The Geochemistry of Submerged Marine Landscapes: Lipid, Isotopic and Inorganic composition of Sediment Cores from the Palaeo-landscape of Doggerland

Abstract

Ten thousand years ago Great Britain was a part of the European continent, where the surface of the North Sea was about 70 metres below present sea level. The large, prehistoric submerged landmass that connected the island of Great Britain to the European continent is now widely known as Doggerland. 85 samples from six different cores, which were collected from this prehistoric landscape, were studied using multi proxy -organic and inorganic- geochemical methods. Thermal analysis determined the organic matter and carbonate content, which were utilized as characterizing indices, dividing each core into various depositional units. In addition, lipid analysis studying three sets of biomarkers (n-alkanes, fatty acids and sterols), was used to distinguish between various depositional environments, especially between terrestrial and aquatic. Furthermore, the cores were mineralogically analysed using the detected clay and non-clay minerals as depositional indicators; significant states such as high and low energy environments, palaeosoil, type of weathering and stone types were identified and used to recognize any mineralogical and thus depositional alteration. Finally, the sulfur isotope analysis identified different sources of sulfur, which were then used as environmental distinguishing proxies. An integration of these analytical results provided a detailed geochemical history of each core; importantly, a Storegga tsunami deposit was detected in core ELF01A. The primary contribution of this thesis was establishing an analytical approach using combined results from a range of analytical methods. The established approach can be used to study the depositional settings for any cored sediments.