[1]Integrated Ocean Drilling Program (IODP) Planning Sub-Committee (IPSC). Earth, Oceans and Life, IODP Initial Science Plan: 2003-2013[R].Translated by Marine Geology Key Laboratory of MOE, Tongji University. Shanghai: Tongji University Press, 2003.[IODP科学规划委员会.地球、海洋与生命,IODP初始科学计划:2003-2013[R].同济大学海洋地质教育部重点实验室译.上海:同济大学出版社,2003.] [2]Kennett J, Scott L. Abrupt deep sea warming, paleoceanographic changes and benthic extinctions at the end of the Paleocene[J].Nature,1991,353:319-322. [3]Liu Zhifei, Hu Xiumian. Extreme climates events in the Cretaceous and Paleogene[J].Advances in Earth Science,2003,18 (5):681-690.[刘志飞,胡修棉.白垩纪至早第三纪的极端气候事件[J].地球科学进展, 2003,18(5):681-690.] [4]Gingerich P. Environment and evolution through the Paleocene-Eocene thermal maximum[J].Trends in Ecology and Evolution,2006,21(5):246-253. [5]Cramer B, Kent D. Bolide summer: The Paleocene/Eocene thermal maximum as a response to an extraterrestrial trigger[J].Palaeogeography, Palaeoclimatology, Palaeoecology,2005, 224: 144-166. [6]Moran K, Backman J, Brinkhuis H, et al. The Cenozoic palaeoenvironment of the Arctic Ocean[J]. Nature,2006,441:601-605. [7]Zachos J, Wara M, Bohaty S, et al. A transient rise in tropical sea surface temperature during the Paleocene-Eocene thermal maximum[J].Science,2003,302(28):1 551-1 554. [8]Nunes F, Norris R. Abrupt reversal in ocean overturning during the Paleocene/Eocene warm period [J].Nature,2006, 439: 60-63. [9]Bowen G, Beerling D, Koch P, et al. A humid climate state during the Palaeocene/Eocene Thermal Maximum[J].Nature,2004, 432:495-499. [10]Crouch E,Heilmann-Clausen C, Brinkhuis H, et al. Global dinoflagellate event associated with the late Paleocene thermal maximum[J].Geology,2001,29:315-318. [11]Gibbs S, Bralower T, Bowen P, et al. Shelf and open-ocean calcareous phytoplankton assemblages across the Paleocene-Eocene Thermal Maximum: Implications for global productivity gradients[J].Geology,2006,34(4):233-236. [12]Lu G, Keller G. Ecological stasis and saltation: species richness change in planktic foraminifera during the late Paleocene to early Eocene, DSDP Site 577[J].Palaeogeography, Palaeoclimatology, Palaeoecology,1995,117:211-227. [13]Bains S, Norris R, Corfield R, et al. Termination of global warmth at the Palaeocene/Eocene boundary through productivity feedback[J].Nature,2000,407:171-174. [14]Kelly D, Bralower T, Zachos J, et al. Rapid diversification of planktonic foraminifera in the tropical Pacific (ODP Site 865) during the late Paleocene thermal maximum[J].Geology,1996,24(5):423-426. [15]Beerling D. Increased terrestrial carbon storage across the Palaeocene-Eocene boundary[J].Palaeogeography, Palaeoclimatology, Palaeoecology,2000,161:395-405. [16]Wing S, Harrigton G, Smith F, et al. Transient floral change and rapid global warming at the Paleocene-Eocene boundary[J].Science,2005,310:993-996. [17]Bowen G, Clyde W, Koch P, et al. Mammalian dispersal at the Paleocene/Eocene boundary [J].Science,2002,295:2 062-2 065. [18]Clyde W, Khan I, Gingerich P. Stratigraphic response and mammalian dispersal during initial India Asia collision: Evidence from the Ghazij Formation, Baluchistan, Pakistan [J].Geology, 2003,31(12):1 097-1 100. [19]Clyde W, Gingerich P. Mammalian community response to the latest Paleocene thermal maximum: An isotaphonomic study in the northern Bighorn basin, Wyoming [J].Geology,1998, 26(11):1 011-1 014. [20]Bains S, Corfield R, Norris R. Mechanisms of climate warming at the end of the Paleocene[J].Science,1999,285:724-727. [21]Dickens G, O'Neil J, Rea D, et al. Dissociation of oceanic methane hydrate as a cause of the carbon isotope excursion at the end of the Paleocene [J].Paleoceanography,1995,10:965-971. [22]Thomas D, Zachos J, Bralower T, et al. Warming the fuel for the fire: Evidence for the thermal dissociation of methane hydrate during the Paleocene-Eocene thermal maximum [J].Geology,2002,30(12):1 067-1 070. [23]Zachos J, Röhl U, Schellenberg S, et al. Rapid acidification of the ocean during the Paleocene-Eocene thermal maximum[J]. Science, 2005,308:1 611-1 615. [24]Eldholm O, Thomas E. Environmental impact of volcanic margin formation[J]. Earth and Planetary Science Letters,1993,117:319-329. [25]Bice K, Marotzke J. Numerical evidence against reversed thermohaline circulation in the warm Paleocene/Eocene ocean[J].Journal of Geophysical Research,2001,106:11 529-11 542. [26]Thomas D, Bralower T, Jones C. Neodymium isotopic reconstruction of late Paleocene-early Eocene thermohaline circulation[J].Earth and Planetary Science Letters,2003,209:309-322. [27]Bralower T, Thomas D, Zachos J, et al. High-resolution records of the late Paleocene thermal maximum and circum-Caribbean volcanism: Is there a causal link[J].Geology,1997,25(11):963-966. [28]Svensen H,Planke S, Malthe-S renssen A, et al. Release of methane from a volcanic basin as a mechanism for initial Eocene global warming[J].Nature,2004,429:542-545. [29]Lourens L, Sluijs A, Kroon D, et al. Astronomical pacing of late Palaeocene to early Eocene global warming events[J].Nature,2005, 435: 1 083-1 087. [30]Katz M, Cramer B, Mountain G, et al. Uncorking the bottle: What triggered the Paleocene/Eocene thermal maximum methane release[J].Paleocenography,2001,16(6):549-562. [31]Maclennan J, Jones S. Regional uplift, gas hydrate dissociation and the origins of the Paleocene-Eocene thermal maximum[J].Earth and Planetary Science Letters,2006, 245:65-80. [32]Kent D, Cramer B, Lanci L, et al. A case for a comet impact trigger for the Paleocene/Eocene thermal maximum and carbon isotope excursion[J].Earth and Planetary Science Letters, 2003, 211:13-26. [33]Higgins J, Schrag D. Beyond methane: Towards a theory for the Paleocene-Eocene thermal maximum[J].Earth and Planetary Science Letters,2006, 245:523-537. [34]Kurtz A, Kump L, Arthur M, et al. Early Cenozoic decoupling of the global carbon and sulfur cycles[J].Paleoceanography,2003, 18(4):1 090, doi: 10.1029/2003PA000908. |