Reconstructing Past Environments: A study to the ecological changes in the Middle Pleistocene site Schöningen 13 II

This thesis discusses the environmental changes in flora and fauna from the Middle Pleistocene site Schöningen 13 II, Germany. The data in this thesis consists of the ecological data from Schö 13 II as well as faunal data from Middle Pleistocene archaeological sites and data from present day national parks in Europe. This data is used to get insight in species compositions in various types of environments. The archaeological data, comprising flora and fauna, are analysed as an entity to gain insight into the structure of the environmental changes at this site. The environment in Schöningen changed gradually in the four levels, Schö 13 II-1 to 13 II-4 from interglacial optimum to stadial phase with an onset to a glacial phase. The floral data gave detailed indications of fluctuations in the environment, whereas the faunal data showed a more gradual change in the environment. The elements in Schö 13 II-1 are indicative for an interglacial phase, 13 II-2 contains elements of both...Show moreThis thesis discusses the environmental changes in flora and fauna from the Middle Pleistocene site Schöningen 13 II, Germany. The data in this thesis consists of the ecological data from Schö 13 II as well as faunal data from Middle Pleistocene archaeological sites and data from present day national parks in Europe. This data is used to get insight in species compositions in various types of environments. The archaeological data, comprising flora and fauna, are analysed as an entity to gain insight into the structure of the environmental changes at this site. The environment in Schöningen changed gradually in the four levels, Schö 13 II-1 to 13 II-4 from interglacial optimum to stadial phase with an onset to a glacial phase. The floral data gave detailed indications of fluctuations in the environment, whereas the faunal data showed a more gradual change in the environment. The elements in Schö 13 II-1 are indicative for an interglacial phase, 13 II-2 contains elements of both interglacial and (inter)stadial phases and levels 13 II-3 and 13 II-4 are indicative for stadial contexts. Characteristic for the patterns in species diversity is that it is variable throughout the levels. Schö 13 II-1 and 13 II-3 both show a relatively low diversity, whereas the diversity in 13 II-2 and 13 II-4 is higher, but still not exceptionally high if compared to other Middle Pleistocene sites. These differences in diversity can be explained by potential deformations by taphonomical processes. The non-analoguous patterns in large mammal compositions of the site can be explained in terms of species behaviour and taphonomical processes.Show less

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Reconstructing Past Environments: A study to the ecological changes in the Middle Pleistocene site Schöningen 13 II