Stow Cum Quy Fen Pond Survey
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Local Directory
Local Directory Emergency Services FIRE, or POLICE or medical emergency, only 999 POLICE Customer Services Centre (for suspicious incidents, crimes, etc.) 101 NHS Helpline (non-emergency care and out of hours service) 111 MINICOM (for deaf and hard of hearing) 01480 422493 RNID TypeTalk (for deaf, blind and speech impaired) 0800 515152 Police Anti-social behaviour co-ordinator Brian Tully 01353 656641 Electricity power cut 0800 7838838 Neighbourhood Watch East Cambs (Secretary) Kevin Evans 01353 614892 Park End Robin Sewell 01223 811632 Local Councils Cambridgeshire County Councillor Mathew Schuter 01638 508729 East Cambridgeshire District Councillor Allen Alderson 01638 741744 Parish Council contacts Parish Clerk ([email protected]) Diane Bayliss 01353 664632 Chairman Sue Romero 01223 813635 Vice Chairman Mary Smith 01223 812025 Councillor Kay Ballard 01223 812249 Councillor Nicky Bates 01223 813592 Councillor Peter Raby 01223 811264 Councillor Lynn Reed 01223 811777 Councillor Gordon Reid 01223 811245 Councillor Robin Sewell 01223 811632 Councillor John Trapp 01223 812120 Local Services St. Mary’s Church: Reverend Sue Giles ([email protected]) 01223 812726 Churchwardens: Christopher Welton 01223 811501 Peter Goldsmith 01223 812525 Swaffham Bulbeck Primary School (Head Teacher): 01223 811595 Parent Staff Association (Chair): Toni Rogers 01223 813720 Bottisham Village College: Main Reception 01223 811250 Adult Education 01223 811372 Dentist at Bottisham 01223 811844 Doctors: Bottisham Surgery 01223 810030 Burwell Surgery 01638 741234 Sanctuary Housing Association Freephone 0800131 3348 Community Room Hire (Downing Court) 0800131 3348 Women’s Institute (President) Mrs P. Cook 01638 742224 Relief-in-Need Charity (Clerk) Mrs C. Ling 01223 813885 Public transport information line 08712 002233 Dial-a-Ride 01638 664304 Swaffhams Cricket Club James Aldridge 01223 811798 Mitchell Lodge Bowls Club (Secretary) Mr M. -
Thorne Moors :A Palaeoecological Study of A
T...o"..e MO<J "S " "",Ae Oe COlOOIC'" S T<.OY OF A e"ONZE AGE slTE - .. "c euc~ , A"O a • n ,• THORNE MOORS :A PALAEOECOLOGICAL STUDY OF A BRONZE AGE SITE A contribution to the history of the British Insect fauna P.c. Buckland, Department of Geography, University of Birmingham. © Authors Copyright ISBN ~o. 0 7044 0359 5 List of Contents Page Introduction 3 Previous research 6 The archaeological evidence 10 The geological sequence 19 The samples 22 Table 1 : Insect remains from Thorne Moors 25 Environmental interpretation 41 Table 2 : Thorne Moors : Trackway site - pollen and spores from sediments beneath peat and from basal peat sample 42 Table 3 Tho~ne Moors Plants indicated by the insect record 51 Table 4 Thorne Moors pollen from upper four samples in Sphagnum peat (to current cutting surface) 64 Discussion : the flooding mechanism 65 The insect fauna : notes on particular species 73 Discussion : man, climate and the British insect fauna 134 Acknowledgements 156 Bibliography 157 List of Figures Frontispiece Pelta grossum from pupal chamber in small birch, Thorne Moors (1972). Age of specimen c. 2,500 B.P. 1. The Humberhead Levels, showing Thorne and Hatfield Moors and the principal rivers. 2 2. Thorne Moors the surface before peat extraction (1975). 5 3. Thorne Moors the same locality after peat cutting (1975). 5 4. Thorne Moors location of sites examined. 9 5. Thorne Moors plan of trackway (1972). 12 6. Thorne Moors trackway timbers exposed in new dyke section (1972) • 15 7. Thorne Moors the trackway and peat succession (1977). -
Mangrove Swamp (Caroni Wetland, Trinidad)
FIGURE 1.3 Swamps. (a) Floodplain swamp (Ottawa River, Canada). (b) Mangrove swamp (Caroni wetland, Trinidad). FIGURE 1.4 Marshes. (a) Riverine marsh (Ottawa River, Canada; courtesy B. Shipley). (b) Salt marsh (Petpeswick Inlet, Canada). FIGURE 1.5 Bogs. (a) Lowland continental bog (Algonquin Park, Canada). (b) Upland coastal bog (Cape Breton Island, Canada). FIGURE 1.6 Fens. (a) Patterned fen (northern Canada; courtesy C. Rubec). (b) Shoreline fen (Lake Ontario, Canada). FIGURE 1.7 Wet meadows. (a) Sand spit (Long Point, Lake Ontario, Canada; courtesy A. Reznicek). (b) Gravel lakeshore (Tusket River, Canada; courtesy A. Payne). FIGURE 1.8 Shallow water. (a) Bay (Lake Erie, Canada; courtesy A. Reznicek). (b) Pond (interdunal pools on Sable Island, Canada). FIGURE 2.1 Flooding is a natural process in landscapes. When humans build cities in or adjacent to wetlands, flooding can be expected. This example shows Cedar Rapids in the United States in 2008 (The Gazette), but incidences of flood damage to cities go far back in history to early cities such as Nineveh mentioned in The Epic of Gilgamesh (Sanders 1972). FIGURE 2.5 Many wetland organisms are dependent upon annual flood pulses. Animals discussed here include (a) white ibis (U.S. Fish and Wildlife Service), (b) Mississippi gopher frog (courtesy M. Redmer), (c) dragonfly (courtesy C. Rubec), and (d) tambaqui (courtesy M. Goulding). Plants discussed here include (e) furbish lousewort (bottom left; U.S. Fish and Wildlife Service) and ( f ) Plymouth gentian. -N- FIGURE 2.10 Spring floods produce the extensive bottomland forests that accompany many large rivers, such as those of the southeastern United States of America. -
This Article Appeared in a Journal Published by Elsevier. the Attached
This article appeared in a journal published by Elsevier. The attached copy is furnished to the author for internal non-commercial research and education use, including for instruction at the authors institution and sharing with colleagues. Other uses, including reproduction and distribution, or selling or licensing copies, or posting to personal, institutional or third party websites are prohibited. In most cases authors are permitted to post their version of the article (e.g. in Word or Tex form) to their personal website or institutional repository. Authors requiring further information regarding Elsevier’s archiving and manuscript policies are encouraged to visit: http://www.elsevier.com/copyright Author's personal copy Quaternary Research 75 (2011) 531–540 Contents lists available at ScienceDirect Quaternary Research journal homepage: www.elsevier.com/locate/yqres Response of a warm temperate peatland to Holocene climate change in northeastern Pennsylvania Shanshan Cai, Zicheng Yu ⁎ Department of Earth and Environmental Sciences, Lehigh University, 1 West Packer Avenue, Bethlehem, PA 18015, USA article info abstract Article history: Studying boreal-type peatlands near the edge of their southern limit can provide insight into responses of Received 11 September 2010 boreal and sub-arctic peatlands to warmer climates. In this study, we investigated peatland history using Available online 18 February 2011 multi-proxy records of sediment composition, plant macrofossil, pollen, and diatom analysis from a 14C-dated sediment core at Tannersville Bog in northeastern Pennsylvania, USA. Our results indicate that peat Keywords: accumulation began with lake infilling of a glacial lake at ~9 ka as a rich fen dominated by brown mosses. -
Managing Iowa Habitats
Managing Iowa Habitats Fen Wetlands Introduction Why should I be concerned? Fens are the rarest of Iowa’s wetland commu- Fens are an important and unique wetland nities and of great scientific interest. While type. Not only are the fens themselves rare, but their geology varies, they all are the products they shelter over 200 plant species, 20 of which of the seepage of groundwater to the surface. are Iowa endangered and threatened species. Because the water is rich in calcium and other Many of the plant species have been in these minerals, only a select group of plants is able to areas for thousands of years. The fen’s vegeta- grow there. As a result, fens contain many tion, in turn, shelters wildlife by providing plant species considered endangered or valuable habitat. threatened in Iowa. Fens are valuable to humans as well. They are A few of the oldest fens contain plant remains important as sites of groundwater discharge — that date back 10,000 years, though most Iowa good indicators of shallow aquifers. Vegetation fens are less than 5,000 years old. A few of in all wetlands plays an important role in these “younger” fens may have existed 10,000 recycling nutrients, trapping eroding soil, and years ago, but because of dramatic climate filtering out polluting chemicals such as changes, they may have dried up and lost the nitrates. However, the rarity of fens and their plant remains (by burning or erosion) that relatively small size makes it important could prove their age. When the climate grew to protect them from overloading by wetter again about 5,000 years ago, these fens these materials. -
Stow-Cum-Quy
Services and Facilities Study South Cambridgeshire March 2012 District Council STOW-CUM-QUY Settlement Size Settlement Population Dwelling Stock Category (mid-2010 estimate) (mid-2010 estimate) Infill Village 530 240 Transport Bus Service: A) Summary Bus Service Monday – Friday Saturday Sunday Cambridge / Market Town Frequency Frequency Frequency To / From Cambridge Hourly Hourly No Service To / From Newmarket Hourly Hourly No Service B) Detailed Bus Service Monday - Friday Cambridge / Market Service 7:00-9:29 9:30-16:29 16:30-18:59 19:00-23:00 Town To Cambridge 10 4 Buses Hourly 2 Buses No Service From Cambridge 10 2 Buses Hourly Hourly No Service To Newmarket 10 2 Buses Hourly 2 Buses 1 Bus From Newmarket 10 3 Buses Hourly 1 Bus No Service Saturday Cambridge / Market Service 7:00-9:29 9:30-16:29 16:30-18:59 19:00-23:00 Town To Cambridge 10 3 Buses Hourly 2 Buses No Service From Cambridge 10 2 Buses Hourly Hourly No Service To Newmarket 10 1 Bus Hourly 2 Buses 1 Bus From Newmarket 10 3 Buses Hourly 1 Bus No Service Sunday Cambridge / Market Service 9:00-18:00 Town To Cambridge 10 No Service From Cambridge 10 No Service Services & Facilities Study March 2012 629 South Services and Facilities Study Cambridgeshire District Council March 2012 Sunday Cambridge / Market Service 9:00-18:00 Town To Newmarket 10 No Service From Newmarket 10 No Service C) Journey Duration Cambridge / Market Timetabled Service Bus Stops Town Journey Time To / From Stow cum Quy, St. Mary's Church – 10 25 / 17 Minutes Cambridge Cambridge, Drummer Street To / From Stow cum Quy, St. -
Northern Fen Communitynorthern Abstract Fen, Page 1
Northern Fen CommunityNorthern Abstract Fen, Page 1 Community Range Prevalent or likely prevalent Infrequent or likely infrequent Absent or likely absent Photo by Joshua G. Cohen Overview: Northern fen is a sedge- and rush-dominated 8,000 years. Expansion of peatlands likely occurred wetland occurring on neutral to moderately alkaline following climatic cooling, approximately 5,000 years saturated peat and/or marl influenced by groundwater ago (Heinselman 1970, Boelter and Verry 1977, Riley rich in calcium and magnesium carbonates. The 1989). community occurs north of the climatic tension zone and is found primarily where calcareous bedrock Several other natural peatland communities also underlies a thin mantle of glacial drift on flat areas or occur in Michigan and can be distinguished from shallow depressions of glacial outwash and glacial minerotrophic (nutrient-rich) northern fens, based on lakeplains and also in kettle depressions on pitted comparisons of nutrient levels, flora, canopy closure, outwash and moraines. distribution, landscape context, and groundwater influence (Kost et al. 2007). Northern fen is dominated Global and State Rank: G3G5/S3 by sedges, rushes, and grasses (Mitsch and Gosselink 2000). Additional open wetlands occurring on organic Range: Northern fen is a peatland type of glaciated soils include coastal fen, poor fen, prairie fen, bog, landscapes of the northern Great Lakes region, ranging intermittent wetland, and northern wet meadow. Bogs, from Michigan west to Minnesota and northward peat-covered wetlands raised above the surrounding into central Canada (Ontario, Manitoba, and Quebec) groundwater by an accumulation of peat, receive inputs (Gignac et al. 2000, Faber-Langendoen 2001, Amon of nutrients and water primarily from precipitation et al. -
Lode with Longmeadow Walks
LODE WALKS A selection of walks in and around Lode with Longmeadow Revised version – August 2012 Free to download 1 Lode with Longmeadow Walks Circular walks from 3km to 20km starting at Lode Church All distances in this guide are given in metres (m) or kilometres (km) 1km is just under two thirds of a mile. The walks are listed below in increasing order of distance Parish walks Map Short walk via Saxon Farm (3km) 3 Quy water and the old railway (3.5km) 4 Docking Drove and Cranney Drove (6km) 3 White Fen Drove and the Festival Site (6km) 1 Quy Water and Quy Fen (7km) 4 The Sportsman via Red Tile Farm (8.5km) 3 Bottisham and Swaffham Bulbeck (9km) 2 Quy Water and Quy Fen via Allicky Farm (9km) 4 In Search of a Hill (12km) 2 Oily Hall and the River Cam (12km) 1 Going the extra mile (14km) 2 Pub walks The Bell Inn at Bottisham and The Black Horse at Swaffham Bulbeck are both found on the Parish Walk illustrated on Map 2 (9km) 2 The Plough and Fleece at Horningsea (10.5km) 5 The Red Lion at Swaffham Prior - this is a variation of the Reach pub walk (13km) 6 The Dyke’s End at Reach (15 or 17km) 6 The Carpenter’s Arms at Great Wilbraham (19km) 7 The No Hurry Inn - Five Miles from Anywhere at Upware (20km) 8 If you are going on one of the pub walks, check opening times beforehand and, if you want food, check serving hours. -
FEN BOG from the Website North Yorkshire for the Book Discover Butterflies in Britain © D E Newland 2009
FEN BOG from www.discoverbutterflies.com the website North Yorkshire for the book Discover Butterflies in Britain © D E Newland 2009 The North Yorkshire Moors Railway passes along the western edge of Fen Bog Fen Bog is 20 ha (50 acres) of This well-known site in TARGET SPECIES boggy marshland at the head Yorkshire is noted for its Large Heath (June and early of Newtondale, near Pickering many different species of July), Small Pearl-bordered in North Yorkshire. It is 3 butterflies, moths and and Dark Green Fritillaries; miles south of Goathland and dragonflies. There is a deep commoner species. lies on the route of the North bed of peat where many Yorkshire Moors Railway different bog plants flourish. It from Pickering to Grosmont. lies within a wide valley with heather, hard fern, mat grass and purple moor grass all growing stongly. The reserve is cared for by the Yorkshire Wildlife Trust. The North York Moors became one of our first National Parks in 1952. Its moors are one of the largest areas of heather moorland in Britain and cover an area of 550 square miles. It is hard to imagine that they were once permanently covered in ice and snow. When global warming took effect at the end of the Ice Age, the snowfields began to melt and melt water flowed south. It gouged out the deep valley of Newtondale where the Pickering Beck now flows. Newtondale runs roughly north-south parallel to the A169 Whitby to Pickering road and is a designated SSSI of 940 ha (2,300 acres). -
A Fen Is a Rare, Low Shrub- and Herb- Dominated Wetland That Is Fed by Calcareous Groundwater Seepage
Habitat fact sheet Fen A fen is a rare, low shrub- and herb- dominated wetland that is fed by calcareous groundwater seepage. Fens almost always occur in areas influenced by carbonate bedrock (e.g., limestone and marble), and are identified by their low, often sparse vegetation and their distinctive plant community. Tussocky vegetation and small BellK. 2006 seepage rivulets are often present, and some fens have substantial areas of bare mineral Typical plants soil or organic muck. • Grasses and sedges such as spike-muhly, sterile sedge, porcupine sedge, yellow sedge, and woolly-fruit sedge • Shrubs including shrubby cinquefoil, K. BellK. 2007 alder-leaf buckthorn, and autumn willow Bog turtle • Wildflowers including grass-of- Parnassus and bog goldenrod Species of conservation concern Purple cliffbrake • More than 12 state-listed rare plants are found almost exclusively in fen habitats, including handsome sedge, Schweinitz’s sedge, bog valerian, scarlet Indian paintbrush, spreading globeflower, and swamp birch • Rare butterflies such as Dion skipper and black dash • Rare dragonflies such as forcipate emerald and Kennedy’s emerald • Bog turtle (Endangered in New York) • Spotted turtle, ribbon snake • Sedge wren, northern harrier These are just a few of the species of regional or statewide conservation concern that are known to occur in fen habitats. See Kiviat & Stevens (2001) Bell 2006 K. for a more extensive list. Fringed gentian Hudsonia Ltd. PO Box 5000, Annandale, NY 12504 (845) 758-7053 www.hudsonia.org Habitat fact sheet Page 2 Threats to fens Fens are highly vulnerable to degradation from direct disturbance and from activities in nearby upland areas. -
Coleoptera: Hydrophilidae) Are Specialist Predators of Snails
Eur. J. Entomol. 112(1): 145–150, 2015 doi: 10.14411/eje.2015.016 ISSN 1210-5759 (print), 1802-8829 (online) Larvae of the water scavenger beetle, Hydrophilus acuminatus (Coleoptera: Hydrophilidae) are specialist predators of snails TOSHIO INODA1, YUTA INODA1 and JUNE KATHYLEEN RULLAN 2 1 Shibamata 5-17-10, Katsushika, Tokyo 125-0052, Japan; e-mail: [email protected] 2 University of the Philippines, Manila, Philippines; e-mail: [email protected] Key words. Coleoptera, Hydrophilidae, Hydrophilus acuminatus, feeding preferences, snail specialist Abstract. Hydrophilus acuminatus larvae are known to feed on aquatic prey. However, there is no quantitative study of their feeding habits. In order to determine the feeding preferences and essential prey of larvae of H. acuminatus, both field and laboratory experi- ments were carried out. Among the five potential species of prey,Austropeplea ollula (Mollusca: Lymnaeidae), Physa acuta (Mollusca: Physidae), Asellus hilgendorfi (Crustacea: Asellidae), Palaemon paucidens (Crustacea: Palaemonidae) and larvae of Propsilocerus akamusi (Insecta: Chironomidae), the first instar larvae of H. acuminatus strongly prefered the Austropeplea and Physa snails in both cafeteria and single-prey species experiments. Larvae that were provided with only snails also successfully developed into second instar larvae, while larvae fed Palaemon, Propsilocerus larvae or Asellus died during the first instar. In addition, the size of adult H. acuminatus reared from first-instar larvae and fed only snails during their entire development was not different from that of adult H. acuminatus collected in the field. This indicates that even though the larvae ofH. acuminatus can feed on several kinds of invertebrates, they strongly prefer snails and without them cannot complete their development. -
New Orleans, LA USA
July 28-August 1, 2014 | New Orleans, LA USA CEER 2014 Conference on Ecological and Ecosystem Restoration ELEVATING THE SCIENCE AND PRACTICE OF RESTORATION A Collaborative Effort of NCER and SER July 28-August 1, 2014 New Orleans, Louisiana, USA www.conference.ifas.ufl.edu/CEER2014 Welcome to the UF/IFAS OCI App! The University of Florida IFAS Office of Conferences & Institutes is happy to present a mobile app for the Conference on Ecological and Ecosystem Restoration. To access the conference app, scan the QR Code or search “IFAS OCI” in the App Store or Google Play on your Apple or Android device. Log in with the email address you used to register, a social media account, or as a guest. You will be prompted to select an event – choose CEER 2014. The event password is eco14. The app allows you to build a personal conference agenda, stay updated with conference announcements, and connect with sponsors, exhibitors, and fellow attendees. Should you have any questions about the app, please stop by our registration desk for assistance. Stay connected! #CEER2014 July 28-August 1, 2014 | New Orleans, LA USA Table of Contents Welcome Letter ...................................................................................................... 3 In Honor of David Allen Vigh ................................................................................... 4 About CEER ............................................................................................................. 6 About the Society for Ecological Restoration ........................................................