Abstract

Vegetation is changing across the Arctic in response to increasing temperatures, which may influence archaeological sites in the region. At the moment, very little is known about how different plant species influence archaeological remains. In this study we visited 14 archaeological sites stretching across a climatic gradient from the outer coast to the inner fjords in the Nuuk Fjord area of West Greenland to assess the impact of vegetation growth on archaeological preservation. Examination of the physical disturbance of archaeological layers and materials by roots from different plant species showed that horsetail (Equisetum arvense) was particularly destructive because of its deep penetrating rhizomes and ubiquity across the study area. Willow (Salix glauca) also caused physical disturbance due to a dense root network, but its roots were mainly found in the upper 30 cm of the soil. Focus was also given to the impact from vegetation on the visibility of sites, where growth of willow was found be the main problem, especially in the inner fjords. Historic descriptions and aerial photographs from the sites show that shrub growth was already widespread in the region by the 1930s, but photos of some of the sites investigated show that the willow shrubs are significantly taller today, which has decreased the visibility of site features. The impact from horsetail and willow on archaeological sites may be mitigated using geotextiles and grazing by livestock, but both methods require further studies before being implemented in the study area.

Highlights

  • Archaeological sites in the Arctic represent an irreplaceable record of human history

  • The present study focuses on two effects from vegetation: (1) root damage to buried archaeological remains and (2) limited access and reduced visibility of the archaeological sites due to vegetation overgrowth

  • We evaluate if the impact from vegetation has increased significantly in recent years, if the impacts are similar on archaeological sites compared to those on surrounding areas, and if it is possible to mitigate the negative effects from the vegetation

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Summary

Introduction

Archaeological sites in the Arctic represent an irreplaceable record of human history. Several recent studies show that vegetation patterns are currently changing in Arctic and alpine areas, with shrub habitat especially increasing (Normand et al, 2013; Formica et al, 2014; Myers-Smith et al, 2015a). It is currently uncertain if these results apply to archaeological sites, as their vegetation cover may differ from the surrounding areas due to accumulated soil nutrients (Forbes, 1996; Derry et al, 1999; Forbes et al, 2002; Fenger-Nielsen et al, 2019). These effects have only been discussed for archaeological sites in temperate regions and not for the Arctic, where the ongoing vegetation changes call for an urgent study of the effects

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