[1] Zachos J C, Quinn T M, Salamy K A. High-resolution (104 years) deep-sea foraminiferal stable isotope records of the Eocene-Oligocene climate transition[J]. Paleoceanography, 1996, 11: 251-266.
[2] Zachos J C, Stott L D, Lohmann K C. Evolution of early Cenozoic marine temperatures[J]. Paleoceanography, 1994, 9(2): 353-387.
[3] Kennett J P, Shackleton N J. Oxygen isotopic evidence for the development of the psychrosphere 38 Ma ago[J]. Science, 1976, 260: 513-515.
[4] Tripati A, Backman J, Elderfield H, et al. Eocene bipolar glaciation associated with global carbon cycle changes[J]. Nature, 2005, 436: 341-346.
[5] Lawver L A, Gahagan L M. Evolution of Cenozoic seaways in the circum-Antarctic region[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2003, 198: 11-37.
[6] Coxall H K, Wilson P A, Palike H, et al. Rapid stepwise onset of Antarctic glaciation and deeper calcite compensation in the Pacific ocean[J]. Nature, 2005, 433: 53-57.
[7] Deconto R M, Pollard D. Rapid Cenozoic glaciation of Antarctica induced by declining atmospheric CO2[J]. Nature, 2003, 421: 245-249.
[8] Zachos J C, Kump L R. Carbon cycle feedbacks and the initiation of Antarctic glaciation in the earliest Oligocene[J]. Global and Planetary Change, 2005, 47: 51-66.
[9] Wang Pinxian, Tian Jun, Cheng Xinrong, et al. Exploring cyclic changes of the ocean carbon reservoir[J]. Chinese Science Bulletin, 2003, 48(23):2 356-2 548. [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.]
[10] Elderfield H. Carbonate mysteries[J]. Science, 2002, 296: 1 618-1 621.
[11] Broecker W S, Sanyal A. Magnitude of the CaCO3 dissolution events making the onset of times of glaciation[J]. Paleoceanography, 1997, 12: 530-532.
[12] Anderson D M, Archer D. Glacial-interglacial stability of ocean pH inferred from foraminifer dissolution rates[J]. Nature, 2002, 416:70-73.
[13] Shipboard Scientific Party. Leg 208 summary[C]∥Zachos J C, Kroon D, Blum P, et al. Proceeding Ocean Drilling Program Init Repts 208: College Station TX (Ocean Drilling Program), 2004:1-112.
[14] Tuo Shouting, Liu Zhifei, Zhao Quanhong, et al. The earliest Oligocene glacial maximum: Records from ODP site 1265, south Atlantic[J]. Earth Science,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ODP 1265站的记录[J].地球科学,2006,31(2): 151-158.]
[15] Diester-Haass L. Middle Eocene to early Oligocene paleoceanography of the Antarctic Ocean (Maud Rise, ODP Leg 113, Site 689): Change from a low to high productivity ocean[J]. Palaeogeography, Palaeoclimatology, Palaeocology, 1995, 113: 311-334.
[16] Stuut J B, Prins M, Schneider R, et al. A 300-kyr record of aridity and wind strength in southwestern Africa: Inferences from grain-size distributions of sediments on Walvis ridge, SE Atlantic[J]. Marine Geology, 2002, 180: 221-233.
[17] Liu Zhifei, Xu Jian, Tian Jun, et al. Calcium carbonate pump during Quaternary glacial cycles in the south China sea[J]. Chinese Science Bulletin, 2003, 48(17): 1 862-1 869. [刘志飞,徐建,田军,等.南海第四纪冰期旋回中的碳酸钙泵[J].科学通报, 2003, 48(9): 962-968.]
[18] Treguer P, Pondaven P. Silica control of carbon dioxide[J]. Nature, 2000, 406: 358-359.
[19] Liu Zhifei, Tuo Shouting, Zhao Quanhong, et al. Deep sea-water earliest Oligocene glacial maxmiun in south Atlantic[J]. Chinese Science Bulletin,2004,49(20): 2 190-2 197.[刘志飞,拓守廷,赵泉鸿,等.南大西洋深水渐新世初大冰期事件[J].科学通报, 2004, 49 (17):1 793-1 800.]
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