Hostname: page-component-586b7cd67f-t7czq Total loading time: 0 Render date: 2024-11-29T01:30:03.176Z Has data issue: false hasContentIssue false

AMS Radiocarbon Dating Problems Between 10 and 8 Ka BP in Lacustrine Deposits from Lake Gun Nur, Northern Mongolia

Published online by Cambridge University Press:  18 July 2016

F Q Chang
Affiliation:
Key Laboratory of Plateau Lake Ecology and Global Change, College of Tourism and Geography, Yunnan Normal University, No. 1 Yuhua District, Chenggong, 650500 Kunming, China.
H C Zhang*
Affiliation:
Key Laboratory of Plateau Lake Ecology and Global Change, College of Tourism and Geography, Yunnan Normal University, No. 1 Yuhua District, Chenggong, 650500 Kunming, China.
Q Z Ming
Affiliation:
Key Laboratory of Plateau Lake Ecology and Global Change, College of Tourism and Geography, Yunnan Normal University, No. 1 Yuhua District, Chenggong, 650500 Kunming, China.
G J Chen
Affiliation:
Key Laboratory of Plateau Lake Ecology and Global Change, College of Tourism and Geography, Yunnan Normal University, No. 1 Yuhua District, Chenggong, 650500 Kunming, China.
W X Zhang
Affiliation:
Key Laboratory of Plateau Lake Ecology and Global Change, College of Tourism and Geography, Yunnan Normal University, No. 1 Yuhua District, Chenggong, 650500 Kunming, China.
Z T Shi
Affiliation:
Key Laboratory of Plateau Lake Ecology and Global Change, College of Tourism and Geography, Yunnan Normal University, No. 1 Yuhua District, Chenggong, 650500 Kunming, China.
Z D Feng
Affiliation:
Department of Geology, Baylor University, Waco, Texas 76712, USA.
*
Corresponding author. Email: [email protected].
Rights & Permissions [Opens in a new window]

Abstract

Core share and HTML view are not available for this content. However, as you have access to this content, a full PDF is available via the ‘Save PDF’ action button.

Accelerator mass spectrometry (AMS) radiocarbon dating a continuous core from Lake Gun Nur, northern Mongolia, shows a period between 10 and 8 ka BP that could not be dated accurately. Further dating on alkali-insoluble residue and humic acid from the same samples in the Gun Nur core suggest that this AMS 14C date anomaly is neither analytical nor material related. We hypothesize that the 14C anomaly may be derived from increasing production rates of 14C caused by diminished solar activity, a low 14CO2/14CO ratio in the atmosphere, or an unstable 14C flux in the lower atmosphere caused by changing geomagnetic field strength. Our results imply that the 14C data used for 14C age calibration cannot correct the age-depth regression between 8 and 10 ka BP to fit the age-depth model along with other time intervals.

Type
Articles
Copyright
Copyright © 2011 The Arizona Board of Regents on behalf of the University of Arizona 

References

Bard, E. 1998. Geochemical and geophysical implications of the radiocarbon calibration. Geochimica et Cosmochimica Acta 62(12):2025–38.Google Scholar
Bard, E, Fairbanks, R, Arnold, M, Maurice, P, Duprat, J, Moyes, J, Duplessy, J-C. 1989. Sea-leave estimates during the last deglaciation based on δ18O and accelerator mass spectrometry 14C ages measured in Globierina bulloides. Quaternary Research 31(3):381–91.Google Scholar
Bard, E, Arnold, M, Mangerud, J, Paterne, M, Labeyrie, L, Duprat, J, Mélières, M-A, Sønstegaard, E, Duplessy, J-C. 1994. The North Atlantic atmosphere-sea surface 14C gradient during the Younger Dryas climatic event. Earth and Planetary Science Letters 126(4):275–87.CrossRefGoogle Scholar
Engel, A, Möbius, T, Bönisch, H, Schmidt, U, Heinz, R, Levin, I, Atlas, E, Aoki, S, Nakazawa, T, Sugawara, S, Moore, F, Hurst, D, Elkins, J, Schauffle, S, Andrews A Boering, K. 2009. Age of stratospheric air unchanged within uncertainties over the past 30 years. Nature Geoscience 2(1):2831.CrossRefGoogle Scholar
Feng, ZD, Wang, WG, Guo, LL, Khosbayar, P, Narantsetseg, T, Jull, AJT, An, CB, Li, XQ, Zhang, HC, Ma, YZ. 2005. Holocene climate changes in the Mongolian Plateau: preliminary results. Quaternary International 136(1):2532.Google Scholar
Geyh, MA, Schleicher, H. 1990. Absolute Age Determination—Physical and Chemical Dating Methods and Their Application. Berlin: Springer-Verlag. p 162–80.CrossRefGoogle Scholar
Hajdas, I, Ivy, SD, Beer, J, Bonani, G, Imboden, D, Lotter, AF, Sturm, M, Suter, M. 1993. AMS radiocarbon dating and varve chronology of Lake Soppensee: 6000 to 12000 14C years BP. Climate Dynamics 9(3):107–16.Google Scholar
Kitagawa, H, van der Plicht, J. 1998. A 40,000-year varve chronology from Lake Suigetsu, Japan: extension of the 14C calibration curve. Radiocarbon 40(1):505–15.Google Scholar
Lal, D, Jull, AJT, Pollard, D, Vacher, L. 2005. Evidence for large century time-scale changes in solar activity in the past 32 kyr, based on in-situ cosmogenic 14C in ice at Summit, Greenland. Earth and Planetary Science Letters 234(3–4):335–49.Google Scholar
Mingram, J, Schettler, G, Nowaczyk, N, Luo, XJ, Lu, HY, Liu, JQ, Negendank, JFW. 2004. The Huguang maar lake – a high-resolution record of palaeoenvironmental and palaeoclimatic changes over the last 78,000 years from South China. Quaternary International 122(1):85107.CrossRefGoogle Scholar
Reimer, PJ, Baillie, MGL, Bard, E, Bayliss, A, Beck, JW, Blackwell, PG, Buck, CE, Burr, GS, Cutler, KB, Damon, PE, Edwards, RL, Fairbanks, RG, Friedrich, M, Guilderson, TP, Herring, C, 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, C. 2004. IntCal04 terrestrial radiocarbon age calibration, 0–26 cal kyr BP. Radiocarbon 46(3):1029–58.Google Scholar
Ricketts, RD, Johnson, TC, Brown, ET, Rasmussen, KA, Romanovsky, VV. 2001. The Holocene paleolimnology of Lake Issyk-Kul, Kyrgyzstan: trace element and stable isotope composition of ostracodes. Palaeogeography, Palaeoclimatology, Palaeoecology 176(1–4):207–27.Google Scholar
Sikes, EL, Samson, CR, Guilderson, TP, Howard, WR. 2000. Old radiocarbon ages in the southwest Pacific Ocean during the last glacial period and deglaciation. Nature 405(6786):555–9.Google Scholar
Solanki, SK, Usoskin, IG, Kromer, B, Schüssler, M, Beer, J. 2004. Unusual activity of the Sun during recent decades compared to the previous 11,000 years. Nature 431(7012):1084–7.Google Scholar
Stuiver, M, Braziunas, T. 1993. Modeling atmospheric 14C influences and 14C ages of marine samples to 10,000 BC. Radiocarbon 35(1):137–89.Google Scholar
Stuiver, M, Braziunas, TF, Becker, B, Kromer, B. 1991. Climatic, solar, oceanic, and geomagnetic influences on Late-Glacial and Holocene atmospheric 14C/12C change. Quaternary Research 35:124.Google Scholar
Wang, WG, Feng, ZD, Lee, XQ, Zhang, HC, Ma, YZ, An, CB, Guo, LL. 2004. Holocene abrupt climate shifts recorded in Gun Nur lake core, Northern Mongolia. Chinese Science Bulletin 49(5):520–26.Google Scholar
Yang, S, Odah, H, Shaw, J. 2000. Variations in the geomagnetic dipole moment over the last 12000 years. Geophysical Journal International 140(1):158–62.Google Scholar
Zhang, HC, Li, B, Yang, MS, Lei, GL, Ding, H, Niu, J, Fan, HF, Zhang, WX, Chang, FQ. 2006a. Dating paleosol and animal remains in loess deposits. Radiocarbon 48(1):109–16.Google Scholar
Zhang, HC, Ming, QZ, Lei, GL, Zhang, WX, Fan, HF, Chang, FQ, Wünnemann, B, Hartman, K. 2006b. Dilemma of dating on lacustrine deposits in a hyperarid inland basin of NW China. Radiocarbon 48(2):219–26.Google Scholar
Zhang, HC, Fan, HF, Chang, FQ, Zhang, WX, Lei, GL, Yang, MS, Lei, YB, Yang, LQ. 2008. AMS dating on the shell bar section from Qaidam Basin, NE Tibetan Plateau, China. Radiocarbon 50(2):255–65.Google Scholar