[1] Prell W L. Oxygen and carbon isotope stratigraphy of the Quaternary of Hole 502B: Evidence for two modes of isotopic variability [J]. Initial Reports of the DSDP, 1982, 68: 455-464.
[2] Berger W H, Bickert T, Jansen E, et al. The central mystery of the Quaternary Ice Age [J]. Oceanus, 1993, 36: 53-56.
[3] Shackleton N J. The 100,000-year ice-age cycle identified and found to lag temperature, carbon dioxide, and orbital eccentricity [J]. Science, 2000, 289: 1 897-1 902.
[4] Wang Pinxian, Tian Jun, Cheng Xinrong. Transition of Quaternary glacial cyclicity in deep-sea records at Nansha, the South China Sea[J]. Science in China (Series D), 2001, 44: 926-933. [汪品先,田军,成鑫荣.第四纪冰期旋回转型在南沙深海的记录[J]. 中国科学:D辑,2001,31(10):793-799.]
[5] De Garidel-Thoron T, Rosenthal Y, Bassinot F, et al. Stable sea surface temperatures in the western Pacific warm pool over the past 1.75 million years [J]. Nature, 2005, 433:294-298.
[6] Wang P, Prell W L, Blum P, et al. Proceedings of the Ocean Drilling Program, Initial Reports 184 [M]. College Station, TX: Ocean Drilling Program, 2000.
[7] Wang Pinxian, Zhao Quanhong, Jian Zhimin, et al. Thirty million year deep-sea records in the South China Sea[J]. Chinese Science Bulletin, 2003,48(23):2 524-2 535.[汪品先, 赵泉鸿, 翦知湣, 等.南海三千万年的深海记录[J].科学通报,2003,48:2 206-2 215.]
[8] Tian J, Wang P, Cheng X. Development of the East Asian monsoon and North Hemisphere glaciation: Oxygen isotope records from the South China Sea[J]. Quaternary Science Review,2004,23:2 007-2 016.
[9] Tian J, Wang P, Cheng X. Responses of foraminiferal isotopic variations at ODP Site 1143 in the southern south China sea to orbital forcing[J]. Science in China (Series D), 2004, 47: 943-953.
[10] Xu Jian. Quaternary planktonic foraminiferal assemblages in the southern South China Sea and Paleoclimatic variations[D]. Shanghai:Tongji University, 2004. [徐建. 南海南部第四纪浮游有孔虫群与古气候变化[D].上海:同济大学,2004.]
[11] Liu Chuanlian, Cheng Xinrong. Exploring variations in upper ocean structure for the last 2 Ma of the Nansha area by means of calcareous nannofossils[J]. Science in China(Series D), 2001, 44: 905-911. [刘传联,成鑫荣.从超微化石看南沙海区近2 Ma海水上层结构的变化[J].中国科学:D辑,2001,31: 834-839.]
[12] Yang Lihong, Chen Muhong, Wang Rujian, et al. Radiolarian record to paleoecological environment change events over the past 1.2 MaBP in the southern South China Sea [J]. Chinese Science Bulletin,2002,47:1 478-1 483.[杨丽红,陈木宏,王汝建,等. 南海南部1.2 Ma BP以来古生态环境变化事件的放射虫记录[J].科学通报,2002,47:1 098-1 102.]
[13] Bühring C, Sarnthein M, Erlenkeuser H. Toward a high-resolution stable isotope stratigraphy of the last 1.1 million years: Site 1144, South China Sea[J]. Proceedings of the Ocean Drilling Program, Scientific Results, 2004, 184:1-29.
[14] Sun X, Luo Y, Huang F, et al. Deep-sea pollen from the South China Sea: Pleistocene indicators of east Asian monsoon[J]. Marine Geology, 2003, 201: 97-118.
[15] Zheng F, Li Q, Tu X, et al. A millennial scale planktonic foraminiferal record of mid-Pleistocene climate transition in the northern South China Sea[J]. Palaeogeography, Palaeoclimatology, Palaeoecology,2005, 223: 349-363.
[16] Clemens S C, Prell W L. Oxygen and carbon isotopes from Site 1146, northern South China Sea [J]. Proceedings of the Ocean Drilling Program, Scientific Results, 2003, 184:1-8.
[17] Huang Baoqi, Li Baohua, Jian Zhimin. Comparison of variations in upper water temperatures between the northern and southern South China Sea since 1.5 MaBP[J]. Marine Geology & Quaternary Geology, 2004, 24: 79-83. [黄宝琦, 李保华, 翦知湣. 1.5 Ma以来南海南北上部水体温度变化对比[J]. 海洋地质与第四纪地质, 2004, 24:79-83.]
[18] Thompson P R. Planktonic foraminifera in the West North Pacific during the past 150,000 years: Comparison of modern and fossil assemblages[J]. Palaeogeography Palaeoclimatology Palaeoecology, 1981, 35: 241-279.
[19] Jian Z, Wang P, Chen M, et al. Foraminiferal responses to major Pleistocene paleoceanographic changes in the southern South China Sea [J]. Paleoceanography, 2000, 15: 229-243.
[20] Shyu J-P, Chen M-B, Shieh Y-T, et al. A Pleistocene paleoceanographic record from the north slope of the Spratly Islands, southern South China Sea[J]. Marine Micropaleontology, 2001, 42: 61-93.
[21] Wang R, Abelmann A. Radiolarian responses to paleoceanographic events of the southern South China Sea during the Pleistocene [J]. Marine Micropaleontology, 2002, 46: 25-44.
[22] Berger W H, Bickert T, Schmidt H, et al. Quaternary oxygen isotope record of pelagic foraminifers: Site 806, Ontong Java Plateau[J]. Proceedings of the Ocean Drilling Program, Scientific Results, 1993, 130: 381-395.
[23] Cheng X, Huang B, Jian Z, et al. Foraminiferal isotopic evidence for monsoonal activity in the South China Sea: A present-LGM comparison [J]. Marine Micropaleontology, 2005, 54: 125-139.
[24] Xu J, Wang P, Huang B, et al. Response of planktonic foraminifera to glacial cycles: Mid-Pleistocene change in the southern South China Sea[J]. Marine Micropaleontology,2005, 54: 89-105.
[25] Zheng Fan, Li Qianyu, Chen Muhong, et al. Late Pleistocene paleoceanographic characteristics of the southern South China Sea since 500 ka[J]. Earth Science—Journal of University of China Geosciences, 2005, 30: 534-542. [郑范,李前裕,陈木宏,等.南海西南部晚更新世500ka以来的古海洋学特征[J]. 地球科学——中国地质大学学报,2005, 30: 534-542. ]
[26] 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: 245-284.
[27] Pflaumann U, Jian Z. Modern distribution patterns of planktonic foraminifera in the South China Sea and western Pacific: A new transfer technique to estimate regional sea-surface temperatures[J]. Marine Geology,1999, 156: 41-83.
[28] Li B, Wang J, Huang B, et al. South China Sea surface water evolution over the last 12 Myr: A south-north comparison from Ocean Drilling Program Sites 1143 and 1146[J]. Paleoceanography,2004,19:PA1009, doi:10.1029/2003PA000906.
[29] Ruddiman W F, Raymo M E, Martinson D G. Pleistocene evolution: Northern hemisphere ice sheet and North Atlantic Ocean [J]. Paleoceanography,1989, 4: 353-412.
[30] Schmieder F, von Dobeneck T, Bleil U. The Mid-Pleistocene climate transition as documented in the deep South Atlantic Ocean: Initiation, interimstate and terminal event[J]. Earth and Planetary Science Letters, 2000, 179: 539-549.
[31] Gong S Y, Mii H S, Wei K Y, et al. Dry climate near the western Pacific Warm Pool: Pleistocene caliches of the Nansha Islands, south China sea[J]. Palaeogeography Palaeoclimatology Palaeoecology, 2005, 226: 205-213.
[32] Raymo M E, Oppo D W, Flower B P, et al. Stability of North Atlantic water masses in face of pronounced climate variability during the Pleistocene [J]. Paleoceanography,2004,19: PA2008, doi:10.1029/2003PA000921.
[33] Shackleton N J, Berger A, Peltier W R. An alternative calibration of the lower Pleistocene timescale based on ODP Site 677[J]. Transactions of the Royal Society of Edinburgh Earth Science,1990,81:251-261.
[34] Rutherford S, D'Hondt S. Early onset and tropical forcing of 100,000-year Pleistocene glacial cycles[J]. Nature,2000,408: 72-75.
[35] Raymo M E, Oppo D W, Curry W. The mid-Pleistocene climate transition: A deep sea carbon isotopic perspective[J]. Paleoceanography,1997,12: 546-559.
[36] Wang P, Tian J, Cheng X, et al. Carbon reservoir changes preceded major ice-sheet expansion at the mid-Brunhes event [J]. Geology,2003, 31:239-242.
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