Chalk Grassland Strategy Report
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Historic Environment Action Plan West Wight Chalk Downland
Directorate of Community Services Director Sarah Mitchell Historic Environment Action Plan West Wight Chalk Downland Isle of Wight County Archaeology and Historic Environment Service October 2008 01983 823810 archaeology @iow.gov.uk Iwight.com HEAP for West Wight Chalk Downland. INTRODUCTION The West Wight Chalk Downland HEAP Area has been defined on the basis of geology, topography and historic landscape character. It forms the western half of a central chalk ridge that crosses the Isle of Wight, the eastern half having been defined as the East Wight Chalk Ridge . Another block of Chalk and Upper Greensand in the south of the Isle of Wight has been defined as the South Wight Downland . Obviously there are many similarities between these three HEAP Areas. However, each of the Areas occupies a particular geographical location and has a distinctive historic landscape character. This document identifies essential characteristics of the West Wight Chalk Downland . These include the large extent of unimproved chalk grassland, great time-depth, many archaeological features and historic settlement in the Bowcombe Valley. The Area is valued for its open access, its landscape and wide views and as a tranquil recreational area. Most of the land at the western end of this Area, from the Needles to Mottistone Down, is open access land belonging to the National Trust. Significant historic landscape features within this Area are identified within this document. The condition of these features and forces for change in the landscape are considered. Management issues are discussed and actions particularly relevant to this Area are identified from those listed in the Isle of Wight HEAP Aims, Objectives and Actions. -
Dorset Downs and Cranborne Chase
Responding to the impacts of climate change on the natural environment: Natural England publications are available as accessible pdfs from: Dorset Downs and Cranborne Chase www.naturalengland.org.uk/publications Should an alternative format of this publication be required, please contact our enquiries line for more information: A summary 0845 600 3078 or email: [email protected] Printed on Defra Silk comprising 75% recycled fibre. www.naturalengland.org.uk Introduction Natural England is working to deliver Downs and Cranborne Chase. The a natural environment that is healthy, others are the Cumbria High Fells, enjoyed by people and used in a Shropshire Hills, and the Broads. sustainable manner. However, the natural environment is changing as a consequence This leaflet is a summary of the more of human activities, and one of the major detailed findings from the pilot project challenges ahead is climate change. (these are available on our website at www.naturalengland.org.uk). The leaflet: Even the most optimistic predictions show us locked into at least 50 years identifies significant biodiversity, of unstable climate. Changes in landscape, recreational and historic temperature, rainfall, sea levels, and the environment assets; magnitude and frequency of extreme assesses the potential risks climate weather events will have a direct impact change poses to these assets; and on the natural environment. Indirect impacts will also arise as society adapts suggests practical actions that would to climate change. These impacts make them more resilient to the impacts may create both opportunities and of climate change. threats to the natural environment. What we learn from the four pilot Natural England and its partners therefore projects will be used to extend the need to plan ahead to secure the future approach across England as part of of the natural environment. -
Downland Mosaic Large Scale Found Throughout the Hampshire Downs, but Most Extensive in Mid and North Hampshire
LANDSCAPE CHARACTER TYPE: Downland Mosaic Large Scale Found throughout the Hampshire Downs, but most extensive in mid and north Hampshire. SIMILAR AND ASSOCIATED TYPES HAMPSHIRE DISTRICT AND BOROUGH LEVEL ASSESSMENTS Basingstoke: Primary association: Semi Enclosed Chalk and Clay Farmland, Enclosed Chalk and Clay Farmland large Scale. Secondary association: Open Arable, Parkland and Estate Farmland East Hampshire Downland Mosaic Open Eastleigh n/a Fareham n/a Gosport n/a Hart Enclosed Arable Farmland Havant n/a New Forest n/a Rushmoor n/a Test Valley Enclosed Chalk and Clay Woodland (where woodlands are large and extensive) Winchester Primary association: Chalk and Clay Farmland Secondary association: Scarp Downland Grassland and some Chalk and Clay Woodland SIMILAR AND ASSOCIATED TYPES IN NEIGHBOURING AUTHORITY ASSESSMENTS Dorset West Berkshire West Sussex Wiltshire Hampshire County 1 Status: FINAL Draft Autumn 2010 Integrated Character Assessment Downland Mosaic Large Scale KEY IDENTIFYING CHARACTERISTICS AND BOUNDARY DEFINITIONS A Downs landscape which has moderately heavy soils and more clay soil content than in Open Downs landscapes. Can have mini scarps which are individually identified in some local assessments. Large scale character influenced by rolling topography, medium to large size fields, fewer wooded hedges than the small scale type and can have large woodland blocks. Large blocks of ancient woodland and varied height hedgerow network which contrasts with areas of more open predominantly arable fields. Deeply rural quiet landscapes with sense of space and expansiveness uninterrupted by development the large woodland blocks add to the sense ruralness and of an undeveloped landscape. Low density road and lane network where this type occurs in mid and west Hampshire –higher density further east. -
Open Downland
8. LANDSCAPE TYPE 1: OPEN DOWNLAND Location and Boundaries 8.1. The landscape type encompasses a number of distinct downland blocks from the Marlborough Downs (1A) and Horton Down (1C) in the west running through to the Lambourn Downs (1B) and Blewbury Downs (1D) in the east. Boundaries are mainly defined by topography and the Upper Chalk geology, and in the north relate to the top of the Scarp (landscape type 5). To the south, the edge of the chalk similarly forms a distinct boundary. Overview The Open Downlands are the remote heart and core of the North Wessex Downs, with the dramatic landscapes created by the underlying chalk rocks being one of the defining features of the AONB. The subtle curves and undulations of the landform are revealed by the uniform clothing of cropped grass or cereals creating a landscape with a simple and elemental quality, accentuated by vast skies. The open, expansive views are punctuated by distinctive beech clumps crowning the downland summits, forming prominent and highly visible landmarks. Sparsely populated, the downlands possess a strong sense remoteness and isolation. Predominantly in arable cultivation these are landscapes of great seasonal variation, with muted browns and greys of the chalk and flinty soils in the ploughed autumn fields, giving way to fresh greens of the emerging crops in winter and spring and sweeping yellows and golds of summer. The characteristic close-cropped springy downland turf of the surviving herb-rich chalk grassland provides an important habitat and this landscape type contains the largest areas of designated chalk grassland in the AONB, with 15 Sites of Special Scientific Interest (SSSI). -
Luton SUE Site Size (Ha): 283.81
Site: NLP426 - North Luton SUE Site size (ha): 283.81 Parcel: NLP426f Parcel area (ha): 89.74 Stage 1 assessment Stage 2 assessment Parcel: L2 Parcel: n/a Highest contribution: Purpose 3 - Strong Contribution: contribution Contribution to Green Belt purposes Purpose Comments Purpose 1: Checking The parcel is located adjacent to the large built up area and development here would relate the unrestricted to the expansion of Luton. The parcel is only separated from the settlement edge to the sprawl of large, built- south by occasional hedgerow trees. However, the low hedgerows, and intermittent up areas hedgerow trees along the remaining boundaries provide little separation between the parcel and the rolling farmland beyond the parcel to the north, west and east, so that despite its proximity to Luton, the parcel relates more strongly to the wider countryside and its release would constitute significant sprawl into the countryside. Purpose 2: The development of the parcel would result in little perception of the narrowing of the gap Preventing the between neighbouring towns because the larger towns to the north of Luton, including merger of Flitwick, are separated by the chalk escarpment running east-west which would limit the neighbouring towns impact. Purpose 3: The proximity of the adjacent residential settlement edge has some urbanising influence on Safeguarding the the parcel particularly as the occasional hedgerow trees on the boundary offer little countryside from separation. However, there is no urban development within the parcel itself and openness encroachment and undulating topography of the parcel give it a stronger relationship with the wider downland countryside. -
Landowner Deposits Register
Register of Landowner Deposits under Highways Act 1980 and Commons Act 2006 The first part of this register contains entries for all CA16 combined deposits received since 1st October 2013, and these all have scanned copies of the deposits attached. The second part of the register lists entries for deposits made before 1st October 2013, all made under section 31(6) of the Highways Act 1980. There are a large number of these, and the only details given here currently are the name of the land, the parish and the date of the deposit. We will be adding fuller details and scanned documents to these entries over time. List of deposits made - last update 12 January 2017 CA16 Combined Deposits Deposit Reference: 44 - Land at Froyle (The Mrs Bootle-Wilbrahams Will Trust) Link to Documents: http://documents.hants.gov.uk/countryside/Deposit44-Bootle-WilbrahamsTrustLand-Froyle-Scan.pdf Details of Depositor Details of Land Crispin Mahony of Savills on behalf of The Parish: Froyle Mrs Bootle-WilbrahamWill Trust, c/o Savills (UK) Froyle Jewry Chambers,44 Jewry Street, Winchester Alton Hampshire Hampshire SO23 8RW GU34 4DD Date of Statement: 14/11/2016 Grid Reference: 733.416 Deposit Reference: 98 - Tower Hill, Dummer Link to Documents: http://documents.hants.gov.uk/rightsofway/Deposit98-LandatTowerHill-Dummer-Scan.pdf Details of Depositor Details of Land Jamie Adams & Madeline Hutton Parish: Dummer 65 Elm Bank Gardens, Up Street Barnes, Dummer London Basingstoke SW13 0NX RG25 2AL Date of Statement: 27/08/2014 Grid Reference: 583. 458 Deposit Reference: -
HBIC Annual Monitoring Report 2018
Monitoring Change in Priority Habitats, Priority Species and Designated Areas For Local Development Framework Annual Monitoring Reports 2018/19 (including breakdown by district) Basingstoke and Deane Eastleigh Fareham Gosport Havant Portsmouth Winchester Produced by Hampshire Biodiversity Information Centre December 2019 Sharing information about Hampshire's wildlife The Hampshire Biodiversity Information Centre Partnership includes local authorities, government agencies, wildlife charities and biological recording groups. Hampshire Biodiversity Information Centre 2 Contents 1 Biodiversity Monitoring in Hampshire ................................................................................... 4 2 Priority habitats ....................................................................................................................... 7 3 Nature Conservation Designations ....................................................................................... 12 4 Priority habitats within Designated Sites .............................................................................. 13 5 Condition of Sites of Special Scientific Interest (SSSIs)....................................................... 14 7. SINCs in Positive Management (SD 160) - Not reported on for 2018-19 .......................... 19 8 Changes in Notable Species Status over the period 2009 - 2019 ....................................... 20 09 Basingstoke and Deane Borough Council .......................................................................... 28 10 Eastleigh Borough -
Monitoring Change in Priority Habitats, Priority Species and Designated Areas
Monitoring Change in Priority Habitats, Priority Species and Designated Areas For Local Development Framework Annual Monitoring Reports 2018/19 (including breakdown by district) Basingstoke and Deane Eastleigh Fareham Gosport Havant Portsmouth Winchester Produced by Hampshire Biodiversity Information Centre December 2019 Sharing information about Hampshire's wildlife The Hampshire Biodiversity Information Centre Partnership includes local authorities, government agencies, wildlife charities and biological recording groups. Hampshire Biodiversity Information Centre 2 Contents 1 Biodiversity Monitoring in Hampshire ................................................................................... 4 2 Priority habitats ....................................................................................................................... 7 3 Nature Conservation Designations ....................................................................................... 12 4 Priority habitats within Designated Sites .............................................................................. 13 5 Condition of Sites of Special Scientific Interest (SSSIs)....................................................... 14 7. SINCs in Positive Management (SD 160) - Not reported on for 2018-19 .......................... 19 8 Changes in Notable Species Status over the period 2009 - 2019 ....................................... 20 09 Basingstoke and Deane Borough Council .......................................................................... 28 10 Eastleigh Borough -
THE Systematic List for 2009
THE SystemaTic List for 2009 The 2009 systematic list was prepared by a team of species account writers (see below) and edited by Chris Heard and Renton Righelato. We try to restrict records to those within the long and tortuous border of Berkshire. However, this is not always possible and it should be noted, for example, that monthly peak counts of wildfowl at Eversley GPs may include some birds in Hampshire and some records on the Thames and Blackwater rivers may have been over the midline and outside Berkshire. Moreover, references to Atlas survey data include counts in the whole of border tetrads, resulting in the survey area being almost 25% larger than the area of Berkshire itself. Species account writers of the 2009 systematic list Mute Swan to Egyptian Goose Ken Moore Ruddy Shelduck to Mallard Ray Reedman Pintail to Ruddy Duck Renton Righelato Red-legged Partridge to Grey Heron Andy Horscroft Red Kite to Peregrine* Steve Ricks Water Rail to Coot Renton Righelato Oystercatcher to Grey Phalarope Marek Walford Arctic Skua to Arctic Tern Paul Bright-Thomas Feral Pigeon to Cuckoo Jim Reid Barn Owl to Lesser Spotted Woodpecker Bill Nicoll Woodlark to Dunnock Peter Gipson Robin to Greenland Wheatear Renton Righelato Ring Ouzel to Firecrest* Richard Burness Spotted Flycatcher to Treecreeper Roger Stansfield Great Grey Shrike to House Sparrow Bill Nicoll Chaffinch to Corn Bunting Richard Burness Escapes and hybrids Chris Heard *Honey Buzzard, Montagu’s Harrier, Goshawk, Yellow-browed Warbler were written by Renton Righelato abbreviations and place names Abbreviations used in the systematic lists are shown below. -
Historic Landscape Character Areas and Their Special Qualities and Features of Significance
Historic Landscape Character Areas and their special qualities and features of significance Volume 1 Third Edition March 2016 Wyvern Heritage and Landscape Consultancy Emma Rouse, Wyvern Heritage and Landscape Consultancy www.wyvernheritage.co.uk – [email protected] – 01747 870810 March 2016 – Third Edition Summary The North Wessex Downs AONB is one of the most attractive and fascinating landscapes of England and Wales. Its beauty is the result of many centuries of human influence on the countryside and the daily interaction of people with nature. The history of these outstanding landscapes is fundamental to its present‐day appearance and to the importance which society accords it. If these essential qualities are to be retained in the future, as the countryside continues to evolve, it is vital that the heritage of the AONB is understood and valued by those charged with its care and management, and is enjoyed and celebrated by local communities. The North Wessex Downs is an ancient landscape. The archaeology is immensely rich, with many of its monuments ranking among the most impressive in Europe. However, the past is etched in every facet of the landscape – in the fields and woods, tracks and lanes, villages and hamlets – and plays a major part in defining its present‐day character. Despite the importance of individual archaeological and historic sites, the complex story of the North Wessex Downs cannot be fully appreciated without a complementary awareness of the character of the wider historic landscape, its time depth and settlement evolution. This wider character can be broken down into its constituent parts. -
Carbon Storage in Phosphorus Limited Grasslands May 2 Decline in Response to Elevated Nitrogen Deposition: a Long- 3 Term Field Manipulation and Modelling Study
https://doi.org/10.5194/bg-2020-392 Preprint. Discussion started: 9 November 2020 c Author(s) 2020. CC BY 4.0 License. 1 Carbon storage in phosphorus limited grasslands may 2 decline in response to elevated nitrogen deposition: a long- 3 term field manipulation and modelling study 4 Christopher R. Taylor1, Victoria Janes-Bassett3, Gareth Phoenix1, Ben Keane1, Iain P. Hartley2, Jessica 5 A.C. Davies3 6 1Department of Animal and Plant Sciences, University of Sheffield, Sheffield, UK 7 2Geography, College of Life and Environmental Science, University of Exeter, Exeter, UK 8 3Lancaster Environment Centre, Lancaster University, Lancaster, UK 9 10 Corresponding author: Christopher Taylor ([email protected]) 11 12 13 14 15 16 17 18 19 20 21 22 23 24 Page 1 of 37 https://doi.org/10.5194/bg-2020-392 Preprint. Discussion started: 9 November 2020 c Author(s) 2020. CC BY 4.0 License. 25 Abstract 26 In many temperate ecosystems, nitrogen (N) limits productivity, meaning anthropogenic N 27 deposition can stimulate plant growth and subsequently carbon (C) sequestration. Phosphorus 28 (P) and N-P co-limited grasslands are widespread, yet there is limited understanding of their 29 responses to N deposition, which may transition more ecosystems toward P-limited or N-P co- 30 limited states. Here, we investigate the consequences of enhanced N addition on the C-N-P 31 pools of grasslands in different states of nutrient limitation. We explored the response of a long- 32 term nutrient-manipulation experiment on two N-P co-limited grasslands; an acidic grassland of 33 stronger N-limitation and a calcareous grassland of stronger P-limitation, by combining data with 34 an integrated C-N-P cycling model (N14CP). -
Lowland Calcareous Grassland Creation And
BPG LOWLAND CALCAREOUS GRASSLAND NOTE 18 Best Practice Guidance Creation and management in for Land Regeneration land regeneration (Photo: © Tim O’Hare Associates) Frank Ashwood Introduction Calcareous grasslands are characterised by species-rich grass and herb communities which grow on shallow, lime-rich soils (Figure 1). UK biodiversity legislation recognises both upland and lowland calcareous grasslands and that these are of principal importance in England (Natural England, 2010), Scotland (Anon, 2013), Wales (Wales Biodiversity Partnership, 2008) and Northern Ireland (Department of the Environment Northern Ireland and the Northern Ireland Environment Agency, 2011). This guidance note focuses on the lowland types. Current estimates suggest that up to 30 000 ha of lowland calcareous grassland remain in the UK, following significant decreases of about 13 000 ha in the area of this habitat between 1990 and 2007 (Natural Environment Research Council, 2009). Major concentrations are found on the chalk downs of Wiltshire, Dorset, Kent and Figure 1 Chalk downland flora Sussex, with other significant areas in the Chilterns, Mendips and Cotswolds, and (Photo: © Natural England/Chris Gomersall) along the limestone outcrops and coastal cliffs of north and south Wales. Only small areas are found in Scotland and Northern Ireland. Losses are mostly due to agricultural improvement and reductions in traditional grazing management practices. While natural calcareous grasslands typically develop on dry valley slopes, semi-natural calcareous grasslands can develop in areas disturbed by human activities, including on exposed rock in disused chalk and limestone workings, along road verges and railway cuttings, and on post-industrial land (JNCC, 2011). The establishment of calcareous grassland on reclaimed land is contributing to UK national conservation targets for this priority habitat (e.g.