DIVERSITY DYNAMICS OF MICROFOSSILS ACROSS THE CRETACEOUS–PALEOGENE AND EOCENE–OLIGOCENE TRANSITIONS
Results from these analyses demonstrate a steep rise in extinction rate at 66 Ma coupled with very low speciation rates within calcareous groups. This coincides temporally with the end-Cretaceous bolide impact that induced a global mass extinction. A decline in net diversification rates and mean species longevity reflect this extinction event, indicating a perturbation in diversity for 4-5 Myrs. Following the impact, disaster fauna with low diversity and short species turnover, recolonised vacant niches and are likely the cause of highly significant changes in speciation rate. This is not reflected in the siliceous radiolarians however, that show no significant extinction in their entire fossil record. Results for the Eocene-Oligocene transition demonstrate periods of significant diversity change, especially at the Middle Eocene Climatic Optimum. However, evidence of an expected gradual biotic turnover due to long-term climate change, is not shown to occur across the Eocene-Oligocene boundary. This analysis further investigates whether microfossil size can impact upon their survivability and promote selectivity during these shifts in diversity dynamics. Additional work with palaeoclimatic modelling will ensure increased understanding of what external factors drive diversity change across major transitions.