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
- Humboldt Postdoctoral Fellow, 2018
- ETH Fellow, 2017
- Udall Scholar, 2007
- NOAA Hollings Scholar, 2007
Selected Publications
Drier winters drove Cenozoic open habitat expansion in North America
Toward a Cenozoic history of atmospheric CO2
The Hydroclimate and Environmental Response to Middle Miocene Warming in the Southwestern USA: Stable Isotope Evidence
Stable isotopes (d18O and d2H) of surface water in the arid Chinese Pamir, Central Asia: Implications for moisture sources and paleoenvironmental reconstructions
Stable isotope evidence for rapid uplift of the central Apennines since the Late Pliocene
Neogene evolution of paleoenvironments in the North American Great Plains from a stable isotope perspective
Isotope Mass Balance Constraints Preclude that Mafic Weathering Drove Neogene Cooling
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
Cenozoic stable isotope constraints on the Eurasian continental interior hydroclimate response to high CO2
CO2 drawdown from weathering is maximized at moderate erosion rates
Memberships
- Geochemical Society
- European Geosciences Union
- American Geophysical Union
- Geological Society of America