of Japan and Okhotsk Sea). Nuclear Instruments and Methods in Physics Research B 259(1):460–462.Google Scholar
Machida, H. 2002. Volcanoes and tephras in the Japan Area. Global Environmental Research 6(2):19–28.Google Scholar
Nakamura, T, Masuda, K, Miyake, F, Hakozaki, M, Kimura, K, Nishimoto, H, Hitoki, E. 2016. High-precision age determination of Holocene samples by radiocarbon dating with accelerator mass spectrometry at Nagoya University. Quaternary International 397:250–257.CrossRefGoogle Scholar
Nakanishi, T, Hong, W, Sung, KS, Lim, J. 2013. Radiocarbon reservoir effect from shell and plant pair in Holocene sediments around the Yeongsan River in Korea. Nuclear Instruments and Methods in Physics Research B 294:444–451.Google Scholar
Nakanishi, T, Hong, W, Sung, KS, Sung, KH, Nakashima, R. 2015. Offsets in radiocarbon ages between plants and shells from same horizons of coastal sediments in Korea. Nuclear Instruments and Methods in Physics Research B 361:670–679.Google Scholar
Nakata, T, Shimazaki, K. 1997. Geo-slicer, a newly invented soil sample, for high-resolution active fault studies. Journal of Geography 106:59–69. In Japanese with English abstract.Google Scholar
Nummedal, D, Riley, GW, Templet, PL. 1993. High-resolution sequence architecture: a chronostratigraphic model based on equilibrium profile studies. In: Posamentier HW, Summerhayes CP, Haq BU, Allen GP, editors. Sequence Stratigraphy and Facies Associations Volume 18. Ghent: International Association of Sedimentologists Special Publication. p 55–68.CrossRefGoogle Scholar
Okutani, T. 2000. Marine Mollusks in Japan. Tokai: Tokai University Press. 1173 p.Google Scholar
Philippsen, B, Olsen, J, Lewis, JP, Rasmussen, P, Ryves, DB, Knudsen, KL. 2013. Mid- to late-Holocene reservoir-age variability and isotope-based palaeoenvironmental reconstruction in the Limfjord, Denmark. The Holocene 23(7):1017–1027.Google Scholar
Reimer, PJ, Bard, E, Bayliss, A, Beck, JW, Blackwell, PG, Bronk Ramsey, C, Buck, CE, Cheng, H, Edwards, RL, Friedrich, M, Grootes, PM, Guilderson, TP, Haflidason, H, Hajdas, I, Hatté, C, Heaton, TJ, Hoffmann, DL, Hogg, AG, Hughen, KA, Kaiser, KF, Kromer, B, Manning, SW, Niu, M, Reimer, RW, Richards, DA, Scott, EM, Southon, JR, Staff, RA, Turney, CSM, van der Plicht, J. 2013. IntCal13 and Marine13 radiocarbon age calibration curves 0–50,000 years cal BP. Radiocarbon 55(4):1869–1887.Google Scholar
Shimoyama, S, Iso, N, Kuroki, T, Okamura, M. 2014. Investigation for the fault activity and paleoseismology of active faults in and around the Hakata Bay. Report on Evaluation of Earthquake of Kego Fault Zone (Southeastern Area). Tokyo: Headquarters for Earthquake Research Promotion. p 241–87. In Japanese.Google Scholar
Shishikura, M, Echigo, T, Kaneda, H. 2007. Marine reservoir correction for the Pacific coast of central Japan using 14C ages of marine mollusks uplifted during historical earthquakes. Quaternary Research 67(2):286–291.Google Scholar
Smith, VC, Staff, RA, Blockley, SPE, Bronk Ramsey, C, Nakagawa, T, Mark, DF, Takemura, K, Danhara, T, Suigetsu Project Members. 2013. Identification and correlation of visible tephras in the Lake Suigetsu SG06 sedimentary archive, Japan: chronostratigraphic markers for synchronizing of east Asian/west Pacific palaeoclimatic records across the last 150 ka. Quaternary Science Reviews 67:121–137.Google Scholar
Southon, J, Kashgarian, M, Fontugne, M, Metivier, B, Yim, WWS. 2002. Marine reservoir corrections for the. Indian Ocean and southeast Asia. Radiocarbon 44(1):167–180.Google Scholar
Stuiver, M, Reimer, PJ. 1993. Extended 14C data base and revised CALIB 3.0 14C age calibration program. Radiocarbon 35(1):215–230.Google Scholar
Stuiver, M, Pearson, GW, Braziunas, T. 1986. Radiocarbon age calibration of marine samples back to 9000 cal yr BP. Radiocarbon 28(2B):980–1021.Google Scholar
Yokoyama, Y, Nakada, M, Maeda, Y, Nagaoka, S, Okuno, J, Matsumoto, E, Sato, H, Matsushima, Y. 1996. Holocene sea-level change and hydro-isostasy along the west coast of Kyushu, Japan. Paleogeography, Paleoclimatology, Paleoecology 123(1–4):29–47.Google Scholar
Yoneda, M, Uno, H, Shibata, Y, Suzuki, R, Kumamoto, Y, Yoshida, K, Sasaki, T, Suzuki, A, Kawahata, H. 2007. Radiocarbon marine reservoir ages in the western Pacific estimated by pre-bomb molluscan shells. Nuclear Instruments and Methods in Physics Research B 259(1):432–437.Google Scholar