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Dating Paleosol and Animal Remains in Loess Deposits

Published online by Cambridge University Press:  18 July 2016

H C Zhang*
Affiliation:
National Laboratory of Western China's Environmental Systems, MOE; College of Earth Sciences and Environments, Lanzhou University, Lanzhou 730000, China. Also: Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences (CAS), Nanjing 210008, China
B Li
Affiliation:
National Laboratory of Western China's Environmental Systems, MOE; College of Earth Sciences and Environments, Lanzhou University, Lanzhou 730000, China. Also: Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences (CAS), Nanjing 210008, China
M S Yang
Affiliation:
National Laboratory of Western China's Environmental Systems, MOE; College of Earth Sciences and Environments, Lanzhou University, Lanzhou 730000, China. Also: Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences (CAS), Nanjing 210008, China
G L Lei
Affiliation:
National Laboratory of Western China's Environmental Systems, MOE; College of Earth Sciences and Environments, Lanzhou University, Lanzhou 730000, China. Also: Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences (CAS), Nanjing 210008, China
H Ding
Affiliation:
College of Graduate Studies, Chinese Academy of Sciences (CAS), Beijing 100049, China
Jie Niu
Affiliation:
National Laboratory of Western China's Environmental Systems, MOE; College of Earth Sciences and Environments, Lanzhou University, Lanzhou 730000, China. Also: Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences (CAS), Nanjing 210008, China
H F Fan
Affiliation:
National Laboratory of Western China's Environmental Systems, MOE; College of Earth Sciences and Environments, Lanzhou University, Lanzhou 730000, China. Also: Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences (CAS), Nanjing 210008, China
W X Zhang
Affiliation:
National Laboratory of Western China's Environmental Systems, MOE; College of Earth Sciences and Environments, Lanzhou University, Lanzhou 730000, China. Also: Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences (CAS), Nanjing 210008, China
F Q Chang
Affiliation:
National Laboratory of Western China's Environmental Systems, MOE; College of Earth Sciences and Environments, Lanzhou University, Lanzhou 730000, China. Also: Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences (CAS), Nanjing 210008, China
*
Corresponding author. Email: zhanghc@niglas.ac.cn.
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Abstract

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Accurate and reliable dating of paleosols, animal remains, and artifacts is of crucial importance in reconstructing environmental change and understanding the interrelationship between human activities and natural environments. Dating different materials in the same sample can help resolve problems such as soil carbon sources and carbon storage state. Conventional radiocarbon dating of soil (inorganic and organic matter) and accelerator mass spectrometry (AMS) dating of animal remains (fossil bones and teeth) result in different ages for materials from the same sample position in a typical loess section at Xinglong Mountain, Yuzhong County, Gansu Province in NW China. Inorganic matter is ∼3400 yr older than organic matter, 4175 ± 175 cal BP to 3808 ± 90 cal BP. A 1610-yr difference between the 14C ages of fossils (animal bones and teeth) and soil organic matter suggests that a depositional hiatus exists in the studied profile. The varying 14C ages of fossils and soil organic and inorganic matter have important implications for paleoclimate reconstructions from loess sections. It is critical to consider the meaning of the variable 14C ages from different material components from the same sample position in terms of soil organic and inorganic carbon storage, vegetation history reconstruction, archaeology, and the study of ancient civilizations.

Type
Articles
Copyright
Copyright © 2006 by the Arizona Board of Regents on behalf of the University of Arizona 

References

An, CB, Feng, Z, Tang, L. 2004. Environmental change and cultural response between 8000 and 4000 cal yr BP in the western Loess Plateau, northwest China. Journal of Quaternary Science 19(6):529–35.Google Scholar
Bellamy, PH, Loveland, PJ, Bradley, RI, Lark, RM, Kirk, GJD. 2005. Carbon losses from all soils across England and Wales 1978–2003. Nature 437:245–8.CrossRefGoogle ScholarPubMed
Cao, M, Woodward, FI. 1998. Dynamic responses of terrestrial ecosystem carbon cycling to global climate change. Nature 393:249–52.Google Scholar
Cox, PM, Betts, RA, Jones, CD, Spall, SA, Totterdell, IJ. 2000. Acceleration of global warming due to carbon-cycle feedbacks in a coupled climate model. Nature 408:184–7.Google Scholar
Ding, Z, Yu, Z, Rutter, NW, Liu, T. 1994. Towards an orbital time scale for Chinese loess deposits. Quaternary Science Reviews 13:3970.Google Scholar
Guo, LB, Gifford, RM. 2002. Soil carbon stocks and land use change: a meta analysis. Global Change Biology 8:345–60.CrossRefGoogle Scholar
Guo, Z, Biscaye, P, Wei, L, Chen, X, Peng, S, Liu, T. 2000. Summer monsoon variations over the last 1.2 Ma from the weathering of loess-soil sequences in China. Geophysical Research Letters 27(12):1751–4.Google Scholar
Guo, ZTWF, Hao, QZ, Wu, HB, Qiao, YS, Zhu, RX, Peng, SZ, Wei, JJ, Yuan, BY, Liu, TS. 2002. Onset of Asian desertification by 22 Myr ago inferred from loess deposits in China. Nature 416:159–63.CrossRefGoogle ScholarPubMed
Houghton, RA. 2003. Revised estimates of the annual net flux of carbon to the atmosphere from changes in land use and land management 1850–2000. Tellus B 55:378–90.Google Scholar
Jickells, TD, An, ZS, Andersen, KK, Baker, AR, Bergametti, G, Brooks, N, Cao, JJ, Boyd, PW, Duce, RA, Hunter, KA, Kawahata, H, Kubilay, N, laRoche, J, Liss, PS, Mahowald, N, Prospero, JM, Ridgwell, AJ, Tegen, I, Torres, R. 2005. Global iron connections between desert dust, ocean biogeochemistry, and climate. Science 308(1):6771.Google Scholar
Knorr, W, Prentice, IC, House, JI, Holland, EA. 2005. Long-term sensitivity of soil carbon turnover to warming. Nature 433:298301.Google Scholar
Kukla, G, An, ZS, Melice, JL, Gavin, J, Xiao, JL. 1990. Magnetic susceptibility record of Chinese loess. Transactions of the Royal Society of Edinburgh: Earth Sciences 81:263–88.Google Scholar
Liu, JQ, Chen, TM, Cai, LZ. 1994. Dating and reconstruction of the high resolution time series in the Weinan loess section of the last 150,000 years. Quaternary Science (China) 3:193202. In Chinese.Google Scholar
Mayewski, PA, Rohling, EE, Stager, JC, Karlén, W, Maasch, KA, Meeker, LD, Meyerson, EA, Gasse, F, van Kreveld, S, Holmgren, K, Lee-Thorp, J, Rosqvist, G, Rack, F, Staubwasser, M, Schneider, RR, Steig, EJ. 2004. Holocene climate variability. Quaternary Research 62:243–55.Google Scholar
Porter, SC, Zhisheng, A. 1995. Correlation between climate events in the North Atlantic and China during the last glaciation. Nature 375:305–8.CrossRefGoogle Scholar
Powlson, D. 2005. Will soil amplify climate change? Nature 433:204–5.Google Scholar
Schramm, A, Mordechai, S, Goldstein, SL. 2000. Calibration of the 14C time scale to >40 ka by 234U-230Th dating of Lake Lisan sediments (last glacial Dead Sea). Earth and Planetary Science Letters 175:2740.CrossRefGoogle Scholar
Wang, S, Tian, H, Liu, J, Pan, S. 2003. Pattern and change of soil organic carbon storage in China: 1960s–1980s. Tellus B 55:416–27.Google Scholar
Wang, YQ, Zhang, XY, Arimoto, R, Cao, JJ, Shen, ZX. 2005. Characteristics of carbonate content and carbon and oxygen isotopic composition of northern China soil and dust aerosol and its application to tracing dust sources. Atmospheric Environment 39:2631–42.Google Scholar
Xia, ZK, Yang, XY. 2003. Preliminary study on the flood events about 4 ka BP in north China. Quaternary Science 6:661–74. In Chinese.Google Scholar
Yang, XY, Xia, ZK. 2001. Summarizing the environmental archaeology development in China. Progress in Geography 6:761–8. In Chinese.Google Scholar
Yin, JH, Pen, G, Jiao, WQ. 1997. A preliminary study on the radiocarbon dating of different organic fractions separated from peat. Seismology and Geology 3:227–80.Google Scholar
Zhang, HC. 1993. The carbonate stable carbon and oxygen isotopes of the Jiuzhoutai loess profile and their climate significance. Journal of Lanzhou University 29(3):232–40. In Chinese.Google Scholar
Zhang, HC, Ma, YZ, Li, JJ. 1998. Preliminary research on Holocene paleoclimatic change in the southern Tengger Desert. Chinese Science Bulletin 44(16):550–5. In Chinese.Google Scholar
Zhang, HC, Ma, YZ, Wünnemann, B, Pachur, H-J. 2000. A Holocene climatic record from arid northwestern China. Palaeogeography, Palaeoclimate, Palaeoecology 162:389401.CrossRefGoogle Scholar
Zhang, GL, He, Y, Gong, ZT. 2004. Characteristics of organic carbon distribution in anthropogenic soils and its implication on carbon sequestration. Quaternary Science (China) 2:149–59. In Chinese.Google Scholar
Zhisheng, A, Tunghseng, L, Yanchou, L, Porter, SC, Kukla, G, Xihao, W, Yingming, H. 1990. The long-term paleomonsoon variation recorded by the loess-paleosol sequence in central China. Quaternary International 8:91–5.Google Scholar
Zhisheng, A, Kutzbach, JE, Prell, WL, Porter, SC. 2001. Evolution of Asian monsoon and phased uplift of the Himalaya-Tibetan Plateau since Late Miocene times. Nature 411:62–6.Google Scholar
Zhou, QY, Huang, H Ch, Pang, JL. 2004. Study in the relationship between pedogenic environment changes and human impact in the Holocene soil of the loess plateau in the upper reaches of Jing He. Arid Land Geography 4:4351. In Chinese.Google Scholar