[1] (1)Martin R L, et al.Distribution of n - paraffines in Crude oilsand their implication to origin of petroleum.Nature, 1963,199: 110~113.

(2) Powell T G, et al.The g eochemical characterization of Aus-tralian crude oils.Aust pet Expl Assoc J, 1972, 55: 125~131.

(3)Illich H A, et al.Comment on “ comparison of Michigan Basincrude oil ” by Vogler et al., Geochim.Cosmochim.Acta,1983, 47: 1157~1159.

(4) Fowler M G, et al.Distribution and structure of hydrocarbonsin four organic rich Ordovician rocks.Org.Geochem., 1984,6: 105~114.

(5)Reed J D, et al.Biochemical evolutionary significance of Or-dovician oils and their sources.Adv ances in O rganic Geochem-istry, 1986, 347~358, Pergamon Press, Ox ford.

(6) Rullko tter J, et al.Oil generation in the Michigan Basin: a bi-ological marker and stable isotope approach.Advances in Or-ganic Geochemistry, 1986, 359 ~375, Pergamon Press, Ox-ford.

(7) Longman M W, et al.Organic geochemistry of mid-continentMiddle and Late Ordovician oils, APACE, 1987, 71: 227~242.

(8)Hoffmann G F, et al.Hydrocarbon biomarkers from Ordovi-cian sediments and the fossil alga Gloeocapsomorpha prisca Za-lessky 1917, Geochim.Cosmochim.Acta, 1987, 51: 2681~2697.

(9) Derenne S, et al.Characterization of Estonian Kukersite byspectroscopy and pyrolysis: Evidence for abundant alky Ⅰphenolic moieties in an Ordovician, marine, type Ⅱ ' Ⅰ kero-g en, Org.Ceochem., 1990, 16: 875~888.

(10) Huang Difan, et al.The geochemical characteristics of ma-rine oils in China.The papers of petroleum g eology to 30th In-ternational Geological Congress(In Press).

(11) 黄第藩等.塔里木盆地满加尔油气系统下古生界油源油中蜡质烃来源的成因分析.第六届全国有机地球化学会议论文摘要集, 1996.

(12) 黄第藩等.下古生界海相原油中含蜡的成因— 干酪根热解分析的证据.沉积学报, 1996, 14(2): 12~20.

(13) Foster C B, et al.Hydrocarbon source potential of the Gold-wyer Formation, Barbwire Terrace, Canning Basin, WesternAustralia, Aust.Pet.Expl.Assoc.J.1986, 26: 142~155.

(14) Traverse A.Occurrence of the oil-forming alga Botryococousin lig nites and other Tertiary sediments, Micropaleontology,1955, 1: 343~350.

(15)Stasiuk L D, et al.Organic microfacies and basinal tectoniccontrol on source rock accumulation: a microscopic approachwith examples from an intracratonic and extensional basin, Ⅰnt.J.Coal Geol., 1991, 19: 457~481.

(16) Moldowan J M, et al.Head- to- head linked isoprenoid hy-drocarbons in petroleum, Science, 1979, 204: 169~171.

(17)Chappe B, et al.Molecular fossils of archaebacteria as selec-tive deg radation products of kerogeh, Advanced in OrganicGeochemistry, 1980, 265~274, Pergamon Press, Oxford.

(18) Chappe B, et al.Polar lipids of archaebacteria in sedimentsand petroleum.science, 1982, 217: 65~66.

(19)Albaiges J.Identification and geochemical sig nificance of longchain acyclic isoprenoid hydrocarbons in crude oils, Advancesin Organic Geochemistry, 1980, 19~28, Pergamon, Ox fo rd.

(20) 华阿新,黄等藩,徐永昌等.华北中、上元古界有机质成烃作用及生物标记化合物特征.中国科学院兰州地质研究所生物、气体地球化学开放研究实验室研究年报 (1988~1989),兰州:甘肃科学技术出版社, 1989, 10~43.

(21) Petrov A A, et al.Isoprenoid alkanes with irreg ular “ head-to- head ” linkages, Org.Geochem., 1990, 16: 1001~1005.

(22) 张水昌等.海洋古细菌化石.地球科学, 1993, 18: 381~392.

(23)Durisson G, et al.The hopanoids.Palaeochemistry and bio-chemistry of a group natural products, Pure and AppliedChemistry, 1979, 51: 709~729.

(24) Rohmer M, et al.Distribution of hopanoid triterpenes inprokaryotes.J.Gen.Microbiol,1984, 30: 1137~ 1150.