His goal is to try to understand the processes and mechanisms of organic
microfossil preservation and to reconstruct the biology, and environmental conditions and perturbations of the Neoproterozoic.
«Periods of very intense North Atlantic circulation and higher Northern Hemisphere temperatures increased the
preservation of
microfossils in the sediment cores, whereas those with slower circulation, when the study site was primarily influenced from the south, were linked with decreased carbonate ion concentrations at our core site which led to partial dissolution,» said co-author Dr Luke Skinner, also from Cambridge's Department of Earth Sciences.
Even when
microfossils are found, there are often controversies about their biological origin, since parameters that lead to a good
preservation of
microfossils are not well constrained.