吐哈盆地侏罗纪煤系油气主力源岩探讨

煤系地层中的石油主要来源于煤系泥岩还是煤层的问题是目前石油地质学家和地球化学家们争论的热点。本文以吐哈盆地台北凹陷为例,深入研究了侏罗纪煤系源岩和原油的地球化学特征,发现煤系泥岩很发育,中下,侏罗统暗色泥岩厚达４００－１０００ｍ,且生油潜力较高,主要生油层八道湾组热解生油潜量平均４ｍｇ／ｇ左右,西山窑组也在２ｍｇ／ｇ左右,目前钻井获得西山窑组一八道湾组的成熟度Ｒ０＝０．６％－１．３％,具备了形成油     

三种有机紫外吸收剂对菲律宾蛤仔(Ruditapes philippinarum)鳃组织抗氧化能力和细胞凋亡相关基因表达的影响

二苯甲酮-3 (BP-3)、4-甲基苄亚基樟脑(4-MBC)和4-甲氧基肉桂酸-2-乙基己酯(EHMC)是三种常用的有机紫外吸收剂, 在水环境中被频繁检出, 对水生生态系统安全构成潜在威胁。为探究三种有机紫外吸收剂对菲律宾蛤仔(Ruditapes philippinarum)鳃组织抗氧化响应和相关细胞凋亡基因的影响, 将蛤仔分别暴露于环境相关浓度的三种紫外吸收剂溶液中, 检测鳃组织抗氧化酶活性和细胞凋亡相关基因转录水平, 并通过第二代整合生物标志物响应法(IBRv2)对三种紫外吸收剂的生物毒性进行比较分析。结果显示, 三种紫外吸收剂短期暴露会诱导抗氧化响应提高抗氧化能力, 而长期高浓度暴露会导致抗氧化能力的降低。BP-3、4-MBC和EHMC可能通过启动线粒体途径和fas介导的死亡受体途径诱导菲律宾蛤仔鳃组织产生细胞凋亡。通过IBRv2分析发现, 在环境常见浓度1 μg/L的暴露水平下, 短期(1 d, 7 d)暴露时, BP-3对菲律宾蛤仔鳃组织表现出的综合毒性效应最强, 而随着暴露时间的延长(28 d), 三种紫外吸收剂表现出的综合毒性效应相近。研究结果为水环境中有机紫外吸收剂的生态风险评估提供了参考数据。     

辽西建昌盆地油页岩发育特征及沉积环境

辽西地区建昌盆地含有丰富的油页岩资源。利用野外露头、钻井和化验分析等资料,分析油页岩分布、岩石学特征、地球化学特征和沉积环境。研究表明：油页岩发育于下白垩统九佛堂组一段、二段和三段,共计9个矿组,九佛堂组三段油页岩平均含油率高、厚度大;建昌盆地油页岩平均含油率为5.15%,平均灰分质量分数可达81.9%,平均发热量为5.19 kJ/g,全硫质量分数低,属于中品位高灰分中高发热量低硫型油页岩,开发时对环境污染小;碱厂、五家子、九佛堂、七道泉子和敖汉旗大青山含矿区累计油页岩查明技术可采资源8.22×10⁸ t,油页岩油查明可回收资源3.17×10⁷ t,建昌盆地预测油页岩资源9.27×10¹⁰ t。有机地化特征显示,建昌盆地油页岩有机质丰度较高,有机质类型主要为Ⅰ型和Ⅱ₁型,成熟度较低,处于未成熟—低成熟阶段。九佛堂组时期气候温暖湿润,来源于陆地和湖泊的有机质大量沉积于淡水—咸水的湖泊中,水底为还原环境,有利于有机质的保存。     

The Biomarkers in the Mesoproterozoic Organic-rich Rocks of North China Craton: Implication for the Precursor and Preservation of Organism in the Prokaryotic Realm

Mesoproterozoic marine organic-rich rocks are widely distributed in the North China Craton,include the Gaoyuzhuang(GYZ),the Hongshuizhuang(HSZ),and the Xiamaling(XML)formations.According to the T;value and isomerisation ratio of C;homohopanes,the XML,HSZ,and GYZ samples were in low mature,mature and high mature stage,respectively.Biomarker distribution in extractable organic matter(EOM)of three Mesoproterozoic organic-rock samples in different maturity were analysed to reveal the organic precursor and preservation pathway of in the Mesoproterozoic Combined with gold-tube pyrolysates of three Mesoproterozoic samples,it could further illuminate the chemical composition of Mesoproterozoic kerogen,given excluding.The results indicated that the three formations were all deposited under reducing condition and their organic precursors mainly were some aquatic organisms.High content of rearranged hopanes was detected in EOM of XML and HSZ samples,whereas they were relatively low in the high mature GYZ sample.Contrast to that in EOM,the relative concentration of rearranged hopanes sharply decreased in the gold-tube pyrolysates of the XML kerogen,then slightly increased but was still significantly lower than the EOM of XML sample,which indicated that catalysis of clay minerals in the early diagenesis only changed the chemical composition of the unstable functional groups of the kerogen during the preservation.Due to the thriving heterotrophic microbes and low sink rate of particulate organic matter during the Mesoproterozoic,primary producers suffered extensive degradation during sinking process,only some resistant biopolymers lacking of lipid compounds survived from heterotrophic degradation,while heterotrophic microbes contained more proportion of organic precursors.Abundant pristane(Pr)and phytane(Ph)were only released in high mature stage because of the protection of the macromolecular structure of resistant biopolymers which prevented biomarkers from being altered by the thermal stress.The absence of 13α(n-alkyl)-tricyclic terpanes in the high matured hydrocarbon products also indicated the different precursors between different parts of Mesoproterozoic kerogen.The evolution of the biomarker composition and content of Mesoproterozoic kerogen showed some special characteristics differing from those of Phanerozoic kerogen.The total concentrations of hopanes displayed with an order of low mature stage>high mature stage>mature stage.Relative content of rearranged hopanes in the hydrocarbon generated in high mature stage was significantly lower than that in the low maturity stage.The ratios of Pr/n-C₁₇ and Ph/n-C₁₈ increased with thermal maturity,and the ratio of nC_21-/nC₂₂₊ decreased in the high maturity stage,thus displaying another order of mature stage>high maturity stage>low maturity stage.The unique preservation pathway of Mesoproterozoic organisms was attributed to the special evolution characteristics of biomarker distributions,which should be considered in the Mesoproterozoic marine environment and biological studies.