青藏高原的隆起与海洋锶同位素组成的演化

doi:10.11867/j.issn.1001-8166.1999.06.0582

近年来,随着构造隆升驱动气候变化假说的提出,青藏高原的隆起受到越来越多的关注,并将之与大陆化学风化速率及海洋锶同位素的演化紧密联系。围绕青藏高原的隆升及其环境与气候效应,对海洋锶同位素组成的演化特征及其影响因素的较为全面而详细的论述表明:将青藏高原的隆升与全球气候变化、大陆化学风化速率及海洋锶同位素组成的演化相联系,也许是解决目前关于海洋锶同位素组成的演化及其物源问题的重要手段,根据海洋锶同位素的演化历史来研究全球气候变化规律及青藏高原的构造演化历史将是本研究领域的重点。

关键词: 青藏高原隆起, 大陆化学风化速率, 海洋锶同位素组成

In the past few years, following the hypothesis of tectonically driven climate change, the uplift of Tibetan plateau receives increasing interest and is tightly connected with the rate of continental chemical weathering and the evolution of marine strontium isotope. This paper thoroughly and minutely discusses the influences of Tibet plateau uplift and the changes in the global environment and climate on marine Sr isotopic evolution and the possible factors influencing the evolution. It is an important approach to solve the problem of the evolution and sources of marine strontium isotope by combining the uplift of Tibetan plateau, the global climate change and the rate of continental chemical weathering. Research work in this field should be focused on the rules of global climate change and the tectonic evolution of Tibet plateau on the basis of the evolutionary history of marine strontium isotope.

Key words: Tibet plateau uplift, The rate of continental chemical weathering, Marine strontium isotopic composition.

中图分类号:

P542+.2
P597

〔1〕李吉均,文世宣,张青松,等.青藏高原隆升的时代、幅度和形式的探讨〔J〕.中国科学,1976,6:608～616.
〔2〕李吉均,方小敏.青藏高原隆升与环境变化研究〔J〕.科学通报,1998,43(15):1 569～1 574.
〔3〕Coleman M. Evidence for Tibetan uplift before 14 Ma ago from a new minimum age for east-west extension〔J〕. Nature, 1995,374:49～52.
〔4〕Kroon D ,Steens T N F ,Troelstra S R. Onset of monsoonal related upwelling in the western Arabian Sea〔J〕.Proc ODP,Sci Results,1991,17:257～263.
〔5〕Quade J, Cerling T E, Bowman J R. Development of Asian monsoon revealed by marked ecological shift during the Latest Miocene in north Pakistan〔J〕. Nature ,1989,342:163～166.
〔6〕Harrison T M, Copeland P,Kidd W S F,et al. Raising Tibet〔J〕. Science,1992,255(27):1 663～1 670.
〔7〕王彦斌,王军,王世成.高喜马拉雅地区聂拉木地区花岗岩快速抬升的裂变径迹证据〔J〕.地质论评,1998,44(4):430～434.
〔8〕钟大赉,丁林.青藏高原的隆起过程及其机制探讨〔J〕.中国科学(D辑),1996,26(4):289～301.
〔9〕施雅风,汤懋苍,马玉贞.青藏高原二期隆升与亚洲季风孕育关系探讨〔J〕.中国科学(D辑),1998,28(3):263～271.
〔10〕崔之久,高全洲,刘耕年,等.夷平面、古岩溶与青藏高原隆升〔J〕.中国科学(D辑),1996,26(4):278～285.
〔11〕王富葆,李升峰,申旭辉,等.吉隆盆地的形成演化、环境变迁与喜马拉雅山隆起〔J〕.中国科学(D辑),1996,20(4);329～335.
〔12〕中国科学院青藏高原综合考察队.青藏高原隆起的时代、幅度和形式问题〔M〕.北京:科学出版社,1981.
〔13〕中国科学院青藏高原综合考察队.西藏气候〔M〕.北京:科学出版社,1984.
〔14〕Kutzbach J E, Guetter P J, Ruddiman W F,et al. Sensitivity of climate to Late Cenozoic uplift in Southern Asia and the America West :numerical experiments〔J〕. Journal Geophysical Research, 1989,94(D15) :18 393～18 407.
〔15〕Birchfield G E, Weertman J. Topography, albedo-temperature feedback and climate sensitivity〔J〕. Science,1983,219:284～285.
〔16〕王建,席萍,刘泽纯,等.柴达木盆地西部新生代气候与地形演变〔J〕.地质论评,1996,42(2):166～173.
〔17〕滕吉文,张中杰,张秉铭,等.青藏高原的隆升与环境变化〔J〕.地学前缘,1997,4(2):247～254.
〔18〕安芷生,王苏民,吴锡浩,等.中国黄土高原的风积证据:晚新生代北半球大冰期开始及青藏高原的隆升驱动〔J〕.中国科学(D辑),1998,28(6):481～490.
〔19〕刘东生等著.黄土与环境〔M〕.北京:科学出版社,1985.
〔20〕吴锡浩、安芷生.黄土高原黄土—古土壤序列与青藏高原隆起〔J〕.中国科学(D辑),1996,26(2):103～110.
〔21〕刘东生,郑绵平,郭正堂.亚洲季风系统的起源和发展及其与两极冰盖和构造运动的时代耦合性〔J〕.第四纪研究,1998,8(3):194～204.
〔22〕王富葆,韩辉友,阎革,等.青藏高原东北部30 ka以来的古植被与古气候演变序列〔J〕.中国科学(D辑),1996,26(2):111～117.
〔23〕An Z S, Liu T S, Lu Y C,et al. The long-term paleomonsoon variation recorded by the loess-paleosoil sequence in central China〔J〕. Quaternary International, 1990,7/8:91～95.
〔24〕Palmer M R, Edmond J M. Controls over the strontium isotope composition of river water〔J〕. Geochimica et Cosmichimica Acta,1992, 56:2 099～2 111.
〔25〕Quade J, Roe L, DeCelles P G,et al. The late Neogene 87Sr/86Sr record of lowland Himalayan rivers〔J〕. Science,1997,276:1 828～1 831.
〔26〕Blum J D, Gazis C A, Jacobson A D,et al. Carbonate versus silicate weathering in the Raikhot watershed within the High Himalayan Crystalline Series〔J〕. Geology, 1998,26(5):411～414.
〔27〕Christlan F L, Derry L A. Organic carbon burial forcing of the carbon cycle from Himalayan erosion〔J〕. Nature, 1997,390(6):65～67.
〔28〕卢演俦,丁国瑜.与亚洲古季风有关的中国及邻区新生代构造演化的几个问题〔J〕.第四纪研究,1998,8(3):205～212.
〔29〕Ramstein G, Fluteanu F, Besse J,et al. Effect of orogeny,plate motion and land-sea distribution on Eurasian climate change over the past 30 million years〔J〕. Nature, 1997,386:788～795.
〔30〕福尔G,鲍威尔J L.锶同位素地质学〔M〕.北京:科学出版社,1975.
〔31〕Dia A N, Cohen A S, Nions R K O,et al. Seawater Sr isotope variation over the past 300 ka and influence of global climate cycles〔J〕. Nature, 1992, 356(30):786～788.
〔32〕Clemens S C, Farrell J W, Gromet L P. Synchronous changes in seawater strontium isotope composition and global climate〔J〕. Nature, 1993, 363(17):607～610.
〔33〕Palmer M P, Edmond J M. The strontium isotope budget of the modern ocean〔J〕. Earth and Planetary Science Letters,1989, 92:11～26.
〔34〕Edmond J M. Himalayan tectonics, weathering processes,and the strontium isotope record in marine limestones〔J〕.Science,1992, 258(4):1 594:1 597.
〔35〕刘英俊,曹励明,李兆麟,等.元素地球化学〔M〕.北京:科学出版社,1984.
〔36〕Miller E K, Blum J D, Friedland A J. Determination of soil exchangeable-cation loss and weathering rates using Sr Isotope〔J〕. Nature,1993, 362:438～441.
〔37〕Martin E E, Macdougall J D. Sr and Nd isotope at the Permain/Triassic boundary: A record of climate change〔J〕.Chemical Geology, 1995, 125:73～99.
〔38〕Richter F M, Rowley D B, DePaolo D J. Sr isotope evolution of seawater: the role of tectonics〔J〕. Earth and Planetary Science Letters, 1992, 109:11～23.
〔39〕Palmer M R, Elderfield H. Sr isotope composition of sea water over the past 75 Ma〔J〕. Nature, 1985,314(11):526～528.
〔40〕Hodell A D, Mueller P A, Garrido J R. Variations in the strontium isotopic composition of seawater during the Neogene〔J〕. Geology,1991(19):24～27.
〔41〕Hodell D A, Mueller P A, McKenzie J A,et al. Strontium isotope stratigraphy and geochemistry of the late Neogene ocean〔J〕. Earth and Planetary Science Letters,1989,(92):165～178.
〔42〕Capo R C, Depaolo D J. Seawater Strontium isotopic variations from 2.5 million years ago to the present〔J〕. Science,1990, 249:51～55.
〔43〕Hodell D A. Editorial: Progress and paradox in strontium isotope stratigraphy〔J〕. Paleoceanography, 1994, 9 (3):395～398.
〔44〕马英军,刘从强.地壳风化系统中的Sr同位素地球化学〔J〕.矿物学报,1998,18(3):350～358.
〔45〕Raymo M E, Ruddiman W F. Tectonic forcing of late Cenozoic climate〔J〕. Nature, 1992, 359(10): 117～122.
〔46〕Copeland P, Harrison T M. Episodic rapid uplift in the Himalaya revealed by40Ar/39Ar analysis of detrital K-feldspar and muscovite, Bengal fan〔J〕. Geology, 1990, 18: 354～357.
〔47〕Richter F M, Lovera O M, Harrison T M,et al. Tibetan tectonics from40Ar/39Ar analysis of a single K-feldspar sample〔J〕. Earth Planetary Science Letters, 1991,105(1):266～278.
〔48〕Zeitler P K. Cooling history of the NW Himalaya, Pakistan〔J〕. Tectonics, 1985,4(1):127～151.
〔49〕Chen Jun, An Zhisheng, John Head. Variation of Rb/Sr ratios in the loess-paleosol sequences of central China during the last 130 000 years and their implications for monsoon paleoclimatology〔J〕. Quarter Research, 1999, (in press).

[1]	吴运高,李继亮,樊敬亮. 造山带逆冲推覆构造研究的主要新进展[J]. 地球科学进展, 2000, 15(4): 426-433.

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摘要

TIBET PLATEAU UPLIFT AND THE EVOLUTION OF MARINE STRONTIUM ISOTOPIC COMPOSITION