Latest News - Day Five - Ecological Briefing - The Berghaus Dragon's Back Race™

Day Five - Ecological Briefing

26th Jun 2015

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Above: At the 2012 Dragon's Back Race competitors head towards the summit of Fan Brycheiniog. © Jon Brooke

 

THE FOLLOWING INFORMATION IS PRESENTED TO THE COMPETITORS

 

The Berghaus Dragon’s Back Race™ passes through the full range of Wales’ outstanding upland landscapes, including all of the highest mountain ranges in the country. These are recognised as areas of national and international importance for their upland wildlife habitats, flora and fauna. Occasionally, the features that provide this interest can be vulnerable to the wear and tear that may result from the passage of Berghaus Dragon’s Back Race™ competitors. The risk of ecological damage is carefully assessed during early stages in the planning process for the event, when every effort is made to avoid the need for competitors to cross areas of special ecological interest. 

For situations where competitors might need to pass through areas of ecological sensitivity we are keen to encourage personal route selection choices that avoid the risk of local ecological disturbance. This Ecological Briefing Note has been prepared for Day Five of the 2015 Berghaus Dragon’s Back Race™ event to identify key features that contribute to the special ecological value of the event area, with route selection comments to help minimise the risk of localised ecological disturbance.


 

DAY FIVE INTRODUCTION

 

The northern section of the 2015 Berghaus Dragon’s Back Race Day™ Five event area passes through lower lying farmland before crossing the striking upland landscape of the western Brecon Beacons (Black Mountain), part of the Brecon Beacons National Park. 

Features of special nature conservation interest are concentrated within the southern section of the event area, a landscape of varied sedimentary geology with often spectacular glacial landforms. The great variety of rock types and topography within the southern part of the event area is reflected in a variety of upland wildlife habitat and vegetation types. Extensive tracts of significant upland habitat and vegetation are present, including widespread areas of national and international nature conservation importance. These typically comprise a variety of sub-montane grassland types that have developed within an area of considerable geological variety. In places patches of blanket bog have developed, occasionally occupying extensive areas.

The majority of sub-montane dry acid grassland and calcareous grassland vegetation types along the Day Five route are relatively robust in terms of potential trampling damage from competitors. In places, however, vegetation and habitats are more vulnerable to disturbance. These include locations where upland wet grassland and bog vegetation is present, and several locations known for their striking arctic alpine flora. In addition, a number of streams are present within the southern part of the event area that are of potentially significant ecological interest.


DAY FOUR ECOLOGY


•    Dry acid grassland is a widespread vegetation type within the event area, formed where centuries of livestock grazing has converted heather moorland to open grassland. These areas provide a relatively robust vegetation type that can generally withstand the trampling effects of fell running. 

•    Specialised arctic-alpine plant species are present at locations within dry acid grassland on higher level, north-facing slopes throughout the event area. These species are part of a relict post-glacial flora that survives in British uplands and comprises some of the most highly valued nature conservation sites in the Brecon Beacons National Park. It is important to avoid vegetation disturbance wherever possible in situations where route choices involve crossing steep, north-facing slopes.

•    Nutrient-rich groundwater can appear as springs on high level, steep slopes where vegetation rich in specialised arctic-alpine moss and liverwort species can be present. Wherever possible, route choices should avoid disturbance to these features.

•    Areas of wet acid grassland will be encountered where impeded drainage occurs within relatively level acid grassland areas or where groundwater emerges at the surface as seepages across more steeply sloping ground. Wet acid grassland can be of special nature conservation interest, in particular where groundwater seepages provide conditions for communities of specialised mosses, liverworts and other plants. These vegetation types can be vulnerable to persistent disturbance effects of trampling and should ideally be avoided wherever possible by selecting routes that keep to dry acid grassland to by-pass wet grassland patches.

•    Wet acid grassland at groundwater seepages on steep ground can be difficult to avoid where they cross valuable contouring lines. Complete avoidance of these areas could involve a significant route change and deviation from the desired contour level. Despite this, it would be ideal if damage to seepage zone vegetation could be minimised, often located within shallow gulleys, re-entrant features or associated with ground level rock outcrops that cross steep slopes.

•    Dry calcareous grassland is a locally extensive vegetation type within the western part of the event area, occurring as hill pasture over limestone and lime-rich moraine deposits. This vegetation type is often accompanied by low rock outcrops and scree slopes. Dry calcareous grassland within the Brecon Beacons is an important vegetation type, and includes several uncommon plant species. The vegetation typically forms on relatively shallow soils and as such can be quickly eroded by trampling. Some of the highest quality grassland of this type develops on shallow soils over limestone rock outcrops and within areas of limestone scree and as such are especially vulnerable to erosion. Care should be taken with route selection through areas with grassland, limestone rock outcrops and scree to avoid excessive vegetation wear, especially when negotiating vegetated outcrops and scree.

•    On hillsides, soil movements within dry acid and calcareous grassland areas can develop well-defined micro-terrace systems, often referred to as sheep walks or trods. These typically follow the contours and can provide extremely useful running lines. Grassland vegetation at the edge of these micro-terraces is often friable and easily dislodged. Care should be taken when using these features for contouring to avoid running on the edge of these terraces to minimise grassland damage. Areas of saturated ground can occur where groundwater issues into terrace formations. These locations are especially vulnerable to running damage and should be avoided where possible.

•    Blanket bog is an important feature of several locations within the event area. Many of these areas comprise degraded blanket bog where peat hags (erosion gulleys) have formed where bog vegetation has been lost and the underlying peat is being eroded. Vegetation loss may have been caused by a variety of factors in the past such as air pollution, moorland management with burning and drainage, but the resulting loss of peat and blanket bog vegetation is an important conservation management issue for the Brecon Beacons National Park.  In many cases, the bare peat exposed in hags may have become stabilised, allowing a slow recovery of blanket bog vegetation that will eventually help to prevent the loss of peat through erosion. More locally, areas of high quality, intact blanket bog are present within the event area. These comprise vegetation with a high proportion of Sphagnum mosses on deep peat with limited evidence of peat erosion and gulley formation.

•    Disturbance of recovering blanket bog by runners churning through the peat hags has the potential to trigger further peat erosion by de-stabilising the peat surface. Wherever possible, route choices in these areas should try to link the strips and patches of surviving moorland vegetation between the peat hags. These are often quite well-drained, providing areas of relatively robust vegetation and resistant to the trampling effects of running. If crossing peat hags is unavoidable, routes should try to link cushions of remnant moorland vegetation as ‘stepping stones’ across the bare peat surfaces. In some situations, the extent of peat erosion has been sufficient to expose the bedrock and glacial material underlying the peat. Running on this material is unlikely to cause significant harm to recovering peat surfaces.

•    Limestone pavement is present at locations to the west of the event area, providing features of considerable nature conservation importance. The main ecological interest within this area is associated with communities of mosses, ferns and other plants that utilise the special microclimate of deep cracks (grykes) within the limestone pavement. Their location deep within the limestone pavement will ensure that they are protected from disturbance by runners. Occasionally, patches of limestone grassland are present on the surface of the pavement and these are vulnerable to fragmentation by disturbance from runners, and should be avoided if possible when selecting routes across limestone pavement areas. In addition to their botanical interest, limestone pavements are of considerable geological interest. Weathering the limestone surface has formed a variety of finely sculpted rock flutings and runnels with friable edges that could be easily snapped off when running across the pavements. This risk should be considered when selecting routes in the limestone pavement area.

•    The event area contains a complex network of streams and rivers, some of which are potentially vulnerable to ecological disturbance from repeated crossing by runners. In particular, stream channels within the event area that cross limestone bedrock have the potential to support valuable populations of a highly protected aquatic invertebrate species called the White Clawed Crayfish. This animal is generally inactive during the day, and if present during the race will be sheltering in burrows excavated into stream margins. Other important mammal species may be present along stream margins, including Otter and Water Vole. Wherever possible, stream crossings should avoid sliding down banks into streams to avoid the potential for disturbing the stream margin burrows and resting places of these animals.