Abstract
This study emphasizes to testify the potential of geochemical proxies of lacustrine sediments as indicative of past climatic changes since the last deglaciation over the catchment of a small closed lake in South China. Based on the study on the core K02 from Dahu Swamp, a small lake in the eastern Nanling Mountains, we inferred that chemical features of clastic materials, which were mainly derived from the granite weathering crust and transported by surface runoff into this lake, possibly had played an important role in affecting chemical characteristics of the sediments. Wetter climatic conditions would lead to stronger chemical weathering intensity (CWI), resulting in more soluble and mobile elements being easily leached downward in granite weathering crusts and the insoluble ones being enriched in the top materials of the weathering crusts. In contrast, dry conditions would exert a converse influence. Although this study presents a different climatic implication of geochemistry from lacustrine sediments in South China from that in north-central China, the results demonstrate that chemical elements of sediments in the small lake in South China can be utilized to reflect the CWI, which was closely in association with variations in temperature and precipitation in the lake catchment.
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References
Alley RB, Mayewski PA, Sowers T, Stuiver M, Taylor KC, Clark PU (1997) Holocene climatic instability, a prominent, widespread event 8200 years ago. Geology 25:483–486
Andrey VD, Saarinen TJ (2008) Geochemical records seasonal climate variability from varved lake sediments. Chin J Geochem 25:6–7
Barber DC, Bilodeau G, Southon J, Morehead MD, Kerwin MW, McNeely R, Gagnon JM, Dyke A, Andrews JT, Jennings AE, Hillaire-Marcel C (1999) Forcing of the cold event of 8200 years ago by catastrophic drainage of Laurentide lakes. Nature 400:344–348
Blands W, Rolls D (1998) Weathering, an introduction to the scientific principles. Arnold, London, p 271
Brijraj KD, Birgit GH (2003) Geochemistry of Rewalsar Lake sediment, Lesser Himalaya, India: implications for source-area weathering, provenance and tectonic setting. Geosci J 2003(7):299–312
Brown ET, Le Callonnec L, German CR (2000) Geochemical cycling of redox sensitive metals in sediments from Lake Malawi: a diagnostic paleotracer for episodic changes in mixing depth. Geochim Cosmochim Acta 64:3515–3523
China Vegetation Editing Committee (1990) China vegetation. Science Press, Beijing, pp 272–273 (in Chinese)
Craig H (1957) Isotopic standards for carbon and oxygen and correction factors for mass-spectrometric analysis of carbon dioxide. Geochim Cosmochim Acta 12:133–149
Davison W (1993) Iron and manganese in lakes. Earth Sci Rev 34:119–163
Dykoski CA, Edwards RL, Cheng H, Yuan DX, Cai YJ, Zhang ML, Lin Y, An ZS, Revenaugh J (2005) A high-resolution, absolute-dated Holocene and deglacial Asian monsoon record from Dongge Cave, China. Earth and Planet Sci Lett 233:71–86
Haberyan KA, Hecky RE (1987) The late Pleistocene and Holocene stratigraphy and paleolimnology of Lakes Kivu and Tanganyika. Palaeogeogr Palaeoclimatol Palaeoecol 61:169–197
Herzschuh U (2006) Palaeo-moisture evolution in monsoonal Central Asia during the last 50,000 years. Quat Sci Rev 25:163–178
Janssens JA (1983) A quantitative method for stratigraphic analysis of bryophytes in Holocene peat. J Ecol 71:189–196
Jin ZD, Wu JL, Cao JJ, Wang SM (2004) Holocene chemical weathering and climatic oscillations in north China: evidence from lacustrine sediments. Boreas 33:260–266
Jin ZD, Li FC, Cao JJ, Wang SM, Yu JM (2006) Geochemistry of Daihai Lake sediments, Inner Mongolia, north China: Implications for provenance, sedimentary sorting, and catchment weathering. Geomorphology 80:147–163
Karin AK, William S, André FL, Christian O, Michael S (2003) 9000 years of geochemical evolution of lithogenic major and trace elements in the sediment of an alpine lake-the role of climate, vegetation, and landuse history. J Paleolimn 30:307–320
Lasaga AC, Soler JM, Ganor J, Burch TE, Nagy KL (1994) Chemical weathering rate laws and global geochemical cycles. Geochim Cosmochim Acta 58:2361–2386
Liu JQ, Lu HY, Negendank J, Mingram J, Luo XJ, Wang WY, Chu GQ (2000) Periodicity of Holocene climatic variations in the Huguangyan Maar Lake. Chin Sci Bull 45:1712–1717
Mackereth FJH (1966) Some chemical observations on postglacial lake sediments. Philos Trans R Soc Biol Sci 250:165–213
Magny M, Begeot C (2004) Hydrological changes in the European mid-latitudes associated with freshwater outbursts from Lake Agassiz during the Younger Dryas event and the early Holocene. Quat Res 61:181–192
Peng YJ, Xiao JL, Nakamurab T, Liu BL, Inouchi Y (2005) Holocene East Asian monsoonal precipitation pattern revealed by grain-size distribution of core sediments of Daihai Lake in Inner Mongolia of north-central China. Earth Planet Sci Lett 233:467–479
Sai LN, Roger HK (2004) Geochemistry of lake sediments as a record of environmental change in a high Arctic watershed. Geochem 64:257–275
Stuiver M, Reimer PJ, Bard E, Beck JW, Burr GS, Hughen KA, Kromer B, Mc Cormac G, Van der Plicht J, Spurk M (1998) Intcal 98 radiocarbon age calibration, 24,000–0 cal BP. Radiocarbon 40:1041–1083
Sun QL, Wang SM, Zhou J, Chen ZY, Shen J, Xie XP, Wu F, Chen P (2010) Sediment geochemistry of Lake Daihai, north-central China, implications for catchments weathering and climate change during the Holocene. J Paleolimn 43:75–87
Wang SM (1992) Lake records of the Holocene climatic changes in China. In: Shi YF (ed) The Holocene climatic optimum and associated environment in China. Science Press, Beijing, pp 146–152 (in Chinese)
White AF, Blum AE (1995) Effects of climate on chemical weathering in watersheds. Geochim Cosmochim Acta 59:1729–1747
Xiao JY, Lu HB, Zhou WJ, Zhao ZJ, Hao RH (2007) Evolution of vegetation and climate since the last glacial maximum recorded at Dahu peat site, South China. Sci China Ser D Earth Sci 50:1209–1217
Yang SY, Li CX, Cai JG (2006) Geochemical compositions of core sediments in eastern China: implication for Late Cenozoic palaeoenvironmental changes. Palaeogeogr Palaeoclimatol Palaeoecol 229:287–302
Zhao J, Chen YW, Han YF (1997) Physical Geography of China. Higher Education Press, Beijing, pp 15–20 (in Chinese)
Zhong W, Xue JB, Zheng YM, Ma QH, Cai Y, Ouyang J, Xu LB, Zhou SZ (2009) Variations of monsoonal precipitation over the last 16,000 years in the eastern Nanling Mountains, South China. J Paleolimnol. doi:10.1007/s10933-009-9395-7
Zhong W, Xue JB, Cao JX, Zheng YM, Ma QH, Ouyang J, Cai Y, Zeng ZG, Liu W (2010a) Bulk organic carbon isotopic record of lacustrine sediments in Dahu Swamp, eastern Nanling Mountains in South China: Implication for catchment environmental and climatic changes in the last 16, 000 years. J Asian Earth Sci 38:162–169
Zhong W, Xue JB, Zheng YM, Ouyang J, Ma QH, Cai Y, Tang XH (2010b) Climatic changes since the last deglaciation inferred from a lacustrine sedimentary sequence in the eastern Nanling Mountains, south China. J Quat Sci. doi:10.1002/jqs.1384
Zhou WJ, Yu XF, Timothy JAJ, Burr G, Xiao JY, Lu XF, Xian F (2004) High-resolution evidence from southern China of an early Holocene optimum and a mid-Holocene dry event during the past 18000 years. Quat Res 62:39–48
Zolitschka B, Negendank JFW (1996) Sedimentology, dating and palaeoclimatic interpretation of a 76.3 ka record from Lago Grande di Monticchio, southern Italy. Quat Sci Rev 15:101–112
Acknowledgments
Analysis of radiocarbon dates was conducted at the Key Lab. of Western China’s Environmental Systems (Ministry of Education of China), Lanzhou University. Major and trace elements were measured at the Key Lab. of Geographical Process in Zhejiang Normal University, China. The X-ray diffraction measurement was done at Southeast University, China. We feel grateful to Prof. Chenjun Zhang, Prof. Jixiu Cao and Prof. Wei Ye for their help with laboratory analyses. We sincerely thank the anonymous reviewers for their thorough comments and constructive suggestions, which significantly improved the manuscript. This work was supported by National Natural Science Foundation (NSF) of China (No. 41071137 and 40671189), Research Program of Guangdong Province for High-level Talents, Natural Science Foundation of Guangdong Province (No. 8151063101000044) and the Fok Ying Tung Education Foundation grants (No. 91021).
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Zhong, W., Xue, J., Zheng, Y. et al. Sediment geochemistry of Dahu Swamp in the Nanling Mountains, South China: implication for catchment weathering during the last 16,000 years. Int J Earth Sci (Geol Rundsch) 101, 453–462 (2012). https://doi.org/10.1007/s00531-011-0680-0
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DOI: https://doi.org/10.1007/s00531-011-0680-0