Blanket Bogs

Total Page:16

File Type:pdf, Size:1020Kb

Blanket Bogs SCOTTISH INVERTEBRATE HABITAT MANAGEMENT Blanket bogs Claish Moss © Scottish Natural Heritage Introduction that may also provide important sub-habitats. Britain has about 10-15% of the total global area Invertebrates in upland moorland or bog habitats of blanket bog, making it one of the most are an essential component of the diet of many important international locations for this habitat. bird species; cranefly larvae and adults have 80-85% of Britain’s blanket bog habitat is found in been shown to be important food for grouse Scotland, covering 1.8 million hectares, and chicks and breeding waders, such as Golden representing 23% of the country’s land area. This plover. Adult grouse may also eat craneflies to makes Scotland an internationally important supplement their diet of heather shoots. country for blanket bog. Managing habitats to benefit these invertebrates Blanket bog is found in cool, wet, typically is thus likely to have a significant impact on the oceanic climates, where it can cover whole survival of upland birds. landscapes, such as in the North-West of In addition, the Scottish Invertebrate Species Scotland. Peat accumulates slowly over many Knowledge Dossiers: Pseudoscorpiones years and can reach depths exceeding 5m, indicated the possibility that the Bog chelifer although 0.5-3m is more typical. Blanket bog is (Microbisium brevifemoratum ) is likely to occur in “ombrotrophic”, that is, the water and mineral Scottish bogs—highlighting that there may yet be supply comes entirely from atmospheric sources unrecorded species in this important Scottish (rainwater, mist, cloud-cover). The water habitat (Legg, 2010). chemistry is nutrient-poor and acidic and the Support for management described in this habitat is dominated by acid-loving plant document is available through Scotland Rural communities, especially Sphagnum mosses. A Development Programme (SRDP) Rural blanket mire landscape may also contain Development Contracts (RDC). A summary of minerotrophic systems (those that are affected by this support (at time of publication) can be found ground-water and the nutrients in it), such as in this document. springs, flushes, stream margins and valley mires. These support different vegetation types Threats eroding peat both in gullies and flatter areas. Peat extraction Eutrophication of water supply Peat extraction may be either domestic or Examples of potential causes of eutrophication commercial, and results in habitat loss. (nutrient enrichment) include run-off from road drainage, agricultural pollution, and nutrient Drainage enrichment from sewage. Drainage ditches, both new and old will lower the Water-course liming water table and may initiate erosion and oxidation of the peat. Even unmaintained old drains will Blanket bog habitats are naturally acidic. If lime is continue to affect the hydrology of a site. added to lochs, lakes and rivers as a treatment Lowered water tables will alter the species for acidification, this may have a detrimental composition of the surface vegetation and have a effect on adjacent areas of blanket bog. detrimental affect on specialist invertebrates. Fertilisers Drainage at the margins of bogs will lower the The application of fertilisers and lime to increase water table and may modify the surface stock grazing productivity will inevitably modify patterning, such as loss of Sphagnum hollows. the ecology to the detriment of the blanket bog Afforestation by exotic conifers invertebrate fauna. Coniferous trees have been planted on extensive Atmospheric pollution areas of blanket bog in the past. The trees will Many bogs, especially those in the North of continue to affect the hydrology and species England, have been affected by atmospheric composition of adjacent areas of blanket mire as pollution. This alters nutrient availability, and they mature and require more water. hence the plant community composition. Afforestation has generally been accompanied by furrowing of the ground, and these highly destructive drainage channels become a long- lasting scar. Habitat management Development Maintain the hydrology The construction of wind farms and As a peat bog consists of 95-98% water held by communication masts, together with associated Sphagnum peat, the water level is the most infrastructure such as access and maintenance crucial aspect to consider when managing this roads can cause significant hydrological Priority habitat type. Operations some distance disruption. Links to the national grid via landlines away from the ombrotrophic Sphagnum or more usually pylons also have an impact on communities can therefore have a devastating very fragile blanket bog during construction. effect if they are on sites within the same hydrological unit. In order to conserve the Livestock & game management characteristic bog communities, it is necessary to Heavy grazing (by Sheep, Red deer, Cattle and look at the whole system, which may extend Horses) will have a significant impact on mire beyond the boundaries of a particular site. vegetation, especially if there is supplementary Drainage ditches and forestry plantations will feeding (which will increase the nutrient input) remove water from surface layers of the bog and and other management measures such as ultimately lower the bog surface, favouring plants drainage, burning or fencing. which grow in drier conditions, thus adversely affecting any specialist invertebrate species. Wet Burning blanket bog is of great importance to many Serious fires can result in the loss of surface invertebrates such as spiders and leaf-hopper vegetation and the death of peat-forming species. bugs. Drying peat will shrink and oxidise, creating These can slowly recover over time (>20 years), erosion problems and increasing vulnerability to but invertebrate communities and populations will fire damage, so it is essential to maintain water be seriously affected. levels. On sites that are drying, raising the water Erosion levels should be considered. Erosion on blanket bog exposes more of the peat Blocking any existing drains to retain rainwater to the atmosphere, increasing drying and will allow the water table to re-stabilise and peat- oxidation of the peat. Hag erosion may be forming Sphagnum species to colonise areas that instigated, resulting in extensive patches of bare have dried or been affected by peat cutting or milling. Unless the peat has been removed down Page 2 Blanket bogs to the level of the mineral substrate, secondary Prevent nutrient enrichment and pollution of bog vegetation will return over time. Water flow is the water table essential for some species, such as the caddisfly Pollution incidents and nutrient enrichment lead Oxyethira mirabilis , so care should be taken that to the loss of Sphagnum bog vegetation reducing any work does not compromise the survival of its ability to support species. these invertebrates. The use of pesticides should also be avoided. Maintain habitat diversity Prevent invasion of scrub and trees It is important to maintain a habitat mosaic both within and beyond the bog. The natural structure If water table levels are maintained then of the surface of an undamaged blanket bog significant scrub invasion should not present a provides a variety of aquatic and semi-aquatic major problem as the very wet, infertile ground habitats each supporting different invertebrates. conditions, altitude and exposure of the blanket Management should aim to recognise and bogs often makes tree or shrub growth difficult. monitor these valuable microhabitats: boggy However, in areas of bog that have already pools, flushes, wet peat, sedge ( Carex spp.) and begun to dry as a result of drainage or rush ( Juncus spp.) stands and localised poor fen. agricultural operations, scrub invasion can be Retaining extensive areas of inundated prevented by cutting or light grazing, but it is Sphagnum is particularly important for important not to overgraze. Grazing can cause invertebrate species with a high nature problems to blanket bog habitats, causing conservation status. damage to the vegetation by trampling and affecting the species composition if nutrient It is also important to consider the fringes of bogs enrichment occurs by the deposition of dung. and ensure that they support a rich marginal vegetation. Tussocky vegetation of taller Molinia Afforestation is a major threat to this habitat and spp., Carex spp. or Juncus spp. and the should be discouraged. associated litter build-up provides cooler, more Minimise disturbance sheltered microhabitats for adult craneflies and Excessive trampling through over-grazing or drier sites for over-wintering invertebrates such large numbers of ramblers is a problem, as it as spiders. Ericaceous dwarf shrubs also support affects the growth of fragile Sphagnum mosses many heather-feeding moths and other insects, and can ultimately alter the species composition as well as providing a well-developed vegetation or lead to erosion of the peat. structure for spiders. Scrub on the fringes of blanket bog in habitats such as streamsides Natural pools within the Sphagnum lawns should supports its own fauna and provides shelter; be left unmanaged and not cleared or deepened. sallow catkins may be the best spring nectar source for many adult insects. Exceptions to general habitat management Avoid burning Ampedus pomorum is a nationally scarce click Burning destroys large numbers of invertebrates, beetle associated with the dead heartwood of potentially entire populations of species living mature birch trees and is characteristic
Recommended publications
  • Wind Turbines, Sensitive Bird Populations and Peat Soils
    Charity No. 229 325 Wind Turbines, Sensitive Bird Populations and Peat Soils: A Spatial Planning Guide for on-shore wind farm developments in Lancashire, Cheshire, Greater Manchester and Merseyside. July 2008 For more details, contact Tim Youngs [email protected] or Steve White [email protected] Produced by the RSPB and The Wildlife Trust for Lancashire, Manchester & North Merseyside (LWT), in partnership with Lancashire County Council, Natural England and the Merseyside Environmental Advisory Service (EAS) 1 Contents Section Map Annex Page Background 2 How to use the alert maps 4 Introduction 4 Key findings 5 Maps showing ‘important populations’ of ‘sensitive bird 1-5 6- 10 species’ and deep peat sensitive areas in Lancashire, Cheshire, Greater Manchester and Merseyside Legal protection for birds and habitats 11 Methodology and definitions 12- 15 Caveats and notes 16 Distribution of Whooper Swan, Bewick’s Swan and Pink- 17- 22 footed Goose in inland areas of Lancashire, Cheshire, Greater Manchester and Merseyside Thresholds for ‘important’ populations’ (of sensitive species) 1 23 Definition of terms relating to ‘sensitive species’ of bird 2 24 Background The Inspectors who carried out the Examination in Public of the draft NW Regional Spatial Strategy (RSS) between December 06 to February 07, proposed that 'Maps of broad areas where the development of particular types of renewable energy may be considered appropriate should be produced as a matter of urgency and incorporated into an early review of RSS'. This proposal underpins the North West Regional Assembly’s (NWRA) research that is being carried out by Arup consultants. The Secretary of State's response is 'In line with PPS22, we consider that an evidence-based map of broad locations for installation of renewable energy technologies would benefit planning authorities and developers.
    [Show full text]
  • Questioning Ten Common Assumptions About Peatlands
    Questioning ten common assumptions about peatlands University of Leeds Peat Club: K.L. Bacon1, A.J. Baird1, A. Blundell1, M-A. Bourgault1,2, P.J. Chapman1, G. Dargie1, G.P. Dooling1,3, C. Gee1, J. Holden1, T. Kelly1, K.A. McKendrick-Smith1, P.J. Morris1, A. Noble1, S.M. Palmer1, A. Quillet1,3, G.T. Swindles1, E.J. Watson1 and D.M. Young1 1water@leeds, School of Geography, University of Leeds, UK 2current address: Centre GEOTOP, CP 8888, Succ. Centre-Ville, Montréal, Québec, Canada 3current address: Geography, College of Life and Environmental Sciences, University of Exeter, UK _______________________________________________________________________________________ SUMMARY Peatlands have been widely studied in terms of their ecohydrology, carbon dynamics, ecosystem services and palaeoenvironmental archives. However, several assumptions are frequently made about peatlands in the academic literature, practitioner reports and the popular media which are either ambiguous or in some cases incorrect. Here we discuss the following ten common assumptions about peatlands: 1. the northern peatland carbon store will shrink under a warming climate; 2. peatlands are fragile ecosystems; 3. wet peatlands have greater rates of net carbon accumulation; 4. different rules apply to tropical peatlands; 5. peat is a single soil type; 6. peatlands behave like sponges; 7. Sphagnum is the main ‘ecosystem engineer’ in peatlands; 8. a single core provides a representative palaeo-archive from a peatland; 9. water-table reconstructions from peatlands provide direct records of past climate change; and 10. restoration of peatlands results in the re-establishment of their carbon sink function. In each case we consider the evidence supporting the assumption and, where appropriate, identify its shortcomings or ways in which it may be misleading.
    [Show full text]
  • Assessment on Peatlands, Biodiversity and Climate Change: Main Report
    Assessment on Peatlands, Biodiversity and Climate change Main Report Published By Global Environment Centre, Kuala Lumpur & Wetlands International, Wageningen First Published in Electronic Format in December 2007 This version first published in May 2008 Copyright © 2008 Global Environment Centre & Wetlands International Reproduction of material from the publication for educational and non-commercial purposes is authorized without prior permission from Global Environment Centre or Wetlands International, provided acknowledgement is provided. Reference Parish, F., Sirin, A., Charman, D., Joosten, H., Minayeva , T., Silvius, M. and Stringer, L. (Eds.) 2008. Assessment on Peatlands, Biodiversity and Climate Change: Main Report . Global Environment Centre, Kuala Lumpur and Wetlands International, Wageningen. Reviewer of Executive Summary Dicky Clymo Available from Global Environment Centre 2nd Floor Wisma Hing, 78 Jalan SS2/72, 47300 Petaling Jaya, Selangor, Malaysia. Tel: +603 7957 2007, Fax: +603 7957 7003. Web: www.gecnet.info ; www.peat-portal.net Email: [email protected] Wetlands International PO Box 471 AL, Wageningen 6700 The Netherlands Tel: +31 317 478861 Fax: +31 317 478850 Web: www.wetlands.org ; www.peatlands.ru ISBN 978-983-43751-0-2 Supported By United Nations Environment Programme/Global Environment Facility (UNEP/GEF) with assistance from the Asia Pacific Network for Global Change Research (APN) Design by Regina Cheah and Andrey Sirin Printed on Cyclus 100% Recycled Paper. Printing on recycled paper helps save our natural
    [Show full text]
  • Peat from Penguins to Palm Trees
    Organic Soils in the UK Overseas Territories and Crown Dependencies. Peat from Penguins to Palm Trees Janet Moxley [email protected] (CEH), Chris Evans (CEH), Nicole Archer (BGS), Mary-Ann Smyth (Crichton Carbon Centre) Introduction The UK has 14 Overseas Territories (OTs) and 3 Crown Dependencies (CDs). The Falkland Islands contain large areas of organic soils, with smaller areas in the Isle of Man and the Caribbean OTs. Where sufficient data are available GHG emissions from the OTs and CDs which have ratified or are likely to ratify the UN Framework Convention on Climate Change and the Kyoto Protocol are included in the UK GHG inventory. We review current understanding of organic soils in these areas. The Falkland Islands Estimates of peat area vary between 282 kha (BGS and CEH, unpublished data) and 548 kha (Wilson et al, 1993). The BGS/CEH estimate assumes that all valley-bottom deposits, and 33% of upland organo-mineral soils on shallow slopes, are peat, based on new field survey data. Falkland peatlands comprise a mixture of upland blanket bog covered with Astelia pumila, White grass (Cortadelia pilosa), Diddle Dee (Empetrum rubrum), and white grass-dominated valley mire. Rainfall is low, resulting in only low presence of Sphagnum magellanicum, and (combined with high wind speeds) in high susceptibility to erosion. The main pressures are from grazing by large numbers of sheep, use of prescribed fire for vegetation management, dredging of stream channels to increase drainage, wildfires, effects of historic bomb craters, domestic peat extraction, and the use of turf banks as windbreaks. Peat distribution has been mapped, but peat condition has not been documented.
    [Show full text]
  • Blanket Bog Toolkit
    BLANKET Outcomes and BOG improvements LAND MANAGEMENT GUIDANCE CONTENTS Introduction 3 Introduction 3 How to use this pack 4 Blanket bog toolkit This guidance for land managers and conservation advisers has been collaboratively 7 State 2: Bare Peat produced by representatives of the Uplands Management Group (UMG) in response to a 11 State 3: Dwarf shrub dominated blanket bog request from the Uplands Stakeholder Forum (USF) for best practice guidance. 15 State 4: Grass and/or sedge dominated blanket bog 19 State 5: Modified blanket bog It is designed to put into practice the joint voluntary Defra Blanket Bog Restoration Strategy agreed by the Uplands Stakeholder Forum (USF). 23 State 6: Active hummock/hollow/ridge blanket bog This guidance will enable land managers to take steps to improve the vegetation characteristics and hydrological properties of blanket bog, which is defined by a peat depth of over 0.4m, across the uplands of England (see Q1–2). The five agreed outcomes (see Q5) sought by land managers and conservationists via this approach are: = the capture and storage of carbon = improved water quality and flow regulation = high levels of biodiversity = a healthy red grouse population = good quality grazing The UMG provides practitioner input to the USF, chaired by Defra. The Group seeks to produce guidance for practitioners covering a range of upland management activity. For more information go to: www.uplandsmanagement.co.uk HOW TO USE THIS PACK The guidance consists of: = DECISION MAKING TOOLKIT Use it out on the hill to agree the starting condition of the blanket bog and to decide on the best management methods to improve it.
    [Show full text]
  • Ecohydrological Characteristics of a Newly Identified Coastal Raised Bog on the Western Olympic Peninsula, Washington State, USA
    Received: 3 September 2020 Revised: 12 December 2020 Accepted: 9 February 2021 DOI: 10.1002/eco.2287 RESEARCH ARTICLE Ecohydrological characteristics of a newly identified coastal raised bog on the western Olympic Peninsula, Washington State, USA F. Joseph Rocchio1 | Edward Gage2 | Tynan Ramm-Granberg1 | Andrea K. Borkenhagen2 | David J. Cooper2 1Washington Department of Natural Resources, Natural Heritage Program, Abstract Olympia, Washington, USA In western North America, ombrotrophic bogs are known to occur as far south as 2 Department of Forest and Rangeland coastal regions of British Columbia. A recent discovery of a peatland with a raised Stewardship, Colorado State University, Fort Collins, Colorado, USA peat surface on the western Olympic Peninsula in Washington State (Crowberry Bog), USA, suggested that the distribution range of this ecosystem type extends fur- Correspondence F. Joseph Rocchio, Washington Department of ther south along the coast. To confirm if the site was an ombrotrophic peatland, we Natural Resources, Natural Heritage Program, analysed its topography, hydrologic regime, water chemistry and vegetation. LiDAR Olympia, WA, USA Email: [email protected] data indicated that the peatland is elevated nearly 3 m above the surrounding land- scape. Water table variations in the plateau were strongly associated with seasonal Present address Andrea K. Borkenhagen, Advisian, Calgary, and daily precipitation events, indicating ombrotrophy. The hydraulic gradient on the Alberta, Canada. plateau is downward through most of the year, demonstrating that precipitation is percolating vertically into deeper peat layers. In the rand, the hydraulic gradients are horizontal over much of the year, indicating that the plateau is draining through the rand to the lagg.
    [Show full text]
  • JNCC Guidelines for the Selection of Sssis
    SUBJECT TO REVISION For further information see http://jncc.defra.gov.uk/page-2303 Guidelines for the selection of biological SSSI’s Part 2: Detailed guidelines for habitats and species groups 8 BOGS To view other chapters of the guidelines visit : http://jncc.defra.gov.uk/page-2303 SUBJECT TO REVISION For further information see http://jncc.defra.gov.uk/page-2303 8 BOGS 1 Introduction 1.1 Ombrotrophic (rain-fed) mire, so called because its mineral nutrients are derived principally from rainfall rather than ground-water sources, is the other main class of peatland. In Britain these mires are termed bogs and in contrast to fens, which are fed by mineral-enriched waters, their vegetation is characterized by acidophilous upland communities in which the genus Sphagnum usually is, or has been, a conspicuous component. In the humid, oceanic climate of Britain, “ombrogenous” (= rain-generated) bogs are an especially important element of the original range of vegetation formations. They are an extensive feature of western and northern areas, where measurable rain falls on two days out of three. This regular input of precipitation produces a fairly constant level of surface seepage on many bogs, which gives rise to other distinctive communities which in Fennoscandia would be regarded as fen (minerotrophic mire) but in Britain are considered to be part of bog complexes. In lowland areas with predominantly acidic substrata there are examples of valley and basin mires which received acidic surface seepage giving rise to ombrotrophic vegetation similar to that of ombrogenous mire. These may be classifies as fen/bog complexes (see Chapter 7, section 4, NCC 1989).
    [Show full text]
  • Valuing Wetlands
    Wetland Futures Report 2013: The Value of Healthy Wetlands Citation Freeman, H. (2014) Wetland Futures 2013: The Value of Healthy Wetlands, Wildfowl & Wetlands Trust Steering group contributors THE TRUSTS Sponsors Front cover: wetlands discovery, Arundel photo: Heather Tait Contents Executive summary 2 Healthy wetlands for land management Jason Beedell 15 Acknowledgements 3 The benefits of healthy wetlands from a local Introduction 4 planning perspective Prof. Alister Scott 16 Keynote speech Prof. Chris Baines 5 Ripon City Quarry: a corporate ecosystem valuation Overall policy panel Delia Shannon 17 Two key sectors to engage with – agriculture & planning Constructed wetlands: a water company Alister Driver 6 perspective Dr Gabriela Dotro 18 Scotland: wetland policy challenges and opportunities The International Water Stewardship Standard Lisa Webb 7 Claire Bramley 18 Wetlands in Wales: key challenges for Natural Working with wetlands: achieving catchment Resources Wales benefits for wetlands and land managers Chris Uttley 8 on Tweed Prof. Chris Spray 19 Wetlands and agricultural panel Peat and food security The Great Fen project: the multiple benefits of Prof. Joe Morris 9 wetland restoration Kate Carver 20 Catchment Sensitive Farming James Grischeff 11 Floodplain meadows project: the multiple benefits A farming perspective Prof. David Gowing 21 Richard Murray Wells 11 Implications of an ecosystem service agenda What is the value of wetlands? for wetland conservation Dr Peter Glaves 12 Dr Richard Bradbury 22 The economics of ecosystems and Climate change and wetlands biodiversity (TEEB) for water and wetlands Dr Mike Morecroft 22 Daniela Russi 12 Introduction to the Blueprint for Water Waterlogged wealth: realising the multiple Carrie Hume 23 benefits of healthy wetlands Prof.
    [Show full text]
  • Blanket Bog Blanket Bog Is One of the Most Important Habitats in the Park
    Blanket Bog Blanket bog is one of the most important habitats in the Park. Bogs consist of waterlogged soils upon which only a limited number of plants will survive. The Park contains the best example of bog in the east coast of Ireland. Formation of Blanket Bogs Around 4000 years ago Ireland's climate became wetter and milder. Heavy rainfall caused minerals to be leached from the soil forming an impermeable layer in the soil known as an iron pan. Water couldn't soak through this layer, so the soil above the iron pan became waterlogged and peat began to form. Peat is brownish/black in colour and consists of approximately 90% water. Peat is made up of partially decomposed remains of dead plant material, which have accumulated on top of each other over thousands of years. The dead plant material consists of mosses, grasses and heathers. The roots of trees are often found in bogs. These trees are from ancient forests that were swallowed by the bog. The lack of oxygen prevents the complete breakdown of the plant material, resulting in the formation of peat. Peat only grows about 1mm a year but can reach depths of several metres. The name 'blanket bog' is derived from the fact that these bogs consist of a carpet of peat extending over large areas of land. Blanket bogs receive all their nutrients from rainfall, resulting in very acidic conditions (pH levels from 3.5 to 4.2). The lack of nutrients, low oxygen levels and high acidity means that there are only certain plants that will grow in this hostile environment.
    [Show full text]
  • Conservation
    Offshore Energy SEA 3: Appendix 1 Environmental Baseline Appendix 1J: Conservation A1j.1 Introduction and purpose There is a wide range of international treaties and conventions, European and national legislation and other measures which have application in relation to the protection and conservation of species and habitats in the UK. These are summarised below as a context and introduction to the site listings which follow. This Appendix provides an overview of the various types of sites relevant to the SEA which have been designated for their international or national conservation importance as well as sites designated for their wider cultural relevance such as World Heritage Sites and sites designated for landscape reasons etc. Other non-statutory sites potentially relevant to the SEA are also included. Using a Geographic Information System (GIS), coastal, marine and offshore sites were identified relevant to each of the regional sea areas and mapped. Terrestrial sites which are wholly or in part within a landward 10km coastal buffer and selected other sites are also mapped. Terrestrial sites outside the buffer are not included here with the exception of summaries for sites whose interest features might be affected by activities offshore e.g. sites designated for breeding red throated divers which may feed offshore. Maps are grouped for each Regional Sea with a brief introduction followed by an outline of the sites and species of nature conservation importance within that Regional Sea. Regional Sea areas 9, 10 and 11 have no contiguous coastline and contain only offshore conservation sites and are grouped with Regional Sea 8. Regional Sea 5 also has no contiguous coastline; it is grouped with Regional Sea 4.
    [Show full text]
  • Wetlands-Different Types, Their Properties and Functions
    Technical Report TR-04-08 Wetlands – different types, their properties and functions Erik Kellner Dept of Earth Sciences/Hydrology Uppsala University August 2003 Wetlands – different types, their properties and functions Erik Kellner Dept of Earth Sciences/Hydrology Uppsala University August 2003 Keywords: Bog, Wetlands, Mire, Biosphere, Ecosystem, Hydrology, Climate, Process. This report concerns a study which was conducted for SKB. The conclusions and viewpoints presented in the report are those of the author and do not necessarily coincide with those of the client. A pdf version of this document can be downloaded from www.skb.se Summary In this report, different Swedish wetland types are presented with emphasis on their occurrence, vegetation cover, soil physical and chemical properties and functions. Three different main groups of wetlands are identified: bogs, fens and marshes. The former two are peat forming environments while the term ‘marshes’ covers all non-peat forming wetlands. Poor fens are the most common type in Sweden but (tree-covered) marshes would probably be dominating large areas in Southern Sweden if not affected by human activity such as drainage for farming. Fens and bogs are often coexisting next to each other and bogs are often seen to be the next step after fens in the natural succession. However, the development of wetlands and processes of succession between different wetland types are resulting from complicated interactions between climate, vegetation, geology and topography. For description of the development at individual sites, the hydrological settings which determine the water flow paths seem to be most crucial, emphasizing the importance of geology and topography.
    [Show full text]
  • Carbon Sequestration in Blanket Bogs
    Doolough Protection Group …………….seeking the conservation of our environment and the future of our community. CARBON SEQUESTRATION IN BLANKET BOGS - ESSAY - January 2005 Carbon sequestration in blanket bogs 1. Introduction Mention carbon sequestration by natural ecosystems, and lush tropical rainforests come to mind. It comes thus as a surprise to learn that peatlands can absorb more carbon per hectare and per year than tropical rainforests, and that standing stocks of carbon per hectare are also on average higher than in tropical rainforests. It is estimated that peatlands contain on average 5,000 tonnes of carbon per hectare and absorb carbon from the air at 0.7 tonnes per hectare per year. Globally, peat bogs contain more carbon than all the world's tropical rainforests. They are estimated to store 3.0 - 4.6 x 10 17 g C within 350 million ha.[1] A particular type of peatlands, blanket bogs, cover 10 million hectares of the earth's surface. Ireland possesses 8% of the world's blanket bogs and is the most important country in Europe for this type of habitat. [2] 2. Description of blanket bog habitat [2] There are two major peatland types found in Ireland: fens, which are alkaline and connected to ground water, and bogs, which are acid and rely solely on nutrient-poor rainwater. Bogs can be further divided into two different types: raised bogs and blanket bogs. Blanket bogs are found along the west coast of Ireland and in mountainous areas around the country where rainfall is 1,200mm per year or more. Depending on the altitude, scientists distinguish between Atlantic blanket bog (below 200m) and mountain blanket bog (above 200m).
    [Show full text]