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Author [ Title(Desc)] Type Year
G
Kendall, B., Dahl, T.W. & Anbar, A.D. Good golly, why moly? The stable isotope geochemistry of molybdenum. Reviews in Mineralogy and Geochemistry: Non-Traditional Stable Isotopes 82, 683-732 (2017).
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Dong, A. et al. Insights from modern diffuse flow hydrothermal systems into the origin of post-GOE deep-water Fe-Si precipitates. Geochimica et Cosmochimica Acta 317, 1-17 (2022).
Kendall, B. et al. Inverse correlation between the molybdenum and uranium isotope compositions of Upper Devonian black shales caused by changes in local depositional conditions rather than global ocean redox variations. Geochimica et Cosmochimica Acta 287, 141-164 (2020).
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Deline, M.L. et al. Lithium isotopes differentially modify mitochondrial amorphous calcium phosphate cluster size distribution and calcium capacity. Frontiers in Physiology 14, 1200119 (2023).
Charette, B. et al. Long-lived anatexis in the exhumed middle crust of the Torngat Orogen: constraints from phase equilibria modeling and garnet, zircon, and monazite chronology. Lithos 388-389, 106022 (2021).
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Lu, X. et al. Marine redox conditions during deposition of Late Ordovician and Early Silurian organic-rich mudrocks in the Siljan ring district, central Sweden. Chemical Geology 457, 75-94 (2017).
Li, J., Azmy, K. & Kendall, B. The Mo- and U-isotope signatures in alternating shales and carbonate beds of rhythmites: a comparison and implications for redox conditions across the Cambrian-Ordovician boundary. Chemical Geology 602, 120882 (2022).
Sheen, A.I. et al. A model for the oceanic mass balance of rhenium and implications for the extent of Proterozoic ocean anoxia. Geochimica et Cosmochimica Acta 227, 75-95 (2018).
Kendall, B., Gordon, G.W., Poulton, S.W. & Anbar, A.D. Molybdenum isotope constraints on the extent of late Paleoproterozoic ocean euxinia. Earth and Planetary Science Letters 307, 450-460 (2011).
Kunert, A., Clarke, J.D.A. & Kendall, B. Molybdenum isotope constraints on the origin of vanadium hyper-enrichments in Ediacaran-Phanerozoic marine mudrocks. Minerals 10, 1075 (2020).
Duan, Y. et al. Molybdenum isotope evidence for mild environmental oxygenation before the Great Oxidation Event. Geochimica et Cosmochimica Acta 74, 6655-6668 (2010).
Tan, Z. et al. Molybdenum isotope evidence from restricted-basin mudstones for an intermediate extent of oxygenation in the late Ediacaran ocean. Chemical Geology 623, 121410 (2023).
Qin, Z. et al. Molybdenum isotope-based redox deviation driven by continental margin euxinia during the early Cambrian. Geochimica et Cosmochimica Acta 325, 152-169 (2022).
Dong, A. et al. A multi-isotope approach towards constraining the origin of large-scale Paleoproterozoic B-(Fe) mineralization in NE China. Precambrian Research 292, 115-129 (2017).
Ostrander, C.M. et al. Multiple negative molybdenum isotope excursions in the Doushantuo Formation (South China) fingerprint complex redox-related processes in the Ediacaran Nanhua Basin. Geochimica et Cosmochimica Acta 261, 191-209 (2019).
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Li, Z. et al. New constraints on mid-Proterozoic ocean redox from stable thallium isotope systematics of black shales. Geochimica et Cosmochimica Acta 315, 185-206 (2021).
Lu, X., Edwards, C.T. & Kendall, B. No evidence for expansion of global ocean euxinia during the base Stairsian mass extinction event (Tremadocian, Early Ordovician). Geochimica et Cosmochimica Acta 341, 116-131 (2023).
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Sahoo, S.K. et al. Ocean oxygenation in the wake of the Marinoan glaciation. Nature 489, 546-549 (2012).
Sahoo, S.K. et al. Oceanic oxygenation events in the anoxic Ediacaran ocean. Geobiology 14, 457-468 (2016).
Kendall, B. An osmium-based method for assessing the source of dissolved rhenium and molybdenum to Archean seawater. Chemical Geology 385, 92-103 (2014).

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