Prof. Kennett is retired and is not teaching and is not accepting graduate students.
Research largely deals with earth system history during the Cenozoic, including the Pleistocene, based on the analyses of the deep-sea sedimentary record and the uplifted marine record on land. A variety of paleoenvironmental proxies are used (stable isotopes, fossils, sediments) to reconstruct paleoclimatic, oceanographic and biotic changes in the sedimentary record.
Of greatest interest is to help develop better understanding of the past global environmental/ paleoclimatic changes and to evaluate the dynamic interactions that constantly occurred in the past between the several global spheres (lithosphere, ocean, atmosphere, cryosphere, and biosphere).
The kinds of questions we think about include the following: What is the climate evolution of the polar regions? When and how did the major ice sheets form? How have changes in ocean circulation affected global climate development? How did the oceans circulate during times of global warming? How tight are the linkages between climate change and thermohaline circulation? How abruptly do climate and oceans switch between different states and what processes drive these changes?
How has the global climate changed during the classic ice-age period and how has this affected North American climate? What is the history and causes of abrupt climate changes? What is the origin of climatic behavior, at brief and longer intervals in the recent ice-age period? How and when has instability of methane hydrates affected abrupt climatic change? What is the record of biological evolution in the oceans and how does this help with the understanding of biotic evolutionary processes? Data related to this and other questions are generated in light stable isotope mass spectrometry and micropaleontological and sedimentary laboratories.