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Buried Ancient Forest and Implications for Paleoclimate Since the Mid-Holocene in South China

  • C D Shen (a1) (a2), P Ding (a1), N Wang (a1), W X Yi (a1), X F Ding (a2), D P Fu (a2), K X Liu (a2) and L P Zhou (a3)...

Abstract

The historical evolution of an ancient forest that developed at Gaoyao, south China, can be divided into 4 stages of radiocarbon intervals (1.1–1.5, 2.0–3.5, 3.6–4.0, and 4.3–4.9 ka) in which the last 3 stages all developed in a wetland and formed humic layers of 2.0, 0.5, and 0.7 m depth, respectively. The humic layers were interrupted by 2 white-gray silty clay layers that most likely formed during climate fluctuations. Four drought events were identified during the evolution of the ancient forest, occurring around 4.3, 3.6, 2.0, and 1.1 ka, respectively, with durations of ∼1000 14C yr. These events are consistent with other records both in low- and high-latitude areas, in particular with the little ice ages occurring since the mid-Holocene. Precipitation likely increased from 5.0 to 3.6 ka in south China, then decreased, which is probably the main cause for the development as well as the demise of the ancient forest.

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Copyright

Corresponding author

Corresponding author. Email: cdshen@gig.ac.cn.

References

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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.
Bond, G, Showers, W, Cheseby, M, Lotti, R, Almasi, P, deMenocal, P, Priore, P, Cullen, H, Hajdas, I, Bonani, G. 1997. A pervasive millennial-scale cycle in North Atlantic Holocene and glacial climates. Science 278(5341):1257–66.
Bond, G, Kromer, B, Beer, J, Muscheler, R, Evans, MN, Showers, W, Hoffmann, S, Lotti-Bond, R, Hajdas, I, Bonani, G. 2001. Persistent solar influence on North Atlantic climate during the Holocene. Science 294(5549):2130–6.
Chen, QQ, Shen, CD, Sun, YM, Peng, SL, Yi, WY, Li, ZA, Jiang, MT. 2005. Spatial and temporal distribution of carbon isotopes in soil organic matter at the Dinghushan Biosphere Reserve, South China. Plant and Soil 273(1–2):115–28.
deMenocal, P, Ortiz, J, Guilderson, T, Sarnthein, M. 2000. Coherent high- and low- latitude climate variability during the Holocene warm period. Science 288(5474):2198–202.
Ding, P, Shen, CD, Wang, N, Yi, WX, Liu, KX, Ding, XF, Fu, DP. 2009. Carbon isotopic composition and its implications on paleoclimate of the underground ancient forest ecosystem in Sihui, Guangdong. Science in China Series D 52(5):638–46.
Haug, GH, Hughen, KA, Sigman, DM, Peterson, LC, Röhl, U. 2001. Southward migration of the intertropical convergence zone through the Holocene. Science 293(5533):1304–8.
Hodell, DA, Curtis, JH, Brenner, M. 1995. Possible role of climate in the collapse of Classic Maya civilization. Nature 375(6530):391–4.
Holmgren, K, Lee-Thorp, JA, Cooper, GRJ, Lundblad, K, Partridge, TC, Scott, L, Sithaldeen, R, Talma, AS, Tyson, PD. 2003. Persistent millennial-scale climatic variability over the past 25,000 years in southern Africa. Quaternary Science Reviews 22(21–22):2311–26.
Li, FG, Xia, NH. 2004. The geographical distribution and cause of threat to Glyptostrobus pensilis (Taxodiaceae). Journal of Tropical and Subtropical Botany 12:1320. In Chinese with English abstract.
Li, PR, Zheng, JS, Fang, GX. 1991. Quaternary Geology in the Guangzhou Area. Guangzhou: Hunnan University of Science and Technology Press. p 5381. In Chinese.
Li, PR, Cui, HT, Tan, HZ. 2001. A study on Holocene buried timbers in Guangdong. Tropical Geography 21:195–7. In Chinese with English abstract.
Stuiver, M, Reimer, PJ. 1993. Extended 14C data base and revised CALIB 3.0 14C age calibration program. Radiocarbon 35(1):215–30.
Stuiver, M, Grootes, PM, Braziunas, TF. 1995. The GISP2 δ18O climate record of the past 16,500 years and the role of the sun, ocean and volcanoes. Quaternary Research 44(3):341–54.
Wang, YJ, Chen, 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.
Xu, JH. 1998. Sun, climate, famine and nationality migrations. Science in China Series D 28:366–84. In Chinese.
Xu, XM, Trumbore, SE, Zheng, SH, Southon, JR, McDuffee, KE, Luttgen, M, Liu, JC. 2007. Modifying a sealed tube zinc reduction method for preparation of AMS graphite targets: reducing background and attaining high precision. Nuclear Instruments and Methods in Physics Research B 259(1):320–9.
Yancheva, G, Norbert, NR, Mingram, J, Dulski, P, Schettler, G, Negendank, JFW, Liu, J, Sigman, DM, Peterson, LC, Haug, GH. 2007. Influence of the intertropical convergence zone on the East Asian monsoon. Nature 445(7123):74–7.
Yi, ZG, Fu, SL, Yi, WM, Zhou, GY, Mo, JM, Zhang, DQ, Ding, MM, Wang, XM, Zhou, LX. 2007. Partitioning soil respiration of subtropical forests with different successional stages in south China. Forest Ecology and Management 243(2–3):178–86.
Yu, KF, Liu, DS, Shen, CD. 2002. High-frequency climatic oscillations recorded in a Holocene coral reef at Leizhou Peninsula, South China Sea. Science in China Series D 45(12):1057–67.
Yu, ZY, Peng, SL. 1995. The artificial and natural restoration of tropical and subtropical forests. Acta Ecologica Sinica 15(A):117. In Chinese with English abstract.
Zhang, DE, Lu, LH. 2007. Anti-correlation of summer/winter monsoons? Nature 450(7168):E7E9.
Zhou, HY, Guan, HZ, Chi, BH. 2007. Record of winter monsoon strength. Nature 450(7168):E10E11.
Zong, YQ. 2004. Mid-Holocene sea-level highstand along the southeast coast of China. Quaternary International 117(1):5567.

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