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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PhD Positions
DFG-funded PhD position The causes and consequences of inception of glaciation at the Eocene- Oligocene boundary The Topic One of the most important climate transitions in the past ~100 Myr is the establishment of permanent glaciation on Antarctica. This...
A solution to the climate crisis
Enhanced Chemical Weathering
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Why is the Earth Habitable?
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PhD Positions
DFG-funded PhD position The causes and consequences of inception of glaciation at the Eocene- Oligocene boundary The Topic One of the most important climate transitions in the past ~100 Myr is the establishment of permanent glaciation on Antarctica. This...