JIA Jianjun, YANG Yang, CAI Tinglu, GAO Jianhua, XIA Xiaoming, LI Yan, GAO Shu. On the sediment age estimated by 210Pb dating: probably misleading “prolonging” and multiple-factor-caused “loss”[J]. Acta Oceanologica Sinica, 2018, 37(6): 30-39. doi: 10.1007/s13131-018-1214-4
Citation: JIA Jianjun, YANG Yang, CAI Tinglu, GAO Jianhua, XIA Xiaoming, LI Yan, GAO Shu. On the sediment age estimated by 210Pb dating: probably misleading “prolonging” and multiple-factor-caused “loss”[J]. Acta Oceanologica Sinica, 2018, 37(6): 30-39. doi: 10.1007/s13131-018-1214-4

On the sediment age estimated by 210Pb dating: probably misleading “prolonging” and multiple-factor-caused “loss”

doi: 10.1007/s13131-018-1214-4
  • Received Date: 2018-01-05
  • Rev Recd Date: 2018-02-09
  • The radionuclide 210Pb is suitable for century-scale dating and has been used to calculate the sedimentation rate in a variety of environments. However, two common ways to apply 210Pb dating techniques may give misleading results. One is "prolonging of age", i.e., using the calculated sedimentation rate to date back to 200 or 300 years. This practice must be treated with caution because the 210Pb dating techniques do not guarantee direct dating for ages much older than 100 years. Another is "loss of age", i.e., the calculated time span between the topmost layer and the 210Pb background layer in cores is less than 100 years when an apparent sedimentation rate is used in the calculation. Here, we propose that based on the principle of 210Pb dating, the upper limit of age suitable for direct 210Pb dating is between 110 and 155 years. The "prolonging" application is acceptable only if the sedimentary environment in the past several hundred years was stable and the sedimentation rate was generally constant, and verification with independent evidence (such as historical records or biomarker methodology) is needed. Furthermore, after analyzing many published and collected data, we found four possible reasons for the "loss of age". First, the compaction effect of sediment should be corrected in laboratory analysis or else the calculated age will be underestimated. Second, the accuracy and uncertainty of 210Pb activity measurement affect the judgment of the background. To be cautious, researchers are apt to choose a background activity with a younger age. Third, use of a slightly smaller value of supported 210Pb activity in a calculation will lead to considerable underestimation of the time span. Finally, later-stage erosion and migration are common for sedimentation, which lead to loss of sedimentary records and are often reflected as a "loss of age" in cores. We believe that proper use of 210Pb dating data may provide helpful information on our understanding of sediment records and recent environmental changes.
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  • Alexander C R, Demaster D J, Nittrouer C A. 1991. Sediment accumulation in a modern epicontinental-shelf setting:the Yellow Sea. Marine Geology, 98(1):51-72
    Appleby P G, Oldfield F, Thompson R, et al. 1979. 210Pb dating of annually laminated lake sediments from Finland. Nature, 280(5717):53-55
    Appleby P G, Oldfield F. 1978. The calculation of lead-210 dates assuming a constant rate of supply of unsupported 210Pb to the sediment. Catena, 5(1):1-8
    Appleby P G, Oldfieldz F. 1983. The assessment of 210Pb data from sites with varying sediment accumulation rates. Hydrobiologia, 103(1):29-35
    BETA (Beta Analytic Radiocarbon Dating). 2017. Calibration of Carbon 14 Dating Results. https://www.radiocarbon.com/calendar-calibration-carbon-dating.htm[2014-05-15/2017-12-20]
    Binford M W. 1990. Calculation and uncertainty analysis of 210Pb dates for PIRLA project lake sediment cores. Journal of Paleolimnology, 3(3):253-267
    Cai Chonggui. 2005. A proof of the secular equilibrium formula in radioactive cascade decay series. College Physics (in Chinese), 24(8):44-46
    Chen Fei, Yin Liangliang, Kong Xiangyin, et al. 2016. Uncertainty evaluation of strontium-90 analysis in biological samples. Journal of Radiation Research and Radiation Processing (in Chinese), 34(1):59-64
    Chen Zhongyuan, Saito Y, Kanai Y, et al. 2004. Low concentration of heavy metals in the Yangtze estuarine sediments, China:a diluting setting. Estuarine, Coastal and Shelf Science, 60(1):91-100
    CNS (China National Standard). 1996. Analytical method for radionuclides by alpha spectrometry (GB/T 16141–1995). http://www.nhfpc.gov.cn/ewebeditor/uploadfile/2014/10/20141030160815598.pdf[2014-10-30/2017-12-20]
    Dai Zeheng. 1992. Comprehensive Survey Report on the Coastal Zone and Coastal Resources in Zhejiang Province (in Chinese). Beijing:China Ocean Press, 121-130
    Demaster D J, Mckee B A, Nittrouer C A, et al. 1985. Rates of sediment accumulation and particle reworking based on radiochemical measurements from continental shelf deposits in the East China Sea. Continental Shelf Research, 4(1-2):143-158
    Donnelly J P, Bryant S S, Butler J, et al. 2001. A 700 yr sedimentary record of intense hurricane landfalls in southern New England. GSA Bulletin, 113(6):714-727
    Eilers J M, Kann J, Cornett J, et al. 2004. Paleolimnological evidence of change in a shallow, hypereutrophic lake:Upper Klamath Lake, Oregon, USA. Hydrobiologia, 520(1-3):7-18
    Fan Dejiang, Yang Zuosheng, Guo Zhigang. 2000. Review of 210Pb dating in the continental shelf of China. Advance in Earth Sciences (in Chinese), 15(3):297-302
    Flemming B W, Delafontaine M T. 2000. Mass physical properties of muddy intertidal sediments:some applications, misapplications and non-applications. Continental Shelf Research, 20(10-11):1179-1197
    Gao Jianhua, Jia Jianjun, Sheng Hui, et al. 2017. Variations in the transport, distribution, and budget of 210Pb in sediment over the estuarine and inner shelf areas of the East China Sea due to Changjiang catchment changes. Journal of Geophysical Research:Earth Surface, 122(1):235-247
    Gao S, Collins M B. 2014. Holocene sedimentary systems on continental shelves. Marine Geology, 352:268-294
    Goldberg E D. 1963. Geochronology with 210Pb. In:Radioactive Dating, Proceedings of the Symposium on Radioactive Dating Held by the International Atomic Energy Agency in Co-operation with the Joint Commission on Applied Radioactivity. Athens:International Atomic Energy Agency, 121-131
    Hall R I, Leavitt P R, Quinlan R, et al. 1999. Effects of agriculture, urbanization, and climate on water quality in the northern Great Plains. Limnology and Oceanography, 44(3 Part 2):739-756
    Jia Jianjun, Gao Jianhua, Liu Yifei, et al. 2012. Environmental changes in Shamei Lagoon, Hainan Island, China:Interactions between natural processes and human activities. Journal of Asian Earth Sciences, 52:158-168
    Jin Xianglong. 1992. Submarine Geology of East China Sea. Beijing:China Ocean Press (in Chinese), 524
    Koide M, Soutar A, Goldberg E D. 1972. Marine geochronology with 210Pb. Earth and Planetary Science Letters, 14:442-446
    Li Fengye, Shi Yulan, Shen Shunxi, et al. 1996. Isotopic record of modern sedimentary environment in the South Yellow Sea. Oceanologia et Limnologia Sinica (in Chinese), 27(6):584-589
    Li Jun, Hu Bangqi, Dou Yanguang, et al. 2012. Modern sedimentation rate, budget and supply of the muddy deposits in the East China Seas. Geological Review (in Chinese), 58(4):745-756
    Liu Guangshan. 2010. Isotopic Oceanography (in Chinese). Zhengzhou:Zhengzhou University Press, 1-9
    Liu Shengfa, Shi Xuefa, Liu Yanguang, et al. 2009. Sedimentation rate of mud area in the East China Sea inner continental shelf. Marine Geology & Quaternary Geology (in Chinese), 29(6):1-6
    Nittrouer C A, Sternberg R W, Carpenter R, et al. 1979. The use of 210Pb geochronology as a sedimentological tool:application to the Washington continental shelf. Marine Geology, 31:296-316
    Oldfield F, Appleby P G, Battarbee R W. 1978. Alternative 210Pb dating:results from the New Guinea Highlands and Lough Erne. Nature, 271(5643):339-442
    Oldfield F, Appleby P G. 1984. Empirical testing of 210Pb dating models for lake sediments. In:Haworth E T, Lund J W G, eds. Lake Sediments and Environmental History. Leicester:Leicester University Press
    Qian Jiangchu, DeMaster D J, Nittrouer C A, et al. 1985. Geochemistry features of Pb-210 in the estuary of the Changjiang River and it adjacent shelf. Acta Sedimentologica Sinica (in Chinese), 3(4):31-44
    Qin Yunsan, Zhao Yiyang, Chen Lirong, et al. 1996. Geology of the East China Sea. Beijing:Science Press
    Robbins J A. 1978. Geochemical and geophysical applications of radioactive lead. In:Nriagu J O, ed. Biogeochemistry of Lead in the Environment. Amsterdam:Elsevier Scientific, 285-393
    Sanchez-Cabeza J A, Ruiz-Fernández A C. 2012. 210Pb sediment radiochronology:An integrated formulation and classification of dating models. Geochimica et Cosmochimica Acta, 82:183-200
    Sawai Y. 2002. Evidence for 17th-century tsunamis generated on the Kuril-Kamchatka subduction zone, Lake Tokotan, Hokkaido, Japan. Journal of Asian Earth Sciences, 20(8):903-911
    Su Xianze, Ma Wentong, Xu Shengli, et al. 1984. The method of lead-210 geochronology for marine sediments. Taiwan Strait (in Chinese), 3(1):50-58
    Wan Guojiang. 1997. 210Pb Dating for recent sedimentation. Quaternary Sciences (in Chinese), 17(3):230-239
    Xia Xiaoming, Xie Qinchun, Li Yan, et al. 1999. 137Cs and 210Pb profiles of the seabed cores along the East China Sea coast and their implications to sedimentary environment. Donghai Marine Science (in Chinese), 17(4):20-27
    Xia Xiaoming, Yang Hui, Li Yan, et al. 2004. Modern sedimentation rates in the contiguous sea area of Changjiang Estuary and Hangzhou Bay. Acta Sedimentologica Sinica (in Chinese), 22(1):130-135
    Xie Qinchun, Ma Liming, Li Bogen, et al. 2001. Rapid storm sedimentation of Maotou deep trough in the Sanmen Bay of Zhejiang. Haiyang Xuebao (in Chinese), 23(5):78-86
    Zhang Jing, Mou Dehai, Du Jinzhou, et al. 2008. Study on comparison of excess 210Pb chronology of several models. Marine Environmental Science (in Chinese), 27(4):370-374, 382
    Zhang Rui, Pan Shaoming, Wang Yaping, et al. 2009. Sedimentation rates and characteristics of radionuclide 210Pb at the subaqueous delta in Changjiang Estuary. Acta Sedimentologica Sinica (in Chinese), 27(4):704-713
    Zhou Liang, Gao Shu, Yang Yang, et al. 2017. Typhoon events recorded in coastal lagoon deposits, southeastern Hainan Island. Acta Oceanologica Sinica, 36(4):37-45
    Zou Hanyang, Su Xianze, Yu Xingguang, et al. 1982. Determination of recent sedimentation rates on the continental shelf of the East China Sea using 210Pb method. Journal of Oceanography in Taiwan Strait (in Chinese), 1(2):30-40
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