Kamerling Ilse M, Schofield J Edward, Edwards Kevin J, Aronsson Kjell-Åke
1Department of Geography and Environment, School of Geosciences, University of Aberdeen, Elphinstone Road, Aberdeen, AB24 3UF UK.
2Department of Archaeology, School of Geosciences, University of Aberdeen, Elphinstone Road, Aberdeen, AB24 3UF UK.
Veg Hist Archaeobot. 2017;26(4):369-388. doi: 10.1007/s00334-016-0596-5. Epub 2016 Nov 18.
The limited availability of historical and archaeological evidence means that much is still unknown about the development of Sami reindeer herding in Fennoscandia in both the recent and more distant past. To address this problem, high-resolution palynological analyses, C and Pb dating were undertaken on two adjacent (<25 m apart) peat profiles collected at a recently abandoned reindeer gathering pen () near Jokkmokk (~66.6°N, 19.8°E) in the boreal forest of northern Sweden. The aim was to assess the impact of Sami reindeer herding on the local environment through a study of pollen, coprophilous fungal spores, microscopic charcoal and sedimentology. The samples collected from within an annex to the indicate cycles of use and abandonment of the pen on a multi-decadal timescale between ~ad 1800-2008, most obviously in the coprophilous fungal spore archive. The pattern and timing of these cycles confirm events previously known only from oral histories. Although the local pollen assemblage zones associated with the phasing of activity were reproducible in a second peat core beyond the boundary of the , the coprophilous fungal spore signal in this paired profile was much less distinctive, possibly due to the typically shorter dispersal distances for these microfossils in comparison to pollen grains.
历史和考古证据的有限性意味着,对于近代和更久远过去芬诺斯坎迪亚地区萨米人驯鹿放牧的发展情况,仍有许多未知之处。为解决这一问题,对在瑞典北部针叶林约科莫克(北纬66.6°,东经19.8°)附近一个最近废弃的驯鹿圈栏(两者相距<25米)采集的两个相邻泥炭剖面进行了高分辨率孢粉学分析、碳和铅年代测定。目的是通过研究花粉、粪生真菌孢子、微观木炭和沉积学来评估萨米人驯鹿放牧对当地环境的影响。从该驯鹿圈栏附属建筑内采集的样本显示,在公元1800年至2008年的数十年时间尺度上,该圈栏存在使用和废弃的循环,这在粪生真菌孢子档案中最为明显。这些循环的模式和时间证实了此前仅从口述历史中得知的事件。尽管与活动阶段相关的当地花粉组合带在驯鹿圈栏边界之外的第二个泥炭岩芯中是可重现的,但在这个配对剖面中粪生真菌孢子信号的独特性要低得多,这可能是因为与花粉粒相比,这些微化石的典型传播距离较短。