Brasier M D,Shields G.2000b.Neoproterozoic chemostratigraphy and correlation of the Port Askaig glaciation,Dalradian Supergroup of Scotland.J.Geol.Soc.London,157:909~914.
[3]
Condon D J,Prave A R,Benn D I.2002.Neoproterozoic glacialrain-out intervals:observations and implications.Geology,30:35~38.
[4]
Conway Morris S.1998.The crucible of creation --The Burgess Shale and Rise of Animals.Oxford:Oxford University Press,1~242.
[5]
Corsetti F A,Kaufman A J.2003.Stratigraphic investigations of carbon isotope anomalies and Neoproterozoic ice ages in Death Valley,California.GSA Bull.,115:916~932.
[6]
Knoll A H.2000.Learning to tell Neoproterozoic time.Precambrian Research,100:3~20.
[7]
Macouin M,Basse J,Ader M,Gilder S,Yang Z,Sun Z,Agrinier P.2004.Combined paleomagnetic and isotopic data from the Doushantuo carbonates,South China:implications for the "snowball Earth" hypothesis.Earth and Planetary Science Letters,224:387~398.
[8]
Stoll H M,Schrag D P.2000.High-resolution stable isotope records from the Upper Cretaceous rocks of Italy and Spain:Glacial episodes in a greenhouse planet? Geol.Soc.Am.Bull.,112:308~319.
[9]
Walter M R,Veevers J J,Calver C R,Gorjan P,Hill A C.2000.Dating the 830~544 Ma Late Neoproterozoic interval by isotopes of strontium,carbon (carbonate and organic),and sulfur (sulfate) in seawater.Precambrian Research,100:371~433.
[10]
Xiao Shuhai,Bao Huiming,Wang Haifeng,Kaufman A J,Zhou Chuanming,Li Guoxiang,Yuan Xunlai,Ling Hongfei.2004.The Neoproterozoic Quruqtagh Group in eastern Chinese Tianshan:evidence for a post-Marinoan glaciation.Precambrian Research,130:1~26.
[11]
Xu B,Zhang H,Yao H,Li Y.2003.C-isotope composition and significance of the Sinian on the Tarim plate.Chinese Sci.Bull.,48:385~389.
[12]
Yang Ruidong,Zhang Chuanlin,Luo Xinrong.2006.Worm-like fossils from the Lower Cambrian Xidashan Formation in Quruqtagh area,Xinjiang.Progress in Natural Science,16(5):559~562.
[13]
Yang Ruidong,Zhang Chuanlin,Wang Baixuan,Luo Xingrong.2007.Chemostratigraphy and lithological characters of Neoproterozoic cap carbonates from the Quruqtagh Mountain,Xinjiang,west China.Chinese Journal of Geochemistry,26(1):32~39.
[14]
Young G M.2002.Stratigraphic and tectonic settings of Proterozoic glaciogenic rocks and banded iron-formations:relevance to the snowball Earth debate.Journal of African Earth Sciences,35:451~466.
Barfod G H,Albarede F,Knoll A H,Xiao S,Telouk P,Frei R,Baker J.2002.New Lu-Hf and Pb-Pb age constraints on the earliest animal fossils.Earth Planet.Science Letter,201(1):203~212.
[17]
Bowring S,Myrow P,Landing E,Ramezani J,Grotzinger J.2003.Geochronological constraints on terminal Neoproterozoic events and the rise of metazoans.Geophys.Res.Abstracts 5,13219.
[18]
Brasier M,McCarron G,Tucker R,Leather J,Allen P,Shields G.2000a.New U-Pb zircon dates for the Neoproterozoic Ghubrah glaciation and for the top of the Huqf Supergroup,Oman.Geology,28:175~178.
[19]
Donnadieu Y,Fluteau F,Ramstein G,Ritz C,Besse J.2003.Is there a conflict between the Neoproterozoic glacial deposits and the snowball Earth interpretation:an improved understanding with numerical modeling.Earth and Planetary Science Letters,208:101~112.
[20]
Di Bona P A.1991.A previously unrecognized Late Proterozoic succession:Upper Wilpena Group,northern Flinders Ranges,South Australia.Geol.Surv.South Aust.Quart.Geol.Notes,117:2~9.
[21]
Grey K,Corkeron M.1998.Late Neoproterozoic stromatolites in glaciogenic successions of the Kimberley region,Western Australia:evidence for a younger Marinoan glaciation.Precambrian Research,92:65~87.
[22]
Hoffman P F,Kaufman A J,Halverson G P,Schrag D P.1998.A Neoproterozoic snowball Earth.Science,281:1342~1346.
[23]
Hyde W T,Crowley T J,Baum S K,Peltier W R.2000.Neoproterozoic snowball Earth simulations with a coupled climate/ice-sheet model.Nature,405:425~429.
[24]
Kaufman A J,Knoll A H,Narbonne G M.1997.Isotopes,ice ages,and terminal Proterozoic earth history.Proc.Natl.Acad.Sci.U.S.A.,94:6600~6605.
[25]
Kennedy M J,Runnegar B,Prave A R,Hoffmann K H,Arthur M A.1998.Two or four Neoproterozoic glaciations? Geology,26:1059~1063.