[1]Milliman J D, Meade R H. World wide delivery of river sediment to the ocean[J].Journal of Geology, 1983,91(1):1-21. [2]Wang Pinxian, et al. South China Sea Since 150ka[M]. Shanghai: Tongji University Press,1995.[汪品先,等.十五万年来的南海[M].上海:同济大学出版社,1995.] [3]Zhu Zhaoyu, Qiu Yan, Zhou Houyun, et al.A summary review of research progress on global change in the South China Sea[J].Journal of Geomechanics,2002,8(4):315-323.[朱照宇,邱燕,周厚云,等.南海全球变化研究进展[J].地球力学学报,2002,8(4):315-323.] [4]Huang C Y, Liew P M, Zhao M,et al.Deep sea and lake records of the Southeast Asian paleomonsoons for the last 25 thousand years[J].Earth and Planetary Science Letters,1997,146:59-72. [5]Jian Z, Huang B, Kuhnt W,et al.Late Quaternary upwelling intensity and East Asian monsoon forcing in the South China Sea[J].Quaternary Research, 2001,55:363-370. [6]Sun Donghuai, An Zhisheng, Su Ruixia, et al.Mathematical separation of grain size groups from sediments in paleoenvironment researching and its applications[J].Progress in Natural Science,2001,11(3):269-276.[孙东怀,安芷生,苏瑞侠,等.古环境中沉积物粒度组分分离的数学方法及其应用[J].自然科学进展, 2001,11(3):269-276.] [7]Prins M A, Postma G, Weltje G J. Controls on terrigenous sediments supply to the Arabian Sea during the late Quaternary: The Makran continental slope[J].Marine Geology,2000, 169: 351-371. [8]Weltje G J, Prins M A. Muddled or mixed? Inferring palaeoclimate from size distributions of deep-sea clastics[J].Sedimentary Geology,2003, 162: 39-62. [9]Sun Youbin, Gao Shu, Li Jun. Preliminary analysis of grain-size populations with environmentally sensitive terrigenous component in marginal sea setting[J].Chinese Science Bulletin,2003,48(2):184-187. [10]Boulay S, Colin C, Trentesaux A,et al. Mineralogy and Sedimentology of Pleistocene Sediment in the South China Sea (ODPSite1144)[R].Proceedings of the Ocean Drilling Program, Scientific Results,2003,184:1-21. [11]Liu Zhifei, Colin C, Trentesaux A, et al.Late Quaternary weathering and erosion of the eastern Tibetan Plateau and the Mekong Basin and East Asian monsoon evolution recorded by the sediments from the South China sea[J].Bulletin of Mineralogy, Petrology and Geochemistry,2005,24(1):30-38.[刘志飞,Colin C,Trentesaux A,等. 青藏高原东部及湄公河盆地晚第四纪风化剥蚀与东亚季风演化在南海中的记录[J]. 矿物岩石地球化学通报,2005,24(1):30-38.] [12]Tuo Shouting, Liu Zhifei, Zhao Quanhong, et al.The earliest Oligocene glacial maximum: Records from ODP Site 1265, South Atlantic[J].Earth Science—Journal of China University of Geosciences,2006,31(2):151-158.[拓守廷,刘志飞,赵泉鸿,等. 渐新世初大冰期事件:南大西洋ODP1265站的记录[J].地球科学——中国地质大学学报,2006,31(2):151-158.] [13]Xiang Rong, Yang Zuosheng, Guo Zhigang,et al.Paleoenvironmental implications of grain size component variations in the mud area south west of Cheju Island, ECS[J].Earth Science—Journal of China University of Geosciences,2005,30(5):582-588.[向荣,杨作升,郭志刚,等.济州岛西南泥质区粒度组分变化的古环境应用[J]. 地球科学——中国地质大学学报,2005, 30(5):582-588.] [14]Ye Fang, Liu Zhifei, Tuo Shouting, et al.Grain size record of terrigenous clast during mid-Pleistocene transition (0.78~1.0 Ma) in the northern South China sea[J].Marine Geology and Quaternary Geology,2007, 27(2):77-83.[叶芳,刘志飞,拓守廷,等.南海北部中更新世0.78~1.0 Ma期间的陆源碎屑粒度记录[J].海洋地质与第四纪地质,2007,27(2):77-83.] [15]Shao L, Li X H, Wei G J,et al.Provenance of a prominent sediment drift on the northern slope of the South China Sea[J].Science in China(Series D),2001,44: 919-925. [16]Liu Zhifei, Trentesaux A, Clemens S,et al.Quaternary clay mineralogy in the northern South China Sea(ODP Site1146):Implications for oceanic current transport and East Asian monsoon evolution[J].Science in China(SeriesD),2003,46(12):1 223-1 235. [17]Wang L, Sarnthein M, Erlenkeuser H,et al.East Asian monsoon climate during the Late Pleistocene: High-resolution sediment records from the South China sea[J].Marine Geology,1999,156(1/4): 245-284. [18]Chen Longxun, Zhu Qian'gen, Luo Huibang,et al.The East Asian Monsoon[M].Beijing:Meteorology Press,1991:28-61.[陈隆勋,朱乾根,罗会帮,等.东亚季风[M].北京:气象出版社,1991:28-61.] [19]Wang L,Sarnthein M,Grootes P M,et al.Millenial reoccurrence of century-scale abrupt events of East Asian monsoon: A possible heat conveyor for the global deglaciation[J].Paleoceanography,1999,14(6):725-731. [20]Pettke T, Halliday A, Hall C,et al.Dust production and deposition in Asia and the North Pacific Ocean over the past 12Ma[J].Earth and Planetary Science Letters,2000, 178:397-413. [21]Jones C, Halliday A, Rea D,et al.Neodymium isotopic variation in North Pacific modern silicate sediment and their significance of detrital REE contributions to sea water[J].Earth and Planetary Science Letters,1994,127:55-66. [22]Wehausen R, Brumsack H J.Astronomical forcing of the East Asian monsoon mirrored by the composition of Pliocene South China Sea sediments[J].Earth and Planetary Science Letters,2002, 201: 621-636. [23]Laskar J. The chaotic motion of the solar system:A numerical estimate of the size of the chaotic zones[J].Icarus,1990, 88:266-291. [24]Paillard D, Labeyrie L, Yiou P. Analyseries 1.0: A Macintosh software for the analysis of geographical time-series[J].EOS,1996,77:379. [25]Wang Shuyun, Lu Houyuan, Liu Jiaqi,et al. The early Holocence optimum inferred from a highresolution pollen record of Huguanyan Maar Lake in southern China[J].Chinese Science Bulletin,2007,52(20):2 829-2 836. [26]Sirocko F, Sarnthein M, Erlenkenkeuser,et al.Century-scale events in monsoonal climate over the past 24000 years[J].Nature,1993, 364:322-324. [27]Blunier T J, Chappellaz J, Schwander B,et al.Variations in atmospheric methane concentration during the Holocene epoch[J].Nature,1995, 374:46-49. [28]Porter S C,An Z. Correlation between climate events in the North Atlantic and China during the last glaciation[J].Nature,1995, 375:305-308. [29]Wang Y J, Cheng H, Edwards R L,et al.A high-resolution absolute-dated late Pleistocene monsoon record from Hulu Cave,China[J].Science,2001,294:2 345-2 348. [30]Dykoski C A, Edwards R L, Cheng H,et al.A high-resolution, absolute-dated Holocene and deglacial Asian monsoon record from Dongge Cave, China[J].Earth and Planetary Science Letters,2005,233(1/2):71-86. |