Publications
Oxygenation of a Cryogenian ocean (Nanhua Basin, South China) revealed by pyrite Fe isotope compositions. Earth and Planetary Science Letters 429, 11-19 (2015).
Oxygenation of the Proterozoic Earth’s surface: An evolving story. Treatise on Geochemistry 3rd Edition in press (2024).
Recent advances in geochemical paleo-oxybarometers. Annual Review of Earth and Planetary Sciences 49, 399-433 (2021).
Redox conditions across the Cambrian-Ordovician boundary: elemental and isotopic signatures retained in the GSSP carbonates. Palaeogeography, Palaeoclimatology, Palaeoecology 440, 440-454 (2015).
Re-Os age constraints and new observations of Proterozoic glacial deposits in the Vazante Group, Brazil. Precambrian Research 238, 199-213 (2013).
Re-Os and Mo isotope systematics of black shales from the Middle Proterozoic Velkerri and Wollogorang Formations, McArthur Basin, northern Australia. Geochimica et Cosmochimica Acta 73, 2534-2558 (2009).
Selectively reducing nitrate into NH3 in neutral media by PdCu single-atom alloy electrocatalysis. ACS Catalysis 13, 10560-10569 (2023).
Shale heavy metal isotope records of low environmental O2 between two Archean oxidation events. Frontiers in Earth Science 10, 833609 (2022).
Significance of 56Fe depletions in late-Archean shales and pyrite. Geochimica et Cosmochimica Acta 316, 87-104 (2022).
187Re-187Os geochronology of Precambrian organic-rich sedimentary rocks. The Geological Society, London, Special Publications 326, 85-107 (2009).
Technical comment on “Reexamination of 2.5-Ga 'whiff' of oxygen interval points to anoxic ocean before GOE”. Science Advances 9, eabq3736 (2023).
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).
Trace elements at the intersection of marine biological and geochemical evolution. Earth-Science Reviews 163, 323-348 (2016).
Transient episodes of mild environmental oxygenation and oxidative continental weathering during the late Archean. Science Advances 1, e1500777 (2015).
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).
Uranium and molybdenum isotope evidence for globally extensive marine euxinia on continental margins and in epicontinental seas during the Devonian-Carboniferous Hangenberg Crisis. Geochimica et Cosmochimica Acta 352, 133-156 (2023).
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).
Uranium isotope fractionation suggests oxidative uranium mobilization at 2.50 Ga. Chemical Geology 362, 105-114 (2013).