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2. Structural, Electrochemical, and Magnetic Studies of Bulky Uranium(III) and Uranium(IV) Metallocenes

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   Boreen, Michael A.; Lussier, Daniel J.; Skeel, Brighton A.; Lohrey, Trevor D.; Watt, Fabian A.; Shuh, David K.; Long, Jeffrey R.; Hohloch, Stephan; Arnold, John (November 2019, Inorganic Chemistry)
3. Conversion of Trivalent Uranium Anilido to Tetravalent Uranium Imido Species via Oxidative Deprotonation

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   Perales, Diana; Ford, Shannon A.; Salpage, Sahan R.; Collins, Tyler S.; Zeller, Matthias; Hanson, Kenneth; Bart, Suzanne C. (September 2020, Inorganic Chemistry)

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   Gothmann, Anne M.; Higgins, John A.; Adkins, Jess F.; Broecker, Wally; Farley, Kenneth A.; McKeon, Ryan; Stolarski, Jarosław; Planavsky, Noah; Wang, Xiangli; Bender, Michael L. (April 2019, Geochimica et Cosmochimica Acta)
5. Uranium–Thorium Dating of Speleothems

   https://doi.org/10.2138/gselements.17.2.87  

   Wendt, Kathleen A.; Li, Xianglei; Edwards, R. Lawrence (April 2021, Elements)

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   Speleothems are important timekeepers of Earth’s climate history. A key advantage of speleothems is that they can be dated using U–Th techniques. Mass spectrometric methods for measuring U and Th isotopes has led to vast improvements in measurement precision and a dramatic reduction in sample size. As a result, the timing of past climate, environment, and Earth system changes can be investigated at exceptional temporal precision. In this review, we summarize the principles and history of U–Th dating of speleothems. Finally, we highlight three studies that use U–Th dated speleothems to investigate past changes to the Asian monsoon, constrain the timing of sociopolitical change in ancient civilizations, and develop a speleothem-based calibration of the 14C timescale. 

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