Speaker: Ms Melanie Sieber (RSES)
The carbon content in the atmosphere has a strong influence on climate and has changed dramatically over geological times.
Speaker: Helen Fricker (UC San Diego)
Antarctic ice loss is accelerating and will soon become the largest contributor to sea-level rise.
Speaker: Dominik Weiss (Imperial College London)
Variations in stable isotope ratios of trace metals are increasingly used to address fundamental challenges to air, water and soil quality.
Speaker: Mr Michael Anenburg (RSES)
Carbonatites are unusual igneous rocks that primarily contain carbonate minerals such as calcite or dolomite.
Speaker: Hrvoje Tkalčić (RSES)
More than 75 years ago, the Earth’s core was hypothesized to be solid in the centre as a result of a liquid–solid phase change in iron, which implies that shear waves in its sol