闫晶晶. 吉林农安地区青山口组和嫩江组生物地层及古气候变化[D]. 北京:中国地质大学,2007. [Yan Jingjing. Mid-Cretaeeous biostratigraphy and palaeoclimate change from the Qingshankou and Nenjiang Formations in Nong'an area, Jilin province[D]. Beijing: China University of Geosciences, 2007.]
[2]
侯启军,冯志强,冯子辉. 松辽盆地陆相石油地质学[M]. 北京:石油工业出版社,2009:65-88. [Hou Qijun, Feng Zhiqiang, Feng Zihui. Continental Petroleum Geology in the Songliao Basin[M]. Beijing: Petroleum Industry Press, 2009: 65-88.]
[3]
王成善,冯志强,吴河勇,等. 中国白垩纪大陆科学钻探工程:松科一井科学钻探工程的实施与初步进展[J]. 地质学报,2008,82(1):9-20. [Wang Chengshan, Feng Zhiqiang, Wu Heyong, et al. Preliminary achievement of the Chinese Cretaceous: Continental scientific drilling project-SK-Ⅰ[J]. Acta Geologica Sinica, 2008, 82(1): 9-20.]
[4]
Wan X Q, Zhao J, Scott R W, et al. Late Cretaceous stratigraphy, Songliao Basin, NE China: SK1 cores[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2012, 385: 31-43.
[5]
王国栋,程日辉,王璞珺,等. 松辽盆地嫩江组白云岩形成机理-以松科1井南孔为例[J]. 地质学报,2008,82(1):48-54. [Wang Guodong, Cheng Rihui, Wang Pujun, et al. The forming mechanism of Dolostone of Nengjiang Formation in Songliao Basin-Example from CCSD-SK-1[J]. Acta Geologica Sinica, 2008, 82(1): 48-54.]
[6]
Emerson S, Hedges J I. Processes controlling the organic carbon content of open ocean sediments[J]. Paleoceanography, 1988, 3(5): 621-634.
[7]
Meyers P A, Doose H. Sources, preservation, and thermal maturity of organic matter in Pliocene-Pleistocene organic-carbon-rich sediments of the Western Mediterranean Sea[J]. Proceedings of the Ocean Drilling Program, Scientific Results, 1999, 161: 383-390.
[8]
Peters K E. Guidelines for evaluating petroleum source rock using programmed pyrolysis[J]. AAPG Bulletin, 1986, 70(3): 318-329.
[9]
Meyers P A, Yum J-G, Wise S W. Origins and maturity of organic matter in mid-Cretaceous black shales from ODP Site 1138 on the Kerguelen Plateau[J]. Marine and Petroleum Geology, 2009, 26(6): 909-915.
[10]
Song Z G, Yin Q, George S C, et al. A biomarker study of depositional paleoenvironments and source inputs for the massive formation of Upper Cretaceous lacustrine source rocks in the Songliao Basin, China[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2013, 385: 137-151.
[11]
王晓伏,王成善,金玮. 湖盆类型与烃源岩形成的关系研究新进展[J]. 大庆石油地质与开发,2011,30(1):1-6. [Wang Xiaofu, Wang Chengshan, Jin Wei. New research progress of relation between lake-basin types and formation of source rocks[J]. Petroleum Geology and Oilfield Development in Daqing, 2011, 30(1): 1-6.]
[12]
闫晶晶,席党鹏,于涛,等. 松辽盆地青山口地区嫩江组下部生物地层及环境变化[J]. 地层学杂志,2007,31(3):296-302. [Yan Jingjing, Xi Dangpeng, Yu Tao, et al. Biostratigraphy and paleoenvironmental change of the lower Nenjiang Formation in the Qingshankou area, Songliao Basin[J]. Journal of Stratigraphy, 2007, 31(3): 296-302.]
[13]
Frey F A, Coffin M A, Wallace P J. Proceedings Ocean Drilling Program, Initial Reports Ocean Drilling Program College Station, TX. Shipboard Scientific Party. Site 1138. 2000.
[14]
叶得泉,黄清华,张莹,等. 松辽盆地白垩纪介形类生物地层学[M]. 北京:石油工业出版社,2002:1-289. [Ye Dequan, Huang Qinghua, Zhang Yin, et al. Cretaceous Ostracoda Biostratigraphy in Songliao Basin[M]. Beijing: Petroleum Industry Press, 2002: 1-289.]
[15]
Dumitrescu M, Brassell S C. Compositional and isotopic characteristics of organic matter for the early Aptian Oceanic Anoxic Event at Shatsky Rise, ODP Leg 198[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2006, 235(1/2/3): 168-191.
[16]
Meyers P A. Pleoceanographic and paleoclimatic similarities between Mediterranean sapropels and Cretaceous black shales[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2006, 235(1/2/3): 305-320.
[17]
Bechtel A, Jia J L, Strobl S A I, et al. Palaeoenvironmental conditions during deposition of the Upper Cretaceous oil shale sequences in the Songliao Basin (NE China): Implications from geochemical analysis[J]. Organic Geochemistry, 2012, 46: 76-95.
[18]
van Mooy B A S, Keil R G, Devol A H. Impact of suboxia on sinking particulate organic carbon: Enhanced carbon flux and preferential degradation of amino acids via denitrification[J]. Geochimica et Cosmochimica Acta, 2002, 66(3): 457-465.
[19]
Arthur M A,黄泽辉. 现代海洋有机碳中13C的异常富集[J]. 海洋石油,1986(3):63-66. [Arthur M A, Huang Zehui. The abnormal enrichment of δ13C in modern marine organic carbon[J]. Marine Oil, 1986(3): 63-66.]
[20]
Meyers P A. Sources and deposition of organic matter in Cretaceous passive margin deep-sea sediments: a synthesis of organic geochemical studies from Deep Sea Drilling Project Site 603, outer Hatteras Rise[J]. Marine and Petroleum Geology, 1989, 6(2): 182-189.
[21]
Tsikos H, Jenkyns H C, Walsworth-Bell B, et al. Carbon-isotope stratigraphy recorded by the Cenomanian-Turonian Oceanic Anoxic Event: correlation and implications based on three key localities[J]. Journal of the Geological Society, 2004, 161(4): 711-719.
[22]
Kolonic S, Wagner T, Forster A, et al. Black shale deposition on the northwest African Shelf during the Cenomanian/Turonian oceanic anoxic event: Climate coupling and global organic carbon burial[J]. Paleoceanography, 2005, 20(1): PA1006.
[23]
Norris R D, Bice K L, Magno E A, et al. Jiggling the tropical thermostat in the Cretaceous hothouse[J]. Geology, 2002, 30(4): 299-302.
[24]
Blumer M, Guillard R R L, Chase T. Hydrocarbons of marine phytoplankton[J]. Marine Biology, 1971, 8(3): 183-189.
[25]
江继刚. 江汉盆地咸水湖相潜江组油、气的生成[J]. 石油学报,1981,2(4):83-92. [Jiang Jigang. Origin of oil and gas in Qian Jiang Formation of saline lake facies in the Jianghan Basin[J]. Acta Petrolei Sinica, 1981, 2(4): 83-92.]
[26]
黄杏珍,邵宏舜. 柴达木盆地的油气形成与寻找油气田方向[M]. 兰州:甘肃科学技术出版社,1993:212-341. [Huang Xingzhen, Shao Hongshun. Formation of Petroleum and Exploration Direction in the Qaidam Basin, Northwest China[M]. Lanzhou: Gansu Science and Technology Publishing House, 1993: 212-341.]
[27]
张枝焕,杨藩,李东明,等. 中国新生界咸水湖相烃源岩和原油生物标志物组合特征[J]. 沉积学报,1998,16(3):119-123,131. [Zhang Zhihuan, Yang Fan, Li Dongming, et al. Biomarker assemblage characteristics of source rocks and associated crude oils in saline lake facies of Cenozoic in China[J]. Acta Sedimentologica Sinica, 1998, 16(3): 119-123, 131.]
[28]
宋宁,王铁冠,李美俊. 江苏金湖凹陷古近系奇碳优势和偶碳优势共存的正构烷烃[J]. 沉积学报,2007,25(2):307-313. [Song Ning, Wang Tieguan, Li Meijun. An n-alkane coexisting even and odd carbon number predominance of Paleogene in Jinhu sag[J]. Acta Sedimentologica Sinica, 2007, 25(2): 307-313.]
[29]
Didyk B M, Simoneit B R T, Brassell S C, et al. Organic geochemical indicators of palaeoenvironmental conditions of sedimentation[J]. Nature, 1978, 272(5650): 216-222.
[30]
van Kaam-Peters H M E, Schouten S, De Leeuw J W, et al. A molecular and carbon isotope biogeochemical study of biomarkers and kerogen pyrolysates of the Kimmeridge Clay Facies: palaeoenvironmental implications[J]. Organic Geochemistry, 1997, 27(7/8): 399-422.
[31]
Metzger P, Largeau C, Casadevall E. Lipids and macromolecular lipids of the hydrocarbon-rich microalga Botryococcus braunii. Chemical structure and biosynthesis. Geochemical and biotechnological importance[M]//Fortschritte der Chemie organischer Naturstoffe/Progress in the Chemistry of Organic Natural Products. Vienna: Springer, 1991: 1-70.
[32]
Gelpi E, Schneider H, Mann J, et al. Hydrocarbons of geochemical significance in microscopic algae[J]. Phytochemistry, 1970, 9(3): 603-612.
[33]
冯子辉,方伟,王雪,等. 松辽盆地海侵制约油页岩形成的微体古生物和分子化石证据[J]. 中国科学 D辑:地球科学,2009,39(10):1375-1386. [Feng Zihui, Fang Wei, Wang Xue, et al. Microfossils and molecular records in oil shales of the Songliao Basin and implications for paleo-depositional environment[J]. Science in China Series D: Earth Sciences, 2009, 52(10): 1559-1571.]
[34]
Moldowan J M, Fago F J, Lee C Y, et al. Sedimentary 24-n-propylcholestanes, molecular fossils diagnostic of marine algae[J]. Science, 1990, 247(4940): 309-312.
[35]
McCaffrey M A, Moldowan J M, Lipton P A, et al. Paleoenvironmental implications of novel C30 steranes in Precambrian to Cenozoic Age petroleum and bitumen[J]. Geochimica et Cosmochimica Acta, 1994, 58(1): 529-532.
[36]
侯读杰,黄清华,黄福堂,等. 松辽盆地海侵地层的分子地球化学特征[J]. 石油学报,1999,20(2):30-34. [Hou Dujie, Huang Qinghua, Huang Futang, et al. The characteristics of molecular geochemistry of marine transgression strata in Songliao Basin[J]. Acta Petrolei Sinica, 1999, 20(2): 30-34.]
[37]
Brocks J J, Summons R E. Sedimentary hydrocarbons, biomarkers for early life[J]. Treatise on Geochemistry, 2003, 8: 63-115.
[38]
Fu J M, Sheng G Y, Xu J Y, et al. Application of biological markers in the assessment of paleoenvironments of Chinese non-marine sediments[J]. Organic Geochemistry, 1990, 16(4/6): 769-779.
[39]
陈笑夜,曹剑,施春华,等. 陆相湖盆海侵地质事件识别及其对烃源岩形成影响[J]. 地质论评,2012,58(5):901-910. [Chen Xiaoye, Cao Jian, Shi Chunhua, et al. A review on distinguishing of marine transgression in continental basins and its impacts on the formation of hydrocarbon source rocks[J]. Geological Review, 2012, 58(5): 901-910.]
[40]
吕炳全,王红罡,胡望水,等. 扬子地块东南古生代上升流沉积相及其与烃源岩的关系[J]. 海洋地质与第四纪地质,2004,24(4):29-35. [Lü Bingquan, Wang Honggang, Hu Wangshui, et al. Relationship between Paleozoic up welling facies and hydrocarbon in southeastern margin Yangtze Block[J]. Marine Geology & Quaternary Geology, 2004, 24(4): 29-35.]
[41]
吴敬禄,蒋雪中,夏威岚,等. 云南程海近500年来湖泊初始生产力的演化[J]. 海洋地质与第四纪地质,2002,22(2):95-98. [Wu Jinglu, Jiang Xuezhong, Xia Weilan, et al. Climate and primary productivity over the last 500 years of the Chenghai Lake, Yunnan[J]. Marine Geology & Quaternary Geology, 2002, 22(2): 95-98.]
[42]
Meyers P A. Organic geochemical proxies of paleoceanographic, paleolimnologic, and paleoclimatic processes[J]. Organic Geochemistry, 1997, 27(5/6): 213-250.
[43]
沈吉,吴瑞金,安芷生. 大布苏湖沉积剖面有机碳同位素特征与古环境[J]. 湖泊科学,1998,10(3):8-12. [Shen Ji, Wu Ruijin, An Zhisheng. Characters of the organic δ13C and paleoenvironment in the section of Dabusu Lake[J]. Journal of Lake Sciences, 1998, 10(3): 8-12.]
[44]
Eglinton G, Hamilton R J. Leaf epicuticular waxes[J]. Science, 1967, 156(3780): 1322-1335.
[45]
Cranwell P A, Eglinton G, Robinson N. Lipids of aquatic organisms as potential contributors to lacustrine sediments-II[J]. Organic Geochemistry, 1987, 11(6): 513-527.
[46]
Zheng Y H, Zhou W J, Meyers P A, et al. Lipid biomarkers in the Zoigê-Hongyuan peat deposit: Indicators of Holocene climate changes in West China[J]. Organic Geochemistry, 2007, 38(11): 1927-1940.
[47]
Hou D J, Li M W, Huang Q H. Marine transgressional events in the gigantic freshwater lake Songliao: paleontological and geochemical evidence[J]. Organic Geochemistry, 2000, 31(7/8): 763-768.
[48]
Moldowan J M, Seifert W K, Gallegos E J. Relationship between petroleum composition and depositional environment of petroleum source rocks[J]. AAPG Bulletin, 1985, 69(8): 1255-1268.
[49]
王东坡,刘招君,刘立. 松辽盆地演化与海平面升降[M]. 北京:地质出版社,1994. [Wang Dongpo, Liu Zhaojun, Liu Li. Evolution and Sea Level Change in the Songliao Basin[M]. Beijing: Geological Publishing House, 1994.]
[50]
王成善. 白垩纪地球表层系统重大地质事件与温室气候变化研究-从重大地质事件探寻地球表层系统耦合[J]. 地球科学进展,2006,21(8):838-842. [Wang Chengshan. Coupling of the earth surface system: inferring from the Cretaceous major geological events[J]. Advances in Earth Science, 2006, 21(8): 838-842.]
[51]
Wang C S, Feng Z Q, Zhang L M, et al. Cretaceous paleogeography and paleoclimate and the setting of SKI borehole sites in Songliao Basin, northeast China[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2012, 385: 17-30.
[52]
高瑞祺,蔡希源,等. 松辽盆地油气田形成条件与分布规律[M]. 北京:石油工业出版社,1997:104-106. [Gao Ruiqi, Cai Xiyuan, et al. Formation and Distribution of Oil and Gas in Songliao Basin[M]. Beijing: Petroleum Industry Press, 1997: 104-106.]
[53]
黄清华,陈春瑞,王平在,等. 松辽盆地晚白垩世生物演化与古湖泊缺氧事件[J]. 微体古生物报,1998,15(4):417-425. [Huang Qinghua, Chen Chunrui, Wang Pingzai, et al. The Late Cretaceous bio-evolution and anoxic events in the Songliao Basin[J]. Acta Micropalaeontologica Sinica, 1998, 15(4): 417-425.]
