4 research outputs found

    Pollen record from Lake Skogstjern, Telemark, Southeast Norway

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    From the small-sized Lake Skogstjern (c. 2.6 ha, 57.2 m a.s.l.), a sediment core of 418 cm was investigated palynologically. The lake is situated in the county of Telemark in Southeast Norway. The pollen record consists of 245 pollen spectra and has a temporal resolution of c. 12-38 yr/cm. The chronology of the core is based on eight 14C dates from terrestrial plant remains and wood

    Towards a refined understanding of the use of coastal zones in the Mesolithic: New investigations on human–environment interactions in Telemark, southeastern Norway

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    The study of the effects of human presence on vegetation in the Mesolithic has been controversial. It is often assumed that hunter-gatherers did not change or affect their environment in a way that can be detected by means of pollen analysis. In this paper, we explore potential human impact on the vegetation during the Mesolithic by comparing pollen data from a high-resolution sediment core from Lake Skogstjern with archaeological data obtained through extensive excavation and survey in Bamble, in the county of Telemark, southeastern Norway. The aim of this interdisciplinary approach is to reach a better understanding of the development and use of Mesolithic woodlands with regard to the availability of different resources, but also to put the question of human impact on Mesolithic vegetation on the agenda. Mesolithic settlement in southeastern Norway was to a very large degree shore bound, and the pollen analysis from Lake Skogstjern, situated in the coastal hinterland, allows for new perspectives on and interpretations of the use of the coastal wider landscape. Wieckowska-Lüth, M., et al. "Towards a refined understanding of the use of coastal zones in the Mesolithic: New investigations on human–environment interactions in Telemark, southeastern Norway." Journal of Archaeological Science: Reports 17 (2018): 839-851. © 2018. This manuscript version is made available under the CC-BY-NC-ND 4.0 license
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