高级搜索

留言板

尊敬的读者、作者、审稿人, 关于本刊的投稿、审稿、编辑和出版的任何问题, 您可以本页添加留言。我们将尽快给您答复。谢谢您的支持!

姓名
邮箱
手机号码
标题
留言内容
验证码

事件沉积及其周期性的氦同位素指示

叶先仁 任建国 陶明信 王宗礼

叶先仁, 任建国, 陶明信, 王宗礼. 事件沉积及其周期性的氦同位素指示[J]. 沉积学报, 2003, 21(4): 640-647.
引用本文: 叶先仁, 任建国, 陶明信, 王宗礼. 事件沉积及其周期性的氦同位素指示[J]. 沉积学报, 2003, 21(4): 640-647.
YE Xian ren, REN Jian guo, TAO Ming xin, WANG Zong li. Helium Isotope Tracing on Depositional Events[J]. Acta Sedimentologica Sinica, 2003, 21(4): 640-647.
Citation: YE Xian ren, REN Jian guo, TAO Ming xin, WANG Zong li. Helium Isotope Tracing on Depositional Events[J]. Acta Sedimentologica Sinica, 2003, 21(4): 640-647.

事件沉积及其周期性的氦同位素指示

基金项目: 国家自然科学基金(批准号:40173006)和气体地球化学国家重点实验室开放基金(2002-03WMB)资助
详细信息
    作者简介:

    叶先仁 男 1966 年出生 副研究员 地球化学

  • 中图分类号: P597

Helium Isotope Tracing on Depositional Events

  • 摘要: 物理、化学或生物事件所造成的事件沉积一般都会在沉积层中留下痕迹.事件沉积的突发性使得不同物源的物质比如稀有气体He在尚未达到平衡时就被保存在沉积地层中.海底沉积物中地球4He的丰度受古大陆尘所支配,海底沉积物中的He主要源于3He/4He比率不足0.1Ra的大陆物质(Ra = 1.40×10-6,是空气的3He/4He比率)和3He/4He比率大于100Ra的地球外星际尘粒.计算表明:亚洲风成尘粒总的质量累积速率(mass accumulation rate,MAR)与4He通量之间有一个显著的相关性.由氧同位素变化所记录的冰期-间冰期循环的100 kyr周期的起始点与地壳4He通量中100 kyr周期的起始点清晰地匹配.在大洋钻探计划中,用海底沉积物中地球外3He的通量来考查星际尘粒的全球生长速率发现:3He埋藏通量也与100 kyr冰期-间冰期循环周期相关.对白垩纪-第三纪界面(KTB)粘土中较高的地球外3He( [3He]Et)计算,发现该界面事件的短期性.来自中国梅山和日本西南部Sasayama的二叠纪-三叠纪界面(PTB)富勒烯的He同位素限定了这种富勒烯形成于地球外环境.在整个宇宙体系中,各物源之间的He及其同位素组成存在着很大差异,这为解析沉积事件提供了新的高灵敏度的手段.
  • [1] Aharon P, Goldstein S L, Wheeler C W, et al. Sea-level events in the South Pacific linked with the Messinian salinity crisis[J]. Geology, 1993, 21: 771~775
    [2] Alvarez W, Asaro F, Montanari A. Iridium profile for 10 million years across the Cretaceous-Tertiary at Gubbio (Italy)[J]. Science, 1990, 250: 1700~1702.
    [3] Becker L, Poreda R J, Bada J L. Extraterrestrial helium trapped in fullerenes in the Sudbury impact structure[J]. Science, 1996, 272: 249~252
    [4] Becker L, Poreda R J, Bunch Th E. Fullerenes: an extraterrestrial carbon carrier phase for noble gases[J]. Proc Natl Acad Sci USA, 2000, 97: 2979~2983.
    [5] Becker L, Poreda R J, Hunt A G, et al. Impact event at the Permian-Triassic boundary: Evidence from extraterrestrial noble gases in fullerenes[J]. Science, 2001, 291(5508): 1530~1533
    [6] Berger W H, Yasuda M K, Bickert T, et al. Quaternary timescale for the Ontong Java Plateau: Milankovitch template for Ocean Drilling Program Site 806[J]. Geology, 1994, 22:463~467
    [7] Bowring S A, Erwin D H, Jin Y G, et al. U/Pb zircon geochronology and tempo of the end-Permian mass extinction[J]. Science, 1998, 280: 1039~1045
    [8] Chuey J M, Rea D K, Pisias N G. Late Pleistocene paleoclimatology of the central equatorial Pacific: a quantitative record of eolian and carbonate deposition[J]. Quatary Research, 1987, 28: 323~339
    [9] Clemens S C, Prell W L. Late Pleistocene variability of Arabian Sea summer monsoon winds and continental aridity: Eolian records from the lithogenic component of deep-sea sediments[J]. Paleoceanography, 1990, 5:109~145
    [10] Erwin D H. The Permo-Triassic extinction[J]. Nature, 1994, 367: 231~236
    [11] Farley K A, and Patterson D B. A 100-kyr periodicity in the flux of extraterrestrial 3 He to the seafloor[J]. Nature, 1995, 378: 600~603
    [12] Farley K A, Montanari A, Schoemaker E M, et al. Geochemical evidence for a comet shower in the Late Eocene[J]. Science, 1998, 280: 1250~1252
    [13] Farley K A. Cenozoic variations in the flux of interplanetary dust recorded by 3 He in a deep-sea sediment[J]. Nature, 1995, 376:153~156
    [14] Herbert T D, D'Hondt S L. Precessional climate cyclicity in late Cretaceous-Tertiary boundary events[J]. Earth Planet Science Letter, 1990, 99: 263~275
    [15] Heymann D. Buckminsterfullerene, its siblings, and soot-carriers of trapped inert-gases in meteorites[J]. Journal of Geophysical Research, 1986, 91(B13): E135~138
    [16] Hofmann C, Feraud G, Courtillot V. 40 Ar/39Ar dating of mineral separates and whole rocks from the Western Ghats lava pile: further constraints on duration and age of the Deccan traps[J]. Earth Planet Science Letter, 2000, 180: 13~27
    [17] Hovan S A, Rea D K, Pisias N G. Late Pleistocene continental climate and oceanic variability recorded in northwest Pacific sediments[J]. Paleoceanography, 1991, 6: 349~298
    [18] Hovan S A, Rea D K, Pisias N G, et al. A direct link between the China loess and marine δ18O records: Aeolian flux to the north Pacific[J]. Nature, 1989, 340: 296~298
    [19] Hut P, Alvarez W, Elder W P, et al. Comet showers as a cause of mass extinctions[J]. Nature, 1987, 329: 118~126
    [20] Jin Y G, Wang Y, Wang W, et al. Pattern of marine mass extinction near the Permian-Triassic boundary in South China[J]. Science, 2000, 289: 432~436
    [21] Keller G, MacLeod N, Lyons J B, et al. Is there evidence for Cretaceous-Tertiary boundary-age deep-water deposits in the Caribbean and Gulf of Mexico[J]. Geology, 1993, 21: 776~780
    [22] Kutzbach J E, Guetter P J, Ruddiman W F, et al. Sensitivity of climate to late Cenozoic uplift in Southern Asia and the American West: Numerical experiments[J]. Journal of Geophysical Research, 1989, 94:18393~18407
    [23] Kyte F T, Leinen M, Heath G R, et al. Cenozoic sedimentation history of the central North Pacific: inference from the elemental geochemistry of Core LL44-GPC3[J]. Geochimica et Cosmochimica Acta, 1993, 57:1719~1740
    [24] Kyte F T. A meteorite from the Cretaceous/Tertiary boundary[J]. Nature, 1998, 396: 237~239
    [25] Marcantonio F, Anderson R F, Stute M, et al. Extraterrestrial 3 He as a tracer of marine sediment transport and accumulation[J]. Nature, 1996, 383: 705~707
    [26] Marcantonio F, Higgins S, Anderson R F, et al. Terrigenous helium in marine sediments: A provenance indicator. Eos, 1997, 78: F390
    [27] Middleton N J. Effect of drought on dust production in the Sahel[J]. Nature, 1985, 316: 431~434
    [28] Mukhopadhyay S, Farley K A, Montanari A. A 35 Myr record of helium in pelagic limestones from Italy: implications for interplanetary dust accretion from the early Maastrichtian to the middle Eocene[J]. Geochimica et Cosmochimica Acta, 2001, 65: 653~669
    [29] Mukhopadhyay S, Farley K A, Montanari A. A short duration of the Cretaceous-Tertiary boundary event: evidence from extraterrestrial helium-3[J]. Science, 2001, 291: 1952~1955
    [30] Muller R A, MacDonald G J. Glacial cycles and orbital inclination[J]. Nature, 1995, 377: 107~108
    [31] Muller R A, MacDonald G J. Glacial cycling and astronomical forcing[J]. Science, 1997, 277: 215~218
    [32] Muller R A, MacDonald G J. Simultaneous presence of orbital inclination and eccentricity in proxy climate records from Ocean Drilling Program Site 806[J]. Geology, 1997, 25: 3~6
    [33] Nier A O, Schlutter D J. Helium and neon isotopes in stratospheric particles[J]. Meteoritics, 1990, 25: 263~267
    [34] Officer C B, Hallam A, Drake C L, et al. Late Cretaceous and paroxysmal Cretaceous Tertiary extinctions[J]. Nature, 1987, 326: 143~149
    [35] Ozima M, Takayanagi M, Zashu S, et al. High 3 He/4He in ocean sediments[J]. Nature, 1984, 311: 449~451
    [36] Patterson D B, Farley K A, Norman M D. 4 He as a tracer of continental dust: A 1.9 million year record of Aeolian flux to the west equatorial Pacific Ocean[J]. Geochimica et Cosmochimica Acta, 1999, 63: 615~625
    [37] Patterson D B, Farley K A, Schmitz B. Preservation of extraterrestrial 3 He in 480-Ma-Old marine limestones[J]. Earth Planet Science Letter, 1998, 163: 315~325
    [38] Patterson D B, Farley K A. Extraterrestrial 3 He in seafloor sediments: Evidence for correlated 100kyr periodicity in the accretion rate of interplanetary dust, orbital parameters, and Quaternary climate[J]. Geochimica et Cosmochimica Acta, 1998, 62: 3669~3682
    [39] Prospero J M, and Tees R T. Impact of the North African drought and El Nino on mineral dust in the Barbados trade winds[J]. Nature, 1986, 320: 735~738
    [40] Rampino M R, Prokoph A, Adler A. Tempo of the end-Permian event: High-resolution cyclostratigraphy at the Permian-Triassic boundary[J]. Geology, 2000, 28: 643~646
    [41] Raup D M. Size of the Permo-Triassic bottleneck and its evolutionary implications[J]. Science, 1979, 206: 217~218
    [42] Rea D K, Leinen M, Janecek T R. Geologic approach to the long-term history of atmospheric circulation[J]. Science, 1985, 227: 721~725
    [43] Rea D K. The paleoclimatic record provided by eolian deposition in the deep sea: The geologic history of wind[J]. Review Geophysics, 1994, 32: 159~195
    [44] Renne P R, Zhang Z C, Richards M A, et al. Synchrony and causal relations between Permian-Triassic boundary crises and Siberian flood volcanism[J]. Science, 1995, 269: 1413~1416
    [45] Retallack G J, Seyedolali A, Krull E S, et al. Search for evidence of impact at the Permian-Triassic boundary in Antarctica and Australia[J]. Geology, 1998, 26: 979~982
    [46] Ruddiman W F, and Kutzbach J E. Forcing of late Cenozoic northern hemisphere climate by plateau uplift in Southern Asia and the American West[J]. Journal of Geophysical Research, 1989, 94: 18409~18427
    [47] Saunders M, Jimenez-Vazquez H A, Cross R J, et al. Stable compounds of helium and neon-He at the cost of C60 and Ne at the cost of C60[J]. Science, 1993, 259: 1428~1430
    [48] Sepkoski J J, Periodicity in extinction and the problem of catastrophism in the history of life[J]. Journal of Geological Sociaty of London, 1989, 146: 7~19
    [49] Shukolyukov A, Lugmair G W. Isotopic evidence for the Cretaceous-Tertiary impactor and its type[J]. Science, 1998, 282: 927~929
    [50] Takayanagi M, Ozima M. Temporal variation of 3 He/4He ratio recorded in deep-sea sediment cores[J]. Journal of Geophysical Research, 1987, 92: 12531~12538
    [51] Tiedemann R, Sarnthein M, Shackleton N J. Astronomic timescale for the Pliocene Atlantic δ18O and dust flux records of Ocean Drilling site 659[J]. Paleoceanography, 1994, 9: 619~638
    [52] Vischer H, Brinkhuis H, Dilcher D L, et al. The terminal Paleozoic fungal event: Evidence of terrestrial ecosystem destabilization and collapse[J]. Proc Natl Acad Sci USA, 1996, 93: 2155~2158
    [53] Ward P D, Montgomery D R, Smith R. Altered river morphology in South Africa related to the Permian-Triassic extinction[J]. Science, 2000, 289: 1740~1743
    [54] 孙明良, 陈践发. 真空电磁破碎器粉碎盐岩颗粒及稀有气体同位素组成测量的实验研究[J]. 沉积学报, 1998, 16(1): 103~106. [Sun Mingliang, Chen Jianfa. Study on the salt deposit crushing by the vacuum-electric-breaker and measurement of noble gas isotope composition[J]. Acta Sedimentologica Sinica, 1998, 16(1): 103~106]
    [55] 孙明良, 叶先仁. 固体样品中He、Ar同位素的质谱测定[J]. 沉积学报, 1997, 15(1): 48~53[Sun Mingliang, Ye Xianren. Measurement on He and Ar isotopic compositions in solid samples by mass spectrometry [J]. Acta Sedimentologica Sinica, 1997, 15(1): 48~53]
    [56] 王璞君, 刘万洙, 单玄龙,等. 事件沉积:导论实例应用[M]. 长春:吉林省科学技术出版社, 2001. 181[Wang Pujun, Liu Wanzhu, Shan Xuanlong, et al. Depositional Events: Introduction Example Application[M]. Changchun: Jilin Science & Technology Press, 2001, 181]
    [57] 王先彬. 稀有气体同位素地球化学和宇宙化学[M]. 北京:科学出版社, 1989. 451[Wang Xianbin. Noble gas isotope geochemistry and comoschemistry[M]. Beijing: Science Press, 1989. 451]
  • [1] 夏攀, 甯濛, 文华国, 郎咸国.  镁同位素示踪碳酸盐岩沉积—成岩过程 . 沉积学报, 2021, 39(6): 1546-1564. doi: 10.14027/j.issn.1000-0550.2021.112
    [2] 邱振, 邹才能.  非常规油气沉积学:内涵与展望 . 沉积学报, 2020, 38(1): 1-29. doi: 10.14027/j.issn.1000-0550.2019.116
    [3] 马帅, 陈世悦, 孙娇鹏, 贾贝贝, 王志金.  柴达木盆地北缘早古生代沉积—构造事件耦合关系 . 沉积学报, 2019, 37(4): 674-689. doi: 10.14027/j.issn.1000-0550.2018.171
    [4] 马强, 张殿伟, 王贵文, 朱东亚, 张荣强, 李天义.  断层流体锶、碳、氧同位素示踪评价断层垂向封闭性——以焦石坝背斜带为例 . 沉积学报, 2017, 35(6): 1205-1216. doi: 10.14027/j.cnki.cjxb.2017.06.012
    [5] 周锡强, 陈代钊, 刘牧, 胡建芳.  中国沉积学发展战略:沉积地球化学研究现状与展望 . 沉积学报, 2017, 35(6): 1293-1316. doi: 10.14027/j.cnki.cjxb.2017.06.020
    [6] 李文宝, 王汝建, 万随.  沉积过程中有机碳及Globigerinoides ruber氧、碳同位素变化特征——以南海南部为例 . 沉积学报, 2017, 35(4): 730-739. doi: 10.14027/j.cnki.cjxb.2017.04.007
    [7] 程红光, 李心清, 黄思静, 王兵, 程建中.  腕足壳体与碳酸盐岩全岩中碳、氧、锶同位素差异 . 沉积学报, 2015, 33(1): 60-66. doi: 10.14027/j.cnki.cjxb.2015.01.006
    [8] 长江上游水系沉积物锶—钕同位素组成及物源示踪 . 沉积学报, 2014, 32(2): 290-295.
    [9] 南海表层沉积物与沉降颗粒物中有机碳的δ13C对比研究及其古环境再造意义 . 沉积学报, 2012, 30(2): 340-345.
    [10] 秦黎明.  新疆西北部和什托洛盖盆地侏罗系低熟煤系烃源岩地球化学特征及生烃条件分析 . 沉积学报, 2009, 27(4): 740-751.
    [11] 袁文芳, 陈世悦, 曾昌民.  渤海湾盆地古近纪海侵问题研究进展及展望 . 沉积学报, 2005, 23(4): 604-612.
    [12] 冯建辉, 任战利, 崔军平, 任来义, 马维民, 孙明良.  东濮凹陷杜桥白地区天然气气源岩分析 . 沉积学报, 2003, 21(2): 350-354.
    [13] 孙省利, 曾允孚.  西成矿化集中区热水沉积岩物质来源的同位素示踪及其意义 . 沉积学报, 2002, 20(1): 41-46.
    [14] 张玉宾.  由恐龙化石论晚白垩世事件沉积 . 沉积学报, 1998, 16(2): 124-128.
    [15] 邓云山, 吴志勇, 吉利民, 阎存凤.  准噶尔盆地东北缘二叠纪地层时代划分 . 沉积学报, 1996, 14(3): 97-102.
    [16] 张同伟, 陈践发, 王先彬, 邵波, 李春园.  天然气运移的气体同位素地球化学示踪 . 沉积学报, 1995, 13(2): 70-76.
    [17] 贾炳文, 郭成印.  冀东晚古生代煤系中火山碎屑岩研究 . 沉积学报, 1993, 11(1): 65-74.
    [18] 刘焕杰, 贾玉如, 龙耀珍, 何康林, 马宏英, 郭英海, 施健, 桑树勋.  海相成煤论进展 . 沉积学报, 1992, 10(3): 47-56.
    [19] 徐永昌, 沈平, 李玉成.  中国最古老的气藏——四川威远震旦纪气藏 . 沉积学报, 1989, 7(4): 3-13.
    [20] 刘焕杰, 贾玉如, 龙耀珍, 王宏伟.  华北石炭纪含煤建造的陆表海堡岛体系特点及其事件沉积 . 沉积学报, 1987, 5(3): 73-80.
  • 加载中
计量
  • 文章访问数:  568
  • HTML全文浏览量:  2
  • PDF下载量:  385
  • 被引次数: 0
出版历程
  • 收稿日期:  2003-01-14
  • 修回日期:  2003-05-15
  • 刊出日期:  2003-12-10

目录

    事件沉积及其周期性的氦同位素指示

      基金项目:  国家自然科学基金(批准号:40173006)和气体地球化学国家重点实验室开放基金(2002-03WMB)资助
      作者简介:

      叶先仁 男 1966 年出生 副研究员 地球化学

    • 中图分类号: P597

    摘要: 物理、化学或生物事件所造成的事件沉积一般都会在沉积层中留下痕迹.事件沉积的突发性使得不同物源的物质比如稀有气体He在尚未达到平衡时就被保存在沉积地层中.海底沉积物中地球4He的丰度受古大陆尘所支配,海底沉积物中的He主要源于3He/4He比率不足0.1Ra的大陆物质(Ra = 1.40×10-6,是空气的3He/4He比率)和3He/4He比率大于100Ra的地球外星际尘粒.计算表明:亚洲风成尘粒总的质量累积速率(mass accumulation rate,MAR)与4He通量之间有一个显著的相关性.由氧同位素变化所记录的冰期-间冰期循环的100 kyr周期的起始点与地壳4He通量中100 kyr周期的起始点清晰地匹配.在大洋钻探计划中,用海底沉积物中地球外3He的通量来考查星际尘粒的全球生长速率发现:3He埋藏通量也与100 kyr冰期-间冰期循环周期相关.对白垩纪-第三纪界面(KTB)粘土中较高的地球外3He( [3He]Et)计算,发现该界面事件的短期性.来自中国梅山和日本西南部Sasayama的二叠纪-三叠纪界面(PTB)富勒烯的He同位素限定了这种富勒烯形成于地球外环境.在整个宇宙体系中,各物源之间的He及其同位素组成存在着很大差异,这为解析沉积事件提供了新的高灵敏度的手段.

    English Abstract

    叶先仁, 任建国, 陶明信, 王宗礼. 事件沉积及其周期性的氦同位素指示[J]. 沉积学报, 2003, 21(4): 640-647.
    引用本文: 叶先仁, 任建国, 陶明信, 王宗礼. 事件沉积及其周期性的氦同位素指示[J]. 沉积学报, 2003, 21(4): 640-647.
    YE Xian ren, REN Jian guo, TAO Ming xin, WANG Zong li. Helium Isotope Tracing on Depositional Events[J]. Acta Sedimentologica Sinica, 2003, 21(4): 640-647.
    Citation: YE Xian ren, REN Jian guo, TAO Ming xin, WANG Zong li. Helium Isotope Tracing on Depositional Events[J]. Acta Sedimentologica Sinica, 2003, 21(4): 640-647.
    参考文献 (57)

    目录

      /

      返回文章
      返回