Burns Bog Ecological Conservancy Area Management Plan May 2007
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Riparian Vegetation Management
Engineering in the Water Environment Good Practice Guide Riparian Vegetation Management Second edition, June 2009 Your comments SEPA is committed to ensuring its Good Practice Guides are useful and relevant to those carrying out activities in Scotland’s water environment. We welcome your comments on this Good Practice Guide so that we can improve future editions. A feedback form and details on how to send your comments to us can be found at the back of this guide in Appendix 1. Acknowledgements This document was produced in association with Northern Ecological Services (NES). Page 1 of 47 Engineering in the Water Environment Good Practice Guide: Riparian Vegetation Management Second edition, June 2009 (Document reference: WAT-SG-44) Contents 1 Introduction 3 1.1 What’s included in this Guide? 3 2 Importance of riparian vegetation 6 3 Establishing/creating vegetation 8 3.1 Soft or green engineering techniques 8 3.2 Seeding and planting of bare soil 10 3.3 Creating buffer strips 11 3.4 Planting trees and shrubs 15 3.5 Marginal vegetation 18 3.6 Urban watercourses 21 4 Managing vegetation 24 4.1 Management of grasses and herbs 24 4.2 Management of heath and bog 27 4.3 Management of adjacent wetlands 28 4.4 Management of non-native plant species 29 4.5 Management of scrub and hedgerows 31 4.6 Management of individual trees 31 4.7 Management of trees – riparian woodland 33 4.8 Management of trees – conifer plantations 35 4.9 Large woody debris 37 4.10 Marginal vegetation 37 4.11 Urban watercourses 40 4.12 Use of herbicides 40 4.13 Environmental management of vegetation 41 4.14 Vegetation management plans 41 5 Sources of further information 42 5.1 Publications 42 5.2 Websites 44 Appendix 1: Feedback form – Good Practice Guide WAT-SG-44 45 Page 2 of 47 1 Introduction This document is one of a series of good practice guides produced by SEPA to help people involved in the selection of sustainable engineering solutions that minimise harm to the water environment. -
A Unique Raised Bog at Urbana, Ohio.*
A UNIQUE RAISED BOG AT URBANA, OHIO.* ROBERT B. GORDON, Ohio State University. Located just north of the Champaign County Fair Grounds at Urbana, Ohio, is a unique dome-shaped bog, covered with shrubby vegetation for the most part, in which the center is raised at least ten feet above the margins. An old road crosses the bog. I have been told that it was once the main thorofare from Urbana to Columbus. Horses and wagons passed over it, I suppose, the drivers never realizing that a mat of fibrous roots less than one foot thick was all that held them over a body of water twelve feet in depth. Raised bogs, called "high moors" and "Hochmoore" in foreign literature, have long been known throughout Europe. N. S. Shaler is credited by Nichols with being the first to call attention to these peculiar swamps in North America, in 1888-89. Those which Shaler observed were "mostly limited to the eastern portion of Maine, near the shores of the Bay of Fundy," but some of lesser magnitude were reported for New Hampshire, northern Michigan, and Minnesota. Similar bogs, with centers about 13 feet above their margins, have been reported in the province of New Brunswick by Ganong (1897). Nichols (1919) described bogs of this type encountered in Maine, in which the elevation of the center above the margin varied from 2 or 3 feet to as high as 18 feet (e. g., Denbo Heath, covering several square miles in area). He asserts: "(1) that in the state of Maine raised bogs, in so far as they constitute a distinctive swamp type, are virtually restricted to the proximity of the seacoast; and (2) that in other portions of New England and of the eastern United States this type of bog is practically absent, although in occasional swamps it is possible to detect a slight elevation of the surface above the level of permanent ground water." Warming (1909) has summarized concisely the characteristic features of "Hochmoore." They owe their development to the growth of sphagnum mosses which absorb water that falls in the form of rain or snow. -
National Water Summary Wetland Resources: Maine
National Water Summary-Wetland Resources 213 Maine Wetland Resources M aine is rich in wetland resources. About 5 million acres, or one System Wetland description fourth of the State, is wetland. Maine has a wide variety of wetlands, Palustrine .................. Nontidal and tidal-freshwater wetlands in which ranging from immense inland peatlands to salt marshes and mud vegetation is predominantly trees (forested wet flats along the coast. lands); shrubs (scrub-shrub wetlands); persistent Wetlands are an integral part of Maine's natural resources. or nonpersistent emergent, erect, rooted herba ceous plants (persistent- and nonpersistent Wetlands provide essential habitat for certain types of wildlife and emergent wetlands); or submersed and (or) vegetation, including rare and endangered species. They are used floating plants (aquatic beds). Also, intermit for timber and peat; hunting, fishing, and shellfishing; education tently to permanently flooded open-water bod and research; and bird, wildlife and plant observation, all of which ies of less than 20 acres in which water is less than 6.6 feet deep. boost tourism and the general economy. Wetlands also provide flood control, bank and shoreline-erosion control, sediment retention, lacustrine ................. Nontidal and tidal-freshwater wetlands within an intermittently to permanently flooded lake or water fi ltration, and nutrient uptake. In recognition of the impor reservoir larger than 20 acres and (or) deeper tance of wetlands, many government and private organizations have than 6.6 feet. Vegetation, when present, is pre worked to preserve wetlands and educate the public about wetland dominantly nonpersistent emergent plants (non values. For example, the Maine Department of Conservation owns persistent-emergent wetlands), or submersed and (or) floating plants (aquatic beds), or both. -
This Document Was Withdrawn on 6 November 2017
2017. November 6 on understanding withdrawn was water for wildlife document This Water resources and conservation: the eco-hydrological requirements of habitats and species Assessing We are the Environment Agency. It’s our job to look after your 2017. environment and make it a better place – for you, and for future generations. Your environment is the air you breathe, the water you drink and the ground you walk on. Working with business, Government and society as a whole, we are makingNovember your environment cleaner and healthier. 6 The Environment Agency. Out there, makingon your environment a better place. withdrawn was Published by: Environment Agency Rio House Waterside Drive, Aztec West Almondsbury, Bristol BS32 4UD Tel: 0870document 8506506 Email: [email protected] www.environment-agency.gov.uk This© Environment Agency All rights reserved. This document may be reproduced with prior permission of the Environment Agency. April 2007 Contents Brief summary 1. Introduction 2017. 2. Species and habitats 2.2.1 Coastal and halophytic habitats 2.2.2 Freshwater habitats 2.2.3 Temperate heath, scrub and grasslands 2.2.4 Raised bogs, fens, mires, alluvial forests and bog woodland November 2.3.1 Invertebrates 6 2.3.2 Fish and amphibians 2.3.3 Mammals on 2.3.4 Plants 2.3.5 Birds 3. Hydro-ecological domains and hydrological regimes 4 Assessment methods withdrawn 5. Case studies was 6. References 7. Glossary of abbreviations document This Environment Agency in partnership with Natural England and Countryside Council for Wales Understanding water for wildlife Contents Brief summary The Restoring Sustainable Abstraction (RSA) Programme was set up by the Environment Agency in 1999 to identify and catalogue2017. -
Lowland Raised Bog (UK BAP Priority Habitat Description)
UK Biodiversity Action Plan Priority Habitat Descriptions Lowland Raised Bog From: UK Biodiversity Action Plan; Priority Habitat Descriptions. BRIG (ed. Ant Maddock) 2008. This document is available from: http://jncc.defra.gov.uk/page-5706 For more information about the UK Biodiversity Action Plan (UK BAP) visit http://www.jncc.defra.gov.uk/page-5155 Please note: this document was uploaded in November 2016, and replaces an earlier version, in order to correct a broken web-link. No other changes have been made. The earlier version can be viewed and downloaded from The National Archives: http://webarchive.nationalarchives.gov.uk/20150302161254/http://jncc.defra.gov.uk/page- 5706 Lowland Raised Bog The definition of this habitat remains unchanged from the pre-existing Habitat Action Plan (https://webarchive.nationalarchives.gov.uk/20110303150026/http://www.ukbap.org.uk/UKPl ans.aspx?ID=20, a summary of which appears below. Lowland raised bogs are peatland ecosystems which develop primarily, but not exclusively, in lowland areas such as the head of estuaries, along river flood-plains and in topographic depressions. In such locations drainage may be impeded by a high groundwater table, or by low permeability substrata such as estuarine, glacial or lacustrine clays. The resultant waterlogging provides anaerobic conditions which slow down the decomposition of plant material which in turn leads to an accumulation of peat. Continued accrual of peat elevates the bog surface above regional groundwater levels to form a gently-curving dome from which the term ‘raised’ bog is derived. The thickness of the peat mantle varies considerably but can exceed 12m. -
Lowland Raised Bog, Duddon Mosses NNR, Cumbria
Lowland raised bog, Duddon Mosses NNR, Cumbria. © Natural England/Jacqueline Ogden 17. Lowland raised bog Climate Change Sensitivity: Medium Climate Change Adaptation Manual Evidence to support nature conservation in a changing climate 159 Introduction An intact, fully functioning lowland raised bog is expected to be relatively resilient to projected climate change, although both changes to patterns of rainfall, including extreme events and summer warming, will place increasing pressure on the habitat. In England, however, there are no raised bogs in this condition. The impact of historic and current land management has a significant impact on the vulnerability of sites. Damage through peat cutting or drainage (both on and off-site) that alters the hydrology of sites has significant adverse impacts on the ability of the bog to withstand reduced rainfall and extreme events such as drought. Degraded bogs are also more vulnerable to climate change impacts on the quality and quantity of ground water. In England, most remaining lowland raised bog habitat is found on the central or core area of the original dome. Surrounding this is an area of degraded peatland, often now under alternative land use, making the remaining bog increasingly vulnerable to off-site impacts and land-use change. Habitat Description Lowland raised bogs are peatland ecosystems which develop primarily in lowland areas such as at the head of estuaries, along river flood-plains and in topographic depressions. In such locations drainage has been impeded by a high groundwater table or by low permeability of the substrata. The resultant water-logging provides anaerobic conditions which slow down the decomposition of plant material, which in turn leads to an accumulation of peat. -
Irish Wildlife Manuals No. 128, the Habitats of Cutover Raised
ISSN 1393 – 6670 N A T I O N A L P A R K S A N D W I L D L I F E S ERVICE THE HABITATS OF CUTOVER RAISED BOG George F. Smith & William Crowley I R I S H W I L D L I F E M ANUAL S 128 National Parks and Wildlife Service (NPWS) commissions a range of reports from external contractors to provide scientific evidence and advice to assist it in its duties. The Irish Wildlife Manuals series serves as a record of work carried out or commissioned by NPWS, and is one means by which it disseminates scientific information. Others include scientific publications in peer reviewed journals. The views and recommendations presented in this report are not necessarily those of NPWS and should, therefore, not be attributed to NPWS. Front cover, small photographs from top row: Limestone pavement, Bricklieve Mountains, Co. Sligo, Andy Bleasdale; Meadow Saffron Colchicum autumnale, Lorcan Scott; Garden Tiger Arctia caja, Brian Nelson; Fulmar Fulmarus glacialis, David Tierney; Common Newt Lissotriton vulgaris, Brian Nelson; Scots Pine Pinus sylvestris, Jenni Roche; Raised bog pool, Derrinea Bog, Co. Roscommon, Fernando Fernandez Valverde; Coastal heath, Howth Head, Co. Dublin, Maurice Eakin; A deep water fly trap anemone Phelliactis sp., Yvonne Leahy; Violet Crystalwort Riccia huebeneriana, Robert Thompson Main photograph: Round-leaved Sundew Drosera rotundifolia, Tina Claffey The habitats of cutover raised bog George F. Smith1 & William Crowley2 1Blackthorn Ecology, Moate, Co. Westmeath; 2The Living Bog LIFE Restoration Project, Mullingar, Co. Westmeath Keywords: raised bog, cutover bog, conservation, classification scheme, Sphagnum, cutover habitat, key, Special Area of Conservation, Habitats Directive Citation: Smith, G.F. -
Washington Natural Heritage Program Presented to the Natural Heritage Advisory Council December 5, 2014
Crowberry Bog Proposed Natural Area Preserve Natural Area Recommendation Submitted by Washington Natural Heritage Program Presented to the Natural Heritage Advisory Council December 5, 2014 Size Three boundary options are presented in this document ranging in size from 248 to 469 acres. Option 1 is 258 acres, Option 2 is 348 acres and Option 3 is 469 acres. Location The site is located within the Pacific Coast ecoregion, approximately 2.5 miles east of Highway 101, 0.3 miles south of the Hoh River and 0.3 miles north of the Hoh Mainline Road in Jefferson County (Figures 1 and 2). The legal description for each option proposed boundary is: Option 1(Figure 3): portions of T27N R12W Sec 25; Sec 26; Sec. 35, and Sec 36. Option 2 (Figure 4): portions of T27N R11W Sec 31; T27N R12W Sec 25; Sec 26; Sec 35, Sec 36; T27N R11W Sec. 31. Option 3 (Figure 5): portions of T27N R11W Sec. 31; T27N R12W Sec 25; Sec 26; Sec 35; and Sec 36. Ownership Ownership is primarily Washington Department of Natural Resources (DNR) with the remainder including DNR-held conservation easements on private lands, and Fruit Growers Supply Co. (Figure 6). Primary Features Crowberry Bog may be the only known coastal plateau bog in the western conterminous United States and the southern-most known in western North America. The proposed NAP (pNAP) would provide an opportunity to protect this unique and very rare feature as well as three elements listed as priorities in the 2011 State of Washington Natural Heritage Plan (Table 1; Figures 3-5): Forested Sphagnum Bog (Priority 2), Low Elevation Sphagnum Bog (Priority 3), and Makah copper butterfly (Priority 2). -
REVIEW Postglacial History of New Zealand Wetlands and Implications
MCGLONE:Available on-line NEW at: ZEALANDhttp://www.newzealandecology.org/nzje/ POSTGLACIAL WETLANDS 1 REVIEW Postglacial history of New Zealand wetlands and implications for their conservation Matt S. McGlone Landcare Research, PO Box 40, Lincoln 7640, New Zealand (Email:[email protected]) Published on-line: 9 March 2009 ___________________________________________________________________________________________________________________________________ Abstract: Most New Zealand wetlands formed at or after the end of the last glaciation (c. 18 000 cal yrs BP). Those associated with major rivers and close to the coast tend to be young as erosive processes both destroy and initiate wetlands. However, there is a strong linear trend in initiations since 14 000 cal yrs BP, which suggests that geomorphic processes such as soil deterioration, landslides, sand dune movement and river course changes are constantly adding new, permanent wetlands. Most wetlands began as herbaceous fens but usually transitioned to shrub- or forest-covered bog–fen systems, in particular after the beginning of the Holocene (11 500 cal yrs BP). Raised bogs formed from fens during the late-glacial and early Holocene, when river down-cutting isolated them from groundwater inflow. As climates warmed through the late-glacial and early Holocene, wooded wetlands spread and over 75% of lowland peat profiles preserve wood layers. Large basins with high water inflow often contain lakes or lagoons and have maintained herbaceous swamps, whereas those with limited catchments have become almost entirely covered with forest or shrubs. Wetlands in drier districts tend to have been initiated during the mid- and late Holocene as the climate cooled and rain-bearing systems penetrated more often. -
Lowland Raised Bogs
SCOTTISH INVERTEBRATE HABITAT MANAGEMENT Lowland raised bogs Wester Moss © Paul Kirkland / Butterfly Conservation Introduction Scottish records of the Bilberry pug moth (Pasiphila debiliata ) is from Kirkconnell Flow There has been a dramatic decline in the area of (Dumfries and Galloway) while the Bog sun- lowland raised bog habitat in the past 100 years. jumper spider ( Heliophanus dampfi ) is known The area of lowland raised bog in the UK only from two sites in the UK – one of which is retaining a largely undisturbed surface is Flanders Moss (Stirlingshire). In addition, there is estimated to have diminished by around 94% a possibility that the Bog chelifer ( Microbisium from an original 95,000 ha to 6,000 ha. In brevifemoratum ) is likely to occur in Scottish Scotland, it is estimated that the original 28,000 bogs—highlighting that there may yet be ha of lowland raised bog habitat has now unrecorded species in this important habitat diminished to a current 2,500 ha. Most of the (Legg, 2010). remaining lowland raised bog in Scotland is Support for management described in this located in the central and north-east lowlands. document is available through the Scotland Rural Historically the greatest decline has occurred Development Programme (SRDP) Rural through agricultural intensification, afforestation Development Contracts (RDC). A summary of and commercial peat extraction. Future decline is this support (at time of publication) can be found likely to be the result of the gradual desiccation of in this document. bogs, damaged by a range of drainage activities and/or a general lowering of groundwater tables. Lowland raised bogs support many rare and localised invertebrates, such as the Large heath butterfly (Coenonympha tullia ) and the 6 spotted pot beetle ( Cryptocephalus sexpunctatus ). -
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. -
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).