Banakar V, Galy A, Sukumaran N, et al. 2003. Himalayan sedimentary pulses recorded by silicate detritus within a ferromanganese crust from the Central Indian Ocean. Earth Planet Sci Lett, 205: 337-348
[8]
Barrett P. 2003. Palaeoclimatology: Cooling a continent. Nature, 421: 221-223
[9]
Berggren W A, Kent D V, Flynn J J. 1985. Jurassic to Paleogene: Part 2 Paleogene geochronology and chronostratigraphy. Geol Soc London Mem, 10: 141-195
[10]
Bolli H M, Saunders J B, Perch-Nielsen K. 1989. Plankton Stratigraphy: Volume 1, Planktic Foraminifera, Calcareous Nannofossils and Calpionellids. CUP Archive
[11]
Bukry D. 1973a. Coccolith stratigraphy, eastern equatorial Pacific, Leg 16, Deep Sea Drilling Project. Initial Reports of the Deep Sea Drilling Project, 16: 653-711
[12]
Bukry D. 1973b. Phytoplankton stratigraphy, deep sea drilling project leg 20, western Pacific Ocean. Init Repts DSDP, 20: 307-317
[13]
Bukry D. 1975. Coccolith and silicoflagellate stratigraphy, northwestern Pacific Ocean. Deep Sea Drilling Project Leg 32. Init Repts DSDP, 32: 677-701
[14]
Bukry D. 1978. Biostratigraphy of Cenozoic marine sediment by calcareous nannofossils. Micropaleontology, 24: 44-60
[15]
Clouard V, Bonneville A. 2005. Ages of seamounts, islands, and plateaus on the Pacific plate. Special Papers-Geol Soc Am, 388: 71
[16]
Cowen J P, DeCarlo E H, MCGee D L. 1993. Calcareous nannofossil biostratigraphic dating of a ferromanganese crust from Schumann Seamount. Mar Geol, 115: 289-306
[17]
Coxall H K, Wilson P A, P?like H, et al. 2005. Rapid stepwise onset of Antarctic glaciation and deeper calcite compensation in the Pacific Ocean. Nature, 433: 53-57
[18]
Dallai L, Ghezzo C, Longinelli A. 2001. Fossil hydrothermal systems tracking Eocene climate change in Antarctica. Geology, 29: 931-934
[19]
DeConto R M, Pollard D. 2003. Rapid Cenozoic glaciation of Antarctica induced by declining atmospheric CO2. Nature, 421: 245-249
[20]
Dupont-Nivet G, Krijgsman W, Langereis C G, et al. 2007. Tibetan plateau aridification linked to global cooling at the Eocene-Oligocene transition. Nature, 445: 635-638
[21]
Edwards A, Perch-Nielsen K. 1975. Calcareous nannofossils from the southern southwest Pacific. Init Repts DSDP, 29: 469-540
[22]
Eisenhauer A, G?gen K, Pernicka E, et al. 1992. Climatic influences on the growth rates of Mn crusts during the Late Quaternary. Earth Planet Sci Lett, 109: 25-36
[23]
Elderfield H. 2002. Carbonate mysteries. Science, 296: 1618-1621
[24]
Gartner S. 1977. Nannofossils and biostratigraphy: An overview. Earth-Sci Rev, 13: 227-250
[25]
Hein J R, Bohrson W A, Schulz M S, et al. 1992. Variations in the fine-scale composition of a central Pacific ferromanganese crust: Paleoceanographic implications. Paleoceanography, 7: 63-77
[26]
James P C, Eric H D C, Donald L M. 1993. Calcareous nannofossil biostratigraphic dating of a ferromanganese crust from Schumann Seamount. Mar Geol, 115: 289-306
[27]
Janin M C. 1987a. The Imprints of Cenozoic Calcareous Nannofossils from Polymetallic Concretions: Biostratigraphic Significance for two Crusts from the Central Pacific (Line Islands Ridge and Mid-Pacific Mountains). Abh Geol, 39: 121-141
[28]
Janin M. 1987b. Micropaleontology of polymetallic concretions from the central Pacific: Clarion-Clipperton zone, Mid-Pacific Mountains, Line Islands and Tuamotu Archipelago (Eocene-Recent). Mem Soc géol FrSer, 152: 315
[29]
Jeong K, Jung H, Kang J, et al. 2000. Formation of ferromanganese crusts on northwest intertropical Pacific seamounts: Electron photomicrography and microprobe chemistry. Mar Geol, 162: 541-559
[30]
Katz M E, Miller K G, Wright J D, et al. 2008. Stepwise transition from the Eocene greenhouse to the Oligocene icehouse. Nature Geosci, 1: 329-334
[31]
Matsuoka A. 1992. Jurassic-Early Cretaceous tectonic evolution of the Southern Chichibu terrane, southwest Japan. Paleogeogr Paleoclimatol Paleoecol, 96: 71-88
[32]
McMurtry G, VonderHaar D, Eisenhauer A, et al. 1994. Cenozoic accumulation history of a Pacific ferromanganese crust. Earth Planet Sci Lett, 125: 105-118
[33]
Melnikov M E, Pulyeva I A. 1994. Ferromanganese crusts of Markus- Wake Rise and Magellan Seamounts of the Pacific Ocean (in Russian). Tikhooceanskaya Geologia, 4: 13-27
[34]
Meng J, McKenna M C. 1998. Faunal turnovers of Palaeogene mammals from the Mongolian Plateau. Nature, 394: 364-367
[35]
Miller K G, Wright J D, Fairbanks R G. 1991. Unlocking the ice house: Oligocene-Miocene oxygen isotopes, eustasy, and margin erosion. J Geophys Res (1978-2012), 96: 6829-6848
[36]
Okada H, Bukry D. 1980. Supplementary modification and introduction of code numbers to the low-latitude coccolith biostratigraphic zonation. Mar Micropaleontol, 5: 321-325
[37]
Pagani M, Zachos J C, Freeman K H, et al. 2005. Marked decline in atmospheric carbon dioxide concentrations during the Paleogene. Science, 309: 600-603
[38]
Pearson P N, Foster G L, Wade B S. 2009. Atmospheric carbon dioxide through the Eocene-Oligocene climate transition. Nature, 461: 1110-1113
[39]
Pearson P N, McMillan I K, Wade B S, et al. 2008. Extinction and environmental change across the Eocene-Oligocene boundary in Tanzania. Geology, 36: 179-182
[40]
Prothero D R. 1994. The late Eocene-Oligocene extinctions. Annu Rev Earth Planet Sci, 22: 145-165
[41]
Prothero D R. 1999. Does climatic change drive mammalian evolution. GSA Today, 9: 1-5
[42]
Retallack G J, Orr W N, Prothero D R, et al. 2004. Eocene-Oligocene extinction and paleoclimatic change near Eugene, Oregon. Geol Soc Am Bull, 116: 817-839
[43]
Ridgway K, Sweet A. 1995. Climatically induced floristic changes across the Eocene-Oligocene transition in the northern high latitudes, Yukon Territory, Canada. Geol Soc Am Bull, 107: 676-696
[44]
Roth P. 1973. Calcareous nannofossils. Init Repts DSDP, 17: 695-795
[45]
Salamy K A, Zachos J C. 1999. Latest Eocene-Early Oligocene climate change and Southern Ocean fertility: Inferences from sediment accumulation and stable isotope data. Paleogeogr Paleoclimatol Paleoecol, 145: 61-77
[46]
Shumenko S. 1987. Calcareous Nanoplankton(in Russia). Moscow: Nedra
[47]
Tripati A, Backman J, Elderfield H, et al. 2005. Eocene bipolar glaciation associated with global carbon cycle changes. Nature, 436: 341-346
[48]
Van Andel T H. 1975. Mesozoic/Cenozoic calcite compensation depth and the global distribution of calcareous sediments. Earth Planet Sci Lett, 26: 187-194
[49]
Williams M. 2007. Deep-time perspectives on climate change: Marrying the signal from computer models and biological proxies. Geol Soc London
[50]
Zachos J, Pagani M, Sloan L, et al. 2001. Trends, rhythms, and aberrations in global climate 65 Ma to present. Science, 292: 686-693
[51]
Zachos J C, Dickens G R, Zeebe R E. 2008. An early Cenozoic perspective on greenhouse warming and carbon-cycle dynamics. Nature, 451: 279-283
[52]
Zachos J C, Quinn T M, Salamy K A. 1996. High-resolution (104 years) deep-sea foraminiferal stable isotope records of the Eocene-Oligocene climate transition. Paleoceanography, 11: 251-266
[53]
Zhang H S, Zhao J, Han Z B, et al. 2013. Calcareous nannofossils and molecular fossils in cobalt-rich crusts and their response to the P/E global event. Acta Geol Sin, 87: 1264-1274
[54]
刘怀宝, Watkins D K. 2004. 北美西部内陆海盆Niobrara组的钙质超微化石及其环境意义Ⅱ: 古环境研究. 高校地质学报, 10: 26-38
[55]
刘志飞, Trentesaux A, Clemens S C, 等. 2003. 南海北坡ODP1146站第四纪粘土矿物记录: 洋流搬运与东亚季风演化. 中国科学D辑: 地球科学, 33: 271-280
Koppers A P, Morgan J P, Morgan J W, et al. 2001. Testing the fixed hotspot hypothesis using 40Ar/39Ar age progressions along seamount trails. Earth Planet Sci Lett, 185: 237-252
[63]
Lear C H, Bailey T R, Pearson P N, et al. 2008. Cooling and ice growth across the Eocene-Oligocene transition. Geology, 36: 251-254
[64]
Liu Z, Alain T, Steven C C, et al. 2003. Quaternary clay mineralogy in the northern South China Sea (ODP Site 1146)—Implications for oceanic current transport and East Asian monsoon evolution. Sci China Ser-D Earth Sci, 46: 1223-1235
[65]
Liu Z, Pagani M, Zinniker D, et al. 2009. Global cooling during the Eocene-Oligocene climate transition. Science, 323: 1187-1190
[66]
Müller R D, Roest W R, Royer J Y, et al. 1997. Digital isochrons of the world''s ocean floor. J Geophys Res (1978-2012), 102: 3211-3214
[67]
Marino M, Flores J A. 2002. Middle Eocene to early Oligocene calcareous nannofossil stratigraphy at Leg 177 Site 1090. Mar Micropaleontol, 45: 383-398
[68]
Martini E. 1971. Standard Tertiary and Quaternary calcareous nannoplankton zonation. In: Proceedings of the Second Planktonic Conference, Roma. 739-785
[69]
Martini E, Worsley T. 1970. Standard Neogene calcareous nannoplankton zonation. Nature, 225: 289-290
[70]
Martini E, Worsley T. 1971. Tertiary calcareous nannoplankton from the western equatorial Pacific. Init Repts DSDP, 7: 1471-1511