Our research centers on understanding how terrestrial landscapes and organisms respond to past climate change.
We primarily use stable isotopic records to study interactions between mammals, vegetation, and climate in past ecosystems. Our work involves a combination of geologic fieldwork, isotopic lab work, and modern analog studies. Active projects include reconstructing Plio-Pleistocene environments from sedimentary and isotopic records preserved in the East African Rift system, isotope hydrology in Ethiopia, paleoecological and sedimentology of mid-Pleistocene sites in South Africa, and mass-dependent Δ17O variation in the sedimentary record and the hydrosphere.
The admissions cycle for Fall 2018 is closed but if you’re interested in graduate school for Fall 2019 or any other information about joining the group, click here.
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