Redox status of the Mesoproterozoic epeiric sea in North China

doi:10.7605/gdlxb.2011.05.010

JOURNAL OF PALAEOGEOGRAPHY ›› 2011, Vol. 13 ›› Issue (5): 563-580. doi: 10.7605/gdlxb.2011.05.010

• GEOCHEMISTRY AND SEDIMENTARY ENVIRONMENT • Previous Articles

Redox status of the Mesoproterozoic epeiric sea in North China

Tang Dongjie¹, Shi Xiaoying^1,2, Pei Yunpeng¹, Jiang Ganqing³, Zhao Guisheng¹

1 School of the Earth Sciences and Resources，China University of Geosciences(Beijing)，Beijing100083
2 State Key Laboratory of Geological Processes and Mineral Resources，China University of Geosciences(Beijing)，Beijing100083
3 Department of Geosciences，University of Nevada，Las Vegas，NV 89154-4010，USA

Received:2011-04-25 Revised:2011-05-27 Online:2011-10-01 Published:2011-10-01
About author:Tang Dongjie，born in 1985，is a Ph.D.candidate of paleontology and stratigraphy.E-mail: dongjtang@126.com.
About the corresponding author Shi Xiaoying，born in 1956，is a professor of paleontology and stratigraphy in China University of Geosciences(Beijing).E-mail: shixyb@cugb.edu.cn.

华北中元古代陆表海氧化还原条件^*

汤冬杰¹ 史晓颖^1,2 裴云鹏¹ 蒋干清³ 赵贵生¹

1 中国地质大学(北京)地球科学与资源学院，北京100083
2 中国地质大学(北京)地质过程与矿产资源国家重点实验室，北京100083
3 美国内华达大学地球科学系，美国拉斯维加斯，NV 89154-4010

通讯作者: 通讯作者简介史晓颖，男，1956年生，教授，博士生导师，主要从事地层古生物及沉积学方面的教学与研究. 电话：13426082816 E-mail:dongjtang@126.com
作者简介:汤冬杰，男，1985年生，博士研究生，主要从事地球生物学与沉积学方面的研究。E-mail: dongjtang@126.com。电话：13426082816。
通讯作者简介史晓颖，男，1956年生，教授，博士生导师，主要从事地层古生物及沉积学方面的教学与研究。E-mail: shixyb@cugb.edu.cn。
基金资助:
国家自然科学基金项目(编号：40972022，40921062)及国家“973”项目(编号：2011CB808806)资助成果

Abstract

Abstract: Marine authigenic aragonite crystal fans and isopachous cements are mainly formed in anoxic-dysoxic seawater or pore waters with oversaturated CaCO₃ derived from bacterial sulfate reduction(BSR).Their presence can be used as a potential indicator for redox conditions of the depositional environment.Carbonate units from the Mesoproterozoic Wumishan Formation(ca.1.5～1.45 Ga)in North China Platform show that aragonite fans and cements are common in deep subtidal deposits，but decline in shallow subtidal and disappear in intertidal deposits.Particularly the biolaminites deposited from deep-subtidal environments are composed of submillimeter-scale dark-light couplets of microbial mat and isopachous aragonite.Microscopically，the isopachous aragonites are composed of fibrous crystals or fan-shaped aggregates，similar to those recognized from the Archean strata of South Africa.Carbonates commonly form shallowing-upward cycles with shallow subtidal facies(Unit A) at the base，intertidal facies(Unit B) in the middle and supratidal facies(Unit C) at the top.The shallow subtidal facies(Unit A)contain abundant thrombolites，in which meso-clots consist typically of fabrous or fan-shaped aragonite aggregates surrounding organic-rich nuclei or pyrite grains，but rarely with carbonates micritic grains.Intertidal facies(Unit B)are dominated by laminated dolostone with interbeds of grainstones or packstones.Aragonite fans and cements are present but not abundant.Most of the aragonites in this unit grow on mat fragments or previously formed minerals，either as isopachous，fan-shaped or as botryoidal aggregates that fill cavities.Supratidal facies(Unit C)consists of micritic dolostone with pseudomorphs of halite and desiccated microbial mats but no aragonite crystal fans or cements. Geochemical analysis shows that V/Th，Mo/Th and U/Th increase from Unit C to Unit A，suggesting progressive anoxic condition with increasing water depth.Our study shows that during deposition of the Wumishan Formation(ca.1.5～1.45 Ga)，the North China epeiric sea was likely anoxic below the fair-weather wave base，but the abundance of aragonite crystal fans and fibrous cements in deep-subtidal environments imply the availability of sulfate in shelf environments of the Mesoproterozoic epeiric sea.

Key words: Mesoproterozoic, palaeooceanographic conditions, aragonite sea-floor precipitates, redox sensitive elements, North China Platform

摘要： 文石海底沉淀是地球早期大气高CO₂浓度、海洋贫氧条件下，CaCO₃过饱和而直接沉淀于海底所形成的自生碳酸盐，可反映古海洋贫氧状态。对华北中元古界雾迷山组(ca 1.50～1.45 Ga)碳酸盐岩的研究发现：潮下带下部黑色纹层石由针状文石假晶等厚层与微生物席层交互堆叠而成;潮下带中部凝块石白云岩(A单元)主要由针状文石假晶形成的环带或扇状集合体包裹有机质团块所组成，少见碳酸盐微粒。潮下带上部—潮间带下部纹层白云岩(B单元)以自然沉淀的碳酸盐微粒为主，含少量等厚层和扇状、葡萄状文石假晶集合体，以及以孔洞充填形式产出的针状文石假晶。而潮坪成因的泥晶白云岩(C单元)则完全由含有石盐假晶和微生物席裂痕的泥晶质微晶白云岩组成，不含针状文石沉淀。对构成雾迷山组典型副层序基本单元的氧化还原敏感元素比值分析显示：由C单元至A单元，V/Th、Mo/Th、U/Th值逐渐增大，在A单元可能达贫氧富集程度。研究表明，在雾迷山组沉积期，华北陆表海潮下带中部及其以下可能长期处于贫氧状态，而潮下带上部则处于氧化状态，氧化—还原界面接近于正常浪基面底。这个认识对进一步了解中元古代海洋条件、生物与环境相互作用过程及烃源岩勘查具有重要意义。

关键词: 中元古代, 古海洋条件, 文石海底沉淀, 氧化还原敏感元素, 华北地台

CLC Number:

P736.4

Tang Dongjie, Shi Xiaoying, Pei Yunpeng, Jiang Ganqing, Zhao Guisheng. Redox status of the Mesoproterozoic epeiric sea in North China[J]. JOURNAL OF PALAEOGEOGRAPHY, 2011, 13(5): 563-580.

汤冬杰, 史晓颖, 裴云鹏, 蒋干清, 赵贵生. 华北中元古代陆表海氧化还原条件^*[J]. 古地理学报, 2011, 13(5): 563-580.

/ / Recommend / Download Citations

URL: http://www.gdlxb.cn/EN/10.7605/gdlxb.2011.05.010

http://www.gdlxb.cn/EN/Y2011/V13/I5/563

References

常华进，储雪蕾，冯连君，等.2009.氧化还原敏感微量元素对古海洋沉积环境的指示意义［J］.地质论评，55(1):91-99.
高林志，张传恒，刘鹏举，等.2009.华北—江南地区中新元古代地层格架的再认识［J］.地球学报，30(4):433-446.
高林志，张传恒，史晓颖，等.2007.华北青白口系下马岭组凝灰岩锆石SHRIMP U-Pb 定年［J］.地质通报，26(3)：249-255.
高林志，张传恒，尹崇玉，等.2008.华北古陆中，新元古代年代地层框架SHRIMP 锆石年龄新依据［J］.地球学报，29(3):366-376.
李怀坤，朱士兴，相振群，等.2010.北京延庆高于庄组凝灰岩的锆石U-Pb定年研究及其对华北北部中元古界划分新方案的进一步约束［J］.岩石学报，26(7):2131-2140.
陆松年，李惠民.1991.蓟县长城系大红峪组火山岩的单颗粒锆石U-Pb 法准确定年［J］.中国地质科学院院报，22(1):137-145.
乔秀夫，高林志，张传恒.2007.中朝板块中新元古界年代地层柱与构造环境新思考［J］.地质通报，26(5):503-509.
史晓颖，蒋干清，张传恒，等.2008a.华北地台中元古代串岭沟组页岩中的砂脉构造——17×10⁸年前甲烷气逃逸的沉积标识？［J］.地球科学，33(5):577-590.
史晓颖，王新强，蒋干清，等.2008b.贺兰山地区中元古代微生物席成因构造——远古时期微生物群活动的沉积标识［J］.地质论评，54(5):577-586.
史晓颖，张传恒，蒋干清，等.2008c.华北地台中元古代碳酸盐岩中的微生物成因构造及其生烃潜力［J］.现代地质，22(5):669-682.
苏文博，李怀坤，Huff W，等.2010.铁岭组钾质斑脱岩锆石SHRIMP U-Pb 年代学研究及其地质意义［J］.科学通报，55(22): 2197-2206.
张传恒，武振杰，高林志，等.2007.华北中元古界雾迷山组地震驱动的软沉积物变形构造及其地质意义［J］.中国科学(D辑): 地球科学，37(3):336-343.
周洪瑞，梅冥相，杜本明，等.2006.天津蓟县雾迷山组高频旋回沉积特征［J］.现代地质，20(2):209-215.
Algeo T J.2008.Can marine anoxic events draw down the trace element inventory of seawater？［J］.Geology，32(12):1057-1060.
Algeo T J，Maynard J B.2008.Trace metal covariation as a guide to water-mass conditions in ancient anoxic marine environments［J］.Geosphere，4(5):872-887.
Algeo T J，Tribovillard N.2009.Environmental analysis of paleoceanographic systems based on molybdenum-uranium covariation［J］.Chemical Geology，268(3-4): 211-225.
Anbar A D，Knoll A H.2002.Proterozoic ocean chemistry and evolution: A bioinorganic bridge？［J］.Science，297(5584):1137-1142.
Arnold G L，Anbar A D，Barling J， et al. 2004.Molybdenum isotope evidence for widespread anoxia in mid-Proterozoic oceans［J］.Science，304(5667):87-90.
Bartley J K，Kah L C.2004.Marine carbon reservoir，C_org-C_carb coupling，and the evolution of the Proterozoic carbon cycle［J］.Geology，32(2):129-132.
Bartley J K，Knoll A H，Grotzinger J P， et al.2000.Lithification and Fabric Genesis in Precipitated Stromatolites and Associated Peritidal Carbonates Mesoproterozoic Billyakh Group Siberia［C］.In: Grotzinger J P， James N P（eds). Carbonate Sedimentation and Diagenesis in the Evolving Precambrian World Society of Economic Paleontologists and Mineralogists，Special Publication，67: 59-74.
Breit G N，Wanty R B.1991.Vanadium accumulation in Carbonaceous rocks: A review of geochemical controls during deposition and diagenesis［J］.Chemical Geology，91(2):83-97.
Brocks J J，Love G D，Summons R E， et al. 2005.Biomarker evidence for green and purple sulphur bacteria in a stratified Palaeoproterozoic sea［J］.Nature，437(7060):866-870.
Canfield D E.1998.A new model for Proterozoic ocean chemistry［J］.Nature，396(6710):450-453.
Catling D C，Claire M W，Zahnle K J.2007.Anerobic methanotrophy and the rise of atmosphere oxygen［J］.Philosophical Transactions of the Royal Society A: Mathematical，Physical and Engineering Sciences，365(1856):1867-1888.
Chaillou G，Anschutz P，Lavaux G， et al. 2002.The distribution of Mo，U，and Cd in relation to major redox species in muddy sediments of the Bay of Biscay［J］.Marine Chemistry，80(1):41-59.
Chen J Y，Bottjer D J，Oliveri P， et al.2004.Small bilaterian fossils from 40 to 55 million years before the Cambrian［J］.Science，305(5681):218-222.
Dahla T W，Hammarlund E U，Anbare A D.2009.Devonian rise in atmospheric oxygen correlated to the radiations of terrestrial plants and large predatory fish［J］.Proceedings of the National Academy of Sciences of the United States of America，107(42):17911-17915.
de Leeuw N H.2002.Molecular dynamics simulations of the growth inhibiting effect of Fe²⁺，Mg²⁺，Cd²⁺ and Sr²⁺ on calcite crystal growth［J］.Journal of Physical Chemistry B，106(20):5241-5249.
Emerson S R，Huested S S.1991.Ocean anoxia and the concentrations of molybdenum and vanadium in seawater［J］.Marine Chemistry，34(3-4): 177-196.
Erickson B E，Helz G R.2000.Molybdenum(Ⅵ)speciation in sulfidic waters: Stability and lability of thiomolybdates［J］.Geochimica et Cosmochimica Acta，64(7):1149-1158.
Farquhar J，Wu N，Canfield D E， et al. 2010.Connections between sulfur cycle evolution，sulfur isotopes，sediments，and base metal sulfide deposits［J］.Economic Geology，105(3):509-533.
Fike D A，Grotzinger J P，Pratt L M， et al. 2006.Oxidation of the Ediacaran Ocean［J］.Nature，444(7120):744-747.
Francois R.1988.A study on the regulation of the concentrations of some trace metals(Rb，Sr，Zn，Pb，Cu，V，Cr，Ni，Mn and Mo)in Saanich Inlet sediments，British Columbia，Canada［J］.Marine Geology，83(1-4): 285-308.
Frei R，Gaucher C，Poulton S W， et al. 2009.Fluctuations in Precambrian atmospheric oxygenation recorded by chromium isotopes［J］.Nature,461(7261):250-254.
Grotzinger J P，James N P.2000.Precambrian Carbonates: Evolution of Understanding［C］.In: Grotzinger J P， James N P（eds).Carbonate Sedimentation and Diagenesis in the Evolving Precambrian World Society of Economic Paleontologists and Mineralogists，Special Publication，67: 3-22.
Grotzinger J P，Knoll A H.1995.Anomalous carbonate precipitates: Is the Precambrian the key to the Permian？［J］.Palaios，10(6):578-596.
Grotzinger J P，Reed J F.1983.Evidence for primary aragonite precipitation，Lower Proterozoic(1.9 Ga)Rocknest dolomite，Wopmay orogen，northwest Canada［J］.Geology，11(12):710-713.
Grotzinger J P.1986.Evolution of Early Proterozoic passive-margin carbonate platform，Rocknest Formation，Wopmay Orogen，Northwest Territories，Canada［J］.Journal of Sedimentary Research，56(6):831-847.
Helz G R，Bura-Nakic′ E，Mikac N， et al.， 2011.New model for molybdenum behavior in euxinic waters［J］.Chemical Geology，284(3-4): 323-332.
Helz G R，Miller C V，Charnock J M， et al. 1996.Mechanism of molybdenum removal from the sea and its concentration in black shales: EXAFS evidence［J］.Geochimica et Cosmochimica Acta，60(19):3631-3642.
Holland H D.2006.The oxygenation of the atmosphere and oceans［J］.Philosophical Transactions of the Royal Society B：Biological Sciences，361(1470):903-915.
Jones B，Manning D A C.1994.Comparison of geochemical indices used for the interpretation of palaeoredox conditions in ancient mudstones［J］.Chemical Geology，111(1-4): 111-129.
Kah L C，Grotzinger J P.1992.Early Proterozoic 1.9 Ga thrombolites of the Rocknest Formation Northwest Territories Canada［J］.Palaios，7: 305-315.
Kah L C，Lyons T W，Frank T D.2004.Low marine sulphate and protracted oxygenation of the Proterozoic biosphere［J］.Nature，431(7010):834-838.
Kasting J F，Howard M T，Wallmann K， et al. 2006.Paleoclimates，ocean depth，and the oxygen isotopic composition of seawater［J］.Earth and Planetary Science Letters，252(1-2): 82-93.
Kasting J F.2004.When methane made climate［J］.Scientific American，291(1):78-85.
Kerr R A.2004.Low oxygen in old oceans［J］.Science，304(5667): 13.
Knoll A H，Javaux E J，Hewitt D， et al. 2006.Eukaryotic organisms in Proterozoic oceans［J］.Philosophical Transactions of the Royal Society B: Biological Sciences，361(1470):1023-1038.
Kump.2008.The rise of atmospheric oxygen［J］.Nature，451(7176):277-278.
Lyons T W，Anbar A D，Severmann S， et al. 2009.Tracking euxinia in the ancient ocean: A multiproxy perspective and Proterozoic case study［J］.Annual Review of Earth and Planetary Sciences，37: 507-534.
McFadden K A，Huang J，Chu X L， et al.2008.Pulsed oxidation and biological evolution in the Ediacaran Doushantuo Formation［J］.Proceedings of the National Academy of Sciences of the United States of America，105(9):3197-3202.
McManus J，Berelson W M，Klinkhammer G P， et al.2005.Authigenic uranium: Relationship to oxygen penetration depth and organic carbon rain［J］.Geochimica et Cosmochimica Acta，69(1):95-108.
Morford J L，Emerson S.1999.The geochemistry of redox sensitive trace metals in sediments［J］.Geochimica et Cosmochimica Acta，63(11-12): 1735-1750.
Morford J L，Russell A D，Emerson S.2001.Trace metal evidence for changes in the redox environment associated with the transition from terrigenous clay to diatomaceous sediment，Saanich Inlet，BC［J］.Marine Geology，174(1-4): 355-369.
Neubert N，Ngler T F，Bttcher M E.2008.Sulfidity controls molybdenum isotope fractionation into euxinic sediments: Evidence from the modern Black Sea［J］.Geology，36(10):775-778.
Planavsky N J，Rouxel O J，Bekker A， et al.2010.The evolution of the marine phosphate reservoir［J］.Nature，467(7319):1088-1090.
Poulton S，Bekker A，Canfield D E.2009.Early Paleoproterozoic fluctuations in biospheric oxygenation［J］.Geochimica et Cosmochimica Acta，73: A1047.
Pruss S B，Corsetti F A，Fischer W W.2008.Seafloor-precipitated carbonate fans in the Neoproterozoic Rainstorm Member，Johnnie Formation，Death Valley Region，USA［J］.Sedimentary Geology，207(1-4): 34-40.
Riding R.2000.Microbial carbonates: The geological record of calcified bacterial-algal and biofilms［J］.Sedimentology，47(s1): 179-214.
Rouxel O J，Bekker A，Edwards K J.2005.Iron isotope constraints on the Archean and Paleoproterozoic ocean redox state［J］.Science，307(5712):1088-1091.
Russell A D，Morford J L.2001.The behavior of redox-sensitive metals across a laminated-massive-laminated transition in Saanich Inlet，British Columbia［J］.Marine Geology，174(1-4): 341-354.
Schrder 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，London，164(1):175-187.
Scott C，Lyon T W，Bekker A， et al.2008.Tracing the stepwise oxygenation of the Proterozoic ocean［J］.Nature，452(7186):456-459.
Shen Y，Knoll A H，Walter M R.2003.Evidence for low sulphate and anoxia in a mid-Proterozoic marine basin［J］.Nature，423(6940):632-635.
Shi X Y，Jiang G Q，Zhang C H， et al. 2008a.Sand veins and MISS from the Mesoproterozoic black shale(ca.1.7 Ga)in North China: Implication for methane degassing from microbial mats［J］.Science in China(Series D): Earth Sciences，51(11):1525-1536.
Shi X Y，Zhang C H，Jiang G Q， et al. 2008b.Microbial Mats in the Mesoproterozoic carbonates of the North China Platform and their potential for hydrocarbon generation［J］.Journal of China University of Geosciences，19(5):549-566.
Slack J F，Grenne T，Bekker A， et al.2007.Suboxic deep seawater in the late Paleoproterozoic: Evidence from hematitic chert and iron formation related to seafloor hydrothermal sulfide deposits，central Arizona，USA［J］.Earth and Planetary Science Letters，255(1-2): 243-256.
Sumner D Y，Grotzinger J P.1996.Were kinetics of Archean calcium carbonate precipitation related to oxygen concentration？［J］.Geology，24(2):119-22.
Sumner D Y，Grotzinger J P.2000.Late Archean Aragonite Precipitation: Petrography，Facies Associations，and Environmental Significance［C］.In: Grotzinger J P， James N P(eds).Carbonate Sedimentation and Diagenesis in the Evolving Precambrian World.Society of Economic Paleontologists and Mineralogists，Special Publication，67: 123-144.
Sumner D Y，Grotzinger J P.2004.Implications for Neoarchean ocean chemistry from primary carbonate mineralogy of the Campbellrand-Malmani Platform，South Africa［J］.Sedimentary Geology，51(6):1-27.
Su W，Zhang S，Huff W D， et al.2008.SHRIMP U-Pb ages of K-bentonite beds in the Xiamaling Formation: Implications for revised subdivision of the Meso-to Neoproterozoic history of the North China Craton［J］.Gondwana Research，14(3):543-553.
Tribovillard N，Riboulleau A，Lyons T， et al.2004.Enhanced trapping of molybdenum by sulfurized marine organic matter of marine origin in Mesozoic limestones and shales［J］.Chemical Geology，213(4):385-401.
Tribovillard N，Algeo T J，Lyons T， et al. 2006.Trace metals as paleoredox and paleoproductivity proxies: An update［J］.Chemical Geology，232(1-2): 12-32.
Turekian，K K，Wedepohl K H.1961.Distribution of the elements in some major units of the Earths crust［J］.Geological Society of America Bulletin，72(2)：175-192.
Vorlicek T P，Kahn M D，Kasuza Y， et al. 2004.Capture of molybdenum in pyrite-forming sediments: Role of ligand-induced reduction by polysulfides［J］.Geochimica et Cosmochimica Acta，68(3):547-556.
Wang X Q，Shi X Y.2009.Spatio-temporal Carbon isotope variation during the Ediacaran period in South China and its impact on bio-evolution［J］.Science in China(Series D)：Earth Science，52(10):1520-1528.
Wanty R B，Goldhaber R.1992.Thermodynamics and kinetics of reactions involving vanadium in natural systems: Accumulation of vanadium in sedimentary rocks［J］.Geochimica et Cosmochimica Acta，56(4):171-183.
Wignall P B，Myers K J.1988.Interpreting benthic oxygen levels in mudrocks: A new approach［J］.Geology，16(5):452-455.
Woods A D，Bottjer D J，Mutti M， et al. 1999.Lower Triassic large sea-floor carbonate cements: Their origin and a mechanism for the prolonged biotic recovery from the end-Permian mass extinction［J］.Geo￣logy，27(7):645-648.
Xiao S H，Zhang Y，Knoll A H.1998.Three-dimensional preservation of algae and animal embryos in a Neoproterozoic phosphorite［J］.Nature，391(6667):553-558.
Yin L M，Zhu M Y，Knoll A H， et al. 2007.Doushantuo embryos preserved inside diapause egg cysts［J］.Nature，446(7136):661-663.
Yuan X L，Chen Z，Xiao S H， et al. 2011.An early Ediacaran assemblage of macroscopic and morphologically differentiated eukaryotes［J］.Nature，470(7334):390-393.
Zheng Y，Anderson R F，Van Geen A， et al.2000.Authigenic molybdenum formation in marine sediments: A link to pore water sulfide in the Santa Barbara Basin［J］.Geochimica et Cosmochimica Acta，64(24):4165-4178.
Zheng Y，Anderson R F，Van G A， et al.2002a.Preservation of particulate non-lithogenic uranium in marine sediments［J］.Geochimica et Cosmochimica Acta，66(17):3085-3092.
Zheng Y，Anderson R F，Van G A， et al. 2002b.Remobilization of authigenic uranium in marine sediments by bioturbation［J］.Geochimica et Cosmochimica Acta，66(10):1759-1772.
Zhu M Y，Gehling J G，Xiao S H， et al.2008.Eight-armed Ediacara fossil preserved in contrasting taphonomic windows from China and Australia［J］.Geology，36(11):867-870.郑秀娟

[1]	Mei Ming-Xiang. Giant ooids induced and predominated by photosynthetic biofilms of filamentous cyanobacteria: an example from the Miaolingian Xuzhuang Formation at the Shijing section in Xin'an County of Henan Province,North China Platform [J]. JOPC, 2021, 23(1): 105-124.
[2]	Jin Song, Guo Hua, Yu Wen-Chao, Du Yuan-Sheng, Ma Peng-Fei. Evolution of Yanliao aulacogen in the Paleo-Mesoproterozoic and its control on manganese deposit [J]. JOPC, 2020, 22(5): 841-854.
[3]	Guo Yan-Qin, Li Wen-Hou, Guo Bin-Cheng, Zhang Qian, Chen Qiang, Wang Ruo-Gu, Liu Xi, Ma Yao, Li Zhi-Chao, Zhang Meng-Ting, Li Bai-Qiang. Sedimentary systems and palaeogeography evolution of Ordos Basin [J]. JOPC, 2019, 21(2): 293-320.
[4]	Kuang Hong-Wei, Liu Yong-Qing, Geng Yuan-Sheng, Bai Hua-Qing, Peng Nan, Fan Zheng-Xiu, Song Huan-Xin, Xia Xiao-Xu, Wang Yu-Chong, Chen Xiao-Shuai. Important sedimentary geological events of the Meso-Neoproterozoic and their significance [J]. JOPC, 2019, 21(1): 1-30.
[5]	Peng Nan, Kuang Hong-Wei, Liu Yong-Qing, Geng Yuan-Sheng, Xia Xiao-Xu, Wang Yu-Chong, Chen Xiao-Shuai, Zheng Hang-Hai. Recognition of geological age for acanthomorphic acritarchs from the Ruyang Group,southern margin of North China Craton and its implication for evolution of early eukaryotes [J]. JOPC, 2018, 20(4): 595-608.
[6]	Kuang Hong-Wei, Liu Yong-Qing, Fan Zheng-Xiu, Peng Nan, Geng Yuan-Sheng, Zhu Zhi-Cai, Xu Huan, An Wei, Wang Neng-Sheng, Xia Xiao-Xu, Wang Yu-Chong. Sedimentary characteristics of the Mesoproterozoic Shennongjia Group in northern margin of Yangtze Craton [J]. JOPC, 2018, 20(4): 523-544.
[7]	Tang Dongjie, Shi Xiaoying, Zhang Wenhao, Liu Yun, Wu Jinjian. Mesoproterozoic herringbone calcite from North China Platform:Genesis and paleoenvironmental significance [J]. JOPC, 2017, 19(2): 227-240.
[8]	Zhang Wenhao, Shi Xiaoying, Tang Dongjie, Wang Xinqiang. Mass-occurrence of oncoids in the Early-Middle Cambrian transition at western margin of North China Platform：A response of microbial community to shallow marine anoxia [J]. JOPC, 2014, 16(3): 305-318.
[9]	Su Dechen, Sun Aiping. Soft-sediment deformation and occurrence frequency of palaeoearthquake in the Mesoproterozoic Wumishan Formation， Yongding River Valley，Beijing [J]. JOURNAL OF PALAEOGEOGRAPHY, 2011, 13(6): 591-614.
[10]	Tang Dongjie，Shi Xiaoying，Liu Juan，Wang Xinqiang，Pei Yunpeng. Authigenic carbonate precipitation and pyrites from sand veins in the Chuanlinggou Formation of the North China Platform—Evidence for anaerobic oxidation of methane in the Mesoproterozoic [J]. JOURNAL OF PALAEOGEOGRAPHY, 2009, 11(4): 361-.

Please choose a citation manager

Content to export

Redox status of the Mesoproterozoic epeiric sea in North China

华北中元古代陆表海氧化还原条件^*

RichHTML

PDF

Knowledge

Cited

Abstract

Cite this article

share this article

References

Related Articles 10

Recommended Articles

Metrics

Comments

模态框（Modal）标题

Please choose a citation manager

Content to export

Redox status of the Mesoproterozoic epeiric sea in North China

华北中元古代陆表海氧化还原条件*

RichHTML

PDF

Knowledge

Cited

Abstract

Cite this article

share this article

References

Related Articles 10

Recommended Articles

Metrics

Comments

华北中元古代陆表海氧化还原条件^*