Knockfin Heights: a high-altitude Flow Country peatland showing extensive erosion of uncertain origin

Peatland erosion has important implications for ecosystem services such as carbon storage and biodiversity conservation. The extensive blanket bogs of Scotland’s Flow Country include some of the least damaged peatlands in the UK; nevertheless, erosion features occur widely in the area. Here we descr...

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Main Authors: M.H. Hancock, B. England, N.R. Cowie
Format: Article
Language:English
Published: International Mire Conservation Group and International Peatland Society 2018-10-01
Series:Mires and Peat
Subjects:
Online Access:http://mires-and-peat.net/media/map23/map_23_02.pdf
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author M.H. Hancock
B. England
N.R. Cowie
author_facet M.H. Hancock
B. England
N.R. Cowie
author_sort M.H. Hancock
collection DOAJ
description Peatland erosion has important implications for ecosystem services such as carbon storage and biodiversity conservation. The extensive blanket bogs of Scotland’s Flow Country include some of the least damaged peatlands in the UK; nevertheless, erosion features occur widely in the area. Here we describe a high-altitude (340–440 m) heavily eroded peatland at Knockfin Heights in the Flow Country. The causes of this erosion are poorly understood, and could include both human and natural factors. Restoration management has been considered for the site, although this might be unnecessary if spontaneous recovery is taking place. Our study aimed to contribute to understanding whether recovery was occurring, by (i) accurately and repeatably measuring bare peat extent using ground surveys, in 2005; and (ii) comparing the fullness of pools (strictly, pool area covered in standing water) using aerial photographs taken during 1946–2016. Estimated bare peat cover in the study area in 2005 was 10.5 % (95 % confidence limits 6.8–15). When placing a horizontal 1 m cane on the ground, bare peat was recorded under an average of 2.7 (2.2–3.2) 10 cm sections out of a possible maximum of ten per cane. Bare peat was most extensive on the flattest ground. Pools largely covered by standing water made up 30–60 % of pools in five pool groups, in five surveys during 1946–2005; but 75 % (standard error ~ 8) in 2016 - significantly higher than some earlier years. Active restoration management is merited for anthropogenic erosion but is more questionable for erosion that arose naturally or shows strong spontaneous recovery. We recommend follow-up studies during the next ten years to clarify the trajectories and causes of erosion at Knockfin; specifically, a repeat of this ground survey alongside remote sensing, experimental and palaeoecological work.
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spelling doaj.art-32f0020840e7411f8d04c74e06989d162023-09-03T02:30:22ZengInternational Mire Conservation Group and International Peatland SocietyMires and Peat1819-754X2018-10-01230212010.19189/MaP.2018.OMB.334Knockfin Heights: a high-altitude Flow Country peatland showing extensive erosion of uncertain originM.H. Hancock0B. England1N.R. Cowie2RSPB Centre for Conservation Science, Inverness, Scotland, UKRSPB Centre for Conservation Science, Inverness, Scotland, UKRSPB Centre for Conservation Science, Edinburgh, Scotland, UKPeatland erosion has important implications for ecosystem services such as carbon storage and biodiversity conservation. The extensive blanket bogs of Scotland’s Flow Country include some of the least damaged peatlands in the UK; nevertheless, erosion features occur widely in the area. Here we describe a high-altitude (340–440 m) heavily eroded peatland at Knockfin Heights in the Flow Country. The causes of this erosion are poorly understood, and could include both human and natural factors. Restoration management has been considered for the site, although this might be unnecessary if spontaneous recovery is taking place. Our study aimed to contribute to understanding whether recovery was occurring, by (i) accurately and repeatably measuring bare peat extent using ground surveys, in 2005; and (ii) comparing the fullness of pools (strictly, pool area covered in standing water) using aerial photographs taken during 1946–2016. Estimated bare peat cover in the study area in 2005 was 10.5 % (95 % confidence limits 6.8–15). When placing a horizontal 1 m cane on the ground, bare peat was recorded under an average of 2.7 (2.2–3.2) 10 cm sections out of a possible maximum of ten per cane. Bare peat was most extensive on the flattest ground. Pools largely covered by standing water made up 30–60 % of pools in five pool groups, in five surveys during 1946–2005; but 75 % (standard error ~ 8) in 2016 - significantly higher than some earlier years. Active restoration management is merited for anthropogenic erosion but is more questionable for erosion that arose naturally or shows strong spontaneous recovery. We recommend follow-up studies during the next ten years to clarify the trajectories and causes of erosion at Knockfin; specifically, a repeat of this ground survey alongside remote sensing, experimental and palaeoecological work.http://mires-and-peat.net/media/map23/map_23_02.pdfaerial photographsbare peatblanket bogdeerpools
spellingShingle M.H. Hancock
B. England
N.R. Cowie
Knockfin Heights: a high-altitude Flow Country peatland showing extensive erosion of uncertain origin
Mires and Peat
aerial photographs
bare peat
blanket bog
deer
pools
title Knockfin Heights: a high-altitude Flow Country peatland showing extensive erosion of uncertain origin
title_full Knockfin Heights: a high-altitude Flow Country peatland showing extensive erosion of uncertain origin
title_fullStr Knockfin Heights: a high-altitude Flow Country peatland showing extensive erosion of uncertain origin
title_full_unstemmed Knockfin Heights: a high-altitude Flow Country peatland showing extensive erosion of uncertain origin
title_short Knockfin Heights: a high-altitude Flow Country peatland showing extensive erosion of uncertain origin
title_sort knockfin heights a high altitude flow country peatland showing extensive erosion of uncertain origin
topic aerial photographs
bare peat
blanket bog
deer
pools
url http://mires-and-peat.net/media/map23/map_23_02.pdf
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AT nrcowie knockfinheightsahighaltitudeflowcountrypeatlandshowingextensiveerosionofuncertainorigin