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Late Holocene Natural and Human-Induced Environmental Change Reconstructed from Peat Records in Eastern Central China

Published online by Cambridge University Press:  18 July 2016

Yan Zhao ,
Adam Hölzer  and
Zicheng Yu
Yan Zhao*
Affiliation:
MOE Key Laboratory of Western China's Environmental System, College of Earth and Environmental Sciences, Lanzhou University, Lanzhou 730000, China
Adam Hölzer
Affiliation:
National Natural History Museum, Karlsruhe, Erbprinzenstr 13, D76133 Karlsruhe, Germany
Zicheng Yu
Affiliation:
MOE Key Laboratory of Western China's Environmental System, College of Earth and Environmental Sciences, Lanzhou University, Lanzhou 730000, China Department of Earth and Environmental Sciences, Lehigh University, 31 Williams Drive, Bethlehem, Pennsylvania 18015, USA
*
Corresponding author. Email: yanzhao@lzu.edu.cn
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Abstract

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We present a high-resolution multiproxy record (geochemistry, macrofossil, and pollen) from a peatland in the Dajiuhu Basin in eastern central China. The chronology of the 120-cm peat profile was controlled by 6 accelerator mass spectrometry (AMS) 14C dates on plant remains, including 2 post-bomb dates. The age model was based on linear interpolations of calibrated ages. Plant macrofossil results indicate a major transition around 3600 cal BP from Sphagnum section Subsecunda and Drepanocladus sp. to Sphagnum imbricatum dominance, followed by the disappearance of S. imbricatum at 700 cal BP. These changes suggest a general sequence of local environment changes from a wet fen, through a Sphagnum-dominated peatland, to a dry sedge-dominated marsh, which are also reflected by change in peat lithology and composition. The drying trend after 3600 cal BP is in general agreement with the speleothem isotope record from this region and other paleoclimate records from east China, indicating a weakening summer monsoon resulting from a decrease in summer insolation. The shift to a dry environment at 700 cal BP might have been caused by human activities. Appearance of Cerealia pollen at 3600–3200 cal BP suggests the first introduction of crop farming in the region, while its absence at 3200–2000 cal BP could be attributed to abandonment of farmland. The increase of Ti and Si since 1300 cal BP may be related to agricultural activity and landscape erosion. A 2-step increase in Pb concentration at 1600 and 600 cal BP suggests 2 phases of industrial pollution intensity.

Type
Articles
Information
Radiocarbon , Volume 49 , Issue 2 , 2007 , pp. 789 - 798
Copyright
Copyright © 2007 by the Arizona Board of Regents on behalf of the University of Arizona 

References

Allen, SE. 1974. Chemical Analysis of Ecological Materials. Oxford: Blackwell Scientific Publications. 565 p.Google Scholar
An, ZS, Porter, SC, Kutzbach, JE, Wu, XH, Wang, SM, Liu, XD, Li, XQ, Zhou, WJ. 2000. Asynchronous Holocene optimum of the East Asian monsoon. Quaternary Science Reviews 19(8):743–62.CrossRefGoogle Scholar
members, COHMAP. 1988. Climatic changes of the last 18,000 years: observations and model simulations. Science 241(4869):1043–52.Google Scholar
Damman, AWH. 1978. Distribution and movement of elements in ombrotrophic peat bogs. Oikos 30(3):480–95.CrossRefGoogle Scholar
Dean, WE. 1974. Determination of carbonate and organic matter in calcareous sediments and sedimentary rocks by loss on ignition: comparison with other methods. Journal of Sedimentary Research 44(1):242–8Google Scholar
Faegri, K, Iversen, J. 1989. Textbook of Pollen Analysis. 4th edition. London: John Wiley and Sons. 338 p.Google Scholar
He, Y, Theakstone, WH, Zhang, ZL, Zhang, D, Yao, TD, Chen, T, Shen, YP, Pang, HX. 2004. Asynchronous Holocene climate change across China. Quaternary Research 61(1):52–63.Google Scholar
Hölzer, A, Hölzer, A. 1998. Silicon and titanium in peat profiles as indicators of human impact. The Holocene 8(6):685–96.Google Scholar
Hong, YT, Jiang, HB, Liu, TS, Zhou, LP, Beer, J, Li, HD, Leng, XT, Hong, B, Qin, XG. 2000. Response of climate to solar forcing recorded in a 6000-year δ18O time-series of Chinese peat cellulose. The Holocene 10(1):1–7.Google Scholar
Junmei, L, Zhang, Q, Shiyan, T, Jianhua, J. 2006. The onset and advance of the Asian summer monsoon. Chinese Science Bulletin 51:80–8.Google Scholar
Küster, H, Rehfuess, K-E. 1997. Pb and Cd concentrations in a southern Bavarian bog profile and the history of vegetation as recorded by pollen analysis. Water, Air and Soil Pollution 100(3–4):379–86.Google Scholar
Kutzbach, JE. 1981. Monsoon climate of the early Holocene: climate experiment with the Earth's orbital parameters for 9000 years ago. Science 214(4516):59–61.CrossRefGoogle ScholarPubMed
Lang, HQ, Jin, SR, Zhu, WC. 1983. Marsh in China. Shandong, China: Science and Technology Press. 25 p. In Chinese.Google Scholar
Li, WY, Yao, ZJ. 1993. Late Quaternary Vegetation and Environment of North and Middle Subtropical Region of China. Beijing: Ocean Press. p 27–47. In Chinese.Google Scholar
Li, XJ, Si, H. 1999. Sphagnaceae–Leucobryaceae. In: Gao, C, He, S, Crosby, MR, editors. Moss Flora of China. Volume 1. St. Louis: Missouri Botanical Garden. 273 p.Google Scholar
Nilsson, M, Klarqvist, M, Bohlin, E, Possnert, G. 2001. Variation in 14C age of macrofossils and different fractions of minute peat samples dated by AMS. The Holocene 11(5):579–86.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, Bindler, R, Brännvall, M-L. 2001. Using the historical atmospheric lead-deposition record as a chronological marker in sediment deposits in Europe. The Holocene 11(5):511–6.Google Scholar
Shennongjia Chorography Group. 1996. Chorography of Shennongjia. Wuhan, China: Hubei Science and Technology Press. p 1–79. In Chinese.Google Scholar
Shi, YF, Kong, ZC, Wang, SM, Tang, LY, Wang, FB, Yao, TD, Zhao, XT, Zhang, PY, Shi, SH. 1993. Mid-Holocene climates and environments in China. Global and Planetary Change 7(1–3):219–33.Google Scholar
Shotyk, W, Weiss, D, Appleby, PG, Cheburkin, AK, Frei, R, Gloor, M, Kramers, JD, Reese, S, Van Der Knaap, WO. 1998. History of atmospheric lead deposition since 12,370 14C yr BP from a peat bog, Jura Mountains, Switzerland. Science 281(5383):1635–40.CrossRefGoogle Scholar
Wang, FX, Qian, NF, Zhang, YL. 1995. Pollen Flora of China. Beijing: Science Press. 461 p. In Chinese.Google Scholar
Wang, YJ, Cheng, H, Edwards, RL, He, YQ, Kong, XG, An, ZS, Wu, JY, Kelly, MJ, Dykoski, CA, Li, XD. 2005. The Holocene Asian monsoon: links to solar changes and North Atlantic climate. Science 308(5723):854–7.Google Scholar
Xiao, P. 2002. Gusu Civilization and Sanxingdui Culture. Chengdu, China: Sichuan People's Press. In Chinese.Google Scholar
Xie, SC, Evershed, RP. 2002. Peat molecular fossils recording paleoclimatic change and organic replacement. Chinese Science Bulletin 46:1749–52.Google Scholar
Xu, H, Hong, YT, Lin, QH. 2002. Temperature variations in the past 6000 years inferred from δ18O of peat cellulose from Hongyuan, China. Chinese Science Bulletin 47:1181–6.Google Scholar
Yang, XQ. 1980. The development of ancient culture in west Hubei and the formation of Chu culture. In: Proceedings of the 2nd Chinese Archaeology Annual Meeting. Beijing: Cultural Relics Publishing House. p 21–37. In Chinese.Google Scholar
Zhang, M, Yuan, D, Lin, Y, Qin, J, Bin, L, Cheng, H, Edwards, RL. 2004. A 6000-year high-resolution climatic record from a stalagmite in Xiangshui Cave, Guilin, China. The Holocene 14(5):697–702.Google Scholar
Zhou, WJ, Lu, XF, Wu, ZK. 2002. Peat record reflecting Holocene climatic change in the Zoige Plateau and AMS radiocarbon dating. Chinese Science Bulletin 47:66–70.Google Scholar