[1]Haq B U, Hardenbol J, Vail P R. Chronology of fluctuating sea levels since the Triassic[J]. Science, 1987, 235:1 156-1 167.
[2]Stoll H M, Schrag D P. Evidence for glacial control of rapid sea level changes in the early Cretaceous[J]. Science, 1996, 272: 1 771-1 774.
[3]Gerta K. Cretaceous climate, volcanism, impacts, and biotic effects[J]. Cretaceous Research,2008, 29: 754-771.
[4]Gradstein F M, Ogg J G, Smith A G. A Geologic TimeScale 2004[M]. Cambridge: Cambridge University Press, 2004:355-358.
[5]Crowley T J, Kim K Y. Comparison of long-term greenhouse projections with the geologic record[J]. Geophysical Research Letters,1995, 22: 933-936.
[6]Herman A B, Spicer R A. Palaeobotanical evidence for a warm Cretaceous Arctic Ocean[J].Nature, 1996, 380: 330-333.
[7]Dai Shuang, Huang Yongbo, Zhao Jie, et al. The climate change during 128.11-119.05 Ma recorded by the susceptibility of the sediments of Liupanshan Group[J].Earth Science Frontiers,2010,17(3):242-248.[戴霜,黄永波,赵杰,等.六盘山群沉积物磁化率记录的早白垩世气候变化[J].地学前缘,2010,17(3):242-248.]
[8]Kong Li, Dai Shuang, Liu Xue, et al. Climate changes during 128.10-115.30 Ma recorded by colors of sediments in the Liupanshan Basin along Huoshizhai section[J]. Journal of Lanzhou University (Natural Sciences), 2010, 46(5):44-49.[孔立,戴霜,刘学,等.六盘山群火石寨剖面沉积物色度记录的128.10-115.30气候变化[J].兰州大学学报:自然科学版,2010,46(5):44-49.]
[9]Zhang Mingzhen, Dai Shuang, Zhang Yongquan, et al. Early Cretaceous Palynological assemblage and its environmental significance in the sediments of Liupanshan Group (Sikouzi Section) , Liupanshan Region, central China[J]. Arid Land Geography,2012,35(1):99-108.[张明震,戴霜,张永全,等.六盘山地区寺口子剖面早白垩世晚期的孢粉组合及其环境意义[J].干旱区地理,2012,35(1):99-108.]
[10]Sun Zhiming, Yang Zhenyu, Yang Tianshui, et al. New Early Cretaceous palaeoseomagnetic results from the Haiyuan area and its tectonic implications[J]. Chinese Journal of Geophysics,2001, 44(5):678-686.[孙知明,杨振宇,杨天水,等.海原地区早白垩世古地磁结果及其构造意义[J].地球物理学报,2001, 44(5):678-686.]
[11]Yin Hongfu. The Palaeobiogeography of China[M].Beijing:China University of Geosciences Press, 1988: 250-267.[殷鸿福.中国古生物地理学[M].武汉:中国地质大学出版社,1988: 250-267.]
[12]Qi Hua. The Ostracods of lower Liupanshan Group, Guyuan, Ningxia[C]∥The Collection of the Theses of Paleontology,1987,18:74-147.[齐骅.宁夏固原六盘山群下部的介形类化[C]∥地层古生物论文集.1987,18:74-147.]
[13]Li Jianguo, Du Baoan. Palynofloras from the Liupanshan Group (Cretaceous) at Anguo Town of Pingliang,Gansu[J]. Acta Palaeontologica Sinica,2006,45(4):498-513.[李建国,杜宝安.甘肃平凉安国镇白垩系六盘山群的孢粉植物群[J].古生物学报,2006,45(4): 498-513.]
[14]Li Zhaosheng. Early Cr Etaceous Sporo-Pollen Assemblages from Liupanshan of Ningxia and their bearing on Paleo-Vegetation and Paleo-Climatology[J]. Acta Palaeontologica Sinica,1983,22(5):517-526.[刘兆生.宁夏六盘山地区早白垩世孢粉组合及其古植被、古气候的意义[J].古生物学报,1983,22(5): 517-526.]
[15]Dai Shuang, Zhu Qiang, Hu Hongfei,et al. Magnetostratigraphy of the Liupanshan Group, Central China[J].Journal of Stratigraphy,2009,3(2):188-92.[戴霜,朱强,胡鸿飞,等.六盘山群磁性地层年代[J].地层学杂志,2009,33(2):188-192.]
[16]Wedepohl K H. Environmental influences on the chemical composition of shales and clays[C]∥Ahrens L H, Press F, Runcorn S K, et al,eds. Physics and Chemistry of the Earth. Pergamon, Oxford, UK, 1971:307-331.
[17]Wedepohl K H.The composition of the upper Earth’s crust and the natural cycles of selected metals[C]∥Merian E ed. Metals and Their Compounds in the Natural Environment.VCH,Weinheim,Germany,1991:3-17.
[18]Feng R, Kerrich R. Geochemistry of fine grained clastic sediments in the archean Abitibi greenstone belt. Cananda: Implications for the provenance and tectonic setting[J]. Geochimica et Cosmochimica Acta, 1990,54:1 061-1 081.
[19]Gu X X.Geochemical characteristics of the Triassic ththys-turbidites in the northwestern Sichuan, China: Implications for provenance and interpretation of the tectonic setting[J]. Geochimica et Cosmochimica Acta, 1994,58:4 615-4 631.
[JP2][20]Kong Li. Measurement and Paleoclimatic Significance of Color and Clay Minerals of Sediments of Liupanshan Group[D].Lanzhou:Lanzhou University,2010.[孔立.六盘山群沉积物色度和粘土矿物测量及古气候意义[D].兰州:兰州大学,2010.][JP]
[21]Nesbitt H W, Young G M. Early Proterozoic climates and plate motions inferred from major element chemistry of lutites[J].Nature,1982,299:715-717.
[22]McLennan S M. Weathering and global denudation[J].Journal of Geology,1993,101:295-303.
[23]Feng Lianjun, Chu Xuelei, Zhang Qirui, et al. CIA and its applications in the Neoproterozoic clastic rocks[J].Earth Science Frontiers,2003,10(4):539-544.[冯连君,储雪蕾,张启锐,等.化学蚀变指数(CIA)及其在新元古代碎屑岩中的应用[J].地学前缘,2003,10(4):539-544.]
[24]Fedo C M, Nesbitt H W. Unravelling the effects of potassium metasomatism in sedimentary rocks and paleosoles, with implications for palaeoweathering conditions and provenance[J]. Geology, 1995,23:921-924.
[25]Fedo C M, Young G M. Potassic and Sodic metasomatism in the Southern province of the Canadian Shield: Evidence from the Paleoproterozoic Serpent Formation, Huronian Supergroup, Canada[J]. Precambrian Research, 1997,84:17-36.
[26]Nesbitt H W, Markovics G, Price R C. Chemical processes affecting alkalis and alkaline earths during continental weathering[J]. Geochimica et Cosmochimica Acta,1980, 44:1 659-1 666.
[27]Nesbitt H W, Young G M. Prediction of some weathering trends of plutonic and volcanic rocks based on thermodynamic and kinetic considerations[J]. Geochimica et Cosmochimica Acta,1984, 48:1 523-1 534.
[28]Nesbitt H W, Young G M. Formation and diagenesis of weathering profiles[J]. Journal of Geology, 1989, 97:129-147.
[29]Panahi A, Young G M, Rainbird R H. Behavior of major and trace elements (including REE) during Paleoproterozoic pedogenesis and diagenetic alteration of an Archean granite near Ville Marie Quebec, Canada[J]. Cosmochimica et Cosmochimica Acta, 2000, 64: 2 199-2 220.
[30]Nesbitt H W, Young G M. Effects of chemical weathering and sorting on the petrogenesis of silieiclastic sediments, with implications for provenance studies[J]. Journal of Geology, 1996, 104:525-542.
[31]Liu Junwei. The Early Cretaceous Deposit and Tectonic Evolution of Liupanshan Basin[D]. Lanzhou:Lanzhou University,2010.[刘俊伟.早白垩世六盘山盆地沉积—构造演化[D].兰州:兰州大学,2010.]
[32]Cai Yuanfeng, Hu Xiaoxiao, Li Xiang, et al. Origin of the red colour in a red limestone from the Vispi Quarry section (central Italy): A high-resolution transmission electron microscopy analysis[J]. Cretaceous Research,2012,38:97-102.
[33]Arthur M A. Origin of upper cretaceous multicolored claystones of the western Atlantic[C]∥Tucholke P R, Vogt P R, et al, eds. Initial Reports of the Deep Sea Drilling Project 43, Washington, DC:U. S. Government Printing Office,1979:417-420.
[34]Dean E W, Arthur M A, Stow A V. Origin and geochemistry of Cretaceous deep-sea black shales and multicolored claystones, with emphasis on Southern Angola Basin[C]∥Hay W W, Sibuet J C , et al, eds. Initial Reports of the Deep Sea Drilling Project 43, Washington, DC:U. S. Government Printing Office, 1984:819-844.
[35]Jakobsson M, Lovlie R, Al-Hanbali H, et al. Manganese and color cycles in Arctic Ocean sediments constrain Pleistocene chronology[J]. Geology,2000,28(1): 23-26.
[36]Jiang Shaoyong, Luba Jansa, Petr Skupien, et al. Geochemistry of intercalated red and gray pelagic shales from the Mazak Formation of Cenomanian age in Czech Republic[J].Episodes, 2009,32(1):3-12.
[37]Cai Yuanfeng, Li Xiang, Hu Xiumian, et al. Paleoclimatic approach to the origin of the coloring of Turonian pelagic limestones from the Vispi Quarry section (Cretaceous, central Italy)[J]. Cretaceous Research,2009,30(5):1 205-1 216.
[38]Fang Xiaomin, Li Jijun, Zhu Junjie, et al. A 30 million year record of the carbonate content of the Linxia Basin and its climate implications[M]∥Expert Committee of the Tibet Project ed. Studies of Evolvement Environmental Transition and Ecological System of Tibetan Plateau. Beijing: Science Press,1995:55-65.[方小敏,李吉均,朱俊杰,等.临夏盆地约30 Ma以来CaCO3含量变化与气候演变[M].青藏项目专家委员会.青藏高原形成演化、环境变迁与生态系统研究.北京:科学出版社,1995:55-65.]
[39]Chen Jing’an, Wan Guojiang, Huang Ronggui. Recent Climatic changes and the chemical records in Chenghai Lake[J].Marine Geology & Quaternary Geology,2000,20(1):39-42.[陈敬安,万国江,黄荣贵.程海近代气候变化的化学记录[J].海洋地质与第四纪地质,2000,20(1):39-42.]
[40]Wen Qizhong. Geochemistry of Loess, China[M].Beijing: Science Press,1989:115-145.[文启忠.中国黄土地球化学[M].北京:科学出版社,1989:115-145.]
[41]Zhang Jinliang, Zhang Xin. The element geochemical features of ancient oceanic sedimentary environments in the Silurian Period in the Tarim Basin[J].Periodical of Ocean University of China,2006, 36(2):200-208.[张金亮,张鑫.塔里木盆地志留系古海洋沉积环境的元素地球化学特征[J].中国海洋大学学报,2006,36(2):200-208.]
[42]Wang Suiji, Huang Xingzhen, Tuo Jincai, et al. Evolutional characteristics and their paleoclimate significance of trace elements in the Hetaoyuan Formation, Biyang Depression[J]. Acta Sedimentologica Sinica,1997,15(1):65-70.[王随继,黄杏珍,妥进才,等.泌阳凹陷核桃园组微量元素演化特征及其古气候意义[J].沉积学报,1997,15(1):65-70.]
[43]Chen Jun, Wang Yongjin, Chen Chang,et al. Rb and Sr geochemical characterization of the Chinese Loess and its implications for pelaeomonsoon climate[J]. Acta Geological Sinica,2001,75(2):259-266.[陈骏,汪永进,陈旸,等.中国黄土地层Rb和Sr地球化学特征及其古季风气候意义[J].地质学报, 2001,75(2):259-266.]
[44][JP2]Ye He,Zhang Kexin,Ji Junliang.Major and trace elements characters of the sediments and palaeoclimate evolvement during about 23.1-5.0 Ma in Xunhua Basin, Qinghai[J].Earth Science—Journal of China University of Geosciences,2010,35(5):811-820.[叶荷,张克信,季军良,等.青海循化盆地23.1~5.0 Ma沉积地层中常量、微量元素组成特征及其古气候演变[J].地球科学——中国地质大学学报,2010,35(5):811-820.][JP]
[45]Zhao Zhenhua. Trace Element Geochemical Principle[M].Beijing: Sciences Press, 1997.[赵振华.微量元素地球化学原理[M].北京:科学出版社,1997.]
[46]Anderson N J, Rippey B, Gibson C E. A comparison of sedimentary and diatom-inferred phosphorus profiles: Implications for defining pre-disturbance nutrient conditions[J].Hydrobiologia,1993, 253: 357-366.
[47]Wang Yong, Yang Xiangdong, Shen Ji, et al. A 0.1 ka-year record of environmental evolution in Hongjiannao Lake, Shaanxi Province[J].Journal of Lake Sciences,2004,16(2):105-112.[汪勇,羊向东,沈吉,等.陕西红碱淖近百年来环境变化的湖泊沉积记录[J].湖泊科学, 2004, 16(2): 105-112.] |