Abstract

Blanket peatlands are globally rare, and many have been severely eroded. Natural recovery and revegetation (‘self-restoration’) of bare peat surfaces are often observed but are poorly understood, thus hampering the ability to reliably predict how these ecosystems may respond to climatic change. We hypothesised that morphometric/topographic-related microclimatic variables may be key controls on successional pathways and vegetation patterning in self-restoring blanket peatlands. We predicted the occurrence probability of four common peatland plant species (Calluna vulgaris, Eriophorum vaginatum, Eriophorum angustifolium, and Sphagnum spp.) using a digital surface model (DSM) generated from drone imagery at a pixel size of 20 cm, a suite of variables derived from the DSM, and an ensemble learning method (random forests). All four species models provided accurate fine-scale predictions of habitat suitability (accuracy > 90%, area under curve (AUC) > 0.9, recall and precision > 0.8). Mean elevation (within a 1 m radius) was often the most influential variable. Topographic position, wind exposure, and the heterogeneity or ruggedness of the surrounding surface were also important for all models, whilst light-related variables and a wetness index were important in the Sphagnum model. Our approach can be used to improve prediction of future responses and sensitivities of peatland recovery to climatic changes and as a tool to identify areas of blanket peatlands that may self-restore successfully without management intervention.

Highlights

  • The results suggest poor vertical accuracy due to the absence of Ground control points (GCPs) during processing, precision was high ($ 11 cm) and the digital surface model (DSM) was deemed fit for purpose, stated elevation values should be interpreted as relative rather than absolute

  • We used topographic and morphometric variables derived from a high-spatial-resolution DSM to investigate microtopographic controls on vegetation patterning in a blanket peatland recovering from erosion

  • This study is the first of its kind to use a fine-scale topographic model to explore the wide range of factors thought to influence revegetation in eroded blanket peatlands

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Summary

Introduction

They occur in disjunct oceanic and hyper-oceanic high-latitude regions where precipitation (mostly rainfall) is common throughout the year and maintains wet conditions at the soil surface so that peat-forming plants (principally Sphagnum mosses and the cotton grasses (Eriophorum spp.)) can establish (Lindsay 2010 Unpublished; Gallego-Sala and Prentice 2013). In such areas, peat may cover or cloak whole landscapes. Despite suggestions that blanket peatlands formed in response to forest clearance in the Neolithic and Bronze Age (for example, Tallis 1998), there is strong evidence they are natural phenomena (Lawson and others 2007; Gallego-Sala and others 2016)

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