Abstract
Banded iron formations (BIFs) are chemical sediments that reflect the composition of the seawater from which they were deposited. Therefore, they provide a key part of the evidence for the modern scientific understanding of paleoenvironmental conditions in Archean and Paleoproterozoic times. Although BIFs have been extensively studied, many aspects (e.g., specific mechanisms controlling iron (Fe) and silicon (Si) precipitations) of their origin still remain enigmatic because of the lack of modern analogues. In China, abundant BIFs occur throughout within the late Neoarchean volcanic and sedimentary succession and therefore are the principal source of Fe for the Chinese steel industry. Here, we examine the ~ 2.53 Ga Qidashan BIF, one of the most extensive BIFs in China, by conducting a detailed petrographic and multi-proxy investigation to well constrain its formation mechanism. The BIF consists mainly of magnetite and quartz with lesser amounts of calcite and various types of silicate minerals, of which the content of Al-rich minerals (i.e., chlorite) is rare, coupled with a low abundance of detrital geochemical indicators (e.g., Al and Ti), suggesting that the BIF is relatively pure with insignificant terrigenous contamination. A wide range of Nd isotope compositions and shale-normalized patterns and specific anomalies of rare earth elements, especially highly positive Eu anomalies, indicate that the BIF precipitated from seawater imprinted by high-temperature hydrothermal fluids. Furthermore, there is a significantly negative correlation between Nd isotope values and total Fe contents of the BIF. This suggests that such enhanced hydrothermal activity provided vast volumes of dissolved Fe(II) necessary for the formation of the BIF via alteration of ancient continental crust. In addition, the Qidashan BIF was deposited under pervasively anoxic conditions, as revealed by the absence of shale-normalized Ce anomalies and the presence of consistently positive Fe isotope values. Hence, anoxygenic photosynthesis is the most plausible mechanism responsible for Fe(II) oxidation. Given that Fe─Si bonding has a strong impact on Si isotope fractionation, the formation of primary Fe(III) oxyhydroxides should have exerted a first-order control on the negative Si isotope signatures observed in the studied BIF samples. It is also noted that the BIF possesses a variation of negative Si isotope values, further implying that diagenetic dissolution and reprecipitation of silica took place after primary Si precipitation associated with Fe.
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References
Alexander BW, Bau M, Andersson P (2009) Neodymium isotopes in Archean seawater and implications for the marine nd cycle in Earth’s early oceans. Earth Planet Sci Lett 283:144–155. https://doi.org/10.1016/j.epsl.2009.04.004
Alexander BW, Bau M, Andersson P, Dulski P (2008) Continentally-derived solutes in shallow Archean seawater: rare earth element and nd isotope evidence in iron formation from the 2.9 Ga Pongola Supergroup, South Africa. Geochim Cosmochim Acta 72:378–394. https://doi.org/10.1016/j.gca.2007.10.028
Alibert C, McCulloch MT (1993) Rare earth element and nd isotopic compositions of the banded iron-formations and associated shales from Hamersley, Western Australia. Geochim Cosmochim Acta 57:187–204. https://doi.org/10.1016/0016-7037(93)90478-F
Alibo DS, Nozaki Y (1999) Rare earth elements in seawater: particle association, shale- normalization, and ce oxidation. Geochim Cosmochim Acta 63:363–372. https://doi.org/10.1016/S0016-7037(98)00279-8
André L, Cardinal D, Alleman LY, Moorbath S (2006) Silicon isotopes in ∼3.8 Ga West Greenland rocks as clues to the Eoarchaean Supracrustal Si cycle. Earth Planet Sci Lett 245(1–2):162–173. https://doi.org/10.1016/j.epsl.2006.02.046
Basile-Doelsch I, Meunier JD, Parron C (2005) Another continental pool in the terrestrial silicon cycle. Nature 433(7024):399–402. https://doi.org/10.1038/nature03217
Bau M (1993) Effects of syn- and post-depositional processes on the rare-earth element distribution in Precambrian Iron-formations. Eur J Mineral 5:257–267. https://doi.org/10.1127/ejm/5/2/0257
Bau M (1999) Scavenging of dissolved yttrium and rare earths by precipitating Fe oxyhydroxide: experimental evidence for ce oxidation, Y–Ho fractionation, and lanthanide tetrad effect. Geochim Cosmochim Acta 63:67–77. https://doi.org/10.1016/S0016-7037(99)00014-9
Bau M, Alexander BW Distribution of high field strength elements (Y, Zr REE, Hf, Ta (2009) Th, U) in adjacent magnetite and chert bands and in reference standards FeR-3 and FeR-4 from the Temagami iron-formation, Canada, and the redox level of the Neoarchean ocean. Precambrian Res 174: 337–346. https://doi.org/10.1016/j.precamres.2009.08.007
Bau M, Dulski P (1996) Distribution of yttrium and rare-earth elements in the Penge and Kuruman iron formations, Transvaal Supergroup, South Africa. Precambrian Res 79:37–55. https://doi.org/10.1016/0301-9268(95)00087-9
Bau M, Dulski P (1999) Comparing yttrium and rare earths in hydrothermal fluids from the Mid-atlantic Ridge: implications for Y and REE behaviour during near-vent mixing and for the Y/Ho ratio of Proterozoic seawater. Chem Geol 155:77–90. https://doi.org/10.1016/S0009-2541(98)00142-9
Bau M, Höhndorf A, Dulski P, Beukes NJ (1997) Sources of rare-earth elements and iron in Paleoproterozoic ironformations from the Transvaal Supergroup, South Africa: evidence from neodymium isotopes. J Geol 105:121–129. https://doi.org/10.1086/606152
Bau M, Schmidt K, Koschinsky A, Hein J, Kuhn T, Usui A (2014) Discriminating between different genetic types of marine ferro-manganese crusts and nodules based on rare earth elements and yttrium. Chem Geol 381:1–9. https://doi.org/10.1016/j.chemgeo.2014.05.004
Bekker A, Planavsky N, Rasmussen B, Krapež B, Hofmann A, Slack J, Rouxel O, Konhauser K (2014) Iron formations: Their origins and implications for ancient seawater chemistry. In: Mackenzie FT (ed) Sediments, Diagenesis and Sedimentary Rocks. Elsevier, Amsterdam, Treatise on Geochemistry (2nd Ed), 9, pp 561–628. https://doi.org/10.1016/B978-0-08-095975-7.00719-1
Bekker A, Slack JF, Planavsky NJ, Krapež B, Hofmann A, Konhauser KO, Rouxel OJ (2010) Iron formation: the sedimentary product of a Complex interplay among Mantle, Tectonic, Oceanic, and biospheric processes. Econ Geol 105:467–508. https://doi.org/10.2113/gsecongeo.105.3.467
Bolhar R, Hofmann A, Siahi M, Feng YX, Delvigne C (2015) A trace element and pb isotopic investigation into the provenance and deposition of stromatolitic carbonates, ironstones and associated shales of the ~ 3.0 Ga Pongola Supergroup, Kaapvaal Craton. Geochim Cosmochim Acta 158:57–78. https://doi.org/10.1016/j.gca.2015.02.026
Bolhar R, Kamber BS, Moorbath S, Fedo CM, Whitehouse MJ (2004) Characterisation of early archaean chemical sediments by trace element signatures. Earth Planet Sci Lett 222:43–60. https://doi.org/10.1016/j.epsl.2004.02.016
Bolhar R, Van Kranendonk MJ (2007) A non-marine depositional setting for the northern Fortescue Group, Pilbara Craton, inferred from trace element geochemistry of stromatolitic carbonates. Precambrian Res 155:229–250. https://doi.org/10.1016/j.precamres.2007.02.002
Bonnand P, Lalonde SV, Boyet M, Heubeck C, Homann M, Nonnotte P, Foster I, Konhauser KO, Köhler I (2020) Post-depositional REE mobility in a Paleoarchean banded iron formation revealed by La-Ce geochronology: a cautionary tale for signals of ancient oxygenation. Earth Planet Sci Lett 547:116452. https://doi.org/10.1016/j.epsl.2020.116452
Brengman LA, Fedo CM, Whitehouse MJ, Jabeen I, Banerjee NR (2021) Evaluating the geochemistry and paired silicon and oxygen isotope record of quartz in siliceous rocks from the ~ 3 Ga Buhwa Greenstone Belt, Zimbabwe, a critical link to deciphering the Mesoarchean silica cycle. Chem Geol 577:120300. https://doi.org/10.1016/j.chemgeo.2021.120300
Busigny V, Planavsky NJ, Jézéquel D, Crowe S, Louvat P, Moureau J, Viollier E, Lyons TW (2014) Iron isotopes in an Archean ocean analogue. Geochim Cosmochim Acta 133:443–462. https://doi.org/10.1016/j.gca.2014.03.004
Byrne R, Sholkovitz E (1996) Marine chemistry and geochemistry of the lanthanides. In: Gschneider KA, Eyring L (eds) Handbook on the Physics and Chemistry of the Rare Earths, vol 23. Elsevier, Amsterdam, pp 497–593. https://doi.org/10.1016/S0168-1273(96)23009-0
Cantrell K, Byrne R (1987) Rare earth element complexation by carbonate and oxalate ions. Geochim Cosmochim Acta 51:597–605. https://doi.org/10.1016/0016-7037(87)90072-X
Chakrabarti R, Knoll AH, Jacobsen SB, Fischer WW (2012) Si isotope variability in Proterozoic cherts. Geochim Cosmochim Acta 91:187–201. https://doi.org/10.1016/j.gca.2012.05.025
Chu ZY, Wu FY, Walker RJ, Rudnick RL, Pitcher L, Puchtel IS, Yang YH, Wilde SA (2009) Temporal evolution of the lithospheric mantle beneath the eastern North China Craton. J Petrol 50:1857–1898. https://doi.org/10.1093/petrology/egp055
Condie KC (2000) Episodic continental growth models: afterthoughts and extensions. Tectonophysics 322:153–162. https://doi.org/10.1016/S0040-1951(00)00061-5
Criss RE (1999). Principles of stable isotope distribution. Oxford University Press, New York.
Crowe SA, Jones C, Katsev S, Magen C, O’Neill AH, Sturm A, Canfield DE, Haffner GD, Mucci A, Sundby B, Fowle DA (2008) Photoferrotrophs thrive in an Archean Ocean analogue. Proc Nat Acad Sci USA 105:15938–15943. https://doi.org/10.1073/pnas.0805313105
Czaja AD, Johnson CM, Beard BL, Roden EE, Li WQ, Moorbath S (2013) Biological Fe oxidation controlled deposition of banded iron formation in the ca. 3770 Ma Isua Supracrustal Belt (West Greenland). Earth Planet Sci Lett 363:192–203. https://doi.org/10.1016/j.epsl.2012.12.025
Czaja AD, Johnson CM, Roden EE, Beard BL, Voegelin AR, Nägler TF, Beukes NJ, Wille M (2012) Evidence for free oxygen in the Neoarchean ocean based on coupled iron–molybdenum isotope fractionation. Geochim Cosmochim Acta 86:118–137. https://doi.org/10.1016/j.gca.2012.03.007
Danielson A, Möller P, Dulski P (1992) The europium anomalies in banded iron formations and the thermal history of the oceanic crust. Chem Geol 97:89–100. https://doi.org/10.1016/0009-2541(92)90137-T
Dauphas N, Cates NL, Mojzsis SJ, Busigny V (2007) Identification of chemical sedimentary protoliths using iron isotopes in the > 3750 Ma Nuvvuagittuq supracrustal belt, Canada. Earth Planet Sci Lett 254(3–4):358–376. https://doi.org/10.1016/j.epsl.2006.11.042
Dauphas N, John SG, Rouxel O (2017) Iron isotope systematics. Rev Mineral Geochem 82(1):415–510. https://doi.org/10.2138/rmg.2017.82.11
Dauphas N, Van Zuilen M, Wadhwa M, Davis AM, Marty B, Janney PE (2004) Clues from Fe isotope variations on the origin of early Archean BIFs from Greenland. Science 306(5704):2077–2080. https://doi.org/10.1126/science.1104639
De Baar HJW, Brewer PG, Bacon MP (1985) Anomalies in rare earth distributions in seawater: Gd and Tb. Geochim Cosmochim Acta 4:1961–1969. https://doi.org/10.1016/0016-7037(85)90090-0
De La Rocha CL, Brzezinkski MA, DeNiro MJ (2000) A first look at the distribution of the stable isotopes of silicon in natural waters. Geochim Cosmochim Acta 64:2467–2477. https://doi.org/10.1016/S0016-7037(00)00373-2
Delstanche S, Opfergelt S, Cardinal D, Elsass F, André L, Delvaux B (2009) Silicon isotopic fractionation during adsorption of aqueous monosilicic acid onto iron oxide. Geochim Cosmochim Acta 73(4):923–934. https://doi.org/10.1016/j.gca.2008.11.014
DePaolo DJ (1981) Neodymium isotopes in the Colorado Front Range and crust-mantle evolution in the Proterozoic. Nature 291:193–196. https://doi.org/10.1038/291193a0
Ding TP, Gao JF, Tian SH, Fan CF, Zhao Y, Wan DF, Zhou JX (2017) The δ30Si peak value discovered in middle Proterozoic chert and its implication for environmental variations in the ancient ocean. Sci Rep 7(1):1–15. https://doi.org/10.1038/srep44000
Ding TP, Jiang SY, Wang D (1996) Silicon Isotope Geochemistry. Geological Publishing House, Beijing
Dong CY, Wan YS, Xie HQ, Nutman AP, Xie SW, Liu SJ, Ma MZ, Liu DY (2017) The Mesoarchean Tiejiashan-Gongchangling potassic granite in the Anshan-Benxi area, North China Craton: origin by recycling of Paleo-to Eoarchean crust from U-pb-nd-hf-o isotopic studies. Lithos 290:116–135. https://doi.org/10.1016/j.lithos.2017.08.009
Døssing LN, Frei R, Stendal H, Mapeo RBM (2009) Characterization of enriched lithospheric mantle components in ~ 2.7 Ga Banded Iron formations: an example from the Tati Greenstone Belt, Northeastern Botswana. Precambrian Res 172:334–356. https://doi.org/10.1016/j.precamres.2009.06.004
Elderfield H, Upstill-Goddard R, Sholkovitz ER (1990) The rare earth elements in rivers, estuaries, and coastal seas and their significance to the composition of ocean waters. Geochim Cosmochim Acta 54:971–991. https://doi.org/10.1016/0016-7037(90)90432-K
Ernst DM, Bau M (2021) Banded iron formation from Antarctica: the 2.5 Ga old Mt. Ruker BIF and the antiquity of lanthanide tetrad effect and super-chondritic Y/Ho ratio in seawater. Gondwana Res 91:97–111. https://doi.org/10.1016/j.gr.2020.11.011
Farquhar J, Zerkle AL, Bekker A (2011) Geological constraints on the origin of oxygenic photosynthesis. Photosynth Res 107:11–36. https://doi.org/10.1007/s11120-010-9594-0
Fischer WW, Knoll AH (2009) An iron shuttle for deepwater silica in late Archean and early paleoproterozoic iron formation. Geol Soc Am Bull 121(1–2):222–235. https://doi.org/10.1130/B26328.1
Frei R, Polat A (2007) Source heterogeneity for the major components of ~ 3.7 Ga banded iron formations (Isua Greenstone Belt, Western Greenland): tracing the nature of interacting water masses in BIF formation. Earth Planet Sci Lett 253:266–281. https://doi.org/10.1016/j.epsl.2006.10.033
Froelich PN, Blanc V, Mortlock RA, Chillrud SN, Dunstan W, Udomkit A, Peng TH (1992) River fluxes of dissolved silica to the ocean were higher during glacials: Ge/Si in diatoms, rivers, and oceans. Paleoceanography 7:739–767. https://doi.org/10.1029/92PA02090
Frost CD, von Blanckenburg F, Schoenberg R, Frost BR, Swapp SM (2007) Preservation of Fe isotope heterogeneities during diagenesis and metamorphism of banded iron formation. Contrib Mineral Petr 153(2):211–235. https://doi.org/10.1007/s00410-006-0141-0
Geilert S, Vroon PZ, van Bergen MJ (2016) Effect of diagenetic phase transformation on the silicon isotope composition of opaline sinter deposits of Geysir, Iceland. Chem Geol 433:57–67. https://doi.org/10.1016/j.chemgeo.2016.04.008
German CR, Barreiro BA, Higgs NC, Nelson TA, Ludford EM, Palmer MR (1995) Seawater-metasomatism in hydrothermal sediments (Esca-naba Trough, northeast Pacific). Chem Geol 119:175–190. https://doi.org/10.1016/0009-2541(94)00052-A
German CR, Elderfield H (1990) Application of the ce anomaly as a paleoredox indicator: the ground rules. Paleoceanography 5:823–833. https://doi.org/10.1029/PA005i005p00823
Guo RR, Li ZH, Liu SW, Wang MJ, Bao H, Wang W, Huang X, Dou YX (2022) Late neoarchean geodynamic regime of the northeastern North China Craton: constraints from metamorphosed volcanic rocks of the Anshan-Benxi greenstone belt. Precambrian Res 371:106583. https://doi.org/10.1016/j.precamres.2022.106583
Hamade T, Konhauser KO, Raiswell R, Goldsmith S, Morris RC (2003) Using Ge/Si ratios to decouple iron and silica fluxes in precambrian banded iron formations. Geology 31(1):35–38. https://doi.org/10.1130/0091-7613(2003)031%3C0035:UGSRTD%3E2.0.CO;2
Haugaard R, Frei R, Stendal H, Konhauser K (2013) Petrology and geochemistry of the ~ 2.9 Ga Itilliarsuk banded iron formation and associated supracrustal rocks, West Greenland: source characteristics and depositional environment. Precambrian Res 229:150–176. https://doi.org/10.1016/j.precamres.2012.04.013
Heck PR, Huberty JM, Kita NT, Ushikubo T, Kozdon R, Valley JW (2011) SIMS analyses of silicon and oxygen isotope ratios for quartz from Archean and Paleoproterozoic banded iron formations. Geochim Cosmochim Acta 75(20):5879–5891. https://doi.org/10.1016/j.gca.2011.07.023
Hegler F, Posth NR, Jiang J, Kappler A (2008) Physiology of phototrophic iron(II)-oxidizing bacteria: implications for modern and ancient environments. FEMS Microbiol Ecol 66:250–260. https://doi.org/10.1111/j.1574-6941.2008.00592.x
Heimann A, Johnson CM, Beard BL, Valley JW, Roden EE, Spicuzza MJ, Beukes NJ (2010) Fe, C, and O isotope compositions of banded iron formation carbonates demonstrate a major role for dissimilatory iron reduction in ~ 2.5 Ga Marine environments. Earth Planet Sci Lett 294(1–2):8–18. https://doi.org/10.1016/j.epsl.2010.02.015
Holland HD (1973) The oceans; a possible source of iron in iron-formations. Econ Geol 68(7):1169–1172. https://doi.org/10.2113/gsecongeo.68.7.1169
Holland HH (1984) The Chemical evolution of the atmosphere and the oceans. Princeton University Press
Hou KJ, Li YH, Gao JF, Liu F, Qin Y (2014) Geochemistry and Si-O-Fe isotope constraints on the origin of banded iron formations of the Yuanjiacun Formation, Lvliang Group, Shanxi, China. Ore Geol Rev 57:288–298. https://doi.org/10.1016/j.oregeorev.2013.09.018
Isley AE, Abbott DH (1999) Plume-related mafic volcanism and the deposition of banded iron formation. J Geophys Res-Sol Ea 104(B7):15461–15477. https://doi.org/10.1029/1999JB900066
Jacobsen SB, Pimentel-Klose MR (1988) Nd isotopic variations in precambrian banded iron formations. Geophys Res Lett 15:393–396. https://doi.org/10.1029/GL015i004p00393
James HL (1954) Sedimentary facies of iron-formation. Econ Geol 49:235–293. https://doi.org/10.2113/gsecongeo.49.3.235
Johnson C, Beard B, Weyer S (2020) Iron Geochemistry: an isotopic perspective. Springer, Switzerland. https://doi.org/10.1007/978-3-030-33828-2
Johnson CM, Beard BL, Klein C, Beukes NJ, Roden EE (2008) Iron isotopes constrain biologic and abiologic processes in banded iron formation genesis. Geochim Cosmochim Acta 72(1):151–169. https://doi.org/10.1016/j.gca.2007.10.013
Kamber BS, Webb GE, Gallagher M (2014) The rare earth element signal in archaean microbial carbonate: information on ocean redox and biogenicity. J Geol Soc 171(6):745–763. https://doi.org/10.1144/jgs2013-110
Kappler A, Pasquero C, Konhauser KO, Newman DK (2005) Deposition of banded iron formations by anoxygenic phototrophic fe (II)-oxidizing bacteria. Geology 33:865–868. https://doi.org/10.1130/G21658.1
Klinkhammer GP, Elderfield H, Edmond JM, Mitra A (1994) Geochemical implications of rare-earth element patterns in hydrothermal fluids from mid-ocean ridges. Geochim Cosmochim Acta 58:5105–5113. https://doi.org/10.1016/0016-7037(94)90297-6
Knauth LP (1994) Petrogenesis of chert. Rev Mineral Geochem 29:233–258
Konhauser KO, Amskold L, Lalonde SV, Posth NR, Kappler A, Anbar A (2007) Decoupling photochemical Fe (II) oxidation from shallow-water BIF deposition. Earth Planet Sci Lett 258(1–2):87–100. https://doi.org/10.1016/j.epsl.2007.03.026
Konhauser KO, Hamade T, Raiswell R, Morris RC, Ferris FG, Southam G, Canfield DE (2002) Could bacteria have formed the precambrian banded iron formations? Geology 30:1079–1082. https://doi.org/10.1130/0091-7613(2002)030%3C1079:CBHFTP%3E2.0.CO;2
Konhauser K, Planavsky N, Hardisty D, Robbins L, Warchola T, Haugaard R, Lalonde S, Partin C, Oonk P, Tsikos H (2017) Iron formations: a global record of Neoarchaean to Palaeoproterozoic environmental history. Earth-Sci Rev 172:140–177. https://doi.org/10.1016/j.earscirev.2017.06.012
Lawrence MG, Kamber BS (2006) The behaviour of the rare earth elements during estuarine mixing—revisited. Mar Chem 100(1–2):147–161. https://doi.org/10.1016/j.marchem.2005.11.007
Lepp H, Goldich SS (1964) Origin of precambrian iron formations. Econ Geol 59(6):1025–1060. https://doi.org/10.2113/gsecongeo.59.6.1025
Li LX, Li HM, Liu MJ, Yang XQ, Meng J (2016) Timing of deposition and tectonothermal events of banded iron formations in the Anshan-Benxi area, Liaoning Province, China: evidence from SHRIMP U-Pb zircon geochronology of the wall rocks. J Asian Earth Sci 129:276–293. https://doi.org/10.1016/j.jseaes.2016.08.022
Liu DY, Nutman AP, Compston W, Wu JS, Shen QH (1992) Remnants of ≥ 3800 ma crust in the Chinese part of the sino-korean craton. Geology 20:339–342. https://doi.org/10.1130/0091-7613(1992)020%3C0339:ROMCIT%3E2.3.CO;2
Liu DY, Wilde SA, Wan YS, Wu JS, Zhou HY, Dong CY, Yin XY (2008) New U-Pb and Hf isotopic data confirm Anshan as the oldest preserved segment of the North China Craton. Am J Sci 308(3):200–231. https://doi.org/10.2475/03.2008.02
Liu XM, Gaschnig RM, Rudnick RL, Hazen RM, Shahar A (2022) Constant iron isotope composition of the upper continental crust over the past 3 Gyr. Geochem Perspect Lett 22:16–19. https://doi.org/10.7185/geochemlet.2221
Li WQ, Beard BL, Johnson CM (2015) Biologically recycled continental iron is a major component in banded iron formations. Proc Nat Acad Sci USA 112(27):8193–8198. https://doi.org/10.1073/pnas.1505515112
Li YH, Hou KJ, Wan DF, Zhang ZJ, Yue GL (2014) Precambrian banded iron formations in the North China Craton: Silicon and oxygen isotopes and genetic implications. Ore Geol Rev 57:299–307. https://doi.org/10.1016/j.oregeorev.2013.09.011
Luo Y, Sun M, Zhao G, Li S, Ayers JC, Xia X, Zhang J (2008) A comparison of U–Pb and Hf isotopic compositions of detrital zircons from the North and South Liaohe Groups: constraints on the evolution of the Jiao-Liao-Ji Belt, North China Craton. Precambrian Res 163(3–4):279–306. https://doi.org/10.1016/j.precamres.2008.01.002
Lyons TW, Diamond CW, Konhauser KO (2020) Shedding light on manganese cycling in the early oceans. Proc Nat Acad Sci USA 117(42):25960–25962. https://doi.org/10.1073/pnas.2016447117
Marin-Carbonne J, Chaussidon M, Robert F (2012) Micrometer-scale chemical and isotopic criteria (O and Si) on the origin and history of Precambrian cherts: implications for paleo-temperature reconstructions. Geochim Cosmochim Acta 92:129–147. https://doi.org/10.1016/j.precamres.2012.09.016
Marin-Carbonne J, Robert F, Chaussidon M (2014) The silicon and oxygen isotope compositions of precambrian cherts: a record of oceanic paleo-temperatures? Precambrian Res 247:223–234. https://doi.org/10.1016/j.precamres.2014.03.016
Marin J, Chaussidon M, Robert F (2010) Microscale oxygen isotope variationsin 1.9 Ga Gunflint cherts: assessments of diagenesis effects and implicationsfor oceanic paleo-temperature reconstructions. Geochim Cosmochim Acta 74:116–130. https://doi.org/10.1016/j.gca.2009.09.016
McLennan SM (1989) Rare earth elements in sedimentary rocks: influence of provenance and sedimentary processes. Rev Mineral Geochem 21:169–200
Men YK, Mi ZJ, Wang ED, Han LD, Wang YJ, Jia SS, Xia JM, Song K (2023) Geology and geochemistry of the Jianshan Banded Iron Formation in Shanxi Province, China: constraints on the genesis. J Geol 130:429–518. https://doi.org/10.1086/724438
Men YK, Wang ED, Fu JF, Jia SS, You XW, He QW (2019) Geology and geochemistry of the Yuanjiacun banded iron formation in Shanxi Province, China: constraints on the genesis of the Yuanjiacun BIF. Geol Mag 156(11):1839–1862. https://doi.org/10.1017/S0016756819000219
Millero FJ, Sotolongo S, Izaguirre M (1987) The oxidation kinetics of Fe(II) in seawater. Geochim Cosmochim Acta 51:793–801. https://doi.org/10.1016/0016-7037(87)90093-7
Miller RG, O’Nions RK (1985) Sources of precambrian chemical and clastic sediments. Nature 314:325–330. https://doi.org/10.1038/314325a0
Mortlock RA, Froelich PN, Feely RA, Massoth GJ, Butterfield DA, Lupton JE (1993) Silica and germanium in Pacific Ocean hydrothermal vents and plumes. Earth Planet Sci Lett 119:365–378. https://doi.org/10.1016/0012-821X(93)90144-X
Narduzzi F, Bosch D, Philippot P (2021) Evolution of seawater continentally-sourced nd isotopic composition prior to and during the great oxidation event. Precambrian Res 362:106292. https://doi.org/10.1016/j.precamres.2021.106292
Peng P, Wang XP, Windley BF, Guo JH, Zhai MG, Li Y (2014) Spatial distribution of ~ 1950 – 1800 Ma metamorphic events in the North China Craton: implications for tectonic subdivision of the craton. Lithos 202–203:250–266. https://doi.org/10.1016/j.lithos.2014.05.033
Peng ZD, Wang CL, Tong XX, Zhang LC, Zhang BL (2018) Element geochemistry and neodymium isotope systematics of the Neoarchean banded iron formations in the Qingyuan greenstone belt, North China Craton. Ore Geol Rev 102:562–584. https://doi.org/10.1016/j.oregeorev.2018.09.008
Piepgras DJ, Wasserburg GJ (1985) Strontium and neodymium isotopes in Hot Springs on the East Pacific Rise and Guaymas Basin. Earth Planet Sci Lett 72:341–356. https://doi.org/10.1016/0012-821X(85)90057-3
Planavsky N, Bekker A, Rouxel OJ, Kamber B, Hofmann A, Knudsen A, Lyons TW (2010) Rare earth element and yttrium compositions of Archean and Paleoproterozoic Fe formations revisited: new perspectives on the significance and mechanisms of deposition. Geochim Cosmochim Acta 74:6387–6405. https://doi.org/10.1016/j.gca.2010.07.021
Planavsky N, Rouxel OJ, Bekker A, Hofmann A, Little CT, Lyons TW (2012) Iron isotope composition of some Archean and Proterozoic iron formations. Geochim Cosmochim Acta 80:158–169. https://doi.org/10.1016/j.gca.2011.12.001
Reddy TR, Zheng XY, Roden EE, Beard BL, Johnson CM (2016) Silicon isotope fractionation during microbial reduction of Fe(III)–Si gels under Archean seawater conditions and implications for iron formation genesis. Geochim Cosmochim Acta 190:85–99. https://doi.org/10.1016/j.gca.2016.06.035
Rego ES, Busigny V, Lalonde SV, Philippot P, Bouyon A, Rossignol C, Babinski M, de Cássia Zapparoli A (2021) Anoxygenic photosynthesis linked to Neoarchean iron formations in Carajás (Brazil). Geobiology 19(4):326–341. https://doi.org/10.1111/gbi.12438
Robbins LJ, Lalonde SV, Planavsky NJ, Partin CA, Reinhard CT, Kendall B, Scott C, Hardisty DS, Gill BC, Alessi DS, Dupont CL, Saito MA, Crowe SA, Poulton SW, Bekker A, Lyons TW, Konhauser KO (2016) Trace elements at the intersection of marine biological and geochemical evolution. Earth-Sci Rev 163:323–348. https://doi.org/10.1016/j.earscirev.2016.10.013
Rodushkin I, Pallavicini N, Engström E, Sörlin D, Öhlander B, Ingri J, Baxter DC (2016) Assessment of the natural variability of B, cd, Cu, Fe, Pb, Sr, Tl and Zn concentrations and isotopic compositions in leaves, needles and mushrooms using single sample digestion and two-column matrix separation. J Anal Atom Spectrom 31(1):220–233. https://doi.org/10.1039/C5JA00274E
Rousseau TCC, Sonke JE, Chmeleff J, van Beek P, Souhaut M, Boaventura G, Seyler P, Jeandel C (2015) Rapid neodymium release to marine waters from lithogenic sediments in the Amazon estuary. Nat Comm 6:7592. https://doi.org/10.1038/ncomms8592
Rouxel OJ, Bekker A, Edwards KJ (2005) Iron isotope constraints on the Archean and Paleoproterozoic ocean redox state. Science 307:1088–1091. https://doi.org/10.1126/science.1105692
Rudnick RL, Gao S (2014) Composition of the continental crust. In: Rudnick RL (ed) Sediments, Diagenesis and Sedimentary Rocks. Elsevier, Amsterdam, Treatise on Geochemistry (2nd Ed), 4, pp 1–51. https://doi.org/10.1016/B978-0-08-095975-7.00301-6
Schier K, Bau M, Smith AJB, Beukes NJ, Coetzee LL, Viehmann S (2020) Chemical evolution of seawater in the Transvaal Ocean between 2426 Ma (Ongeluk large Igneous Province) and 2413 ma ago (Kalahari Manganese Field). Gondwana Res 88:373–388. https://doi.org/10.1016/j.gr.2020.09.001
Severmann S, Johnson CM, Beard BL, German CR, Edmonds HN, Chiba H, Green DRH (2004) The effect of plume processes on the Fe isotope composition of hydrothermally derived Fe in the deep ocean as inferred from the Rainbow vent site, Mid-atlantic Ridge, 36°14′ N. Earth Planet Sci Lett 225(1–2):63–76. https://doi.org/10.1016/j.epsl.2004.06.001
Shimizu H, Umemoto N, Masuda A, Appel PWU (1990) Sources of iron-formations in the Archean Isua and Malene supracrustals, West Greenland: evidence from La–Ce and Sm–Nd isotopic data and REE. Geochim Cosmochim Acta 54:1147–1154. https://doi.org/10.1016/0016-7037(90)90445-Q
Sholkovitz ER, Landing WM, Lewis BL (1994) Ocean particle chemistry: the fractionation of rare earth elements between suspended particles and seawater. Geochim Cosmochim Acta 58:1567–1579. https://doi.org/10.1016/0016-7037(94)90559-2
Siever R (1992) The silica cycle in the Precambrian. Geochim Cosmochim Acta 56(8):3265–3272. https://doi.org/10.1016/0016-7037(92)90303-Z
Steinhoefel G, Horn I, von Blanckenburg F (2009) Micro-scale tracing of Fe and Si isotope signatures in banded iron formation using femtosecond laser ablation. Geochim Cosmochim Acta 73(18):5343–5360. https://doi.org/10.1016/j.gca.2009.05.037
Steinhoefel G, von Blanckenburg F, Horn I, Konhauser KO, Beukes NJ, Gutzmer J (2010) Deciphering formation processes of banded iron formations from the Transvaal and the Hamersley successions by combined Si and Fe isotope analysis using UV femtosecond laser ablation. Geochim Cosmochim Acta 74(9):2677–2696. https://doi.org/10.1016/j.gca.2010.01.028
Tebo BM, Johnson HA, McCarthy JK, Templeton AS (2005) Geomicrobiology of manganese (II) oxidation. Trends Microbiol 13:421–428. https://doi.org/10.1016/j.tim.2005.07.009
Tricca A, Stille P, Steinmann M, Kiefel B, Samuel J (1999) Rare earth elements and Sr and Nd isotopic compositions of dissolved and suspended loads from small river systems in the Vosges Mountains (France), the river Rhine and groundwater. Chem Geol 160:139–158. https://doi.org/10.1016/S0009-2541(99)00065-0
van den Boorn SHJM, van Bergen MJ, Vroon PZ, De Vries ST, Nijman W (2010) Silicon isotope and trace element constraints on the origin of ~ 3.5 Ga cherts: implications for early archaean marine environments. Geochim Cosmochim Acta 74(3):1077–1103. https://doi.org/10.1016/j.gca.2009.09.009
van den Boorn SH, van Bergen MJ, Nijman W, Vroon PZ (2007) Dual role of seawater and hydrothermal fluids in early Archean chert formation: evidence from silicon isotopes. Geology 35(10):939–942. https://doi.org/10.1130/G24096A.1
Viehmann S, Bau M, Hoffmann JE, Münker C (2015a) Geochemistry of the Krivoy Rog Banded Iron Formation, Ukraine, and the impact of peak episodes of increased global magmatic activity on the trace element composition of precambrian seawater. Precambrian Res 270:165–180. https://doi.org/10.1016/j.precamres.2015.09.015
Viehmann S, Bau M, Smith AJ, Beukes NJ, Dantas EL, Bühn B (2015b) The reliability of ~ 2.9 Ga old Witwatersrand banded iron formations (South Africa) as archives for Mesoarchean seawater: evidence from REE and nd isotope systematics. J Afr Earth Sci 111:322–334. https://doi.org/10.1016/j.jafrearsci.2015.08.013
Wang CL, Huang H, Tong XX, Zheng MT, Peng ZD, Nan JB, Zhang LC, Zhai MG (2016b) Changing provenance of late Neoarchean metasedimentary rocks in the Anshan-Benxi area, North China Craton: implications for the tectonic setting of the world-class Dataigou banded iron formation. Gondwana Res 40:107–123. https://doi.org/10.1016/j.gr.2016.08.010
Wang CL, Konhauser KO, Zhang LC (2015) Depositional environment of the Paleoproterozoic Yuanjiacun Banded Iron Formation in Shanxi Province, China. Econ Geol 110:1515–1539. https://doi.org/10.2113/econgeo.110.6.1515
Wang CL, Konhauser KO, Zhang LC, Zhai MG, Li WJ (2016a) Decoupled sources of the 2.3–2.2 Ga Yuanjiacun banded iron formation: implications for the nd cycle in Earth’s early oceans. Precambrian Res 280:1–13. https://doi.org/10.1016/j.precamres.2016.04.016
Wang CL, Peng ZD, Tong XX, Huang H, Zheng MT, Zhang LC, Zhai MG (2017a) Late neoarchean supracrustal rocks from the Anshan-Benxi terrane, North China Craton: New geodynamic implications from the geochemical record. Am J Sci 317(10):1095–1148. https://doi.org/10.2475/10.2017.02
Wang CL, Robbins LJ, Planavsky NJ, Beukes NJ, Patry LA, Lalonde SV, Lechte MA, Asael D, Reinhard CT, Zhang LC, Konhauser KO (2023) Archean to early paleoproterozoic iron formations document a transition in iron oxidation mechanisms. Geochim Cosmochim Acta 343:286–303. https://doi.org/10.1016/j.gca.2022.12.002
Wang CL, Wu HY, Li WJ, Peng ZD, Zhang LC, Zhai MG (2017b) Changes of Ge/Si, REE + Y and Sm-Nd isotopes in alternating Fe- and Si-rich mesobands reveal source heterogeneity of the ~ 2.54 Ga Sijiaying banded iron formation in Eastern Hebei, China. Ore Geol Rev 80:363–376. https://doi.org/10.1016/j.oregeorev.2016.06.036
Wang CL, Zhang LC, Dai YP, Li WJ (2014) Source characteristics of the ~ 2.5 Ga Wangjiazhuang banded iron formation from the Wutai greenstone belt in the North China Craton: evidence from neodymium isotopes. J Asian Earth Sci 93:288–300. https://doi.org/10.1016/j.jseaes.2014.07.038
Wang SL, Zhang RH (1995) U-Pb isotope age of individual zircon from biotite leptynite in the Qidashan iron deposit and its significance. Mineral Deposits 3:216–219
Wan YS, Dong CY, Liu DY, Kröner A, Yang CH, Wang W, Du LL, Xie HQ, Ma MZ (2012) Zircon ages and geochemistry of late Neoarchean syenogranites in the North China Craton: a review. Precambrian Res 222:265–289. https://doi.org/10.1016/j.precamres.2011.05.001
Wan YS, Ma MZ, Dong CY, Xie HQ, Xie SW, Ren P, Liu DY (2015) Widespread late Neoarchean reworking of Meso- to Paleoarchean continental crust in the Anshan-Benxi area, North China Craton, as documented by u-pb-nd-hf-o isotopes. Am J Sci 315:620–670. https://doi.org/10.2475/07.2015.02
Wu LL, Beard BL, Roden EE, Johnson CM (2011) Stable iron isotope fractionation between aqueous Fe(II) and hydrous ferric oxide. Environ Sci Technol 45:1847–1852. https://doi.org/10.1021/es103171x
Wu LL, Percak-Dennett EM, Beard BL, Roden EE, Johnson CM (2012) Stable iron isotope fractionation between aqueous Fe(II) and model Archean ocean Fe–Si coprecipitates and implications for iron isotope variations in the ancient rock record. Geochim Cosmochim Acta 84:14–28. https://doi.org/10.1016/j.gca.2012.01.007
Zhai MG, Santosh M (2011) The early precambrian odyssey of the North China Craton: a synoptic overview. Gondwana Res 20:6–25. https://doi.org/10.1016/j.gr.2011.02.005
Zhai MG, Windley BF, Sills JD (1990) Archaean gneisses, amphibolites and banded iron-formations from the Anshan area of Liaoning Province, NE China: their geochemistry, metamorphism and petrogenesis. Precambrian Res 46(3):195–216. https://doi.org/10.1016/0301-9268(90)90002-8
Zhang LC, Zhai MG, Wan YS, Guo JH, Dai YP, Wang CL, Liu L (2012) Study of the precambrian BIF-iron deposits in the North China Craton: progresses and questions. Acta Petrol Sin 28:3431–3445
Zhao GC, Cawood PA, Wilde SA, Sun M, Zhang J, He YH, Yin CQ (2012) Amalgamation of the North China Craton: key issues and discussion. Precambrian Res 222–223:55–76. https://doi.org/10.1016/j.precamres.2012.09.016
Zheng XY, Beard BL, Reddy TR, Roden EE, Johnson CM (2016) Abiologic silicon isotope fractionation between aqueous Si and Fe(III)-Si gel in simulated Archean seawater: implications for Si isotope records in Precambrian sedimentary rocks. Geochim Cosmochim Acta 187: 102–122. https://doi.org/10.1016/j.gca.2016.05.012
Zhou ST (1994) Geology of the BIF in Anshan-Benxi area. Geological Publishing House, Beijing
Acknowledgements
We thank editor Bernd Lehmann, Alexandre Cabral, and two anonymous reviewers for their constructive comments.
Funding
We acknowledge the financial support provided by the National Natural Science Foundation of China (grant 42150104 and 42302073), Key Research Program of Frontier Sciences, Chinese Academy of Sciences (grant ZDBS-LY-DQC037), the Key Research Program of the Institute of Geology and Geophysics, Chinese Academy of Sciences (grant IGGCAS-201905), and Youth Innovation Promotion Association, Chinese Academy of Sciences.
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C.L.W. conceived the study. C.L.W. collected samples for this study. C.L.W. processed the samples. C.L.W., Z.D.P., X.X.T., and L.G. conducted geochemical analyses. All authors contributed to writing and editing the manuscript.
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126_2024_1245_MOESM1_ESM.xlsx
Supplementary Material 1: Table S1. Electron proble microanalyses (wt %) of hematite, magnetite, amphibole, carboante minerals, and calcite within the Qidashan BIF samples
126_2024_1245_MOESM2_ESM.xlsx
Supplementary Material 2: Table S2. Major (wt %) and trace element (ppm) compositions of the Qidashan BIF samples and relevant standards
126_2024_1245_MOESM3_ESM.xlsx
Supplementary Material 3: Table S3. Sm-Nd, Fe, and Si isotopic data of the Qidashan and Dataigou BIF samples along with geostandard samples
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Wang, C., Peng, Z., Tong, X. et al. Geochemistry and Sm─Nd─Fe─Si isotope compositions as insights into the deposition of the late Neoarchean Qidashan banded iron formation, North China Craton. Miner Deposita (2024). https://doi.org/10.1007/s00126-024-01245-8
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DOI: https://doi.org/10.1007/s00126-024-01245-8