Palaeoclimate research at Birmingham integrates sedimentologists, palaeontologists, geochemists and climate modelers to produce an integrated view of ancient palaeoenvironmental change.

Our time periods of study stretch from detailed investigations of the sedimentology and glacial process of Proterozoic “snowball earth” events, to super high-resolution speleothem reconstructions and General Circulation Model simulations of Holocene climate. Analytical facilities available to palaeoclimate researchers in the group include a new organic geochemistry suite dedicated to palaeoenvironmental reconstruction (GC-FID, GC-MS, GC-ir-MS, LC-APCI-MS) as well as trace metal (ICP-MS and –OES), stable isotope and nannoparticle characterisation facilities within the School. Researchers also benefit from significant recent investment in central University analytical capability including, SEM/TEM suite, Secondary Ionistation Mass Spectrometry (SIMS), state-of-the-art XRF and XRD suite. We also have a strong relationship with the NERC Ion Microprobe Facility at the University of Edinburgh with numerous successful grants in the past 2/3 years.