Geology and Archaeology: Submerged Landscapes of the Continental Shelf
Sea-level change has influenced human population globally since prehistoric times. Even in early phases of cultural development human populations were faced with marine regression and transgression as a result of changing climate and corresponding glacio-isostatic adjustment. Global marine regression during the last glaciation changed the palaeogeography of the continental shelf, converting former marine environments to attractive terrestrial habitats for prehistoric humans. These areas of the shelf were used as hunting and gathering areas, as migration routes between continents, and most probably witnessed the earliest developments in seafaring and marine exploitation, until the postglacial transgression re-submerged these palaeo-landscapes. Based on modern marine research technologies and the integration of large databases, proxy data are increasingly available for the reconstruction of Quaternary submerged landscapes. Also, prehistoric archaeological remains from the recent sea bottom are shedding new light on human prehistoric development driven by rapidly changing climate and environment. This publication contributes to the exchange of ideas and new results in this young and challenging field of underwater palaeoenvironmental investigation.
Deglaciation, sea-level change and the Holocene colonization of Norway
-
Published:January 01, 2016
Abstract
The Norwegian coast facing the Atlantic Ocean was ice free as early as the Allerød oscillation in the late Pleistocene. The landscape was probably habitable for humans. It has, therefore, been assumed by several scholars that this coastline was visited or inhabited from the Late Glacial period onwards. In part, this argumentation is based on the presumed proximity of the Norwegian mainland and Doggerland, which existed between present-day Denmark and Great Britain because of a much lower global sea level. The aim of this paper is to examine the 14C dates available from the oldest Norwegian settlement sites, and to compare them to the Quaternary processes of deglaciation and sea-level change. The hypothesis is advanced that humans did not settle in present-day Norway before a sheltering passage of islands and peninsulas had developed between the Swedish west coast (Bohuslän) and the Oslo area. This happened in the second half of the Preboreal period, at approximately 9.3 cal ka BC, or in the final centuries of the tenth millenniun BC.
14C dates used in Figures 2, 4 and 9 are available at http://www.geolsoc.org.uk/SUP18779.
- absolute age
- Allerod
- archaeological sites
- archaeology
- artifacts
- C-14
- carbon
- Cenozoic
- colonization
- deglaciation
- Europe
- history
- Holocene
- human activity
- human ecology
- isotopes
- Mesolithic
- migration
- moraines
- Norway
- Oslo Norway
- paleoclimatology
- paleoecology
- paleoenvironment
- Pleistocene
- Preboreal
- Quaternary
- radioactive isotopes
- Scandinavia
- Scandinavian ice sheet
- sea-level changes
- shorelines
- Stone Age
- uplifts
- upper Pleistocene
- upper Quaternary
- upper Weichselian
- Weichselian
- Western Europe
- Younger Dryas
- Doggerland
- Fosna-Komsa Complex