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Mechanism of molybdenum removal from the sea and its concentration in black shales: EXAFS evidence
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“in the presence of abundant (10 -3 -10 -4 M) free hydrogen sulfide, Mo is converted to a series of particle-reactive thiomolybdates and is efficiently removed from seawater (the so-called Mo”
From Trace elements at the intersection of marine biological and geochemical evolution (2016) · cites this paper as Helz et al., 1996
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“For example, authigenic U accumulation commences at the Fe(II)–Fe(III) redox boundary, whereas authigenic Mo accumulation requires the presence of H2S (Helz et al. 1996; Zheng et al. 2002).”
BackgroundO'Sullivan, E., Nagler, T., & Babechuk, M. (2021) · Chemical Geology · doi:10.1016/j.chemgeo.2020.120039 · Cited by 13
Xue, Y., Lei, Y., Zhang, J., Chen, S., Chen, L., Zhong, K., He, L., Li, D., & Wu, Q. (2021) · Natural Gas Industry B · doi:10.1016/j.ngib.2021.11.001 · Cited by 12
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“These elements differ in the redox potential (Eh) at which they are oxidized/reduced and in their responses to geochemical variables such as sorption to reactive metal oxides, complexation with organic matter or sulfide, and the activity of certain microbial species (Rai et al., 1989; Wanty and Goldhaber 1992; Barnes…”
BackgroundXia, P., Hao, F., Tian, J.-Q., Zhou, W., Fu, Y., Guo, C., Yang, Z., Li, K., & Wang, K. (2022) · Energies · doi:10.3390/en15134551 · Cited by 12
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Paleo-Redox Conditions of the Albian-Danian Carbonate Rocks of the Cauvery Basin, South India
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“It should be noted that the accumulation of authigenic Mo, which occurred in the TOC-poor OM formed under oxic conditions, may be affected by oxic conditions due to the lack of H2S required to convert MoO4 2 to MoOxS4-x 2 or MoS4 2 (Helz et al., 1996; Algeo and Rowe, 2012).”
BackgroundInfluentialZhang, 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
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“Mo occurs primarily as soluble MoO 4 in oxygenated marine waters, and its reduction to particle reactive thiomolybdates (MoOxS 2− 4x ) under anoxia or molybdenum sulfide (MoS 4 ) under euxinia results in authigenic enrichment of sedimentary Mo (Crusius et al., 1996; Helz et al., 1996; Zheng et al., 2000; Vorlicek and…”
BackgroundWang, Y., Chen, J., Shen, W., & Li, M. (2022) · Frontiers in Earth Science · doi:10.3389/feart.2022.879658 · Cited by 12
“highly activated thiomolybdate, which is eventually captured by ferromangous hydroxide or forms metal complexes with humic acid (Helz et al., 1996; Helz et al., 2011).”
BackgroundLian, J., Xu, S., Yu, C., & Han, C. (2012) · Toxicological & Environmental Chemistry Reviews · doi:10.1080/02772248.2012.655694 · Cited by 11
“It may exist as MoS2 in reducing environments although the formation may be kinetically limited (Helz et al. 1996).”
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“In anoxic seawater and pore fluids, Mo is converted to the particle reactive thiomolybdate anion ( ) 2 x 4 x MoO S − (x = 0 to 3) [12] [13].”
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“However, MoO4 22 cannot be removed with the ‘nascent’ sulphide by coprecipitation–adsorption method which has been verified in geochemical field.(27,28) Therefore, Mo removal efficiency begins to reduce with the increasing Cu dosage.”
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“The chemical species of dissolved molybdenum and tungsten depend on the concentrations of oxygen and sulfide in the aquatic environment (Emerson and Huested, 1991; Helz et al., 1996; Cui et al., 2021), which in turn change their concentrations and stable isotope ratios in the sediments (Tsujisaka et al.”
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“Here, we have considered the anoxic condition as the intermediate reducing Mo sink with low H 2 S abundance (<11 μM; Helz et al., 1996) and particulate shuttling/ generation possibilities, where a complete conversion of molybdate ions to thiomolybdate complexes is unlikely.”
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“When sulfide is absent, or below 11 μ mol L (cid:0) 1 , molybdate diffuses into the sediments and is then scavenged via iron-Mo-sulfides, and possibly, organic matter (Helz et al., 1996; Zheng et al., 2000; Helz and Vorlicek, 2019).”
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“thiomolybdates, in sediments where oxygen penetrates 0.3 cm or less below the sediment–water interface ( Helz et al. 1996; Morford et al. 2005; Vorlicek et al. 2004).”
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“Under hypoxic-sulfidic conditions, when the concentration of hydrogen sulfide reaches a certain level (approximately 50–250 μM), Mo becomes active, leading to the transformation of molybdate ions into thiomolybdate ions [48,50], which easily associate with sulfidic organic matter or iron sulfide to deposit and accumul…”
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“Its removal from the water column to sediments requires a reduction reaction through which H2S/HS transforms stable molybdate to particle-reactive thiomolybdates (Helz et al., 1996).”
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“In the presence of free H2S, molybdate present in sediment pore water is able to react to form particle-reactive thiomolybdates (MoOxS4-x) (Helz et al. 1996), which are easily scavenged by sulphur-rich organic molecules, metal-rich compounds (Tribovillard et al. 2004; Helz et al. 1996, 2011) and…”
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Ma, Z., Hu, S., Liu, X., Zhou, C., Wen, W., Zhang, Q., Huang, J., & Xiao, M. (2021) · Geological Journal · doi:10.1002/gj.4106 · Cited by 7
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Paul, K., Hermans, M., Jokinen, S., Brinkmann, I., Filipsson, H., & Jilbert, T. (2023) · Biogeosciences · doi:10.5194/bg-20-5003-2023 · Cited by 6
“…and generally follow the same pattern as F1, suggesting that Mo initially stored in labile thiomolybdate intermediates on mineral surfaces (e.g., Helz et al., 1996; Vorlicek et al., 2018) may also become more permanently incorporated into Fe oxides and OM (e.g., Chappaz et al., 2014; Dahl et…”
BackgroundInfluentialRedox changes in the Iapetus Ocean during the Late Ordovician extinction crises
Sánchez-Roda, A., Wignall, P. B., Xiong, Y., & Poulton, S. W. (2024) · Journal of the Geological Society · doi:10.1144/jgs2023-195 · Cited by 7
Wang, X., Ye, Y., Wang, H., & Zhang, S. (2021) · Marine and Petroleum Geology · doi:10.1016/j.marpetgeo.2021.105243 · Cited by 7
Iron minerals as archives of Earth’s redox and biogeochemical evolution
Peacock, C. L., Lalonde, S. V., & Konhauser, K. O. (2017) · White Rose Research Online (University of Leeds, The University of Sheffield, University of York) · Cited by 7
Takahashi, S., Nakada, R., Watanabe, Y., & Takahashi, Y. (2018) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/j.palaeo.2018.12.014 · Cited by 7
Early diagenesis and benthic fluxes of redox-sensitive metals in eastern China shelf sediments
Wang, X., Li, L., Ren, Y., Cao, P., Zhu, A., Liu, J., & Shi, X. (2023) · Frontiers in Marine Science · doi:10.3389/fmars.2023.1154248 · Cited by 6
“thiomolybdates (Mo4S 2− 4−x, x=0 to 3) (Helz et al., 1996; Zheng et al., 2000) and finally scavenged as particle-reactive thiomolybdate (MoS 4 ) by Fe sulfides and/or sulfur-rich organic materials (Tribovillard et al.”
Wang, C., Dong, T., He, Z., Guo, X., & Liu, S. (2024) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/j.palaeo.2024.112546 · Cited by 6
Liang, Q., Huang, H., Sun, Y., Gong, S., Wang, X., Xiao, X., Dong, Y., Feng, J., & Feng, D. (2022) · Frontiers in Marine Science · doi:10.3389/fmars.2022.945908 · Cited by 6
“Thiomolybdate then reacts with either Fe sulfides through thiomolybdate–Fe sulfide interactions or organic matter (OM) through Mo–OM interactions, resulting in Mo enrichment in sediments (Helz et al., 1996; Helz et al., 2011).”
BackgroundRepartitioning of co-precipitated Mo(VI) during Fe(II) and S(-II) driven ferrihydrite transformation
Schoepfer, V. A., & Lindsay, M. B. J. (2022) · Chemical Geology · doi:10.1016/j.chemgeo.2022.121075 · Cited by 5
Schneider, A. B., Velasquez, I. B., Paul, S. A. L., Krause, C. H., & Koschinsky, A. (2022) · Marine Chemistry · doi:10.1016/j.marchem.2022.104182 · Cited by 6
Metadata
- Authors
- Helz, G. R., Miller, C. V., Charnock, J. M., Mosselmans, J. F. W., Pattrick, R. A. D., Garner, C. D., & Vaughan, D. J.
- Affiliations
- University of Maryland, College Park (US)
- Daresbury Laboratory (GB)
- University of Manchester (GB)
- Venue
- Geochimica et Cosmochimica Acta
- Publisher
- Elsevier BV
- Published
- 1996-10
- Volume
- 60
- Issue
- 19
- Pages
- 3631-3642
- ISSN
- 0016-7037 (ISSN-L)
- OpenAlex
- W2042505381
- Cited by
- 921
- References
- 58
- Citations by year
- 2026: 28 · 2025: 46 · 2024: 46 · 2023: 65 · 2022: 52 · 2021: 69 · 2020: 54 · 2019: 48 · 2018: 45 · 2017: 56 · 2016: 43 · 2015: 50 · 2014: 29 · 2013: 41 · 2012: 29
- FWCI
- 5.39
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Geochimica et Cosmochimica Acta (publishedVersion)
- Research Explorer (The University of Manchester) (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 › Physics and Astronomy › Radiation › X-ray Spectroscopy and Fluorescence Analysis
- Keywords
- molybdenum removal, black shales, molybdenum speciation, MoS2, humic acid, sulfidic waters, hydrogen sulfide, molybdenum oxidation state
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