[1] Wang Pinxian, Jian Zhimin, Liu Zhifei. Interactions between the Earth spheres: Deep-sea processes and records(Ⅰ).Research progress and achivement[J]. Advances in Earth Science,2006,21(4):331-337.[汪品先,翦知湣,刘志飞.地球圈层相互作用中的深海过程和深海记录(Ⅰ):研究进展与成果[J].地球科学进展,2006,21(4):331-337.]
[2] Imbrie J, Berger A, Boyle E A, et al. On the structure and origin of major glaciation cycles, 2, the 100,000-year cycle[J].Paleoceanography,1993,8:699-735.
[3] Webster P J. The role of hydrological processes in ocean-atmosphere interaction[J]. Reviews of Geophysics, 1994, 32:427-476.
[4] Jian Z, Yu Y, Li B, et al. Phased evolution of the south-north hydrographic gradient in the South China Sea since the middle Miocene[J]. Palaeogeography, Palaeoclimatology, Palaeoecology,2006,230:251-263.
[5] Zhao P, Zhou X, Jian Z, et al. Modeling the Tropical Climate and the Impact of the Western Pacific SST at the Last Glacial Maximum[J]. Journal of Geophysical Research—Atmosphere,109, D08105, doi:10.1029/2003JD004095.2004.
[6] Liu Chuanlian, Cheng Xinrong. Exploring variations in upper ocean structure for the last 2 Ma of the Nansha area by means of calcareous mannofossils[J]. Science in China(Series D),2001,44(10):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(10):834-839.]
[7] 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 Micropaloentology,2005,54: 89-105.
[8] 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.
[9] Wang P, Clemens S, Beaufort L, et al. Evolution and variability of the Asian Monsoon System: Status of the art and outstanding issues[J]. Quaternary Science Reviews,2005,24:595-629.
[10] Wang P, Prell W, Blum P, et al. Proceeding, Ocean Drilling Program, Initial Reports 184[R]. ODP, Texas A&M, College Station, USA,2000.
[11] Wang Pinxian, Jian Zhimin, Zhao Quanhong, et al. Evolution of the South China Sea and monsoon history revealed in deep-sea records[J]. Chinese Science Bulletin,2003,48(23):2 524-2 535.
[汪品先, 翦知湣, 赵泉鸿,等.南海演变与季风历史的深海证据[J].科学通报,2003,48(21):2 228-2 239.]
[12] Jia Guodong, Peng P, Zhou Q, et al. Changes in terrestrial ecosystem since 30 Ma in East Asia: Isotopic evidence from black carbon in the South China Sea[J].Geology,2003,31:1 093-1 096.
[13] Guo Z T, Ruddiman W F, Hao Q Z, et al. Onset of Asian desertification by 22 Ma ago inferred from loess deposits in China[J]. Nature,2002,416:159-163.
[14] Sun X, Wang P. How old is the Asian monsoon system? Palaeobotanical records from China[J]. Palaeogeography, Palaeoclimatology, Palaeoecology,2005,222:181-222.
[15] Jian Z, Zhao Q, Cheng X, et al. Pliocene-Pleistocene stable isotope and paleoceanographic changes in the northern South China Sea[J]. Palaeogeography, Palaeoclimatology, Palaeoecology,2003,193:425-442.
[16] Liu Z, Trentesaux A, Clemens S C, et al. Clay mineral assemblages in the northern South China Sea: I mplications for East Asian monsoon evlution over the past 2 million years[J]. Marine Geology, 2003,201:133-146.
[17] Wang R, Clemens S, Huang B, et al. Late Quaternary paleoceanographic changes in the northern South China Sea (ODP Site 1146): radiolarian evidence[J]. Journal of Quaternary Science,2003,18(8):745-756.
[18] 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.
[19] Tian J, Wang P, Chen R, et al. Quaternary upper ocean thermal gradient variations in the South China Sea: Implications for east Asian monsoon climate[J]. Paleoceanography,2005,20, PA4007, doi:10.1029/2004PA001115.
[20] Wang Pinxian, Tian Jun, Cheng Xinrong, et al. Exploring cyclic changes of the ocean carbon reservoir[J]. Chinese Science Bulletin,2003,48(23):2 536-2 548.[汪品先, 田军, 成鑫荣,等.探索大洋碳储库的演变周期[J]. 科学通报,2003,48(21):2 216-2 227.]
[21] Tu Xia, Zheng Fan, Wang Jiliang, et al. An abrupt cooling event early in the last interglacial in the northern South China Sea[J]. Science in China(Series D),2001,44(10):865-870.[涂霞, 郑范, 王吉良,等.南海北部末次间冰期的突然降温事件[J]. 中国科学:D辑,2001,31: 823-827.]
[22] Luo Y, Su X, Jian Z, et al. Environmental change during the penultimate glacial cycle: A high-resolution pollen record from ODP Site 1144, South China Sea[J]. Marine Micropaloentology,2005,54:107-123.
[23] Yu K, Zhao J, Collerson K D, et al. Storm cycles in the last millennium recorded in Yongshu Reef, southern South China Sea[J]. Palaeogeography, Palaeoclimatology, Palaeoecology,2004,210(1):89-100.
[24] Tian J, Wang P, Cheng X, et al. Astronomically tuned Plio-Pleistocene benthic δ18O record from South China Sea and Atlantic-Pacific comparison[J]. Earth and Planetary Science Letters,2002,203:1 015-1 029.
[25] Wang P,Tian J,Cheng X,et al. Major Pleistocene stages in a carbon perspective:The South China Sea record and its global comparison[J]. Paleoceanography,2004,19,doi: 10.1029/2003PA000991.2004.
[26] Cramer B S, Wright J D, Kent D V, et al. Orbital climate forcing of δ13C excursions in the late Paleocene-early Eocene (chrons C24n-C25n)[J]. Paleoceanography,2003,18(4),1097, doi: 10.1029/2003PA000909.
[27] Wade B S,Pölike H. Oligocene climate dynamics[J].Paleoceanography,2004,19,4019,doi: 10.1029/2004PA001042.
[28] Holbourn A, Kuhnt W, Schulz M, et al. Impacts of orbital forcing and atmospheric carbon dioxide on Miocene ice-sheet expansion[J]. Nature,2005,438:483-487.
[29] Williams T, Kroon D, Spezzaferri S. Middle and upper Miocene cyclostratigraphy of downhole logs and short- to long-term astronomical cycles in carbonate production of the Great Bahama Bank[J]. Marine Geology,2002, 185:75-93.
[30] Wang P, Tian J, Cheng X, et al. Carbon reservoir change preceded major ice-sheet expansion at the Mid-Brunhes event[J]. Geology,2003,31:239-242.
[31] 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.
[32] Ruddiman W F. Earth's Climate: Past and Future[M]. New York: Freeman & Co.,2001:465.
[33] Wehausen R, Brumsack H J. As tronomical forcing of the East Asian monsoon mirrored by the composition of Pliocene South China Sea sediments[J].EPSL,2002,201:621-636.
[34] Haug G H, Sigman D M, Tiedemann R, et al. Onset of permanent stratification in the subarctic Pacific Ocean[J]. Nature,1999,401:779-782.
[35] Kemp A E S, Pike J, Pearce R B, et al. The "Fall dump" a new perspective on the role of a "shade flora" in the annual cycle of diatom production and export flux[J]. Deep-Sea Research II,2000,47:2 129-2 154.
[36] Shi Yafen, Liu X, Li B, et al. A very strong summer monsoon event during the 30-40 ka BP in the Qinhai-Xizang (Tibet) Plateau and its relation to precessional cycle[J]. Chinese Science Bulletin,1999,44:1 851-1 857.
[37] Linsley B. Oxygen-isotope record of sea level and climate variations in the Sulu Sea over the past 150,000 years[J]. Nature,1996,380:234-237.
|