[1] Lu Longfei, Cai Jingong, Bao Yujin,et al. Summary of processes and significance of clay minerals in marine sedimentary organic matter preservation and in global carbon cycle [J].Advances in Earth Science,2006,21(9):931-937. [卢龙飞,蔡进功,包于进,等.粘土矿物保存海洋沉积有机质研究进展及其碳循环意义 [J].地球科学进展,2006,21(9):931-937.] [2] Lin S W, Hsieh I-Jy, Huang K M,et al. Influence of the Yangtze River and grain size on the spatial variations of heavy metals and organic carbon in the East China Sea continental shelf sediments [J].Chemical Geology,2002, 182:377-394. [3] Milliman J D,Xie Q C,Yang Z S.Transfer of particulate organic carbon and nitrogen from the Yangtze River to ocean [J].American Journal of Science,1984,284:824-834. [4] Edmond J M,Spivack A,Grant B C, et al. Chemical dynamics of the Changjiang Estuary [J].Continental Shelf Research,1985,4:17-36. [5] Tan F C,Cai D L,Edmond J M.Carbon isotope geochemistry of the Changjiang Estuary [J].Estuary Coastal and Shelf Science,1991,32:395-403. [6] Cai D L,Han Y B.Carbon isotopic composition and flux of particulate organic matter in the Changjiang [J].Acta Oceanology Sinica,1998,17:337-342. [7] Wu Y, Zhang J, Liu S M, et al. Sources and distribution of carbon within the Yangtze River system [J].Estuarine Coastal and Shelf Science,2007,71:13-25. [8] Wu Y, Dittmar T, Ludwichowski K U, et al. Tracing suspended organic nitrogen from the Yangtze River catchments into the East China Sea [J].Marine Chemistry,2007,107:367-377. [9] Zhang J,Wu Y,Jennerjahn,T C, et al. Distribution of organic matter in the Changjiang (Yangtze River) Estuary and their stable carbon and nitrogen isotopic ratios: Implications for source discrimination and sedimentary dynamics [J].Marine Chemistry, 2007, 106:111-126. [10] Gao Jianhua,Wang Yaping,Pan Shaoming,et al. Source and Distribution of organic matter in seabed sediments of the Changjiang River estuary and its adjacent sea area [J].Acta Geographica Sinica,2007,62(9):981-991. [高建华,汪亚平,潘少明,等.长江口外海域沉积物中有机物的来源及分布 [J].地理学报,2007,62(9): 981-991.] [11] Lü Xiaoxia,Zhai Shikui,Niu Lifeng.Study on the C/N ratios of orgaic matters in the core sediments of the Yangtze River Estuary [J].Environmental Chemistry,2005,24(3):255-259. [吕晓霞,翟世奎,牛丽凤.长江口柱状沉积物中有机质C/N比的研究 [J].环境化学,2005,24(3):255-259.] [12] Chen Qingqiang, Meng Yi, Zhou Juzhen,et al. Constraints for distribution of soil organic carbon with depth due to evolution of the salt marsh in the Yangtze River Estuary [J].Advances in Earth Science,2007,22(1):26-32. [陈庆强,孟翊,周菊珍,等.长江口盐沼滩面发育对有机碳深度分布的制约 [J].地球科学进展,2007,22(1):26-32.] [13] Zhao Yiyang,Yan Mingcai. Geochemistry of Sediments of the China Shelf Sea [M].Beijing:Science Press,1994:203. [赵一阳,鄢明才.中国浅海沉积物地球化学 [M].北京:科学出版社,1994:203.] [14] Fan Dejiang,Yang Zuosheng,Sun Xiaogong,et al. Quantitative evaluation of sediment provenance on the north area of the East China Sea Shelf [J].Journal of Ocean University of Qingdao,2002:748-756. [范德江,杨作升,孙效功,等.东海陆架北部长江、黄河沉积物影响范围的定量估算 [J].青岛海洋大学学报,2002:748-756.] [15] Wu Ying, Zhang Jing, Zhang Zaifeng, et al. Seasonal variability of stable carbon and nitrogen isotope of suspended particulate matter in the Changjiang River [J].Oceanologia et Limnologia Sinica,2002,33(5):546-552. [吴莹,张经,张再峰,等.长江悬浮颗粒物中稳定碳、氮同位素的季节分布 [J].海洋与湖沼,2002,33(5):546-552.] [16] Cai Deling, Tan F C, Edmond J M. Organic carbon isotope geochemistry of the Changjiang (Yangtze River) estuary [J].Geochimica,1992,(3):305-312. [蔡德陵,Tan F C,Edmond J M.长江口区有机碳同位素地球化学 [J].地球化学,1992,(3):305-312.] [17] Minoura K, Hoshino K, Nakamura T, et al. Late Pleistocene—Holocene paleoproductivity circulation in the Japan Sea: Sea-level control on δ13C and δ15N records of sediment organic material [J].Palaeogeography, Palaeoclimatology Palaeoecology,1997,135:41-50.
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