| Summary of the Botanical Investigations Cupola Surface |
The cupola surface has retained a high water table despite the attempt
to drain it. This high and relatively stable water table has facilitated
a rapid recovery of the bog vegetation. The quadrats recorded show
that total vegetation cover of the surface varies between 75% (wet
areas) and 25% (in the driest areas). Most parts have a vegetation
cover of around 50%.
The plants recorded were those typically found on an intact bog, there
was a good balance between the species typical of wet aeas such as
the Sphagnum sp. And Narthecium ossifragum and those associated with
dry areas such as Calluna vulgaris.
Sphagnum species were found to be recovering well with development
spreading from fragments left behind after the surface vegetation was
removed. The occasional larger hummock was found which had escaped
removal. These appear to be acting as centres for the on-going recovery
process. In total, 7 species of Sphagnum were recorded on the cupola
including the principal hummock building species Sphagnum papillosum,
S, magellanicum and S. subnitens.
A total 20 species were recorded on the cupola. These included most
of the constant and companion species recorded for raised bogs in Northern
Ireland by Leach and Corbett (1987) and also in Britain in the National
Vegetation Classification (Rodwell, 1991).
Molinea caerulea was present in only one quadrat. This is a highly
invasive species which comes to dominate areas with low or highly fluctuating
water tables (Schouwenaars, 1988). Its near absence and the high cover
of Eriophorum species recorded indicates the continuation of stable
wet conditions which are needed for ombrotrophic bog vegetation development.
These areas were cut-over by hand for domestic fuel under turbary
arrangements, as was common throughout Ireland during the last few
hundred years (Van Eck, 1984). They are now little used and have been
allowed to revert to a semi-natural vegetation cover. Vegetation regeneration
of this type has been documented in Ireland by White (1930) among others
and it is currently being researched by the author at the University
of Ulster at Coleraine.
In recent years some areas have been re-worked by extrusion ‘sausage
machines. These areas are small relative to the area of the whole site,
and overall disturbance by extrusion machine cutting can be said to
be minimal. A range of different vegetation types in various stages
of development were found. Most notable were the mature cuttings which
had developed vegetation communities closely resembling those which
are found on intact raised bogs. All the species which were found on
the cupola were also found in the cuttings.
An additional 21 raised bog species were found in the cut-away areas.
Most notable amongst these was Vaccinium oxycoccus which is normally
only found growing across Sphagnum hummocks in the pool systems of
intact raised bogs. It was found on only 22 sites in Northern Ireland
by Leach and Corbett (1987). In this case it was found on only 22 sites
in Northern Ireland by Leach and Corbett (1987). In this case it was
found in cuttings which had developed a high cover of Sphagnum magellanicum
and other hummock building Sphagnum species.
Cuttings were also found with assemblages of species normally found
in the wetter parts of the pool areas of intact raised bogs. These
included Sphagnum recurvum and S,. cuspidatum and Narthecium ossifragum.
These cuttings are acting as refuge for the flora and fauna formerly
found on the bog surface. They are a rich and diverse source of species
which would be available for the regeneration of the damaged bog surface.
The northern edge of the bog has had little peat cutting compared
to the southern edge. The margin vegetation in the south is of ombnrotrophic
peat cutting communities. In the north however, adjacent to the Glenullin
Water, it is very different, with a community of fen species existing
along much of the margin.
This community closely resembles the lagg fen communities formerly
found on the margins of intact raised bogs but now very rare in Ireland.
Only 12 bogs in Northern Ireland were recorded as having any lagg fen
remaining by Leach and Corbett 1987). Forty one species typically found
in transitional bog/fen areas were recorded along the northern edge
of Glenullin Bog
During the survey buzzards and kestrels were seen hunting across the
bog. Numerous snipe were also seen. It was reported by local sources
that curlews nested on the bog this year. An otter spraint was observed
in the northern fen area adjacent to the river.
Despite the recent damage to the bog it remains a valuable ecological
resource.
1. The gross moprphology of the site remains intact. It is of special
value because of the combination of a large and relatively intact cupola,
and an extensive lagg fen area.
2. The continued presencec of a high water table on the cupola has
enabled a rapid revegetation of the bog surface with ombrotrophic bog
species.
3. The former cut-away areas surrounding the bog are a refuge for
the flora and fauna founace of the raised dome of the bog. Most notable
amongst the species found was Vaccinium oxycoccous. These are of value
as they provide species source of regeneration of the cupola.
Any further disturbance of the site would cause lasting damage to the
hydrology of the site. Any lowering of the water table will have the
effect of drying out the whole site, not just the central dome area.
This would be detrimental to the cology of the cutting and lagg areas
and cause changes in vegetation.
| Paleocological Investigations |
Glenullin Bog was used for paleocological investigation of the deglaciation
of the Agivey river basin by Johnson (1974). Peat cores were taken
from Glenullin Bog for pollen and macrofossil analysis. The aim was
to interpret the history of the vegetation of this area during the
end of the last ice age. Removal of the Glenullin deposit would prevent
any continuation of this work.
Aside from the ecological value of the site, the bog is an intrinsic
part of the landscape of Glenullin. It is a focal point for the whole
valley adding colour and texture to the overall scene. Removal of the
bog would seriously degrade the visual environment within Glenullin.
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