The DOI matches its Crossref record; 26 of the 27 references it cites were found in a registry or an index.
Evidence from detrital zircons for the existence of continental crust and oceans on the Earth 4.4 Gyr ago
Abstract
No crustal rocks are known to have survived since the time of the intense meteor bombardment that affected Earth between its formation about 4,550 Myr ago and 4,030 Myr, the age of the oldest known components in the Acasta Gneiss of northwestern Canada. But evidence of an even older crust is provided by detrital zircons in metamorphosed sediments at Mt Narryer and Jack Hills in the Narryer Gneiss Terrane, Yilgarn Craton, Western Australia, where grains as old as approximately 4,276 Myr have been found. Here we report, based on a detailed micro-analytical study of Jack Hills zircons, the discovery of a detrital zircon with an age as old as 4,404+/-8 Myr--about 130 million years older than any previously identified on Earth. We found that the zircon is zoned with respect to rare earth elements and oxygen isotope ratios (delta18O values from 7.4 to 5.0%), indicating that it formed from an evolving magmatic source. The evolved chemistry, high delta18O value and micro-inclusions of SiO2 are consistent with growth from a granitic melt with a delta18O value from 8.5 to 9.5%. Magmatic oxygen isotope ratios in this range point toward the involvement of supracrustal material that has undergone low-temperature interaction with a liquid hydrosphere. This zircon thus represents the earliest evidence for continental crust and oceans on the Earth.
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
“Elevated 18O/16O in 4.3-Ga-old zircons was possibly inherited from 18O-enriched, weathered surface rocks that were later buried and melted, which implies the presence of surficial liquid water and even land (17, 18).”
From The Archean atmosphere (2020) · cites this paper as [18]
In the citing paper
“Earlier estimates of low temperatures (<150 • C), based on isotopic analyses of oxygen isotopes the zircons (Wilde et al. 2001), may have been confounded by later contamination of the oxygen isotopic history of the zircons (Valley et al. 2014) but the salient message is that, quite early in the history of the Earth, the planet was covered by water.”
From The Emergence of Life (2019) · cites this paper as Wilde et al. 2001
In the citing paper
“Evidence of mineral interactions with water suggest that oceans may have started to form by 4.2 Ga (Cavosie et al., 2005) or possibly as early as 4.4 Ga (Wilde et al., 2001).”
From The Astrobiology Primer v2.0 (2016) · cites this paper as Wilde et al., 2001
Citations
Cites
Microfossils of the early Archean apex chert: New evidence of the antiquity of life
Schopf, J. W. (1993) · Science · doi:10.1126/science.260.5108.640 · Cited by 1,363
Earth's earliest biosphere : its origin and evolution
Schopf, J. W. (1983) · Cited by 1,287
Zircon U-Pb ages for the Early Cambrian time-scale
Compston, W., Williams, I. S., Kirschvink, J. L., Zhang, Z., & Guogan, M. (1992) · Journal of the Geological Society · doi:10.1144/gsjgs.149.2.0171 · Cited by 1,137
Applications of Microanalytical Techniques to Understanding Mineralizing Processes
(1997) · doi:10.5382/rev.07 · Cited by 1,090
Zircon megacrysts from kimberlite: oxygen isotope variability among mantle melts
Valley, J. W., Kinny, P. D., Schulze, D. J., & Spicuzza, M. J. (1998) · Contributions to Mineralogy and Petrology · doi:10.1007/s004100050432 · Cited by 974
Self-citationGeochronology, Time Scales and Global Stratigraphic Correlation
Berggren, W. A., Kent, D. V., Aubry, M., & Hardenbol, J. (1995) · SEPM (Society for Sedimentary Geology) eBooks · doi:10.2110/pec.95.04 · Cited by 922
Nature of the Earth's earliest crust from hafnium isotopes in single detrital zircons
Amelin, Y., Lee, D., Halliday, A. N., & Pidgeon, R. T. (1999) · Nature · doi:10.1038/20426 · Cited by 785
Vidal, G. (1985) · Lethaia · doi:10.1111/j.1502-3931.1985.tb00704.x · Cited by 597
Priscoan (4.00–4.03 Ga) orthogneisses from northwestern Canada
Bowring, S. A., & Williams, I. S. (1999) · Contributions to Mineralogy and Petrology · doi:10.1007/s004100050465 · Cited by 568 · cited 1×
“between its formation about 4,550 Myr ago and 4,030 Myr, the age of the oldest known components in the Acasta Gneiss of northwestern Canad”
BackgroundClaoué-Long, J. C., Compston, W., Roberts, J., & Fanning, C. M. (1995) · SEPM (Society for Sedimentary Geology) eBooks · doi:10.2110/pec.95.04.0003 · Cited by 549
Research works printed but not linked: 6
- Ryder, G. Chronology of early bombardment in the inner solar system. Geol. Soc. Am. Abstr. Progm 21, A299 ( 1992).
- Wilde, S. A. & Pidgeon, R. T. in 3rd International Archaean Symposium (Perth), Excursion Guidebook (eds Ho, S. E., Glover, J. E., Myers, J. S. & Muhling, J. R.) 82–95 (University of Western Australia Extension Publication, Vol. 21, Perth, 1990).
- Nelson, D. R. Compilation of SHRIMP U-Pb geochronology data, 1996. Geol. Surv. Western Australia Rec. 1997/2, 1–11 (1997).
- Muehlenbachs, K. in Stable Isotopes (eds Valley, J. W. et al.) MSA Rev. Min. 16, 425–444 ( 1986).
- Pidgeon, R. T. et al. in Eighth Int. Conf. Geochron., Cosmochron. Isotope Geol. (eds Lanphere, M. A., Dalrymple, G. B. & Turrin, B. D.) 251 (US Geological Survey Circular 1107, Denver, Colorado, 1994).
- Valley, J. W., Graham, C. M., Harte, B., Eiler, J. M. & Kinny, P. D. in Applications of Microanalysis to Understanding Mineralizing Processes (eds McKibben, M. A., Shanks III, W. C. & Ridley, W. I.) 73–98 ( xReviews in Economic Geology, Vol. 7, Society of Economic Geologists, Littleton, Colorado, 1998).
Cited by
Sorted by citations
Items 601–700 of 999
Thöni, M., & Miller, C. (2004) · Chemical Geology · doi:10.1016/j.chemgeo.2004.03.006 · Cited by 35
Early assembly of cellular life
Trevors, J. T. (2003) · Progress in Biophysics and Molecular Biology · doi:10.1016/s0079-6107(03)00018-x · Cited by 34
“Peck et al. (2001) and Wilde et al. (2001) provided evidence that the crust and oceans were present on the Earth 4.4 billion years.”
BackgroundInfluentialThe Chemical Basis of Membrane Bioenergetics
Berry, S. (2002) · Journal of Molecular Evolution · doi:10.1007/s00239-001-0056-3 · Cited by 35
“The solar system and the Earth formed about 4.5 billion years (Ga) ago (Nisbet 1985; Sleep et al. 2001); recent evidence indicates the presence of oceans as early as 4.3–4.4 Ga ago (Mojzsis et al. 2001; Wilde et al. 2001).”
BackgroundInfluentialKranendonk, M. J. V. (2004) · Precambrian Research · doi:10.1016/j.precamres.2003.12.008 · Cited by 35
Ancient and recycled sulfur sampled by the Iceland mantle plume
Ranta, E., Gunnarsson-Robin, J., Halldórsson, S. A., Ono, S., Izon, G., Jackson, M. G., Reekie, C. D. J., Jenner, F. E., Guðfinnsson, G. H., Jónsson, Ó. P., et al. (2022) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2022.117452 · Cited by 34
Can thin cirrus clouds in the tropics provide a solution to the faint young Sun paradox?
Rondanelli, R., & Lindzen, R. S. (2010) · Journal of Geophysical Research: Atmospheres · doi:10.1029/2009jd012050 · Cited by 34
“At the same time, geological evidence shows the presence of a stable ocean and liquid water in the planet at least after 3.9 Ga (and perhaps even earlier [e.g., Wilde et al., 2001; Pinti, 2005]).”
BackgroundInfluentialOnset of the Earth’s hydrological cycle four billion years ago or earlier
Gamaleldien, H., Wu, L., Olierook, H. K. H., Kirkland, C. L., Kirscher, U., Li, Z., Johnson, T. E., Makin, S., Li, Q., Jiang, Q., et al. (2024) · Nature Geoscience · doi:10.1038/s41561-024-01450-0 · Cited by 34
Self-citationThern, E. R., & Nelson, D. R. (2011) · Precambrian Research · doi:10.1016/j.precamres.2011.10.015 · Cited by 34
“…rocks in Eriksson and Wilde (2010)), a fluvialite r braided stream environment (as discussed for the Mt. Narryer etasedimentary rocks in Williams and Myers (1987)), or within shallow-marine shelf environment (as discussed for the Toodyay ake Grace ‘Jimperding Metamorphic Belt’…”
BackgroundCarbon dioxide cycling through the mantle and implications for the climate of ancient Earth
Zahnle, K. J., & Sleep, N. H. (2002) · Geological Society London Special Publications · doi:10.1144/gsl.sp.2002.199.01.12 · Cited by 34
Francis, B. R., Watkins, K. J., & Kubelka, J. (2017) · Life · doi:10.3390/life7030035 · Cited by 36
“Analysis of detrital zircons suggests the presence of granitic material on the early Earth that is indicative of continental crust [87,88], although an alternative interpretation has been proposed [89].”
BackgroundLi, Z., Wei, C., Chen, B., Fu, B., & Gong, M. (2019) · Gondwana Research · doi:10.1016/j.gr.2019.10.020 · Cited by 34
Volatile element chemistry during accretion of the earth
Fegley, B., Lodders, K., & Jacobson, N. S. (2020) · Geochemistry · doi:10.1016/j.chemer.2019.125594 · Cited by 36
Numerous chondritic impactors and oxidized magma ocean set Earth’s volatile depletion
Sakuraba, H., Kurokawa, H., Genda, H., & Ohta, K. (2021) · Scientific Reports · doi:10.1038/s41598-021-99240-w · Cited by 38
High yield shock synthesis of ammonia from iron, water and nitrogen available on the early Earth
Nakazawa, H., SEKINE, T., Kakegawa, T., & Nakazawa, S. (2005) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2005.03.024 · Cited by 33
Oxygen diffusion in titanite: Lattice diffusion and fast-path diffusion in single crystals
Zhang, X. Y., Cherniak, D. J., & Watson, E. B. (2006) · Chemical Geology · doi:10.1016/j.chemgeo.2006.06.005 · Cited by 34
“Zircon is the first candidate for which oxygen isotope composition has been linked with U–Pb ages as a tool to “see through” metamorphism and decipher complex igneous and metamorphic histories (Valley et al., 1994; Wilde et al., 2001; Mojzsis et al., 2001; Peck et al., 2001).”
BackgroundYuan, H., & Bodin, T. (2018) · Tectonics · doi:10.1029/2017tc004834 · Cited by 34
“The cratonic crust holds the oldest direct record of Earth’s evolution (e.g., Wilde et al., 2001), but how it formed remains controversial.”
BackgroundSugahara, H., & Mimura, K. (2015) · Icarus · doi:10.1016/j.icarus.2015.04.029 · Cited by 34
Bizzarri, B. M., Saladino, R., Delfino, I., García-Ruiz, J. M., & Di Mauro, E. (2021) · International Journal of Molecular Sciences · doi:10.3390/ijms22020917 · Cited by 33
Dickeson, Z. I., & Davis, J. M. (2020) · Astronomy & Geophysics · doi:10.1093/astrogeo/ataa038 · Cited by 33
Ion microprobe U–Pb dating of Quaternary zircon: implication for magma cooling and residence time
Sano, Y., Tsutsumi, Y., Terada, K., & Kaneoka, I. (2002) · Journal of Volcanology and Geothermal Research · doi:10.1016/s0377-0273(02)00297-4 · Cited by 33
Polat, A., Frei, R., Fryer, B. J., & Appel, P. W. U. (2009) · Chemical Geology · doi:10.1016/j.chemgeo.2009.09.004 · Cited by 33
Ca isotope fingerprints of early crust-mantle evolution
Kreissig, K., & Elliott, T. R. (2004) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2004.06.026 · Cited by 33
“Evidence for the existence of continental crust up to 4.4 Ga comes from detrital zircons from the Jack Hills and Mount Narryer, Yilgarn Craton, Western Australia (Wilde et al., 2001).”
BackgroundInfluentialGeneral Precambrian Geology in China
Zhai, M., & Zhou, Y. (2015) · Springer geology · doi:10.1007/978-3-662-47885-1_1 · Cited by 33
Extrasolar planets and false atmospheric biosignatures: The role of micrometeoroids
Court, R. W., & Sephton, M. A. (2012) · Planetary and Space Science · doi:10.1016/j.pss.2012.08.026 · Cited by 32
Geosites, Sites of Special Scientific Interest, and Potential Geoparks in the Anti-Atlas (Morocco)
Errami, E., Brocx, M., Semeniuk, V., & Ennih, N. (2015) · Geoheritage, geoparks and geotourism · doi:10.1007/978-3-319-10708-0_4 · Cited by 32
Earth’s thermal evolution, mantle convection, and Hadean onset of plate tectonics
Ernst, E. (2017) · Journal of Asian Earth Sciences · doi:10.1016/j.jseaes.2017.05.037 · Cited by 32
Keller, C. B., Boehnke, P., Schoene, B., & Harrison, T. M. (2019) · Geochronology · doi:10.5194/gchron-1-85-2019 · Cited by 32
“Hadean Jack Hills zircons display oxygen isotope compositions enriched in 18O relative to the mantle, suggesting a parental magma that incorporated silicates, which have interacted with liquid water (Mojzsis et al., 2001; Wilde et al., 2001; Cavosie et al., 2005; Trail et al., 2007).”
BackgroundCesare, B., Parisatto, M., Mancini, L., Peruzzo, L., Franceschi, M., Tacchetto, T., Reddy, S. M., Spiess, R., Nestola, F., & Marone, F. (2020) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2020.116708 · Cited by 33
No evidence of supracrustal recycling in Si-O isotopes of Earth’s oldest rocks 4 Ga ago
Zhang, Q., Zhao, L., Zhou, D., Nutman, A. P., Mitchell, R. N., Liu, Y., Li, Q., Yu, H., Fan, B., Spencer, C. J., et al. (2023) · Science Advances · doi:10.1126/sciadv.adf0693 · Cited by 32
The Evolution of the Lunar Crust
Elardo, S. M., Pieters, C. M., Dhingra, D., Hanna, K. L. D., Glotch, T. D., Greenhagen, B. T., Groß, J., Head, J. W., III, Jolliff, B. L., Klima, R. L., et al. (2023) · Reviews in Mineralogy and Geochemistry · doi:10.2138/rmg.2023.89.07 · Cited by 35
Problems of geodynamics, tectonics, and metallogeny of orogens
Dobretsov, N. L., & Buslov, M. M. (2011) · Russian Geology and Geophysics · doi:10.1016/j.rgg.2011.11.012 · Cited by 32
Montario, M. J., & Garver, J. I. (2009) · The Journal of Geology · doi:10.1086/605778 · Cited by 32
“SHRIMP U/Pb study of zircons from the Adirondacks and adjacent Grenville Province of Canada: a preliminary report.”
InfluentialYang, S., Lou, F., Xu, C., Feng, C., Cao, S., Xu, D., & Tang, Y. (2021) · Ore Geology Reviews · doi:10.1016/j.oregeorev.2021.104598 · Cited by 31
Sawada, H., Isozaki, Y., Sakata, S., Hirata, T., & Maruyama, S. (2016) · Geoscience Frontiers · doi:10.1016/j.gsf.2016.11.010 · Cited by 32
Earth's Oldest Rocks and Minerals
Condie, K. C. (2018) · Elsevier eBooks · doi:10.1016/b978-0-444-63901-1.00011-3 · Cited by 31
Nanoscale constraints on the shock-induced transformation of zircon to reidite
Montalvo, S. D., Reddy, S. M., Saxey, D. W., Rickard, W. D. A., Fougerouse, D., Quadir, Z., & Johnson, T. E. (2019) · Chemical Geology · doi:10.1016/j.chemgeo.2018.12.039 · Cited by 32
Subduction-zone peridotites and their records of crust-mantle interaction
Zheng, J., Xiong, Q., Zhao, Y., & Li, W. (2019) · Science China Earth Sciences · doi:10.1007/s11430-018-9346-6 · Cited by 31
“The initiation of plate subduction on Earth may occur before 3 billion years ago (Shirey and Richardson, 2011) or even Hadean (Wilde et al., 2001).”
BackgroundThe onset of deep recycling of supracrustal materials at the Paleo-Mesoarchean boundary
Wang, X., Tang, M. H., Moyen, J., Wang, D., Kröner, A., Hawkesworth, C. J., Xia, X., Xie, H., ANHAEUSSER, C. R., Hofmann, A., et al. (2021) · National Science Review · doi:10.1093/nsr/nwab136 · Cited by 31
Low volcanic outgassing rates for a stagnant lid Archean earth with graphite-saturated magmas
Guimond, C. M., Noack, L., Ortenzi, G., & Sohl, F. (2021) · Physics of The Earth and Planetary Interiors · doi:10.1016/j.pepi.2021.106788 · Cited by 33
Proterozoic deformation in the northwest of the Archean Yilgarn Craton, Western Australia
Spaggiari, C. V., Wartho, J., & Wilde, S. A. (2007) · Precambrian Research · doi:10.1016/j.precamres.2007.10.004 · Cited by 31
Self-citationBioavailability of Metal Ions and Evolutionary Adaptation
Enriquez, R. P. H., & Do, T. N. (2012) · Life · doi:10.3390/life2040274 · Cited by 34
“9 Ga ago and they were so intense that there is barely any geological record of the earlier conditions in our planet [11].”
BackgroundThe Transition from Geochemistry to Biogeochemistry
Sahai, N., Kaddour, H., & Dalai, P. (2016) · Elements · doi:10.2113/gselements.12.6.389 · Cited by 32
Franck, S., Kossacki, K. J., von Bloh, W., & Bounama, C. (2002) · Tellus B · doi:10.3402/tellusb.v54i4.16669 · Cited by 34
Shu, C., Long, X., Yin, C., Yuan, C., Wang, Q., He, X., Zhao, B., & Huang, Z. (2018) · Gondwana Research · doi:10.1016/j.gr.2018.06.004 · Cited by 30
Secular cooling and crystallization of partially molten Archaean continental crust over 1 Ga
Vanderhaeghe, O., Guergouz, C., Fabre, C., Duchêne, S., & Baratoux, D. (2019) · Comptes Rendus Géoscience · doi:10.1016/j.crte.2019.07.002 · Cited by 32
Lock, S. J., Bermingham, K. R., Parai, R., & Boyet, M. (2020) · Space Science Reviews · doi:10.1007/s11214-020-00729-z · Cited by 35
Lu, G., Spencer, C. J., Tian, Y., & Wang, W. (2021) · Geophysical Research Letters · doi:10.1029/2021gl096049 · Cited by 30
Ages and Growth of the Continental Crust from Radiogenic Isotopes
Patchett, P. J., & Samson, S. D. (2003) · Treatise on Geochemistry · doi:10.1016/b0-08-043751-6/03026-7 · Cited by 30
Li, G., Wang, Q., Huang, Y., Chen, F., & Dong, P. (2015) · Precambrian Research · doi:10.1016/j.precamres.2015.10.003 · Cited by 30
3.8 Ga zircons sampled by Neogene ignimbrite eruptions in Central Anatolia
Paquette, J., & Pennec, J. L. (2012) · Geology · doi:10.1130/g32472.1 · Cited by 30
Mimura, K., & Toyama, S. (2004) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2004.06.020 · Cited by 30
Arvizu, A. I. A. H. E. (2015) · Boletín de la Sociedad Geológica Mexicana · doi:10.18268/bsgm2015v67n3a16 · Cited by 30
Hadean to Paleoarchean Rocks and Zircons in China
Wan, Y., Xie, H., Dong, C., Kröner, A., Wilde, S. A., Bai, W., Liu, S., Xie, S., Ma, M., Li, Y., et al. (2018) · Elsevier eBooks · doi:10.1016/b978-0-444-63901-1.00014-9 · Cited by 30
Self-citationKomiya, T. (2007) · Springer eBooks · doi:10.1007/978-1-4020-5750-2_8 · Cited by 30
Studying the Earth with GeoneutrinosPreprint
Ludhová, L., & Zavatarelli, S. (2014) · Cited by 30
Natural Radioactivity and Chemical Evolution on the Early Earth: Prebiotic Chemistry and Oxygenation
Ершов, Б. Г. (2022) · Molecules · doi:10.3390/molecules27238584 · Cited by 30
“The zircon crystals found in Western Australia [48,49], which might have formed in the presence of water according to isotope and geochemical indications, probably provide evidence for even earlier existence of liquid water on Earth (4.”
BackgroundInfluentialReduced Diversity of Life around Proxima Centauri and TRAPPIST-1
Lingam, M., & Loeb, A. (2017) · The Astrophysical Journal Letters · doi:10.3847/2041-8213/aa8860 · Cited by 29
“We have chosen 4.4 Gyr as this represents the time elapsed after the initial formation of oceans and continental crust (Wilde et al. 2001), thereby enabling evolution.”
MethodInfluentialCometary Glycolaldehyde as a Source of pre-RNA Molecules
Zellner, N. E. B., McCaffrey, V. P., & Butler, J. H. E. (2020) · Astrobiology · doi:10.1089/ast.2020.2216 · Cited by 32
The influence of fractionation of REE-enriched minerals on the zircon partition coefficients
Zhong, S., Li, S., Seltmann, R., Lai, Z., & Zhou, J. (2020) · Geoscience Frontiers · doi:10.1016/j.gsf.2020.10.002 · Cited by 29
Miyazaki, Y., & Korenaga, J. (2022) · Astrobiology · doi:10.1089/ast.2021.0126 · Cited by 34
Huang, G., Pan, J., Xia, F., Yan, J., Chengyong, Z., Wu, D., & Liu, Y. (2022) · Journal of Earth Science · doi:10.1007/s12583-022-1654-9 · Cited by 29
“…ed in light rare earth elements (LREEs) and enriched in heavy rare earth elements (HREEs), with significantly positive Ce anomalies and negative Eu anomalies (Huang G W et al., 2021), which indicates that most of the detrital zircons have a magmatic origin (Corfu et al., 2003; Wilde et al., 2001).”
BackgroundThe Origin and Earliest History of the Earth
Halliday, A. N. (2013) · Elsevier eBooks · doi:10.1016/b978-0-08-095975-7.00123-6 · Cited by 30
“(iv) Mojzsis et al. (2001) and Wilde et al. (2001) have made major advances in studying the Hadean using single zircons.”
BackgroundOpen Questions on the Origin of Life at Anoxic Geothermal Fields
Mulkidjanian, A. Y., Bychkov, A. Y., Dibrova, D. V., Galperin, M. Y., & Koonin, E. V. (2012) · Origins of Life and Evolution of Biospheres · doi:10.1007/s11084-012-9315-0 · Cited by 31
“These data indicate that there were continents 4.3–4.4 Gy ago (Wilde et al. 2001) and subduction zones 4.0–4.2 Gyr ago (Hopkins et al. 2008).. Existence of subduction zones implies stability of continent(s) on a time scale of millions of years, at least, and the existence of inland geothermal…”
InfluentialASTEROIDAL GRANITE-LIKE MAGMATISM 4.53 GYR AGO
Terada, K., & Bischoff, A. (2009) · The Astrophysical Journal · doi:10.1088/0004-637x/699/2/l68 · Cited by 29
Chemical sedimentary protoliths in the >3.75Ga Nuvvuagittuq Supracrustal Belt (Québec, Canada)
Mloszewska, A. M., Mojzsis, S. J., Ernesto Pecoits, A., Papineau, D., Dauphas, N., & Konhauser, K. O. (2012) · Gondwana Research · doi:10.1016/j.gr.2012.11.005 · Cited by 29
Scherstén, A., Szilas, K., Creaser, R. A., Næraa, T., Gool, J. A. M. V., & Østergaard, C. (2012) · Precambrian Research · doi:10.1016/j.precamres.2011.12.014 · Cited by 29
SIMS Measurement of Stable Isotopes
Ireland, T. R. (2004) · Elsevier eBooks · doi:10.1016/b978-044451114-0/50032-6 · Cited by 30
Spaggiari, C. V. (2007) · Precambrian Research · doi:10.1016/j.precamres.2007.02.007 · Cited by 29
Caro, G., Bennett, V. C., Bourdon, B., Harrison, T. M., von Quadt, A., Mojzsis, S. J., & Harris, J. W. (2007) · Chemical Geology · doi:10.1016/j.chemgeo.2007.10.018 · Cited by 29
“Finsch inclusions and Jack Hills zircons are amongst the oldest preserved samples of the terrestrial mantle and crust (Froude et al., 1983; Richardson et al., 1984; Wilde et al., 2001).”
BackgroundEarly Life on Earth: The Ancient Fossil Record
Westall, F. (2004) · Springer eBooks · doi:10.1007/1-4020-2305-7_12 · Cited by 29
Carbon cycle evolution before and after the Great Oxidation of the atmosphere
Canfield, D. E. (2021) · American Journal of Science · doi:10.2475/03.2021.01 · Cited by 28
Crustal growth and evolution of Archean continental crust in the southern North China Craton
Diwu, C. (2021) · Acta Petrologica Sinica · doi:10.18654/1000-0569/2021.02.01 · Cited by 28
Huang, G., Guangzhi, N., Zhanwu, Z., Wang, X., Xu, X., Jun, G., & Yu, F. (2013) · Chinese Science Bulletin · doi:10.1007/s11434-013-5842-y · Cited by 28
Contrasting geochemistry of magmatic and secondary zircons
Balashov, Y. A., & Скублов, С. Г. (2011) · Geochemistry International · doi:10.1134/s0016702911040033 · Cited by 28
Zircon response to high-grade metamorphism as revealed by U–Pb and cathodoluminescence studies
Siebel, W., Shang, C. K., Thern, E. R., Danišík, M., & Rohrmüller, J. (2012) · International Journal of Earth Sciences · doi:10.1007/s00531-012-0772-5 · Cited by 28
“Resistance to Pb diffusion during orogenic cycles gives zircon a unique capacity among geochronometers and allows scientists to observe ancient crust-forming periods in zircons collected from much younger rocks (Wilde et al. 2001).”
Kumari, S., Paul, D., & Stracke, A. (2016) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2016.09.011 · Cited by 28
On the free energy that drove primordial anabolism
Kaufmann, M. (2009) · International Journal of Molecular Sciences · doi:10.3390/ijms10041853 · Cited by 23
“Beyond all question, impacts are hostile events and, provided that life has already come into existence before that as some authors suppose [42-44], the late heavy bombardment is assumed being a sterilizing period wiping out all such life forms, at least on the surface of the early Earth [45,46].”
BackgroundBjørnerud, M. G., & Austrheim, H. (2004) · Geology · doi:10.1130/g20590.1 · Cited by 33
Evidence for Hadean mafic intrusions in the Nuvvuagittuq Greenstone Belt, Canada
Sole, C., OʼNeil, J., Rizo, H., Paquette, J., Benn, D. J. A. E. A. D. I., & Plakholm, J. A. (2025) · Science · doi:10.1126/science.ads8461 · Cited by 30
Bibikova, E. V., Bogdanova, S., Postnikov, A. V., Fedotova, А. А., Claesson, S., Kirnozova, T. I., Fugzan, M. M., & Popova, L. P. (2015) · Stratigraphy and Geological Correlation · doi:10.1134/s0869593815010037 · Cited by 27
“That is the way the Earth’s oldest zircons with age of 4.4 Ga were found in the Ilgarn block (Australia) (Wilde et al., 2001; Kemp et al., 2010).”
BackgroundInfluentialHeavy minerals in provenance studies: an overview
Joshi, K. B., Banerji, U. S., Dubey, C. P., & OLIVEIRA, E. P. D. (2021) · Arabian Journal of Geosciences · doi:10.1007/s12517-021-07687-y · Cited by 28
“Studies from Jack Hills, Australia, have demonstrated that detrital zircons preserve ages (~4.40 Ga) much older than the oldest (~4.03 Ga) exposed bedrock lithologies (Bowring and Williams 1999; Wilde et al. 2001; Reimink et al. 2016).”
BackgroundInfluentialZircons underestimate mantle depletion of early Earth
Liou, P., Guo, J., Mitchell, R. N., Spencer, C. J., Li, X., Zhai, M., Evans, N. J., Li, Y., McDonald, B. J., & Jin, M. (2021) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2021.11.015 · Cited by 27
Applications of scanning electron microscopy in earth sciences
Chen, L., Xu, J., & Chen, J. (2015) · Science China Earth Sciences · doi:10.1007/s11430-015-5172-9 · Cited by 27
Modelling the isotopic evolution of the Earth
Paul, D., White, W. M., & Turcotte, D. L. (2002) · Philosophical Transactions of the Royal Society A Mathematical Physical and Engineering Sciences · doi:10.1098/rsta.2002.1076 · Cited by 27
Liu, W., Yang, X., Shu, S., Liu, L., & Yuan, S. (2018) · Minerals · doi:10.3390/min8080333 · Cited by 27
“The oldest known zircon on Earth is a detrital zircon from the Jack Hills and adjac nt areas in the northern Yilgarn Craton, West rn Australia with a 207Pb/206Pb ag of 4404 ± 8 Ma [72].”
BackgroundKramers, J. D. (2002) · Geological Society London Special Publications · doi:10.1144/gsl.sp.2002.199.01.13 · Cited by 27
Prime controls on Archaean–Palaeoproterozoic sedimentation: Change over time
Eriksson, P. G., Banerjee, S., Catuneanu, O., Sarkar, S., Bumby, A. J., & Mtimkulu, M. N. (2007) · Gondwana Research · doi:10.1016/j.gr.2007.04.004 · Cited by 27
Isotope Evolution of the Depleted Mantle
Vervoort, J. D., & Kemp, A. I. S. (2024) · Annual Review of Earth and Planetary Sciences · doi:10.1146/annurev-earth-031621-112052 · Cited by 26
Wiemer, D., Allen, C. M., Murphy, D. T., & Kinaev, I. (2017) · Chemical Geology · doi:10.1016/j.chemgeo.2017.06.019 · Cited by 26
Detrital zircons and the interpretation of palaeogeography, with the Variscan Orogeny as an example
Franke, W., Cocks, L. R. M., & Torsvik, T. H. (2019) · Geological Magazine · doi:10.1017/s0016756819000943 · Cited by 26
Solubility of hydroxyl groups in pyroxenes: Effect of oxygen fugacity at 0.2–3 GPa and 800–1200 °C
Liu, H., & Yang, X.-Z. (2020) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2020.07.034 · Cited by 23
Ueda, H., & Shibuya, T. (2021) · Minerals · doi:10.3390/min11040389 · Cited by 26
“4 Ga [4] were found from the clastic rocks in Australia.”
BackgroundPuchtel, I. S., Nicklas, R. W., Slagle, J., Horan, M. F., Walker, R. J., Nisbet, E. G., & Locmelis, M. (2021) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2021.11.030 · Cited by 26
Iizuka, T., Nebel, O., & McCulloch, M. T. (2011) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2011.06.006 · Cited by 27
Bibikova, E. V., Claesson, S., Fedotova, А. А., Artemenko, G. V., & Ильинский, Л. C. (2010) · Geochemistry International · doi:10.1134/s0016702910090016 · Cited by 26
Morris, G. A., Kirkland, C. L., & Pease, V. (2015) · Lithosphere · doi:10.1130/l420.1 · Cited by 26
The significance of subduction-related accretionary complexes in early Earth processes
Shervais, J. W. (2006) · Geological Society of America eBooks · doi:10.1130/2006.2405(10 · Cited by 29
Early earth geodynamics: cross examining the geological testimony
Kemp, A. I. S. (2018) · Philosophical Transactions of the Royal Society A Mathematical Physical and Engineering Sciences · doi:10.1098/rsta.2018.0169 · Cited by 26
3 Early Life on Earth and Analogies to Mars
Westall, F. (2005) · Advances in astrobiology and biogeophysics · doi:10.1007/978-3-540-31538-4_3 · Cited by 26
Biomarkers of extrasolar planets and their observability
Selsis, F., Paillet, J., & Allard, F. C. (2007) · Cambridge University Press eBooks · doi:10.1017/cbo9780511536533.010 · Cited by 25
Metadata
- Authors
- Wilde, S. A., Valley, J. W., Peck, W. H., & Graham, C. M.
- Affiliations
- Curtin University (AU)
- University of Wisconsin–Madison (US)
- University of Edinburgh (GB)
- Venue
- Nature
- Published
- 2001-01
- Volume
- 409
- Issue
- 6817
- Pages
- 175-178
- ISSN
- 0028-0836 (ISSN-L)
- 1476-4687
- OpenAlex
- W1615737483
- Cited by
- 1,744
- References
- 27
- Citations by year
- 2026: 60 · 2025: 60 · 2024: 72 · 2023: 96 · 2022: 67 · 2021: 76 · 2020: 93 · 2019: 71 · 2018: 120 · 2017: 71 · 2016: 77 · 2015: 76 · 2014: 85 · 2013: 77 · 2012: 62
- FWCI
- 57.58
- Type
- journal article
- Language
- en
- Open access
- closed
- Licence
- www.springer.com/tdm (tdm)
- Locations
- Nature (publishedVersion)
- PubMed (publishedVersion)
- RePEc: Research Papers in Economics (submittedVersion)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geological and Geochemical Analysis
- Physical Sciences › Earth and Planetary Sciences › Space and Planetary Science › Astro and Planetary Science
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
- Keywords
- detrital zircon, Jack Hills zircons, Yilgarn Craton, early Earth crust, early oceans, zircon oxygen isotopes, granitic melts, hydrosphere, Hf isotopes, Hadean
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