Abstract

The two major aims of this study are (1) To test the performance of the Landscape Reconstruction Algorithm (LRA) to quantify past landscape changes using historical maps and related written sources, and (2) to use the LRA and map reconstructions for a better understanding of the origin of landscape diversity and the recent loss of species diversity. Southern Sweden, hemiboreal vegetation zone. The LRA was applied on pollen records from three small bogs for four time windows between AD 1700 and 2010. The LRA estimates of % cover for woodland/forest, grassland, wetland, and cultivated land were compared with those extracted from historical maps within 3-km radius around each bog. Map-extracted land-use categories and pollen-based LRA estimates (in % cover) of the same land-use categories show a reasonable agreement in several cases; when they do not agree, the assumptions used in the data (maps)-model (LRA) comparison are a better explanation of the discrepancies between the two than possible biases of the LRA modeling approach. Both the LRA reconstructions and the historical maps reveal between-site differences in landscape characteristics through time, but they demonstrate comparable, profound transformations of the regional and local landscapes over time and space due to the agrarian reforms in southern Sweden during the 18th and 19th centuries. The LRA was found to be the most reasonable approach so far to reconstruct quantitatively past landscape changes from fossil pollen data. The existing landscape diversity in the region at the beginning of the 18th century had its origin in the long-term regional and local vegetation and land-use history over millennia. Agrarian reforms since the 18th century resulted in a dramatic loss of landscape diversity and evenness in both time and space over the last two centuries leading to a similarly dramatic loss of species (e.g., beetles).

Highlights

  • These changes were accompanied by large decreases in landscape diversity and evenness, from a relatively even distribution of small patches woodland, grassland, and wetland in TW4 to a less even distribution of larger and smaller land-use/landscape/vegetation units (LuVs) patches with a strong dominance of woodlands and wetlands in time windows (TW) 3 and 2, and a very uneven and monotonous landscape in TW1 with an almost continuous cover of woodlands/forests with few small patches of wetlands and rare patches of grasslands and cultivated land

  • Given that the sources of errors are numerous in both the extraction of land-use/vegetation data from historical maps and the Landscape Reconstruction Algorithm (LRA) reconstructions, the agreement between the two is strikingly good in many of the scenarios

  • A comparison of our test with two other tests of the LRA in NW Europe suggests that careful harmonization of LuVs between different historical maps and between maps and LRA reconstructions, as performed in our study, may improve testing the LRA, in particular for LuVs woodland/forest, grassland, and wetland

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Summary

Introduction

Reconstruction of past vegetation/landscape change in quantitative terms (e.g., percentage (%) cover or biomass of plant taxa) at both regional and local spatial scales may be required to answer questions related to past land cover-climate interactions (e.g. Gaillard et al 2010; Strandberg et al 2014), landscape management and biodiversity conservation (e.g., Smith et al 2010; Lindbladh et al 2013), human impact on natural vegetation (e.g., Nielsen and Odgaard 2010; Fyfe et al 2013), and general land cover/land use – environment relationships (e.g., Dearing 2006). Reconstruction of past vegetation/landscape change in quantitative terms (e.g., percentage (%) cover or biomass of plant taxa) at both regional and local spatial scales may be required to answer questions related to past land cover-climate interactions Pollen-based reconstruction of past vegetation abundance in quantitative terms has long been a challenge for palynologists (Sugita 1994). This is due to the fact that pollen loading in lakes or bogs includes two components: (1) the local pollen coming from plants within a relevant source area of pollen (RSAP sensu Sugita 1994; see definition below) and (2) the background pollen coming from plants outside the RSAP.

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