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Uranium isotopes distinguish two geochemically distinct stages during the later Cambrian SPICE event
Open accessAbstract
Anoxic marine zones were common in early Paleozoic oceans (542-400 Ma), and present a potential link to atmospheric pO 2 via feedbacks linking global marine phosphorous recycling, primary production and organic carbon burial. Uranium (U) isotopes in carbonate rocks track the extent of ocean anoxia, whereas carbon (C) and sulfur (S) isotopes track the burial of organic carbon and pyrite sulfur (primary long-term sources of atmospheric oxygen). In combination, these proxies therefore reveal the comparative dynamics of ocean anoxia and oxygen liberation to the atmosphere over million-year time scales. Here we report high-precision uranium isotopic data in marine carbonates deposited during the Late Cambrian 'SPICE' event, at ca. 499 Ma, documenting a well-defined -0.18‰ negative δ238 U excursion that occurs at the onset of the SPICE event's positive δ13 C and δ34 S excursions, but peaks (and tails off) before them. Dynamic modelling shows that the different response of the U reservoir cannot be attributed solely to differences in residence times or reservoir sizes - suggesting that two chemically distinct ocean states occurred within the SPICE event. The first ocean stage involved a global expansion of euxinic waters, triggering the spike in U burial, and peaking in conjunction with a well-known trilobite extinction event. During the second stage widespread euxinia waned, causing U removal to tail off, but enhanced organic carbon and pyrite burial continued, coinciding with evidence for severe sulfate depletion in the oceans (Gill et al., 2011). We discuss scenarios for how an interval of elevated pyrite and organic carbon burial could have been sustained without widespread euxinia in the water column (both non-sulfidic anoxia and/or a more oxygenated ocean state are possibilities). Either way, the SPICE event encompasses two different stages of elevated organic carbon and pyrite burial maintained by high nutrient fluxes to the ocean, and potentially sustained by internal marine geochemical feedbacks.
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“Model calculations suggest that oceans still would have been homogeneous in U isotope composition during the Cambrian, despite potentially greater U burial in anoxic settings that were generally more common at the time (19).”
From Atmosphere-ocean oxygen and productivity dynamics during early animal radiations (2019) · cites this paper as [19]
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“The δ238U proxy has been applied to better constrain oceanic anoxic events (OAEs) in the past and reliably recorded negative δ238U excursions at times when anoxic water masses expanded in the oceans (19–23).”
From Atmosphere-ocean oxygen and productivity dynamics during early animal radiations (2019) · cites this paper as [19]
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“Deltaic settings are oxygenated and preferentially affect the marine C and S cycle through organic carbon and pyrite sulfur burial (to a greater degree than deltaic burial affects the marine U cycle) (19).”
From Atmosphere-ocean oxygen and productivity dynamics during early animal radiations (2019) · cites this paper as [19]
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Citations
Cites
The biological control of chemical factors in the environment.
Ac, R. (1960) · PubMed · Cited by 3,989
Sedimentary organic matter preservation: an assessment and speculative synthesis
Hedges, J. I., & Keil, R. G. (1995) · Marine Chemistry · doi:10.1016/0304-4203(95)00008-f · Cited by 2,546
Langmuir, D. (1978) · Geochimica et Cosmochimica Acta · doi:10.1016/0016-7037(78)90001-7 · Cited by 2,152
Geochemistry of oceanic anoxic events
Jenkyns, H. C. (2010) · Geochemistry Geophysics Geosystems · doi:10.1029/2009gc002788 · Cited by 1,729
The oxygenation of the atmosphere and oceans
Holland, H. D. (2006) · Philosophical Transactions of the Royal Society B: Biological Sciences · doi:10.1098/rstb.2006.1838 · Cited by 1,535
Sarmiento, J. L. (2006) · Princeton University Press eBooks · doi:10.1515/9781400849079 · Cited by 1,429
Berner, R. A. (1982) · American Journal of Science · doi:10.2475/ajs.282.4.451 · Cited by 1,200
Development of a sequential extraction method for different forms of phosphorus in marine sediments
Ruttenberg, K. C. (1992) · Limnology and Oceanography · doi:10.4319/lo.1992.37.7.1460 · Cited by 1,188
Burial of organic carbon and pyrite sulfur in sediments over phanerozoic time: a new theory
Berner, R. A., & Raiswell, R. (1983) · Geochimica et Cosmochimica Acta · doi:10.1016/0016-7037(83)90151-5 · Cited by 1,044
THE EARLY HISTORY OF ATMOSPHERIC OXYGEN: Homage to Robert M. Garrels
Canfield, D. E. (2005) · Annual Review of Earth and Planetary Sciences · doi:10.1146/annurev.earth.33.092203.122711 · Cited by 1,032
Self-citationFerruginous conditions: a dominant feature of the ocean through Earth's history
Poulton, S. W., & Canfield, D. E. (2011) · Elements · doi:10.2113/gselements.7.2.107 · Cited by 1,018
Self-citationThe Absolute Chronology and Thermal Processing of Solids in the Solar Protoplanetary Disk
Connelly, J. N., Bizzarro, M., Krot, A. N., Nordlund, Å., Wielandt, D., & Ivanova, M. A. (2012) · Science · doi:10.1126/science.1226919 · Cited by 921
Self-citationHayes, J. M., Strauss, H., & Kaufman, A. J. (1999) · Chemical Geology · doi:10.1016/s0009-2541(99)00083-2 · Cited by 843
Production and accumulation of calcium carbonate in the ocean: Budget of a nonsteady state
Milliman, J. D. (1993) · Global Biogeochemical Cycles · doi:10.1029/93gb02524 · Cited by 840
Ferruginous Conditions Dominated Later Neoproterozoic Deep-Water Chemistry
Canfield, D. E., Poulton, S. W., Knoll, A. H., Narbonne, G. M., Ross, G., Goldberg, T., & Strauss, H. (2008) · Science · doi:10.1126/science.1154499 · Cited by 789
Self-citationCalibration of Sulfate Levels in the Archean Ocean
Habicht, K. S., Gade, M., Thamdrup, B., Berg, P., & Canfield, D. E. (2002) · Science · doi:10.1126/science.1078265 · Cited by 756
Self-citationUranium in the oceans: Where it goes and why
Klinkhammer, G. P., & Palmer, M. R. (1991) · Geochimica et Cosmochimica Acta · doi:10.1016/0016-7037(91)90024-y · Cited by 703
Sarmiento, J., & Gruber, N. (2006) · Princeton University Press eBooks · doi:10.2307/j.ctt3fgxqx · Cited by 613
Calibration of Sulfate Levels in the Archean Ocean
Gao, X., Thiemens, M. H., Farquhar, J. D., Jackson, T. L., Savarino, J., Airieau, S., Albarède, F., van der Hilst, R. D., & Kárason, H. (2002) · Cited by 607
COPSE: A new model of biogeochemical cycling over Phanerozoic time
Bergman, N. M. (2004) · American Journal of Science · doi:10.2475/ajs.304.5.397 · Cited by 599
Cappellen, P. V., & Ingall, E. (1994) · Paleoceanography · doi:10.1029/94pa01455 · Cited by 512
Natural fractionation of 238U/235U
Weyer, S., Anbar, A. D., Gerdes, A., Gordon, G. W., Algeo, T. J., & Boyle, E. A. (2008) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2007.11.012 · Cited by 509 · cited 5×
“Previous work suggests that the U isotope record constitutes a primary signal of global ocean chemistry, consistent with model predictions presented in this work (Brennecka et al., 2011a; Montoya-Pino et al., 2010; Weyer et al., 2008).”
BackgroundResultInfluentialWidespread iron-rich conditions in the mid-Proterozoic ocean
Planavsky, N. J., McGoldrick, P., Scott, C. T., Li, C., Reinhard, C. T., Kelly, A. E., Chu, X., Bekker, A., Love, G. D., & Lyons, T. W. (2011) · Nature · doi:10.1038/nature10327 · Cited by 505
Schauble, E. A. (2007) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2007.02.004 · Cited by 488
Gondwe, M., Krol, M., Gieskes, W. W. C., Klaassen, W., & de Baar, H. J. W. (2003) · Global Biogeochemical Cycles · doi:10.1029/2002gb001937 · Cited by 482
Oceanic Euxinia in Earth History: Causes and Consequences
Meyer, K. M., & Kump, L. R. (2008) · Annual Review of Earth and Planetary Sciences · doi:10.1146/annurev.earth.36.031207.124256 · Cited by 475
Geochemical evidence for widespread euxinia in the Later Cambrian ocean
Gill, B. C., Lyons, T. W., Young, S. A., Kump, L. R., Knoll, A. H., & Saltzman, M. R. (2011) · Nature · doi:10.1038/nature09700 · Cited by 456
Self-citationThe isotopic composition of sedimentary sulfur through time
Strauß, H. (1997) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/s0031-0182(97)00067-9 · Cited by 452
Dahl, T. W., Hammarlund, E. U., Anbar, A. D., Bond, D. P. G., Gill, B. C., Gordon, G. W., Knoll, A. H., Nielsen, A. T., Schovsbo, N. H., & Canfield, D. E. (2010) · Proceedings of the National Academy of Sciences · doi:10.1073/pnas.1011287107 · Cited by 443
Self-citationSaltzman, M. R., & Thomas, E. (2012) · The Geologic Time Scale · doi:10.1016/b978-0-444-59425-9.00011-1 · Cited by 436
Redox Stabilization of the Atmosphere and Oceans by Phosphorus-Limited Marine Productivity
Van Cappellen, P., & Ingall, E. D. (1996) · Science · doi:10.1126/science.271.5248.493 · Cited by 412
Partin, C. A., Bekker, A., Planavsky, N. J., Scott, C. T., Gill, B. C., Li, C., Podkovyrov, V., Maslov, A., Konhauser, K. O., Lalonde, S. V., et al. (2013) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2013.03.031 · Cited by 404
Self-citationMolybdenum and uranium geochemistry in continental margin sediments: Paleoproxy potential
McManus, J., Berelson, W. M., Severmann, S., Poulson, R. L., Hammond, D. E., Klinkhammer, G. P., & Holm, C. (2006) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2006.06.1564 · Cited by 399
High isotope fractionations during sulfate reduction in a low-sulfate euxinic ocean analog
Canfield, D. E., Farquhar, J. D., & Zerkle, A. L. (2010) · Geology · doi:10.1130/g30723.1 · Cited by 364
Self-citationRapid expansion of oceanic anoxia immediately before the end-Permian mass extinction
Brennecka, G. A., Herrmann, A. D., Algeo, T. J., & Anbar, A. D. (2011) · Proceedings of the National Academy of Sciences · doi:10.1073/pnas.1106039108 · Cited by 360
A reevaluation of the oceanic uranium budget for the Holocene
Dunk, R. M., Mills, R. A., & Jenkins, W. J. (2002) · Chemical Geology · doi:10.1016/s0009-2541(02)00110-9 · Cited by 341
Low-temperature isotopic fractionation of uranium
Stirling, C. H., Andersen, M. B., Potter, E.-K., & Halliday, A. N. (2007) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2007.09.019 · Cited by 337
Isotopic fractionation of oxygen and nitrogen in coastal marine sediments
Brandes, J. A., & Devol, A. H. (1997) · Geochimica et Cosmochimica Acta · doi:10.1016/s0016-7037(97)00041-0 · Cited by 335
Phanerozoic atmospheric oxygen: New results using the GEOCARBSULF model
Berner, R. A. (2009) · American Journal of Science · doi:10.2475/07.2009.03 · Cited by 314
Uranyl Incorporation into Calcite and Aragonite: XAFS and Luminescence Studies
Reeder, R. J., Nugent, M., Lamble, G. M., Tait, C. D., & Morris, D. E. (2000) · Environmental Science & Technology · doi:10.1021/es990981j · Cited by 293
Telus, M., Dauphas, N., Moynier, F., Tissot, F. L. H., Teng, F., Nábělek, P. I., Craddock, P. R., & Groat, L. A. (2012) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2012.08.024 · Cited by 290
Saltzman, M. R., Ripperdan, R. L., Brasier, M. D., Lohmann, K. C., Robison, R. A., Chang, W. T., Peng, S., Ergaliev, E. K., & Runnegar, B. (2000) · Palaeogeography, Palaeoclimatology, Palaeoecology · doi:10.1016/s0031-0182(00)00128-0 · Cited by 286
Lyons, T. W. (1997) · Geochimica et Cosmochimica Acta · doi:10.1016/s0016-7037(97)00174-9 · Cited by 277
Berry, W. B. N., & Wilde, P. (1978) · American Journal of Science · doi:10.2475/ajs.278.3.257 · Cited by 277
Pyrite and organic matter in Phanerozoic normal marine shales
Raiswell, R., & Berner, R. A. (1986) · Geochimica et Cosmochimica Acta · doi:10.1016/0016-7037(86)90252-8 · Cited by 273
Scholz, F., Hensen, C., Noffke, A., Rohde, A., Liebetrau, V., & Wallmann, K. (2011) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2011.08.007 · Cited by 262
Fry, B., Jannasch, H., Molyneaux, S. J., Wirsen, C., Muramoto, J., & King, S. (1991) · Deep Sea Research Part A Oceanographic Research Papers · doi:10.1016/s0198-0149(10)80021-4 · Cited by 250
Monteiro, F., Pancost, R. D., Ridgwell, A. J., & Yannick Donnadieu, A. (2012) · Paleoceanography · doi:10.1029/2012pa002351 · Cited by 249
The Ordovician Biodiversification: revolution in the oceanic trophic chain
Servais, T., Lehnert, O., Li, J., Mullins, G. L., Munnecke, A., Nützel, A., & Vecoli, M. (2008) · Lethaia · doi:10.1111/j.1502-3931.2008.00115.x · Cited by 221
Tetravalent Uranium in Calcite
Sturchio, N. C., Antonio, M. R., Soderholm, L., Sutton, S. R., & Brannon, J. C. (1998) · Science · doi:10.1126/science.281.5379.971 · Cited by 218
Green rust formation controls nutrient availability in a ferruginous water column
Zegeye, A., Bonneville, S., Benning, L. G., Sturm, A., Fowle, D. A., Jones, C., Canfield, D. E., Ruby, C., MacLean, L. C., Nomosatryo, S., et al. (2012) · Geology · doi:10.1130/g32959.1 · Cited by 214
Self-citationRomaniello, S. J., Herrmann, A. D., & Anbar, A. D. (2013) · Chemical Geology · doi:10.1016/j.chemgeo.2013.10.002 · Cited by 212
Uranium Isotope Fractionation during Adsorption to Mn-Oxyhydroxides
Brennecka, G. A., Wasylenki, L. E., Bargar, J., Weyer, S., & Anbar, A. D. (2011) · Environmental Science & Technology · doi:10.1021/es103061v · Cited by 205
Uranium redox transition pathways in acetate-amended sediments
Bargar, J., Williams, K. H., Campbell, K. M., Long, P. E., Stubbs, J. E., Suvorova, E. I., Lezama-Pacheco, J. S., Alessi, D. S., Stylo, M., Webb, S. M., et al. (2013) · Proceedings of the National Academy of Sciences · doi:10.1073/pnas.1219198110 · Cited by 196
Nielsen, A. T., & Schovsbo, N. H. (2011) · Earth-Science Reviews · doi:10.1016/j.earscirev.2010.12.004 · Cited by 194
Redfield revisited: 2. What regulates the oxygen content of the atmosphere?
Lenton, T. M., & Watson, A. J. (2000) · Global Biogeochemical Cycles · doi:10.1029/1999gb900076 · Cited by 192 · cited 1×
“…where enhanced organic carbon burial into sediments represents a source of O2 to the atmosphere, thereby reducing anoxia in a net negative feedback (Lenton and Watson, 2000; Van Cappellen and Ingall, 1994), thought (for example) to have been relevant to Cretaceous oceanic anoxic events (Handoh…”
BackgroundSelf-citationLimits for Combustion in Low O 2 Redefine Paleoatmospheric Predictions for the Mesozoic
Belcher, C. M., & McElwain, J. C. (2008) · Science · doi:10.1126/science.1160978 · Cited by 190
Montoya-Pino, C., Weyer, S., Anbar, A. D., Pross, J., Oschmann, W., van de Schootbrugge, B., & Arz, H. W. (2010) · Geology · doi:10.1130/g30652.1 · Cited by 190
Pulse of atmospheric oxygen during the late Cambrian
Saltzman, M. R., Young, S. A., Kump, L. R., Gill, B. C., Lyons, T. W., & Runnegar, B. (2011) · Proceedings of the National Academy of Sciences · doi:10.1073/pnas.1011836108 · Cited by 188 · cited 7×
“The SPICE event is thought to represent a 2–4 Myr interval when anoxic and sulfidic water masses expanded over the shallow ocean, contemporaneous with enhanced burial of organic carbon (Gill et al., 2011; Saltzman et al., 2011), as well as pyrite and molybdenum (Gill et al.”
BackgroundInfluentialSelf-citationKinetics of Uranium(VI) Reduction by Hydrogen Sulfide in Anoxic Aqueous Systems
Hua, B., Xu, H., Terry, J., & Deng, B. (2006) · Environmental Science & Technology · doi:10.1021/es051804n · Cited by 159
Saltzman, M. R., Cowan, C. A., Runkel, A. C., Runnegar, B. N., Stewart, M. C., & Palmer, A. R. (2004) · Journal of Sedimentary Research · doi:10.1306/120203740366 · Cited by 158
Gill, B. C., Lyons, T. W., & Frank, T. D. (2008) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2008.07.001 · Cited by 155
Self-citationControls on Mo isotope fractionations in a Mn-rich anoxic marine sediment, Gullmar Fjord, Sweden
Goldberg, T., Archer, C., Vance, D., Thamdrup, B., McAnena, A., & Poulton, S. W. (2012) · Chemical Geology · doi:10.1016/j.chemgeo.2011.12.020 · Cited by 153
Tryon, M. D., Henry, P., Çağatay, M. N., Zitter, T. A. C., Géli, L., Gasperini, L., Burnard, P. G., Bourlange, S., & Grall, C. (2010) · Geochemistry Geophysics Geosystems · doi:10.1029/2010gc003177 · Cited by 145
Reductive Immobilization of Uranium(VI) by Amorphous Iron Sulfide
Hua, B., & Deng, B. (2008) · Environmental Science & Technology · doi:10.1021/es801225z · Cited by 144
Handoh, I. C., & Lenton, T. M. (2003) · Global Biogeochemical Cycles · doi:10.1029/2003gb002039 · Cited by 141
Self-citationColman, A. S., & Holland, H. D. (2000) · SEPM (Society for Sedimentary Geology) eBooks · doi:10.2110/pec.00.66.0053 · Cited by 141
Uranium diagenesis in sediments underlying bottom waters with high oxygen content
Morford, J. L., Martin, W. R., & Carney, C. M. (2009) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2009.02.014 · Cited by 132
KOUCHINSKY, A., BENGTSON, S., GALLET, Y., KOROVNIKOV, I., PAVLOV, V., RUNNEGAR, B., SHIELDS, G., VEIZER, J., YOUNG, E., & ZIEGLER, K. (2008) · Geological Magazine · doi:10.1017/s0016756808004913 · Cited by 125
Ahlberg, P., Axheimer, N., Babcock, L. E., Eriksson, M. E., Schmitz, B., & Terfelt, F. (2009) · Lethaia · doi:10.1111/j.1502-3931.2008.00127.x · Cited by 121
Isotopic composition (238U/235U) of some commonly used uranium reference materials
Condon, D. J., McLean, N. M., Noble, S. R., & Bowring, S. A. (2010) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2010.09.019 · Cited by 120
Clark, S. K., & Johnson, T. M. (2008) · Environmental Science & Technology · doi:10.1021/es801814v · Cited by 115
Kitchen, J. W., Johnson, T. M., Bullen, T. D., Zhu, J., & Raddatz, A. L. (2012) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2012.04.049 · Cited by 111
Gradstein, F. M. (2006) · The Paleontological Society Papers · doi:10.1017/s1089332600001376 · Cited by 109
Variations in 238U/235U in uranium ore deposits: Isotopic signatures of the U reduction process?
Bopp, C. J., Lundstrom, C. C., Johnson, T. M., & Glessner, J. J. G. (2009) · Geology · doi:10.1130/g25550a.1 · Cited by 108
Bopp, C. J., Lundstrom, C. C., Johnson, T. M., Sanford, R. A., Long, P. E., & Williams, K. H. (2010) · Environmental Science & Technology · doi:10.1021/es100643v · Cited by 105
Carbon isotope composition of lower palaeozoic kerogen: Effects of maturation
Buchardt, B., Clausen, J. V., & Thomsen, E. (1986) · Organic Geochemistry · doi:10.1016/0146-6380(86)90016-1 · Cited by 104
Redox dynamics in the Chesapeake Bay: The effect on sediment/water uranium exchange
Shaw, T. J., Sholkovitz, E. R., & Klinkhammer, G. P. (1994) · Geochimica et Cosmochimica Acta · doi:10.1016/0016-7037(94)90173-2 · Cited by 104
Buchardt, B., & Schovsbo, N. H. (1997) · Research at the University of Copenhagen (University of Copenhagen) · Cited by 82
In search of live 247Cm in the early solar system
Stirling, C. H., Halliday, A. N., & Porcelli, D. (2005) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2004.06.034 · Cited by 75
Uranium enrichment shorewards in black shales: A case study from the Scandinavian Alum Shale
Schovsbo, N. H. (2002) · GFF · doi:10.1080/11035890201242107 · Cited by 75
Alkenone producers during late Oligocene–early Miocene revisited
Plancq, J., Grossi, V., Henderiks, J., Simon, L., & Mattioli, E. (2011) · Paleoceanography · doi:10.1029/2011pa002164 · Cited by 73
Hetzel, R., Echtler, H., Seifert, W., Schulte, B., & Ivanov, K. S. (1998) · Geological Society of America Bulletin · doi:10.1130/0016-7606(1998)110 · Cited by 58
Sulfur diagenesis and burial on the Amazon shelf: Major control by physical sedimentation processes
Aller, R. C., & Blair, N. E. (1996) · Geo-Marine Letters · doi:10.1007/bf01218830 · Cited by 51
Middle Archean continent formation by crustal delamination
Zegers, T. E., & van Keken, P. E. (2001) · Geology · doi:10.1130/0091-7613(2001)029
Self-citationSibley, D. F., Dedoes, R. E., & Bartlett, T. R. (1987) · Geology · doi:10.1130/0091-7613(1987)15
Research works printed but not linked: 2
- Derry, 2013, Resolving inconsistent sedimentary carbon mass balances: implications for ancient C and S cycles, Mineral. Mag., 77, 978
- Garrels, 1974, Cycling of carbon, sulfur, and oxygen through geologic time, vol. 5, 303
Cited by
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Trace elements at the intersection of marine biological and geochemical evolution
Robbins, L. J., Lalonde, S. V., Planavsky, N. J., Partin, C. A., Reinhard, C. T., Kendall, B., Scott, C., Hardisty, D. S., Gill, B. C., Alessi, D. S., et al. (2016) · Earth-Science Reviews · doi:10.1016/j.earscirev.2016.10.013 · Cited by 227
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Andersen, M. B., Stirling, C. H., & Weyer, S. (2017) · Reviews in Mineralogy and Geochemistry · doi:10.2138/rmg.2017.82.19 · Cited by 218
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Metadata
- Authors
- Dahl, T. W., Boyle, R. A., Canfield, D. E., Connelly, J. N., Gill, B. C., Lenton, T. M., & Bizzarro, M.
- Affiliations
- University of Copenhagen (DK)
- University of Southern Denmark (DK)
- Virginia Tech (US)
- University of Exeter (GB)
- Corresponding author
- Dahl, Tais W.
- ORCID
- Venue
- Earth and Planetary Science Letters
- Publisher
- Elsevier BV
- Published
- 2014-09
- Volume
- 401
- Pages
- 313-326
- ISSN
- 0012-821X (ISSN-L)
- PMC
- PMC4326682
- OpenAlex
- W2067022994
- Cited by
- 172
- References
- 86
- Citations by year
- 2026: 11 · 2025: 13 · 2024: 11 · 2023: 16 · 2022: 17 · 2021: 19 · 2020: 12 · 2019: 16 · 2018: 23 · 2017: 14 · 2016: 11 · 2015: 8 · 2014: 1
- FWCI
- 8.27
- Type
- journal article
- Language
- en
- Open access
- green
- www.ncbi.nlm.nih.gov
- Locations
- Earth and Planetary Science Letters (publishedVersion)
- PubMed (publishedVersion)
- Europe PMC (PubMed Central) (acceptedVersion)
- PubMed Central (acceptedVersion)
- Research at the University of Copenhagen (University of Copenhagen) (submittedVersion)
- University of Southern Denmark Research Portal (University of Southern Denmark) (submittedVersion)
- Funders
- National Science Foundation (EAR-0418270, EAR-0719911)
- Villum Foundation (VKR023127)
- Danish National Research Foundation (DNRF-53, DNRF97)
- European Research Council (616027-STARDUST2ASTEROIDS)
- ERC
- Topics
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geological and Geochemical Analysis
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
- Keywords
- uranium isotopes, Late Cambrian, ocean anoxia, euxinia, organic carbon burial, atmospheric oxygenation, carbon isotopes, sulfur isotopes, sulfate depletion, paleo-oxygenation
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 ›
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