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Current Project

Understanding Climate Recovery From Warming. 

 The Paleocene-Eocene Thermal Maximum (PETM) was a rapid warming event (hyperthermal) 56 million years ago. It is studied as an analogy of current climate warming, so that we understand what happens during increasing temperatures.. We are examining how the climate recovered several tens of thousands of years after the warming started. 

Latest Publication

Tracing silicate weathering processes in the permafrost-dominated Lena River watershed using lithium isotopes


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Why is the Earth Habitable?