油气勘探

重大生物事件与化石能源形成演化——兼论地球系统框架下能源学发展

  • 潘松圻 ,
  • 邹才能 ,
  • 李勇 ,
  • 荆振华 ,
  • 刘恩涛 ,
  • 袁铭 ,
  • 张国生 ,
  • 杨智 ,
  • 吴松涛 ,
  • 邱振 ,
  • 刘翰林
展开
  • 1.中国石油勘探开发研究院,北京 100083;
    2.中国矿业大学(北京),北京 100083;
    3.北京大学,北京 100871;
    4.中国地质大学(武汉),武汉 430074
潘松圻(1986-),男,新疆奎屯人,博士,中国石油勘探开发研究院高级工程师,主要从事非常规油气地质、油气有机地球化学与能源战略等研究。地址:北京市海淀区学院路20号,中国石油勘探开发研究院能源战略综合研究部,邮政编码:100083。E-mail: pansongqi@pku.edu.cn

收稿日期: 2020-12-31

  网络出版日期: 2021-05-21

基金资助

国家自然科学基金(41902151); 中国科学院战略性先导科技专项(XDA14010403); 中国石油直属院所基础研究和战略储备技术研究项目(2018D-500805)

Major biological events and fossil energy formation: On the development of energy science under the earth system framework

  • PAN Songqi ,
  • ZOU Caineng ,
  • LI Yong ,
  • JING Zhenhua ,
  • LIU Entao ,
  • YUAN Ming ,
  • ZHANG Guosheng ,
  • YANG Zhi ,
  • WU Songtao ,
  • QIU Zhen ,
  • LIU Hanlin
Expand
  • 1. PetroChina Research Institute of Petroleum Exploration and Development, Beijing 100083, China;
    2. China University of Mining and Technology-Beijing, Beijing 100083, China;
    3. Peking University, Beijing 100871, China;
    4. China University of Geosciences-Wuhan, Hubei 430074, China

Received date: 2020-12-31

  Online published: 2021-05-21

摘要

地质历史中发生1次生命大爆发和5次生物大灭绝重大生物和环境事件,它们控制地球生态系统演化,对富有机质层系形成具有重要影响和控制作用。寒武纪生命大爆发及奥陶纪末、晚泥盆世、二叠纪末、三叠纪末、白垩纪末5次生物大灭绝重大生物事件,对应全球多套富有机质层系,与地球化石能源形成演化和分布具有密切关系。中国能源禀赋“新能源无限、富煤但油气不足”,决定未来依靠新能源实现“能源独立自主”和碳中和。从地球系统演化角度出发,探究能源与地球、能源与环境、能源与人类的多元关系,开展能源学综合研究。能源学是指立足地球系统演化,从时间和空间尺度,研究各类能源形成分布、评价选区、开发利用、有序替代、发展前景等内容的科学。能源学的内涵包括3个核心内容:①地球系统背景下能源的形成、能源消耗对地球气候环境的反馈,体现地球与能源之间的相互关系;②地球环境孕育人类演进、人类行为改造地球环境,体现地球与人类之间的相互关系;③人类利用技术开发能源、能源驱动人类社会进步,体现人类与能源之间的相互关系。能源学研究聚焦化石能源形成与开发、新能源发展与有序替代、深地与深空能源探索及利用、能源发展战略与规划等4个方面。能源学的提出对完善学科体系、促进能源发展、明确能源转型发展方向、推动碳中和地质学研究建设宜居地球具有重要意义。图2表2参84

本文引用格式

潘松圻 , 邹才能 , 李勇 , 荆振华 , 刘恩涛 , 袁铭 , 张国生 , 杨智 , 吴松涛 , 邱振 , 刘翰林 . 重大生物事件与化石能源形成演化——兼论地球系统框架下能源学发展[J]. 石油勘探与开发, 2021 , 48(3) : 498 -509 . DOI: 10.11698/PED.2021.03.06

Abstract

In geological history, one major life explosion and five times of mass extinction occurred. These major biological and environmental events affected the evolution of the Earth ecosystem and controlled the formation of organic-rich strata. The life explosion occurred in Cambrian and the five mass extinction events happened at the end of Ordovician, Late Devonian, end of Permian, end of Triassic, and end of Cretaceous, respectively. They are corresponded to the formation of multiple suites of organic-rich strata globally, which are crucial to the formation, evolution and distribution of the fossil energy on Earth. From the perspective of the Earth system evolution, we investigate the multiple relationships between energy and Earth, energy and environment, as well as energy and human beings, and carry out comprehensive research on energy. Energy science refers to the science of studying the various energy sources formation and distribution, evaluation and selection, production and utilization, orderly replacement, development prospects, etc. in temporal and spatial scales based on the evolution of the Earth system. The connotation of energy science includes three core contents: (1) The relationship between the Earth and energy, including the formation of energy in the Earth system and the feedback of energy consumption to the Earth's climate and environment; (2) The relationship between the Earth environment and the human beings, including the Earth environment breeding human beings and human activities transforming the earth environment; (3) The relationship between the energy and the human beings, including the development of energy technology by human beings and the progress of human society driven by energy utilization. The energy science focuses on the formation and development of fossil energy, development and orderly replacement of new energy, exploration and utilization of energy in deep earth and deep space, and energy development strategy and planning. The proposal of energy science is of great significance for improving the discipline system, promoting energy development, clarifying the development direction of energy transition, and constructing a habitable Earth.

参考文献

[1] 谢树成, 颜佳新, 史晓颖, 等. 烃源岩地球生物学[M]. 北京: 科学出版社, 2016.
XIE Shucheng, YAN Jiaxin, SHI Xiaoying, et al. Source rock geobiology[M]. Beijing: Science Press, 2016.
[2] 戎嘉余, 黄冰. 生物大灭绝研究三十年[J]. 中国科学: 地球科学, 2014, 44(3): 377-404.
RONG Jiayu, HUANG Bing. Study of mass extinction over the past thirty years: A synopsis[J]. SCIENCE CHINA Earth Sciences, 2014, 44(3): 377-404.
[3] PAYNE J L, BOYER A G, BROWN J H, et al. Two-phase increase in the maximum size of life over 3.5 billion years reflects biological innovation and environmental opportunity[J]. Proceedings of the National Academy of Sciences, 2009, 106(1): 24-27.
[4] ZHANG S, WANG X, WANG H, et al. Sufficient oxygen for animal respiration 1400 million years ago[J]. Proceedings of the National Academy of Sciences, 2016, 113(7): 1731-1736.
[5] KUMP L R. The rise of atmospheric oxygen[J]. Nature, 2008, 451: 277-278.
[6] LYONS T W, REINHARD C T, PLANAVSKY N J. The rise of oxygen in Earth’s early ocean and atmosphere[J]. Nature, 2014, 506(7488): 307-315.
[7] WANG X M, ZHAO W Z, ZHANG S C, et al. The aerobic diagenesis of Mesoproterozoic organic matter[J]. Scientific Reports, 2018, 8(1): 1-10.
[8] CHEN Z Q, YANG H, LUO M, et al. Complete biotic and sedimentary records of the Permian-Triassic transition from Meishan section, South China: Ecologically assessing mass extinction and its aftermath[J]. Earth Science Reviews, 2015, 149: 67-107.
[9] DENIRO M J, EPSTEIN S. Relationship between the oxygen isotope ratios of terrestrial plant cellulose, carbon dioxide, and water[J]. Science, 1979, 204(4388): 51-53.
[10] WILSON M J, SHALDYBIN M V, WILSON L. Clay mineralogy and unconventional hydrocarbon shale reservoirs in the USA. I. Occurrence and interpretation of mixed-layer R3 ordered illite/smectite[J]. Earth-Science Reviews, 2016, 158: 31-50.
[11] 赵贤正, 周立宏, 赵敏, 等. 陆相页岩油工业化开发突破与实践: 以渤海湾盆地沧东凹陷孔二段为例[J]. 中国石油勘探, 2019, 24(5): 589-600.
ZHAO Xianzheng, ZHOU Lihong, ZHAO Min, et al. Breakthrough and practice of industrial development on continental shale oil: A case study on Kong-2 Member in Cangdong Sag, Bohai Bay Basin[J]. China Petroleum Exploration, 2019, 24(5): 589-600.
[12] EIA. U.S. crude oil and natural gas proved reserves at year-end 2018[EB/OL]. (2019-12-13)[2020-12-01]. https://www.eia.gov/naturalgas/crudeoilreserves/index.php.
[13] GENTZIS T. A review of the thermal maturity and hydrocarbon potential of the Mancos and Lewis shales in parts of New Mexico, USA[J]. International Journal of Coal Geology, 2013, 113: 64-75.
[14] PERNIA D, BISSADA K K A, CURIALE J. Kerogen based characterization of major gas shales: Effects of kerogen fractionation[J]. Organic Geochemistry, 2015, 78: 52-61.
[15] FRENCH K L, BIRDWELL J E, LEWAN M D. Trends in thermal maturity indicators for the organic sulfur-rich Eagle Ford Shale[J]. Marine and Petroleum Geology, 2020, 118: 104459.
[16] 邹才能, 杨智, 王红岩, 等. “进源找油”: 论四川盆地非常规陆相大型页岩油气田[J]. 地质学报, 2019, 93(7): 1551-1562.
ZOU Caineng, YANG Zhi, WANG Hongyan, et al. “Exploring petroleum inside source kiechen”: Jurassic unconventional continental giant shale oil & gas field in Sichuan Basin, China[J]. Acta Geologica Sinica, 2019, 93(7): 1551-1562.
[17] 付锁堂, 姚泾利, 李士祥, 等. 鄂尔多斯盆地中生界延长组陆相页岩油富集特征与资源潜力[J]. 石油实验地质, 2020, 42(5): 698-710.
FU Suotang, YAO Jingli, LI Shixiang, et al. Enrichment characteristics and resource potential of continental shale oil in Mesozoic Yanchang Formation, Ordos Basin[J]. Petroleum Geology & Experiment, 2020, 42(5): 698-710.
[18] BLOMQUIST P K. The Wolfcamp Horizontal Play of Midland Basin, West Texas[R]. Las Vegas, NV: AAPG Pacific and Rocky Mountain Sectional Meeting, 2016.
[19] 郭旭光, 何文军, 杨森, 等. 准噶尔盆地页岩油“甜点区”评价与关键技术应用: 以吉木萨尔凹陷二叠系芦草沟组为例[J]. 天然气地球科学, 2019, 30(8): 1168-1179.
GUO Xuguang, HE Wenjun, YANG Sen, et al. Evaluation and application of key technologies of sweet area of shale oil in Junggar Basin: Case study of Permian Lucaogou Formation in Jumusar Depression[J]. Nature Gas Geoscience, 2019, 30(8): 1168-1179.
[20] EIA. Review of emerging resources: U.S. shale gas and shale oil[EB/OL]. (2011-07-08)[2020-12-01]. https://www.baidu.com/link?url=WM4S7cK1SUHxKYehc-NH4jR5vPW-sV_lmzJQFNsIMwVAFZrPDGK4bePTK7z0rH9gs8SqgiASCHhkPO7heH5fEK&wd=&eqid=bf2a4d88000001ac000000035fc5bd21.
[21] LOUCKS R G, RUPPEL S C. Mississippian Barnett Shale: Lithofacies and depositional setting of a deep-water shale-gas succession in the Fort Worth Basin, Texas[J]. AAPG Bulletin, 2007, 91(4): 579-601.
[22] HANDFORD C R. Facies and bedding sequences in shelf-storm- deposited carbonates: Fayetteville Shale and Pitkin Limestone (Mississippian), Arkansas[J]. Journal of Sedimentary Research, 1986, 56(1): 123-137.
[23] BULLIN K, KROUSKOP P. Composition variety complicates processing plans for US shale gas[J]. Oil & Gas Journal, 2009, 10(107): 50-55.
[24] EIA. International energy outlook 2019[EB/OL]. (2019-10-01)[2020- 12-01]. https://www.eia.gov/outlooks/archive/ieo19/https://www.eia.gov/outlooks/archive/ieo19/.
[25] PLANAVSKY N, BEKKER A, ROUXEL O J, et al. Rare earth element and yttrium compositions of Archean and Paleoproterozoic Fe formations revisited: New perspectives on the significance and mechanisms of deposition[J]. Geochimica et Cosmochimica Acta, 2010, 74(22): 6387-6405.
[26] FILIPPELLI G M. Phosphorus and the gust of fresh air[J]. Nature, 2010, 467(7319): 1052-1053.
[27] FROGNER P, GÍSLASON S R, ÓSKARSSON N. Fertilizing potential of volcanic ash in ocean surface water[J]. Geology, 2001, 29(6): 487-490.
[28] JONES M T, GISLASON S R. Rapid releases of metal salts and nutrients following the deposition of volcanic ash into aqueous environments[J]. Geochimica et Cosmochimica Acta, 2008, 72(15): 3661-3680.
[29] DELMELLE P, LAMBERT M, DUFRÊNE Y, et al. Gas/aerosol-ash interaction in volcanic plumes: New insights from surface analyses of fine ash particles[J]. Earth and Planetary Science Letters, 2007, 259(1/2): 159-170.
[30] 沈俊. 二叠纪-三叠纪之交华南火山作用对海洋环境和生物的影响[D]. 北京: 中国地质大学, 2014.
SHEN Jun. Volcanic effects to marine environments and organisms across the Permian-Triassic transition in South China[D]. Beijing: China University of Geosciences, 2014.
[31] BLATTMANN T M, LIU Z, ZHANG Y, et al. Mineralogical control on the fate of continentally derived organic matter in the ocean[J]. Science, 2019, 366(6466): 742-745.
[32] LIN I I, HU C M, LI Y H, et al. Fertilization potential of volcanic dust in the low-nutrient low-chlorophyll western North Pacific subtropical gyre: Satellite evidence and laboratory study[J]. Global Biogeochemical Cycles, 2011, 25(1): B1006.
[33] LANGMANN B, ZAKSEK K, HORT M, et al. Volcanic ash as fertiliser for the surface ocean[J]. Atmospheric Chemistry and Physics, 2010, 10(8): 3891-3899.
[34] 邱振, 董大忠, 卢斌, 等. 中国南方五峰组-龙马溪组页岩中笔石与有机质富集关系探讨[J]. 沉积学报, 2016, 34(6): 1011-1020.
QIU Zhen, DONG Dazhong, LU Bin, et al. Discussion on the relationship between graptolite abundance and organic enrichment in shales from the Wufeng and Longmaxi Formation, South China[J]. Acta Sedimentologica Sinica, 2016, 34(6): 1011-1020.
[35] HU D P, LI M H, ZHANG X L, et al. Large mass-independent sulphur isotope anomalies link stratospheric volcanism to the Late Ordovician mass extinction[J]. Nature Communications, 2020, 11(1): 2297.
[36] 沈树忠, 张华. 什么引起五次生物大灭绝[J]. 科学通报, 2017, 62(11): 1119-1135.
SHEN Shuzhong, ZHANG Hua. What caused mass extinctions[J]. Chinese Science Bulletin, 2017, 62(11): 1119-1135.
[37] 舒德干, 张兴亮, 韩健, 等. 再论寒武纪大爆发与动物树成型[J]. 古生物学报, 2009, 48(3): 414-427.
SHU Degan, ZHANG Xingliang, HAN Jian. Restudy of Cambrian explosion and formation of animal tree[J]. Acta Palaeontologica Sinica, 2009, 48(3): 414-427.
[38] 赵坤, 李婷婷, 朱光有, 等. 下寒武统优质烃源岩的地球化学特征与形成机制: 以鄂西地区天柱山剖面为例[J]. 石油学报, 2020, 41(1): 13-26.
ZHAO Kun, LI Tingting, ZHU Guangyou, et al. Geochemical characteristics and formation mechanism of high-quality Lower Cambrian source rocks: A case study of the Tianzhushan profile in western Hubei[J]. Acta Petrolei Sinica, 2020, 41(1): 13-26.
[39] 张兴亮, 舒德干. 寒武纪大爆发的因果关系[J]. 中国科学: 地球科学, 2014, 44(6): 1155-1170.
ZHANG Xingliang, SHU Degan. Causes and consequences of the Cambrian explosion[J]. SCIENCE CHINA Earth Sciences, 2014, 57(5): 930-942.
[40] SMITH M P, HARPER D A T. Causes of the Cambrian explosion[J]. Science, 2013, 341(6152): 1355.
[41] 陈旭, 樊隽轩, 麦尔钦, 等. 华南奥陶纪末笔石灭绝及幸存的进程与机制[M]//戎嘉余. 生物大绝灭与复苏: 来自华南古生代和三叠纪的证据(上卷). 合肥: 中国科技大学出版社, 2004.
CHEN Xu, FAN Junxuan, MELCHIN M J. The process and mechanism of graptolite extinction and survival at the end of Ordovician in South China[M]//RONG Jiayu. Mass extinction and recovery: Evicences from the Palaeozoic and Triassic of South China. Hefei: China University of Science and Technology Press, 2004.
[42] 王玉珏, 梁昆, 陈波, 等. 晚泥盆世F-F大灭绝事件研究进展[J]. 地层学杂志, 2020, 44(3): 277-298.
WANG Yujue, LIANG Kun, CHEN Bo, et al. Research progress in the late Devonian F-F mass extinction[J]. Journal of Stratigraphy, 2020, 44(3): 277-298.
[43] MCGHEE G R. The late Devonian mass extinction: The Frasnian/ Famennian crisis[M]. New York: Columbia University Press, 1996: 303.
[44] JOACHIMSKI M M, BUGGISCH W. Conodont apatite δ18O signatures indicate climatic cooling as a trigger of the Late Devonian mass extinction[J]. Geology, 2002, 30(8): 711-714.
[45] BERNER R A. The rise of plants and their effect on weathering and atmospheric CO2[J]. Science, 1997, 276(5312): 544-546.
[46] 谢树成, 殷鸿福, 史晓颖. 地球生物学: 生命与地球环境的相互作用和协同演化[M]. 北京: 科学出版社, 2011.
XIE Shucheng, YIN Hongfu, SHI Xiaoying. Geobiology: Interactions and co-evolution between life and the Earth’s environment[M]. Beijing: Science Press, 2011.
[47] 谢树成, 殷鸿福, 曹长群, 等. 二叠纪-三叠纪之交地球表层系统的多幕式变化: 分子地球生物学记录[J]. 古生物学报, 2009, 48(3): 487-496.
XIE Shucheng, YIN Hongfu, CAO Changqun, et al. Episodic changes of the earth surface system across the Permian-Triassic boundary: Molecular geobiological records[J]. Acta Palaeontologica Sinica, 2009, 48(3): 487-496.
[48] GRADSTEIN F M, OGG J G, SCHMITZ M D, et al. The geologic time scale[M]. Boston: Elsevier, 2012: 1129-1144.
[49] FRAKES L A, FRANCIS J E, SYKTUS J I. Climate modes of the Phanerozoic the history of the Earth’s climate over the past 600 million years[M]. Cambridge, New York: Cambridge University Press, 1992: 274.
[50] TAKASHIMA R, NISHI H, HUBER B, et al. Greenhouse world and the Mesozoic ocean[J]. Oceanography, 2006, 19(4): 82-92.
[51] ROYER D L. CO2-forced climate thresholds during the Phanerozoic[J]. Geochimica et Cosmochimica Acta, 2006, 70(23): 5665-5675.
[52] BERNER R A, VANDENBROOKS J M, WARD P D. Oxygen and evolution[J]. Science, 2007, 316(5824): 557-558.
[53] PERCIVAL L M E, WITT M L I, MATHER T A, et al. Globally enhanced mercury deposition during the End-Pliensbachian extinction and Toarcian OAE: A link to the Karoo-Ferrar large igneous province[J]. Earth and Planetary Science Letters, 2015, 428: 267-280.
[54] KELLER G. Impacts, volcanism and mass extinction: Random coincidence or cause and effect[J]. Australian Journal of Earth Sciences, 2005, 52(4/5): 725-757.
[55] RIDGWELL A. A Mid Mesozoic Revolution in the regulation of ocean chemistry[J]. Marine Geology, 2005, 217(3/4): 339-357.
[56] STANLEY S M. Earth system history[M]. Oxford: W. h. Freeman & Co Ltd, 2005: 608.
[57] RAUP D M, SEPKOSKI J J. Periodic extinction of families and genera[J]. Science, 1986, 231(4740): 833-836.
[58] YAN D T, CHEN D Z, WANG Q C, et al. Large-scale climatic fluctuations in the latest Ordovician on the Yangtze block, South China[J]. Geology, 2010, 38(7): 599-602.
[59] SHEEHAN P M, HARRIS M T. Microbialite resurgence after the Late Ordovician extinction[J]. Nature, 2004, 430(6995): 75-78.
[60] CHEN D Z, QING H R, LI R W. The Late Devonian Frasnian-Famennian (F/F) biotic crisis: Insights from δ13Ccarb, δ13Corg and 87Sr/86Sr isotopic systematics[J]. Earth and Planetary Science Letters, 2005, 235(1/2): 151-166.
[61] 刘宇. 五峰—龙马溪组页岩的发育环境与页岩气潜力评价研究[D]. 广州: 中国科学院大学(中国科学院广州地球化学研究所), 2016.
LIU Yu. Development environment and shale gas resources assessment of the Wufeng-Longmaxi Formation[D]. Guangzhou: University of Chinese Academy of Sciences (Guangzhou Institute of Geochemistry), 2016.
[62] BOND D, WIGNALL P B. Chapter 9: Evidence for late devonian (kellwasser) anoxic events in the great basin, western united states[M]//OVER D J, MORROW J R, WIGNALL P B. Developments in Palaeontology and Stratigraphy. Amsterdam: Elsevier, 2005: 225-262.
[63] TRIBOVILLARD N, AVERBUCH O, DEVLEESCHOUWER X, et al. Deep-water anoxia over the Frasnian-Famennian boundary (La Serre, France): A tectonically induced oceanic anoxic event[J]. Terra Nova, 2004, 16(5): 288-295.
[64] WHITE D A, ELRICK M, ROMANIELLO S, et al. Global seawater redox trends during the Late Devonian mass extinction detected using U isotopes of marine limestones[J]. Earth and Planetary Science Letters, 2018, 503: 68-77.
[65] BROWNE T N, HOFMANN M H, MALKOWSKI M A, et al. Redox and paleoenvironmental conditions of the Devonian-Carboniferous Sappington Formation, southwestern Montana, and comparison to the Bakken Formation, Williston Basin[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2020, 560: 110025.
[66] DEXIN H. The features of Devonian coal-bearing deposits in South China, The People’s Republic of China[J]. International Journal of Coal Geology, 1989, 12(1): 209-223.
[67] CHEN Jun, SHEN Shuzhong, LI Xianhua, et al. High-resolution SIMS oxygen isotope analysis on conodont apatite from South China and implications for the End-Permian mass extinction[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2016, 448(S1): 26-38.
[68] ROMANO C, GOUDEMAND N, VENNEMANN T W, et al. Climatic and biotic upheavals following the End-Permian mass extinction[J]. Nature Geoscience, 2013, 6(1): 57-60.
[69] 杨江海, 颜佳新, 黄燕. 从晚古生代冰室到早中生代温室的气候转变: 兼论东特提斯低纬区的沉积记录与响应[J]. 沉积学报, 2017, 35(5): 981-993.
YANG Jianghai, YAN Jiaxin, HUANG Yan. The earth’s penultimate icehouse-to-greenhouse climate transition and related sedimentary records in low-latitude regions of Eastern Tethys[J]. Acta Sedimentologica Sinica, 2017, 35(5): 981-993.
[70] LARRY T. Coal geology[M]. Chichester, West Sussex: Wiley-Blackwell, 2013: 444.
[71] BLACKBURN T J, OLSEN P E, BOWRING S A, et al. Zircon U-Pb geochronology links the end-Triassic extinction with the Central Atlantic Magmatic Province[J]. Science, 2013, 340(6135): 941-945.
[72] BERNER R A. Atmospheric oxygen over Phanerozoic time[J]. Proceedings of the National Academy of the Sciences of the United States of America, 1999, 96(20): 10955-10957.
[73] RIGO M, ONOUE T, TANNER L, et al. The Late Triassic extinction at the Norian/Rhaetian boundary: Biotic evidence and geochemical analysis[J]. Earth-Science Reviews, 2020: 103180.
[74] GREENE S E, MARTINDALE R C, RITTERBUSH K A, et al. Recognising ocean acidification in deep time: An evaluation of the evidence for acidification across the Triassic-Jurassic boundary[J]. Earth-Science Reviews, 2012, 113(1/2): 72-93.
[75] ALVAREZ L W, ALVAREZ W, ASARO F, et al. Extraterrestrial cause for the Cretaceous-Tertiary extinction[J]. Science, 1980, 208(4448): 1095-1108.
[76] WIGNALL P B. Large igneous provinces and mass extinctions[J]. Earth-Science Reviews, 2001, 53(1): 1-33.
[77] GIRALDO-GÓMEZ V M, MUTTERLOSE J, BEIK I, et al. Oil shales from the K-Pg boundary interval of Jordan-Climate controlled archives of surface and bottom water conditions in a shelf setting[J]. Marine and Petroleum Geology, 2021, 123: 104724.
[78] SEPKOSKI J J. A kinetic model of Phanerozoic taxonomic diversity. III. Post-Paleozoic families and mass extinctions[J]. Paleobiology, 1984, 10(2): 246-267.
[79] IRVING E, NORTH F K, COUILLARD R. Oil, climate, and tectonics[J]. Canadian Journal of Earth Sciences, 1974, 11(1): 1-17.
[80] ZHANG S C, WANG X M, HAMMARLUND E U, et al. Orbital forcing of climate 1.4 billion years ago[J]. Proceedings of the National Academy of Sciences, 2015, 112(12): E1406.
[81] 郭正堂. 《地球系统与演变》: 未来地球科学的脉络[J]. 科学通报, 2019, 64(9): 882-883.
GUO Zhengtang. Earth system and evolution: A future frame of earth sciences[J]. Chinese Science Bulletin, 2019, 64(9): 882-883.
[82] 汪品先. 地球系统与演变[M]. 北京: 科学出版社, 2018.
WANG Pinxian. Earth system and evolution[M]. Beijing: Science Press, 2018.
[83] 邹才能, 潘松圻, 荆振华, 等. 页岩油气革命及影响[J]. 石油学报, 2020, 41(1): 1-12.
ZOU Caineng, PAN Songqi, JING Zhenhua, et al. Shale oil and gas revolution and its impact[J]. Acta Petrolei Sinica, 2020, 41(1): 1-12.
[84] LEWIS S L, MASLIN M A. Defining the Anthropocene[J]. Nature, 2015, 519(7542): 171-180.
文章导航

/