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Nd isotope composition of the Ediacaran and earliest Cambrian phosphorite nodules and Fe sulphide from the East European Platform

Published online by Cambridge University Press:  19 August 2020

Sergey B Felitsyn Open the ORCID record for Sergey B Felitsyn [Opens in a new window]  and
Eugeny S. Bogomolov
Sergey B Felitsyn*
Affiliation:
Institute of Precambrian Geology and Geochronology, Russian Academy of Sciences, Makarova 2, 199034St Petersburg, Russia
Eugeny S. Bogomolov
Affiliation:
Institute of Precambrian Geology and Geochronology, Russian Academy of Sciences, Makarova 2, 199034St Petersburg, Russia
*
Author for correspondence: Sergey B. Felitsyn, Email: [email protected]
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Abstract

An enhanced concentration of phosphorus has been found at the stratigraphic level of the disappearance of Ediacaran taxa in two areas, the Cis-Dniester region and the Moscow syneclise, on the East European Platform (EEP). The isotope composition of neodymium was determined in Fe sulphide and phosphorite in the same beds. Measured εNd(t) values in diagenetic phosphate nodules are similar to those in iron sulphide from the same layer. During the Ediacaran − Early Cambrian, accumulation of radiogenic Nd in the epeiric basins on the EEP increased progressively from −17.9 and −19.4 in pyrite from the sequence bottom to −7.9 and −8.5 in the Early Cambrian pyrite of the central part of the EEP. The Ediacaran phosphate nodules show εNd(t) ranging from −12.9 to −15.0, while that in the Early Cambrian nodules is typically c. −9.0. These data indicate the secular change in Nd isotope composition of the water reservoir on the EEP from Ediacaran to Cambrian.

Keywords

East European PlatformEdiacaranCambriandiagenetic iron sulphidephosphoriteNd isotope composition
Type
Original Article
Information
Geological Magazine , Volume 157 , Issue 12 , December 2020 , pp. 2081 - 2088
Copyright
© The Author(s), 2020. Published by Cambridge University Press

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References

Afanasieva, MS, Burzin, MB, Mikhailova, MV and Kuzmenko, YuT (1995) Depositional conditions of the potentially oil-generated sediments. Oil and Gas Geology 4, 42–8 (in Russian).Google Scholar
Bayon, G, Toucanne, S, Skonieczny, C, André, L, Bermell, S, Cheron, S, Dennielou, B., Etoubleau, J, Freslon, N, Gauchery, T, Germain, Y, Jorry, SJ, Ménot, G, Monin, L, Ponzevera, E, Rouget, M-L, Tachikawa, K and Barrat, J-A (2015) Rare earth elements and neodymium isotopes in world river sediments revisited. Geochimica et Cosmochimica Acta 170, 17–38.CrossRefGoogle Scholar
Borkhvardt, DV and Felitsyn, SB (1992) Geochemistry of volcanic tuff from Redkino Horizon, Upper Vendian, Russian Platform. Volcanology and Seismology 1, 32–45.Google Scholar
Bouvier, A, Vervoort, JD and Patchett, PJ (2008) The Lu-Hf and Sm-Nd isotopic composition of CHUR: constraints from unequlibrated chondrites and implications for the bulk composition of terrestrial planets. Earth and Planetary Sciences Letters 273, 48–57.CrossRefGoogle Scholar
Bowring, SA, Grotzinger, JP, Isachsen, CE, Knoll, AH, Pelechaty, SM and Kolosov, P (1993) Calibrating rates of Early Cambrian evolution. Science 261, 1293–8.CrossRefGoogle ScholarPubMed
Brasier, MD (1992) Paleoceanography and changes in the biological cycling of phosphorus across the Precambrian-Cambrian Boundary. In Origin and Early Evolution of the Metazoa (eds Lipps, JH and Signor, PhW), pp. 483–523. New York: Plenum Press.CrossRefGoogle Scholar
Charbonnier, G, Pucéat, E, Bayon, G, Desmares, D, Dera, G, Durlet, Ch, Deconinck, J-F, Amédro, F, Gourlan, AT, Pellenard, P and Bomou, B (2012) Reconstruction of the Nd isotope composition of seawater on epicontinental seas: testing the potential of Fe-Mn oxyhydroxide coating on foraminifera tests for deep-time investigations. Geochimica et Cosmochimica Acta 99, 39–56.CrossRefGoogle Scholar
Compston, W, Sambridge, MS, Reinfrank, RF, Moczydłowska, M, Vidal, G and Claesson, S (1995) Numerical ages of volcanic rocks and the earliest faunal zone within the Late Precambrian of east Poland. Journal of the Geological Society, London 152, 599–611.CrossRefGoogle Scholar
Cook, PJ and Shergold, JH (1984) Phosphorus, phosphorites and skeletal evolution at the Precambrian-Cambrian boundary. Nature 308, 231–6.CrossRefGoogle Scholar
Emsbo, P, McLaughlin, PI, Breit, GN, du Bray, EA and Koenig, AE (2015) Rare earth elements in sedimentary phosphate deposits: solution to the global REE crisis? Gondwana Research 27, 776–85.CrossRefGoogle Scholar
Felitsyn, S and Gubanov, A (2002) Nd isotope composition of early Cambrian discrete basins. Geological Magazine 139, 159–69.CrossRefGoogle Scholar
Felitsyn, S and Morad, S (2002) REE patterns in latest Neoproterozoic – early Cambrian phosphate concretions and associated organic matter. Chemical Geology 187, 257–65.CrossRefGoogle Scholar
Felitsyn, SB and Sochava, AV (1996) Eu/Eu* in Upper Vendian clay shale of the Russian Platform. Doklady Earth Sciences 351, 521–4.Google Scholar
Felitsyn, SB, Vidal, G and Moczydłowska, M (1998) Trace elements and Sr and C isotopic signatures in late Neoproterozoic and earliest Cambrian sedimentary organic matter from siliciclastic successions in the East European Platform. Geological Magazine 135, 537–51.CrossRefGoogle Scholar
Golonka, J and Gawęda, A (2012) Plate tectonic evolution of the southern margin of Laurussia in the Paleozoic.. In Tectonic Recent Advances (ed Sharkov, EV), pp. 261–82. Moscow: InTech.Google Scholar
Haley, B, Klinkhammer, GP and McManus, J (2004) Rare earth elements in pore waters of marine sediments. Geochimica et Cosmochimica Acta 68, 1265–79.CrossRefGoogle Scholar
Hein, JR, Koschinsky, A, Mikesell, M, Mizell, K, Glenn, CR and Wood, R (2016) Marine phosphorites as potential resources for heavy rare earth elements and yttrium. Minerals 88, 1–22.Google Scholar
Himmler, T, Haley, B, Torres, ME, Klinkhammer, GP, Bohrmann, G and Peckmann, J (2013) Rare earth element geochemistry in cold-waters of Hydrate Ridge, northeast Pacific Ocean. Geo-Marine Letters 33, 369–79.CrossRefGoogle Scholar
Huerta-Diaz, MA and Morse, JW (1992) Pyritization of trace metals in anoxic marine sediments. Geochimica et Cosmochimica Acta 56, 2681–702.CrossRefGoogle Scholar
Jweda, J, Bolge, L, Class, C and Goldstein, SL (2015) High precision Sr-Nd-Hf-Pb isotopic compositions of USGS Reference Material BCR-2. Geostandards and Geoanalytical Research 40, 101–15.CrossRefGoogle Scholar
Kitamura, M, Matsuda, H and Morimoto, N (1986) Direct observation of the Cottrell atmosphere in olivine. Proceedings of the Japan Academy, Series B 62, 149–52.CrossRefGoogle Scholar
Kopeliovich, AV (1965) Epigenesis of the Old Series, South Western Part of the Russian Platform. Moscow: Nauka, 310 pp. (in Russian).Google Scholar
Krasilnikova, NA, Krasilnikova, IG & Yudin, NI (1989) Composition and conditions of formation of Precambrian phosphate nodules. In Precambrian Concretions (eds Golovenok, VK and Sochava, AV), pp. 44–50. Leningrad: Nauka (in Russian).Google Scholar
Lacan, F, Tchikawa, K and Jeandel, C (2012) Neodymium isotopic composition of the oceans: a compilation of seawater data. Chemical Geology 300–301, 177–184.Google Scholar
Landing, E, Geyer, G, Buchwaldt, R and Bowring, SA (2014) Geochronology of the Cambrian: a precise Middle Cambrian U-Pb zircon date from the German margin of West Gondwana. Geological Magazine 152, 28–40.CrossRefGoogle Scholar
Linnemann, U, Ovtcharova, M, Schaltegger, U, Gatrner, A, Hautmann, M, Geyer, G, Vickers-Rich, P, Rich, T, Plessen, B, Hofmann, M, Zieger, J, Krause, R, Kriesfeld, L and Smith, J (2019) New high-resolution age data from the Ediacaran−Cambrian boundary indicate rapid, ecologically driven onset of the Cambrian explosion. Terra Nova 31, 44–58.CrossRefGoogle Scholar
Malinowsky, FM (1955) Sulphide-bearing phosphorite in Podolia. Proceedings of the All-Union Mineralogical Society 84, 30–42 (in Russian).Google Scholar
Mao, G, Hua, R, Gao, J, Li, W, Zhao, K, Long, G and Lu, H (2009) Existing forms of REE in gold-bearing pyrite in the Jinshan gold deposit, Jiangxi Province. Journal of Rare Earths 27, 1079–87.CrossRefGoogle Scholar
Martin, MW, Grazhdankin, DV, Bowring, SA, Evans, DAD, Fedonkin, MA and Kirschvink, JI (2000) Age of Neoproterozoic Bilaterian body and trace fossils, White Sea, Russia: implications for Metazoan Evolution. Science 288, 841–45.CrossRefGoogle ScholarPubMed
Mikova, J and Denkova, P (2007) Modified chromatographic separation scheme for Sr and Nd isotope analysis in geological silicate samples. Journal of Geosciences 52, 221–26.Google Scholar
Moczydłowska, M (1991) Acritarch biostratigraphy of the Lower Cambrian and the Precambrian-Cambrian boundary in south-eastern Poland. Fossils and Strata 29, 1–127.Google Scholar
Paul, SAL, Gaye, B, Haeckel, M, Kasten, S and Koschinsky, A (2018) Biogeochemical regeneration of a nodule mining disturbance site: trace metals, DOC, and amino acids in deep-sea sediments and pore waters. Frontiers of Marine Sciences 5, 1–17.Google Scholar
Raczek, I, Stoll, B, Hofmann, AW and Jochum, KP (2001) High-precision trace element data for the USGS reference materials BCR-1, BCR-2, BHVO-1, BHVO-2, AGV-1, AGV-2, DTS-1, DTS-2, GSP-1 and GSP-2 by ID-TIMS and MIC-SSMS. Geostandards Newsletter 25, 77–86.CrossRefGoogle Scholar
Reddy, SM, Riessen, AV, Saxey, DW, Johnson, TE, Rickard, WDA, Fougerouse, D, Fisher, S, Prosa, TJ, Rice, KP, Reinhard, DA, Chen, Y and Olson, D (2016) Mechanisms of deformation-induced trace element migration in zircon resolved by atom probe and correlative microscopy, Geochimica et Cosmochimica Acta 196, 158–70.CrossRefGoogle Scholar
Reynard, B, Lécuyer, C and Grandjean, P (1999) Crystal-chemical controls of rare-earth element concentrations in fossil biogenic apatites and implication for paleoenvironmental reconstructions. Chemical Geology 155, 233–41.CrossRefGoogle Scholar
Rickard, D and Luther, GW (2007) Chemistry of iron sulfides. Chemical Review 107, 514–62.CrossRefGoogle ScholarPubMed
Scheiber, J (2011) Iron sulfide formation. In Encyclopedia of Geobiology (eds Reiner, J and Tiel, V), pp. 486–502. Dordrecht: Springer Verlag.CrossRefGoogle Scholar
Shatrov, VA, Woitsekhowsky, GV and Sirotin, VN (2007) Microelements in pyrites from sedimentary cover, Voronezh anteclise: opportunities for the reconstruction of conditions during the sedimentation. Vestnik VGU, Geology 2, 53–62 (in Russian).Google Scholar
Shaw, HF and Wasserburg, GJ (1985) Sm-Nd in marine carbonates and phosphates: implications for Nd isotopes in seawater and crustal ages. Geochimica et Cosmochimica Acta 49, 503–18.CrossRefGoogle Scholar
Sochava, AV, Korenchuk, LV, Pirrus, E and Felitsyn, SB (1992) Geochemistry of Upper Vendian rocks in the Russian Platform. Lithology and Mineral Resources 2, 71–89.Google Scholar
Sochava, AV, Podkovyrov, VN and Felitsyn, SB (1994) The evolution of terrigenous rocks in Late Precambrian. Stratigraphy and Geological Correlation 2, 307–24.Google Scholar
Sokolov, BS and Fedonkin, MA (eds) (1990) The Vendian System 2. Berlin: Springer Verlag: 273 pp.Google Scholar
Soldatenko, Y, El Albani, A, Ruzina, M, Fontaine, C, Nesterovsky, V, Paquette, J-L, Meunier, A and Ovtcharova, M (2019) Precise U-Pb age constraints on the Ediacaran biota in Podolia, East European Platform, Ukraine. Scientific Reports 9, 1675. doi: 10.1038/s41598-018-38448-9.CrossRefGoogle Scholar
Strauss, H, Vidal, G, Moczydłowska, M and Pacześna, J (1997) Carbon isotope geochemistry and paleontology of Neoproterozoic to early Cambrian siliciclastic successions in the East European Platform. Geological Magazine 134, 1–16.CrossRefGoogle Scholar
Sturesson, U, Popov, LE, Holmer, LE, Basset, MG, Felitsyn, SB and Belyatsky, BV (2005) Neodymium isotopic composition of Cambrian–Ordovician biogenic apatite in the Baltoscandian Basin: implications for palaeogeographical evolution and patterns of biodiversity. Geological Magazine 142, 419–39.CrossRefGoogle Scholar
Sverjensky, DA (1984) Europium redox equilibria in aqueous solution. Earth and Planetary Science Letters 67, 70–8.CrossRefGoogle Scholar
Tachikava, K, Arsouze, T, Bayon, G, Bory, A, Colin, C, Dutay, J-C, Frank, N, Giraud, X, Gourlan, AT, Jeandel, C, Lacan, F, Meynadier, L, Montagna, P, Piotrowski, AM, Plancherel, Y, Pucéat, E, Roy, M and Waelbroeck, C (2017) The large-scale evolution of neodymium isotopic composition in the global modern and Holocene ocean revealed from seawater and archive data. Chemical Geology 457, 137–48.Google Scholar
Tanaka, T, Kamioka, H, Togashi, S and Dragusanu, CJ (2000) Ndi-1: a neodymium isotopic reference in consistency with La Jolla neodymium. Chemical Geology 168, 279–81.CrossRefGoogle Scholar
Trueman, CN and Tuross, N (2002) Trace elements in recent and fossil bone apatite. Reviews in Mineralogy and Geochemistry 48, 489–521.CrossRefGoogle Scholar
van de Flierdt, T, Griffiths, AM, Lambelet, M, Little, SH, Stichel, T and Wilson, DJ (2016) Neodymium in the oceans global data base, a regional comparison and implications for palaeoceanographic research. Philosophical Transactions of the Royal Society A 374, 20150293. doi: 10.1098/rsta.2015.0293.Google Scholar
Văscăutzanu, Th (1931) Les formations siluriennes de la rive roumaine du Dniester. Anuarul Institutului Geologic al României 15, 585–663.Google Scholar
Vidal, G and Moczydłowska, M (1995) The Neoproterozoic of Baltica – stratigraphy, paleobiology and general geological evolution. Precambrian Research 73, 197–216.CrossRefGoogle Scholar