2013
DOI: 10.1371/journal.pone.0063086
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Long-Term Impacts of Forest Ditching on Non-Aquatic Biodiversity: Conservation Perspectives for a Novel Ecosystem

Abstract: Artificial drainage (ditching) is widely used to increase timber yield in northern forests. When the drainage systems are maintained, their environmental impacts are likely to accumulate over time and along accompanying management, notably after logging when new forest develops on decayed peat. Our study provides the first comprehensive documentation of long-term ditching impacts on terrestrial and arboreal biodiversity by comparing natural alder swamps and second-generation drained forests that have evolved f… Show more

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Cited by 41 publications
(21 citation statements)
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“…Two stands were old eutrophic boreo-nemoral stands and nine stands were post-wildfire stands in Scots pine-dominated dry boreal or paludified (Polytrichum and Vaccinium) sites (documented by [23,59], respectively). In six wildfire stands (three naturally regenerating and three salvage logged Our study system included 127 forest stands distributed among the following five common forest site-type groups (sensu [57]): (1) 35 dry boreal forests (mostly Vaccinium vitis-idaea type) on higher fluvioglacial landforms and till mounds with podzols (pH KCl 3.5 to 5.0) where the top layer is periodically dry and ground water deeper than 2 m; (2) 24 meso-eutrophic forests (mostly Oxalis type) on till mounds or rolling plains with podzols or stagnic Luvisols (pH KCl 3.2 to 4.2) where ground water is usually deeper than 2 m; (3) 26 eutrophic boreo-nemoral forests (mostly Aegopodium type) predominantly on undulating sandy till plains with favorably moist (in springtime anaerobic) Gleyic Cambisols or Luvisols (pH KCl 4.7 to 6.5) almost lacking organic horizon; (4) 20 mobile-water swamp forests on thin seasonally flooded Eutric histosols and Fluvisols with a peat layer >30 cm (pH KCl 5.0 to 6.5) in lowlands and valleys along rivers or around bogs; (5) 24 artificially drained swamp forests (Oxalis type, originating from type 4, see [16]) on well decomposed peat soils (pH KCl 4.0 to 6.5). The dry boreal stands were dominated by Scots pine (Pinus sylvestris) (Figure 2a-c); the other sites hosted conifer/deciduous mixtures with Norway spruce (Picea abies) ( Figure 2d-e) or, in some Oxalis type stands, with Scots pine.…”
Section: Study Areamentioning
confidence: 99%
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“…Two stands were old eutrophic boreo-nemoral stands and nine stands were post-wildfire stands in Scots pine-dominated dry boreal or paludified (Polytrichum and Vaccinium) sites (documented by [23,59], respectively). In six wildfire stands (three naturally regenerating and three salvage logged Our study system included 127 forest stands distributed among the following five common forest site-type groups (sensu [57]): (1) 35 dry boreal forests (mostly Vaccinium vitis-idaea type) on higher fluvioglacial landforms and till mounds with podzols (pH KCl 3.5 to 5.0) where the top layer is periodically dry and ground water deeper than 2 m; (2) 24 meso-eutrophic forests (mostly Oxalis type) on till mounds or rolling plains with podzols or stagnic Luvisols (pH KCl 3.2 to 4.2) where ground water is usually deeper than 2 m; (3) 26 eutrophic boreo-nemoral forests (mostly Aegopodium type) predominantly on undulating sandy till plains with favorably moist (in springtime anaerobic) Gleyic Cambisols or Luvisols (pH KCl 4.7 to 6.5) almost lacking organic horizon; (4) 20 mobile-water swamp forests on thin seasonally flooded Eutric histosols and Fluvisols with a peat layer >30 cm (pH KCl 5.0 to 6.5) in lowlands and valleys along rivers or around bogs; (5) 24 artificially drained swamp forests (Oxalis type, originating from type 4, see [16]) on well decomposed peat soils (pH KCl 4.0 to 6.5). The dry boreal stands were dominated by Scots pine (Pinus sylvestris) (Figure 2a-c); the other sites hosted conifer/deciduous mixtures with Norway spruce (Picea abies) ( Figure 2d-e) or, in some Oxalis type stands, with Scots pine.…”
Section: Study Areamentioning
confidence: 99%
“…Lobaria pulmonaria (epiphytic macrolichen) Dispersal/establishment Spatio-temporal connectivity of nemoral broad-leaved trees and aspen in reserves [42,77,96,[105][106][107][108] Menegazzia terebrata (epiphytic macrolichen) Air moisture and quality Hydrologically intact semi-open moist and wet forests [16,105,109,110] Chaenotheca gracilenta (epixylic microlichen) Microhabitat Supply of shady moist microhabitats on dying and uprooted old trees in reserves [15,43,50,105] Xylopsora friesii (epiphytic/epixylic microlichen) Disturbance regime Conifer forests with continuity of small-scale disturbances and slow-grown old trees [46,111] Species sensitive to reduced rotations and functioning of mature production stands…”
Section: Old-growth Dependent Species In Protected Forestsmentioning
confidence: 99%
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“…The protection of late-succession habitats and continuous forest areas (including areas with natural disturbances) is the primary goal in Estonian forest nature conserva-tion (Nature Conservation Act). Longtime human influence on forests and especially rapid intensification of forest clear-cutting and ditching during the last centuries have resulted in low continuity of forest landscapes (Laasimer, 1965;Lõhmus et al, 2004;Etverk & Meikar, 2008;Lõhmus & Kraut, 2010;Remm et al, 2013). Most especially valuable habitats in Estonia are now maintained within nature conservation areas or special strict protection zones in national parks and landscape protection areas.…”
Section: Introductionmentioning
confidence: 99%