Eugene Bergh is an Invertebrate Palaeontologist and Geologist at Iziko Museums of South Africa, a position he has held since 2011. His main focus is academic research and publications on the use of microfossils (foraminifera and ostracods) as proxies to determine changes in marine palaeoenvironments, palaeoclimate and palaeoceanography in the southeast Atlantic during the late Cenozoic (16 million years ago to present-day). Eugene also aids in creating and managing exhibitions.
Educational development in the palaeosciences is incredibly important to Eugene and this has seen him lecturing and supervising post-graduate students at the University of Cape Town since 2012.
My broad research interests are in Palaeontology, specifically Invertebrate Palaeontology. My current study area is along the southern African margin where the Benguela Upwelling System (BUS) plays a major role in the geology, oceanography and socio-economic aspects of the region. The system is one of the most productive in the world and has been driven by climate and oceanographic changes during the late Cenozoic period. The sediments and microfossils from the ocean floor can give us information as to how this system initiated and developed over geologic time.
My current research is aimed at understanding how the southern African margin has been influenced during the initiation and intensification of the BUS by analysing the occurrences and geochemistry of a group of marine invertebrate microfossils called foraminifera. These organisms are unicellular, and while alive they produce a multi-chambered shell, called a test. It is the test that remains preserved as the fossil after they have died. Most foraminifera are very small (less than 1 mm in size) and can only be identified under the microscope. Some extinct forms are larger and could grow to more than 10 cm in diameter. These microfossils are extremely useful and can aid in determining the age of marine sediments and rock strata, the environments in which they lived and ocean processes associated with the time when they were alive. Foraminifera can incorporate seawater elements into their tests as they grow, and as such, reflect the ocean conditions at that particular point in time. Through isotopic analyses this information can be unlocked to enhance palaeoclimate, palaeoceanographic and palaeoenvironmental reconstructions. Through understanding past geologic processes related to climate and sea level changes, scientists are moving towards developing future climate models which can be used in informed decision making.