Our group uses the isotopic and chemical composition of microfossils (i.e., foraminifera) and marine sediments to investigate changes in ocean circulation, ocean chemistry, and climate during the last 66 million years of Earth’s history (Cenozoic). Our long-term goal is to study the interactions among the oceans, the atmosphere, and the biosphere over long geological time scales to improve our ability to forecast how these interactions will evolve in the future.
Research opportunities exists for undergraduate students interested in term-time or summer research. Ph.D. position(s) may also be available. Prospective students are welcome to contact me for additional information.
