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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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“…42 (cid:0) is sequentially transformed into highly particle-reactive Mo-sulfide species such as thiomolybdate (Mo VI O x S 2 (cid:0) 4 - x ; x = 1 – 4, Helz et al., 1996; Erickson and Helz, 2000), Mo polysulfide (Mo IV O(S 4 )S 2 (cid:0) ; Vorlicek et al., 2004), or an inorganic FeMo VI S 4 phase.”
BackgroundBowyer, F. T., Krause, A. J., Song, Y., Huang, K., Fu, Y., Shen, B., Li, J., Zhu, X., Kipp, M. A., van Maldegem, L. M., et al. (2023) · Science Advances · doi:10.1126/sciadv.adf9999 · Cited by 30
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Early diagenesis and trace element accumulation in North American Arctic margin sediments.
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“…org and C org /P tot , sedimentary enrichment in Mo is a widely used proxy to determine the degree of oxygen depletion in marine sediments, with increasing sedimentary Mo concentrations pointing to more reducing conditions (e.g. Emerson and Huested, 1991; Helz et al., 1996; Scott and Lyons, 2012).”
Dahl, T. W., & Wirth, S. B. (2017) · Chemical Geology · doi:10.1016/j.chemgeo.2017.04.018 · Cited by 28
“…in euxinic settings, molybdenum is sourced as MoO42− in oxic surface waters and ultimately ends in the sediments as reduced Mo(IV)-sulfides complexed with organic matter and/or Fe-sulfides in the sediments (Chappaz et al., 2014; Dahl et al., 2013a, 2016; Freund et al., 2016; Helz et al., 1996).”
Liu, W., Etschmann, B. E., Mei, Y., Guan, Q., Testemale, D., & Brugger, J. (2020) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2020.08.003 · Cited by 28
Onoue, T., Soda, K., & Isozaki, Y. (2021) · Frontiers in Earth Science · doi:10.3389/feart.2020.613126 · Cited by 17
“Enrichment factors for Mn, Ni, Cu, Zn, Tl, V, U, and Mo have been widely used to characterize the redox conditions of marine environment (e.g., Calvert and Pedersen, 1993; Calvert and Pedersen, 2007; Algeo and Tribovillard, 2009; Takahashi et al., 2014; Algeo and Li, 2020), which can be generally classified as oxic, d…”
BackgroundInfluentialGeochemistry of Fine-Grained, Organic Carbon-Rich Facies
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“Molybdenum concentration has been suggested to be enhanced in the presence of sulphides (Helz et al. 1996; Adelson et al. 2001; Zheng et al. 2000; Vorlicek & Helz 2002; Lyons et al. 2003; Algeo & Maynard 2004; Rimmer et al. 2004; Tribovillard et al. 2004c).”
BackgroundIkeda, M., Bôle, M., & Baumgartner, P. O. (2016) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/j.palaeo.2016.06.009 · Cited by 28
Sperling, E. A., Balthasar, U., & Skovsted, C. B. (2018) · Emerging Topics in Life Sciences · doi:10.1042/etls20170163 · Cited by 28
“anion to tetrathiomolybdate, which increases particle reactivity and hence the removal of Mo 142 from the water column into the sediment (31,32).”
BackgroundRazum, I., Miko, S., Ilijanić, N., Hasan, O., Miko, M. Š., Brunović, D., & Pawlowsky‐Glahn, V. (2020) · Applied Geochemistry · doi:10.1016/j.apgeochem.2020.104574 · Cited by 28
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“For example, molybdate is precipitated from sea water in the form of molybdenum‐iron–sulfur compounds present in black shales and sea sediments (Helz et al., 1996).”
BackgroundWu, C., Zhang, L., Zhang, T., Tuo, J., Song, D., Liu, Y., Zhang, M., & Xing, L. (2019) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/j.palaeo.2019.109457 · Cited by 26
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“…due to various reasons, for example, hydroxide particles of Mn and Fe can adsorb Mo in seawater, leading to a large enrichment of Mo in sediments (Helz et al. 1996), which results in that Mo/TOC and U-MO covariant models cannot effectively that determine the water restricted degree in studies on…”
BackgroundQiao, J., Littke, R., Grohmann, S., Zhang, C., Jiang, Z., Strauß, H., & Zieger, L. (2022) · International Journal of Coal Geology · doi:10.1016/j.coal.2022.103958 · Cited by 25
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“The presence of dissolved hydrogen sulfide (H 2 S) in the water column or pore waters promotes the conversion of molybdates (MoO 4 2− ) to thiomolybdates (MoS 4 − x O x 2− ; with 1 < x < 4; e.g., Erickson & Helz, 2000; Helz et al., 1996, 2011; Zheng et al., 2000).”
BackgroundZhai, L., Wu, C., Ye, Y., Zhang, S., & An, Z. (2016) · Geological Journal · doi:10.1002/gj.2878 · Cited by 24
“In anoxic environments, MoO4 2 is converted to a series of particle-reactive thiomolybdate ions (MoS4 xOx(2) ) (Helz et al., 1996) in the presence of small amounts of dissolved hydrogen sulphide.”
BackgroundNeumeister, S., Algeo, T. J., Bechtel, A., Gawlick, H., Gratzer, R., & Sachsenhofer, R. F. (2016) · Mitteilungen der Österreichischen Geologischen Gesellschaft/Austrian journal of earth sciences · doi:10.17738/ajes.2016.0010 · Cited by 24
“…(free H 2 S in the water column) the accumulation of TEs is linked to the precipitation of authigenic solid TE phases (e.g., Morse and Luther, 1999) or conversion of reduced TEs to particle-active phases (e.g., Helz et al., 1996), resulting in strong TE enrichment and weak TE-TOC covariation.”
BackgroundWang, X.-B., Tang, Y.-G., Jiang, Y.-F., Xie, P., Zhang, S., & Chen, Z.-L. (2017) · International Journal of Coal Geology · doi:10.1016/j.coal.2016.12.006 · Cited by 22
Zwiep, K., Hennekam, R., Donders, T. H., van Helmond, N. A. G. M., de Lange, G. J., & Sangiorgi, F. (2018) · Quaternary Science Reviews · doi:10.1016/j.quascirev.2018.08.026 · Cited by 24
“Specifically, elevated sedimentary Mo concentrations are associated with euxinic conditions in bottom- and/or pore waters, as Mo is scavenged in the presence of free sulfide (H2S; Helz et al., 1996), while similarly S concentrations relate to pyrite formation under sulfate-reducing conditions (e.”
An expanded shale δ98Mo record permits recurrent shallow marine oxygenation during the Neoarchean
Ostrander, C. M., Kendall, B., Olson, S. L., Lyons, T. W., Gordon, G. W., Romaniello, S. J., Zheng, W., Reinhard, C. T., Roy, M., & Anbar, A. D. (2019) · Chemical Geology · doi:10.1016/j.chemgeo.2019.119391 · Cited by 24
“In anoxic and H2S-bearing ("euxinic") settings, the formation of particlereactive thiomolybdate species (MoO4-xSx) can result in efficient transfer of Mo from seawater into marine sediments (particularly when H2S[aq] ≥ 11 μM (Helz et al., 1996; Erickson and Helz, 2000)).”
BackgroundSondi, I., Mikac, N., Vdović, N., Ivanić, M., Furdek, M., & Skapin, S. D. (2016) · Chemosphere · doi:10.1016/j.chemosphere.2016.10.134 · Cited by 24
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“Thus, sedimentation on this margin responds to global-scale processes in the sea.”
BackgroundGeochemical response to pulsed sedimentation: Implications for the use of Mo as a paleo-proxy
McKay, J., & Pedersen, T. (2014) · Chemical Geology · doi:10.1016/j.chemgeo.2014.05.009 · Cited by 16
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“=O bond, substituting S for O to form a series of thiomolybdate ions (MoO4-xSx 2, x=1–4) and finally MoS4 2 (Helz et al., 1996).”
BackgroundRuebsam, W., Dickson, A., Hoyer, E.-M., & Schwark, L. (2017) · Gondwana Research · doi:10.1016/j.gr.2016.10.017 · Cited by 24
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“An important pathway for Mo enrichment is the transformation of molybdate to thiomolybdates (MoOxS 2− 4−x, where x = 0 ∼ 4), which are highly particle reactive (Helz et al., 1996; Erickson and Helz, 2000; Scholz et al., 2017).”
BackgroundAdsorption of Tetrathiomolybdate to Iron Sulfides and Its Impact on Iron Sulfide Transformations
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“2009), Mo (Helz et al. 1996) and As (Turner 1987, Ko et al.”
El‐Shafeiy, M., El-Kammar, A., El-Barkooky, A. N., & Meyers, P. A. (2016) · Marine and Petroleum Geology · doi:10.1016/j.marpetgeo.2016.03.007 · Cited by 22
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“…to be close to the 254 average value (1.1 ppm) of upper continental crust under dysoxic‒oxic conditions (Algeo and 255 Maynard, 2004), under anoxic conditions, and especially under sulfidic waters and sediments Mo 256 would be significantly elevated (Helz et al., 1996; Tribovillard et al., 2006).”
BackgroundInfluentialAtar, E., März, C., Aplin, A. C., Dellwig, O., HERRINGSHAW, L. G., Lamoureux-Var, V., Leng, M. J., Schnetger, B., & Wagner, T. (2019) · Climate of the past · doi:10.5194/cp-15-1581-2019 · Cited by 21
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“The conservative molybdate anion can transition to a particle reactive thiomolybdate anion (MoO4 2- to MoO4 − xSx 2-, x = 1–4) in the presence of H2S (Helz et al., 1996).”
BackgroundElbaz-Poulichet, F., Sabatier, P., Dezileau, L., & Freydier, R. (2014) · The Holocene · doi:10.1177/0959683614540957 · Cited by 16
Muñoz, P., Dezileau, L., Lange, C., Cardenas, L., Sellanes, J., Salamanca, M., & Maldonado, A. (2012) · Progress In Oceanography · doi:10.1016/j.pocean.2011.07.010 · Cited by 16
“Thiomolybdates react with particles such as Fe sulfides and organic molecules via S bridges (Helz et al., 1996).”
BackgroundTrace element systematics in cold seep carbonates and associated lipid compounds
Wang, X., Bayon, G., Kim, J.-H., Lee, D., Kim, D., Guéguen, B., Rouget, M., Barrat, J., Toffin, L. M. A. A., & Feng, D. (2019) · Chemical Geology · doi:10.1016/j.chemgeo.2019.119277 · Cited by 21
“conversion of soluble molybdate (MoO4) into particle-reactive thiomolybdate (MoOxS4-x) species that are then sequestered within the sediment (Helz et al., 1996; 2011).”
BackgroundZheng, B., Mou, C., Wang, X., Chen, H., & Xiao, Z. (2020) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/j.palaeo.2020.110166 · Cited by 21
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Li, S., Wignall, P., Poulton, S., Hedhli, M., & Grasby, S. (2022) · Palaeogeography, Palaeoclimatology, Palaeoecology · doi:10.1016/j.palaeo.2022.110835 · Cited by 19
Xiao, B., Guo, D., Zhao, Z., Xiong, S., Feng, M., Zhao, Z., & Li, S. (2024) · ACS Omega · doi:10.1021/acsomega.4c01129 · Cited by 21
Reprint of: New Applications of Trace Metals as Proxies in Marine Paleoenvironments
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Bura‐Nakić, E., Sondi, I., Mikac, N., & Andersen, M. B. (2019) · Chemical Geology · doi:10.1016/j.chemgeo.2019.119441 · Cited by 21
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Wang, B., Lei, H., & Huang, F. (2022) · Marine and Petroleum Geology · doi:10.1016/j.marpetgeo.2022.105578 · Cited by 20
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Ritzer, S. R., Schoepfer, S. D., Bussian, B., Farrell, Ú. C., Fraser, T. A., Henderson, C. M., Kang, J., Mwinde, C. N., Patch, A., & Sperling, E. A. (2024) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/j.palaeo.2024.112266 · Cited by 21
“…quantitative reduction to its particle-reactive thio-molybdate form, allowing for rapid sequestration in the sediment by binding to organic material and precipitation as authigenic sulfide minerals (Emerson and Huested, 1991; Erickson and Helz, 2000; Helz et al., 1996; Scott and Lyons, 2012).”
Yang, N.-F., Welch, K. A., Mohajerin, T. J., Telfeyan, K., Chevis, D. A., Grimm, D. A., Lyons, W. B., White, C., & Johannesson, K. (2015) · Chemical Geology · doi:10.1016/j.chemgeo.2015.03.029 · Cited by 21
Redox fluctuations, trace metal enrichment and phosphogenesis in the ~2.0 Ga Zaonega Formation
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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
Valdivieso-Ojeda, J., Huerta-Diaz, M., & Delgadillo-Hinojosa, F. (2014) · Chemical Geology · doi:10.1016/j.chemgeo.2013.11.021 · Cited by 20
The marine biogeochemistry of molybdenum
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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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