四川盆地及周缘地区震旦(埃迪卡拉)系划分与对比
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摘要
通过对四川盆地及周缘十余条露头剖面和覆盖区数十口油气探井的研究,将四川盆地及周缘震旦(埃迪卡拉)系划分为雅安—南江、峨边—仪陇、威远—开县、宜宾—石柱、雷波、龙门山、城口—巫溪、桐梓—恩施和沿河—大庸等9个地层小区,对其中在油气勘探中较重要的4个小区的地层基本特征作了阐述。将震旦系划分为下部的陡山沱组/喇叭岗组和上部的灯影组,后者进一步分为4个岩性段。把灯影组中上部的一套碎屑岩视为一个标志性的岩性段;并将原归于灯影组顶部,以麦地坪段为代表,含早寒武世小壳类化石的地层从该组中分出,作为寒武系底部的一个组一级岩石地层单位。依据最新的中国震旦系年代地层划分标准,将震旦系底界置于陡山沱组盖帽白云岩之底,顶以麦地坪组底平行不整合为界;陡山沱组相当于震旦系下统到上统下部,即包括下统九龙湾阶、陈家园子阶和上统下部吊崖坡阶,而喇叭岗组只相当于吊崖坡阶,灯影组则仅相当于上统上部灯影峡阶。以岩性、古生物、稳定碳同位素、放射性同位素测年以及测井曲线等为依据建立了四川盆地及周缘震旦系的对比关系,并与湖北峡东地区震旦系标准剖面进行了对比。
Based on stratigraphic data from more than 10 outcrops sections and several dozens of boreholes,nine stratigraphic sub-regions have been recognized for the Sinian(Ediacaran)System of the Sichuan Basin and its adjacent area.They are:1)the Ya'an-Nanjiang stratigraphic sub-region,2)the Ebian-Yilong stratigraphic sub-region,3)the Weiyuan-Kaixian stratigraphic sub-region,4)the Yibin-Shizhu stratigraphic sub-region,5)the Leibo stratigraphic sub-region,6)the Longmenshan stratigraphic sub-region,7)the Chengkou-Wuxi stratigraphic subregion,8)the Tongzi-Enshi stratigraphic sub-region,and 9)the Yanhe-Dayong stratigraphic sub-region.Four of them are described in detail.The Sinian sequences are subdivided into the Doushantuo Formation/Labagang Formation and the Dengying Formation in ascending order.The latter includes four lithological members.A siliciclastic unit in the middle-upper Dengying Formation is considered as a key marker bed,which is considered as Member3 of the Dengying Formation.We propose that the Maidiping Member which yields early Cambrian small shelly animal fossils and was traditionally considered as the Member 4in the uppermost Dengying Formation,be removed from the Dengying Formation and be elevated to the Maidiping Formation.According to the latest chronostratigraphic chart of China,the base of the Sinian System is placed at the base of the Doushantuo cap dolostone,and the top of the Sinian System is represented by aparallel unconformity between the Dengying and Maidiping formations.The Doushantuo Formation corresponds to the Lower Sinian Series to the lower part of the Upper Sinian Series,including the Jiulongwan Stage,Chenjiayuanzi Stage and the Diaoyapo Stage.The Labagang Formation is only equivalent to the Diaoyapo Stage.The Dengying Formation corresponds to the Dengyingxia Stage of the upper part of the Upper Sinian Series.Stratigraphic correlation of the Sinian sequences of the Sichuan Basin and its adjacent area have been established based on lithostratigraphic,biostratigraphic,chemostratigraphic,geochronological,and well-log data.The sequence has also been correlated with the standard section of the Sinian System in the Yangzi Gorges area in Hubei Province.
Based on stratigraphic data from more than 10 outcrops sections and several dozens of boreholes,nine stratigraphic sub-regions have been recognized for the Sinian(Ediacaran)System of the Sichuan Basin and its adjacent area.They are:1)the Ya'an-Nanjiang stratigraphic sub-region,2)the Ebian-Yilong stratigraphic sub-region,3)the Weiyuan-Kaixian stratigraphic sub-region,4)the Yibin-Shizhu stratigraphic sub-region,5)the Leibo stratigraphic sub-region,6)the Longmenshan stratigraphic sub-region,7)the Chengkou-Wuxi stratigraphic subregion,8)the Tongzi-Enshi stratigraphic sub-region,and 9)the Yanhe-Dayong stratigraphic sub-region.Four of them are described in detail.The Sinian sequences are subdivided into the Doushantuo Formation/Labagang Formation and the Dengying Formation in ascending order.The latter includes four lithological members.A siliciclastic unit in the middle-upper Dengying Formation is considered as a key marker bed,which is considered as Member3 of the Dengying Formation.We propose that the Maidiping Member which yields early Cambrian small shelly animal fossils and was traditionally considered as the Member 4in the uppermost Dengying Formation,be removed from the Dengying Formation and be elevated to the Maidiping Formation.According to the latest chronostratigraphic chart of China,the base of the Sinian System is placed at the base of the Doushantuo cap dolostone,and the top of the Sinian System is represented by aparallel unconformity between the Dengying and Maidiping formations.The Doushantuo Formation corresponds to the Lower Sinian Series to the lower part of the Upper Sinian Series,including the Jiulongwan Stage,Chenjiayuanzi Stage and the Diaoyapo Stage.The Labagang Formation is only equivalent to the Diaoyapo Stage.The Dengying Formation corresponds to the Dengyingxia Stage of the upper part of the Upper Sinian Series.Stratigraphic correlation of the Sinian sequences of the Sichuan Basin and its adjacent area have been established based on lithostratigraphic,biostratigraphic,chemostratigraphic,geochronological,and well-log data.The sequence has also been correlated with the standard section of the Sinian System in the Yangzi Gorges area in Hubei Province.
引文
曹瑞骥,杨万容,尹磊明,张俊明,李再平,赵文杰.1979.西南地区的震旦系//中国科学院南京地质古生物研究所编.西南地区碳酸盐生物地层.北京:科学出版社.1-36.
曹瑞骥,赵文杰.1978.西南地区晚震旦世灯影组藻类植物群.中国科学院南京地质古生物研究所集刊,10:1-40.
陈孟莪,陈祥高,劳秋元.1975.陕南震旦系上部地层中的后生动物化石及其地层意义.地质科学,(2):181-190.
陈孟莪,陈忆元,钱逸.1981.峡东区震旦系—寒武系底部的管状化石.中国地质科学院天津地质矿产研究所所刊,3:117121.
陈孟莪,萧宗正,袁训来.1994a.晚震旦世的特种生物群落——庙河生物群新知.古生物学报,33(4):291-304.
陈孟莪,鲁刚毅,萧宗正.1994b.皖南上震旦统蓝田组的宏体藻类化石——蓝田植物群的初步研究.中国科学院地质研究所论文集:252-267.
陈孟莪,萧宗正.1991.峡东区上震旦统陡山沱组发现宏体化石.地质科学,(4):317-324.
陈孟莪.1999.震旦纪生命大爆炸!——浅论地史早期动物的演化.前寒武纪研究进展,22:36-47.
陈孝红,汪啸风,王传尚,李志宏,陈立德.1999.湘西震旦系留茶坡组炭质宏化石初步研究.华南地质矿产,(2):15-30.
陈宗清.2013.论四川盆地下古生界五次地壳运动与油气勘探.中国石油勘探,18(5):15-23.
程裕淇.1962.中国前寒武系//全国地层会议学术报告汇编总论.北京:科学出版社.103-117.
丁莲芳,李勇,胡夏嵩,肖娅萍,苏春乾,黄建成.1996.震旦纪庙河生物群.北京:地质出版社.1-221.
丁莲芳,张录易,李勇,董军社.1992.扬子地台北缘晚震旦世—早寒武世早期生物群研究.北京:科学技术文献出版社.1-156.
丁启秀,陈忆元.1981.湖北峡东地区震旦纪软体后生动物的发现及意义.地球科学,(2):53-57.
丁启秀,邢裕盛,尹崇玉,高林志.1993.湖北秭归庙河—莲沱地区灯影组管状化石及遗迹化石.地质论评,39(2):116-123.
丁文江,曾世英.1931.川广铁道路线初勘报告.地质专报,乙种,4:1-85.
樊茹,邓胜徽,张学磊.2011.寒武系碳同位素漂移事件的全球对比性分析.中国科学(地球科学),41(12):1829-1839.
高林志,乔秀夫.2005.震旦系//汪啸风,陈孝红.中国各地质时代地层划分与对比.北京:地质出版社.35-66.
何春荪.1942.云南澂江县东山磷矿地质.中央地质调查所地质汇报,35.
何廷贵,杨暹和.1982.扬子区西部下寒武统梅树村阶及小壳动物群.中国地质科学院成都地质矿产研究所所刊,3:69-95.
侯方浩,方少仙,王兴志,黄继祥,李凌,王安平,郭莉,李少华.1999.四川震旦系灯影组天然气藏储渗体的再认识.石油学报,20(6):16-21.
华洪,陈哲,张录易.2004a.Shaanxilithes在贵州的发现及其意义.地层学杂志,28(3):265-269.
华洪,陈哲,张录易.2004b.陕南早寒武世磷酸盐化囊胚期及原肠胚期动物化石.科学通报,49(2):177-180.
华洪,陈哲,张录易.2005.陕南新元古代末期微体管状疑难化石.古生物学报,44(4):487-493.
华洪,张录易,张子福,王静平.2000.晚震旦世高家山生物群化石新材料.古生物学报,39(3):381-390.
华洪,张录易,张子福,王静平.2001.高家山生物群化石组合面貌及其特征.地层学杂志,25(1):13-17.
刘鹏举,尹崇玉,陈寿铭.2012.华南峡东地区埃迪卡拉(震旦)纪年代地层划分初探.地质学报,86(6):850-866.
刘鹏举,尹崇玉,高林志,唐烽,陈寿铭.2009.湖北宜昌樟村坪埃迪卡拉系陡山沱组微体化石新材料及锆石SHRIMP U-Pb年龄.科学通报,54(6):774-780.
刘云焕,李勇,邵铁全,王瑶培,于波,韩会平,杨盒.2005.陕西南部早寒武世原始锥石类Carinachitids两新种记述.微体古生物学报,22(3):311-321.
刘云焕,李勇,邵铁全,朱志新,于波,王焯,张琬茜,李荣西.2006.陕西南部早寒武世具口部磷酸盐化Punctatus及胚胎化石研究.古生物学报,45(2):182-194.
罗惠麟,蒋志文,徐重九,宋学良,薛啸峰.1980.云南晋宁梅树村、王家湾震旦系-寒武系界线研究.地质学报,54(2):95-111.
罗惠麟,李勇,胡世学,傅晓平,侯蜀光,刘兴尧,李锋军,庞纪院,刘琦,2008.云南东部早寒武世马龙动物群和关山动物群.昆明:云南科技出版社.1-134.
罗惠麟,武希彻,欧阳麟.1991.云南东部震旦系-寒武系界线地层的相变与横向对比.岩相古地理,4:27-35.
全国地层委员会.2002.中国区域年代地层(地质年代)表说明书.北京:地质出版社.1-72.
全国地层委员会《中国地层表》编委会.2014.中国地层表(2014).北京:地质出版社..
四川省地质矿产局.1990.四川省区域地质志.北京:地质出版社.1-730.
四川石油管理局川西研究队下古生界组.1970.川西地区震旦系地层含油气远景初步总结.
谭锡畴,李春昱.1933.四川峨眉山地质.中央地质调查所地质汇报,20:13-42.
谭锡畴,李春昱.1931.西康东部地质矿产志略.中央地质调查所地质汇报,19.
唐烽,宋学良,尹崇玉,刘鹏举,Awramik S.M.,王自强,高林志.2006.华南滇东地区震旦(Ediacaran)系顶部Longfengshaniaceae藻类化石的发现及意义.地质学报,80(11):1643-1649.
唐烽,尹崇玉,高林志.1997.安徽休宁陡山沱期后生植物化石的新认识.地质学报,71:289-296.
唐烽,尹崇玉,刘鹏举,王自强,高林志.2007.滇东埃迪卡拉(震旦)系顶部旧城段多样宏体化石群的发现.古地理学报,9(5):533-54.
唐天福,张俊明,蒋先健.1978.湘鄂西部晚震旦世地层与生物的发现及其意义.地层学杂志,2(1):32-44.
汪啸风,陈孝红,王传尚,陈立德.2001.震旦系底界及内部年代地层单位划分.地层学杂志,25(增刊):370-378.
汪泽成,姜华,王铜山,鲁卫华,谷志东,徐安娜,杨雨,徐兆辉.2014.四川盆地桐湾期古地貌特征及成藏意义.石油勘探与开发,3:305-312.
王约,王训练,黄禹铭.2007.黔东北伊迪卡拉纪陡山沱组的宏体藻类.地球科学——中国地质大学学报,32(6):828-844.
项礼文,朱兆玲,李善姬,周志强.1999.中国地层典寒武系.北京:地质出版社.1-95.
谢家荣,郭文魁,王超翔.1941.叙昆铁路沿线昆明威宁间地质矿产调查.西南矿产勘测处临时报告,第一号.
谢家荣.1941.云南矿产概论.地质论评,6(1):1-42.
邢裕盛等.1989.中国地层中国的上前寒武系.北京:地质出版社.1-314.
邢裕盛,高振家,王自强,高林志,尹崇玉.1996.中国地层典新元古界.北京:地质出版社.1-117.
邢裕盛,刘桂芝,乔秀夫,高振家,王自强,朱鸿,陈忆元,全秋琦.1982.中国的上前寒武系//中国地质科学院主编.中国地层概论.北京:地质出版社.47-81.
邢裕盛,刘桂芝.1978.峡东震旦纪微古植物及其它化石的研究//湖北地质局三峡地层研究组.峡东地区震旦纪至二叠纪地层古生物.北京:地质出版社.109-127.
邢裕盛,乔秀夫,王自强,赵自强,马国干,林蔚兴.1987.震旦系的划分与对比//国际末前寒武系及寒武系地质讨论会论文摘要集.59.
邢裕盛,尹崇玉,高林志.1999.震旦系的范畴、时限及内部划分.现代地质,13(2):202-204.
邢裕盛,毕治国,王贤方,1985.皖南震旦系发现宏观藻类化石.中国地质科学院地质研究所所刊,12:32.
薛耀松,唐天福,俞从流.1992.贵州晚震旦世陡山沱期具骨骼动物化石的发现及其意义.古生物学报,31(5):530-539.
薛耀松,唐天福,俞从流.1995.贵州瓮安─开阳地区陡山沱期含磷岩系的大型球形绿藻化石.古生物学报,34(6):688-706.
杨暹和,陈远德.1981.西南地区地层总结震旦系.成都:地质部成都地质矿产研究所.1-164.
杨暹和,何原相,邓守和.1983.四川南江地区震旦系-寒武系界线及小壳化石群.中国地质科学院成都地质矿产研究所所刊,4:91-110.
殷继成,丁莲芳,何廷贵,李世麟,沈丽娟.1980.四川峨眉-甘洛地区震旦纪地层古生物及沉积环境.成都:四川人民出版社.1-231.
殷继成,何廷贵,李世麟,蔡学林,温春齐,袁海华,叶祥华.1993.四川盆地周边及邻区震旦亚代地质演化与成矿作用.成都:成都科技大学出版社.1-198.
殷宗军,朱茂炎.2010.埃迪卡拉纪瓮安生物群中动物胚胎化石研究进展.科技导报,6(28):103-111.
尹崇玉.2001.Papillomembrana compata在贵州瓮安的发现——兼论陡山沱期大型具刺疑源类的对比及时代.地层学杂志,25(4):253-260.
尹崇玉,刘鹏举,陈寿铭,唐烽,高林志,王自强.2009.峡东地区埃迪卡拉系陡山沱组疑源类生物地层序列.古生物学报,48(2):146-154.
尹崇玉,柳永清,高林志.2007.震旦(伊迪卡拉)纪早期磷酸盐化生物群——瓮安生物群特征及其环境演化.北京:地质出版社.1-132.
尹磊明,李再平.1978.西南地区前寒武纪微体植物群及其地层意义.中国科学院南京地质古生物研究所所刊,10:41-108.
尹赞勋,徐道一,浦庆余.1965.中国地壳运动名称资料汇编.地质论评,1965,23(增刊):20-81
袁训来,王启飞,张昀.1993.贵州瓮安磷矿晚前寒武纪陡山沱期的藻类化石群.微体古生物学报,10(4):409-420.
袁训来,肖书海,尹磊明,安德鲁.诺尔,周传明,穆西南.2002.陡山沱期生物群——早期动物辐射前夕的生命.合肥:中国科学技术出版社.1-171.
袁训来,陈哲,肖书海,万斌,关成国,王伟,周传明,华洪.2012.蓝田生物群:一个认识多细胞生物起源和早期演化的新窗.科学通报,57(34):3219-3227.
岳昭,何廷贵.1989.四川甘洛、峨眉早寒武世小壳化石再研究.微体古生物学报,6(4):389-407.
曾繁礽,何春荪.1949.瓦山峨嵋山区之地质构造.地质学报,29(1-4):111-126.
张录易,董军社,田淑华.1992.高家山生物群//丁莲芳.扬子地台北缘晚震旦世—早寒武世早期生物群研究.北京:科学技术文献出版社.33-63.
张云湘,段国连,李存帅等.1958.力马河铜矿成矿规律的初步探讨.地质月刊,6:19-28.
赵亚曾.1929.四川地质简报.中国地质学会志,8(2):137-149.
赵自强,邢裕盛,丁启秀等.1988.湖北震旦系.武汉:中国地质大学出版社.1-205.
赵自强,邢裕盛,马国干.1980.湖北峡东震旦系//中国地质科学院天津地质矿产研究所.中国震旦亚界(前寒武地质研究).天津:天津科学技术出版社.31-55.
中国科学院南京地质古生物研究所.1974.西南地区地层古生物手册.北京:科学出版社.1-454.
中国科学院南京地质古生物研究所.1979.西南地区碳酸盐生物地层.北京:科学出版社.1-336.
朱茂炎.2010.动物的起源和寒武纪大爆发:来自中国的化石证据.古生物学报,49(3):269-287.
Heim A.1932.四川峨眉山地质构造之研究.徐瑞麟译.两广地质调查所特刊,13号.
Cai Y P,Hua H,Schiffbauer J D,Sun B&Yuan X L.2014.Tube\sgrowth patterns and microbial mat-related lifestyles in the Ediacaran fossil Cloudina,Gaojiashan Lagersttte,South China.Gondwana Research,25(3):1008-1018.
Cai Y P,Hua H,Xiao S H,Schiffbauer J D&Li P.2010.Biostratinomy of the late Ediacaran pyritized Gaojiashan Lagersttte\sfrom southern Shaanxi,South China:importance of event deposits.Palaios,25:487-506.
Cai Y P,Hua H&Zhang X L.2013.Tube construction and life\smode of the Late Ediacaran tubular fossil Gaojiashania cyclus\sfrom the Gaojiashan Lagersttte.Precambrian Research,224:255-267.
Cai Y P,Schiffbauer J D,Hua H&Xiao S H.2012.Preservational\smodes in the Ediacaran Gaojiashan Lagersttte:pyritization,aluminosilicification,and carbonaceous compression.Palaeogeography Palaeoclimatology Palaeoecology,326-328:109-117.
Cai Y P,Schiffbauer J D,Hua H&Xiao S H.2011.Morphology\sand paleoecology of the late Ediacaran tubular fossil Conotubus\shemiannulatus from the Gaojiashan Lagersttte of southern\sShaanxi Province,South China.Precambrian Research,191:46-57.
Chen Z,Bengtson S,Zhou C M,Hua H&Yue Z.2008.Tube\sstructure and original composition of Sinotubulites:shelly fossils from the late Neoproterozoic in southern Shaanxi,China.Lethaia,41:37-45.
Chen Z,Zhou C M,Xiao S H,Wang W,Guan C G,Hua H&Yuan X L.2014.New Ediacara fossils preserved in marine\slimestone and their ecological implications.Scientific Report,4:41-80.
Chen Z,Zhou C M,Meyerb M,Xiang K,Schiffbauer D J,Yuan XL&Xiao S H.2013.Trace fossil evidence for Ediacaran bilaterian animals with complex behaviors.Precambrian Research,224:690-701.
Condon D,Zhu M Y,Bowring S,Wang W,Yang A H&Jin Y G.2005.U-Pb ages from the Neoproterozoic Doushantuo Formation,China.Science,308(1):95-98.
Hua H,Chen Z,Yuan X L,Zhang LY&Xiao S H.2005.Skeletogenesis and asexual reproduction in the earliest biomineralizing\sanimal Cloudina.Geology,33:277-280.
Hua H,Chen Z&Yuan X L.2007.The advent of mineralized skeletons in Neoproterozoic Metazoa:new fossil evidence from the\sGaojiashan Fauna.Geological Journal,42:263-279.
Hua H,Pratt B R&Zhang L Y.2003.Borings in Cloudinashells:complex predatorprey dynamics in the terminal Neoproterozoic.Palaios,18:454-459.
Lee J S&Chao Y T.1924.Geology of the Gorge district of the\sYangtze(from Ichang to Tzekuei)with special reference to development of the Goeges.Bull Geol Soc China,3(3-4):351-391.
Li C W,Chen J Y&Hua T.1998.Precambrian sponges with cellular structures.Science,279:879-882.
Ling H F,Feng H Z,Pan J Y,Jiang S Y,Chen Y Q&Chen X.2007.Carbon isotope variation through the Neoproterozoic\sDoushantuo and Dengying Formations,South China:implications for chemostratigraphy and paleoenvironmental change.Palaeogeography,Palaeoclimatology,Palaeoecology,254:158-174.
Liu P J,Chen S M,Zhu M Y,Li M,Yin C Y&Shang X D.2014b.High-resolution biostratigraphic and chemostratigraphic\sdata from the Chenjiayuanzi section of the Doushantuo Formation in the Yangtze Gorges area,South China:implication for\ssubdivision and global correlation of the Ediacaran System.Precambrian Research,249:199-214.
Liu P J,Xiao S H,Yin C Y,Chen S M,Zhou C M&Li M.2014a.Ediacaran acanthomophic acritarchs and other microfossils from\schert nodules of the upper Doushantuo Formation in the Yangtze Gorges area,South China.Journal of Paleontology,88(supplement):1-139.
Liu P J,Xiao S H,Yin C Y,Tang F&Gao L Z.2009.Silicified\stubular microfossils from the upper Doushantuo Formation(Ediacaran)in the Yangtze Gorges area,South China.Journal\sof Palaeontology,83(4):630-633.
Liu P J,Xiao S H,Yin C Y,Zhou C M,Gao L Z&Tang F.2008.Systematic description and phylogenetic affinity of tubular microfossils from the Ediacaran Doushantuo Formation at Weng'an\sSouth China.Palaeontology,51(2):339-366.
Liu P J,Yin C Y,Chen S M,Tang F&Gao L Z.2013.The biostratigraphic succession of acan-thomorphic acritarchs of the Ediacaran Doushantuo Formation in the Yangtze Gorges area,South China and its biostratigraphic correlation with Australia.Precambrian Research,225:29-43.
Liu P J,Yin C Y&Tang F.2006.Discovery of the budding phosphatized globular fossils from the Neoproterozoic Doushantuo\sFormation at Weng'an,Guizhou Province,China.Progress in\sNature Science,16(10):1079-1083.
Meyer M,Schiffbauer J D,Xiao S H,Cai Y P&Hua H.2012.Taphonomy of the late Ediacaran enigmatic ribbon-like fossil\sShaanxilithes.Palaios,27:354-372.
Misch P.1942.Sinian stratigraphy of central easteral eastern Yunnan.The National University of Peking,College of Science\sContribution,4.
Steiner M,Erdtmann B-D&Chen J Y.1992.Preliminary assessment of new Late Sinian(Late Neoproterozoic)large siphonous\sand filamentous“megaalage”from eastern Wulingshan,north\scentral Hunan,China.Berliner Geowissens Chaftliche Abhandlungen(E):305-319.
Tang F,Yin C Y,Bengtson S,Liu P J,Wang Z&Gao L Z.2008.Octoradiate spiral organisms in the Ediacaran of South China:Acta Geologica Sinica.82:27-34.
Weber B,Steiner M&Zhu M Y.2007.Precambrian-Cambrian\strace fossils from the Yangtze Platform(South China)and the\searly evolution of bilaterian lifestyles.Palaeogeography,Palaeoclimatology,Palaeoecology,254:328-349.
Xiao S H,Hagadorn J W,Zhou C M&Yuan X L.2007.Rare helical spheroidal fossils from the Doushantuo Lagersta¨tte:Ediacaran animal embryos come of age?Geology,35:115-118.
Xiao S H,Shen B,Zhou C M,Xie G W&Yuan X L.2005.A uniquely preserved Ediacaran fossil with direct evidence for a\squilted bodyplan.Proceedings of the National Academy of Sciences,USA,102:10227-10232.
Xiao S H,Yuan X L,Steiner M&Knoll A H.2002.Macroscopic\scarbonaceous compressions in a terminal Proterozoic shale:a\ssystematic reassessment of the Miaohe biota,South China.Journal of Paleontology,76:347-376.
Xiao S H,Zhang Y&Knoll A H.1998.Three-dimensional preservation of algae and animal embryos in a Neoproterozoicphos\sphorite.Nature,391:553-558.
Xiao S H,Zhou C M,Liu P J,Wang D&Yuan X L.2014.Phosphatized acanthomorphic acritarchs and related microfossils from\sthe Ediacaran Doushantuo Formation at Weng'an(South China)and their implications for biostratigraphic correlation.Journal of\sPaleontology,88:1-67.
Yin L M&Xue Y S.1993.An extraordinary microfossil assemblage from Terminal Proterozoic phosphate deposits in South\sChina.Chinese Journal of Botany,5:168-175.
Yuan X L,Li J&Cao R J.1999.A diverse metaphyte assemblage\sfrom the Neoproterozoic black shales of South China.Lethaia,32:143-155.
Yuan X L&Hofmann H J.1998.New micropaleontological data\sfrom Neoproterozoic Sinian Doushantuo phosphorite rocks,Weng'an,Guizhou Province,Southwestern China.Alcheringa,22:189-222.
Yuan X L,Xiao S H,Li J,Yin L M&Cao R J.2001.Pyritized\schuarids with excystment structures from the late Neoproterozoic Lantian Formation in Anhui,South China.Precambrian\sResearch,107:251-261.
Yuan X L,Chen Z,Xiao S H,Zhou C M&Hua H.2011.An early\sEdiacaran assemblage of macroscopic and morphologically differentiated eukaryotes.Nature,470:390-393.
Zhang S H,Jiang G Q,Zhang J M,Song B,Kennedy J M&Christie-Blick N.2005.U-Pb sensitive high-resolution ion microprobe ages from the Doushantuo Formation in South China:constraints on Late Neoproterozoic glaciations.Geology,33(6):473-476.
Zhang Y,Yin L M,Xiao S H&Knoll A H.1998.Permineralized\sfossils from the terminal Doushantou Formation,South China.The Paleontological Society,Journal of Palaeontology,Memoir,50:1-52.
Zhao Y L,Chen M E,Peng J,Yu M Y,He M H,Wang Y,YangR D,Wang P L&Zhang Z H.2004.Discovery of a Miaohetype Biota from the Neoproterozoic Doushantuo Formation in\sJiangkou County,Guizhou Province,China.Chinese Science\sBulletin,49:2224-2226.
Zhou C M&Xiao S H.2007.Ediacaran Delta-13 C chemostratigraphy of South China.Chemical Geology,237:89-108.
Zhu M Y,Babcock L E&Peng S C.2006.Advances in Cambrian\sstratigraphy and paleontology:integrating correlation techniques,palaeobiology,taphonomy and paleoenvironmental reconstruction.Palaeoworld,15:217-222.
Zhu M Y,Gehling G J,Xiao S H,Zhao Y L&Droser L M.2008.Eight-armed Ediacara fossil preserved in contrasting taphonomic\swindows from China and Australia.Geology,36:867-870.
Zhu M Y,Zhang J M&Yang A H.2007.Integrated Ediaearan(Sinian)chronostratigraphy of South China Palaeogeography,Palaeoelimatology,Palaeoeeology,254(1-2):7-61.
Zhu M Y&Zhang J M.2005.Ediacaran-Cambrian boundary sections and Early Cambrian Chengjiang nonmineralized fossils in\seastern Yunnan Province,southwestern China:Introduction//Peng S C,Babcock L,Zhu M Y&Li G X eds.Cambrian System of China and Korea.Guide to Field Excursions.Hefei:U-niversity of Science and Technology of China Press.1-12.
Zhu M Y.2007.From snowball earth to the Cambrian bioradiation:calibration of Ediacaran-Cambrian earth history in South China.Palaeogeography,Palaeoclimatology,Palaeoecology,254:1-6.
Zhu M Y,Lu M,Zhang J M,Zhao F C,Li G X,Yang A H,Zhao\sX&Zhao M J.2013.Carbon isotope chemostratigraphy and\ssedimentary facies evolution of the Ediacaran Doushantuo Formation in western Hubei,South China.Precambrian Research,225:7-28.
曹瑞骥,赵文杰.1978.西南地区晚震旦世灯影组藻类植物群.中国科学院南京地质古生物研究所集刊,10:1-40.
陈孟莪,陈祥高,劳秋元.1975.陕南震旦系上部地层中的后生动物化石及其地层意义.地质科学,(2):181-190.
陈孟莪,陈忆元,钱逸.1981.峡东区震旦系—寒武系底部的管状化石.中国地质科学院天津地质矿产研究所所刊,3:117121.
陈孟莪,萧宗正,袁训来.1994a.晚震旦世的特种生物群落——庙河生物群新知.古生物学报,33(4):291-304.
陈孟莪,鲁刚毅,萧宗正.1994b.皖南上震旦统蓝田组的宏体藻类化石——蓝田植物群的初步研究.中国科学院地质研究所论文集:252-267.
陈孟莪,萧宗正.1991.峡东区上震旦统陡山沱组发现宏体化石.地质科学,(4):317-324.
陈孟莪.1999.震旦纪生命大爆炸!——浅论地史早期动物的演化.前寒武纪研究进展,22:36-47.
陈孝红,汪啸风,王传尚,李志宏,陈立德.1999.湘西震旦系留茶坡组炭质宏化石初步研究.华南地质矿产,(2):15-30.
陈宗清.2013.论四川盆地下古生界五次地壳运动与油气勘探.中国石油勘探,18(5):15-23.
程裕淇.1962.中国前寒武系//全国地层会议学术报告汇编总论.北京:科学出版社.103-117.
丁莲芳,李勇,胡夏嵩,肖娅萍,苏春乾,黄建成.1996.震旦纪庙河生物群.北京:地质出版社.1-221.
丁莲芳,张录易,李勇,董军社.1992.扬子地台北缘晚震旦世—早寒武世早期生物群研究.北京:科学技术文献出版社.1-156.
丁启秀,陈忆元.1981.湖北峡东地区震旦纪软体后生动物的发现及意义.地球科学,(2):53-57.
丁启秀,邢裕盛,尹崇玉,高林志.1993.湖北秭归庙河—莲沱地区灯影组管状化石及遗迹化石.地质论评,39(2):116-123.
丁文江,曾世英.1931.川广铁道路线初勘报告.地质专报,乙种,4:1-85.
樊茹,邓胜徽,张学磊.2011.寒武系碳同位素漂移事件的全球对比性分析.中国科学(地球科学),41(12):1829-1839.
高林志,乔秀夫.2005.震旦系//汪啸风,陈孝红.中国各地质时代地层划分与对比.北京:地质出版社.35-66.
何春荪.1942.云南澂江县东山磷矿地质.中央地质调查所地质汇报,35.
何廷贵,杨暹和.1982.扬子区西部下寒武统梅树村阶及小壳动物群.中国地质科学院成都地质矿产研究所所刊,3:69-95.
侯方浩,方少仙,王兴志,黄继祥,李凌,王安平,郭莉,李少华.1999.四川震旦系灯影组天然气藏储渗体的再认识.石油学报,20(6):16-21.
华洪,陈哲,张录易.2004a.Shaanxilithes在贵州的发现及其意义.地层学杂志,28(3):265-269.
华洪,陈哲,张录易.2004b.陕南早寒武世磷酸盐化囊胚期及原肠胚期动物化石.科学通报,49(2):177-180.
华洪,陈哲,张录易.2005.陕南新元古代末期微体管状疑难化石.古生物学报,44(4):487-493.
华洪,张录易,张子福,王静平.2000.晚震旦世高家山生物群化石新材料.古生物学报,39(3):381-390.
华洪,张录易,张子福,王静平.2001.高家山生物群化石组合面貌及其特征.地层学杂志,25(1):13-17.
刘鹏举,尹崇玉,陈寿铭.2012.华南峡东地区埃迪卡拉(震旦)纪年代地层划分初探.地质学报,86(6):850-866.
刘鹏举,尹崇玉,高林志,唐烽,陈寿铭.2009.湖北宜昌樟村坪埃迪卡拉系陡山沱组微体化石新材料及锆石SHRIMP U-Pb年龄.科学通报,54(6):774-780.
刘云焕,李勇,邵铁全,王瑶培,于波,韩会平,杨盒.2005.陕西南部早寒武世原始锥石类Carinachitids两新种记述.微体古生物学报,22(3):311-321.
刘云焕,李勇,邵铁全,朱志新,于波,王焯,张琬茜,李荣西.2006.陕西南部早寒武世具口部磷酸盐化Punctatus及胚胎化石研究.古生物学报,45(2):182-194.
罗惠麟,蒋志文,徐重九,宋学良,薛啸峰.1980.云南晋宁梅树村、王家湾震旦系-寒武系界线研究.地质学报,54(2):95-111.
罗惠麟,李勇,胡世学,傅晓平,侯蜀光,刘兴尧,李锋军,庞纪院,刘琦,2008.云南东部早寒武世马龙动物群和关山动物群.昆明:云南科技出版社.1-134.
罗惠麟,武希彻,欧阳麟.1991.云南东部震旦系-寒武系界线地层的相变与横向对比.岩相古地理,4:27-35.
全国地层委员会.2002.中国区域年代地层(地质年代)表说明书.北京:地质出版社.1-72.
全国地层委员会《中国地层表》编委会.2014.中国地层表(2014).北京:地质出版社..
四川省地质矿产局.1990.四川省区域地质志.北京:地质出版社.1-730.
四川石油管理局川西研究队下古生界组.1970.川西地区震旦系地层含油气远景初步总结.
谭锡畴,李春昱.1933.四川峨眉山地质.中央地质调查所地质汇报,20:13-42.
谭锡畴,李春昱.1931.西康东部地质矿产志略.中央地质调查所地质汇报,19.
唐烽,宋学良,尹崇玉,刘鹏举,Awramik S.M.,王自强,高林志.2006.华南滇东地区震旦(Ediacaran)系顶部Longfengshaniaceae藻类化石的发现及意义.地质学报,80(11):1643-1649.
唐烽,尹崇玉,高林志.1997.安徽休宁陡山沱期后生植物化石的新认识.地质学报,71:289-296.
唐烽,尹崇玉,刘鹏举,王自强,高林志.2007.滇东埃迪卡拉(震旦)系顶部旧城段多样宏体化石群的发现.古地理学报,9(5):533-54.
唐天福,张俊明,蒋先健.1978.湘鄂西部晚震旦世地层与生物的发现及其意义.地层学杂志,2(1):32-44.
汪啸风,陈孝红,王传尚,陈立德.2001.震旦系底界及内部年代地层单位划分.地层学杂志,25(增刊):370-378.
汪泽成,姜华,王铜山,鲁卫华,谷志东,徐安娜,杨雨,徐兆辉.2014.四川盆地桐湾期古地貌特征及成藏意义.石油勘探与开发,3:305-312.
王约,王训练,黄禹铭.2007.黔东北伊迪卡拉纪陡山沱组的宏体藻类.地球科学——中国地质大学学报,32(6):828-844.
项礼文,朱兆玲,李善姬,周志强.1999.中国地层典寒武系.北京:地质出版社.1-95.
谢家荣,郭文魁,王超翔.1941.叙昆铁路沿线昆明威宁间地质矿产调查.西南矿产勘测处临时报告,第一号.
谢家荣.1941.云南矿产概论.地质论评,6(1):1-42.
邢裕盛等.1989.中国地层中国的上前寒武系.北京:地质出版社.1-314.
邢裕盛,高振家,王自强,高林志,尹崇玉.1996.中国地层典新元古界.北京:地质出版社.1-117.
邢裕盛,刘桂芝,乔秀夫,高振家,王自强,朱鸿,陈忆元,全秋琦.1982.中国的上前寒武系//中国地质科学院主编.中国地层概论.北京:地质出版社.47-81.
邢裕盛,刘桂芝.1978.峡东震旦纪微古植物及其它化石的研究//湖北地质局三峡地层研究组.峡东地区震旦纪至二叠纪地层古生物.北京:地质出版社.109-127.
邢裕盛,乔秀夫,王自强,赵自强,马国干,林蔚兴.1987.震旦系的划分与对比//国际末前寒武系及寒武系地质讨论会论文摘要集.59.
邢裕盛,尹崇玉,高林志.1999.震旦系的范畴、时限及内部划分.现代地质,13(2):202-204.
邢裕盛,毕治国,王贤方,1985.皖南震旦系发现宏观藻类化石.中国地质科学院地质研究所所刊,12:32.
薛耀松,唐天福,俞从流.1992.贵州晚震旦世陡山沱期具骨骼动物化石的发现及其意义.古生物学报,31(5):530-539.
薛耀松,唐天福,俞从流.1995.贵州瓮安─开阳地区陡山沱期含磷岩系的大型球形绿藻化石.古生物学报,34(6):688-706.
杨暹和,陈远德.1981.西南地区地层总结震旦系.成都:地质部成都地质矿产研究所.1-164.
杨暹和,何原相,邓守和.1983.四川南江地区震旦系-寒武系界线及小壳化石群.中国地质科学院成都地质矿产研究所所刊,4:91-110.
殷继成,丁莲芳,何廷贵,李世麟,沈丽娟.1980.四川峨眉-甘洛地区震旦纪地层古生物及沉积环境.成都:四川人民出版社.1-231.
殷继成,何廷贵,李世麟,蔡学林,温春齐,袁海华,叶祥华.1993.四川盆地周边及邻区震旦亚代地质演化与成矿作用.成都:成都科技大学出版社.1-198.
殷宗军,朱茂炎.2010.埃迪卡拉纪瓮安生物群中动物胚胎化石研究进展.科技导报,6(28):103-111.
尹崇玉.2001.Papillomembrana compata在贵州瓮安的发现——兼论陡山沱期大型具刺疑源类的对比及时代.地层学杂志,25(4):253-260.
尹崇玉,刘鹏举,陈寿铭,唐烽,高林志,王自强.2009.峡东地区埃迪卡拉系陡山沱组疑源类生物地层序列.古生物学报,48(2):146-154.
尹崇玉,柳永清,高林志.2007.震旦(伊迪卡拉)纪早期磷酸盐化生物群——瓮安生物群特征及其环境演化.北京:地质出版社.1-132.
尹磊明,李再平.1978.西南地区前寒武纪微体植物群及其地层意义.中国科学院南京地质古生物研究所所刊,10:41-108.
尹赞勋,徐道一,浦庆余.1965.中国地壳运动名称资料汇编.地质论评,1965,23(增刊):20-81
袁训来,王启飞,张昀.1993.贵州瓮安磷矿晚前寒武纪陡山沱期的藻类化石群.微体古生物学报,10(4):409-420.
袁训来,肖书海,尹磊明,安德鲁.诺尔,周传明,穆西南.2002.陡山沱期生物群——早期动物辐射前夕的生命.合肥:中国科学技术出版社.1-171.
袁训来,陈哲,肖书海,万斌,关成国,王伟,周传明,华洪.2012.蓝田生物群:一个认识多细胞生物起源和早期演化的新窗.科学通报,57(34):3219-3227.
岳昭,何廷贵.1989.四川甘洛、峨眉早寒武世小壳化石再研究.微体古生物学报,6(4):389-407.
曾繁礽,何春荪.1949.瓦山峨嵋山区之地质构造.地质学报,29(1-4):111-126.
张录易,董军社,田淑华.1992.高家山生物群//丁莲芳.扬子地台北缘晚震旦世—早寒武世早期生物群研究.北京:科学技术文献出版社.33-63.
张云湘,段国连,李存帅等.1958.力马河铜矿成矿规律的初步探讨.地质月刊,6:19-28.
赵亚曾.1929.四川地质简报.中国地质学会志,8(2):137-149.
赵自强,邢裕盛,丁启秀等.1988.湖北震旦系.武汉:中国地质大学出版社.1-205.
赵自强,邢裕盛,马国干.1980.湖北峡东震旦系//中国地质科学院天津地质矿产研究所.中国震旦亚界(前寒武地质研究).天津:天津科学技术出版社.31-55.
中国科学院南京地质古生物研究所.1974.西南地区地层古生物手册.北京:科学出版社.1-454.
中国科学院南京地质古生物研究所.1979.西南地区碳酸盐生物地层.北京:科学出版社.1-336.
朱茂炎.2010.动物的起源和寒武纪大爆发:来自中国的化石证据.古生物学报,49(3):269-287.
Heim A.1932.四川峨眉山地质构造之研究.徐瑞麟译.两广地质调查所特刊,13号.
Cai Y P,Hua H,Schiffbauer J D,Sun B&Yuan X L.2014.Tube\sgrowth patterns and microbial mat-related lifestyles in the Ediacaran fossil Cloudina,Gaojiashan Lagersttte,South China.Gondwana Research,25(3):1008-1018.
Cai Y P,Hua H,Xiao S H,Schiffbauer J D&Li P.2010.Biostratinomy of the late Ediacaran pyritized Gaojiashan Lagersttte\sfrom southern Shaanxi,South China:importance of event deposits.Palaios,25:487-506.
Cai Y P,Hua H&Zhang X L.2013.Tube construction and life\smode of the Late Ediacaran tubular fossil Gaojiashania cyclus\sfrom the Gaojiashan Lagersttte.Precambrian Research,224:255-267.
Cai Y P,Schiffbauer J D,Hua H&Xiao S H.2012.Preservational\smodes in the Ediacaran Gaojiashan Lagersttte:pyritization,aluminosilicification,and carbonaceous compression.Palaeogeography Palaeoclimatology Palaeoecology,326-328:109-117.
Cai Y P,Schiffbauer J D,Hua H&Xiao S H.2011.Morphology\sand paleoecology of the late Ediacaran tubular fossil Conotubus\shemiannulatus from the Gaojiashan Lagersttte of southern\sShaanxi Province,South China.Precambrian Research,191:46-57.
Chen Z,Bengtson S,Zhou C M,Hua H&Yue Z.2008.Tube\sstructure and original composition of Sinotubulites:shelly fossils from the late Neoproterozoic in southern Shaanxi,China.Lethaia,41:37-45.
Chen Z,Zhou C M,Xiao S H,Wang W,Guan C G,Hua H&Yuan X L.2014.New Ediacara fossils preserved in marine\slimestone and their ecological implications.Scientific Report,4:41-80.
Chen Z,Zhou C M,Meyerb M,Xiang K,Schiffbauer D J,Yuan XL&Xiao S H.2013.Trace fossil evidence for Ediacaran bilaterian animals with complex behaviors.Precambrian Research,224:690-701.
Condon D,Zhu M Y,Bowring S,Wang W,Yang A H&Jin Y G.2005.U-Pb ages from the Neoproterozoic Doushantuo Formation,China.Science,308(1):95-98.
Hua H,Chen Z,Yuan X L,Zhang LY&Xiao S H.2005.Skeletogenesis and asexual reproduction in the earliest biomineralizing\sanimal Cloudina.Geology,33:277-280.
Hua H,Chen Z&Yuan X L.2007.The advent of mineralized skeletons in Neoproterozoic Metazoa:new fossil evidence from the\sGaojiashan Fauna.Geological Journal,42:263-279.
Hua H,Pratt B R&Zhang L Y.2003.Borings in Cloudinashells:complex predatorprey dynamics in the terminal Neoproterozoic.Palaios,18:454-459.
Lee J S&Chao Y T.1924.Geology of the Gorge district of the\sYangtze(from Ichang to Tzekuei)with special reference to development of the Goeges.Bull Geol Soc China,3(3-4):351-391.
Li C W,Chen J Y&Hua T.1998.Precambrian sponges with cellular structures.Science,279:879-882.
Ling H F,Feng H Z,Pan J Y,Jiang S Y,Chen Y Q&Chen X.2007.Carbon isotope variation through the Neoproterozoic\sDoushantuo and Dengying Formations,South China:implications for chemostratigraphy and paleoenvironmental change.Palaeogeography,Palaeoclimatology,Palaeoecology,254:158-174.
Liu P J,Chen S M,Zhu M Y,Li M,Yin C Y&Shang X D.2014b.High-resolution biostratigraphic and chemostratigraphic\sdata from the Chenjiayuanzi section of the Doushantuo Formation in the Yangtze Gorges area,South China:implication for\ssubdivision and global correlation of the Ediacaran System.Precambrian Research,249:199-214.
Liu P J,Xiao S H,Yin C Y,Chen S M,Zhou C M&Li M.2014a.Ediacaran acanthomophic acritarchs and other microfossils from\schert nodules of the upper Doushantuo Formation in the Yangtze Gorges area,South China.Journal of Paleontology,88(supplement):1-139.
Liu P J,Xiao S H,Yin C Y,Tang F&Gao L Z.2009.Silicified\stubular microfossils from the upper Doushantuo Formation(Ediacaran)in the Yangtze Gorges area,South China.Journal\sof Palaeontology,83(4):630-633.
Liu P J,Xiao S H,Yin C Y,Zhou C M,Gao L Z&Tang F.2008.Systematic description and phylogenetic affinity of tubular microfossils from the Ediacaran Doushantuo Formation at Weng'an\sSouth China.Palaeontology,51(2):339-366.
Liu P J,Yin C Y,Chen S M,Tang F&Gao L Z.2013.The biostratigraphic succession of acan-thomorphic acritarchs of the Ediacaran Doushantuo Formation in the Yangtze Gorges area,South China and its biostratigraphic correlation with Australia.Precambrian Research,225:29-43.
Liu P J,Yin C Y&Tang F.2006.Discovery of the budding phosphatized globular fossils from the Neoproterozoic Doushantuo\sFormation at Weng'an,Guizhou Province,China.Progress in\sNature Science,16(10):1079-1083.
Meyer M,Schiffbauer J D,Xiao S H,Cai Y P&Hua H.2012.Taphonomy of the late Ediacaran enigmatic ribbon-like fossil\sShaanxilithes.Palaios,27:354-372.
Misch P.1942.Sinian stratigraphy of central easteral eastern Yunnan.The National University of Peking,College of Science\sContribution,4.
Steiner M,Erdtmann B-D&Chen J Y.1992.Preliminary assessment of new Late Sinian(Late Neoproterozoic)large siphonous\sand filamentous“megaalage”from eastern Wulingshan,north\scentral Hunan,China.Berliner Geowissens Chaftliche Abhandlungen(E):305-319.
Tang F,Yin C Y,Bengtson S,Liu P J,Wang Z&Gao L Z.2008.Octoradiate spiral organisms in the Ediacaran of South China:Acta Geologica Sinica.82:27-34.
Weber B,Steiner M&Zhu M Y.2007.Precambrian-Cambrian\strace fossils from the Yangtze Platform(South China)and the\searly evolution of bilaterian lifestyles.Palaeogeography,Palaeoclimatology,Palaeoecology,254:328-349.
Xiao S H,Hagadorn J W,Zhou C M&Yuan X L.2007.Rare helical spheroidal fossils from the Doushantuo Lagersta¨tte:Ediacaran animal embryos come of age?Geology,35:115-118.
Xiao S H,Shen B,Zhou C M,Xie G W&Yuan X L.2005.A uniquely preserved Ediacaran fossil with direct evidence for a\squilted bodyplan.Proceedings of the National Academy of Sciences,USA,102:10227-10232.
Xiao S H,Yuan X L,Steiner M&Knoll A H.2002.Macroscopic\scarbonaceous compressions in a terminal Proterozoic shale:a\ssystematic reassessment of the Miaohe biota,South China.Journal of Paleontology,76:347-376.
Xiao S H,Zhang Y&Knoll A H.1998.Three-dimensional preservation of algae and animal embryos in a Neoproterozoicphos\sphorite.Nature,391:553-558.
Xiao S H,Zhou C M,Liu P J,Wang D&Yuan X L.2014.Phosphatized acanthomorphic acritarchs and related microfossils from\sthe Ediacaran Doushantuo Formation at Weng'an(South China)and their implications for biostratigraphic correlation.Journal of\sPaleontology,88:1-67.
Yin L M&Xue Y S.1993.An extraordinary microfossil assemblage from Terminal Proterozoic phosphate deposits in South\sChina.Chinese Journal of Botany,5:168-175.
Yuan X L,Li J&Cao R J.1999.A diverse metaphyte assemblage\sfrom the Neoproterozoic black shales of South China.Lethaia,32:143-155.
Yuan X L&Hofmann H J.1998.New micropaleontological data\sfrom Neoproterozoic Sinian Doushantuo phosphorite rocks,Weng'an,Guizhou Province,Southwestern China.Alcheringa,22:189-222.
Yuan X L,Xiao S H,Li J,Yin L M&Cao R J.2001.Pyritized\schuarids with excystment structures from the late Neoproterozoic Lantian Formation in Anhui,South China.Precambrian\sResearch,107:251-261.
Yuan X L,Chen Z,Xiao S H,Zhou C M&Hua H.2011.An early\sEdiacaran assemblage of macroscopic and morphologically differentiated eukaryotes.Nature,470:390-393.
Zhang S H,Jiang G Q,Zhang J M,Song B,Kennedy J M&Christie-Blick N.2005.U-Pb sensitive high-resolution ion microprobe ages from the Doushantuo Formation in South China:constraints on Late Neoproterozoic glaciations.Geology,33(6):473-476.
Zhang Y,Yin L M,Xiao S H&Knoll A H.1998.Permineralized\sfossils from the terminal Doushantou Formation,South China.The Paleontological Society,Journal of Palaeontology,Memoir,50:1-52.
Zhao Y L,Chen M E,Peng J,Yu M Y,He M H,Wang Y,YangR D,Wang P L&Zhang Z H.2004.Discovery of a Miaohetype Biota from the Neoproterozoic Doushantuo Formation in\sJiangkou County,Guizhou Province,China.Chinese Science\sBulletin,49:2224-2226.
Zhou C M&Xiao S H.2007.Ediacaran Delta-13 C chemostratigraphy of South China.Chemical Geology,237:89-108.
Zhu M Y,Babcock L E&Peng S C.2006.Advances in Cambrian\sstratigraphy and paleontology:integrating correlation techniques,palaeobiology,taphonomy and paleoenvironmental reconstruction.Palaeoworld,15:217-222.
Zhu M Y,Gehling G J,Xiao S H,Zhao Y L&Droser L M.2008.Eight-armed Ediacara fossil preserved in contrasting taphonomic\swindows from China and Australia.Geology,36:867-870.
Zhu M Y,Zhang J M&Yang A H.2007.Integrated Ediaearan(Sinian)chronostratigraphy of South China Palaeogeography,Palaeoelimatology,Palaeoeeology,254(1-2):7-61.
Zhu M Y&Zhang J M.2005.Ediacaran-Cambrian boundary sections and Early Cambrian Chengjiang nonmineralized fossils in\seastern Yunnan Province,southwestern China:Introduction//Peng S C,Babcock L,Zhu M Y&Li G X eds.Cambrian System of China and Korea.Guide to Field Excursions.Hefei:U-niversity of Science and Technology of China Press.1-12.
Zhu M Y.2007.From snowball earth to the Cambrian bioradiation:calibration of Ediacaran-Cambrian earth history in South China.Palaeogeography,Palaeoclimatology,Palaeoecology,254:1-6.
Zhu M Y,Lu M,Zhang J M,Zhao F C,Li G X,Yang A H,Zhao\sX&Zhao M J.2013.Carbon isotope chemostratigraphy and\ssedimentary facies evolution of the Ediacaran Doushantuo Formation in western Hubei,South China.Precambrian Research,225:7-28.