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Temporal Change of Radiocarbon Reservoir Effect in Sugan Lake, Northwest China during the Late Holocene

Published online by Cambridge University Press:  18 July 2016

Ai-feng Zhou*
Affiliation:
CAEP, Key Laboratory of West China's Environmental System (Ministry of Education), Lanzhou University, Lanzhou 730000, China
Fa-hu Chen
Affiliation:
CAEP, Key Laboratory of West China's Environmental System (Ministry of Education), Lanzhou University, Lanzhou 730000, China
Zong-li Wang
Affiliation:
CAEP, Key Laboratory of West China's Environmental System (Ministry of Education), Lanzhou University, Lanzhou 730000, China
Mei-lin Yang
Affiliation:
Appraisal Center of Environmental Engineering of Yunnan Province, Kunming 650032, China
Ming-rui Qiang
Affiliation:
CAEP, Key Laboratory of West China's Environmental System (Ministry of Education), Lanzhou University, Lanzhou 730000, China
Jia-wu Zhang
Affiliation:
CAEP, Key Laboratory of West China's Environmental System (Ministry of Education), Lanzhou University, Lanzhou 730000, China
*
Corresponding author. Email: zhouaf@lzu.edu.cn
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Abstract

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Many lacustrine chronology records suffer from radiocarbon reservoir effects. A continuous, accurate varve chronology, in conjunction with accelerator mass spectrometry (AMS) 14C dating, was used to determine the age of lacustrine sediment and to quantify the past 14C reservoir effect in Sugan Lake (China). Reservoir age varied from 4340 to 2590 yr due to 14C-depleted water in the late Holocene. However, during the Little Ice Age (LIA), 14C reservoir age was relatively stable. According to this study, 14C reservoir age in the late Holocene may be driven by hydrological and climatic changes of this period. Therefore, special caution should be paid to the correction of the 14C reservoir effect by a unique 14C reservoir age in paleoclimatic and paleolimnological study of northwest China.

Type
Radiocarbon, Archaeology, and Landscape Change
Copyright
Copyright © 2009 by the Arizona Board of Regents on behalf of the University of Arizona 

References

Belmaker, R, Stein, M, Yechieli, Y, Lazar, B. 2007. Controls on the radiocarbon reservoir ages in the modern Dead Sea drainage system and in the last Glacial Lake Lisan. Radiocarbon 49(2):969–82.Google Scholar
Chen, FH, Zhu, Y, Li, JJ, Shi, Q, Jin, LY, Wünnemann, B. 2001. Abrupt Holocene changes of the Asian monsoon at millennial- and centennial-scales: evidence from lake sediment document in Minqin Basin, north China. Chinese Science Bulletin 46(23):1942–7.CrossRefGoogle Scholar
Colman, SM, Jones, GA, Rubin, M, King, JW, Peck, JA, Orem, WH. 1996. AMS radiocarbon analyses from Lake Baikal, Siberia: challenges of dating sediments from a large, oligotrophic lake. Quaternary Science Reviews 15(7):669–84.CrossRefGoogle Scholar
Culleton, BJ. 2006. Implications of a freshwater radiocarbon reservoir correction for the timing of late Holocene settlement of the Elk Hills, Kern County, California. Journal of Archaeological Science 33(9):1331–9.Google Scholar
Geyh, M, Schotterer, U, Grosjean, M. 1998. Temporal changes of the 14C reservoir effect in lakes. Radiocarbon 40(2):921–31.Google Scholar
Goslar, T, Pazdur, A, Pazdur, MF, Walanus, A. 1989. Radiocarbon and varve chronologies of annually laminated lake sediments of Gościąż Lake. Radiocarbon 31(3):940–7.Google Scholar
Grootes, PM, Nadeau, MJ, Rieck, A. 2004. 14C-AMS at the Leibniz-Labor: radiometric dating and isotope research. Nuclear Instruments and Methods in Physics Research B 223–224:5561.Google Scholar
Hajdas, I, Bonani, G, Goslar, T. 1995. Radiocarbon dating the Holocene in the Gościąż lake floating varve chronology. Radiocarbon 37(1):71–4.Google Scholar
Hall, BL, Henderson, GM. 2001. Use of uranium-thorium dating to determine past 14C reservoir effects in lakes: examples from Antarctica. Earth and Planetary Science Letters 193(3):565–77.CrossRefGoogle Scholar
Hendy, CH, Hall, BL. 2006. The radiocarbon reservoir effect in proglacial lakes: examples from Antarctica. Earth and Planetary Science Letters 241(3–4):413–21.Google Scholar
Hutchinson, I, James, TS, Reimer, PJ, Bornhold, BD, Clague, JJ. 2004. Marine and limnic radiocarbon reservoir corrections for studies of late- and postglacial environments in Georgia Basin and Puget Lowland, British Columbia, Canada and Washington, USA. Quaternary Research 61(2):193203.Google Scholar
Liu, KB, Yao, ZY, Thompson, LG. 1998. A pollen record of Holocene climatic changes from Dunde ice cap, Qinghai-Tibetan Plateau. Geology 26(2):135–8.Google Scholar
Moreton, SG, Rosqvist, GC, Davies, SJ, Bentley, MJ. 2004. Radiocarbon reservoir ages from freshwater lakes, South Georgia, sub-Antarctic: modern analogues from particulate organic matter and surface sediments. Radiocarbon 46(2):621–6.Google Scholar
Ojala, AEK, Saarnisto, M. 1999. Comparative varve counting and magnetic properties of the 8400-yr sequence of an annually laminated sediment in Lake Valkiajärvi, central Finland. Journal of Paleolimnology 22(4):335–48.Google Scholar
Ojala, AEK, Heinsalu, A, Saarnisto, M, Tiljander, M. 2005. Annually laminated sediments date the drainage of the Ancylus Lake and early Holocene shoreline displacement in central Finland. Quaternary International 130(1):6373.Google Scholar
Qiang, MR, Chen, FH, Zhang, JW, Gao, SY, Zhou, AF. 2005. Climatic changes documented by stable isotopes of sedimentary carbonate in Sugan Lake, northeastern Tibetan Plateau of China, since 2 ka BP. Chinese Science Bulletin 50(17):1930–9.Google Scholar
Reimer, PJ, Baillie, MGL, Bard, E, Bayliss, A, Beck, JW, Bertrand, CJH, Blackwell, PG, Buck, CE, Burr, GS, Cutler, KB, Damon, PE, Edwards, RL, Fairbanks, RG, Friedrich, M, Guilderson, TP, Hogg, AG, Hughen, KA, Kromer, B, McCormac, G, Manning, S, Bronk Ramsey, C, Reimer, RW, Remmele, S, Southon, JR, Stuiver, M, Talamo, S, Taylor, FW, van der Plicht, J, Weyhenmeyer, CE. 2004. IntCal04 terrestrial radiocarbon age calibration, 0–26 cal kyr BP. Radiocarbon 46(3):1029–58.Google Scholar
Renberg, I. 1981. Improved methods for sampling, photographing and varve counting of varved lake sediments. Boreas 10(3):255–8.Google Scholar
Shen, J, Liu, XQ, Wang, SM, Ryo, M. 2005. Palaeoclimatic changes in the Qinghai Lake area during the last 18,000 years. Quaternary International 136(1):131–40.Google Scholar
Simola, H. 1977. Diatom succession in the formation of annually laminated sediment in Lovojärvi, a small eutrophicated lake. Annales Botanicae Fennici 14:143–8.Google Scholar
Stein, M, Migowski, C, Bookman, R, Lazar, B. 2004. Temporal changes in radiocarbon reservoir age in the Dead Sea Lake Lisan system. Radiocarbon 46(2):649–55.Google Scholar
Stiller, M, Kaufman, A, Carmi, I, Mintz, G. 2001. Calibration of lacustrine sediment ages using the relationship between 14C levels in lake waters and in the atmosphere: the case of Lake Kinneret. Radiocarbon 43(2B):821–30.CrossRefGoogle Scholar
Yao, TD, Thompson, LG, Qin, DH, Tian, LD, Jiao, KQ, Yang, ZH, Xie, C. 1996. Variations in temperature and precipitation in the past 2000a on the Xizang (Tibet) Plateau-Guliya ice core record. Science in China (Series D) 26(4):426–33.Google Scholar
Yu, SY, Shen, J, Colman, SM. 2007. Modeling the radiocarbon the radiocarbon reservoir effect in lacustrine systems. Radiocarbon 49(3):1241–54.Google Scholar
Zhou, AF. 2007a. Varve chronology and Late Holocene environmental changes in Sugan Lake, northern Qaidam Basin [PhD dissertation]. Lanzhou University.Google Scholar
Zhou, AF, Chen, FH, Qiang, M-R, Yang, ML, Zhang, JW. 2007b. The discovery of annually laminated sediments (varves) from shallow Sugan Lake in inland arid China and their paleoclimatic significance. Science in China (Series D) 50(8):1218–24.CrossRefGoogle Scholar