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How does increased palaeosurface reconstruction contribute to understanding of the Arctic? -  Developing a deep time palaeoclimate field laboratory in Svalbard.

A complex tectonic history and global climate change has influenced the land masses bordering the Arctic ocean. On land tectonic movement affects runoff patterns, local hydology such as increased precipitation and local surface elevation, which again affects landform development, coastline distribution, discharge routing and vegetation distribution. Landatmospherebiosphere links and feedback loop with the ocean are continuously refined for use in earth system models for the youngest part of geological history. With access to large data sets, improved technology and new knowledge and methodologies it is now increasingly possible to also reconstruct direct surface response to tectonic movement in deep time.