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Earth Surface Processes and Paleoaltimetry

One of our research interests is the interplay between the processes that shape the Earth’s surface and their geodynamic counterparts at depth, in particular interactions among (paleo-)climate, landscape evolution, and mountain building. We use stable isotope paleoaltimetry including biomarker analytics and clumped isotope ( Δ47) thermometry as a tool to trace (bio-)geochemical processes from the ecosystem to the orogen scale with a particular focus on the Cenozoic evolution of coupled climatic and tectonic processes.

 

Research

Senckenberg Biodiversity and Climate Research Centre

Paleoclimate and Paleoenvironmental Dynamics

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