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《Geochimica》 2004-05
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Response of the n-alkanes and polycyclic aromatic hydrocarbons records in sediments from Lake Liangzi to the environmental change

LIU Jianhua1,2, QI Shihua1, ZHANG Gan2, S.K. Donyinah1, LIU Xiang2,LI Jun2, LIU Guoqing21. Institute of Geochemistry, China University of Geosciences, Wuhan 430074, China; 2. State Key Laboratory of Organic Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China  
Lake Liangzi is located in the southeastern part of Hubei Province and adjacent to the Tonglushan ancient copper ore site. In order to reconstruct the history of the environmental change in this area and identify the impact of anthropogenic activities on the sediment records of Lake Liangzi, a systematic study was made of the organic composition of sediments from the lake. A sediment core 345 cm long was collected in 2002 from the central part of the lake, sliced into 1 cm sections and analyzed by GC for nalkanes, and by GCMS for PAHs (polycyclic aromatic hydrocarbons). The data reveal that sedimentation in Liangzi Lake has changed through time. It’s found that an abrupt upward increase of the contents of nalkanes and PAHs from depth 181~194 cm exists in the sediment core, and the diagnostic ratios of nalkanes indicate that the proportion of landderived longchained components has increased dramatically from depth 181 cm in core too, implying that the increase in the contents of organic matter in sediments is mainly attributed to the increase of the landderived organic matter inputs from 181 cm in core, which corresponds to the Spring Autumn Period (770 B.C.-476 B.C.) and the Warring States Period (475 B.C.-221 B.C.) in China’s history according to 14C dating. It’s suggested that the variations along the core are most probably related to the climatic evolution of this area and the consequent anthropogenic influences on the organic geochemical records in Lake Liangzi.
【Fund】: 国家自然科学基金(40173032)
【CateGory Index】: P593
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