Wignall P B;Twitchett R J Oceanic anoxia and the end Permian mass extinction [J] 1996 doi:10.1126/science.272.5265.1155
[8]
Wedepohl K H,The composition of the continental crust,Geochimica et Cosmochimica Acta,1995.
[9]
葛朝华;韩发,广东大宝山矿床喷气-沉积成因地球化学特征,北京:北京科学技术出版社,1987.
[10]
Webb GE. ；Kamber BS.,Rare earth elements in Holocene reefal microbialites: A new shallow seawater proxy,Geochimica et Cosmochimica Acta?,2000, 64(9).
[11]
Tribovillard, N ；Algeo, TJ ；Lyons, T ；Riboulleau, A,Trace metals as paleoredox and paleoproductivity proxies: An update,Chemical geology?,2006, 232(1-2).
[12]
Sugisaki R;Yamamoto K;Adachi M,Triassic bedded charts in central Japan are not pelagic,Nature,1982(5875).
[13]
Schroder S;Grotzinger J P,Evidence for anoxia at the Ediacaran-Cambrian boundary:the record of redox-sensitive trace elements and rare earth elements in Oman,Journal of the Geological Society(London),2007.
Li Shengrong;Gao Zhenming.Source tracing of noble metal elements in Lower Cambrian black rock series of Guizhou-Hunan Provinces,China[J].Science in China(Series D),2000(6)doi:10.1007/BF02879506
[17]
Kirschvink J L;Ripperdan R L;Evans D A,Evidence for a largescale reorganization of Early Cambrian continental masses by inertial interchange true polar wander,Science,1997.
[18]
Hiroto Kimura ；Yoshio Watanabe,Oceanic anoxia at the Precambrian-Cambrian boundary,Geology?,2001, 29(11).
[19]
Guo Q J;Shields G A;Liu C Q;Strauss H,Zhu M Y,Pi D H,Goldberg T,Yang X L,Trace element chemo-stratigraphy of two Ediacaran-Cambrian successions in South China:Implications for organo-sedimentary metal enrichment and silicification in the earlyCambrian,Palaeogeography,Palaeoclimatology,Palaeoecology,2007.
[20]
Grunow A;Hanson R;Wilson T Were aspects of Pan-African deformation linked to lapetus opening [J] 1996(12) doi:10.1130/0091-7613(1996)024<1063:WAOPAD>2.3.CO;2
[21]
AIberdi G M;Tocco R,Trace metals and organic geochemistry of the Machiques Member (Aptian-Albian) and La Luna Formation (Cenomanian-Campanian),Venezuela,Chemical Geology,1999.
[22]
Adachi M;Yamamoto K;Sugisaki R Hydrothennal chert and associated siliceous rocks from the Northern Pacific:Geological significance as indication of ocean ridge activity [J] 1986 doi:10.1016/0037-0738(86)90075-8
Rimmer S M,Geochemical paleoredox indicators in Devonian/Mississippian black shales,Central Appalachian Basin (USA),Chemical Geology,2004.
[40]
Pease, V ；Daly, JS ；Elming, SA ；Kumpulainen, R ；Moczydlowska, A ；Puchkov, V ；Roberts, D ；Saintot, A ；Stephenson, R,Baltica in the Cryogenian, 850-630 Ma,Precambrian Research?,2008, 160(1/2).
[41]
Murray R W,Chemical criteria to identify the depositional environment of chert:general principles and applications,Sedimentary Geology,1991.
[42]
Mongenot T;Tribovillard N;Desprairies A;Elisabeth L V Fatima L D Trace elements as palaeo-environmental markers in strongly mature hydrocarbon source rocks:the Cretaceous La Luna Formation of Venezuela [J] 1996 doi:10.1016/0037-0738(95)00078-X
[43]
Michard A Rare earth elements systematics in hydrothermal fluids [J] 1989 doi:10.1016/0016-7037(89)90017-3
[44]
Marchig V,Some geochemical indicators for discrimination between diagenetic and hydrothermal metalliferous sediments,Marine Geology,1982.
