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The seabed in southern Scandinavia contains numerous traces of a submerged landscape that is thought to be the remnant of a once important habitat for Mesolithic hunter-gatherers. Large parts of this landscape were gradually flooded by rising seas between 9500 and 4000 BC and perceptions of the Maglemose culture (9500-6400 BC) have, consequently, been based almost exclusively on former inland settlements. As a result, Early and Late Mesolithic societies have been understood as almost diametrically opposed with regards to their reliance upon marine resources and their degree of sedentism. The…mehr

Produktbeschreibung
The seabed in southern Scandinavia contains numerous traces of a submerged landscape that is thought to be the remnant of a once important habitat for Mesolithic hunter-gatherers. Large parts of this landscape were gradually flooded by rising seas between 9500 and 4000 BC and perceptions of the Maglemose culture (9500-6400 BC) have, consequently, been based almost exclusively on former inland settlements. As a result, Early and Late Mesolithic societies have been understood as almost diametrically opposed with regards to their reliance upon marine resources and their degree of sedentism. The main objective of the book is to investigate two questions that are directly related to our current understanding of the populations of the now submerged areas: 1) Do we have a representative picture of the spread of Early Mesolithic sites in southern Scandinavia, or does the weighting towards inland sites reflect the fact that coastal sites have not been identified below present-day sea-level? 2) How did sea-level changes impact Mesolithic populations at different temporal and spatial scales, and how were these experienced from 8000-4000 BC? The book presents an extensive and up-to-date review of various types of evidence from the Boreal period such as faunal remains, fishing instruments, d13C values in bones, settlement positions and available marine resources. These are used to discuss the extent to which marine resources were utilised in the Maglemose culture. Another central component of this book is a series of new coastline models made to determine the Mesolithic sea-level changes / coastline positions. The eight new coastline models are created to facilitate new evaluations of possible relationships between sea-level changes and cultural changes. On the basis of the new coastline models the book also presents the preliminary results of 47 diver investigations conducted with the aim of identifying potential coastal settlements from the Maglemose culture.

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