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.