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伽马蜡烷——水体分层的地球化学标志

张立平 黄第藩 廖志勤

张立平, 黄第藩, 廖志勤. 伽马蜡烷——水体分层的地球化学标志[J]. 沉积学报, 1999, 17(1): 136-140.
引用本文: 张立平, 黄第藩, 廖志勤. 伽马蜡烷——水体分层的地球化学标志[J]. 沉积学报, 1999, 17(1): 136-140.
Zhang Liping, Huang Difan, Liao Zhiqin. Gammacerane —Geochemical Indicator of Water Column Stratification[J]. Acta Sedimentologica Sinica, 1999, 17(1): 136-140.
Citation: Zhang Liping, Huang Difan, Liao Zhiqin. Gammacerane —Geochemical Indicator of Water Column Stratification[J]. Acta Sedimentologica Sinica, 1999, 17(1): 136-140.

伽马蜡烷——水体分层的地球化学标志

详细信息
    作者简介:

    张立平,女,31岁,博士,油气地球化学。

  • 中图分类号: P631.817

Gammacerane —Geochemical Indicator of Water Column Stratification

  • 摘要: 密执安盆地等海相蒸发环境伽马蜡烷的分布表明,伽马蜡烷作为咸水环境的生物标志化合物与高盐度环境并没有绝对的对应关系;松辽盆地淡水-微咸水环境较高含量的伽马蜡烷表明其形成与湖海沟通引起的水体分层事件有关。伽马蜡烷重碳同位素值及微生物学证据均表明了伽马蜡烷的形成与水体分层有关,由于高盐环境往往伴随着密度分层,从而解释了伽马蜡烷经常与高盐环境伴生,但并不仅仅局限于高盐环境的现象。
  • [1] 1 Hi lls I R, Whitehead E V, Anders D E, et al, An optically activetriterpane, gammacerane, in Green River, Colorado, oil shale bi tumen.J.Chem.Soc., Chem.Commun., 1966.752~754

    2 Peters K E, Moldowan J M.The Biomarker Guide :InterpretingMolecular Fossi ls in Pet roleum and Ancient Sediment s.Prentice Hall Inc, 1993.1~347

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    4 Kleemann G, Poralla K, Englert G, et a l.Tet rahymanol from the photot rophic bact erium Rhodopseudomonas palustr is :First report of a gammacerane trit erpene form a prokaryote.J.Gen.Microbiol.,1990,136 :2 551~2 553

    5 Ten Haven H L, Rohmer M, Rullkott er J, Tet rahymanol, the mostlikely precursor of gammacerane, occurs ubiqui tiously in marine sediment s.Geochim.Cosmochim.Act a, 1989, 53 :3 073~3 079

    6 Sinninghe,Damst e J S,Kenig F, Koopmans M P, et al.Evidence for gammacerane as an indicator of water column stratification.Geochim. Cosmochim.Acta, 1995 :59 :1895~1 900

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    8 Oehler J H.Carbonate Source rocks in the Jurassic Smackover trend of Mississippi,Alabama and Florida.In :Palacas J G.ed.Pet roleum Geochemist ry and S ource Rock Pot ential of Carbonate Rocks, AAPGS tudies in Geology, 1984, 18 :63~ 70

    9 Hughes W B, Holba A G, Dzou L I P.The rat ios of dibenzothiopheneto phenantherene and pristane to phytane as indicat ors of depositional environment and lithology of petroleum source rocks.Geochim.Cosmochim.Acta, 1995, 59(17):3 581~3 598

    10 Palacas J G, Anders D E, King J D.South Florida Basin-A prime example of carbonat e source rocks in pet roleum.In :Palacas J G, ed.Pet roleum Geochemist ry and Source Rock Pot ent ial of Carbonate Rocks, AAPG, Studies in Geology, 1984, 8 :71~96

    11 Dahl J, Moblowan J M, Sundararaman P.Relationship of biomarker dist ribution to depositional envi ronment :Phosphria Formation Mont ana, U.S.A Geochim.Cosmochim.Acta.1993, 20 :1001 ~1007

    12 Fu Jiamo, S heng Guoying, Peng Pingan, et al. Peculiarities of salt lake sediment s as pot ent ial source rock s in China.Organic Geochemistry, 1986, 10 :119~126

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    14 Wang Tieguan, Fan Pu, Swain F M.Geochemical characterist ics ofcrude oils and source beds in different continental f acies of four oilbearing basins,C hina.In :Keltsk, Fleet A, Talbot M, eds.Lacust rinePet roleum Source Rocks Blackwell, Oxford, 1988.299~308

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    17 叶淑芳, 魏魁生.松辽盆地白垩系的密集段及海水进侵的新证.地球科学, 1996, 21(3):267~271.

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出版历程
  • 收稿日期:  1998-06-08
  • 修回日期:  1998-07-20
  • 刊出日期:  1999-03-10

目录

    伽马蜡烷——水体分层的地球化学标志

      作者简介:

      张立平,女,31岁,博士,油气地球化学。

    • 中图分类号: P631.817

    摘要: 密执安盆地等海相蒸发环境伽马蜡烷的分布表明,伽马蜡烷作为咸水环境的生物标志化合物与高盐度环境并没有绝对的对应关系;松辽盆地淡水-微咸水环境较高含量的伽马蜡烷表明其形成与湖海沟通引起的水体分层事件有关。伽马蜡烷重碳同位素值及微生物学证据均表明了伽马蜡烷的形成与水体分层有关,由于高盐环境往往伴随着密度分层,从而解释了伽马蜡烷经常与高盐环境伴生,但并不仅仅局限于高盐环境的现象。

    English Abstract

    张立平, 黄第藩, 廖志勤. 伽马蜡烷——水体分层的地球化学标志[J]. 沉积学报, 1999, 17(1): 136-140.
    引用本文: 张立平, 黄第藩, 廖志勤. 伽马蜡烷——水体分层的地球化学标志[J]. 沉积学报, 1999, 17(1): 136-140.
    Zhang Liping, Huang Difan, Liao Zhiqin. Gammacerane —Geochemical Indicator of Water Column Stratification[J]. Acta Sedimentologica Sinica, 1999, 17(1): 136-140.
    Citation: Zhang Liping, Huang Difan, Liao Zhiqin. Gammacerane —Geochemical Indicator of Water Column Stratification[J]. Acta Sedimentologica Sinica, 1999, 17(1): 136-140.
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