About Jeremy
I am interested in understanding long-term controls on the Earth’s climate and hydrological cycle, particularly over the Cenozoic. During this interval, the Earth underwent a fundamental shift in its climate, transitioning from the hot, high-CO2 climate that characterized the Cretaceous and Eocene to the relatively cool, low-CO2 climate of today. Understanding this transition can elucidate first-order controls on Earth’s climate as well as improve understanding of what our future climate may resemble given current projections of CO2 emissions.
Website Google Scholar Profile CVInterests
- Paleoclimate
- Geochemistry
- Earth History
- Tectonics
Education
PhD, Earth System Science - Stanford University
Stanford, CA, 2016
BS, Earth Sciences - Rice University
Houston, TX, 2009
Awards, Honors, Grants
- Warner Outstanding Paper Award, 2021
Selected Publications
Stable isotope evidence for rapid uplift of the central Apennines since the Late Pliocene
Isotope Mass Balance Constraints Preclude that Mafic Weathering Drove Neogene Cooling
Role of the westerlies in Central Asia climate over the Cenozoic
The Neogene de-greening of Central Asia
Late Miocene uplift of the Tian Shan and Altai and reorganization of Central Asia climate
Cenozoic carbon cycle imbalances and a variable weathering feedback
Neogene cooling driven by land surface reactivity rather than increased weathering fluxes
Memberships
- American Geophysical Union
- European Geosciences Union