Measuring geologic time is of fundamental importance to understanding the history of our Earth and solar system. The age constraints provided by geochronology are critical for determining the rates of many physical, chemical and biologic processes that shape our planet. My research focuses on the acquisition, improvement and application of geochronologic data. The U-Pb system is highly versatile, capable of providing extremely high-precision timing constraints on the formation and cooling history of rocks. My specific research projects are diverse, from linking global extinction events to large igneous province eruptions, to measuring the thermal and erosional history of Earth’s oldest continental crust.
The answer to the question “when?” is one of the most compelling parts of any geologic story and a cornerstone to the complete, meaningful interpretation of any geological process or event. My research utilizes isotopic measurement of U and its daughter radionuclides to provide the answer to “when?” in diverse geologic and planetary systems. I apply U-Pb ID-TIMS analyses on accessory phases to answer thermochronologic questions: xenolithic rutiles record the long-term cooling history of the Superior Craton/Province of the Canadian shield, and phosphates from ordinary chondrites provide insight into the formation, cooling, and disruption history of the chondrite parent bodies and the first ~100 Myrs of the Solar System. I use U-Series measurements of glaciogenic sediments to infer the relative and absolute timing of comminution (i.e. wearing down) of sediments to inform the time constraints of glacial and climatic histories.