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Contrasting molybdenum cycling and isotopic properties in euxinic versus non-euxinic sediments and sedimentary rocks: Refining the paleoproxies
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“By contrast, organic-rich black shales deposited under anoxic and sulfidic pore waters may become enriched in redox-sensitive trace metals, especially Mo (Algeo and Lyons, 2006;März et al., 2008;Scott and Lyons, 2012).”
From Trace elements at the intersection of marine biological and geochemical evolution (2016) · cites this paper as Scott and Lyons, 2012
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“Seawater δ 98 Mo values should have been higher (i.e., more strongly fractionated) when ocean oxygenation levels were higher, and lower (i.e., less strongly fractionated) when ocean oxygenation levels were lower (e.g., Arnold et al., 2004; Dahl et al., 2010; Scott & Lyons, 2012; Wille et al., 2007).”
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“Mo content in the sediments rarely exceeds 25 ppm when sulfidic conditions are restricted to porewaters, while Mo content exceeds 60 ppm and even over 100 ppm in the sediments where hydrogen sulfide is present in bottom seawater (Scott and Lyons, 2012).”
BackgroundRugen, E. J., Ineson, J. R., & Frei, R. (2022) · Precambrian Research · doi:10.1016/j.precamres.2022.106781 · Cited by 6
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“Subtle enrichments of redox-sensitive trace metals can be challenging to separate from background levels with no modern analogue for comparisons (Scott & Lyons, 2012 ).”
BackgroundHe, L., Liu, J., Zhang, H., Gao, J., Zhu, A., & Zhang, Y. (2021) · Acta Oceanologica Sinica · doi:10.1007/s13131-021-1775-5 · Cited by 6
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“This sulfidation process facilitates Mo sequestration into iron sulfides or organic phases via adsorption or coprecipitation, representing the primary mechanism for authi-genic Mo enrichment in anoxic sediments (Scott and Lyons, 2012; Jia et al ., 2023).”
Monedero-Contreras, R. D., Rodríguez-Tovar, F. J., & Martı́nez-Ruiz, F. (2024) · Global and Planetary Change · doi:10.1016/j.gloplacha.2024.104387 · Cited by 5
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“Mo concentrations are less than 25 ppm under non-euxinic conditions, 25–100 ppm under intermittent euxinic conditions, and more than 100 ppm under continuous euxinic conditions (Scott and Lyons 2012).”
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“…redox, where these elements have different sensitivities with respect to suboxic/ anoxic, non‐sulfidic versus anoxic, sulfidic (i.e., euxinic) conditions (Algeo & Li, 2020; Algeo & Tribo-villard, 2009; Helz et al., 1996; Lyons et al., 2009; Scott & Lyons, 2012; Tribovillard et al., 2006).”
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“A convincing mechanism to explain the distribution of Mo, As, and Sb is the so-called particulate shuttle process, which illustrates that these elements will be scavenged by Fe- and Mnoxyhydroxides in the water column (Tribovillard et al., 2006; Scott and Lyons, 2012; Tribovillard et al., 2013).”
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“…indicates a non-euxinic setting where H 2 S was restricted to the porewaters; values between 25 ppm and 100 ppm represent an intermittently euxinic setting or permanently Mo-depleted euxinic setting, and greater than 100 ppm records permanently euxinic, Mo-replete settings (Scott & Lyons, 2012).”
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Sediment geochemistry of the Thetis hypersaline anoxic basin (eastern Mediterranean Sea)
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“In the presence of dissolved sulphides, the largely conservative molybdate (MoO4) may be converted to particle-reactive thiomolybdates (MoOxS4 − x −2 ) and scavenged by pyrite and/or organic material (e.g., Brumsack and Thurow, 1986; Brumsack, 1989; Calvert and Pedersen, 1993; Jones and Manning, 1994; Werne et al., 20…”
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“Scott and Lyons (2012) suggested that Mo concentrations above 25 ppm indicated deposition under a euxinic water column in modern oceans.”
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“Modern marine studies have shown that Mo concentrations in sediments are commonly < 25 ppm under non-euxinic conditions, and > 100 ppm for permanently euxinic conditions (see Scott & Lyons, 2012).”
BackgroundLiu, Y., Lu, X., Çağatay, M. N., Zhang, Y., Li, Y., Peng, Y., Ruffine, L., & Lu, H. (2021) · Marine and Petroleum Geology · doi:10.1016/j.marpetgeo.2021.105094 · Cited by 3
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Beaty, B., Foster, W. J., Zuchuat, V., Moller, S. R., Buchwald, S. Z., Brooks, H. L., Rauzi, S., Isson, T. T., Planke, S., Rodríguez-Tovar, F. J., et al. (2025) · Geobiology · doi:10.1111/gbi.70032 · Cited by 2
“In particular, Mo concentrations > 25 ppm have been proposed as indicative of at least intermittent euxinia overlying modern and ancient marine sediments (Scott and Lyons 2012).”
Shi, M., Cao, Q., Zhang, J., Yuan, Y., Lu, H., & Wang, X. (2025) · Ore Geology Reviews · doi:10.1016/j.oregeorev.2025.107021 · Cited by 2
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“However, because Mo preferentially adsorbs onto Mn oxides with minimal adsorption onto Fe oxides (Barling & Anbar, 2004; Kashiwabara et al., 2011; Scott & Lyons, 2012), while W and Tl are efficiently scavenged by both Fe and Mn oxides (Kashiwabara et al., 2017), Fe oxide reduction driven by organic…”
Heavy tungsten isotopes in sulfidic seep sediments linked to carbonate precipitation
Miao, X.-M., Wei, J., Oppo, D., Liu, X.-T., Li, J.-R., Nan, H., Yu, X., Fang, Z., He, Z., Li, J.-T., et al. (2026) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2026.04.033 · Cited by 2
Guidebook for Field Trips in Western Maine and Northern New Hampshire
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“…Mo, U, and V elemental geochemistry has been employed to distinguish suboxic and anoxic-sulphidic redox conditions (Algeo & Maynard, 2004; Scott & Lyons, 2012), using the covariation relationships between the TOC and trace elements (TEs): (a) modest TE enrichment and strong covariation…”
MethodLi, J., Zhu, X., & Tang, S. (2022) · Journal of Earth Science · doi:10.1007/s12583-021-1520-1 · Cited by 3
“The Mo removal rate is 100× to 1 000× greater in euxinic waters than in oxic waters, leading to significant authigenic enrichment that can exceed 100 ppm (Dahl et al., 2013; Scott and Lyons, 2012; Scott et al., 2008).”
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Meehan, K. C., Powell, W., McKirdy, D., Hall, P. A., Nedin, C., Johnston, P. A., & Collom, C. (2022) · Australian Journal of Earth Sciences · doi:10.1080/08120099.2023.2137737 · Cited by 2
“Based on this observation, previous studies have proposed that sedimentary Mo concentrations >25 mg g 1 are indicative of at least intermittently euxinic conditions (Dahl et al., 2013; Scott & Lyons, 2012).”
ResultAyyıldız, T., Varol, B., Özdemir, A., & Gündoğan, İ. (2023) · Geoenergy Science and Engineering · doi:10.1016/j.geoen.2023.211879 · Cited by 2
Redox Conditions of the Late Ediacaran Ocean on the Southern Margin of the North China Craton
Yang, J., Jin, W., Wang, G.-D., Wan, L., & Zeng, Z. (2023) · Minerals · doi:10.3390/min13091124 · Cited by 2
Budko, D. F., Demina, L. L., Krasnova, E. D., & Starodymova, D. P. (2023) · Journal of Marine Science and Engineering · doi:10.3390/jmse11091753 · Cited by 2
“The behavior of Mo in anoxic conditions was elucidated by the reduction of MoO4 oxyanions to MoOxS4-x, forming thiomolybdates that can be adsorbed onto sulfides and organic particles [68,69].”
BackgroundLydites in the North Onega Synclinorium, Karelia: Trace Element Composition and Possible Genesis
Кондрашова, Н. И., & Медведев, П. В. (2023) · Lithology and Mineral Resources · doi:10.1134/s0024490223700219 · Cited by 2
“With allowance for the boundary Mo values (Scott and Lyons, 2012), different sedimentation conditions are inferred for the Tetyugino and Shunga sites: eux-inic conditions (absence of oxygen at simultaneous H 2 S presence) for the former and oxygen-free noneuxinic conditions, for the latter.”
BackgroundMethodWang, X., Xi, Z., Yan, Z., Zhang, S., Tang, S., & Lin, D. (2023) · Processes · doi:10.3390/pr11123436 · Cited by 2
Liu, Z., Tian, H., Sageman, B. B., Wu, Y., Li, T., Wang, X., Cen, W., & Chen, J. (2024) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/j.palaeo.2024.112508 · Cited by 2
Holocene evolution of Lake Faiyum (Egypt): Insights from elemental and molecular proxies
El‐Shafeiy, M., Hamdan, M. A., Birgel, D., Peckmann, J., Karimi, A. W., Zaky, A. S., Flower, R. J., Hassan, F. A., Vogel, H., Anselmetti, F. S., et al. (2024) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/j.palaeo.2024.112677 · Cited by 2
Lin, F., Wang, J., Mansour, A., Fu, X., Su, S., Nie, Y., Ahmed, M. S., Zeng, S., & Li, X. (2025) · Marine and Petroleum Geology · doi:10.1016/j.marpetgeo.2025.107289 · Cited by 2
Dong, Z., Zhang, B.-L., Zhang, L., Dong, F., Li, J., Peng, Z., Wan, B., & Wang, C. (2025) · Mineralium Deposita · doi:10.1007/s00126-024-01343-7 · Cited by 2
“Thresholds for panel B after Scott and Lyons (2012) and Bauer et al. (2022).”
InfluentialAntarctic subglacial trace metal mobility linked to climate change across termination III
Piccione, G. G., Blackburn, T. J., Northrup, P. A., Tulaczyk, S. M., & Rasbury, E. T. (2025) · The Cryosphere · doi:10.5194/tc-19-2247-2025 · Cited by 2
Transient oxygenation of the Mediterranean after the Zanclean megaflood
Amarathunga, U., Brocks, J. J., Meijer, P., Hope, J. M., Zachariasse, W. J., Hennekam, R., van der Hoeven, I., Röhl, U., Rule, S., Troitzsch, U., et al. (2025) · Proceedings of the National Academy of Sciences · doi:10.1073/pnas.2505429122 · Cited by 2
Wu, Y., Tian, H., Li, J., Hu, J., Wang, Y., Gan, C., & Fan, H. (2025) · Chemical Geology · doi:10.1016/j.chemgeo.2025.123017 · Cited by 3
Slack, J. F., Baalen, M. R. V., & Reusch, D. N. (2020) · Atlantic Geology · doi:10.4138/atlgeol.2020.010 · Cited by 3
Leighton, C., Leybourne, M. I., Layton‐Matthews, D., Peter, J. M., Gadd, M. G., & Voinot, A. (2021) · The Canadian Mineralogist · doi:10.3749/canmin.2000075 · Cited by 2
Budko, D. F., & Nemirovskaya, I. A. (2023) · Geochemistry International · doi:10.1134/s0016702923020027 · Cited by 2
“Molybdenum oxy-anions in the H2S presence are subsequently reduced to thiomolybdates, which then are absorbed by sulfides and organic particles (Helz et al., 2011; Scott and Lyons, 2012).”
BackgroundNon-traditional Stable Isotope Geochemistry of Seep Deposits
Jin, M., & Feng, D. (2023) · Springer eBooks · doi:10.1007/978-981-99-1494-4_10 · Cited by 2
Lu, X., Kendall, B., Li, C., Stein, H. J., Hannah, J. L., Gordon, G. W., & Ebbestad, J. O. R. (2015) · UWSpace (University of Waterloo) · Cited by 2
Metadata
- Authors
- Scott, C., & Lyons, T. W.
- Affiliations
- University of California, Riverside (US)
- Corresponding author
- Scott, Clint
- Venue
- Chemical Geology
- Publisher
- Elsevier BV
- Published
- 2012-09
- Volume
- 324-325
- Pages
- 19-27
- ISSN
- 0009-2541 (ISSN-L)
- OpenAlex
- W2005604628
- Cited by
- 745
- References
- 80
- Citations by year
- 2026: 64 · 2025: 71 · 2024: 65 · 2023: 75 · 2022: 64 · 2021: 75 · 2020: 74 · 2019: 43 · 2018: 50 · 2017: 53 · 2016: 37 · 2015: 32 · 2014: 23 · 2013: 13 · 2012: 5
- FWCI
- 17.36
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Chemical Geology (publishedVersion)
- 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, paleoredox proxies, black shales, total organic carbon, bottom water oxygenation, marine sediment, sedimentary rock
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