Lisbeth Prøsch-Danielsen
University of Stavanger, Achaeological Museum, Faculty Member
Bakkevig, S., Griffin, K., Prøsch-Danielsen, L., Selsing, L., Simonsen, A., Thomsen, H. & Wishman, E. 1987: Environmental changes in Rogaland, Southwest Norway, during the last 13500 years. A regional synthesis. IGCP-158B symposium at Höör, Sweden, 18–26 May 1987. Lundqua Report 27, 169–172. Univ...more
Research Interests:
... In the next sample, there is a rise in dinoflagel-late cysts and Ruppia pollen. Ruppia demands a salinity content higher than 1.9%o (Luther 1951). These spectra therefore demonstrate a gradual transition from a brackish to a marine... more
... In the next sample, there is a rise in dinoflagel-late cysts and Ruppia pollen. Ruppia demands a salinity content higher than 1.9%o (Luther 1951). These spectra therefore demonstrate a gradual transition from a brackish to a marine phase. ...
Research Interests:
Page 1. Published by Maney Publishing (c) Association of Environmental Archaeology Environmental Archaeology 8, 2003; pp. 33-50 The Use of Pollen, Magnetic and Carbon Analyses in Identifying Agricultural Activity and Soil Erosion from the... more
Page 1. Published by Maney Publishing (c) Association of Environmental Archaeology Environmental Archaeology 8, 2003; pp. 33-50 The Use of Pollen, Magnetic and Carbon Analyses in Identifying Agricultural Activity and Soil Erosion from the Neolithic to the Iron Age - ...
Research Interests:
Research Interests:
Research Interests:
Page 1. Environmental Archaeology 6, 2001; pp. 39-57 The Environmental Aspects and Palynological Signals of the #Fairy-Circles" - Ancient Earthworks linked to Coastal Heathland in South-Western Norway Lisbeth Pr0sch-Danielsen ...
Research Interests:
Palynological data collected over a period of 60 years have been compiled and re-interpreted in order to reveal the patterns of deforestation and health establishment in the south-western Norwegian coastal heathland. This heathland area... more
Palynological data collected over a period of 60 years have been compiled and re-interpreted in order to reveal the patterns of deforestation and health establishment in the south-western Norwegian coastal heathland. This heathland area has been divided into four sub-regions based on topography, bedrock and drift cover. The palynological investigations are from sites with pollen source areas of different sizes. The palynological signals are interpreted in terms of models that suggest an abrupt, gradual or stepwise deforestation which can be explained by terms of different pollen source areas. The deforestation seems to have been metachronous, leading to a regional mosaic pattern of different vegetation types. The deforestation process spanned more than 3600 calendar years (4000-400 B.C.), with three pronounced clearance periods at 4000-3600 B.C. (Mesolithic/Early Neolithic transition), 2500-2200 B.C. (Middle Neolithic II/Early Late Neolithic transition), and 1900-1400 B.C. (Late Neolithic to Bronze Age period II). The expansion of heathland has also been metachronous and took place over a period of ca. 4000 years between 4000-200 B.C., but was mainly completed by the end of the Bronze Age. Regional differences in the chronology of deforestation and heathland establishment are discussed. Deforestation with subsequent heathland expansion can best be explained in terms of the interaction between land-use history, topography and edaphic conditions under climatic conditions that favoured heathland development.
Research Interests:
Research Interests:
Investigations were undertaken in an area of western Norway, approximately 30 km from the coast. The area is dominated by Molinia caerulea heaths on gentle slopes of silt-dominated glacial deposits. Pollen analyses were made on 3 soil... more
Investigations were undertaken in an area of western Norway, approximately 30 km from the coast. The area is dominated by Molinia caerulea heaths on gentle slopes of silt-dominated glacial deposits. Pollen analyses were made on 3 soil profiles. Each profile could be divided into 2 local pollen assemblage zones (PAZs) corresponding with a change from dry to damp soils. From a comparison of the fossil pollen assemblages with pollen assemblages from surface samples collected from present-day Molinia heaths, and a radiocarbon date, the Molinia heaths can be shown to have originated about 1900 years BP. The persistence of the Molinia heaths is probably related to the high water-holding capacity of the sediments and the influence of human activity.
