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Conservation Council Phortaigh na hÉireann FOR BOGS & WILDLIFE Growing wiser wildlife gardening series Bog factsheets Bogs formation, ecology, distribution and conservation issues Current Issues Specific Campaign Actions Bog watch - a guide to how you can help the Save the Bogs Campaign |
Bog WoodlandsIntroduction The character and vegetation of bog
woodlands These woodlands are typically dominated by birch, usually downy birch but with occasional silver birch (Betula pendula) and sometimes scattered Scots pine (Pinus sylvestris). The trees form a light canopy 6-8m in height, occasionally over 10m, but sometimes much lower, under which occurs a shrub layer of willows (Salix cinerea ssp. oleifolia and S. aurita) and occasionally Scots pine and holly (Ilex aquifolium). A patchy dwarf shrub layer of ling heather (Calluna vulgaris), bilberry (Vaccinium myrtillus) and bog myrtle (Myrica gale), up to a metre in height, is typically present, sometimes intermixed with bramble (Rubus fruticosus agg.). Locally, the lower growing crowberry (Empetrum nigrum), cross-leaved heath (Erica tetralix) and bog rosemary (Andromeda polyfolia) may occur. The herb layer is rather variable and depends on the hydrology. In the wettest areas it is typically characterised by purple moor-grass (Molinia caerulea), cotton grasses (Eriophorum vaginatum and E. angustifolium), bottle sedge (Carex rostrata) and soft rush (Juncus effusus). In drier areas bent grass (Agrostis canina) and Yorkshire fog (Holcus lanatus) may occur with scattered ferns, e.g. buckler ferns (Dryopteris dilatata, D. spinulosa), locally stands of bracken and a little tormentil (Potentilla erecta). The most striking feature of these woodlands, however, is the mosses, particularly species of Sphagnum, which cover the ground to form a thick, spongy, hummocky carpet making walking difficult. The commonest species are the green or yellow-green Sphagnum palustre, S. recurvum, S. squarrosum and S. fimbriatum and the often red-tinged S. capillifolium. On the hummocks and in slightly drier areas a variety of other mosses occur, such as Hylocomium brevirostre, Polytrichum commune and Dicranum scoparium. Another moss, Aulacomnium palustre, indicative of slight water movement, is often present, and numerous smaller mosses and liverworts occur within these robust species. Sometimes this carpet of green is interrupted by patches of grey lichens, especially species of Peltigera and Cladonia, or scattered with the pink flowers or, in autumn and winter, the bright red berries, of cranberry (Vaccinium oxycoccus), which trails over the surface. The trees and shrubs are often festooned with grey-green epiphytic lichens, such as species of Ramalina and Usnea and mosses. Stands of birch with sally (Salix cinerea ssp. oleifolia) also occur very locally in mineral-rich flushes on the edge of the Mayo blanket bogs in the vicinity of Bellacorick. These have been described by Cross (1987) and, in more detail, by Lockhart (1991). They are perhaps better described as scrub as the trees rarely exceed 2-2.5 m in height. The dwarf shrub layer consists of bog myrtle, ling heather and cross-leaved heath. Purple moor grass, black bog-rush (Schoenus nigricans) and devil's bit scabious (Succisa pratensis) are the most common herbs while the presence of bog bean (Menyanthes trifoliata) and reed (Phragmites australis) indicate the very wet nature of the terrain. A variety of mosses, including Aulacomnium palustre, Hylocomium splendens, Rhytidiadelphus squarrosus and the rare Homalothecium nitens also occur. Similar types of birch woodland with well developed carpets of mosses occur occasionally among fen-carr vegetation. These probably represent a stage in the succession from fen to bog where ground water influence is declining. This is discussed in the chapter on fens. Where are bog woodlands found? The stands of birch in the blanket bog flushes occur in very different types of situation. They are present in areas where water seeps up through the underlying mineral-rich substrate and then flows across the bog surface. The water is much less acidic than on the raised bogs and has higher levels of calcium and magnesium. If burning and grazing were removed these stands of birch might expand. In general bog woodlands are small and usually confined to the uppermost part of flushes. The largest, c. 20 ha in extent, is that on All Saint's Bog, Co. Offaly, which was described in detail by Cross (1987). This site is probably drying out as a result of peat removal to the north and east, a process which may encourage expansion of the birch onto the drier peat but will lead ultimately to the loss of the species requiring wet conditions. Only very few bog woodlands are known today but, as the evidence of Osvald and Father Moore indicate, it is probable that in the past they were more widespread. The following raised bogs contain bog woodlands: Addergoole, Corliska, Kilmore and Kilnaborris Bogs, Co. Galway; Clooneen Bog, Co. Longford; All Saint's and Clara Bog, Co. Offaly; Ballynamona, Cloonlarge, Shanville and Trien Bogs, Co. Roscommon. The birch stands in Mayo all occur in the Bellacorrick area. Conservation importance of bog woodlands In early summer large numbers of green hairstreak butterflies (Callophyrs rubi), whose caterpillars feed on bilberry, among other plants, may be seen flying around the birch trees. Dead trees, both standing and fallen, are frequently present providing habitat for fungi and wood dwelling insects. O'Connor and Speight (1987) found a rare fly, Dictenidia bimaculata, which is recognized as part of the ancient forest fauna of Europe, in rotting wood in two bog woodlands (Clara and All Saint's Bog). This suggests that these woodlands have been present on the bog, or have occurred in close proximity to other woodlands, for a very long period. Evidence from the peat on Clara Bog, however, suggests that the woodland there has developed only within the last 150 years. Conclusion References Copyright Dr John Cross |