The DOI matches its Crossref record; 350 of the 354 references it cites were found in a registry or an index.
Iron Formation: The Sedimentary Product of a Complex Interplay among Mantle, Tectonic, Oceanic, and Biospheric Processes
Abstract
Iron formations are economically important sedimentary rocks that are most common in Precambrian sedi-mentary successions. Although many aspects of their origin remain unresolved, it is widely accepted that sec-ular changes in the style of their deposition are linked to environmental and geochemical evolution of Earth. Two types of Precambrian iron formations have been recognized with respect to their depositional setting. Al-goma-type iron formations are interlayered with or stratigraphically linked to submarine-emplaced volcanic rocks in greenstone belts and, in some cases, with volcanogenic massive sulfide (VMS) deposits. In contrast, larger Superior-type iron formations are developed in passive-margin sedimentary rock successions and gener-ally lack direct relationships with volcanic rocks. The early distinction made between these two iron-formation types, although mimimized by later studies, remains a valid first approximation. Texturally, iron formations were also divided into two groups. Banded iron formation (BIF) is dominant in Archean to earliest Paleopro-terozoic successions, whereas granular iron formation (GIF) is much more common in Paleoproterozoic suc-cessions. Secular changes in the style of iron-formation deposition, identified more than 20 years ago, have
Overview
Integrity signals
Registry
Cites
Statistics
Verification
Claims the paper makes
Claims other papers make about this one
Each is checked against this paper’s own text: does it say what the citing paper says it does?
In the citing paper
“Superior-type IFs can be very laterally extensive, with original aerial extents estimated in some cases to be over 100,000 km 2 (Isley, 1995; Bekker et al., 2010).”
From Iron formations: A global record of Neoarchaean to Palaeoproterozoic environmental history (2017) · cites this paper as Bekker et al., 2010
In the citing paper
“The sulfide-facies IF described by James (1954) are now believed to be pyritic carbonaceous shales and ferruginous slates, and therefore do not represent a chemical precipitate (Bekker et al., 2010).”
From Iron formations: A global record of Neoarchaean to Palaeoproterozoic environmental history (2017) · cites this paper as Bekker et al., 2010
In the citing paper
“(ii) most IF precursor sediments were deposited in offshore environments with limited siliciclastic input and low sedimentation rates”
From Iron formations: A global record of Neoarchaean to Palaeoproterozoic environmental history (2017) · cites this paper as Bekker et al., 2010
In the citing paper
“there is nearly unanimous agreement that (i) the size of the DIC reservoir was significantly larger in the Archaean than in the modern ocean”
From Iron formations: A global record of Neoarchaean to Palaeoproterozoic environmental history (2017) · cites this paper as Bekker et al., 2010
In the citing paper
“although IF sedimentation was likely highly pulsed and variable (Bekker et al., 2010; Haugaard et al., 2016a), slow net accumulation rates were probably linked to a low siliciclastic flux that allowed for accumulation of pure chemical sediments”
From Iron formations: A global record of Neoarchaean to Palaeoproterozoic environmental history (2017) · cites this paper as Bekker et al., 2010
In the citing paper
“(iii) proportionally more Fe(III) existed than organic carbon buried with IF precursor sediments relative to typical modern continental margin sediments”
From Iron formations: A global record of Neoarchaean to Palaeoproterozoic environmental history (2017) · cites this paper as Bekker et al., 2010
In the citing paper
“This observation is unlikely to reflect preservational bias because slightly younger 1.84, 1.79, and 1.78 Ga Cu-rich VMS deposits that similarly formed in arc settings contain abundant hematite and magnetite exhalites, jasper, and IF”
From Iron formations: A global record of Neoarchaean to Palaeoproterozoic environmental history (2017) · cites this paper as Bekker et al., 2010
In the citing paper
“Large sedimentary iron deposits that formed during this time gap (1.85-0.75 Ga) are indeed absent, but several small IFs and Fe-rich lithologies in sedimentary rock-dominated successions are known”
From Iron formations: A global record of Neoarchaean to Palaeoproterozoic environmental history (2017) · cites this paper as Bekker et al., 2010
In the citing paper
“Most deposits before 2.4 Ga comprise BIF; those ca. 2.3-0.8 Ga are predominantly GIF; Neoproterozoic Rapitan-type iron formation (~0.715 Ga) are associated with glacial deposits.”
From Iron formations: A global record of Neoarchaean to Palaeoproterozoic environmental history (2017) · cites this paper as Bekker et al., 2010
In the citing paper
“Most deposits before 2.4 Ga comprise BIF; those ca. 2.3-0.8 Ga are predominantly GIF; Neoproterozoic Rapitan-type iron formation (~0.715 Ga) are associated with glacial deposits.”
From Iron formations: A global record of Neoarchaean to Palaeoproterozoic environmental history (2017) · cites this paper as Bekker et al., 2010
In the citing paper
“Most deposits before 2.4 Ga comprise BIF; those ca. 2.3-0.8 Ga are predominantly GIF; Neoproterozoic Rapitan-type iron formation (~0.715 Ga) are associated with glacial deposits.”
From Iron formations: A global record of Neoarchaean to Palaeoproterozoic environmental history (2017) · cites this paper as Bekker et al., 2010
In the citing paper
“Deposition of IF appears tied to periods of enhanced magmatic and hydrothermal activity (associated with large igneous province emplacement; Isley and Abbot, 1999) that delivered large amounts of ferrous iron to anoxic deep oceans (Bekker et al., 2010;2014).”
From Trace elements at the intersection of marine biological and geochemical evolution (2016) · cites this paper as Bekker et al., 2010
In the citing paper
“BIF dominate the Archean and are more important in terms of total IF tonnage (Bekker et al., 2010).”
From Trace elements at the intersection of marine biological and geochemical evolution (2016) · cites this paper as Bekker et al., 2010
In the citing paper
“Dissolved Fe concentrations in the Archean and Paleoproterozoic oceans would have had to have been high in order to permit the formation of extensive IF via Fe(II) oxidation by anoxygenic and oxygenic photosynthesis (Bekker et al., 2010).”
From Trace elements at the intersection of marine biological and geochemical evolution (2016) · cites this paper as Bekker et al., 2010
Citations
Cites
Philosophical transactions of the Royal Society of London. B
Press, H. (1886) · Cited by 10,087
Geochimica et Cosmochimica Acta
Blair, N. E. (1992) · Geochimica et Cosmochimica Acta · doi:10.1016/0016-7037(92)90334-f · Cited by 4,586
The interaction of TIGIT with PVR and PVRL2 inhibits human NK cell cytotoxicity
Stanietsky, N., Simic, H., Arapovic, J., Toporik, A., Levy, O., Novik, A., Levine, Z., Beiman, M., Dassa, L., Achdout, H., et al. (2009) · Proceedings of the National Academy of Sciences · doi:10.1073/pnas.0903474106 · Cited by 3,524
Geological Society of America Abstracts with Programs
Vleeschouwer, D. D., Silva, A. D., Boulvain, F., & Claeys, P. (2010) · Cited by 3,007
(2024) · Elsevier eBooks · doi:10.1016/c2020-1-04096-5 · Cited by 2,772
A Neoproterozoic Snowball Earth
Hoffman, P. F., Kaufman, A. J., Halverson, G. P., & Schrag, D. P. (1998) · Science · doi:10.1126/science.281.5381.1342 · Cited by 2,693
Proceedings of the Ocean Drilling Program, 127/128 Scientific Results
(1992) · doi:10.2973/odp.proc.sr.127128.1992 · Cited by 2,506
The Chemical Evolution of the Atmosphere and Oceans
Holland, H. D. (1984) · doi:10.1515/9780691220239 · Cited by 1,836
Atmospheric Influence of Earth's Earliest Sulfur Cycle
Farquhar, J., Bao, H., & Thiemens, M. (2000) · Science · doi:10.1126/science.289.5480.756 · Cited by 1,805
Bau, M., & Dulski, P. (1996) · Precambrian Research · doi:10.1016/0301-9268(95)00087-9 · Cited by 1,687
Flagged first, then by citations
4 of the 354 references couldn’t be matched to a known paper.
Cited by
Sorted by citations
Items 701–800 of 999
Slabunov, A. I., Нестерова, Н. С., & Максимов, О. А. (2024) · Geochemistry International · doi:10.1134/s0016702924030054 · Cited by 6
Meng, F. W., Han, Z., Hu, X., Jenkyns, H. C., Zhang, B., Chen, X., & Hou, M. (2024) · Sedimentology · doi:10.1111/sed.13218 · Cited by 4
Hydrothermal oxidation in the Biwabik Iron Formation, MN, USA
Losh, S., & Rague, R. (2018) · Mineralium Deposita · doi:10.1007/s00126-017-0783-z · Cited by 5
Pirajno, F., & Huston, D. L. (2018) · Elsevier eBooks · doi:10.1016/b978-0-444-63901-1.00009-5 · Cited by 4
Zhang, Y., Yu, X., Peng, Q.-M., Li, D., Xiaowei, L. I., Kun, S. H. E. N., Zhang, S., & Wei, S. H. A. N. (2020) · Acta Geologica Sinica - English Edition · doi:10.1111/1755-6724.14505 · Cited by 4
Hu, J., Wang, M., Wang, H., Li, S., Santosh, M., Zhao, Y., Li, D., Yan, Q.-H., Dong, R., & Ren, H. (2022) · Ore Geology Reviews · doi:10.1016/j.oregeorev.2022.105165 · Cited by 4
The Geochemistry of Sulfidic Sedimentary Rocks
Rickard, D. T. (2012) · Developments in sedimentology · doi:10.1016/b978-0-444-52989-3.00015-5 · Cited by 4
Li, H., Liang, J. S., Yang, F., Zhai, M., Zhang, L., Voudouris, P. C., Yang, Z., Zhou, Y., He, J., & Spry, P. G. (2019) · Precambrian Research · doi:10.1016/j.precamres.2019.03.011 · Cited by 4
Efficient variography with partition variograms
Hoffimann, J., & Zadrozny, B. (2019) · Computers & Geosciences · doi:10.1016/j.cageo.2019.06.013 · Cited by 4
The Geobiology of Sediment-Hosted Mineral Deposits
Scott, C., Kelley, K. D., & Slack, J. F. (2014) · doi:10.5382/sp.18.02 · Cited by 4
Self-citationMicrobial primary production and phototrophy
Kirchman, D. L. (2011) · Oxford University Press eBooks · doi:10.1093/acprof:oso/9780199586936.003.0004 · Cited by 6
do Vale, J. A. R. (2019) · Digital Library of Theses and Dissertations (Universidade de São Paulo) · doi:10.11606/d.44.2019.tde-30052019-103844 · Cited by 4
Hou, J., Wang, Y., Zhu, P., Yang, N., Liang, L., Yu, T., Niu, M., Konhauser, K. O., & Wang, F. (2022) · bioRxiv (Cold Spring Harbor Laboratory) · doi:10.1101/2022.11.19.517056 · Cited by 4
Self-citationDonkeng, R. S., Fuh, C. G., Makougni, L. L. N., & Nkoumbou, C. (2025) · Journal of African Earth Sciences · doi:10.1016/j.jafrearsci.2025.105700 · Cited by 3
Liu, L., Li, X., Liu, J., Chu, H., Wang, H., & Chu, F. (2025) · Earth-Science Reviews · doi:10.1016/j.earscirev.2025.105205 · Cited by 3
Jiang, W., Wu, X. G., Yang, H., Fu, J., Zeng, Q., Li, S., Luo, R., Yang, Y., Lin, X., & Zhu, J. (2025) · Minerals · doi:10.3390/min15111123 · Cited by 3
Dornellas, L. M. S. M., da Silva, P. G., Auler, A. S., Culver, D. C., & Pipan, T. (2025) · Journal of Biogeography · doi:10.1111/jbi.70082 · Cited by 3
Triple iron isotopes inform iron mineralization and sedimentation at the TAG hydrothermal mound
Heard, A. W., Tivey, M. K., German, C. R., Blusztajn, J., & Nielsen, S. G. (2025) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2025.09.019 · Cited by 3
Smith, A. J. B., Fitton, D., Vorster, C., & Schoenberg, R. (2025) · Ore Geology Reviews · doi:10.1016/j.oregeorev.2025.107060 · Cited by 3
Nwaila, G. T., Durrheim, R., Frimmel, H. E., & Carranza, E. J. M. (2025) · Natural Resources Research · doi:10.1007/s11053-025-10615-6 · Cited by 3
Magnetotelluric constraints on natural hydrogen potential in the southern Gawler Craton, Australia
Margiono, R., Daruso, R., Gubina, A., Heinson, G., Constable, S., Kay, B., & Boren, G. (2026) · Australian Journal of Earth Sciences · doi:10.1080/08120099.2025.2608806 · Cited by 3
Inorganic silicification of ancient carbonate rocks
Banerjee, A., Patranabis‐Deb, S., Saha, D. K., & Santosh, M. (2021) · Journal of Sedimentary Research · doi:10.2110/jsr.2020.099 · Cited by 3
Lei, R., Wu, C., Zhang, K., Yang, X.-F., & Ye, H. (2022) · Ore Geology Reviews · doi:10.1016/j.oregeorev.2022.104946 · Cited by 3
Williams, G. E. (2022) · Australian Journal of Earth Sciences · doi:10.1080/08120099.2023.2150682 · Cited by 3
Chemical Signatures of Ge in Magnetite of Wugang BIF, China
Moon, I., Liu, L., Yang, X., Suh, Y. J., Jung, J., & Ha, Y. (2023) · Applied Sciences · doi:10.3390/app13148246 · Cited by 3
Hernández‐Montenegro, J. D., Bucholz, C. E., Sosa, E. S., Kipp, M. A., & Tissot, F. L. H. (2024) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2024.07.016 · Cited by 3
Cai, Y., Zhang, S., Pei, J., Tong, Y., Zhou, Z., & Hou, L. (2024) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2024.119013 · Cited by 3
Venugopal, A., Tripathy, G. R., Goswami, V., Khan, T., & Ackerman, L. (2025) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2025.09.013 · Cited by 3
Usenko, O. (2017) · Geofizicheskiy Zhurnal · doi:10.24028/gzh.0203-3100.v39i6.2017.116366 · Cited by 4
Eoarchean Life From the Isua Supracrustal Belt (Greenland)
Nutman, A. P., Bennett, V. C., & Friend, C. R. L. (2018) · Elsevier eBooks · doi:10.1016/b978-0-444-63901-1.00039-3 · Cited by 3
de Souza, F. R., Júnior, H. A. N., & de Abreu, A. T. (2019) · Journal of South American Earth Sciences · doi:10.1016/j.jsames.2019.102313 · Cited by 3
Cathodoluminescence of iron oxides and oxyhydroxides
Galili, N., Kaplan‐Ashiri, I., & Halevy, I. (2023) · American Mineralogist · doi:10.2138/am-2022-8843 · Cited by 5
Hu, J., Jin, W., Tian, Y., Deng, X., Li, S., Kong, L., Santosh, M., Liu, Y., Wang, J., Xu, D., et al. (2023) · Precambrian Research · doi:10.1016/j.precamres.2023.107043 · Cited by 3
Vysotskiy, S. V., Ханчук, А. И., Velivetskaya, T. A., Ignatiev, A. V., Асеева, А. В., & Нестерова, Н. С. (2023) · Doklady Earth Sciences · doi:10.1134/s1028334x23600299 · Cited by 4
Peng, Z., Wang, C., Zhang, L., & Zhai, M. (2023) · Precambrian Research · doi:10.1016/j.precamres.2023.107170 · Cited by 3
Datta, S., Sain, A., Goswami, S., et al. (2024) · The Depositional Record · doi:10.1002/dep2.285 · Cited by 3
Artemenko, H., Shumlyanskyy, L. V., Chew, D., et al. (2024) · Geosciences · doi:10.3390/geosciences14100254 · Cited by 3
Section 2. Classification of Natural Resources
Sverdrup, H. U., & Ragnarsdottir, K. V. (2014) · Geochemical Perspectives · Cited by 3
Бортников, Н. С., Novikov, V. M., Боева, Н. М., Zhukhlistov, A. P., Жегалло, Е. А., & Соболева, С. В. (2017) · Doklady Earth Sciences · doi:10.1134/s1028334x17110101 · Cited by 3
Genesis, Uses and Environment Implications of Iron Oxides and Ores
Egirani, D. E., Latif, M. T., Poyi, N. R., Wessey, N., & Acharjee, S. (2018) · InTech eBooks · doi:10.5772/intechopen.75776 · Cited by 4
Kim, N., Koh, S., & Lee, B. H. (2018) · Journal of the Mineralogical Society of Korea · doi:10.9727/jmsk.2018.31.3.215 · Cited by 3
Fru, E. C., Bankole, O. M., Chraiki, I., Youbi, N., Millet, M., Rouxel, O. J., Albani, A. E., & Bouougri, E. H. (2021) · Chemical Geology · doi:10.1016/j.chemgeo.2021.120404 · Cited by 3
Self-citationArchean Itabirites From Ovan, NE-Gabon: Petrography, Mineralogy And Elemental Mapping
Retonda-Kondja, S., Ondo, S. M. N., Edou-Minko, A., Sato, T., Moussavou, B. M., & Moussavou, M. (2021) · European Scientific Journal ESJ · doi:10.19044/esj.2021.v17n25p380 · Cited by 3
14 Germanium Isotope Geochemistry
Rouxel, O. J., & Luais, B. (2017) · De Gruyter eBooks · doi:10.1515/9783110545630-015 · Cited by 3
Self-citationESTUDOS GEOQUÍMICOS DE ITABIRITOS DA SERRA DO SAPO, ESPINHAÇO MERIDIONAL, MINAS GERAIS
Souza, A. D. A. P. E., Silva, R. C. F. E., Rosière, C. A., Dias, G. S., & Morais, F. P. (2014) · Revista Geonomos · doi:10.18285/geonomos.v22i2.313 · Cited by 3
Trendall, A. F. (2012) · Economic Geology · doi:10.2113/econgeo.107.2.377 · Cited by 3
Kirchman, D. L., & Shade, A. L. (2011) · Oxford University Press eBooks · doi:10.1093/9780197831632.003.0008 · Cited by 3
Influence of supercontinent cyclicity on global metallogenic processes: Main tendencies
Tkachev, А. V., & Rundquist, D. V. (2016) · Doklady Earth Sciences · doi:10.1134/s1028334x1608016x · Cited by 3
Section 2. Formation of Mineral Deposits
Arndt, N., Fontboté, L., Hedenquist, J. W., Kesler, S. E., Thompson, J. F., & Wood, D. (2017) · Geochemical Perspectives · Cited by 3
Moving to the Light: The Evolution of Photosynthesis
Ligrone, R. (2019) · Springer eBooks · doi:10.1007/978-3-030-16057-9_4 · Cited by 3
Aubet, N. R., Ernesto Pecoits, A., Bekker, A., Gingras, M. K., Zwingmann, H., Veroslavsky, G., Ana, H. D. S., & Konhauser, K. O. (2012) · Gondwana Research · doi:10.1016/j.gr.2012.09.004 · Cited by 3
Self-citationIron and phosphorus cycling under ferruginous conditions
Thompson, J. A. (2018) · White Rose eTheses Online (University of Leeds, The University of Sheffield, University of York) · Cited by 3
White, W. M. (2017) · Kirk-Othmer Encyclopedia of Chemical Technology · doi:10.1002/0471238961.koe00029 · Cited by 3
Plate Tectonics and Metallogeny
Robb, L. J., & Hawkesworth, C. J. (2020) · Elsevier eBooks · doi:10.1016/b978-0-12-409548-9.12535-7 · Cited by 3
George, P. M., Harlov, D. E., Windley, B. F., Satish-Kumar, M., Sajeev, K., & Zhai, M. (2024) · Mineralogy and Petrology · doi:10.1007/s00710-024-00854-5 · Cited by 3
Kim, H., Moon, I., Kim, M.-K., Lee, H., Choi, H., Uhm, Y. R., Liu, L., Kim, J., & Kim, W. (2025) · PLoS ONE · doi:10.1371/journal.pone.0316540 · Cited by 2
Zhang, Y., Xie, W., Li, D., Liu, Q., Sun, Y., Zhang, C., Geng, K., Wei, P., Zhang, C., & Cai, N. (2025) · Journal of Geochemical Exploration · doi:10.1016/j.gexplo.2025.107691 · Cited by 2
Sugiyama, I., & Halevy, I. (2025) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2025.03.018 · Cited by 3
Siahi, M., & Tsikos, H. (2025) · Sedimentology · doi:10.1111/sed.70015 · Cited by 2
Geology, Structure, Geochemistry, and Origin of Iron Oxide Deposits in Dehbid, Southwest Iran
Rajabi, A., Nozaem, R., Momenipour, S., et al. (2025) · Minerals · doi:10.3390/min15060590 · Cited by 2
Ansari, A. H., Shukla, Y., Singh, G. K., Sonker, A., Ansari, M. A., & Das, A. (2025) · Evolving Earth · doi:10.1016/j.eve.2025.100073 · Cited by 2
Steinhoefel, G., Schmitt, L., Angerer, T., Kirnbauer, T., & Klein, S. (2025) · Geochemistry Geophysics Geosystems · doi:10.1029/2025gc012223 · Cited by 2
Wang, E., Zhang, D., Luan, J., Men, Y., Wang, R., Xia, J., & Zhang, S. (2025) · Minerals · doi:10.3390/min15090996 · Cited by 2
Teece, B. L., Cannelli, S. M. C., Garibello, C. F., McGlynn, S. E., & Barge, L. M. (2025) · Earth-Science Reviews · doi:10.1016/j.earscirev.2025.105311 · Cited by 2
Goswami, S. (2025) · Discover Geoscience · doi:10.1007/s44288-025-00343-y · Cited by 2
Wafik, A., Massoude, M. B., Ntarmouchant, N., Admou, H., Chatiby, R., Atif, Y., & Pour, A. B. (2026) · Journal of African Earth Sciences · doi:10.1016/j.jafrearsci.2026.106006 · Cited by 2
Chen, Y.-R., Sun, G.-M., Li, Z., Chen, Y., & Zhou, Y.-Q. (2026) · Geoscience Frontiers · doi:10.1016/j.gsf.2026.102268 · Cited by 2
Li, R., Hu, J., Li, S., Li, Y., Qin, Z., Dong, R., Cui, H., Liang, X. S., & Konhauser, K. O. (2026) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2026.02.012 · Cited by 3
Self-citationMoon, I., Lee, S., & Liu, L. (2026) · Journal of the Korean Society of Mineral and Energy Resources Engineers · doi:10.32390/ksmer.2026.63.1.173 · Cited by 2
North China and Tarim Cratonic Blocks
Pirajno, F. (2012) · Springer eBooks · doi:10.1007/978-94-007-4444-8_3 · Cited by 2
Kar, E., Mishra, S., & Ghosh, P. (2021) · Journal of the Geological Society of India · doi:10.1007/s12594-021-1712-4 · Cited by 2
Mboudou, G. M. M., Owona, S., Jean-Lavenir, N. M., Agyingi, C. M., Ateba, M. C. B., & Mengu, E. E. (2021) · Geochemistry Exploration Environment Analysis · doi:10.1144/geochem2021-006 · Cited by 2
Zhou, Z., Chen, Y., Tang, H., Wu, Y., Li, Q., & Chen, Z. (2024) · Lithosphere · doi:10.2113/2024/lithosphere_2023_290 · Cited by 2
Oxygenation of the Proterozoic Earth's surface: An evolving story
Kendall, B., & Ostrander, C. M. (2024) · Elsevier eBooks · doi:10.1016/b978-0-323-99762-1.00058-9 · Cited by 3
Khedr, M. Z., Sayed, M. A., Ali, S., Azer, M. K., Ichiyama, Y., Takazawa, E., Kahal, A. Y., Abdelrahman, K. S., & Mahdi, A. M. (2024) · Minerals · doi:10.3390/min14070647 · Cited by 2
Han, X., & Liu, J. (2024) · Precambrian Research · doi:10.1016/j.precamres.2024.107480 · Cited by 2
Khare, S. K., Asthana, D., & Venkatesh, A. S. (2024) · Journal of Earth System Science · doi:10.1007/s12040-024-02366-4 · Cited by 2
Schmitt, L., Kirnbauer, T., Angerer, T., Kraemer, D., Garbe-Schoenberg, D., Fockenberg, T., & Klein, S. (2024) · Mineralium Deposita · doi:10.1007/s00126-024-01307-x · Cited by 2
Late Ordovician ironstone and its relation to ocean redox instability, climate and glaciation
Matheson, E. J., Malone, J. D., Pufahl, P. K., & Hiatt, E. E. (2024) · Sedimentology · doi:10.1111/sed.13247 · Cited by 3
Zhang, J., Cao, H., Zhu, C., et al. (2024) · IEEE Geoscience and Remote Sensing Letters · doi:10.1109/lgrs.2024.3509415 · Cited by 2
Debnath, S., Chakraborty, M., & Mishra, P. K. (2024) · Geochemistry · doi:10.1016/j.chemer.2024.126235 · Cited by 2
Expansion of the aerobic iron biogeochemical cycle during the Paleoproterozoic Lomagundi event
Ajagunjeun, A. A., Ossa, F. O., Kleinhanns, I. C., Marin‐Carbonne, J., Hofmann, A., Suwaidi, A. A., & Schoenberg, R. (2025) · Communications Earth & Environment · doi:10.1038/s43247-025-02106-6 · Cited by 2
Self-citationHodgskiss, M. S. W., Lechte, M. A., Rainbird, R. H., Whelan, M. A., Creaser, R. A., Davis, W. J., Slagstad, T., Mansur, E. T., Kirsimäe, K., Kovalick, A., et al. (2025) · Geological Society of America Bulletin · doi:10.1130/b37948.1 · Cited by 2
Self-citationAdak, S., & Pal, D. C. (2025) · Journal of Earth System Science · doi:10.1007/s12040-025-02575-5 · Cited by 2
Li, Y., Lu, X., Cui, X., Cai, Y., Liu, J., Liu, H., Hu, H., Li, J., Chen, J., & Deng, Z. (2025) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/j.palaeo.2025.113315 · Cited by 2
Bio-Geochemical Processes: Insights from Fe-Mn Mineralization in the Aegean Sea (Greece)
Vasilatos, C., Kampouroglou, E. E., Megremi, I., et al. (2022) · Minerals · doi:10.3390/min12101303 · Cited by 2
Wang, E., Chang-ik, H., Xia, J., et al. (2015) · Journal of Geoscience and Environment Protection · doi:10.4236/gep.2015.35007 · Cited by 2
Wang, C., & Zhang, L. (2016) · Springer geology · doi:10.1007/978-981-10-1064-4_13 · Cited by 2
Дмитриева, Н. В., Letnikova, E. F., Вишневская, И. А., & Serov, P. A. (2017) · Russian Geology and Geophysics · doi:10.1016/j.rgg.2017.07.004 · Cited by 2
Evolution of Photosynthetic System
Hanada, S. (2019) · Astrobiology · doi:10.1007/978-981-13-3639-3_10 · Cited by 2
Elements, biochemicals, and structures of microbes
Kirchman, D. L. (2011) · Oxford University Press eBooks · doi:10.1093/acprof:oso/9780199586936.003.0002 · Cited by 3
Mohanty, S., & Mishra, P. K. (2023) · Physics and Chemistry of Minerals · doi:10.1007/s00269-023-01258-1 · Cited by 2
Velivetskaya, T. A., Ignatiev, A. V., Vysotskiy, S. V., & Асеева, А. В. (2024) · Russian Geology and Geophysics · doi:10.2113/rgg20234602 · Cited by 2
Donia, A. M. A. (2023) · Malaysian Journal of Geosciences · doi:10.26480/mjg.01.2023.22.30 · Cited by 2
Melezhik, V. A., Ihlen, P. M., Bjerkgård, T., Sandstad, J. S., Raaness, A., Кузнецов, А. Б., Solli, A., Gorokhov, I. M., Pokrovsky, B. G., & Fallick, A. E. (2018) · Norwegian Journal of Geology · doi:10.17850/njg98-3-07 · Cited by 2
METAL HOMEOSTASIS IN PLANT MITOCHONDRIA
Vigani, G., & Hanikenne, M. (2017) · Wiley eBooks · doi:10.1002/9781118906583.ch5 · Cited by 2
Magnetic Petrophysics of the Vulcan Iron Formation (Michigan, USA)
Laird, M. S. (2017) · doi:10.37099/mtu.dc.etdr/443 · Cited by 2
The Possible Photochemical Origins of Banded Iron Formations
Castleberry, P. (2017) · Arizona State University Library Digital Repository (Arizona State University) · Cited by 2
Multiple Palaeoproterozoic carbon burial episodes and excursionsPreprint
Martin, A., Condon, D. J., Prave, A. R., Lepland, A., Fallick, A. E., Romashkin, A. E., Медведев, П. В., & Рычанчик, Д. В. (2017) · doi:10.31223/osf.io/h7x5k · Cited by 2
Mloszewska, A. M., Haugaard, R. N., Ernesto Pecoits, A., & Konhauser, K. O. (2015) · Encyclopedia of Astrobiology · doi:10.1007/978-3-662-44185-5_147 · Cited by 2
Self-citation
Metadata
- Authors
- Bekker, A., Slack, J. F., Planavsky, N., Krapez, B., Hofmann, A., Konhauser, K. O., & Rouxel, O. J.
- Venue
- Economic Geology
- Publisher
- Society of Economic Geologists, Inc.
- Published
- 2010-05-01
- Volume
- 105
- Issue
- 3
- Pages
- 467-508
- ISSN
- 0361-0128 (ISSN-L)
- OpenAlex
- W2168225982
- Semantic Scholar
- 2221663277a66ffb05c10389897649a9320dce31
- Cited by
- 1,013
- References
- 354
- Citations by year
- 2026: 51 · 2025: 74 · 2024: 78 · 2023: 73 · 2022: 82 · 2021: 70 · 2020: 58 · 2019: 66 · 2018: 69 · 2017: 75 · 2016: 62 · 2015: 65 · 2014: 57 · 2013: 51 · 2012: 36
- FWCI
- 29.66
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Economic Geology (publishedVersion)
- eSpace (Curtin University) (submittedVersion)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geological and Geochemical Analysis
- Keywords
- iron-formation, banded iron formations, greenstone belts, volcanogenic massive sulfide deposits, Archean, Paleoproterozoic, mantle processes, tectonic setting, oceanic processes, biosphere
About these checks
Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.
Statistics and arithmetic are recomputed, not judged.
Confidence bands are shown only for fields calibrated on our annotated test set. None is calibrated yet, so no band is shown.
What counts as a claim ›How we measure confidence ›How we check this ›
Are you an author, or do you see a problem with this page? Request a review
