[1] J C Zachos,M W Wara,S Bohaty,et al.A transient rise in tropical sea surface temperature during the Paleocene-Eocene ther malmaxi-mum[J].Science,2003,302(5650):1551-1554.
[2] J Zachos,M Pagani,L Sloan,et al.Trends,rhythms,and aberrations in global climate 65 Ma to present[J].Science,2001,292(5517):686-693.
[3] B S Cramer,J R Toggweiler,J D Wright,et al.Ocean overturning since the Late Cretaceous:inferences from a new benthic foraminiferal isotope compilation[J].Paleoceanography,2009,24(4):43-47.
[4] S Morón,J M Feinberg,C Jaramillo,et al.Climate change during the Early Paleogene in the Bogotá Basin(Colombia)inferred from paleosol carbon isotope stratigraphy,major oxides,and environmental magnetism[J].Palaeogeography Palaeoclimatology Palaeoecology,2013,388(3):115-127.
[5] 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. Liu Zhifei,Hu Xiumian.Extreme climates eventsin the cretaceous and paleogene[J].Advance in Earth Sciences,2003,18(5):681-690.
[6] J P Kennett,L D Stott.Abrupt deep-sea warming,palae-oceanographic changes and benthic extinctions at the end of the Palaeocene[J].Nature,1991,353(6341):225-229.
[7] J Zachos,M Pagani,L Sloan,et al.Trends,rhythms,and aberrations in global climate 64Ma to Present[J].Science,2001,292(5517):686-693.
[8] C M John,N R Banerjee,F J Longstaffe,et al.Clay assemblage and oxygen isotopic constraints on the weathering response to the Paleocene-Eocene thermal maximum,east coast of North America[J].Geology,2012,40(7):591-594.
[9] 朱敏,丁仲礼,王旭,等.南阳盆地PETM事件的高分辨率碳同位素记录[J].科学通报,2010,55(24):2400-2405. Zhu Ming,Ding Zhongli,Wang Xu,et al.High-resolution carbon isotope record for the Paleocene-Eocene thernal maximum from the Nanyang basin,central china[J].Chinese Sci Bulletin,2010,55(24):2400-2405.
[10] BS Cramer,J R Toggweiler,J D Wright,et al.Ocean overturning since the Late Cretaceous:inferences from a new benthic foraminiferal isotope compilation[J].Paleoceanography,2009,24(4):43-47.
[11] M García,G Ercilla,B Alonso,et al.Sediment lithofacies,processes and sedimentary models in the Central Bransfi eld Basin,Antarctic Peninsula,since the Last Glacial Maximum[J],.Marine Geology,2011,290(1-4):1-16.
[12] C B Wan,D H Wang.Trend of Santonian(Late Cretaceous)atmospheric CO2 and global mean land surface temperature:Evidence from plant fossils[J].Science China Earth Sciences,2011,54(9):1138-1145.
[13] J F Neff,J W Hagadorn,D Sunderlin,et al.Sedimentology,facies architecture and chemostratigraphy of a continental high-latitude Paleocene-Eocene succession-The Chickaloon Formation,Alaska[J].Sedimentary Geology,2011,240(1):14-29.
[14] D E Penman,B H nisch,R E Zeebe,et al.Rapid and sustained surface ocean acidification during the Paleocene-Eocene Thermal Maximum[J].Paleoceanography,2014,29(5):357-369.
[15] H Kimura,Y Watanabe.Ocean anoxia at the Precambrian-Cambrian boundary[J].Geology,2001,29(1):995-998.
[16] P K Bijl,S Schouten,A Sluijs,et al.Early Palaeogene temperature evolution of the southwest Pacific Ocean[J],Nature,2009,461(7265):776-778
[17] 赵玉龙,刘志飞.古新-始新世最热事件对地球表层循环的影响及其触发机制[J].地球科学进展,2007,22(4):341-349. Zhao Yulong,Liu Zhifei.The Impacts of the Paleocene-Eocene Thermal Maxmium(PETM)Event on earth surface cycles and its trigger mechanism[J].Advances in Earth Science,2007,22(4):341-349.
[18] J C Zachos,G R Dickens,R E Zeebe.An early Cenozoic perspective on greenhouse warming and carbon-cycle dynamics[J].Nature,2008,451(2008):279-283.
[19] T J Bralower,D C Kelly,R M Leckie.Biotic effects of abrupt Paleocene and Cretaceous climate events[J].JOIDES Journal,2002,28(1):29-34.
[20] 陈柞伶,丁仲礼.古新世-始新世极热事件研究进展.第四纪研究[J],2011,31(6):937-950. Chen Zuolin,Ding Zhongli.A review on the Paleocene-Eocene thermal maximum[J].quaternary sciences,2011,31(6):937-950.
[21] 冯有良,周海民,任建业,等.渤海湾盆地东部古近系层序地层及其对构造活动的响应[J].中国科学:地球科学,2010,40(10):156-1376. Feng Youliang,Zhou Haimin,Ren Jianye,et al.Paleogene sequence stratigraphy in the east of the Bohai Bay Basin and its response to structural movement.Sci SinTerrae,2010,40(10):1356-1376.
[22] 谭先锋,王佳,雷丽丹,等.早古近纪陆相断陷型湖泊物质分异作用及其对"PETM"事件的响应:以济阳坳陷孔店组为例[J].地球科学,2016,41(11):1893-1908. Tan Xianfeng,Wang Jia,Lei Lidan,et al.Material differentiation and its response to the "PETM" event in continental fault Lake during the Early Paleogene period-Take the Kongdian Fm.of Paleogene in Jiyang Depression for Example[J].Earth Science,2016,41(11):1893-1908.
[23] 谭先锋,田景春,黄建红,等.陆相碎屑岩旋回沉积记录中的物质响应及聚集规律-以济阳坳陷王家岗地区古近系孔店组为例[J].石油与天然气地质,2013,34(3):332-341. Tan Xianfeng,Tian Jinchun,Huang Jianhong,et al.Material response and accumulation law in the Cyclic sedimentation record of Continental clastic-To the Jiyang Depression Wangjiagang Paleogene Kongdian as an example[J].Oil and Geology,2013,34(3):332-341.
[24] 谭先锋,蒋艳霞,李洁,等.济阳坳陷古近系孔店组高频韵律旋回沉积记录及成因[J].石油与天然气地质,2015,36(1):61-72. Tan Xianfeng,Jiang Yanxia,Li Jie,et al.Sedimentary record of high frequency cycles and its origin of kongdian formation of Paleogene in jiyang depression[J].Oil and Geology,2015,36(1):61-72.
[25] 谭先锋,田景春,林小兵,等.陆相断陷盆地深部碎屑岩成岩演化及控制因素:以东营断陷盆地古近系孔店组为例[J].现代地质,2010,24(5):934-944. Tan Xianfeng,Tian Jinchun,Lin Xiaobin,et al.Diagenetic evolution and controling factors of deep-seated clastic rocks in Terrestrial Fault-depressed Basin[J].Geoscience,2010,24(5):934-944.
[26] 谭先锋,冉天,罗龙,等.滨浅湖环境中"砂-泥"沉积记录及成岩作用系统-以济阳坳陷古近系孔店组为例[J].地球科学进展,2016,31(6):615-63. Tan Xianfeng,Ran Tian,Luo Long,et al.The"sand-mud"sedimentary record and its Diagenetic system in shore-shallow Lacustrine-A case study of Eocene Kongdian Formation in Jiyang Depression[J].Advances in Earth Science,2016,31(6):615-633.
[27] 韦恒叶.古海洋生产力与氧化还原指标[J].沉积与特提斯地质,2012,32(2):76-88. Wei Hengye.Ancient marine productivity and redox index[J].Sedimentary Geology and Tethyan Geology,2012,32(2):76-88.
[28] 邓宏文,钱凯.沉积地球化学与环境分析[M].兰州:甘肃科学技术出版社,1993,18-31. Deng Hongwen,Qian Kai.Sedimentary geochemistry and environmental analysis[M].Lanzhou:Gansu Science and Technology Press,1993,18-31.
[29] 常华进,储雪蕾,冯连君,等.氧化还原敏感微量元素对古海洋沉积环境的指示意义[J].地质论评,2009,55(1):91-99. Chang Huajin,Chu Xuelei,Feng Lianjun,et al.The indicative significance of redox sensitive trace elements to the paleo marine sedimentary environment[J].Geological Review,2009,55(1):91-99.
[30] 尹秀珍,万晓樵,司家亮.松辽盆地G-12井晚白垩世青山口组沉积时期古湖泊学替代指标分析[J].地质学报,2008,82(5):676-682. Yin Xiuzhen,Wan Xiaoqiao,Si Jialiang.Paleolimnological Proxies of Late Cretaceous Qingshankou Sedimentary Period from Wel l G12 in Songliao Basin[J].Acta Geologica Sinica,2008,82(5):676-682.
[31] 刘招君,孟庆涛,柳蓉.古湖泊学研究-以桦甸断陷盆地为例[J].沉积学报,2012,28(5):917-925. Liu Zhaojun,Meng Qingtao,Liu Rong.Paleolimnology study:Taking Huadian fault basin as an example[J].Acta Sedimentologica Sinica,28(5):917-925. |