Trace Elements Characteristics of Black Shales from the Ediacaran Doushantuo Formation, Hubei Province, South China: Implications for Redox and Open vs. Restricted Basin Conditions

Bi Zhu; Shaoyong Jiang; Daohui Pi; Lu Ge; Jinghong Yang

doi:10.1007/s12583-017-0907-5

Volume 29 Issue 2

Mar 2018

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Journal of Earth Science > 2018 > 29(2): 342-352.

Bi Zhu, Shaoyong Jiang, Daohui Pi, Lu Ge, Jinghong Yang. Trace Elements Characteristics of Black Shales from the Ediacaran Doushantuo Formation, Hubei Province, South China: Implications for Redox and Open vs. Restricted Basin Conditions. Journal of Earth Science, 2018, 29(2): 342-352. doi: 10.1007/s12583-017-0907-5

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Bi Zhu, Shaoyong Jiang, Daohui Pi, Lu Ge, Jinghong Yang. Trace Elements Characteristics of Black Shales from the Ediacaran Doushantuo Formation, Hubei Province, South China: Implications for Redox and Open vs. Restricted Basin Conditions. Journal of Earth Science, 2018, 29(2): 342-352. doi: 10.1007/s12583-017-0907-5

Citation:

Bi Zhu, Shaoyong Jiang, Daohui Pi, Lu Ge, Jinghong Yang. Trace Elements Characteristics of Black Shales from the Ediacaran Doushantuo Formation, Hubei Province, South China: Implications for Redox and Open vs. Restricted Basin Conditions. Journal of Earth Science, 2018, 29(2): 342-352. doi: 10.1007/s12583-017-0907-5

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Trace Elements Characteristics of Black Shales from the Ediacaran Doushantuo Formation, Hubei Province, South China: Implications for Redox and Open vs. Restricted Basin Conditions

doi: 10.1007/s12583-017-0907-5

Bi Zhu^1,3,
Shaoyong Jiang^{2,3
,
,},
Daohui Pi²,
Lu Ge¹,
Jinghong Yang³

1.
Institute of Isotope Hydrology, School of Earth Sciences and Engineering, Hohai University, Nanjing 210098, China
2.
State Key Laboratory of Geological Processes and Mineral Resources, Faculty of Earth Resources, Collaborative Innovation Center for Exploration of Strategic Mineral Resources, China University of Geosciences, Wuhan 430074, China
3.
State Key Laboratory for Mineral Deposits Research, School of Earth Sciences and Engineering, Nanjing University, Nanjing 210093, China

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Corresponding author: Shaoyong Jiang, shyjiang@cug.edu.cn
Received Date: 06 Oct 2016
Accepted Date: 07 Feb 2017
Publish Date: 01 Feb 2018

Abstract

Abstract

In the present study, we carried out trace element analyses of black shales of the Ediacaran Doushantou Formation from two sections (Jiulongwan, Baiguoyuan) in Hubei Province, South China. Mo-U characteristics of black shales from the two sections and compiled Mo-U data of Doushantuo black shales from sections of a variety of sedimentary facies described the temporal/spatial variability in the redox conditions of paleo-seawater during deposition of the Doushantuo Formation. Changes in Mo-U patterns of the Doushantuo Member Ⅱ (DST2) shales of open marine environments are consistent with a shift from a predominately oxic to a predominately anoxic ocean during their deposition. Mo-U patterns of the DST2 black shales from intra-shelf sections reflect basin restriction may have happened in the intra-shelf basin and are compatible with the redox-stratified model of the intra-shelf basin. Mo-U patterns of black shales of the Doushantuo Member Ⅳ (DST4) reveal that the shales from intra-shelf sections have more pronounced Mo enrichment and more significant enrichment of Mo over U than the slope shales, indicating the operation of a Mn particulate shuttle in the intra-shelf basin. High Mo/TOC ratios of the DST4 at the intra-shelf sections, in combination with similar Mo-TOC patterns of the DST4 from both intra-shelf and slope sections, indicate the intra-shelf basin was well connected to the open ocean during deposition of the DST4.
- Doushantuo Formation,
- Mo-U covariation,
- Mo/TOC,
- South China

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References

Algeo, T. J., Lyons, T. W., 2006. Mo-Total Organic Carbon Covariation in Modern Anoxic Marine Environments: Implications for Analysis of Paleoredox and Paleohydrographic Conditions. Paleoceanography, 21(1): 279–298. https://doi.org/10.1029/2004pa001112

Algeo, T. J., Maynard, J. B., 2004. Trace-Element Behavior and Redox Facies in Core Shales of Upper Pennsylvanian Kansas-Type Cyclothems. Chemical Geology, 206(3/4): 289–318. https://doi.org/10.1016/j.chemgeo.2003.12.009

Algeo, T. J., Rowe, H., 2012. Paleoceanographic Applications of Trace-Metal Concentration Data. Chemical Geology, 324/325: 6–18. https://doi.org/10.1016/j.chemgeo.2011.09.002

Algeo, T. J., Tribovillard, N., 2009. Environmental Analysis of Paleoceanographic Systems Based on Molybdenum-Uranium Covariation. Chemical Geology, 268(3/4): 211–225. https://doi.org/10.13039/100000001

Algeo, T. J., 2004. Can Marine Anoxic Events Draw down the Trace Element Inventory of Seawater?. Geology, 32(12): 1057. https://doi.org/10.1130/g20896.1

Anbar, A. D., Duan, Y., Lyons, T. W., et al., 2007. A Whiff of Oxygen before the Great Oxidation Event?. Science, 317(5846): 1903–1906. https://doi.org/10.1126/science.1140325

Bjerrum, C. J., Canfield, D. E., 2011. Towards a Quantitative Understanding of the Late Neoproterozoic Carbon Cycle. Proceedings of the National Academy ofSciences, 108(14): 5542–5547. https://doi.org/10.1073/pnas.1101755108

Brasier, M., Antciliffe, J., 2004. Paleobiology: Decoding the Ediacaran Enigma. Science, 305(5687): 1115–1117. https://doi.org/10.1126/science.1102673

Bristow, T. F., Kennedy, M. J., Derkowski, A., et al., 2009. Mineralogical Constraints on the Paleoenvironments of the Ediacaran Doushantuo Formation. Proceedings of the National Academy of Sciences, 106(32): 13190–13195. https://doi.org/10.1073/pnas.0901080106

Canfield, D. E., Poulton, S. W., Narbonne, G. M., 2007. Late-Neoproterozoic Deep-Ocean Oxygenation and the Rise of Animal Life. Science, 315(5808): 92–95. https://doi.org/10.1126/science.1135013

Chen, X., Ling, H. F., Vance, D., et al., 2015. Rise to Modern Levels of Ocean Oxygenation Coincided with the Cambrian Radiation of Animals. Nature Communications, 6: 7142. https://doi.org 10.1038/ncomms8142

Condon, D., Zhu, M., Bowring, S., et al., 2005. U-Pb Ages from the Neoproterozoic Doushantuo Formation, China. Science, 308(5718): 95–98. https://doi.org/10.1126/science.1107765

Crusius, J., Calvert, S., Pedersen, T., et al., 1996. Rhenium and Molybdenum Enrichments in Sediments as Indicators of Oxic, Suboxic and Sulfidic Conditions of Deposition. Earth and Planetary Science Letters, 145(1–4): 65–78. https://doi.org/10.1016/s0012-821x(96)00204-x

Fan, H. F., Zhu, X. K., Wen, H. J., et al., 2014. Oxygenation of Ediacaran Ocean Recorded by Iron Isotopes. Geochimica et Cosmochimica Acta, 140: 80–94. https://doi.org/10.1016/j.gca.2014.05.029

Fike, D. A., Grotzinger, J. P., Pratt, L. M., et al., 2006. Oxidation of the Ediacaran Ocean. Nature, 444(7120): 744–747. https://doi.org/10.1038/nature05345

Guo, Q. J., Shields, G. A., Liu, C. Q., et al., 2007. Trace Element Chemostratigraphy of Two Ediacaran–Cambrian Successions in South China: Implications for Organosedimentary Metal Enrichment and Silicification in the Early Cambrian. Palaeogeography, Palaeoclimatology, Palaeoecology, 254(1/2): 194–216. https://doi.org/10.1016/j.paleo.2007.03.016

Halverson, G. P., Dudás, F. ., Maloof, A. C., et al., 2007. Evolution of the ⁸⁷Sr/⁸⁶Sr Composition of Neoproterozoic Seawater. Palaeogeography, Palaeoclimatology, Palaeoecology, 256(3/4): 103–129. https://doi.org/10.1016/j.paleo.2007.02.028

Halverson, G. P., Wade, B. P., Hurtgen, M. T., et al., 2010. Neoproterozoic Chemostratigraphy. Precambrian Research, 182(4): 337–350. https://doi.org/10.1016/j.precamres.2010.04.007

Hatch, J. R., Leventhal, J. S., 1992. Relationship between Inferred Redox Potential of the Depositional Environment and Geochemistry of the Upper Pennsylvanian (Missourian) Stark Shale Member of the Dennis Limestone, Wabaunsee County, Kansas, U.S.A.. Chemical Geology, 99(1/2/3): 65–82. https://doi.org/10.1016/0009-2541(92)90031-y

Jiang, G. Q., Shi, X. Y., Zhang, S. H., et al., 2011. Stratigraphy and Paleogeography of the Ediacaran Doushantuo Formation (ca. 635–551 Ma) in South China. Gondwana Research, 19(4): 831–849. https://doi.org/10.1016/j.gr.2011.01.006

Jones, B., Manning, D. A. C., 1994. Comparison of Geochemical Indices Used for the Interpretation of Palaeoredox Conditions in Ancient Mudstones. Chemical Geology, 111(1/2/3/4): 111–129. https://doi.org/10.1016/0009-2541(94)90085-x

Kendall, B., Komiya, T., Lyons, T. W., et al., 2015. Uranium and Molybdenum Isotope Evidence for an Episode of Widespread Ocean Oxygenation during the Late Ediacaran Period. Geochimica et Cosmochimica Acta, 156: 173–193. https://doi.org/10.13039/100000001

Kendall, B. S., 2008. Rhenium-Osmium Geochronology of Precambrian Organic-Rich Sedimentary Rocks, Systematics and Applications: [Dissertation]. University of Alberta, Edmonton, Alberta. 59

Kendall, B., Creaser, R. A., Selby, D., 2009. ¹⁸⁷Re-¹⁸⁷Os Geochronology of Precambrian Organic-Rich Sedimentary Rocks. Geological Society, London, Special Publications, 326(1): 85–107. https://doi.org/10.1144/SP326.5

Knoll, A. H., Walter, M. R., Narbonne, G. M., et al., 2004. Geology: A New Period for the Geologic Time Scale. Science, 305(5684): 621–622. https://doi.org/10.1126/science.1098803

Knoll, A., Walter, M., Narbonne, G., et al., 2006. The Ediacaran Period: A New Addition to the Geologic Time Scale. Lethaia, 39(1): 13–30. https://doi.org/10.1080/00241160500409223

Li, C., Love, G. D., Lyons, T. W., et al., 2010. A Stratified Redox Model for the Ediacaran Ocean. Science, 328(5974): 80–83. https://doi.org/10.1126/science.1182369

Li, C., Zhu, M. Y., Chu, X. L., 2016. Preface: Atmospheric and Oceanic Oxygenation and Evolution of Early Life on Earth: New Contributions from China. Journal of Earth Science, 27(2): 167–169. https://doi.org/10.1007/s12583-016-0697-1

Liu, P. J., Yin, C. Y., Gao, L. Z., et al., 2009. New Material of Microfossils from the Ediacaran Doushantuo Formation in the Zhangcunping Area, Yichang, Hubei Province and its Zircon SHRIMP U-Pb Age. Science Bulletin, 54(6): 1058–1064. https://doi.org/10.1007/s11434-008-0589-6

Liu, P. J., Chen, S. M., Zhu, M. Y., et al., 2014. High-Resolution Biostratigraphic and Chemostratigraphic Data from the Chenjiayuanzi Section of the Doushantuo Formation in the Yangtze Gorges Area, South China: Implication for Subdivision and Global Correlation of the Ediacaran System. Precambrian Research, 249: 199–214. https://doi.org/10.1016/j.precamres.2014.05.014

Liu, P. J., Yin, C. Y., Chen, S. M., et al., 2013. The Biostratigraphic Succession of Acanthomorphic Acritarchs of the Ediacaran Doushantuo Formation in the Yangtze Gorges Area, South China and Its Biostratigraphic Correlation with Australia. Precambrian Research, 225: 29–43. https://doi.org/10.1016/j.precamres.2011.07.009

Lyons, T. W., Reinhard, C. T., Planavsky, N. J., 2014. The Rise of Oxygen in Earth's Early Ocean and Atmosphere. Nature, 506(7488): 307–315. https://doi.org/10.1038/nature13068

McArthur, J. M., Algeo, T. J., van de Schootbrugge, B., et al., 2008. Basinal Restriction, Black Shales, Re-Os Dating, and the Early Toarcian (Jurassic) Oceanic Anoxic Event. Paleoceanography, 23(4): PA4217. https://doi.org/10.1029/2008pa001607

McCall, G. J. H., 2006. The Vendian (Ediacaran) in the Geological Record: Enigmas in Geology's Prelude to the Cambrian Explosion. Earth-Science Reviews, 77(1/2/3): 1–229. https://doi.org/10.1016/j.earscirev.2005.08.004

McFadden, K. A., Huang, J., Chu, X., et al., 2008. Pulsed Oxidation and Biological Evolution in the Ediacaran Doushantuo Formation. Proceedings of the National Academy of Sciences, 105(9): 3197–3202. https://doi.org/10.1073/pnas.0708336105

Mi, T. W., Lin, L., Pang, Y. C., et al., 2010. The Sequence Stratigraphy and Genesis of Phosphorites of Doushantuo Formation at Baiguoyuan, Yichang, Hubei. Acta Sedimentologica Sinica, 28(3): 471–480 (in Chinese with English Abstract) https://www.researchgate.net/publication/288846791_The_sequence_stratigraphy_and_genesis_of_phosphorites_of_Doushantuo_Formation_at_Baiguoyuan_Yichang_Hubei

Och, L. M., Cremonese, L., Shields-Zhou, G. A., et al., 2015. Palaeoceanographic Controls on Spatial Redox Distribution over the Yangtze Platform during the Ediacaran–Cambrian Transition. Sedimentology, 63(2): 378–410. https://doi.org/10.13039/501100001659

Perkins, R. B., Piper, D. Z., Mason, C. E., 2008. Trace-Element Budgets in the Ohio/Sunbury Shales of Kentucky: Constraints on Ocean Circulation and Primary Productivity in the Devonian–Mississippian Appalachian Basin. Palaeogeography, Palaeoclimatology, Palaeoecology, 265(1/2): 14–29. https://doi.org/10.1016/j.paleo.2008.04.012

Reinhard, C. T., Planavsky, N. J., Robbins, L. J., et al., 2013. Proterozoic Ocean Redox and Biogeochemical Stasis. Proceedings of the National Academy of Sciences, 110(14): 5357–5362. https://doi.org/10.1073/pnas.1208622110

Ries, J. B., Fike, D. A., Pratt, L. M., et al., 2009. Superheavy Pyrite (³⁴S_pyr > ³⁴S_CAS) in the Terminal Proterozoic Nama Group, Southern Namibia: A Consequence of Low Seawater Sulfate at the Dawn of Animal Life. Geology, 37(8): 743–746. https://doi.org/10.1130/g25775a.1

Rimmer, S. M., 2004. Geochemical Paleoredox Indicators in Devonian–Mississippian Black Shales, Central Appalachian Basin (USA). Chemical Geology, 206(3/4): 373–391. https://doi.org/10.1016/j.chemgeo.2003.12.029

Sahoo, S. K., Planavsky, N. J., Jiang, G., et al., 2016. Oceanic Oxygenation Events in the Anoxic Ediacaran Ocean. Geobiology, 14(5): 457–468. https://doi.org/10.13039/501100001809

Sahoo, S. K., Planavsky, N. J., Kendall, B., et al., 2012. Ocean Oxygenation in the Wake of the Marinoan Glaciation. Nature, 489(7417): 546–549. https://doi.org/10.1038/nature11445

Scott, C., Lyons, T. W., Bekker, A., et al., 2008. Tracing the Stepwise Oxygenation of the Proterozoic Ocean. Nature, 452(7186): 456–459. https://doi.org/10.1038/nature06811

Tribovillard, N., Algeo, T. J., Baudin, F., et al., 2012. Analysis of Marine Environmental Conditions Based Onmolybdenum-Uranium Covariation—Applications to Mesozoic Paleoceanography. Chemical Geology, 324–325: 46–58. https://doi.org/10.1016/j.chemgeo.2011.09.009

Tribovillard, N., Algeo, T. J., Lyons, T., et al., 2006. Trace Metals as Paleoredox and Paleoproductivity Proxies: An Update. Chemical Geology, 232(1/2): 12–32. https://doi.org/10.1016/j.chemgeo.2006.02.012

Vernhet, E., Reijmer, J. J. G., 2010. Sedimentary Evolution of the Ediacaran Yangtze Platform Shelf (Hubei and Hunan Provinces, Central China). Sedimentary Geology, 225(3/4): 99–115. https://doi.org/10.1016/j.sedgeo.2010.01.005

Wignall, P. B., Twitchett, R. J., 1996. Oceanic Anoxia and the End Permian Mass Extinction. Science, 272(5265): 1155–1158. https://doi.org/10.1126/science.272.5265.1155

Xiao, S. H., Muscente, A. D., Chen, L., et al., 2014. The Weng'an Biota and the Ediacaran Radiation of Multicellular Eukaryotes. National Science Review, 1(4): 498–520. https://doi.org/10.1093/nsr/nwu061

Xiao, S. H., Yuan, X. L., Steiner, M., et al., 2002. Macroscopic Carbonaceous Compressions in a Terminal Proterozoic Shale: A Systematic Reassessment of the Miaohe Biota, South China. Journal of Paleontology, 76(2): 347–376. https://doi.org/10.1666/0022-3360(2002)076<0347:mcciat>2.0.co;2 doi: 10.1666/0022-3360(2002)076<0347:mcciat>2.0.co;2

Xiao, S. H., Knoll, A. H., 2007. Fossil Preservation in the Neoproterozoic Doushantuo Phosphorite Lagerst tte, South China. Lethaia, 32(3): 219–238. https://doi.org/10.1111/j.1502-3931.1999.tb00541.x

Yin, L. M., Zhu, M. Y., Knoll, A. H., et al., 2007. Doushantuo Embryos Preserved Inside Diapause Egg Cysts. Nature, 446(7136): 661–663. https://doi.org/10.1038/nature05682

Zhai, L. N., Wu, C. D., Ye, Y., et al., 2016. Marine Redox Variations during the Ediacaran–Cambrian Transition on the Yangtze Platform, South China. Geological Journal. https://doi.org/10.1002/gj.2878

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. Geochimica et Cosmochimica Acta, 64(24): 4165–4178. https://doi.org/10.1016/s0016-7037(00)00495-6

Zhou, C. M., Jiang, S. Y., 2009. Palaeoceanographic Redox Environments for the Lower Cambrian Hetang Formation in South China: Evidence from Pyrite Framboids, Redox Sensitive Trace Elements, and Sponge Biota Occurrence. Palaeogeography, Palaeoclimatology, Palaeoecology, 271(3/4): 279–286. https://doi.org/10.1016/j.paleo.2008.10.024

Zhou, C. M., Xie, G. W., McFadden, K., et al., 2007. The Diversification and Extinction of Doushantuo-Pertatataka Acritarchs in South China: Causes and Biostratigraphic Significance. Geological Journal, 42(3/4): 229–262. https://doi.org/10.1002/gj.1062

Zhu, B., Becker, H., Jiang, S. Y., et al., 2013. Re-Os Geochronology of Black Shales from the Neoproterozoic Doushantuo Formation, Yangtze Platform, South China. Precambrian Research, 225(2013): 67–76. https://doi.org/10.1016/j.precamres.2012.02.002

Zhu, M. Y., Zhang, J. M., Steiner, M., et al., 2003. Sinian-Cambrian Stratigraphic Framework for Shallow-to Deep-Water Environments of the Yangtze Platform: An Integrated Approach. Progress in Natural Science, 13(12): 951–960. https://doi.org/10.1080/10020070312331344710

Zhu, M. Y., Lu, M., Zhang, J. M., et al., 2013. Carbon Isotope Chemostratigraphy and Sedimentary Facies Evolution of the Ediacaran Doushantuo Formation in Western Hubei, South China. Precambrian Research, 225(1): 7–28. https://doi.org/10.1016/j.precamres.2011.07.019

Zhu, M. Y., Zhang, J. M., Yang, A. H., 2007. Integrated Ediacaran (Sinian) Chronostratigraphy of South China. Palaeogeography, Palaeoclimatology, Palaeoecology, 254(1/2): 7–61. https://doi.org/10.1016/j.paleo.2007.03.025

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Trace Elements Characteristics of Black Shales from the Ediacaran Doushantuo Formation, Hubei Province, South China: Implications for Redox and Open vs. Restricted Basin Conditions

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