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Reconstruction of early Cambrian ocean chemistry from Mo isotopes

Wen, Hanjie, Fan, Haifeng, Zhang, Yuxu, Cloquet, Christophe, Carignan, Jean·2015·Geochimica et Cosmochimica Acta

DOI 10.1016/j.gca.2015.05.008

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Show all 0 references

Research works printed but not linked: 51

Amthor, 2003, Extinction of Cloudina and Namacalathus at the Precambrian–Cambrian boundary in Oman, Geology, 31, 431, 10.1130/0091-7613(2003)031<0431:EOCANA>2.0.CO;2 · DOI
Anbar, 2007, Metal stable isotopes in paleoceanography, Annu. Rev. Earth Planet. Sci., 35, 717, 10.1146/annurev.earth.34.031405.125029 · DOI
Barling, 2004, Molybdenum isotope fractionation during adsorption by manganese oxides, Earth Planet. Sci. Lett., 217, 315, 10.1016/S0012-821X(03)00608-3 · DOI
Barling, 2001, Natural mass-dependent variations in the isotopic composition of molybdenum, Earth Planet. Sci. Lett., 193, 447, 10.1016/S0012-821X(01)00514-3 · DOI
Berner, 2003, Phanerozoic atmospheric oxygen, Annu. Rev. Earth Planet. Sci., 31, 105, 10.1146/annurev.earth.31.100901.141329 · DOI · Paper page
Brasier, 1990, The carbon- and oxygen-isotopic record of the Ediacaran–Cambrian boundary interval in China and Iran and their correlation, Geol. Mag., 127, 319, 10.1017/S0016756800014886 · DOI
Calvert, 1993, Geochemistry of recent oxic and anoxic marine sediments: implications for the geological record, Mar. Geol., 113, 67, 10.1016/0025-3227(93)90150-T · DOI · Paper page
Condie, 2001, Precambrian superplumes and supercontinents: a record in black shales, carbon isotopes, and paleoclimates?, Precambr. Res., 106, 239, 10.1016/S0301-9268(00)00097-8 · DOI
Crusius, 1996, Rhenium and molybdenum enrichments in sediments as indicators of oxic, suboxic and sulfidic conditions of deposition, Earth Planet. Sci. Lett., 145, 65, 10.1016/S0012-821X(96)00204-X · DOI
Dahl, 2010, The behavior of molybdenum and its isotopes across the chemocline of sulfidic Lake Cadagno, Switzerland, Geochim. Cosmochim. Acta, 74, 144, 10.1016/j.gca.2009.09.018 · DOI
Goldberg, 2007, Reconstructing marine redox conditions for the Early Cambrian Yangtze Platform: evidence from biogenic sulphur and organic carbon isotopes, Palaeogeogr. Palaeoclimatol. Palaeoecol., 254, 175, 10.1016/j.palaeo.2007.03.015 · DOI
Goldberg, 2009, Mo isotope fractionation during adsorption of Fe (oxyhydr)oxides, Geochim. Cosmochim. Acta, 73, 6502, 10.1016/j.gca.2009.08.004 · DOI · Paper page
Greber, 2012, Δ98/95Mo values and molybdenum concentration data for NIST SRM 610, 612 and 3134: towards a common protocol for reporting Mo data, Geostand. Geoanal. Res., 36, 291, 10.1111/j.1751-908X.2012.00160.x · DOI
Guo, 2007, Carbon isotopic evolution of the terminal Neoproterozoic and early Cambrian: evidence from the Yangtze Platform, South China, Palaeogeogr. Palaeoclimatol. Palaeoecol., 254, 140, 10.1016/j.palaeo.2007.03.014 · DOI
Helz, 2011, New model for molybdenum behavior in euxinic waters, Chem. Geol., 284, 323, 10.1016/j.chemgeo.2011.03.012 · DOI · Paper page
Herrmann, 2012, Anomalous molybdenum isotope trends in Upper Pennsylvanian euxinic facies: significance for the use of δ98Mo as a global marine proxy, Chem. Geol., 324–325, 87, 10.1016/j.chemgeo.2012.05.013 · DOI
Jiang, 2009, Early Cambrian ocean anoxia in South China, Nature, 459, E5, 10.1038/nature08048 · DOI
Kashiwabara, 2011, Molecular-scale mechanisms of distribution and isotopic fractionation of molybdenum between seawater and ferromanganese oxides, Geochim. Cosmochim. Acta, 75, 5762, 10.1016/j.gca.2011.07.022 · DOI
Lehmann, 2007, Highly metalliferous carbonaceous shale and Early Cambrian seawater, Geology, 35, 403, 10.1130/G23543A.1 · DOI
McManus, 2006, Molybdenum and uranium geochemistry in continental margin sediments: paleoproxy potential, Geochim. Cosmochim. Acta, 70, 4643, 10.1016/j.gca.2006.06.1564 · DOI
Meyers, 1992, Geochemistry of metalliferous black shales, Chem. Geol., 99, 65, 10.1016/0009-2541(92)90027-3 · DOI
Morford, 2005, Diagenesis of oxyanions (V, U, Re, and Mo) in pore waters and sediments from a continental margin, Geochim. Cosmochim. Acta, 69, 5021, 10.1016/j.gca.2005.05.015 · DOI
Morford, 2009, A model for uranium, rhenium, and molybdenum diagenesis in marine sediments based on results from coastal locations, Geochim. Cosmochim. Acta, 73, 2938, 10.1016/j.gca.2009.02.029 · DOI
Nägler, 2014, Proposal for an international molybdenum isotope measurement standard and data representation, Geostand. Geoanal. Res., 38, 149, 10.1111/j.1751-908X.2013.00275.x · DOI · Paper page
Nakagawa, 2012, The molybdenum isotopic composition of the modern ocean, Geochem. J., 46, 131, 10.2343/geochemj.1.0158 · DOI
Och, 2013, Redox changes in Early Cambrian black shales at Xiaotan section, Yunnan Province, South China, Precambr. Res., 225, 166, 10.1016/j.precamres.2011.10.005 · DOI
Orberger, 2003, Se, As, Mo, Ag, Cd, In, Sb, Pt, Au, Tl, Re traces in biogenic and abiogenic sulfides from Black Shales (Selwyn Basin, Yukon territories, Canada): a nuclear microprobe study, Nucl. Instrum. Methods Phys. Res., Sect. B, 210, 441, 10.1016/S0168-583X(03)01073-5 · DOI
Partin, 2013, Large-scale fluctuations in Precambrian atmospheric and oceanic oxygen levels from the record of U in shales, Earth Planet. Sci. Lett., 369–370, 284, 10.1016/j.epsl.2013.03.031 · DOI · Paper page
Pi, 2013, Trace and rare earth element geochemistry of black shale and kerogen in the early Cambrian Niutitang Formation in Guizhou province, South China: constraints for redox environments and origin of metal enrichments, Precambr. Res., 225, 218, 10.1016/j.precamres.2011.07.004 · DOI · Paper page
Pietruszka, 2006, Determination of mass-dependent molybdenum isotopic variations by MC-ICP-MS: an evaluation of matrix effects, Chem. Geol., 225, 121, 10.1016/j.chemgeo.2005.09.002 · DOI
Poulson, 2006, Authigenic molybdenum isotope signatures in marine sediments, Geology, 34, 617, 10.1130/G22485.1 · DOI
Poulson, 2009, Molybdenum behavior during early diagenesis: insights from Mo isotopes, Geochem. Geophys. Geosyst., 10, Q06010
Poulton, 2005, Development of a sequential extraction procedure for iron: implications for iron partitioning in continentally derived particulates, Chem. Geol., 214, 209, 10.1016/j.chemgeo.2004.09.003 · DOI
Reitz, 2007, Atypical Mo isotope signatures in eastern Mediterranean sediments, Chem. Geol., 245, 1, 10.1016/j.chemgeo.2007.06.018 · DOI
Schröder, 2004, Stratigraphy and environmental conditions of the terminal Neoproterozoic–Cambrian Period in Oman: evidence from sulphur isotopes, J. Geol. Soc., 161, 489, 10.1144/0016-764902-062 · DOI
Shen, 2000, New C isotope stratigraphy from southwest China: implications for the placement of the Precambrian–Cambrian boundary on the Yangtze Platform and global correlations, Geology, 28, 623, 10.1130/0091-7613(2000)28<623:NCISFS>2.0.CO;2 · DOI
Shields, 2001, Diagenetic constraints on the use of cerium anomalies as palaeoseawater redox proxies: an isotopic and REE study of Cambrian phosphorites, Chem. Geol., 175, 29, 10.1016/S0009-2541(00)00362-4 · DOI
Shields-Zhou, 2011, The case for a Neoproterozoic Oxygenation Event: geochemical evidence and biological consequences, GSA Today, 21, 4, 10.1130/GSATG102A.1 · DOI
Siebert, 2003, Molybdenum isotope records as a potential new proxy for paleoceanography, Earth Planet. Sci. Lett., 211, 159, 10.1016/S0012-821X(03)00189-4 · DOI
Siebert, 2006, Molybdenum isotope signatures in continental margin marine sediments, Earth Planet. Sci. Lett., 241, 723, 10.1016/j.epsl.2005.11.010 · DOI
Steiner, 2001, Submarine hydrothermal exhalative ore layers in black shales from South China and associated fossils – insights into a Lower Cambrian facies and bio-evolution, Palaeogeogr. Palaeoclimatol. Palaeoecol., 169, 165, 10.1016/S0031-0182(01)00208-5 · DOI
Tribovillard, 2012, Analysis of marine environmental conditions based on molybdenum–uranium covariation – applications to Mesozoic paleoceanography, Chem. Geol., 324–325, 46, 10.1016/j.chemgeo.2011.09.009 · DOI
Voegelin, 2009, Molybdenum isotopic composition of modern and carboniferous carbonates, Chem. Geol., 265, 488, 10.1016/j.chemgeo.2009.05.015 · DOI
Wen, 2010, Isotopic delta values of molybdenum standard reference and prepared solutions measured by MC-ICP-MS: proposition for delta zero and secondary references, J. Anal. At. Spectrom., 25, 716, 10.1039/b921060a · DOI
Wen, 2011, Molybdenum isotopic records across the Ediacaran Cambrian boundary, Geology, 39, 775, 10.1130/G32055.1 · DOI · Paper page
Xu, 2011, Re–Os age of polymetallic Ni–Mo–PGE–Au mineralization in Early Cambrian Black Shales of South China – a reassessment, Econ. Geol., 106, 511, 10.2113/econgeo.106.3.511 · DOI
Xu, 2012, Mo isotope and trace element patterns of Lower Cambrian black shales in South China: multi-proxy constraints on the paleoenvironment, Chem. Geol., 318, 45, 10.1016/j.chemgeo.2012.05.016 · DOI
Zhang, 2009, Chemical pretreatment methods for measurement of Mo isotope ratio on geological samples, Chin. J. Anal. Chem., 37, 216
Zheng, 2000, Authigenic molybdenum formation in marine sediments: a link to pore water sulfide in the Santa Barbara Basin, Geochim. Cosmochim. Acta, 64, 4165, 10.1016/S0016-7037(00)00495-6 · DOI
Zheng, 2002, Remobilization of authigenic uranium in marine sediments by bioturbation, Geochim. Cosmochim. Acta, 66, 1759, 10.1016/S0016-7037(01)00886-9 · DOI · Paper page
Zhu, 2007, Integrated Ediacaran(Sinian) chronostratigraphy of South China, Palaeogeogr. Palaeoclimatol. Palaeoecol., 254, 7, 10.1016/j.palaeo.2007.03.025 · DOI

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Background
Vanadium isotope evidence for widespread marine oxygenation from the late Ediacaran to early Cambrian
Wei, W., Chen, X., Ling, H., Wu, F., Dong, L.-H., Pan, S., Jing, Z., & Huang, F. (2022) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2022.117942 · Cited by 31
“…lower Niutitang, and lower Shuijingtuo Formations suggest that the ocean kept extensively oxygenated since ca. 551 Ma, and possibly reached the modern oxygenation level at ca. 521 Ma, in good agreement with the Mo and U isotope evidence (e.g., Wen et al., 2015; Chen et al., 2015; Wei et al., 2021).”
Reconstruction of oceanic redox structures during the Ediacaran-Cambrian transition in the Yangtze Block of South China: Implications from Mo isotopes and trace elements
Wu, Y., Tian, H., Li, J., Li, T., & Ji, S. (2021) · Precambrian Research · doi:10.1016/j.precamres.2021.106181 · Cited by 23
Anomalously high enrichment of mercury in early Cambrian black shales in South China
Zhu, G., Zhao, K., Li, T., Zhang, Z., Tang, S., & Wang, P. (2021) · Journal of Asian Earth Sciences · doi:10.1016/j.jseaes.2021.104794 · Cited by 25
Coupling of the redox history and enrichment of Ni-Mo in black shale during the early Cambrian: Constraints from S-Fe isotopes and trace elements of pyrite, South China
Yang, Z., Wu, P., Fu, Y., Qiao, W.-L., Qin, Y.-J., Li, C., Xia, P., Guo, C., Long, X., & Wu, L. (2022) · Ore Geology Reviews · doi:10.1016/j.oregeorev.2022.104749 · Cited by 22
Oceanic chemistry recorded by cherts during the early Cambrian Explosion, South China
Zhang, H., Fan, H., Wen, H., Zhu, X., & Tian, S. (2020) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/j.palaeo.2020.109961 · Cited by 22
Self-citation
Large Zn isotope variations in the Ni Mo polymetallic sulfide layer in the lower Cambrian, South China
Fan, H.-F., Zhang, H., Xiao, C., Pašava, J., Han, T., Zhou, T., & Wen, H. (2020) · Gondwana Research · doi:10.1016/j.gr.2020.04.009 · Cited by 22
Self-citation
High-resolution paired carbon isotopic records from the Meishucun section in South China: Implications for carbon cycling and environmental changes during the Ediacaran-Cambrian transition
Zhang, X., Zhou, X., & Hu, D. (2019) · Precambrian Research · doi:10.1016/j.precamres.2019.105561 · Cited by 24
The Sirius Passet Lagerstätte of North Greenland—A geochemical window on early Cambrian low‐oxygen environments and ecosystems
Hammarlund, E. U., Smith, M. P., Rasmussen, J. A., Nielsen, A. T., Canfield, D. E., & Harper, D. A. T. (2018) · Geobiology · doi:10.1111/gbi.12315 · Cited by 21
“…data on early Cambrian environments, from which both recurrent water-column stratification (Canfield et al., 2008; Cremonese et al., 2013; Feng, Li, Huang, Chang, & Chu, 2014; Hammarlund et al., 2017; Wen, Fan, Zhang, Cloquet, & Carignan, 2015) and oxygenation (Chen et al., 2015) are inferred.”
Background
Cr isotopic composition of the Laobao cherts during the Ediacaran–Cambrian transition in South China
Huang, J., Liu, J., Zhang, Y., Chang, H., Shen, Y., Huang, F., & Qin, L. (2018) · Chemical Geology · doi:10.1016/j.chemgeo.2018.02.011 · Cited by 26
Self-citation
Redox history of the Three Gorges region during the Ediacaran and Early Cambrian as indicated by the Fe isotope
Sawaki, Y., Tahata, M., Komiya, T., Hirata, T., Han, J., & Shu, D. (2017) · Geoscience Frontiers · doi:10.1016/j.gsf.2017.02.005 · Cited by 27
16 Good Golly, Why Moly? THE STABLE ISOTOPE GEOCHEMISTRY OF MOLYBDENUM
Kendall, B., Dahl, T. W., & Anbar, A. D. (2017) · De Gruyter eBooks · doi:10.1515/9783110545630-017 · Cited by 16
“The δ98Mo values in these 1282 ORMs are persistently high (2.1‰) and close to modern seawater (2.3‰), suggesting that 1283 expanded ocean anoxia was limited to the short duration (~100-200 kyr) of the warming events.”
BackgroundInfluential
High-precision molybdenum isotope analysis of low-Mo igneous rock samples by MC–ICP–MS
Fan, J., Li, J., Wang, Q., Zhang, L., Zhang, J., Zeng, X.-L., Ma, L., & Wang, Z. (2020) · Chemical Geology · doi:10.1016/j.chemgeo.2020.119648 · Cited by 27
Preliminary exploration of molybdenum isotope fractionation during coprecipitation of molybdate with abiotic and microbial calcite
Chen, X., Romaniello, S. J., & Anbar, A. D. (2021) · Chemical Geology · doi:10.1016/j.chemgeo.2021.120102 · Cited by 25
Enhanced weathering as a trigger for the rise of atmospheric O2 level from the late Ediacaran to the early Cambrian
Li, W.-P., Zhao, Y.-Y., Zhao, M.-Y., Zha, X.-P., & Zheng, Y.-F. (2019) · Scientific Reports · doi:10.1038/s41598-019-47142-3 · Cited by 19
Tracking the evolution of seawater Mo isotopes through the Ediacaran–Cambrian transition
Ye, Y., Wang, H., Wang, X., Zhai, L., Wu, C., Canfield, D. E., & Zhang, S. (2020) · Precambrian Research · doi:10.1016/j.precamres.2020.105929 · Cited by 20
Mo marine geochemistry and reconstruction of ancient ocean redox states
Cheng, M., Li, C., Zhou, L., & Xie, S. (2015) · Science China Earth Sciences · doi:10.1007/s11430-015-5177-4 · Cited by 23
Co-evolution of life and environment during the early Cambrian of South China: Implications for organic matter enrichment
Liu, W., Gao, P., Lash, G. G., & Xiao, X. (2025) · Earth-Science Reviews · doi:10.1016/j.earscirev.2025.105294 · Cited by 16
Marine chemical structure during the Cambrian explosion
Xiao, W., Cao, J., Wang, X., Xiao, D., Shi, C., & Zhang, S. (2024) · Earth-Science Reviews · doi:10.1016/j.earscirev.2024.104716 · Cited by 21
Chemostratigraphy Across the Cretaceous‐Paleogene (K‐Pg) Boundary
Sial, A., Chen, J.-B., Lacerda, L. D., Frei, R., Higgins, J., Tewari, V. C., Gaucher, C., Ferreira, V., Cirilli, S., Korte, C., et al. (2018) · Chemostratigraphy Across Major Chronological Boundaries · doi:10.1002/9781119382508.ch12 · Cited by 18
Rare earth element enrichment in sedimentary phosphorites formed during the Precambrian–Cambrian transition, Southwest China
Xing, J., Jiang, Y., Xian, H.-Y., Yang, W.-B., Yang, Y.-P., Niu, H.-C., He, H.-T., & Zhu, J.-X. (2023) · Geoscience Frontiers · doi:10.1016/j.gsf.2023.101766 · Cited by 17
Copper, zinc, chromium and osmium isotopic compositions of the Teplá-Barrandian unit black shales and implications for the composition and oxygenation of the Neoproterozoic-Cambrian ocean
Ackerman, L., Pašava, J., Šípková, A., Martínková, E., Haluzová, E., Rodovská, Z., & Chrastný, V. (2019) · Chemical Geology · doi:10.1016/j.chemgeo.2019.05.013 · Cited by 22
Early Cambrian sedimentary rocks in South China: A link between oceanic oxygenation and biological explosion
Zhao, B., Long, X., & Chang, C. (2024) · Earth-Science Reviews · doi:10.1016/j.earscirev.2024.104708 · Cited by 17
Mercury isotopes record development and attenuation of photic zone euxinia during the earliest Cambrian
Zhao, K., Zhu, G.-Y., Zheng, W., Sun, G.-Y., Li, T., & Zhang, Z.-Y. (2023) · Global and Planetary Change · doi:10.1016/j.gloplacha.2023.104214 · Cited by 16
Trace element enrichment mechanisms in black shales during the early cambrian (ca. 521–514 Ma), South China
Wang, Z., Tan, J.-Q., Hilton, J., Dick, J. M., & Wen, Z. (2023) · Marine and Petroleum Geology · doi:10.1016/j.marpetgeo.2022.106083 · Cited by 16
Precise Mo isotope ratio measurements of low-Mo (ng g −1 ) geological samples using MC-ICP-MS
Liu, J., Wen, H., Zhang, Y., Fan, H., & Zhu, C. (2016) · Journal of Analytical Atomic Spectrometry · doi:10.1039/c6ja00006a · Cited by 27
Self-citation
Nitrogen cycling and marine redox evolution during the Ediacaran–Cambrian transition
Chang, C., & Algeo, T. J. (2024) · Global and Planetary Change · doi:10.1016/j.gloplacha.2024.104679 · Cited by 13
Assessment of the Effect of Organic Matter on Rare Earth Elements and Yttrium Using the Zhijin Early Cambrian Phosphorite as an Example
Wu, S., Yang, H.-Y., Fan, H.-F., Xia, Y., Meng, Q.-T., He, S., & Gong, X.-X. (2022) · Minerals · doi:10.3390/min12070876 · Cited by 14
Self-citation
Inverse Mo versus U isotope correlation of Early Cambrian highly metalliferous black shales in South China indicates synsedimentary metal enrichment from a near-modern ocean
Xu, L., Lehmann, B., Weyer, S., Wen, H., Mao, J., Neubert, N., & Jian, W. (2023) · Mineralium Deposita · doi:10.1007/s00126-023-01201-y · Cited by 19
“Molybdenum isotope measurements were done at the Institute of Geochemistry in Guiyang, China, with a Nu Plasma MC-ICP-MS following the methods of Wen et al. (2010, 2015).”
InfluentialSelf-citation
Petrological and Ni-Mo isotopic evidence for the genesis of the Ni- and Mo-sulfide extremely enriched early Cambrian black shale from Southwest China
Zhang, Y.-N., Wang, Z.-W., Yang, X., Huang, L., Li, Y., & Qin, L. (2022) · Chemical Geology · doi:10.1016/j.chemgeo.2022.120812 · Cited by 13
Self-citation
Molybdenum isotopic evidence for anoxic marine conditions during the end-Permian mass extinction
Zhang, Y., Wen, H., Zhu, C., Fan, H., Xiao, J., & Wen, J. L. (2021) · Chemical Geology · doi:10.1016/j.chemgeo.2021.120259 · Cited by 16
Self-citation
Multiple Proxies on the Paleoenvironment of the Early Cambrian Marine Black Rock Series in the Tarim Basin, NW China: Molybdenum Isotope and Trace Element Evidence
Yao, C., Guo, W., Liu, J.-N., & Li, H. (2017) · International Journal of Geosciences · doi:10.4236/ijg.2017.88055 · Cited by 12
“Wen et al. (2015) reported δ98/95Mo values of early Cambrian black shales, which have a wide range of δ98/95Mo values (0.27‰ - 1.79‰) in carbonaceous shales and cherts (interval 1), and are from 0.11‰ to1.”
BackgroundMethodInfluential
Mass Extinction Coincided With Expanded Continental Margin Euxinia During the Cambrian Age 4
Chang, C., Hu, W., Huang, K., Wang, Z., & Zhang, X. (2023) · Geophysical Research Letters · doi:10.1029/2023gl105560 · Cited by 13
“…black shales favoring euxinic sedimentary environments and require detailed investigation of local redox conditions using multiple proxies, such as iron speciation and redox-sensitive trace elements (e.g., Chen et al., 2015; Cheng et al., 2016; Ostrander et al., 2019; Wen et al., 2015).”
BackgroundMethod
Multiple Controls on Organic Matter Accumulation in the Intraplatform Basin of the Early Cambrian Yangtze Platform, South China
Zhang, Q., Liu, E.-T., Pan, S., Wang, H., Jing, Z., Zhao, Z.-F., & Zhu, R. (2023) · Journal of Marine Science and Engineering · doi:10.3390/jmse11101907 · Cited by 11
Expanded deepwater euxinia recorded in the Ediacaran–Cambrian boundary interval in South China
Yang, H., Yang, L., & Zhou, M. (2022) · Journal of Asian Earth Sciences · doi:10.1016/j.jseaes.2022.105192 · Cited by 14
Controls of Distinct Mineral Compositions on Pore Structure in Over-Mature Shales: A Case Study of Lower Cambrian Niutitang Shales in South China
Niu, X.-G., Yan, D., Hu, M.-Y., Liu, Z., Wei, X., & Zuo, M.-T. (2021) · Minerals · doi:10.3390/min11010051 · Cited by 11
Elemental and isotopic compositions of trench-slope black shales, Bohemian Massif, with implications for oceanic and atmospheric oxygenation in early Cambrian
Pašava, J., Ackerman, L., Žák, J., Veselovský, F., Creaser, R., Svojtka, M., Luais, B., Pour, O., Šebek, O., Trubač, J., et al. (2021) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/j.palaeo.2020.110195 · Cited by 10
Developing a Rate Law for Ce(III) Oxidation by Manganese Oxides
Xu, H., Liu, P., Zhao, S., Wen, Y., & Tang, Y. (2025) · Environmental Science & Technology · doi:10.1021/acs.est.4c12688 · Cited by 11
Extensive Oceanic Anoxia during the early Cambrian: Evidence from Mn-Carbonate and Alabandite Deposition in the Northwestern Yangtze margin, South China
Zhang, Y., Liao, Z., Huang, Q., Xu, Z., Lei, L., & Pan, J. (2024) · Palaeogeography, Palaeoclimatology, Palaeoecology · doi:10.1016/j.palaeo.2024.112549 · Cited by 9
Self-citation
Influence of goethite nanophase on rare-earth element patterns and enrichment in marine phosphates during early diagenesis
Xing, J., Li, S., Wei, H.-Y., Xi, J.-X., Lin, X.-J., Yang, Y.-P., Xian, H.-Y., Tan, W., Wei, J.-M., & Zhu, J.-X. (2024) · Chemical Geology · doi:10.1016/j.chemgeo.2024.122029 · Cited by 9
Multiple ocean oxygenation events during the Ediacaran Period: Mo isotope evidence from the Nanhua Basin, South China
Yuan, L., Zhou, Y., Chen, X., Zhu, M., Poulton, S. W., Tian, Z., Li, D., THIRLWALL, M. F., & Shields, G. (2023) · Precambrian Research · doi:10.1016/j.precamres.2023.107004 · Cited by 12
Reconstruction of the Ediacaran sulfur cycle and oceanic redox evolution in shallow-water regions of the Yangtze platform, South China
Gao, Y., Zhang, X., Fang, C., He, X., Fang, Z., & Zhang, X. (2020) · Precambrian Research · doi:10.1016/j.precamres.2020.106004 · Cited by 12
Chemostratigraphy as a Formal Stratigraphic Method
Sial, A. N., Gaucher, C., Ramkumar, M., & Ferreira, V. P. (2018) · Geophysical monograph · doi:10.1002/9781119382508.ch1 · Cited by 6
“Mo is a redox‐sensitive element, scavenged from seawater into sediments in the form of MoSxO4−x 2−, under anoxic conditions [Wen et al., 2015].”
Background
Oceanic redox variations during the Cambrian Age 2–3 in the Yangtze Block of South China: Evidence from pyrite-based proxies
Fu, F., Zou, C., Zhao, Z., Pan, S., Wang, W., Luo, C., Hua, G., Lu, G., Yuan, M., Yin, J., et al. (2025) · Marine and Petroleum Geology · doi:10.1016/j.marpetgeo.2025.107438 · Cited by 8
Polymetallic mineralization in early Cambrian black shale: Insights from Guizhou, South China
Yang, Z., Zhang, J., & Fu, Y. (2025) · Ore Geology Reviews · doi:10.1016/j.oregeorev.2025.106595 · Cited by 8
Coupling of shallow marine redox change and multi-stage animal radiations during the early Cambrian
Zheng, Y., Chang, C., Li, J., Ding, Y., Tang, X., & Liu, J. (2025) · Gondwana Research · doi:10.1016/j.gr.2025.01.003 · Cited by 6
Possible response of N2O emission to marine redox fluctuation during the Ediacaran-Cambrian transition in Nanhua Basin, South China
Wang, Z., Chang, C., Zhang, X.-L., Ju, P.-C., Lu, Y., Meng, Z.-K., & Huang, K.-J. (2021) · Precambrian Research · doi:10.1016/j.precamres.2021.106409 · Cited by 8
The REY geochemistry of phosphorites during metamorphism of the Haizhou Group, NW Yangtze Block, China
Liu, X.-Q., Fan, H.-F., Zhang, H.-J., Xiao, C., Yang, H.-Y., Zhou, T., Tang, Y., Shang, P., Zhu, C.-W., & Wen, H.-J. (2023) · Chemical Geology · doi:10.1016/j.chemgeo.2023.121781 · Cited by 7
Self-citation
Deep-water dissolved iron cycling and reservoir size across the Ediacaran-Cambrian transition
Xiang, L., Schoepfer, S. D., Zhang, H., Chen, Z., Cao, C., & Shen, S. (2020) · Chemical Geology · doi:10.1016/j.chemgeo.2020.119575 · Cited by 9
“These include platform sections such as the Meishucun section (Wen et al., 2015), the Weng'an section (Jin et al.”
Background
Mo isotopic response to the end of Neoproterozoic Marinoan glaciation: Evidence from a sedimentary profile in South China
Yang, X., Long, X., Li, J., Dong, Y., & Zhao, B. (2020) · Precambrian Research · doi:10.1016/j.precamres.2020.105609 · Cited by 7
Tectonic setting, paleoenvironment and REE source of the Lower Cambrian phosphorites, Yangtze Block (South China)
Guo, C., Fu, Y., Xia, P., Yang, Z., Li, Y., & Pan, Z. (2025) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/j.palaeo.2025.112821 · Cited by 5
Molybdenum isotopic evidence for linked changes in North Pacific Intermediate Water and subtropical Northwest Pacific redox conditions over the last 200 k.y
Dou, Y., Sun, C., Yang, S., Shi, X., Wu, Y., Cong, J., Zhang, Y., Wang, F., Cai, F., & Clift, P. D. (2024) · Global and Planetary Change · doi:10.1016/j.gloplacha.2024.104637 · Cited by 5
Self-citation
Sedimentary records reveal an early Cambrian active margin setting in the NW Yangtze Block, South China
Gu, Z., Jian, X., Zhai, X., Shen, X., & Ye, S. (2025) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/j.palaeo.2025.113207 · Cited by 5
Evidence for low sulfate and anoxic deep waters in early Cambrian
Gong, Y., Li, D., Li, M., Sun, L., Zhang, X., Cui, Y., Fu, Y., Xu, Y., & Shen, Y. (2024) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/j.palaeo.2024.112281 · Cited by 5
Geochemical Characteristics of Trace Elements and Mineralization Model of the Ediacaran-Early Cambrian Phosphorites, South China
Zhang, L., Zhang, M., & Zhu, G. (2024) · ACS Omega · doi:10.1021/acsomega.3c08214 · Cited by 6
Sedimentary Environment and Mineralization of the Black Shale Polymetallic Layer in the Early Cambrian, SW China: Constraints from in situ LA‐ICP‐MS Analysis of Pyrite
Yang, Z., Fu, Y., Li, C., Cai, X., & Guo, C. (2023) · Acta Geologica Sinica (English) · doi:10.1111/1755-6724.15126 · Cited by 5
Copper and Zinc isotopes trace the evolution of the Ediacara-Early Cambrian paleo-ocean redox condition in the Tarim Basin, China
Ai, Y., Zhu, G., Li, T., & Zhu, Z. (2023) · Applied Geochemistry · doi:10.1016/j.apgeochem.2023.105588 · Cited by 7
Rethinking Seawater Mo Isotope Mass‐Balance and the Sedimentary Mo Record
Ostrander, C. M., & Dellwig, O. (2026) · Paleoceanography and Paleoclimatology · doi:10.1029/2025pa005313 · Cited by 6
“…al. (2017), Matthews et al. (2017), In sedimentary rocks from South China formed during these periods, Mo concentrations can approach wt % levels (e.g., Sahoo et al., 2016; Wen et al., 2015; Wille et al., 2008) and δ 98 Mo are sometimes lower than (cid:0) 2‰ (e.g., Ostrander, Sahoo, et al., 2019).”
Influential
Thallium Isotopes Suggest the Global Deep Ocean Did Not Approach Modern Oxygenation During Cambrian Age 3 Metazoan Radiation
Clemente, J. N. R., Fan, H., Ostrander, C. M., Zhang, H., Wen, H., Sperling, E. A., & Nielsen, S. G. (2025) · Geobiology · doi:10.1111/gbi.70028 · Cited by 4
“Contrary to previous suggestions of a shift to near-modern extents of marine oxygenation during Cambrian Age 3 (Chen et al. 2015; Li et al. 2021; Wen et al. 2015), the new Tl isotope data do not record modern extents of marine oxygenation as evidenced by modern Tl isotope compositions either…”
InfluentialSelf-citation
Remobilization of Ni in framboidal pyrite within sulfide nodules in Early Cambrian nickeliferous black shales
Liu, X.-Y., Wu, Y.-F., Gregory, D. D., Evans, K., Williams-Jones, A., Zhang, W., Zhou, M.-F., & Li, J.-W. (2025) · Chemical Geology · doi:10.1016/j.chemgeo.2025.122913 · Cited by 4
Biogenic mineralization controls exceptional REY enrichment in Early Cambrian phosphorites from South China
Peng, R., Yang, R.-D., Chen, J.-Y., Gao, J.-B., Gao, L., & Gao, C. (2025) · Ore Geology Reviews · doi:10.1016/j.oregeorev.2025.106497 · Cited by 4

Authors: Wen, H., Fan, H., Zhang, Y., Cloquet, C., & Carignan, J.
Affiliations: Chinese Academy of Sciences (CN)
Centre National de la Recherche Scientifique (FR)
Corresponding author: Wen, Hanjie
Fan, Haifeng
ORCID: Wen, Hanjie
Fan, Haifeng
Zhang, Yuxu
Cloquet, Christophe
Venue: Geochimica et Cosmochimica Acta
Publisher: Elsevier BV
Published: 2015-09
Volume: 164
Pages: 1-16
ISSN: 0016-7037 (ISSN-L)
DOI: 10.1016/j.gca.2015.05.008
OpenAlex: W307804840
Cited by: 131
References: 0
Citations by year: 2026: 7 · 2025: 21 · 2024: 14 · 2023: 13 · 2022: 10 · 2021: 14 · 2020: 13 · 2019: 6 · 2018: 12 · 2017: 13 · 2016: 3 · 2015: 5
FWCI: 8.34
Type: journal article
Language: en
Open access: closed
Licence: www.elsevier.com/tdm/userlicense/1.0/ (tdm)
Locations: Geochimica et Cosmochimica Acta (publishedVersion)
HAL (submittedVersion)
Funders: 973 Program (2014CB440904)
National Natural Science Foundation of China (40930425, 41173026, 41273024)
CAS-SAFEA International Partnership Program for Creative Research Teams (KZZD-EW-TZ-20)
State Key Laboratory of Ore-deposit Geochemistry, Chinese Academy of Sciences (SKLODG-ZY125-07)
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: molybdenum isotopes, Neoproterozoic-Cambrian transition, redox stratification, anoxic deep water, euxinia, ferruginous conditions, ocean circulation reorganization, Cambrian explosion, South China

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Reconstruction of early Cambrian ocean chemistry from Mo isotopes

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