Frimmel H E. 2009. Trace element distribution in Neoproterozoic carbonates as palaeoenvironmental indicator[J]. Chemical Geology,258:338-353.
[2]
García M G,Lecomte K L,Pasquini A I, et al. 2007. Sources of dissolved REE in mountainous streams draining granitic rocks,Sierras Pampeanas(Córdoba,Argentina)[J]. Geochimica et Cosmochimica Acta,71:5355-5368.
[3]
Goldstein S J,Jacobsen S B. 1988. Rare-earth elements in river waters[J]. Earth and Planetary Science Letters,89:35-47.
[4]
Guo Q J,Shields G A,Liu C Q. 2007. Trace element chemostratigraphy of two Ediacaran-Cambrian successions in South China:Implications for organosedimentary metal enrichment and silicification in the early Cambrian[J]. Palaeogeography,Palaeoclimatology,Palaeoecology,254:194-216.
[5]
Hurtgen M T,Halverson G P,Arthur M A, et al. 2006. Sulfur cycling in the aftermath of a 635-Ma snowball glaciation:Evidence for a syn-glacial sulfidic deep ocean[J]. Earth and Planetary Science Letters,245:551-570.
Algeo T J. 2004. Can marine anoxic events draw down the trace element inventory of seawater？[J]. Geology,32:1057-1060.
[18]
Dolenec M. 2005. The Permian-Traissic Boundary in the Karavanke Mountains(Brsnina section,Solenia):The ratio of Th/U as a possible indicator of changing redox conditions at the P/T transition[J]. RMZ-Materials and the Geoenvironment,52(2):437-445.
[19]
Dolenec T,Lojen S,Ramovs A. 2001. The Permian-Triassic boundary in Western Slovenia(Idrijca Valley section):Magnetostratigraphy,stable isotopes,and elemental variations[J]. Chemical Geology,175(1-2):175-190.
[20]
Douville E,Bienvenu P,Charlou J L, et al. 1999. Yttrium and rare earth elements in fluids from various deep-sea hydrothermal systems[J]. Geochimica et Cosmochimica Acta,63:627.
[21]
Font E,Nedelec A,Trindade R I F, et al. 2006. Chemostratigraphy of the Neoproterozoic Mirassol d‘Oeste cap dolostones(Mato Grosso,Brazil):An alternative model for Marinoan cap dolostone formation[J]. Earth and Planetary Science Letters,250(1-2):89-103.
[22]
Jiang G Q,Kennedy M J,Christie-Blick N, et al. 2006. Stratigraphy,sedimentary structures,and textures of the late Neoproterozoic Doushantuo cap carbonate in south China[J]. Journal of Sediment Research,76:978-995.
[23]
Jones B J,Manning A C. 1994. Comparison of geochemical indices used for the interpretation of palaeoredox conditions in ancient mudstones[J]. Chemical Geology,111:111-129.
[24]
Lawrence M G,Greig A,Collerson K D, et al. 2006. Rare earth element and yttrium variability in South East Queensland waterways[J]. Aquatic Geochemistry,12:39-72.
[25]
Lyons T W,Werne J P,Hollander D J, et al. 2003. Contrasting sulfur geochemistry and Fe/Al and Mo/Al ratios across the last oxic-to-anoxic transition in the Cariaco Basin,Venezuela[J]. Chemical Geology,195:131-157.
[26]
Meyera E E,Quicksallb A N,Landisa J D, et al. 2012. Trace and rare earth elemental investigation of a Sturtian cap carbonate,Pocatello,Idaho:Evidence for ocean redox conditions before and during carbonate deposition[J]. Precambrian Research,192-195:89-106.
[27]
Murray R W,Buchholtz Ten Brink M R,Gerlach D C,et al. 1991. Rare earth,major,and trace elements in chert from the Franciscan Complex and Monterey Group,California:Assessing REE sources to fine-grained marine sediments[J]. Geochimica et Cosmochimica Acta,55:1875-1895.
[28]
Nothdurft L D,Webb G E,Kamber B S. 2004. Rare earth element geochemistry of Late Devonian reefal carbonates,Canning Basin,Western Australia:Confirmation of a seawater REE proxy in ancient limestones[J]. Geochim Cosmochim Acta,68:263-283.
[29]
Nozaki Y,Alibo D S. 2003. Importance of vertical geochemical processes in controlling the oceanic profiles of dissolved rare earth elements in the northeastern Indian Ocean[J]. Earth and Planetary Science Letters,205:155-172.
[30]
Owen A W,Armstrong H A,Floyd J D. 1999. Rare earth element geochemistry of upper Ordovician cherts from the Southern Upland of Scotland[J]. Journal of the Geological Society of London,156:191-204.
[31]
Rimmer S M. 2004. Geochemical paleoredox indicators in Devonian-Mississippian black shales,Central Appalachian Basin(USA)[J]. Chemical Geology,206:373-391.
[32]
Sarkar A,Sarangi S,Ebihara A, et al. 2003. Carbonate geochemistry across the eocene/oligocene boundary of Kutch,western India:Implications to oceanic O2-poor condition and foraminiferal extinction[J]. Chemical Geology,201(3-4):281-293.
[33]
Schroeder S,Grotzinger J P. 2007. Evidence for anoxia at the Ediacaran-Cambrian boundary: The record of redox-sensitive trace elements and rare earth elements in Oman[J]. Journal of the Geological Society of London,164(1):175-187.
[34]
Shen B,Xiao S H,Kaufman A J, et al. 2008. Stratification and mixing of a post-glacial Neoproterozoic ocean:Evidence from carbon and sulfur isotopes in a cap dolostone from northwest China[J]. Earth and Planetary Science Letters,265:209-228.
[35]
Shen Y N,Zhang T G,Hoffman P F. 2008. On the coevolution of Ediacaran oceans and animals[J]. Proceedings of National Academy of Sciences of the United States of America,105(21):7376-7381.
[36]
Spangenberg J E,Bagnoud-Velsquez M,Boggiani P C, et al. 2013. Redox variations and bioproductivity in the Ediacaran:Evidence from inorganic and organic geochemistry of the Corumb Group,Brazil[J]. Gondwana Research,
[37]
Taylor S R,McClennan S M. 1985. The Continental Crustal:Its Composition and Evolution[M]. Oxford:Blackwell,312.
[38]
Tribovillard N,Desprairies A,Lallier-Vergès E, et al. 2006. Geochemical study of organic-rich cycles from the Kimmeridge Clay Formation of Yorkshire(G B): Productivity vs. anoxia[J]. Palaeogeography,Palaeoclimatology,Palaeoecology,108:165-181.
[39]
Wright J,Schrader H,Holser W T. 1987. Paleoredox variations in ancient oceans recorded by rare earth elements in fossil apatite[J]. Geochimica et Cosmochimica Acta,51:631-644.
[40]
Zhao Y Y,Zheng Y F,Chen F K. 2009. Trace element and strontium isotope constraints on sedimentary environment of Ediacaran carbonates in southern Anhui,South China[J]. Chemical Geology,265:345-362.
[41]
Zhou C M,Xiao S H. 2007. Ediacaran δ13C chemostratigraphy of South China[J]. Chemical Geology,237:89-108.
