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Article Navigation >  Acta Sedimentologica Sinica  > 1995  >  13(4): 82-92

Li Jinggui, Fan Pu, Cui Mingzhong, Li Zhenxi, R. P. Philp, J. Allen. C20, C25 and C30 Highly Branched Isoprenoid Alkenes in The Branched and Cyclic Hydrocarbon Fractions of Qinghai Lake Sediments[J]. Acta Sedimentologica Sinica, 1995, 13(4): 82-92.
Citation: Li Jinggui, Fan Pu, Cui Mingzhong, Li Zhenxi, R. P. Philp, J. Allen. C20, C25 and C30 Highly Branched Isoprenoid Alkenes in The Branched and Cyclic Hydrocarbon Fractions of Qinghai Lake Sediments[J]. Acta Sedimentologica Sinica, 1995, 13(4): 82-92.
shu

C20, C25 and C30 Highly Branched Isoprenoid Alkenes in The Branched and Cyclic Hydrocarbon Fractions of Qinghai Lake Sediments

  • 1 Lanzhou Institute of Geology, Academia Sinica, Lanzhou 730000 China;

  • 2 University of Oklahoma, School of Geology and Geophysics, Norman, OK 73019 USA

  • Publish Date: 1995-12-10
  • The very abundant highly branched isoprenoid (HBI) alkenes (C20,C25 and C30) have been detected in four cores of Qinghai Lake recent sediments. This is the first report of these compounds in Chinese recent lake sediments. Diatoms may be the biological source of these sedimentary HBI alkenes.
  • [1] 1.Barrick R. C.，Hedges J. I. and Peterson M. L.(1980) Hydrocarbon geochemistry of the Puget Sound region-I.Sedimentary acydic hydrocarbons. Geochim. Cosmochim. Acta 44. 1349-1362.

    2.Barrick R. C. and Hedges J. I. (1981) Hydrocarbon geochemistry of the Puget Sound region-1 .Sedimentary diter-penoid, steroid and triterpenoid hydrocarbons. Geochim. Cosmochirn. Acta 45. 381-392.

    3.Belt S. T.，Cooke D. A.，Hird S. J. and Rowland S. (1994) Structural Determination of a highly branched Czs sedi-mentary isoprenoid biomarker by NMR spectroscopy and Mass spectrometry. J. ChPm. Snc.，Chem. Commurz. 2077-2078.

    4.Cranwell P..A. (1982) Lipids of aquatic sediments and sedimentary particulates. Prog. Lipid Res. 21,271-308.

    5.Hird S. J.，Evans R. and Rowland S. J. (1992) Isolation and characterization of sedimentary and synthetic highlybranched C20 and C25 monoenes. Mar. Chem. 37,117-129.

    6.Hoefs M. J. L.，Sinninghe Damste J. S. and de Leeuw J. W. (1995) A novel Cas highly branched isoprenoid polyene in recent Indian (kean sediments. prg Geochem. 23, 263-267.

    7.Kohnen M, E. L.，Sinninghe Damste J. S.，Rullkotter J.，ten Haven H. L. and de Leeuw J. W. (1990) Origin and transformation of C25 and C30 highly branched isoprenoid sulphur compounds, further evidence for the formation of or-ganically bound sulphur during early diagenesis. Gexhim. Cosrnochim. Acta 54,3053-3063.

    8.Nichols P. D.，Volkman J. K.，Palmisane A. C.，Smith G. A. and White D. C.(1988) Occurrence of an isoprenoid C25 diunsaturated alkene and high neutral lipid content in Antarctic sea-ice diatom communities. J. Phycol. 24, 90-96.

    9.Requejo A. G. and Quinn J. G. (1983) Geochemistry of C25 and C30 biogenic alkenes in sediments of the Narragansett Bay estuary. Geochim. Cosmochim. Acta 47, 1075-1090.

    10.Requejo A. G.，Quinn J. G.，Gearing J. N. and Gearing P. J. (1984) C25 and C30 biogenic alkenes in a sediment core from the upper anoxic basin of the Pettaquamscutt River (Rhode Island, U. S. A.).Org. Geochem. 7.1-10.

    11.Robson J. N. and Rowland S. J. (1986 ) Indentification of novel widely distributed sedimentary acycGc sesterter-penoids. Nazure 324. 561-563.

    12.Robson J. N. and Rowland S. J.(1988a) Synthesis of a highly branched Csosedimentary hydrocarbon. Tetrahedron Lett. 29, 3837-3840.

    13.Robson J. N. and Rowland S. J. (19886) Biodegradation of highly branched isoporenoid hydrocarbons; A possible ex-planation of sedimentary abundance. In Aduances in Ch}ganic Geochemistry 1987, Chog. Georhern. 13. 691-695.

    14.Rowland S. J.，Yon D. A.，Lewis C. A. and Maxwell J. R. (1985 ) Ocurrence of 2. 6. 10-trimethyl-7(3-methylbutyl)-dodecane and related hydrocarbons in the green alga Enteromorpha prolifera and sediments. Org.Geochem. 8, 207-213.

    15.Rowland S. J. and Robson. J. N. (1990) The widespread occurrence of highly branched acyclic C20. C25 and C30 hy-drocarbons in recent sediments and biota-a review. Mar. Erruvon. Res. 30.191-216.

    16.Sinninghe Damste J. S.，Van Koert E. R.，Kock-van Dalen A. C.，de leeuw J. W. and Schenck P. A. (1989) Char-acteri7ation of highly branched isoprenoid thiophenes occurring in sediments and immature crude oils. Org. Geochem.

    17.Sinninghe Damste J. S. and Rijpstra W. I. C. (1993) Identification of a novel C25 highly branched isoprenoid thiophenein sediments. Org. Geochcm. 20, 327-331.

    18.Volkman J. K.，Barrett S. M. and Dunstan G. A. (1994 ) C25 and C30 branched isoprenoid alkenes in laboratorycultures of two marine diatoms. (kg. Geochem. 21，407-413.

    19.Yon D. A.，Ryback G. and Maxwell J. R. (1982) 2. 6. 10-Trimethyl-7(3-methylbutyl) dodecane. a novelsedi-mentary biological marker compound, Tetrnhedrrm L.ett. 23, 2143-2146.

    20.Yruela I.，Barbe A. and Grimalt J. O. (1990) Determination of double bond position and geometry in Linear andhighly branched hydrocarbons and fatty acids from gas chromatography-mass spectrometry of epoxides and diols gen-erated by stereospecific resin hydration. J. Chrnmmtoqr. Sci. 28. 421-427.
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    Created with Highcharts 5.0.7Chart context menuAccess Area Distribution其他: 3.1 %其他: 3.1 %其他: 1.6 %其他: 1.6 %China: 0.6 %China: 0.6 %United States: 1.6 %United States: 1.6 %[]: 0.3 %[]: 0.3 %上海: 0.9 %上海: 0.9 %中卫: 0.6 %中卫: 0.6 %兰州: 0.3 %兰州: 0.3 %凉山: 0.3 %凉山: 0.3 %北京: 12.6 %北京: 12.6 %南京: 0.9 %南京: 0.9 %台州: 1.3 %台州: 1.3 %哥伦布: 1.3 %哥伦布: 1.3 %宣光: 0.3 %宣光: 0.3 %张家口: 1.3 %张家口: 1.3 %成都: 0.6 %成都: 0.6 %杭州: 1.6 %杭州: 1.6 %泉州: 0.3 %泉州: 0.3 %法兰克福: 0.3 %法兰克福: 0.3 %深圳: 0.3 %深圳: 0.3 %温州: 0.3 %温州: 0.3 %湖州: 0.3 %湖州: 0.3 %滨州: 0.3 %滨州: 0.3 %漯河: 0.3 %漯河: 0.3 %芒廷维尤: 6.6 %芒廷维尤: 6.6 %芝加哥: 0.3 %芝加哥: 0.3 %苏州: 0.6 %苏州: 0.6 %衢州: 1.3 %衢州: 1.3 %西宁: 57.9 %西宁: 57.9 %西安: 0.3 %西安: 0.3 %贵阳: 0.3 %贵阳: 0.3 %银川: 0.6 %银川: 0.6 %青岛: 0.6 %青岛: 0.6 %其他其他ChinaUnited States[]上海中卫兰州凉山北京南京台州哥伦布宣光张家口成都杭州泉州法兰克福深圳温州湖州滨州漯河芒廷维尤芝加哥苏州衢州西宁西安贵阳银川青岛
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  • Published:  1995-12-10

C20, C25 and C30 Highly Branched Isoprenoid Alkenes in The Branched and Cyclic Hydrocarbon Fractions of Qinghai Lake Sediments

  • 1 Lanzhou Institute of Geology, Academia Sinica, Lanzhou 730000 China;
  • 2 University of Oklahoma, School of Geology and Geophysics, Norman, OK 73019 USA
  • Publish Date: 1995-12-10

Abstract: The very abundant highly branched isoprenoid (HBI) alkenes (C20,C25 and C30) have been detected in four cores of Qinghai Lake recent sediments. This is the first report of these compounds in Chinese recent lake sediments. Diatoms may be the biological source of these sedimentary HBI alkenes.

Li Jinggui, Fan Pu, Cui Mingzhong, Li Zhenxi, R. P. Philp, J. Allen. C20, C25 and C30 Highly Branched Isoprenoid Alkenes in The Branched and Cyclic Hydrocarbon Fractions of Qinghai Lake Sediments[J]. Acta Sedimentologica Sinica, 1995, 13(4): 82-92.
Citation: Li Jinggui, Fan Pu, Cui Mingzhong, Li Zhenxi, R. P. Philp, J. Allen. C20, C25 and C30 Highly Branched Isoprenoid Alkenes in The Branched and Cyclic Hydrocarbon Fractions of Qinghai Lake Sediments[J]. Acta Sedimentologica Sinica, 1995, 13(4): 82-92.
shu

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