I I I I I I I I I I I I I I I I I I
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
The First Record of a Mammal from the Insect Limestone Is a Left Lower Incisor of the Rodent Isoptychus (NHMUK.PV.M45566) (Fig.3B)
Vertebrate remains from the Insect Limestone (latest Eocene), Isle of Wight, UK Hooker, J. J., Department of Earth Sciences, Natural History Museum, Cromwell Road, London, SW7 5BD, UK (corresponding author) Evans, S. E., Department of Cell and Developmental Biology, University College London, Anatomy Building, Gower Street, London, WC1E 6BT, UK Davis, P. G., c/o J. J. Hooker Running head: Insect Limestone vertebrates 1 Abstract A small fauna of vertebrates is recorded from the Insect Limestone, Bembridge Marls Member, Bouldnor Formation, late Priabonian, latest Eocene, of the Isle of Wight, UK. The taxa represented are teleost fishes, lizards including a scincoid, unidentified birds and the theridomyid rodent Isoptychus. The scincoid represents the youngest record of the group in the UK. Of particular note is the taphonomic interpretation based on the preservation of anatomical parts of land-based tetrapods that would have been most likely transported to the site of deposition by wind, namely bird feathers and pieces of shed lizard skin. These comprise the majority of the specimens and suggest that the dominant transport mechanism was wind. Keywords: Bembridge Marls – bird – feather – fish – lizard – mammal – rodent – Scincoidea – skin – Squamata – taphonomic – Theridomyidae 2 The Insect Limestone is a discrete bed of fine-grained, hard, muddy, freshwater to hypersaline limestone near the base of the Bembridge Marls Member of the Bouldnor Formation (Munt 2014; Ross & Self 2014). Its age is late Priabonian, thus latest Eocene (Hooker et al. 2009). Insect and plant remains are relatively common, whilst vertebrate remains are exceptionally rare and are limited to fragmentary skeletal elements of fish, lizard, bird and mammal, bird feathers and pieces of shed lizard skin. -
Devonian Plant Fossils a Window Into the Past
EPPC 2018 Sponsors Academic Partners PROGRAM & ABSTRACTS ACKNOWLEDGMENTS Scientific Committee: Zhe-kun Zhou Angelica Feurdean Jenny McElwain, Chair Tao Su Walter Finsinger Fraser Mitchell Lutz Kunzmann Graciela Gil Romera Paddy Orr Lisa Boucher Lyudmila Shumilovskikh Geoffrey Clayton Elizabeth Wheeler Walter Finsinger Matthew Parkes Evelyn Kustatscher Eniko Magyari Colin Kelleher Niall W. Paterson Konstantinos Panagiotopoulos Benjamin Bomfleur Benjamin Dietre Convenors: Matthew Pound Fabienne Marret-Davies Marco Vecoli Ulrich Salzmann Havandanda Ombashi Charles Wellman Wolfram M. Kürschner Jiri Kvacek Reed Wicander Heather Pardoe Ruth Stockey Hartmut Jäger Christopher Cleal Dieter Uhl Ellen Stolle Jiri Kvacek Maria Barbacka José Bienvenido Diez Ferrer Borja Cascales-Miñana Hans Kerp Friðgeir Grímsson José B. Diez Patricia Ryberg Christa-Charlotte Hofmann Xin Wang Dimitrios Velitzelos Reinhard Zetter Charilaos Yiotis Peta Hayes Jean Nicolas Haas Joseph D. White Fraser Mitchell Benjamin Dietre Jennifer C. McElwain Jenny McElwain Marie-José Gaillard Paul Kenrick Furong Li Christine Strullu-Derrien Graphic and Website Design: Ralph Fyfe Chris Berry Peter Lang Irina Delusina Margaret E. Collinson Tiiu Koff Andrew C. Scott Linnean Society Award Selection Panel: Elena Severova Barry Lomax Wuu Kuang Soh Carla J. Harper Phillip Jardine Eamon haughey Michael Krings Daniela Festi Amanda Porter Gar Rothwell Keith Bennett Kamila Kwasniewska Cindy V. Looy William Fletcher Claire M. Belcher Alistair Seddon Conference Organization: Jonathan P. Wilson -
KING CHARLES CHALLENGE Experience Sustainable Transport RED ROUTE BICYCLE ISLAND ITINERARY #10
BE A KING CHARLES CHALLENGE Experience sustainable transport RED ROUTE BICYCLE ISLAND ITINERARY #10 VERY CONFIDENT ON AND OFF ROAD – NOT TOO TECHNICAL BUT FITNESS ESSENTIAL START/FINISH: CARISBROOK PRIORY, WHITCOMBE ROAD, CARISBROOKE PO30 1YS TIME: 2-3 HOURS – Bridleways and trail riding, with great views and a good experience of country life on the Island DISTANCE: km / ELEVATION GAIN: m 23.5 370 Portsmouth To Southampton s y s rr Southsea Fe y Cowe rr Cowe Fe East on - ssenger on - Pa / e assenger l ampt P c h hi Southampt Ve out S THE EGYPT POINT OLD CASTLE POINT e ft SOLENT yd R GURNARD vercra BAY Cowes e 2 5 East Cowes y Gurnard 3 3 rr tsmouth - B B OSBORNE BAY ishbournFe de r Lymington F enger Ho Ry y nger Po rr ass sse Fe P rtsmouth/Pa - Po e hicl Ve rtsmouth - ssenger Po Rew Street Pa T THORNESS AS BAY CO RIVER MEDINA E RYDE AG K E PIER HEAD ERIT Whippingham E H RYDE N C R Ve L Northwood O ESPLANADE A 3 0 2 1 ymington - TT PUCKPOOL hic NEWTOWN OO POINT A BAY W Fishbourne l Marks A 3 e /P Corner T 0 DODNOR a 2 0 A 3 0 5 4 Ryde ssenger AS CREEK & DICKSONS Binstead Ya CO Quarr Hill RYDE COPSE ST JOHN’S ROAD rmouth Wootton Spring Vale G E R CLA ME RK I N Bridge TA IVE HERSEY RESERVE, Fe R Seaview LAKE WOOTTON SEAVIEW DUVER rr ERI Porcheld FIRESTONE y H SEAGR OVE BAY OWN Wootton COPSE Hamstead PARKHURST Common WT FOREST NE Newtown Parkhurst Nettlestone P SMALLBROOK B 0 4 3 3 PRIORY BAY NINGWOOD JUNCTION SCONCE BRIDDLESFORD Havenstreet COMMON P COPSES POINT SWANPOND N ODE’S POINT BOULDNOR Cranmore Newtown deserted HAVENSTREET COPSE -
Final Report for the Blagrave Trust Project Period: April 2015 – March 2018 Reporting Period: Includes Year 3: April 2017– March 2018
Final Report for The Blagrave Trust Project Period: April 2015 – March 2018 Reporting period: includes Year 3: April 2017– March 2018 1.0 How the project has developed over the last 3 years In the three years since the start of the New Leaves Project in 2015, schools on the Isle of Wight have been through a testing time. The reduction of central funding has had a significant impact on smaller schools such as those on the Isle of Wight, particularly when compared with their counterparts just across the Solent. Schools have had to carefully scrutinise budgets and make difficult choices regarding learning opportunities outside the classroom, such as choosing whether the children can attend Forest School programmes or swimming lessons. There has also been an impact on staffing, with some key staff - both support and teaching staff – being cut. Where schools have come to us with budget deficits, we have worked with them to engineer ways for the children to attend the programmes. To this end we have delivered some programmes in school grounds, such as the woodland area and field at St Saviour’s Primary School in Totland; and local natural spaces within walking distance of the school, such as the woodland on the school site at St Mary’s Primary School in Ryde and the local beach which was just a ten minute walk away, which has saved on transport costs. The majority of schools have been able to fund the first six weeks of the programme but have been grateful for the funding from The Blagrave Trust and have understood the benefits of a twelve week programme beyond the initial six weeks. -
Late Eocene and Early Oligocene) of the Hampshire Basin
Cainozoic Research, 4(1-2), pp. 27-39, February 2006 The Neritidae of the Solent Group (Late Eocene and Early Oligocene) of the Hampshire Basin M.F. Symonds The Cottage in the Park, Ashtead Park, Ashtead, Surrey KT21 1LE, United Kingdom Received 1 June 2003; revised version accepted 7 March 2005 Gastropods of the family Neritidae in the Solent Group of the Hampshire Basin, southern England are reviewed and two previously unde- scribed taxa are described. New genus: Pseudodostia. New species: Clithon (Pictoneritina) cranmorensis and Clithon (Vittoclithon) headonensis. Neotypes designated for Neritina planulata Edwards, 1866 and Neritina tristis Forbes, 1856. Amended diagnosis: subgenus Vittoclithon. New combinations: Pseudodostia aperta (J. de C. Sowerby, 1823), Clithon (Pictoneritina) concavus (J. de C. Sowerby, 1823), Clithon (Pictoneritina) planulatus (Edwards, 1866) and Clithon (Pictoneritina) bristowi Wenz, 1929. KEY WORDS: Mollusca, Gastropoda, Neritidae, Palaeogene, Hampshire Basin. Introduction Systematic Palaeontology Family Neritidae Rafinesque, 1815 Although the number of species of Neritidae in the Solent Genus Pseudodostia gen. nov. Group is rather limited, specimens are common at certain horizons and they have received the attention of numerous Type species — Nerita aperta J. de C. Sowerby, 1825. Eo- authors in the past. In particular Curry (1960, 265-270) cene, Headon Hill Formation. dealt in detail with the taxonomy of Theodoxus concavus (J. de C. Sowerby, 1823), Theodoxus planulatus (Edwards, Derivatio nominis — The name reflects the close resem- 1866) and Theodoxus bristowi Wenz, 1929. The purpose of blance between the shell of the type species of this genus this paper is to update Curry’s work and to cover additional and that of Nerita crepidularia Lamarck, 1822, the type species. -
Fossil Ants (Hymenoptera: Formicidae): Ancient Diversity and the Rise of Modern Lineages
Myrmecological News 24 1-30 Vienna, March 2017 Fossil ants (Hymenoptera: Formicidae): ancient diversity and the rise of modern lineages Phillip BARDEN Abstract The ant fossil record is summarized with special reference to the earliest ants, first occurrences of modern lineages, and the utility of paleontological data in reconstructing evolutionary history. During the Cretaceous, from approximately 100 to 78 million years ago, only two species are definitively assignable to extant subfamilies – all putative crown group ants from this period are discussed. Among the earliest ants known are unexpectedly diverse and highly social stem- group lineages, however these stem ants do not persist into the Cenozoic. Following the Cretaceous-Paleogene boun- dary, all well preserved ants are assignable to crown Formicidae; the appearance of crown ants in the fossil record is summarized at the subfamilial and generic level. Generally, the taxonomic composition of Cenozoic ant fossil communi- ties mirrors Recent ecosystems with the "big four" subfamilies Dolichoderinae, Formicinae, Myrmicinae, and Ponerinae comprising most faunal abundance. As reviewed by other authors, ants increase in abundance dramatically from the Eocene through the Miocene. Proximate drivers relating to the "rise of the ants" are discussed, as the majority of this increase is due to a handful of highly dominant species. In addition, instances of congruence and conflict with molecular- based divergence estimates are noted, and distinct "ghost" lineages are interpreted. The ant fossil record is a valuable resource comparable to other groups with extensive fossil species: There are approximately as many described fossil ant species as there are fossil dinosaurs. The incorporation of paleontological data into neontological inquiries can only seek to improve the accuracy and scale of generated hypotheses. -
BULLETIN Feb 09
February 2009 Issue no.51 Bulletin Established 1919 www.iwnhas.org Contents Page(s) Page(s) President`s Address 1-2 Saxon Reburials at Shalfleet 10-11 Natural History Records 2 Invaders at Bonchurch 11 Country Notes 3-4 New Antiquarians 12-13 Brading Big Dig 4-5 General Meetings 13-22 Andy`s Notes 5-7 Section Meetings 22-34 Society Library 7 Membership Secretaries` Notes 34 Delian`s Archaeological Epistle 7-9 White Form of Garden Snail 9-10 President`s Address On Friday 10 th October 2008 a large and varied gathering met at Northwood House for a very special reason. We were attending the launch of HEAP, an unfortunate acronym, which still makes me think of garden rubbish. However, when the letters are opened up we find The Isle of Wight Historic Environ- ment Action Plan, a title which encompasses the historic landscape of the Island, the environment in which we live today and the future which we are bound to protect. It extends the work already being un- dertaken by the Island Biodiversity Action Plan, a little known but invaluable structure, which has al- ready been at work for ten years. This body brings together the diverse groups, national and local, whose concern is with the habitats and species which are part of our living landscape. The HEAP will do much the same at a local level for the landscape of the Island, the villages, towns, standing monuments which take us from the Stone Age to the present day and, most importantly, the agricultural landscape which is particularly vulnerable to intrusion and sometimes alarming change. -
Roman Isle of Wight
ROMAN WIGHT By Malcolm Lyne September 2006 1. A history of previous research Most of the early antiquarian research into Roman Wight, as in other parts of Britain, related to the excavation of villa houses. The earliest such excavation was that at Rock,Brighstone in 1831 (Kell 1856), followed by those at Carisbrooke (Spickernell 1859), Gurnard (Kell 1866) and Brading during the 1880s (Price and Price 1881 and 1900). Other villa sites were noted at Combley and Clatterford during the same period (Kell 1856). The published accounts of most of these excavations are somewhat deficient but, in the case of Gurnard, are supplemented by unpublished manuscript notes of further excavations carried out after publication of the earlier work in 1866. Just a few of the artefacts found at Carisbrooke and Gurnard still survive. The one exception to this sorry tale is Brading: the published accounts of the excavations carried out by Captain Thorp and the Price brothers is more informative than most for this period and most of the pottery and other finds are still extant. Other 19 th c. observations on the Island’s Roman archaeology are largely restricted to brief accounts of coin hoards from Farringford, Wroxall and Cliff Copse, Shanklin written up by Kell (1863). A further hoard found at Wootton in 1833 had to wait for more than 100 years before a reasonably-detailed account was produced (Sydenham 1943). The early years of the 20 th century saw little improvement in the quality of atchaeological activity relating to Roman Wight. Poorly-recorded excavations at Combley villa in 1910 (Sydenham 1945, 426-29) were, however, soon followed by the activities of Ambrose Sherwin as curator of Carisbrooke Castle museum during the 1920s and 30s. -
Military HEAP for the Isle of Wight
Island Heritage Service Historic Environment Action Plan Military Type Report Isle of Wight County Archaeology and Historic Environment Service April 2010 01983 823810 Archaeology @iow.gov.uk Iwight.com Military HEAP for the Isle of Wight 1.0 INTRODUCTION Page 3 2.0 ASSESSMENT OF THE HISTORIC ENVIRONMENT Page 4 2.1 Location, Geology and Topography Page 4 2.2 The Nature of the Historic Environment Resource Page 4 2.3 The Island’s HEAP overview document Page 4 3.0 DEFINING MILITARY STATUS Page 5 4.0 ANALYSIS AND ASSESSMENT OF MILITARY/DEFENCE Page 5 ASSETS 4.1 Principle Historical Processes Page 5 4.2 Surviving Archaeology and Built Environment Page 7 4.3 Relationship with other HEAP Types Page 21 4.4 Contribution of Military/Defence Type to Isle of Wight Historic Page 22 Environment and Historic Landscape Character 4.5 Values, Perceptions and Associations Page 22 4.6 Resources Page 23 4.7 Accessibility and Enjoyment Page 24 4.8 Heritage Assets of Particular Significance Page 26 5.0 CONSERVATION AND MANAGEMENT Page 28 5.1 Forces for Change Page 28 5.2 Management Issues Page 30 5.3 Conservation Designation Page 31 6.0 FUTURE MANAGEMENT Page 33 7.0 GLOSSARY OF TERMS Page 34 8.0 REFERENCES Page 36 2 Iwight.com 1.0 INTRODUCTION The Isle of Wight Historic Environment Action Plan (HEAP) consists of a set of general documents, 15 HEAP Area Reports and a number of HEAP Type reports which are listed in the table below: General Documents HEAP Area Reports HEAP Type Reports HEAP Map of Areas Arreton Valley Agricultural Landscapes HEAP Introduction -
Draft Island Planning Strategy Habitat Regulations Assessment Report
Draft Island Planning Strategy Habitat Regulations Assessment report November 2018 Contents EXECUTIVE SUMMARY ............................................................................................ 1 1. INTRODUCTION .................................................................................................... 4 Background and purpose of this report ........................................................................... 4 The Habitats Directive and Regulations ......................................................................... 5 2. Approach to HRA screening ....................................................................................... 7 3. STAGE ONE – BASELINE INFORMATION GATHERING ................................... 10 European and Ramsar site information ........................................................................ 10 Site information ............................................................................................................ 11 5. Policies that could lead to Likely Significant Effects .................................................. 22 6. STAGE TWO – SCREENING .............................................................................. 25 Draft Island Planning Strategy policy screening ........................................................... 26 Initial Policy screening .................................................................................................. 27 7. STAGE THREE – APPROPRIATE ASSESSMENT ............................................. 36 8. Detailed policy -
Feed Premises
Isle of Wight Council Trading Standards Service Premise Registration No. Categories Chale Farm, Church Place, Chale, Isle Of Wight, PO38 2HB GB867‐1649 R13 4 High Road, Newport, Isle Of Wight, PO30 5PD GB867‐4569 R13 17 Melbourne Street, Newport, Isle Of Wight, PO30 1QY GB867‐8054 R13 17 Lugley Street, Newport, Isle Of Wight, PO30 5HD GB867‐10022 R13 105 Horsebridge Hill, Newport, Isle Of Wight, PO30 5TL GB867‐11781 R13 Highwood House, Highwood Lane, Rookley, Isle Of Wight, PO38 3NN GB867‐17218 R13 Upper Shide Mill House, Blackwater Road, Newport, Isle Of Wight, PO30 3BB GB867‐17311 R13 Marvel Farm, Marvel Lane, Newport, Isle Of Wight, PO30 3DT GB867‐17314 R13 50 Hefford Road, East Cowes, Isle Of Wight, PO32 6QU GB867‐22053 R13 Stockbridge Cottage, Slay Lane, Whitwell, Isle Of Wight, PO38 2QF GB867‐23244 R13 Merstone Cottage, Merstone Lane, Arreton, Isle Of Wight, PO30 3DE GB867‐25574 R13 Cherry Acre Cottage, Rew Lane, Wroxall, Isle Of Wight, PO38 3AX GB867‐26880 R13 1 Lessland Cottages, Lessland Lane, Godshill, Isle Of Wight, PO38 3AS GB867‐27303 R13 Rock Point, Lower Woodside Road, Wootton, Isle Of Wight, PO33 4JT GB867‐28752 R13 Sweet Briar Cottage, East Ashey Lane, Ryde, Isle Of Wight, PO33 4AT GB867‐42499 R13 17 St Michaels Avenue, Ryde, Isle Of Wight, PO33 3DY GB867‐43939 R13 Church Cottage, Main Road, Thorley, Isle Of Wight, PO41 0SS GB86745887 R13 Mattingley Farm, Main Road, Wellow, Isle Of Wight, PO41 0SZ GB867‐48423 R13 Shalcombe Manor, Brook Road, Calbourne, Isle Of Wight, PO41 0UF GB867‐49656 R13 Reeah Ii, Hamstead Road, Cranmore, -
Distribution of Landslides and Geotechnical Properties Within the Hampshire Basin
Distribution of landslides and geotechnical properties within the Hampshire Basin Kwanjai Yuangdetkla, Andy Gibson & Malcolm Whitworth University of Portsmouth, Portsmouth, UK Claire Foster, David Entwisle & Catherine Pennington British Geological Survey, Nottingham UK ABSTRACT This paper outlines the sedimentary sequences and geotechnical properties of the Hampshire Basin, a basin of filled with 700 m of Palaeogene clays, silts, sands and limestones in southern England. The paper presents results so far of a study to synthesize relevant geological and geotechnical data and relate these to the nature of the landslides in this basin. The study has found that stratigraphic sequences and geotechnical properties vary considerably across the basin owing to basin morphology and depositional environments which are correspond to complex paleogeography and tectonic movements during the Tertiary. Over-consolidated clays with low residual shear strengths are extensive on moderately steep slopes and prone to landsliding, especially on over-steepened coastal sections. Landslides vary from mudflows through mudslides, rotational landslides and minor falls. Landslide characteristics are strongly influenced by lithology but gradient appears to be the controlling factor in many cases. The presences of weak strata (clays, lignite, laminated layers), the pre-existing shear surface, the lithological interface (sand overlying clay) play important roles to locally control the position of the shear surface and the type of movements. At a basin scale, inland landslides are associated with the development of drainage system during and since the Tertiary. 1 INTRODUCTION structures trend east-west or northeast-southwest (Melville and Freshney, 1982). Locally, the complex 2 The Hampshire Basin underlies 3 400km of the mainland reactivation of basement faulting has produced many of Southern England and the northern half of the nearby local structures forming gentle hills and valleys such as Isle of Wight (Figure 1).