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
Blog
Latest Posts
Climate Change and Communications with the world
Sometimes it is easy to forget to step outside the academic bubble... This is the first in a range of articles which will bring together ways and means how Climate Change is presented and understood in the world outside of our office doors. Related...
World’s future climate change hotspots mapped
Something of interest Related articles World's future climate change hotspots mapped
Press Release
Press Release: Study shows oxygen loss could be a huge issue for oceans A major study from universities including Birkbeck, UCL, Otago, Exeter and Oxford into an ancient climate change event that impacted a significant percentage of Earth’s oceans...
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Why is the Earth Habitable?
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News
Climate Change and Communications with the world
Sometimes it is easy to forget to step outside the academic bubble... This is the first in a range of articles which will bring together ways and means how Climate Change is presented and understood in the world outside of our office doors. Related...
World’s future climate change hotspots mapped
Something of interest Related articles World's future climate change hotspots mapped
Press Release
Press Release: Study shows oxygen loss could be a huge issue for oceans A major study from universities including Birkbeck, UCL, Otago, Exeter and Oxford into an ancient climate change event that impacted a significant percentage of Earth’s oceans...