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A Case Study Using 10Be-26Al Exposure Dating at the Xi’an AMS Center

Published online by Cambridge University Press:  19 January 2016

Li Zhang ,
Zhenkun Wu ,
Hong Chang ,
Ming Li ,
Guocheng Dong ,
Yunchong Fu ,
Guoqing Zhao  and
Weijian Zhou
Li Zhang
Affiliation:
State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi’an 710061, China Shaanxi Key Laboratory of Accelerator Mass Spectrometry Technology and Application, Xi’an AMS Center, Xi’an 710061, China
Zhenkun Wu
Affiliation:
State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi’an 710061, China Shaanxi Key Laboratory of Accelerator Mass Spectrometry Technology and Application, Xi’an AMS Center, Xi’an 710061, China
Hong Chang
Affiliation:
State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi’an 710061, China
Ming Li
Affiliation:
State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi’an 710061, China Shaanxi Key Laboratory of Accelerator Mass Spectrometry Technology and Application, Xi’an AMS Center, Xi’an 710061, China
Guocheng Dong
Affiliation:
State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi’an 710061, China Shaanxi Key Laboratory of Accelerator Mass Spectrometry Technology and Application, Xi’an AMS Center, Xi’an 710061, China
Yunchong Fu
Affiliation:
State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi’an 710061, China Shaanxi Key Laboratory of Accelerator Mass Spectrometry Technology and Application, Xi’an AMS Center, Xi’an 710061, China
Guoqing Zhao
Affiliation:
State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi’an 710061, China Shaanxi Key Laboratory of Accelerator Mass Spectrometry Technology and Application, Xi’an AMS Center, Xi’an 710061, China
Weijian Zhou*
Affiliation:
State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi’an 710061, China Shaanxi Key Laboratory of Accelerator Mass Spectrometry Technology and Application, Xi’an AMS Center, Xi’an 710061, China Xi’an Jiaotong University, Xi’an 710049, China
*
*Corresponding author. Email: [email protected].
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Abstract

Exposure age dating using in situ10Be and 26Al is a very useful technique for dating fluvial terraces. This is especially true in semiarid regions where other methods suffer from a paucity of suitable dating materials. This article describes sample preparation procedures and analytical benchmarks established at the Xi’an Accelerator Mass Spectrometry (AMS) Center for the study of in situ10Be and 26Al. Four intercomparison samples were analyzed in the study, using an improved sample preparation method. The exposure age results are shown to be in good agreement with published data, and demonstrate the reliability of the dating method. This article also presents new 10Be and 26Al results from quartz samples collected from a series of fluvial terraces from Guanshan River, along the Qilian Shan, northeastern Tibetan Plateau. The ages of three fluvial terraces from the Jinfosi site are shown to be (56.4±5.3) ka for T3, (10.7±1.0) ka for T2, and (7.2±1.0) ka for T1. The dating results are consistent with published data from the same region (10Be, 14C, and optically stimulated luminescence dating methods). A comparison of high-resolution climate records with age constraints for the terrace formation shows a close relationship between terrace formation and climate change.

Keywords

10Be-26Al exposure datingfluvial terracesXi’an AMSQilian Shan.
Type
Research Article
Information
Radiocarbon , Volume 58 , Issue 1 , March 2016 , pp. 193 - 203
Copyright
© 2016 by the Arizona Board of Regents on behalf of the University of Arizona 

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References

REFERENCES

Akçar, N, Deline, P, Ivy-Ochs, S, Alflmov, A, Hajdas, I, Kubik, PW, Christl, M, Schlüchter, C. 2012. The AD 1717 rock avalanche deposits in the upper Ferret Valley (Italy): a dating approach with cosmogenic 10Be. Journal of Quaternary Science 27(4):383–392.CrossRefGoogle Scholar
Balco, G. 2008. A complete and easily accessible means of calculating surface exposure ages or erosion rates from 10Be and 26Al measurements. Quaternary Geochronology 3:174–195.CrossRefGoogle Scholar
Balco, G. 2009. 26Al-10Be exposure age/erosion rate calculators: update from v.2.1 to v.2.2. http://hess.ess.washington.edu/math/.Google Scholar
Bhattacharyya, A. 1989. Vegetation and climate during the last 30,000 years in Ladakh. Palaeogeography, Palaeoclimatology, Palaeoecology 73(1–2):25–38.CrossRefGoogle Scholar
Bookhagen, B, Fleitmann, D, Nishiizumi, K, Strecker, MR, Thiede, RC. 2006. Holocene monsoonal dynamics and fluvial terrace formation in the northwest Himalaya, India. Geology 34(7):601–604.CrossRefGoogle Scholar
Brauer, A, Hajdas, I, Blockley, SP, Bronk Ramsey, C, Christl, M, Ivy-Ochs, S, Moseleye, GE, Nowaczyka, NN, Rasmussenf, SO, Robertsg, HM, Spötle, C, Staffd, RA, Svensson, A. 2014. The importance of independent chronology in integrating records of past climate change for the 60–8 ka INTIMATE time interval. Quaternary Science Reviews 106:47–66.CrossRefGoogle Scholar
Chen, WB. 2003. Principal features of tectonic deformation and their generation mechanism in the Hexi Corridor and its adjacent regions since late Quaternary [PhD dissertation]. Institute of Geology, China Seismological Bureau. p 56–59.Google Scholar
Cockburn, HAP. 2004. Geomorphological applications of cosmogenic isotope analysis. Progress in Physical Geography 28(1):1–42.CrossRefGoogle Scholar
Gosse, JC, Phillips, FM. 2001. Terrestrial in situ cosmogenic nuclides: theory and application. Quaternary Science Reviews 20(14):1475–1560.CrossRefGoogle Scholar
Granger, DE, Lifton, NA, Willenbring, JK. 2013. A cosmic trip: 25 years of cosmogenic nuclides in geology. Geological Society of America Bulletin 125(9–10):1379–1402.CrossRefGoogle Scholar
Gu, ZY, Xu, B, Lv, YW, Aldahan, A, Lal, D. 2006. A report on 10Be dating of terrace surfaces in Nujiang Riser Valley. Quaternary Sciences 26(2):293–294. In Chinese.Google Scholar
Hancock, GS, Anderson, RS, Chadwick, OA, Finkel, RC. 1999. Dating fluvial terraces with 10Be and 26Al profiles: application to the Wind River, Wyoming. Geomorphology 27(1–2):41–60.CrossRefGoogle Scholar
Hetzel, R, Niedermann, S, Ivy-Ochs, S, Kubik, PW, Tao, MX, Gao, B. 2002. 21Ne versus 10Be and 26Al exposure ages of fluvial terraces: the influence of crustal Ne in quartz. Earth and Planetary Science Letters 201(3):575–591.CrossRefGoogle Scholar
Hetzel, R, Niedermann, S, Tao, MX, Kubik, PW, Strecker, MR. 2006. Climatic versus tectonic control on river incision at the margin of NE Tibet: 10Be exposure dating of river terraces at the mountain front of the Qilian Shan. Journal of Geophysical Research 111:F03012.CrossRefGoogle Scholar
Ivy-Ochs, S. 1996. The dating of rock surfaces using in situ produced 10Be, 26Al and 36Cl, with examples from Antarctica and the Swiss Alps [PhD dissertation]. Zurich: ETH.Google Scholar
Jull, AJT, Scott, EM, Bierman, P. 2015. The CRONUS-Earth inter-comparison for cosmogenic isotope analysis. Quaternary Geochronology 26:3–10.CrossRefGoogle Scholar
Kelly, M, Black, S, Rowan, JS. 2000. A calcrete-based U/Th chronology for landform evolution in the Sorbas basin, southeast Spain. Quaternary Science Reviews 19(10):995–1010.CrossRefGoogle Scholar
Kohl, CP, Nishiizumi, K. 1992. Chemical isolation of quartz for measurement of in-situ-produced cosmogenic nuclides. Geochimica et Cosmochimica Acta 56(9):3583–3587.CrossRefGoogle Scholar
Kuhle, M. 1998. Reconstruction of the 2.4 million km2 late Pleistocene ice sheet on the Tibetan Plateau and its impact on the global climate. Quaternary International 45–46:71–108.CrossRefGoogle Scholar
Lal, D. 1991. Cosmic ray labeling of erosion surfaces: in situ nuclide production rates and erosion models. Earth and Planetary Science Letters 104(2–4):424–439.CrossRefGoogle Scholar
Lasserre, P, Morel, PH, Gaudemer, Y, Tapponnier, P, Ryerson, FJ, King, GCP, Metivier, F, Kasser, M, Kashgarian, M, Liu, BC, Lu, TY, Yuan, DY. 1999. Postglacial left slip rate and past occurrence of M≥8 earthquakes on the Western Haiyuan Fault, Gansu, China. Journal of Geophysical Research: Solid Earth 104(B8):17,633–51.CrossRefGoogle Scholar
Li, SJ, Zhang, HL, Shi, YF, Zhu, ZY. 2008. A high resolution MIS3 environmental change record derived from lacustrine deposit of Tianshuihai Lake, Qinghai-Tibet Plateau. Quaternary Sciences 28(1):122–131. In Chinese.Google Scholar
Lisiecki, LE, Raymo, ME. 2005. A Pliocene-Pleistocene stack of 57 globally distributed benthic 18O records. Paleoceanography 20:PA1003.Google Scholar
Merchel, S, Arnold, M, Aumaitre, G, Benedetti, L, Bourles, DL, Braucher, R, Alfimov, V, Freeman, SPHT, Steier, P, Wallner, A. 2008. Towards more precise 10Be and 36Cl data from measurements at the 10–14 level: influence of sample preparation. Nuclear Instruments and Methods in Physics Research B 266:4921–4926.CrossRefGoogle Scholar
Mériaux, AS, Ryerson, FJ, Tapponnier, P. 2004. Rapid slip along the central Altyn Tagh Fault: morphochronologic evidence from Cherchen He and Sulamu Tagh. Journal of Geophysical Research 109:B06401.CrossRefGoogle Scholar
Mériaux, AS, Tapponnier, P, Ryerson, FJ, Xu, XW, King, G, van der Woerd, J, Finkel, RC, Li, HB, Caffee, MW, Xu, ZQ, Chen, WB. 2005. The Aksay segment of the northern Altyn Tagh Fault: tectonic geomorphology, landscape evolution, and Holocene slip rate. Journal of Geophysical Research 110:B04404.CrossRefGoogle Scholar
Nishiizumi, K, Imamura, M, Caffee, MW, Southon, JR, Finkel, RC, McAninch, J. 2007. Absolute calibration of 10Be AMS standards. Nuclear Instruments and Methods in Physics Research B 258:403–413.CrossRefGoogle Scholar
Owen, LA, Spencer, JQ, Ma, HZ, Barnard, RL, Derbyshier, E, Finkel, RC, Caffee, MW, Zeng, YN. 2003. Timing of late Quaternary glaciation along the southwestern slopes of the Qilian Shan, Tibet. Boreas 32:281–291.CrossRefGoogle Scholar
Perrineau, A, van Der Woerd, J, Gaudemer, Y, Liu-Zeng, J, Pik, R, Tapponnier, P, Thuizat, R, Zheng, RZ. 2011. Incision rate of the Yellow River in Northeastern Tibet constrained by 10Be and 26Al cosmogenic isotope dating of fluvial terraces: implications for catchment evolution and plateau building. Geological Society London 353:189–219.CrossRefGoogle Scholar
Repka, JL, Anderson, RS, Finkel, RC. 1997. Cosmogenic dating of fluvial terraces, Fremont River, Utah. Earth and Planetary Science Letters 152(1–4):59–73.CrossRefGoogle Scholar
Rixhon, G, Braucher, R, Bourlès, D, Siame, L, Bovy, B, Demoulin, A. 2011. Quaternary river incision in NE Ardennes (Belgium)—insights from 10Be/26Al dating of river terraces. Quaternary Geochronology 6(2):273–284.CrossRefGoogle Scholar
Schnabel, C, Reinhardt, L, Barrows, TT, Bishop, P, Davidson, A, Fifield, LK, Freeman, S, Kim, JY, Maden, C, Xu, S. 2007. Inter-comparison in 10Be analysis starting from pre-purified quartz. Nuclear Instruments and Methods in Physics Research B 259:571–575.CrossRefGoogle Scholar
Schulte, L, Juliá, R, Burjachs, F, Hilgers, A. 2008. Middle Pleistocene to Holocene geochronology of the River Aguas terrace sequence (Iberian Peninsula): fluvial response to Mediterranean environmental change. Geomorphology 98(1–2):13–33.CrossRefGoogle Scholar
Schumm, SA. 1977. The Fluvial System. Hoboken: John Wiley and Sons.Google Scholar
Stone, JO. 2000. Air pressure and cosmogenic isotope production. Journal of Geophysical Research: Solid Earth 105(B10):23,753–9.CrossRefGoogle Scholar
van der Woerd, J, Klinger, Y, Kerry, Sieh, Tapponnier, P, Ryerson, FJ, Mériaux, A-S. 2006. Long-term slip rate of the southern San Andreas Fault from 10Be-26Al surface exposure dating of an offset alluvial fan. Journal of Geophysical Research: Solid Earth 111:B04407.CrossRefGoogle Scholar
West, AJ, Hetzel, R, Li, G, Jin, ZD, Zhang, F, Hilton, RG, Densmore, AL. 2014. Dilution of 10Be in detrital quartz by earthquake-induced landslides: implications for determining denudation rates and potential to provide insights into landslide sediment dynamics. Earth and Planetary Science Letters 396:143–153.CrossRefGoogle Scholar
Yao, TD, Thompson, LG, Shi, YF, Jiao, KQ, Zhang, XP. 1997. A study on the climate changes from Guliya ice core records since Last Interglacial Period. Science in China (Series D) 6:447–452.Google Scholar
Yuan, DY, Champagnac, JD, Ge, WP, Molnar, P, Zhang, PZ, Zheng, WJ, Zhang, HP, Liu, XW. 2011. Late Quaternary right-lateral slip rates of faults adjacent to the lake Qinghai, northeastern margin of the Tibetan Plateau. Geological Society of America Bulletin 123(9–10):2016–2030.CrossRefGoogle Scholar
Zhang, HC, Ma, YZ, Li, JJ, Pachur, HJ, Wuenneman, B. 1999. The Holocene palaeoclimatic change in southern vicinity of Tengger Desert. Chinese Science Bulletin 44(6):550–555.CrossRefGoogle Scholar
Zhang, L, Zhou, WJ, Chang, H, Zhao, GQ, Song, SH, Wu, ZK. 2012. The extraction of in-situ 10Be and 26Al from rock sample and accelerator mass spectrometric measurements. Rock and Mineral Analysis 3(1):83–89. In Chinese.Google Scholar
Zheng, Y, Jia, J, Nie, XK, Kong, P. 2014. Cosmogenic nuclide burial age of the Sanying Formation and its implications. Science China: Earth Sciences 57(6):1141–1149.Google Scholar
Zhou, WJ, Lu, XF, Wu, ZK, Zhao, WN, Huang, CH, Li, LL, Cheng, P, Xin, ZH. 2007. New results on Xi’an-AMS and sample preparation systems at Xi’an-AMS Center. Nuclear Instruments and Methods in Physics Research B 262:135–142.CrossRefGoogle Scholar