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Pollardstown Fen.(Letter to Members about impact of Kildare Bypass on the Fen)
Pollardstown Fen lies in a shallow depression. It is maintained by groundwater which continuously flows into the fen from approximately 40 springs and seepage zones. Most of the springs arise around the margins of the depression above the level of the fen and carry groundwater from the Curragh Aquifer. The Curragh, or mid-Kildare Aquifer, is a large gravel aquifer which extends below and beyond the Curragh Plains. The Curragh itself is a unique semi-natural, acid grassland on shallow soils over an extensive glacial outwash plain. The gravels of the plain reach a depth of 75m in places. The gravel aquifer has a large catchment area. Its hydrogeology is significant as it is an important source of baseflow for rivers and streams, it influences the ecology of a number of interesting habitats and it is the source of water for Pollardstown Fen. The continual inflow of water at the fen creates waterlogged conditions which lead to peat formation. There are layers of calcareous marl in the fen peats which reflect inundation by calcium-rich water. The peat - marl deposit reaches 6m at its deepest point and is underlain with clay. The fen has been relatively, undisturbed except for some human influence over the last 1,000 years in the form of diversion of the natural water outflow (to power a number of mills and to supply the Grand Canal), turf-cutting and an attempt to reclaim the fen for agriculture in the 1960's and 70's. The fen was re-flooded in 1983 to redress the effects of the attempted reclamation. Subsequent to the reclamation most of the fen has been purchased by the State. The outflow from the fen supplies water to the Grand Canal. The existence of the Grand Canal depends on the uninterrupted flow of water from the Curragh Aquifer via the fen. The pristine quality of water is maintained by its passage through the gravel aquifer and fen wetlands. To the north of Pollardstown are extensive acid-peat bogs. Most ancient Irish fens (similar to Pollardstown) transformed into boglands by growing above the influence of groundwater. The constant inflow of calcium-rich water to Pollardstown did not allow acid-peat to develop (small patches exist on the margins) and the fen, therefore, has remained unchanged for thousands of years. Today, it represents an example of ancient landscape. The Curragh-Pollardstown system has existed and has reached equilibrium over the last 12,000 years. Its undisturbed, slow development has allowed its unique ecology to develop and its many rare species to survive.
Habitats and speciesHabitatsThe vegetation of Pollardstown Fen is varied and species-rich with numerous well-defined plant communities and several rare or unusual species. The dominant plant species are saw-sedge (Cladium mariscus), common reed (Phragmites australis), blunt-flowered rush (Juncus subnodulosus) and a variety of sedges. Scrub vegetation has not developed on the fen but there are free-standing shrubs of willow (Salix sp.). The central fen area is dominated by more uniform and less nutrient-demanding vegetation types such as saw-sedge Cladium mariscus. On the margins, where the water first emerges from the ground, there are species and communities characteristic of more nutrient-rich conditions. Damp grasslands on the margins are species-rich with particularly good displays of orchids in some areas. Regenerating fen occurs on an area of reclaimed land which was re-flooded in 1983 and has now reverted to open water, swamp and fen. Some of the springs are up-welling, some are seepage zones where water oozes from the ground. A number of springs have tufaceous deposits where solid calcium carbonate precipitates from the calcium-rich water. Some of the more unusual species and communities of the fen are located in the vicinity of these tufaceous springs. There are more than sufficient indicator species present to categorize the fen as priority habitat with reference to the E.U. Habitats Directive. Three E.U. Annex 1 habitats can be identified at Pollardstown Fen. Approximately half of it corresponds to habitat Alkaline Fen. Most of the remainder is regarded as the priority habitat Calcareous fens with Cladium mariscus and Carex davalliana. Tufaceous springs are rare and are protected as the E.U. Annex 1 habitat Petrifying springs with tufa formation. Species
Orchids :
Other flowering plants :
Sedges :
Rushes :
Mosses :
Invertebrates : A number of internationally important invertebrates including Diptera (true flies) have been recorded from the site. The rare hoverfly Platycherius amplus was discovered in 1988. 159 species of distinctive and highly interesting butterfly and moth have been recorded. Several scarce fenland moths occur at Pollardstown. Between 1984 and 1990 the first Irish recording of Cosmopterix lienigiella and Elachista triatomea were made. The E. U. Annex l1 species **Marsh fritillary butterfly (Eurodryas aurinia) has also been seen on the fen. A total of 58 spider species have been recorded on the fen. The species Pirata tenuitarsis and Centromerus levitarsis were first recorded for Ireland on the fen in 1993/94.
Vertebrates The fen has ornithological importance for both breeding and wintering birds. Little grebe, teal, mallard, water rail, coot, moorhen, snipe, sedge warbler and reed bunting all breed annually within the fen vegetation. Reed warbler and garganey, both rare breeding species in Ireland, have been recorded at Pollardstown and may have bred. In recent years two very specialized bird species associated with fens, Marsh harrier and Savi's warbler, have been seen at Pollardstown. Woodcock have also been seen. Since the reflooding of the central part of the fen in 1983 wintering waterfowl have been attracted in increasing numbers.
National and international importance
2 Natural Heritage Area (N.H.A.)
3 Special Area of Conservation (S.A.C.)
4 Ramsar Site Ramsar provides for the conservation of wetlands of international importance listed in the Ramsar Convention. A wetland should be considered as internationally important if it is a particularly good example of a specific type of wetland characteristic of its region. The convention notes the presence of rare, vulnerable, endemic or endangered plants or animals as a factor in determining international importance. 47 Ramsar Sites in Ireland, 549 worldwide.
5 Biogenetic Reserve
The Proposed Kildare By-pass
An unfortunate situation has arisen in Co. Kildare in relation to the Kildare Town by-pass. Misconceptions have crept into conversations and debates, both in the public and private domain. Some direct anger at "environmentalists"; others admit to being confused. An Taisce, snails, myself and others have been accused of "trying to stop the motorway". A form of social impasse has crept into the county. This is unfortunate and unfounded since everybody agrees that there must be a solution to Kildare's traffic problems in the interests of those who live in and pass through the county.
The confusion has arisen out of confusion. There has been a lack of available information as to what is really happening. It is most important, at the outset, to state clearly that it is not the existence or route of the motorway which is currently under discussion. The design of the road, whereby it is to be built under the water table, could have consequences for the county. Nobody is trying to stop the construction of the motorway. A number of serious issues have arisen in relation to the construction of the by-pass. These must be explained in the interests of the future of the county and its inhabitants. The following is a summary of procedures, an account of what has happened and is happening. It has been written with reference to the relevant public documentation and professional experience in the area of E.I.S.
Traffic. In recognition of the need for a solution to the traffic congestion Kildare County Council designed a motorway to join the Curragh dual-carriageway with the proposed Monasterevan by-pass. South of Kildare town from the Curragh, between the National Stud and Kildare and joining road close to Monasterevan. Pollardstown Fen could be affected by the construction of the Kildare by-pass following the current design. Pollardstown Fen is well known to most people in Kildare and is now central to the debate on the by-pass. Pollardstown Fen is an area of immense scientific and ecological interest. It is a unique area, having developed from lakes of water left by melting ice after the Ice Age 12,000 years ago. It is a marsh, a post-glacial fen, the only of its kind in Ireland and the best example of its type in Europe. The reason for its uniqueness is that other such fens have long since changed naturally into boglands or have been lost to land drainage. Because it is an ancient habitat it has a number of rare species, both plant and animal, many of which are protected by Irish and European law. The fen depends on inflow of water from the Curragh for its existence. Water drains constantly from the Curragh into the fen. This water flows naturally from the fen via the New River and the Milltown Feeder. The latter is the main source of water for the Grand Canal. The water enters the fen via approximately 40 landsprings and seepage zones. Some of these seepage zones are themselves protected by law. It is important to note the term seepage zone. The flow of water to the fen is from an ancient underground system which has developed and settled over 12,000 years. Most of the water seeps into the fen and flow is not the equivalent of stream or river flow. The fen is held in great respect by many people in Newbridge and other areas around the county. It is visited by individuals, families, parents with children, bird-watchers, teachers, scientific groups. It is held in awe by many who have never even visited the site. It is, therefore, important to the well-being of many people in Kildare. This is a positive interaction with environment. This term interaction is significant - see below.
National Stud
Curragh aquifer and gravels. In the centre of Co. Kildare there is a major aquifer, called the Curragh or Mid-Kildare aquifer. The name "Curragh" aquifer may be misleading since it lies under, not only the Curragh, but an area stretching to the Hill of Allen, Nurney, Suncroft, Newbridge and Kilcullen. It covers an area of approximately 200 square km. Water flows from the aquifer to Pollardstown Fen and the Tully streams. Water movements within the aquifer are extremely complex and there is evidence of movements of water between the Liffey and Barrow via the aquifer. Experts agree that much of the groundwater movement is still unknown.
E.I.S. procedure The purpose of the E.I.A. is, therefore, to identify and eliminate possible problems at the planning stage of a development. E.I.A. should not leave problems unsolved or questions unanswered. E.I.S. are public documents and should be available for inspection by any member of the public.
The problem As a result of this cutting 5.5 million gallons of water will be lost per day forever more from the Curragh aquifer. The water table will fall and there will be consequences for the surrounding areas. Consequences which have been identified are listed below. It is agreed that a reduced volume of water will reach Pollardstown fen. The exact amount of the loss is in dispute but there will be consequences for the fen (see below). The current argument centres around the loss of water to the fen since it is protected by the 1976 Wildlife Act, E.U. law and international agreements relating to Council of Europe Biogenic Reserves and Ramsar Convention. The E.U. cannot fund a project which is likely to damage an area which they have declared to be legally protected.
Story to date
In the Introduction to their report the OPW outlined that Kildare County Council had selected the route without having first taken full account of the relative impacts of alternatives on Pollardstown Fen. They also stated that the Council "seem to have focussed on negotiating the route with the National Stud". It was agreed with the National Stud that the road would be built in a deep cutting to alleviate visual and noise impact and that the parcel of land separated from the main body of the Stud would be rezoned for development which would be of financial benefit to the Stud. The E.I.S. stated that horses are generally not adversely affected by noise and air from motorways but to further reduce the impact on horses in the Stud the road would be built in a deep cutting. The remainder of the report dealt with grave concerns for Pollardstown Fen, the Grand Canal and other areas. It was the opinion of the OPW that the E.I.S. was inadequate, fraught with uncertainties, based on insufficient information and failed to adequately study alternatives. They also outlined concerns for :
Rushden report Dispelling the Misconceptions Mr. Tony Lowes is Chairperson of the Natural Environment Group of An Taisce. An Taisce is a non-government organisation , a respected national organisation who lobby for better policies for Ireland in relation to the natural and built environment. They are a recognised environmental watchdog. An Taisce became aware of the OPW and Chief Planner's Report in 1998 and Mr. Lowes sent these to the European Commission, as is his accepted responsibility. He has not tried to stop the construction of the motorway. He merely argues the proposal to build the road below the water table and has the full support of An Taisce in this matter.
Snails
Road deaths
General concerns The trivialisation of the by-pass issue is damaging in many ways. It detracts from the overall picture of what is happening to and what is good for Kildare. Kildare, as a county is at risk. If the worst case scenario does become a reality Kildare could loose the Pollardstown Fen (a unique habitat). The Curragh , King's Bog, local wetlands streams, vegetation will be affected. Buildings and homes could be affected. The Grand Canal and tourism could suffer. One can imagine the consequence for the social fabric of Kildare. Where are people to go if the worst happens when the traffic has sped by on Friday evenings? Where will they bring their children? How will they feel about their own surroundings? This is negative interaction which has already started with the doubts which are cast over Kildare. For the well-being of its people the county must be intact. Is it worth the risk for the sake of raising the road to the surface. A problem has been identified, albeit at the last hour. Let the E.I.S. process now work for Kildare and its people. This issue is very much about people (Letter to Members about impact of Kildare Bypass on the Fen)
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