[1] Webb G E, Kamber B S. Rare earth elements in Holocene reefal microbialites:A new shallow seawater proxy[J]. Geochimica et Cosmochimica Acta, 2000, 64(9):1557-1565. http://www.sciencedirect.com/science/article/pii/S0016703799004007
[2] Sarkar A, Sarangi S, Ebihara M, et al. Carbonate geochemistry across the Eocene/Oligocene boundary of Kutch, western India:Implications to oceanic O2-poor condition and foraminiferal extinction[J]. Chemical Geology, 2003, 201(3/4):281-293.
[3] Zhou C M, Jiang S Y, Xiao S H, et al. Rare earth elements and carbon isotope geochemistry of the Doushantuo Formation in South China:Implication for Middle Ediacaran shallow marine redox conditions[J]. Chinese Science Bulletin, 2012, 57(16):1998-2006. https://kns.cnki.net/KCMS/detail/detail.aspx?dbcode=CJFD&filename=JXTW201216015
[4] Ling H F, Chen X, Li D, et al. Cerium anomaly variations in Ediacaran-earliest Cambrian carbonates from the Yangtze Gorges area, South China:Implications for oxygenation of coeval shallow seawater[J]. Precambrian Research, 2013, 225:110-127. http://www.sciencedirect.com/science/article/pii/S0301926811002191
[5] 陈雅丽, 储雪蕾, 张兴亮, 等.陕南镇巴地区灯影组白云岩的碳、硫同位素和微量元素指示:埃迪卡拉纪末期浅海的氧化还原环境[J].中国科学(D辑):地球科学, 2015, 45(7):963-981. http://www.cnki.com.cn/Article/CJFDTotal-JDXK201507006.htm

Chen Yali, Chu Xuelei, Zhang Xingliang, et al. Carbon isotopes, sulfur isotopes, and trace elements of the dolomites from the Dengying Formation in Zhenba area, southern Shaanxi:Implications for shallow water redox conditions during the terminal Ediacaran[J]. Science China(Seri. D):Earth Sciences, 2015, 45(7):963-981. http://www.cnki.com.cn/Article/CJFDTotal-JDXK201507006.htm
[6] 任影, 钟大康, 柳慧琳, 等.渝东地区寒武系第四阶龙王庙组古环境演化的稳定同位素与主、微量元素证据[J].地球科学, 2018, 43(11):4066-4095. http://d.old.wanfangdata.com.cn/Periodical/dqkx201811023

Ren Ying, Zhong Dakang, Liu Huilin, et al. Isotopic and elemental evidence for paleoenvironmental evolution of Cambrian Stage 4 Longwangmiao Formation, East Chongqing, China[J]. Earth Science, 2018, 43(11):4066-4095. http://d.old.wanfangdata.com.cn/Periodical/dqkx201811023
[7] Murray R W. Chemical criteria to identify the depositional environment of chert:General principles and applications[J]. Sedimentary Geology, 1994, 90(3/4):213-232. doi:  10.1016-0037-0738(94)90039-6/
[8] 冯帆, 关平, 刘文汇, 等.重庆秀山南沱冰期后的海陆环境变化[J].沉积学报, 2018, 36(3):531-541. http://www.cjxb.ac.cn/CN/abstract/abstract3885.shtml

Feng Fan, Guan Ping, Liu Wenhui, et al. The marine and continental environmental changes after Nantuo Glaciation in Xiushan, Chongqing[J]. Acta Sedimentologica Sinica, 2018, 36(3):531-541. http://www.cjxb.ac.cn/CN/abstract/abstract3885.shtml
[9] Algeo T J, Maynard J B. Trace-element behavior and redox facies in core shales of Upper Pennsylvanian Kansas-type cyclothems[J]. Chemical Geology, 2004, 206(3/4):289-318. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=5a4792d00fd31b168ed93e35ddee792e
[10] Tribovillard N, Algeo T J, Lyons T, et al. Trace metals as paleoredox and paleoproductivity proxies:An update[J]. Chemical Geology, 2006, 232(1/2):12-32. http://www.sciencedirect.com/science/article/pii/S000925410600132X
[11] 梅冥相.华北寒武系二级海侵背景下的沉积趋势及层序地层序列:以北京西郊下苇甸剖面为例[J].中国地质, 2011, 38(2):317-337. http://d.old.wanfangdata.com.cn/Periodical/zgdizhi201102008

Mei Mingxiang. Depositional trends and sequence-stratigraphic successions under the Cambrian second-order transgressive setting in the North China Platform:A case study of the Xiaweidian section in the western suburb of Beijing[J]. Geology in China, 2011, 38(2):317-337. http://d.old.wanfangdata.com.cn/Periodical/zgdizhi201102008
[12] Chen J T, Lee J H, Woo J. Formative mechanisms, depositional processes, and geological implications of Furongian(Late Cambrian)reefs in the North China Platform[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2014, 414:246-259. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=f11a28997f5a3bdaa6572e807c45604c
[13] 梅冥相, Muhammad R, 刘丽, 等.蓝细菌微生物席主导的芙蓉统均一石生物丘:以河北涞源祁家峪剖面为例[J].地质评论, 2019, 65(5):1103-1122. http://d.old.wanfangdata.com.cn/Periodical/dzlp201905004

Mei Mingxiang, Muhammad R, Liu Li, et al. Leiolite bioherm dominated by cyanobacterial mats of the Furongian:An example from the Qijiayu section in Laiyuan county, Hebei province[J]. Geological Review, 2019, 65(5):1103-1122. http://d.old.wanfangdata.com.cn/Periodical/dzlp201905004
[14] Saltzman M R, Young S A. Long-lived glaciation in the Late Ordovician:Isotopic and sequence-stratigraphic evidence from western Laurentia[J]. Geology, 2005, 33(2):109-112. http://www.researchgate.net/publication/253886401_Long-lived_glaciation_in_the_Late_Ordovician_Isotopic_and_sequence-stratigraphic_evidence_from_western_Laurentia
[15] Zhu M Y, Babcock L E, Peng S C. Advances in Cambrian stratigraphy and paleontology:Integrating correlation techniques, paleobiology, taphonomy and paleoenvironmental reconstruction[J]. Palaeoworld, 2006, 15(3/4):217-222. doi:  10.1016-j.palwor.2006.10.016/
[16] Sial A N, Peralta S, Ferreira V P, et al. Upper Cambrian carbonate sequences of the Argentine Precordillera and the Steptoean C-isotope positive excursion(SPICE)[J]. Gondwana Research, 2008, 13(4):437-452. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=e4830db14770f9900fa094f1be018a43
[17] 孟祥化, 乔秀夫, 葛铭.华北古浅海碳酸盐风暴沉积和丁家滩相序模式[J].沉积学报, 1986, 4(2):1-18. http://www.cjxb.ac.cn/CN/abstract/abstract1810.shtml

Meng Xianghua, Qiao Xiufu, Ge Ming. Study on ancient shallow sea carbonate storm deposits(tempestite)in North China and Dingjiatan model of facies sequences[J]. Acta Sedimentologica Sinica, 1986, 4(2):1-18. http://www.cjxb.ac.cn/CN/abstract/abstract1810.shtml
[18] 冯增昭, 彭勇民, 金振奎, 等.中国晚寒武世岩相古地理[J].古地理学报, 2002, 4(3):1-10. http://d.old.wanfangdata.com.cn/Periodical/gdlxb200203001

Feng Zengzhao, Peng Yongmin, Jin Zhenkui, et al. Lithofacies palaeogeography of the Late Cambrian in China[J]. Journal of Palaeogeography, 2002, 4(3):1-10. http://d.old.wanfangdata.com.cn/Periodical/gdlxb200203001
[19] 余宽宏, 畅通, 邱隆伟, 等.华北地台早古生代竹叶状灰岩岩石特征及成因研究进展[J].沉积学报, 2015, 33(6):1111-1125. http://www.cjxb.ac.cn/CN/abstract/abstract3595.shtml

Yu Kuanhong, Chang Tong, Qiu Longwei, et al. Research development of flat-pebble conglomerate characteristics and their origin in Early Paleozoic North China Platform[J]. Acta Sedimentologica Sinica, 2015, 33(6):1111-1125. http://www.cjxb.ac.cn/CN/abstract/abstract3595.shtml
[20] 肖飞, 汪建国, 吴和源, 等.华北地区中北部寒武系层序地层格架[J].石油学报, 2017, 38(10):1144-1157, 1167. http://d.old.wanfangdata.com.cn/Periodical/syxb201710005

Xiao Fei, Wang Jianguo, Wu Heyuan, et al. Cambrian sequence stratigraphic framework in the middle-northern North China[J]. Acta Petrolei Sinica, 2017, 38(10):1144-1157, 1167. http://d.old.wanfangdata.com.cn/Periodical/syxb201710005
[21] 倪胜利.北京西郊下苇甸剖面寒武系叠层石中的底栖鲕粒:基本特征和重要意义[J].地质通报, 2017, 36(2/3):485-491. http://d.old.wanfangdata.com.cn/Periodical/zgqydz201702030

Ni Shengli. The benthic oolite within the stromatolitic bioherm of the Cambrian strata at the Xiaweidian section in the western suburb of Beijing:Essential features and important significance[J]. Geological Bulletin of China, 2017, 36(2/3):485-491. http://d.old.wanfangdata.com.cn/Periodical/zgqydz201702030
[22] 梅冥相, 张瑞, 李屹尧, 等.华北地台东北缘寒武系芙蓉统叠层石生物丘中的钙化蓝细菌[J].岩石学报, 2017, 33(4):1073-1093. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201704005

Mei Mingxiang, Zhang Rui, Li Yiyao, et al. Calcified cyanobacterias within the stromatolotic bioherm for the Cambrian Furongian Series in the northeastern margin of the North-China Platform[J]. Acta Petrologica Sinica, 2017, 33(4):1073-1093. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201704005
[23] 肖恩照, 王皓, 覃英伦, 等.寒武纪芙蓉统均一石沉积组构及环境特征:以河北涞源长山组为例[J].沉积学报, 2020, 38(1):76-90. http://www.cjxb.ac.cn/CN/abstract/abstract4073.shtml

Xiao Enzhao, Wang Hao, Qin Yinglun, et al. Sedimentary fabrics and environmental characteristics of leiolite in Cambrian:A case study from the Changshan Formation in Laiyuan city, Hebei province[J]. Acta Sedimentologica Sinica, 2020, 38(1):76-90. http://www.cjxb.ac.cn/CN/abstract/abstract4073.shtml
[24] 孟祥化, 葛铭, Tucker M E.中国晚寒武世长山期最大海泛事件及其全球对比意义[J].地质学报, 1996, 70(2):108-120. http://www.cnki.com.cn/Article/CJFDTotal-DZXE199602001.htm

Meng Xianghua, Ge Ming, Tucker M E. Changshanian maximum sea flooding events and their global correlation[J]. Acta Geologica Sinica, 1996, 70(2):108-120. http://www.cnki.com.cn/Article/CJFDTotal-DZXE199602001.htm
[25] 史晓颖, 陈建强, 梅仕龙.华北地台东部寒武系层序地层年代格架[J].地学前缘, 1997, 4(3/4):161-173. http://www.cnki.com.cn/Article/CJFDTotal-DXQY7Z2.026.htm

Shi Xiaoying, Chen Jianqiang, Mei Shilong. Cambrian sequence chronostratigraphic frame work of the North China Platform[J]. Earth Science Frontiers, 1997, 4(3/4):161-173. http://www.cnki.com.cn/Article/CJFDTotal-DXQY7Z2.026.htm
[26] 梅冥相.从旋回的有序叠加形式到层序的识别和划分:层序地层学进展之三[J].古地理学报, 2011, 13(1):37-54. http://d.old.wanfangdata.com.cn/Periodical/gdlxb201101005

Mei Mingxiang. From vertical stacking pattern of cycles to discerning and division of sequences:The third advance in sequence stratigraphy[J]. Journal of Palaeogeography, 2011, 13(1):37-54. http://d.old.wanfangdata.com.cn/Periodical/gdlxb201101005
[27] Anderson E J, Goodwin P W. The significance of metre-scale allocycles in the quest for a fundamental stratigraphic unit[J]. Journal of the Geological Society, 1990, 147(3):507-518. http://www.researchgate.net/publication/249546514_The_significance_of_metre-scale_allocycles_in_the_quest_for_a_fundamental_stratigraphic_unit
[28] 赵宗举.全球海平面变化指标及海相构造层序研究方法:以塔里木盆地奥陶系为例[J].石油学报, 2015, 36(3):262-273. http://d.old.wanfangdata.com.cn/Periodical/syxb201503002

Zhao Zongju. Indicators of global sea-level change and research methods of marine tectonic sequences:Take Ordovician of Tarim Basin as an example[J]. Acta Petrolei Sinica, 2015, 36(3):262-273. http://d.old.wanfangdata.com.cn/Periodical/syxb201503002
[29] 吴和源, 赵宗举, 汪建国, 等.华北克拉通北缘寒武系层序地层划分[J].吉林大学学报(地球科学版), 2018, 48(6):1609-1624. http://d.old.wanfangdata.com.cn/Periodical/cckjdxxb201806001

Wu Heyuan, Zhao Zongju, Wang Jianguo, et al. Cambrian sequence stratigraphic framework in northern margin of North China Craton[J]. Journal of Jilin University(Earth Science Edition), 2018, 48(6):1609-1624. http://d.old.wanfangdata.com.cn/Periodical/cckjdxxb201806001
[30] Osleger D, Read J F. Relation of eustasy to stacking patterns of meter-scale carbonate cycles, Late Cambrian, U. S. A. J]. Journal of Sedimentary Research, 1991, 61(7): 1225-1252.
[31] Allan J R, Matthews R K. Isotope signatures associated with early meteoric diagenesis[J]. Sedimentology, 1982, 29(6):797-817. doi:  10.1111-j.1365-3091.1982.tb00085.x/
[32] Calvet F, Tucker M E. Outer ramp cycles in the Upper Muschelkalk of the Catalan Basin, Northeast Spain[J]. Sedimentary Geology, 1988, 57(3/4):185-198. http://www.sciencedirect.com/science/article/pii/0037073888900267
[33] Loucks R G. Domal, thrombolitic, microbialite biostromes and associated lithofacies in the Upper Albian Devils River Trend along the northern, high-energy margin of the Maverick Basin[J]. Sedimentary Geology, 2018, 371:75-88. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ec7778ab75b0441b7bcaa52bb2785dea
[34] Chen J T, Chough S K, Han Z Z, et al. An extensive erosion surface of a strongly deformed limestone bed in the Gushan and Chaomidian formations(Late Middle Cambrian to Furongian), Shandong province, China:Sequence-stratigraphic implications[J]. Sedimentary Geology, 2011, 233(1/2/3/4):129-149. http://www.sciencedirect.com/science/article/pii/S0037073810003179
[35] Chen J T, Chough S K, Lee J H, et al. Sequence-stratigraphic comparison of the Upper Cambrian Series 3 to Furongian succession between the Shandong region, China and the Taebaek area, Korea:High variability of bounding surfaces in an epeiric platform[J]. Geosciences Journal, 2012, 16(4):357-379. doi:  10.1007/s12303-012-0040-5
[36] McLennan S M. Rare earth elements in sedimentary rocks; influence of provenance and sedimentary processes[J]. Reviews in Mineralogy and Geochemistry, 1989, 21(1):169-200. https://www.researchgate.net/publication/313503357_Rare_earth_elements_in_sedimentary_rocks_influence_of_provenance_and_sedimentary_processes
[37] Haq B U, Schutter S R. A chronology of Paleozoic sea-level changes[J]. Science, 2008, 322(5898):64-68. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=604d8f2cb85106dd2b06bbc42e87d69a
[38] 王鹏万, 斯春松, 张润合, 等.滇黔北坳陷寒武系碳酸盐岩古海洋环境特征及地质意义[J].沉积学报, 2016, 34(5):811-818. http://www.cjxb.ac.cn/CN/abstract/abstract3689.shtml

Wang Pengwan, Si Chunsong, Zhang Runhe, et al. Characteristic of the Cambrian carbonate paleo-ocean environment in the Dianqianbei Depression and its geological significance[J]. Acta Sedimentologica Sinica, 2016, 34(5):811-818. http://www.cjxb.ac.cn/CN/abstract/abstract3689.shtml
[39] Kaufman A J, Knoll A H. Neoproterozoic variations in the Cisotopic composition of seawater:Stratigraphic and biogeochemical implications[J]. Precambrian Research, 1995, 73(1/2/3/4):27-49. http://www.sciencedirect.com/science/article/pii/0301926894000708
[40] Hayes J M, Strauss H, Kaufman A J. The abundance of 13C in marine organic matter and isotopic fractionation in the global biogeochemical cycle of carbon during the past 800 Ma[J]. Chemical Geology, 1999, 161(1/2/3):103-125. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=d4db1496349b70f4e06af79409cfedc8
[41] Kump L R, Arthur M A. Interpreting carbon-isotope excursions:Carbonates and organic matter[J]. Chemical Geology, 1999, 161(1/2/3):181-198. http://d.old.wanfangdata.com.cn/NSTLQK/NSTL_QKJJ0210439382/
[42] 常华进, 储雪蕾, 冯连君, 等.氧化还原敏感微量元素对古海洋沉积环境的指示意义[J].地质评论, 2009, 55(1):91-99. http://d.old.wanfangdata.com.cn/Periodical/dzlp200901011

Chang Huajin, Chu Xuelei, Feng Lianjun, et al. Redox sensitive trace elements as paleoenvironments proxies[J]. Geological Review, 2009, 55(1):91-99. http://d.old.wanfangdata.com.cn/Periodical/dzlp200901011
[43] 腾格尔, 刘文汇, 徐永昌, 等.缺氧环境及地球化学判识标志的探讨:以鄂尔多斯盆地为例[J].沉积学报, 2004, 22(2):365-372. http://d.old.wanfangdata.com.cn/Periodical/cjxb200402026

Tonger, Liu Wenhui, Xu Yongchang, et al. The discussion on anoxic environments and its geochemical identifying indices[J]. Acta Sedimentologica Sinica, 2004, 22(2):365-372. http://d.old.wanfangdata.com.cn/Periodical/cjxb200402026
[44] German C R, Elderfield H. Rare earth elements in Saanich Inlet, British Columbia, a seasonally anoxic basin[J]. Geochimica et Cosmochimica Acta, 1989, 53(10):2561-2571. http://www.sciencedirect.com/science/article/pii/0016703789901282
[45] Lawrence M G, Greig A, Collerson K D, et al. Rare earth element and yttrium variability in South East Queensland waterways[J]. Aquatic Geochemistry, 2006, 12(1):39-72. doi:  10.1007-s10498-005-4471-8/
[46] Schrag D P, Berner R A, Hoffman P F, et al. On the initiation of a snowball Earth[J]. Geochemistry, Geophysics, Geosystems, 2002, 3(6):1-21. http://d.old.wanfangdata.com.cn/OAPaper/oai_doaj-articles_8bcccf34131fa5dc679f9309b3458e69