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Artigos de revistas sobre o tema "England – Devon"

Autor: Grafiati

Publicado: 25 de julho de 2024

Última modificação: 31 de julho de 2024

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1

Warrington, G., and R. C. Scrivener. "The Permian of Devon, England." Review of Palaeobotany and Palynology 66, no. 3-4 (1990): 263–72. http://dx.doi.org/10.1016/0034-6667(90)90042-h.

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2

Haynes, R. M. "Radon and Lung Cancer in Cornwall and Devon." Environment and Planning A: Economy and Space 25, no. 9 (1993): 1361–66. http://dx.doi.org/10.1068/a251361.

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The relationship between average indoor levels of radon and lung cancer mortality in the counties of Cornwall and Devon, England, are investigated. The associations of population density, social-class distribution, and regional smoking prevalence with lung cancer mortality in the local-authority districts of England and Wales were estimated by regression analysis. Low rates of lung cancer in Cornwall and Devon were predicted from the relationship. The differences between observed and predicted mortality in Cornwall and Devon districts were compared with average indoor levels of radon, which varied considerably between districts. Residual variations in lung cancer mortality were not significantly correlated with average indoor radon measurements. The current advice of the National Radiological Protection Board to government is to concentrate radon measurements, remedial action, and preventive action principally on Cornwall and Devon, but cross-sectional geographical data do not support the hypothesis that raised levels of radon indoors in southwest England have an important effect on lung cancer mortality.

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3

Taylor, Paul D., and Silviu O. Martha. "Cenomanian cheilostome bryozoans from Devon, England." Annales de Paléontologie 103, no. 1 (2017): 19–31. http://dx.doi.org/10.1016/j.annpal.2016.11.002.

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4

Simmons, M. D., and C. L. Williams. "Cretaceous Orbitolinidae (Foraminifera) from Onshore and Offshore South-West England." Journal of Micropalaeontology 11, no. 1 (1992): 21–30. http://dx.doi.org/10.1144/jm.11.1.21.

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Abstract. The occurrence of orbitolinids in onshore and offshore South-West England is fully documented for the first time. Palorbitolina lenticularis is known from the Early Aptian — Late Barremian sediments of the offshore Fastnet Basin, and may also occur in the Aptian Farringdon Greensand. Late Albian Orbitolina sefini occurs in the Wolborough Limestone of Devon, whilst at Haldon, Devon, the orbitoline faunas are of Early Cenomanian age and referable to Orbitolina cf. concava. The orbitolinids from the Upper Greensand of the south-east Devon coast and the Fastnet Basin cannot be precisely identified, but belong to the Late Albian — Early Cenomanian O. sefini - O. concava plexus. Previous records of Orbitolina from the Upper Greensand at Wilmington are shown to be mistaken. These records are in fact referable to the sponge Porosphaera. The precise identification of some of the orbitolinids from South-West England supports the ages of the Wolborough Limestone and Haldon Sands suggested by Hamblin &amp; Wood (1976). It is thought that orbitolinids migrated from Iberia to South-West England via the South-West Approaches during the Late Albian.

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5

Todd, Malcolm. "Roman Military Occupation at Hembury (Devon)." Britannia 38 (November 2007): 107–23. http://dx.doi.org/10.3815/000000007784016511.

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The large hillfort at Hembury, near Honiton (Devon) is one of the most impressive late prehistoric sites in South-West England. Occupied in the Neolithic and Iron Age, it was taken over by a Roman force about or shortly before A.D. 50. Substantial timber buildings were constructed, including a probablefabrica, in which iron from the adjacent Blackdown hills was worked. The Roman site was abandoned by the early Flavian period and not reoccupied. Though not evidently a conventional fort, Hembury joins a list of hillforts in South-West England which were used by the Roman army in the early decades of conquest. These include Hod Hill and possibly Maiden Castle (Dorset), Ham Hill and South Cadbury (Somerset).

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6

Quiney, Anthony. "The Buildings of England: Devon. By BridgetCherryand NikolausPevsner." Archaeological Journal 147, no. 1 (1990): 467–68. http://dx.doi.org/10.1080/00665983.1990.11077981.

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7

Godfray, H. Charles J., and John J. Day. "Opius pulicariae Fischer (Hymenoptera: Braconidae: Opiinae) added to the British checklist." Entomologist's Monthly Magazine 158, no. 2 (2022): 128–30. http://dx.doi.org/10.31184/m00138908.1582.4134.

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Opius pulicariae Fischer (Braconidae: Opiinae) is added to the British list based on a specimen reared from Ophiomyia pulicaria (Diptera: Agromyzidae) in Devon, England in 2021. Means of distinguishing this species from other Opiinae are given and its host range discussed.

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8

Whitehead, Paul F. "Issus muscaeformis (Schrank, 1781) (Hemiptera: Issidae) new to Devon." Entomologist's Gazette 71, no. 4 (2020): 283–86. http://dx.doi.org/10.31184/g00138894.714.1785.

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9

Gillmore, Gavin K., Paul Phillips, Antony Denman, Malcolm Sperrin, and Gillian Pearce. "Radon Levels in Abandoned Metalliferous Mines, Devon, Southwest England." Ecotoxicology and Environmental Safety 49, no. 3 (2001): 281–92. http://dx.doi.org/10.1006/eesa.2001.2062.

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10

Richards, A. J. "Five new species of Taraxacum section Celtica (Asteraceae) from Britain and Ireland." British & Irish Botany 1, no. 2 (2019): 167–84. http://dx.doi.org/10.33928/bib.2019.01.167.

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Five new species of the mostly west European Taraxacum section Celtica A.J.Richards (Asteraceae) are described. Taraxacum amicorum is only known from Somerset, England; T. atrocollinum has also been found in Devon and Ireland. Taraxacum chrysoglossum is described from Bute and is also recorded from the eastern Highlands, Scotland. Taraxacum elegantifrons occurs on light calcareous soils in Ireland. Taraxacum chlorofrugale P. Oosterv. ex A.J. Richards from Germany, Netherlands, south England and Ireland is described formally for the first time.

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11

Wilson, R. Trevor. "The indigenous domestic livestock of the County of Devon, England." Animal Genetic Resources/Ressources génétiques animales/Recursos genéticos animales 48 (April 2011): 63–77. http://dx.doi.org/10.1017/s2078633610001037.

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12

Larner, Glenn. "The Darlington Event 6, Devon, England, May 14-17, 1998." Australian and New Zealand Journal of Family Therapy 19, no. 4 (1998): ii—iii. http://dx.doi.org/10.1002/j.1467-8438.1998.tb00332.x.

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13

Brereton, Tom, Duncan Jones, Keith Leeves, Kate Lewis, Rachel Davies, and Trudy Russel. "Population structure, mobility and conservation of common bottlenose dolphin off south-west England from photo-identification studies." Journal of the Marine Biological Association of the United Kingdom 98, no. 5 (2017): 1055–63. http://dx.doi.org/10.1017/s0025315417000121.

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In this study photo-identification data were used to better understand movements, population structure and abundance of common bottlenose dolphin (Tursiops truncatus) in south-west England and surrounding waters, to inform conservation efforts. A catalogue of 485 photographic sightings of 113 individuals was compiled from ~150 common bottlenose dolphin encounters made on 87 dates between March 2007 and January 2014. From these and other data, three likely sub-populations were identified in the western English Channel, demarcated by bathymetry and distance to land: (1) south-west England – inshore Cornwall to Devon, (2) offshore English/French waters and (3) inshore France from Brittany to Normandy. Maximum abundance estimates for south-west England coastal waters, using two methods, ranged between 102 and 113 (range 87–142, 95% CL) over the period 2008–2013, likely qualifying the region as nationally important, whilst the yearly maximum was 58 in 2013. The population was centred on Cornwall, where 19 well-marked animals were considered ‘probable’ residents. There were no ‘probable’ resident well-marked individuals found to be restricted to either Devon or Dorset, with animals moving freely within coastal areas across the three counties. Movements were also detected within offshore English waters and French waters (from other studies) of the western English Channel, but no interchange has as yet been detected between the three regions, highlighting the possible separation of the populations, though sample sizes are insufficient to confirm this. Given the findings, south-west England waters should be considered as a separate management unit requiring targeted conservation efforts.

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14

Thorpe, R. S. "Permian K-rich volcanic rocks of Devon: petrogenesis, tectonic setting and geological significance." Transactions of the Royal Society of Edinburgh: Earth Sciences 77, no. 4 (1987): 361–66. http://dx.doi.org/10.1017/s0263593300023233.

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ABSTRACTPotassium (K)-rich volcanic rocks occur within Permian sedimentary rocks in SW England and are approximately contemporaneous with the emplacement of the Cornubian granite batholith. The volcanic rocks have chemical characteristics of subduction-related magmas and may have been derived by small amounts of partial melting of heterogeneous large-ion lithophile (LIL) enriched mantle with the assemblage olivine–pyroxene–garnet–phlogopite–titanate. The LIL enrichment may have occurred during shallow or oblique subduction of oceanic lithosphere below SW England during the Devonian and Carboniferous. Such LIL-enriched mantle may have contributed some components to the Cornubian granite batholith.

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15

Giavarini, V. J. "Lichens of the Dartmoor Rocks." Lichenologist 22, no. 4 (1990): 367–96. http://dx.doi.org/10.1017/s0024282990000421.

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AbstractA description of the lichen communities associated with natural rock outcrops and derelict mine workings in the upland region of Dartmoor, south-west England, is presented. An examination of 34 study sites revealed 270 taxa, of which 28 are reported as new to Devon including several national rarities. Notes on 29 tors have been prepared and reasons for the predominance or decline of particular communities or species are discussed.

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16

Jones, A. P., and J. V. Smith. "Phlogopite and associated minerals from Permian minettes in Devon, South England." Bulletin of the Geological Society of Finland 57, no. 1-2 (1985): 89–102. http://dx.doi.org/10.17741/bgsf/57.1-2.006.

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17

Claughton, Peter. "The crown silver mines and the historic landscape in Devon (England)." ArchéoSciences, no. 34 (April 10, 2010): 299–308. http://dx.doi.org/10.4000/archeosciences.2862.

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18

Davies, D. A. R. "Breeding sheep with 4 teats in a flock in Devon, England." Agricultural and Food Science 60, no. 6 (1988): 620–21. http://dx.doi.org/10.23986/afsci.72324.

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A survey of British breeds and crossbreeds revealed that they contained ewes with extra teats, in many cases even functional. In one flock, a crossbred mix of three breeds, some selection for 4 teats had taken place and 79 of 147 ewes had 4 teats and 2 ewes had 6 teats. Length of the extra teats varied up to a 09:1 ratio relative to the rear. 38 of the 79 ewes had a ratio between 0.6:1 and 0.9:1. The distance from front to rear was generally between 0.2 and 0.5 of that from side to side. In 1986 the 147 ewes were divided into 5 unequal size family groups, A (51), B (53), C (21), D (6), each group mated to one ram with 4 teats, and group E (12) to a ram with 2 teats but whose dam had 4. The mean teat number for the ewes in the groups was 3.26, 2.95, 2.70, 4.00 and 3.76 resp., and for their offspring 3.84 (91), 3.06 (95), 3.4 (37), 3.3 (12) and 3.1 (9), More detailed analysis of the larger groups, A,B and C, showed that the proportion of lambs with 4 teats from 4 teated ewes was 0.96, 0.76 and 0.88, resp., and that in groups A and B the proportion of lambs with 4 teats from 2 teated ewes was 0.78 and 0.31 respectively. Milk production of 14 ewes with well developed fore teats was measured in the first 10 days of lactation using the oxytocin technique. The mean yield of the front teats was only 0.057+ 0.010 of the rear, indicating the wide variation and the limited production of the population at present in the flock.

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19

Willis, R. P., J. C. Martin, and K. J. Ridout. "Water Quality Improvements for Estuaries and Coastal Waters, North Devon, England." Water Science and Technology 25, no. 12 (1992): 13–22. http://dx.doi.org/10.2166/wst.1992.0333.

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Environmental protection legislation and public expectation require increasingly higher quality standards for coastal recreational waters. The immediate objective is compliance with EC Directives and UK legislation but consideration has also to be given to the possibility of higher future standards. The paper describes the environmental and engineering investigations for a major improvement scheme in an area of high amenity value where tourism is a principal source of employment. Schemes must be based on comprehensive survey data and a thorough evaluation to satisfy the requirements of the National Rivers Authority which is the regulatory body for discharges to the aquatic environment. A wide range of improvement options has been considered and the reasons for selecting the preferred options are explained. The significance of disinfection techniques and marine treatment are discussed. Over recent years a considerable interest has developed in environmental issues and consultation with customers, elected representatives and organisations has been important throughout the development of this scheme.

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20

Paar, W. H., A. C. Roberts, A. J. Criddle, and D. Topa. "A new mineral, chrisstanleyite, Ag2Pd3Se4, from Hope's Nose, Torquay, Devon, England." Mineralogical Magazine 62, no. 2 (1998): 257–64. http://dx.doi.org/10.1180/002646198547611.

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AbstractChrisstanleyite, Ag2Pd3Se4, is a new mineral from gold-bearing carbonate veins in Middle Devonian limestones at Hope's Nose, Torquay, Devon, England. It is associated with palladian and argentian gold, fischesserite, clausthalite, eucairite, tiemannite, umangite, a Pd arsenide-antimonide (possibly mertieite II), cerussite, calcite and bromian chlorargyrite. Also present in the assemblage is a phase similar to oosterboschite, and two unknown minerals with the compositions, PdSe2 and HgPd2Se3. Chrisstanleyite occurs as composite grains of anhedral crystals ranging from a few µm to several hundred µm in size. It is opaque, has a metallic lustre and a black streak, VHN100 ranges from 371–421, mean 395 kp/mm2 (15 indentations), roughly approximating to a Mohs hardness of 5. Dcalc = 8.308 g/cm3 for the ideal formula with Z = 2. In plane-polarised reflected light, the mineral is very slightly pleochroic from very light buff to slightly grey-green buff; is weakly bireflectant and has no internal reflections. Bireflectance is weak to moderate (higher in oil). Anisotropy is moderate and rotation tints vary from rose-brown to grey-green to pale bluish grey to dark steel-blue. Polysynthetic twinning is characteristic of the mineral. Reflectance spectra and colour values are tabulated. Very little variation was noted in eleven electron-microprobe analyses on five grains, the mean is: Ag 25.3, Cu 0.17, Pd 37.5, Se 36.4, total 99.37 wt.%. The empirical formula (on the basis of ∑M + Se = 9) is (Ag2.01Cu0.02)∑2.03 Pd3.02Se3.95, ideally Ag2Pd3Se4. Chrisstanleyite is monoclinic, a 6.350(6), b 10.387(4), c 5.683(3) Å β 114.90(5)°, space group P21/m (11) or P21(4). The five strongest X-ray powder-diffraction lines [d in Å (I)(hkl)] are: 2.742 (100) (–121), 2.688 (80) (–221), 2.367 (50) (140), 1.956 (100) (–321,150) and 1.829 (30) (–321, 042). The name is in honour of Dr Chris J. Stanley of The Natural History Museum in London. The mineral and its name have been approved by the Commission on New Minerals and Mineral Names of the International Mineralogical Association.

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21

Hart, Malcolm B. "Cretaceous foraminifera from the Turonian succession at Beer, southeastern Devon, England." Cretaceous Research 29, no. 5-6 (2008): 1035–46. http://dx.doi.org/10.1016/j.cretres.2008.05.019.

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22

Knight, D., P. W. Elliott, J. M. Anderson, and D. Scholefield. "The role of earthworms in managed, permanent pastures in Devon, England." Soil Biology and Biochemistry 24, no. 12 (1992): 1511–17. http://dx.doi.org/10.1016/0038-0717(92)90142-k.

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23

Romon-Ochoa, Pedro, Pankajini Samal, Caroline Gorton, et al. "Cryphonectria parasitica Detections in England, Jersey, and Guernsey during 2020–2023 Reveal Newly Affected Areas and Infections by the CHV1 Mycovirus." Journal of Fungi 9, no. 10 (2023): 1036. http://dx.doi.org/10.3390/jof9101036.

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In England, Cryphonectria parasitica was detected for the first time in 2011 in a nursery and in 2016 in the wider environment. Surveys between 2017 and 2020 identified the disease at different sites in Berkshire, Buckinghamshire, Cornwall, Derbyshire, Devon, Dorset, London, West Sussex, and the island of Jersey, while the present study comprises the results of the 2020–2023 survey with findings in Derbyshire, Devon, Kent, Nottinghamshire, Herefordshire, Leicestershire, London, West Sussex, and the islands of Jersey and Guernsey. A total of 226 suspected samples were collected from 72 surveyed sites, as far north as Edinburgh and as far west as Plymouth (both of which were negative), and 112 samples tested positive by real-time PCR and isolation from 35 sites. The 112 isolates were tested for the vegetative compatibility group (VCG), mating type, and Cryphonectria hypovirus 1 (CHV1). Twelve VCGs were identified, with two of them (EU-5 and EU-22) being the first records in the UK. Both mating types were present (37% MAT-1 and 63% MAT-2), but only one mating type was present per site and VCG, and perithecia were never observed. Cryphonectria hypovirus 1 (CHV1), consistently subtype-I haplotype E-5, was detected in three isolates at a low concentration (5.9, 21.1, and 33.0 ng/µL) from locations in London, Nottinghamshire, and Devon.

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24

Jagt, J. W. M., and H. W. Oosterink. "The echinoid Holaster laevis from the Albian (Lower Cretaceous) of the Winterswijk area, eastern Netherlands." Netherlands Journal of Geosciences - Geologie en Mijnbouw 89, no. 3-4 (2010): 239–41. http://dx.doi.org/10.1017/s0016774600000718.

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AbstractA single internal mould of the holasterid echinoid Holaster laevis (Brongniart, 1822) constitutes the first record of this species from the upper portion (‘Upper Holland Marl’) of the Holland Formation (Rijnland Group), of middle-late Albian age, in the Winterswijk area (eastern Netherlands). The geographic range of H. laevis can thus be extended to this part of western Europe, with previous records from southern England (Wiltshire, Devon) and the Département Ain in east-central France.

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25

Neima, Anna. "The Politics of Community Drama in Interwar England." Twentieth Century British History 31, no. 2 (2019): 170–96. http://dx.doi.org/10.1093/tcbh/hwz035.

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Abstract There was a wave of reform-oriented drama across England in the 1920s and 1930s, which extended from urban, socialist theatre to the ‘late modernist’ enthusiasm for rural pageantry and from adult education to Church revival. Most scholarship looks at drama in these various milieus separately, but this study of three plays that were put on in a corner of South West England—a nativity play, an innovative ‘dance-mime’, and a Workers’ Educational Association narrative piece—brings them together. These plays shared a connection to Dartington Hall, a social and cultural experiment set on a large estate in Devon in 1925 by an American heiress, Dorothy Elmhirst, and her Yorkshire-born husband, Leonard, which became a nexus for the various strands of community-seeking theatre evident in interwar England—as well as for social reform more generally. This article shows how dramatic performances formed part of the quest for communal unity that was a dominant strand in social thinking between the wars: driven by fears about class strife, the effects of democratization, the recurrence of war, and the fragmenting effects of secular modernity, elites, artists, and activists of diverse hues tried to reform the very idea of Englishness by putting on plays—fostering values of community and communality, while often taking inspiration from an idealized vision of the rural community of England’s pre-industrial past.

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26

Groves-Kirkby, C. J., A. R. Denman, P. S. Phillips, R. G. M. Crockett, and J. M. Sinclair. "Comparison of seasonal variability in European domestic radon measurements." Natural Hazards and Earth System Sciences 10, no. 3 (2010): 565–69. http://dx.doi.org/10.5194/nhess-10-565-2010.

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Abstract. Analysis of published data characterising seasonal variability of domestic radon concentrations in Europe and elsewhere shows significant variability between different countries and between regions where regional data is available. Comparison is facilitated by application of the Gini Coefficient methodology to reported seasonal variation data. Overall, radon-rich sedimentary strata, particularly high-porosity limestones, exhibit high seasonal variation, while radon-rich igneous lithologies demonstrate relatively constant, but somewhat higher, radon concentrations. High-variability regions include the Pennines and South Downs in England, Languedoc and Brittany in France, and especially Switzerland. Low-variability high-radon regions include the granite-rich Cornwall/Devon peninsula in England, and Auvergne and Ardennes in France, all components of the Devonian-Carboniferous Hercynian belt.

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27

Braithwaite, R. S. W., W. H. Paar, and J. E. Chisholm. "Phurcalite from Dartmoor, Southwest England, and its identity with ‘nisaite’ from Portugal." Mineralogical Magazine 53, no. 373 (1989): 583–89. http://dx.doi.org/10.1180/minmag.1989.053.373.09.

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AbstractYellow blades on joint surfaces in granite from Merrivale quarry, Dartmoor, Devon, are shown to be of a slightly aresenatian variety of phurcalite by X-ray powder diffraction, infrared spectroscopy, electron microprobe and thermal analyses and optical methods. The results from these techniques are tabulated, including assignments for infrared absorption bands. Comparison of X-ray powder diffraction, infrared spectroscopic and optical data with those obtained from samples of ‘nisaite’, an incompletely described mineral from Nisa, Portugal, indicates that the latter is also phurcalite.

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28

Gamble, B., M. Anderson, and J. S. Griffiths. "Chapter 13 Hazards associated with mining and mineral exploitation in Cornwall and Devon, SW England." Geological Society, London, Engineering Geology Special Publications 29, no. 1 (2020): 321–67. http://dx.doi.org/10.1144/egsp29.13.

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AbstractThe largest UNESCO World Heritage Site in the UK is found in Cornwall and west Devon, and its designation is based specifically on its heritage for metalliferous mining, especially tin, copper and arsenic. With a history of over 2000 years of mining, SW England is exceptional in the nature and extent of its mining landscape. The mining for metallic ores, and more recently for kaolin, is a function of the distinctive geology of the region. The mining hazards that are encountered in areas of metallic mines are a function of: the Paleozoic rocks; the predominant steeply dipping nature of mineral veins and consequent shaft mining; the great depth and complexity of some of the mines; the waste derived from processing metallic ores; the long history of exploitation; and the contamination associated with various by-products of primary ore-processing, refining and smelting, notably arsenic. The hazards associated with kaolin mining are mainly related to the volume of the inert waste products and the need to maintain stable spoil tips, and the depth of the various tailings’ ponds and pits. The extent of mining in Cornwall and Devon has resulted in the counties being leaders in mining heritage preservation and the treatment and remediation of mining-related hazards.

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29

Głuchowski, E., and G. Racki. "Disarticulated crinoid stems from the Devonian and Carboniferous of north Devon, England." Proceedings of the Yorkshire Geological Society 55, no. 3 (2005): 161–72. http://dx.doi.org/10.1144/pygs.55.3.161.

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30

Greenberg, Neil, Keith Lloyd, Chris O'Brien, Sian McIver, Amanda Hessford, and Martin Donovan. "A Prospective Survey of Section 136 in Rural England (Devon and Cornwall)." Medicine, Science and the Law 42, no. 2 (2002): 129–34. http://dx.doi.org/10.1177/002580240204200203.

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31

Turner, P. J. "Stratigraphic and structural variations in the Lifton-Marystow area, West Devon, England." Proceedings of the Geologists' Association 96, no. 4 (1985): 323–35. http://dx.doi.org/10.1016/s0016-7878(85)80021-3.

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32

Jones, Andy M., and Henrietta Quinnell. "Daggers in the West: Early Bronze Age Daggers and Knives in the South-west Peninsula." Proceedings of the Prehistoric Society 79 (May 14, 2013): 165–91. http://dx.doi.org/10.1017/ppr.2013.4.

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This paper describes the results from a project to date Early Bronze Age daggers and knives from barrows in south-west England. Copper alloy daggers are found in the earliest Beaker associated graves and continue to accompany human remains until the end of the Early Bronze Age. They have been identified as key markers of Early Bronze Age graves since the earliest antiquarian excavations and typological sequences have been suggested to provide dating for the graves in which they are found. However, comparatively few southern British daggers are associated with radiocarbon determinations. To help address this problem, five sites in south-west England sites were identified which had daggers and knives, four of copper alloy and one of flint, and associated cremated bone for radiocarbon dating. Three sites were identified in Cornwall (Fore Down, Rosecliston, Pelynt) and two in Devon (Upton Pyne and Huntshaw). Ten samples from these sites were submitted for radiocarbon dating. All but one (Upton Pyne) are associated with two or more dates. The resulting radiocarbon determinations revealed that daggers/knives were occasionally deposited in barrow-associated contexts in the south-west from c. 1900 to 1500 calbc.The dagger at Huntshaw, Devon, was of Camerton-Snowshill type and the dates were earlier than those generally proposed but similar to that obtained from cremated bone found with another dagger of this type from Cowleaze in Dorset: these dates may necessitate reconsideration of the chronology of these daggers

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LOVETT, J. K., P. H. EVANS, S. O'CONNELL, and N. J. GUTOWSKI. "Neuroborreliosis in the South West of England." Epidemiology and Infection 136, no. 12 (2008): 1707–11. http://dx.doi.org/10.1017/s0950268808000472.

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SUMMARYAlthough Lyme borreliosis is increasingly diagnosed in the United Kingdom, few systematic studies have been performed there. UK data suggest that the commonest complications are neurological, but inadequate information exists about their nature and the incidence of late neuroborreliosis. Local data are necessary because clinical presentations may show geographical variation. This study aimed to provide data on clinical manifestations in an area of South West England and to estimate treatment delay. We reviewed clinical records of 88 patients in the Royal Devon and Exeter Hospital catchment area who had positive Borrelia antibody tests during a 5-year period. Fifty-six (64%) reported tick bites. The commonest presentations were erythema migrans (65%) and arthralgia/myalgia (27%). However, 22 patients (25%) had neurological symptoms other than headache alone. Fourteen had facial palsy, eight had confusion/drowsiness, four had meningism, five had radiculopathy, two had sixth nerve palsies, and two had peripheral neuropathies. No late, progressive or atypical neurological syndromes were found. Neurological manifestations were generally predictable and usually included either (or all) of meningoencephalitis, facial palsy or radiculopathy.

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Godfray, H. Charles J. "Laotris luzulae (Hymenoptera, Braconidae, Alysiinae, Dacnusini), a new species from the southwest of England." Journal of Hymenoptera Research 95 (February 17, 2023): 73–83. http://dx.doi.org/10.3897/jhr.95.97490.

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Laotris luzulae Godfray, sp. nov. is described in the small genus Laotris Nixon, 1943, (Braconidae, Alysiinae, Dacnusini) from five specimens reared from Cerodontha silvatica (Groschke, 1957) (Diptera, Agromyzidae) mining Luzula sylvatica (Huds.) Gaudin (Juncaceae) in Devon and Gloucestershire in the southwest of Great Britain. Six further specimens from Somerset caught as adults in the 1950s are also noted. It differs morphologically from the three described species of Laotris and shows a 4.2% and 6.6% genetic distance at the CO1 barcode locus from an undescribed North American species and from the European L. striatula (Haliday, 1839), respectively.

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Carpenter, S., and J. D. Radley. "Discovery and preparation of a large mass of articulated Early Jurassic crinoids from Black Ven (Dorset and East Devon Coast World Heritage Site, south-west England)." Geological Curator 9, no. 3 (2010): 103–6. http://dx.doi.org/10.55468/gc216.

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Early Jurassic marine mudrocks on south-west England's Dorset and East Devon Coast World Heritage Site are well known as a source of spectacularly preserved examples of the fossil crinoid Pentacrinites fossilis Blumenbach. This paper outlines the geological and palaeobiological contexts of a recent find, and the measures taken for its preparation, conservation and preservation.

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Jarvis, Ian, Greg Carson, Malcolm Hart, Paul Leary, and Bruce Tocher. "The Cenomanian-Turonian (late Cretaceous) anoxic event in SW England : evidence from Hooken Cliffs near Beer, SE Devon." Newsletters on Stratigraphy 18, no. 3 (1988): 147–64. http://dx.doi.org/10.1127/nos/18/1988/147.

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Carson, Greg A. "Silicification fabrics from the Cenomanian and basal Turonian of Devon, England: isotopic results." Geological Society, London, Special Publications 36, no. 1 (1987): 87–102. http://dx.doi.org/10.1144/gsl.sp.1987.036.01.08.

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Neville, Julia. "Challenge, Conformity and Casework in Interwar England: the first women councillors in Devon." Women's History Review 22, no. 6 (2013): 971–94. http://dx.doi.org/10.1080/09612025.2013.780846.

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Wignall, P. B. "Sedimentology of the Triassic-Jurassic boundary beds in Pinhay Bay (Devon, SW England)." Proceedings of the Geologists' Association 112, no. 4 (2001): 349–60. http://dx.doi.org/10.1016/s0016-7878(01)80014-6.

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Massey, Anthony C., Michael A. Paul, W. Roland Gehrels, and Dan J. Charman. "Autocompaction in Holocene coastal back-barrier sediments from south Devon, southwest England, UK." Marine Geology 226, no. 3-4 (2006): 225–41. http://dx.doi.org/10.1016/j.margeo.2005.11.003.

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Zhao, H. X., R. A. Moyeed, E. A. Stenhouse, A. G. Demaine, and B. A. Millward. "Space-time clustering of childhood Type 1 diabetes in Devon and Cornwall, England." Diabetic Medicine 19, no. 8 (2002): 667–72. http://dx.doi.org/10.1046/j.1464-5491.2002.00761.x.

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42

Loughran, R. J., B. L. Campbell, and D. E. Walling. "Soil erosion and sedimentation indicated by caesium 137: Jackmoor Brook catchment, Devon, England." CATENA 14, no. 1-3 (1987): 201–12. http://dx.doi.org/10.1016/s0341-8162(87)80018-8.

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Godfrey, Elizabeth, and Sali Tagliamonte. "Another piece for the verbal -s story: Evidence from Devon in southwest England." Language Variation and Change 11, no. 1 (1999): 87–121. http://dx.doi.org/10.1017/s0954394599111050.

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This article aims to contribute (1) new data on verbal -s by systematically examining its behavior in Devon English (DE), a variety spoken in southwest England, and (2) a broader historical and cross-dialectal perspective for understanding the origin and function of verbal -s in nonstandard varieties of English in North America. We focus on the linguistic contexts of its occurrence from the diachronic and synchronic literature. The results show that verbal -s is conditioned by phonological, syntactic, semantic, and lexical factors. These include the few variable constraints on verbal -s attested throughout the evolution of verbal -s in the history of the English language. Moreover, DE exhibits patterns of verbal -s variability that have previously been associated with African American Vernacular English (AAVE). The detailed nature of these linguistic correspondences—not only in frequency of the features examined, but most importantly in the details of an entire set of internal linguistic factors conditioning them—reveal that verbal -s is a linguistic feature of AAVE that originated in British dialects.

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Reed, Stephen, Paul Bidwell, and John Allan. "Excavation at Bantham, South Devon, and Post-Roman Trade in South-West England." Medieval Archaeology 55, no. 1 (2011): 82–138. http://dx.doi.org/10.1179/174581711x13103897378447.

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Phillips, D. R., and J. Vincent. "Privatising residential care for elderly people: The geography of developments in Devon, England." Social Science & Medicine 26, no. 1 (1988): 37–47. http://dx.doi.org/10.1016/0277-9536(88)90043-3.

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Girling, Simon J., Gidona Goodman, Paul Burr, et al. "Evidence of Leptospira species and their significance during reintroduction of Eurasian beavers (Castorfiber) to Great Britain." Veterinary Record 185, no. 15 (2019): 482. http://dx.doi.org/10.1136/vr.105429.

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The Scottish Beaver Trial (SBT) reintroduced the Eurasian beaver (Castor fiber) in 2009 using wild-caught Norwegian beavers. This included a six-month prerelease quarantine in Devon, England. The International Union for Conservation of Nature (IUCN) and government guidelines for health screening were followed, including testing for Leptospira species. Unlicensed beavers, from Germany, were also identified in Scotland (Tayside) and Devon (later forming the River Otter Beaver Trial (ROBT)) and were health-screened under licence. Due to positive Leptospira species results and lack of prerelease screening in ROBT and Tayside, beavers from Germany and Norway (range sources) were screened. One hundred and fifty-six samples from 151 beavers were analysed by Leptospira species quantitative PCR (qPCR) (n=73 kidney (postmortem)/urine samples (antemortem)) or microscopic agglutination test (MAT, Leptospira pools 1–6) (n=83 serum samples). No beavers from Norway (95 per cent confidence interval (CI) 0–5.6 per cent, n=52), Tayside or SBT postrelease (95 per cent CI 0–4.6 per cent, n=63) tested positive. Seven beavers from Germany and Devon were positive. This gives an overall 9.3 per cent (95 per cent CI 5.2-15.1 per cent) exposure level, of which 4.6 per cent (95 per cent CI 1.9-9.3 per cent) suggested infection on a positive qPCR (n=1) or MAT titre of at least 1/400 (n=6), although none had abnormal physical, biochemical or haematological changes. This study suggests that Leptospira species infection in wild Eurasian beavers occurs at a low level, has no sex bias and does not appear to cause significant morbidity or mortality.

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Padel, Oliver. "King Æthelstan and Cornwall." Offa's Dyke Journal 4 (October 18, 2022): 66. http://dx.doi.org/10.23914/odj.v4i0.354.

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During the three centuries from about AD 700 to 1000, Cornwall became a border area through the anglicisation and absorption into Wessex of its neighbour Devon, then ceased to be one when it was itself fully absorbed into the newly-formed kingdom of England. The particular focus here is on the reign of Æthelstan (924–939). Four events relating to Cornwall are considered in detail, including William of Malmesbury’s twelfth-century account of Æthelstan’s treatment of the Cornish. His statement that Æthelstan ‘expelled the Cornish from Exeter’, if accepted, refers not to native Devonians but to economic migrants from Cornwall itself.

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McHARDY, ALISON, and NICHOLAS ORME. "The Defence of an Alien Priory: Modbury (Devon) in the 1450s." Journal of Ecclesiastical History 50, no. 2 (1999): 303–12. http://dx.doi.org/10.1017/s0022046999001694.

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Alien priories, the small dependencies of foreign religious houses established in the years following the Norman Conquest, were partly thank-offerings for military success and partly civilising centres and reminders of home for England's new rulers. Their foundation in the newly-conquered lands mirrored the success of the Anglo-Normans in colonising the British Isles, since later examples were planted in southern Scotland and in Ireland too. In England their establishment dated from the late eleventh to the early thirteenth centuries. They passed out of existence over a time-scale which was almost as long, for from the late thirteenth century, during periods of Anglo-French war, they were under attack from the crown as alleged nests of spies and as exporters of wealth to the enemy. The consequent seizure of these small houses by the crown and their vigorous exploitation by the exchequer reduced monastic life in all these houses and extinguished it in many, so that the mother houses found it advantageous to sell smaller properties while some of the larger priories were prompted to seek denization. Such solutions are evident from the last two decades of the fourteenth century. Apparent landmarks in this process of disintegration and change prove, upon close inspection, to be illusory; neither the ‘expulsion’ of 1378 nor the Act of Dissolution of 1414 were such decisive moments in the history of these houses as was once thought. Instead, we may suggest, each of these small houses must be examined separately, for the later history of each was distinctive. The religious life was entirely extinguished in some, which had become merely manors, by the later fourteenth century. Courtiers under Edward III and Richard II acquired a number which they used for the endowment of new religious houses; the Carthusian order was an especial beneficiary. Henry V endowed his new foundation of Sheen with alien priories, while some others were used to augment the endowments of existing monasteries and even hospitals. Pontefract (Yorkshire), thanks to the good offices of John of Gaunt, became denizen in 1393.

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Philips, David R., John Vincent, and Sarah Blacksell. "The Development of Private Residential Accommodation for the Elderly: the Case of Devon, England." Espace, populations, sociétés 5, no. 1 (1987): 235–48. http://dx.doi.org/10.3406/espos.1987.1195.

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Zhao, H. X., E. Stenhouse, E. Sanderson, et al. "Continued rising trend of childhood Type 1 diabetes mellitus in Devon and Cornwall, England." Diabetic Medicine 20, no. 2 (2003): 168–70. http://dx.doi.org/10.1046/j.1464-5491.2003.00829_3.x.

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