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Author Title Type [ Year(Desc)]
2015
Azmy, K., Kendall, B., Brand, U., Stouge, S. & Gordon, G.W. Redox conditions across the Cambrian-Ordovician boundary: elemental and isotopic signatures retained in the GSSP carbonates. Palaeogeography, Palaeoclimatology, Palaeoecology 440, 440-454 (2015).
Zhang, F. et al. Oxygenation of a Cryogenian ocean (Nanhua Basin, South China) revealed by pyrite Fe isotope compositions. Earth and Planetary Science Letters 429, 11-19 (2015).
Kendall, B. et al. Uranium and molybdenum isotope evidence for an episode of widespread ocean oxygenation during the late Ediacaran Period. Geochimica et Cosmochimica Acta 156, 173-193 (2015).
2016
Robbins, L.J. et al. Trace elements at the intersection of marine biological and geochemical evolution. Earth-Science Reviews 163, 323-348 (2016).
Dong, A. et al. Genesis of a giant Paleoproterozoic strata-bound magnesite deposit: Constraints from Mg isotopes. Precambrian Research 281, 673-683 (2016).
Sahoo, S.K. et al. Oceanic oxygenation events in the anoxic Ediacaran ocean. Geobiology 14, 457-468 (2016).
2017
Lu, X., Kendall, B., Stein, H.J. & Hannah, J.L. Temporal record of osmium concentrations and 187Os/188Os in organic-rich mudrocks: implications for the osmium geochemical cycle and the use of osmium as a paleoceanographic tracer. Geochimica et Cosmochimica Acta 216, 221-241 (2017).
Yang, S., Kendall, B., Lu, X., Zhang, F. & Zheng, W. Uranium isotope compositions of mid-Proterozoic black shales: evidence for an episode of increased ocean oxygenation at 1.36 Ga and evaluation of the effect of post-depositional hydrothermal fluid flow. Precambrian Research 298, 187-201 (2017).
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).
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).
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).
2018
Zhang, F. et al. Extensive marine anoxia during the terminal Ediacaran Period. Science Advances 4, eaan8983 (2018).
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).
2019
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).
Ostrander, C.M. et al. Fully oxygenated water columns over continental shelves before the Great Oxidation Event. Nature Geoscience 12, 186-191 (2019).
2020
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).
Lu, X., Dahl, T.W., Zheng, W., Wang, S. & Kendall, B. Estimating ancient seawater isotope compositions and global ocean redox conditions by coupling the molybdenum and uranium isotope systems of euxinic organic-rich mudrocks. Geochimica et Cosmochimica Acta 290, 76-103 (2020).
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).
Ostrander, C.M. et al. An expanded shale d98Mo record permits recurrent shallow marine oxygenation during the Neoarchean. Chemical Geology 532, 119391 (2020).
2021
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).

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