新近纪海相生物地层事件年龄新编NEW AGES FOR NEOGENE MARINE BIOSTRATIGRAPHIC EVENTS
李前裕,Lucas Lourens,汪品先
摘要(Abstract)：
介绍新近纪海相生物地层研究的新进展。2004年新的"国际地质年代表"以405ka偏心率长周期为基础来划分新近纪的主要地层界线,标志着轨道地层学时代的到来。新生代包括E1—E162偏心率长周期,底界的年龄为65.5±0.3Ma,其中新近纪有E1—E58周期,底界年龄为23.03Ma,并且根据天文调谐得出一系列新的古地磁年龄和生物事件年龄。由于这些新年龄,特别是接近新近纪底部的年龄与早期结果相差0.5Ma或更大,所以将其汇总介绍,以求与当前国际研究保持同步衔接,增强海洋新近纪高分辨率地层工作的准确性。
关键词(KeyWords)： 新近纪;偏心率周期;生物地层;钙质超微;浮游有孔虫;古地磁
基金项目(Foundation): 国家自然科学基金(No40576031、40476030和40321603);; 国家重大基础研究计划项目(G2000078500)资助
作者(Author): 李前裕,Lucas Lourens,汪品先
参考文献(References)：
- 安芷生,艾莉.2005.尚未完成的地质年代表——第四纪悬而未决的前程.地层学杂志,29(2):99—103
- 李前裕,田军,汪品先.2005.认识偏心率周期的地层古气候意义.地球科学,30(5):519—528
- 田军,汪品先,成鑫荣.2004.南沙ODP1143站有孔虫同位素变化对地球轨道驱动的响应.中国科学(D辑),34(5):452—460
- 田军,汪品先,成鑫荣,李前裕.2005.南海ODP1143站上新世至更新世天文年代标尺的建立.地球科学,30(1):31—39
- 汪品先,田军,成鑫荣,刘传联,徐建.2003a.探索大洋碳储库的演变周期.科学通报,48(21):2216—2227
- 汪品先,赵泉鸿,翦知,成鑫荣,黄维,田军,王吉良,李前裕,李保华,苏新.2003b.南海三千万年的深海记录.科学通报,48(21):2206—2215
- 汪品先,翦知,赵泉鸿,李前裕,王汝建,刘志飞,吴国?,邵磊,王吉良,黄宝琦,房殿勇,李建如,李献华,韦刚健,孙湘君,罗运利,苏新,茅绍智,陈木宏.2003c.南海演变与季风历史的深海证据.科学通报,48(21):2228—2239
- 王伟铭,邓涛.2005.新近系研究进展简介.地层学杂志,29(2):104—107
- 赵泉鸿,汪品先.1999.南海第四纪古海洋学研究进展.第四纪研究,(6):481—501
- An Zhi-sheng&Ai Li.2005.I mperfect geologic ti me scale——pendingfuture of the Quaternary.Journal of Stratigraphy,29(2):99—103
- Aubry M-P,Berggren W A,Van Couvering J,McGowran B,Pil-lans B&Hilgen F.2005.Quaternary:status,rank,defini-tion,survival.Episodes,28(2):118—120
- Berger W H,Bickert T&Jansen E.1993.The central mystery ofthe Quaternary Ice Age.Oceanus,36(4):53—56
- Berger W H&Jansen E.1994.Mid-Pleistocene cli mate shift:TheNansen connection.in:Johannessen O Met al.eds.The polaroceans and their role in shaping the global environment.Ameri-can Geophysical Vnion Geophysical Monograph,84:295—311
- Berggren W A,Kent D V,Swisher C CIII&Aubry M-P.1995.Arevised Cenozoic geochronology and chronostratigraphy.In:Berggren WA,Kent D V,Aubry M-P&Hardenbol J eds.Ge-ochronology,Ti me Scales and Global Stratigraphic Correlation.SEPMSpecial Publication,54:129—212
- Cande S C&Kent D V.1995.Revised calibration of the geomagnet-ic polarity ti me scale for the Late Cretaceous and Cenozoic.Journal of Geophysical Research,100(B4):6093—6095
- Gibbard P L,Smith A G,Zalasiewicz J A,Barry T L,Cantrill D,Coe A L,Cope J C W,Gale A S,Gregory F J,Powell J H,Rawson P F,Stone P&Waters C N.2005.What status forthe Quaternary.Boreas,34(1):1—6
- Gradstein F,Ogg J&Smith A eds.2004.A Geologic Ti me Scale2004.Cambridge:Combridge University Press.1—500
- Hodell D A,Charles C D&Ninnemann US.2000.Comparison ofinterglacial stages in the South Atlantic sector of the southernocean for the past450kyr:I mplications for Marine IsotopeStage MIS11.Global and Planetary Change,24(1):7—26
- I mbrie J,Boyle E,Clemens S C,Duffy A,Howard WR,Kukla G,Kutzbach J,Martinson D G,McIntyre A,Mix A C,MolfinoB,Morley J J,Peterson L C,Pisias N G,Prell WL,Raymo ME,Shackleton NJ&Toggweiler J R.1992.On the structureand origin of major glaciation cycles,1,Linear responses to Mi-lankovitch forcing.Paleoceanography,7(2):701—738
- I mbrie J,Berger A,Boyle E,Clemens S C,Duffy A,Howard WR,Kukla G,Kutzbach J,Martinson D G,McIntyre A,Mix A C,Molfino B,Morley J J,Peterson L C,Pisias N G,Prell WL,Raymo ME,Shackleton NJ&Toggweiler J R.1993.On thestructure and origin of major glaciation cycles,2,The100000-year cycle.Paleoceanography,8(6):699—735
- Laskar J,Robutel P,Joutel F,Gastineau1M,Correia A C M&Levrard B.2004.Alongtermnumerical solutionfor theinsola-tion quantities of the Earth Astron.Astrophysics,428:261—285
- Li Qian-yu,Tian Jun&Wang Pin-xian.2005.Recognizingthe stra-tigraphic and paleocli matic significance of the eccentricity cy-cles.Earth Sciences,30(5):519—528
- Lourens L J,Hilgen F J,Laskar J,Shackleton N J&Wilson D.2004.The Neogene Period.In:Gradstein F,Ogg J&Smith Aeds.A Geologic Ti me Scale2004.Cambridge:Cambridge Uni-versity Press.409—440
- Pillans B&Naish T.2004.Defining the Quaternary.QuaternaryScience Reviews,23(23-24):2271—2282
- Raffi I,Backman J,Fornaciari E,Palike H,Rio D,Lourens L&Hil-gen F.2006.Areview of calcareous nannofossil astrobiochrono-logy encompassingthe pass25million years.QuaternaryScienceReviews,25(23-24):3113—3137
- Shackleton NJ.2000.The100000-year ice-age cycle identified andfound to lag temperature,carbon dioxide and orbital eccentrici-ty.Science,289:1897—1902
- Tian Jun,Wang Pin-xian&Cheng Xin-rong.2004.Responses offoraminiferal isotopic variations at ODP Site1143inthe southernSouth China Sea to orbital forcing.Sciencein China(Series D),47(10):943—953
- Tian Jun,Wang Pin-xian,Cheng Xin-rong&Li Qian-yu.2005.Es-tablishment of the Plio-Pleistocene astronomical ti mescale ofODP Site1143,southern South China Sea.Earth Sciences,30(1):31—39
- Wade B S&Palike H.2004.Oligocene cli mate dynamics.Paleo-ceanography,19:PA4019,doi:10.1029/2004PA001042
- Wang P,Prell WL&Blum Pet al.eds.2000.Proceedings of theOcean Drilling Program,Initial Reports.184[CD-ROM].O-cean Drilling Program,Texas A&M University,College Sta-tion TX77845-9547,USA.
- Wang Pin-xian,Tian Jun,Cheng Xin-rong,Liu Chuan-lian&XuJian.2003a.Exploring cyclic changes of the ocean carbon reser-voir.Chinese Science Bulletin,48(23):2536—2548
- Wang Pin-xian,Zhao Quan-hong,Jian Zhi-min,Cheng Xin-rong,Huang Wei,Tian Jun,Wang Ji-liang,Li Qian-yu,Li Bao-hua&Su Xin.2003b.Thirty million year deep-sea records in theSouth China Sea.Chinese Science Bulletin,48(23):2524—2535
- Wang Pin-xian,Jian Zhi-min,Zhao Quan-hong,Li Qian-yu,WangRu-jian,Liu Zhi-fei,Wu Guo-xuan,Shao Lei,Wang Ji-liang,Huang Bao-qi,Fang Dian-yong,Li Jian-ru,Li Xian-hua,WeiGang-jian,Sun Xiang-jun,Luo Yun-li,Su Xin,Mao Shao-zhi&Chen Mu-hong.2003c.Evolution of the South China Sea andmonsoon history revealed in deep sea records.Chinese ScienceBulletin,48(23):2549—2561
- Wang Wei-ming&Deng Tao.2005.A general introduction to re-cent advance in Neogene studies.Journal of Stratigraphy,29(2):99—103
- Zhao Quan-hong&Wang Pin-xian.1999.Progress in QuaternaryPaleoceanography of the South China Sea:a review.Quaterna-ry Studies,(6):481—501
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