[1] | Ravelo A C,Fairbanks R G,Philander G.1990.Reconstructing tropical Atlantic hydrography using planktonic foraminifera and ocean model[J].Paleoeanography,5: 409-431.
|
[2] | Raymo M E,Oppo D W,Curry W.2005.The mid-Pleistocene climate transition: A deep sea carbon isotopic perspective[J].Plaeoceanography,12: 546-559.
|
[3] | Robinson M M,Dowsett H J,Dwyer G S, et al.2008.Reevaluation of Mid-Pliocene North Atlantic sea surface temperatures[J].Paleoceanography,23,doi: 10.1029/2008PA001608.
|
[4] | Ruddiman W F.2006.What is the timing of orbital-scale monsoon changes?[J].Quaternary Science Reviews,25(8): 657-658.
|
[5] | Scroxton N,Bonham S G, et al.2010.Stable isotope ratios on foraminifera from site 846[J].Proc.ODP Sci.Results,138: 104-111.
|
[6] | Shackleton N J,Hall M A.1995.Application to Leg 138 sites[J].Proc.ODP Sci.Results,138: 73-101.
|
[7] | Shackleton N J,Berger A,Peltier W R.1990.An alternative astronomical calibration of the lower Pleistocene timescale based on ODP Site 677[J].Proc.ODP Sci.Results,131: 251-261.
|
[8] | Shackleton N J,Imbrie J,Hall M A.1983.Oxygen and carbon isotope record of East Pacific core V19-30: Implications for the formation of deep water in the late Pleistocene North Atlantic[J].Earth Planet Sci.Lett.,65: 233-244.
|
[9] | Shevenell A E,Kennett J P,Lea D W.2004.Middle Miocene southern ocean cooling and Antarctic cryosphere expansion[J].Science,305: 1766-1770.
|
[10] | Sun X J,Luo Y L,Huang F, et al.2003.Deep sea pollen from the South China Sea:Pleistocene indicators of East Asian monsoon[J].Marine Geology,201: 97-118.
|
[11] | Wang P,Tian J,Cheng X.2001.Transition of Quaternary glacial cyclicity in deep-sea records at Nansha,South China Sea[J].Science in China(Series D),44: 926-933.
|
[12] | Wara M W, Ravelo A C, Delaney M L. 2005.Permanent El Nino-like conditions during the Pliocene warm period[J].Science,309: 758-761.
|
[13] | Weissert H,Lini A,Follmi K B, et al.1998.Correlation of Early Cretaceous carbon isotope stratigraphy and platform drowning events:A possible link?[J].Palaeoceangraphy,137: 189-203.
|
[14] | Xu J,Kuhnt W,Holbourn A, et al.2006.Changes in the vertical profile of the Indonesian throughflow during termination Ⅱ: Evidence from the Timor Sea[J].Paleoceanography,21,doi: 10.1029/2006PA001278.
|
[15] | Yan X H,Zheng Q A, et al.1992.Temperature and size variabilities of the western Pacific warm pool[J].Science,258: 1643-645.
|
[16] | Zachos J S,Pagani M,Sloan L, et al. 2001.Trends,rhythms,and aberrations in global climate 65Ma to present[J].Science,292: 686-693.
|
[17] | 郭建卿,成鑫荣,陈荣华.2010.西太平洋暖池区上新世以来浮游有孔虫氧同位素特征及古海洋学变化[J].海洋地质与第四纪地质,30(3): 88-94.
|
[18] | 金海燕,翦知湣,成鑫荣.2006.赤道西太平洋暖池中更新世过渡期的古海洋变化[J].海洋地质与第四纪地质,26(2): 71-78.
|
[19] | 李前裕,李保华,钟广法.2006.晚中新世西太平洋暖池的浮游有孔虫和氧同位素证据[J].地球科学——中国地质大学学报,31(36): 754-761.
|
[20] | 刘传联,成鑫荣,王汝建.2005.西太平洋暖池区第四纪钙质超微化石氧碳同位素特征及意义[J].地球科学——中国地质大学学报,30(5): 560-564.
|
[21] | 马文涛.2009.晚上新世赤道太平洋气候转型和北极冰盖扩张的轨道驱动[J].科学通报,54(22): 3538-3544.
|
[22] | 田军,汪品先,成鑫荣,等.2005.南海ODP1143站上新世至更新世天文年代标尺的建立[J].地球科学——中国地质大学学报,30(1): 31-39.
|
[23] | 张江勇,金海燕.2008.赤道西太平洋晚第四纪生产力变化:ODP807A孔的变化[J].地球科学——中国地质大学学报,32(3): 304-311.
|
[24] | Beaufort L,De Garidel-Thoron T,Linsley B K, et al.2003.Biomass burning and oceanic primary production estimates in the Sulu Sea area over the last 380 kyr and the East Asian monsoon dynamics[J].Marine Geology,201: 53-65.
|
[25] | Cane M A.1998.A role for the tropical Pacific[J].Science,282: 59-61.
|
[26] | Cane M,Evans M.2000.Do the tropics rule[J].Science,290: 1107-1108.
|
[27] | Danovaro R,DellAnno A,Corinaldesi C, et al.2008.Major viral impact on the functioning of benthic deep-sea ecosystems[J].Nature,454: 1084-1087.
|
[28] | Fedorov A V,Dekens P S,McCarthy M, et al.2006.The Pliocene paradox(Mechanisms for a permanent El Nio)[J].Science,312: 1485-1489.
|
[29] | Ferreri V,Weissert H,DArgenio B, et al. 1997.Carbon isotope stratigraphy: A tool for basin to carbonate platform correlation[J].Terra Nova,9: 57-61.
|
[30] | Herbert T D,Laura C P.2010.Tropical ocean temperatures over the past 3.5 million years[J].Science,328: 1530-1534.
|
[31] | Lawrence K T,Liu Z H,Herbert T D.2006.Evolution of the eastern tropical Pacific through Plio-Pleistocene glaciation[J].Science,312: 79-83.
|
[32] | Molnar P,Cane M A.2002.El Nios tropical climate and teleconnections as a blueprint for pre-Ice Age climates[J].Paleoceanography,17,doi: 10.1029/2001PA000663.
|
[33] | Philander S G,Fedorov A V.2003.Role of tropics in changing the response to Milankovich forcing some three million years ago [J]. Paleoceanography,18,doi:10.1029/2002PA000837.
|
[34] | Prentice M L,Friez J K,Simonds G G, et al.1993.Neogene trends in planktonic foraminifer δ18 O from site 807A core: Implications for global ice volume and western equatorial Pacific sea surface temperat ures[J].ODP Scientific Results, 130: 281-283,295-298.
|
[35] | Ravelo A C,Fairbanks R G.1992.Oxygen isotopic composition of multiple species of planktonic foraminifera: Recorders of the modern photic zone temperature gradient[J].Paleoeanography,6: 815-831.
|
[36] | Ravelo A C,Shackleton N J.1995.Evidence for surface-water circulation changes at site 851 in the eastern tropical Pacific Ocean[J].Proc.ODP Sci. Results.138: 503-514.
|
[37] | Ravelo A C,Andreasen D H,Lyle M, et al.2004.Regional climate shifts caused by gradual global cooling in the Pliocene epoch[J].Nature,429: 263-267.
|