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Uranium isotope reconstruction of ocean deoxygenation during OAE 2 hampered by uncertainties in fractionation factors and local U-cycling

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Ecosystem responses of two Permian biocrises modulated by CO2 emission rates

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Examining the limitations of 238U/235U in marine carbonates as a paleoredox proxy

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238U/235U in calcite is more susceptible to carbonate diagenesis

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^(238)U/^(235)U in marine carbonates as a tracer of Precambrian paleoredox conditions

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Closing in on carbonate uranium isotopes as a paleo-redox proxy based on continuous records from Late Oligocene to Holocene island carbonates

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Controls of eustasy and diagenesis on the 238U/235U of carbonates and evolution of the seawater (234U/238U) during the last 1.4 Myr

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