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666 results for “Wales”
Figs 5-6 in Molophilus (Molophilus) johnmartini nov.sp. from the Blue Mountains in New South Wales, Australia (Diptera: Limoniidae)
Figs 5-6: Molophilus (Molophilus) johnmartini nov.sp., female, terminalia: (5) dorsal; (6) lateral.
Fig. 2. Mecyclothorax moorei n in A New Species of the Genus Mecyclothorax Sharp from New South Wales (Insecta: Coleoptera, Carabidae: Psydrinae)
Fig. 2. Mecyclothorax moorei n.sp., male aedeagus, parameres and genital ring. Scales: 0.25 mm.
Fig. 3. Mecyclothorax moorei n in A New Species of the Genus Mecyclothorax Sharp from New South Wales (Insecta: Coleoptera, Carabidae: Psydrinae)
Fig. 3. Mecyclothorax moorei n.sp., female gonocoxites 1 and 2. Scale: 0.1 mm.
Fig. 14 in A Reassessment of Saltuarius swaini (Lacertilia: Diplodactylidae) in Southeastern Queensland and New South Wales; Two New Taxa, Phylogeny, Biogeography and Conservation
Fig. 14. Rock habitats of Saltuarius
Fig. 7 in A Reassessment of Saltuarius swaini (Lacertilia: Diplodactylidae) in Southeastern Queensland and New South Wales; Two New Taxa, Phylogeny, Biogeography and Conservation
Fig. 7 (continued). V-shaped pattern between eyes in S. wyberba QM J28648.
Micro-CT analysis of Katian radiolarians from the Malongulli Formation, New South Wales, Australia, and implications for skeletogenesis
<p><span>A diverse and well-preserved radiolarian assemblage from the Malongulli Formation, New South Wales, Australia contains 13 species representing ten genera and six families. One new genus: <em>Wiradjuri</em> n. gen. is introduced to accommodate pre-Devonian single-shelled entactiniid taxa and one new species: <em>Secuicollacta</em> <em>malongulliensis</em> n. sp. is recorded together with some previously described forms. The micro-structure of the 'rotasphaerid structure/primary unit' and the 'ectopic spicule' are investigated to validate their roles as fundamental units in the Secuicollactidae together with comprehensive documentation of the previously enigmatic <em>Pseudorotasphaera</em> internal skeleton.</span></p> <p><span>The results of this investigation suggest that, among all radiolarian genera that survived the </span>Late Ordovician Mass Extinction <span>event (LOME) and transitioned into the Silurian, <em>Secuicollacta</em>, <em>Haplotaeniatum</em>, and <em>Palaeoephippium</em> maintained stable body plans during the transition and were more successfully established. The selective advantages these lineages had during the LOME, were most likely spontaneous outcomes of the mode of structural development involving sequential skeletogenesis and a tendency to evolve towards simpler body plans. </span></p>
Fig. 4. A in The geological setting and palaeoenvironmental and palaeoecological reconstructions of the Upper Permian insect beds at Belmont, New South Wales, Australia
Fig. 4. A block model of the Belmont coal swamps and gravel channel system.
Fig. 2 in The geological setting and palaeoenvironmental and palaeoecological reconstructions of the Upper Permian insect beds at Belmont, New South Wales, Australia
Fig. 2. Section of insect seam from Pincombe's Outcrop (site 206, see Fig. 3).
Fig. 3 in The geological setting and palaeoenvironmental and palaeoecological reconstructions of the Upper Permian insect beds at Belmont, New South Wales, Australia
Fig. 3. Map of Belmont insect beds, showing new and old collection sites.
An infoveillance analysis of public interest, national data and wastewater monitoring in Wales, UK
<p>Infoveillance, wastewater and national data.R - The R script used for the analyses and figures present in the manuscript.</p> <p> </p> <p>R functions:</p> <p>flattenCorrMatrix.R -A function for correlation analysis</p> <p>cormtest.R - A function for correlation analysis</p> <p> </p> <p>Data files:</p> <p>Medical data.csv - Data extracted from the UK government portal for COVID-19 cases, deaths and vaccinations</p> <p>South Wales qPCR data.csv - qPCR data for different South Wales sites on each date, with ‘signal’ denoting the signal of SARS-CoV-2 detection in wastewater samples</p> <p>Wales GT data.csv - Google Trends relative search volume data extracted directly from Google Trends for the region of Wales</p>
Canovium Roman Fort, Wales
Canovium Roman Fort and hillfort Pen-y-Castell in N part of Wales. Sadly lidar data is concentrated on valleys, so we cant see 4-5 other hillforts in this #landscape that are on top of a hills. Source: Objaverse 1.0 / Sketchfab
Gop Cairn, Trelawnyd, Flintshire, Wales, UK
Gop Cairn is located on the summit of Gop Hill north of Trelawnyd, Flintshire in Wales. It is the largest prehistoric constructed mound in Wales and the second largest, after Silbury Hill in Wiltshire, in the UK. It dates to the Neolithic period (4300 - 2300 BC). The mound of collected limestone rubble is approximately 14 metres high and 100 x 70 metres across. It was investigated in 1886 by Boyd Dawkins who excavated a shaft in the top and then a 30ft tunnel from the base of the shaft. He claims to have missed the centre of the mound and any burial that may have been there. The only artefacts recovered included some horse bones and the bones of some other animals. The shaft has partly collapsed leaving the present day cratered summit. Gop Cave can be seen downslope of the cairn. Recent clearance of the scrub around the base of the mound has now revealed it once more in its entirety for public viewing . The views from the top are superb in all directions and a visit to Gop Cairn is highly recommended. Source: Objaverse 1.0 / Sketchfab
Tspe_v1 (Telopea speciosissima) genome supplementary files for: Chromosome-level de novo genome assembly of Telopea speciosissima (New South Wales waratah) using long-reads, linked-reads and Hi-C
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Data and code from: Wide-Angle Lung Experiment Segmentation (WALES): A novel methodology for quantitative assessment of lung pathology in model systems
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Reversing the decline of threatened koala (Phascolarctos cinereus) populations in New South Wales: Using genomics to enhance conservation outcomes
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Micro-CT analysis of Katian radiolarians from the Malongulli Formation, New South Wales, Australia, and implications for skeletogenesis
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Examining patterns in opioid prescribing for non-cancer-related pain in Wales: preliminary data from a retrospective cross-sectional study using large datasets
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Data from: Habitat usage of Daubenton's bat (Myotis daubentonii), common pipistrelle (Pipistrellus pipistrellus), and soprano pipistrelle (Pipistrellus pygmaeus) in a North Wales upland river catchment
Distributions of Daubenton's bat (Myotis daubentonii), common pipistrelle, (Pipistrellus pipistrellus), and soprano pipistrelle (Pipistrellus pygmaeus) were investigated along and altitudinal gradient of the Lledr River, Conwy, North Wales, and presence assessed in relation to the water surface condition, presence/absence of bank‐side trees, and elevation. Ultrasound recordings of bats made on timed transects in summer 1999 were used to quantify habitat usage. All species significantly preferred smooth water sections of the river with trees on either one or both banks; P. pygmaeus also preferred smooth water with no trees. Bats avoided rough and cluttered water areas, as rapids may generate high‐frequency echolocation‐interfering noise and cluttered areas present obstacles to flight. In lower river regions, detections of bats reflected the proportion of suitable habitat available. At higher elevations, sufficient habitat was available; however, bats were likely restricted due to other factors such as a less predictable food source. This study emphasizes the importance of riparian habitat, bank‐side trees, and smooth water as foraging habitat for bats in marginal upland areas until a certain elevation, beyond which bats in these areas likely cease to forage. These small‐scale altitudinal differences in habitat selection should be factored in when designing future bat distribution studies and taken into consideration by conservation planners when reviewing habitat requirements of these species in Welsh river valleys, and elsewhere within the United Kingdom.
Data from: Katian (Upper Ordovician) conodonts from Wales
Middle and Upper Katian conodonts are previously known in the British Isles from relatively small collections obtained from a few localities. The present study is mainly based on 17 samples containing more than 17,000 conodont elements from an approximately 14 m thick succession of the Sholeshook Limestone in a road cut near Whitland, South Wales that yielded a diverse fauna of more than 40 taxa. It is dominated by representatives of Amorphognathus, Aphelognathus/Plectodina, and Eocarniodus along with several coniform taxa. Representatives of Decoriconus, Istorinus and Sagittodontina are reported from the Ordovician of UK for the first time. The fauna is a typical representative of the British Province of the Atlantic Realm and includes a mixture of taxa of North American, Baltoscandic, and Mediterranean affinities along with pandemic species. Based on the presence of many elements of Amorphognathus ordovicicus and some morphologically advanced specimens of A. superbus, the Sholeshook Limestone is referred to the lower A. ordovicicus Zone. Most of the unit is also coeval with Zone 2 of the Cautleyan Stage in the British regional stage classification, and Stage Slice Ka3 of the middle Katian Stage in the global stratigraphical classification, an age assignment consistent with data from trilobites, graptolites, and chitinozoans. The unusually large collection of M elements of Amorphognathus provides insight into the complex morphological variation of this element of some Katian species of this genus. The Sholeshook conodont fauna is similar to those of the Crûg and Birdshill limestones but differs in several respects from the slightly older ones from the Caradocian type area in the Welsh Borderland. Although having some species in common, the Sholeshook conodont fauna clearly differs from coeval Baltoscandic faunas, and is even more different in composition compared with equivalent North American Midcontinent faunas.
Data from: Lower Jurassic foraminifera from the Llanbedr (Mochras Farm) Borehole, North Wales, UK
The complete, fully cored Lower Jurassic (Hettangian, Sinemurian, Pliensbachian, Toarcian) succession from the Llanbedr (Mochras Farm) Borehole, North Wales, the thickest known British section, has yielded a diverse and well preserved foraminiferal fauna, comprising 270 species and subspecies which are described and illustrated. An additional nine taxa, not encountered at Mochras, are also described. This typical European Boreal Atlantic foraminiferal fauna is dominated by members of the Lagenida, with the Ceratobuliminoidea, Miliolida, Spirillinina, Involutinina, Buliminida and Textulariida as important accessory groups. The Ceratobuliminoidea and Miliolida are unusually diverse, with Reinholdella and Ophthalmidium being notably abundant. The presence of the family Oberhauserellidae is significant. A benthonic foraminiferal biozonation scheme for the Lower Jurassic, comprising 16 biozones and tied to the standard ammonite-based chronostratigraphy, is described in detail. It is recognizable across the northern European Boreal province and as far south as Spain and France, and is applicable to subsurface hydrocarbon exploration of the UK continental shelf and onshore Europe. Three new genera (Duoplanum, Extonia and Haynesella) are described as well as 19 new species (Citharina sherringtoni, Duoplanum inaequale, D. leve, Glomospirella liassica, Lagena? haeusleri, L. semisulcata, Lagenammina pseudofusiformis, L. tangentia, Loxostomum liassicum, Marginulina turneri, Neobulimina bangae, Nodosaria pseudoclaviformis, Ophthalmidium strictum, Reinholdella? mochrasensis, R. robusta, Reussoolina? lacrimaforma, Semiiinvoluta excelsa, Tubinella pseudoinornata, and Vinelloidea lordi), and 10 new subspecies (Berthelinella involuta striata, Ichthyolaria terquemi barnardi, I. terquemi mediumcostata, Lenticulina varians barnardi, Loxostomum liassicum liassicum, L. liassicum teres, Ophthalmidium macfadyeni tenuiloculare, Paralingulina cernua ssp. A, Reinholdella margarita dorsoplana, and R. pachyderma humilis). Two further species are renamed as Nodosaria whittakeri and Paralingulina paranodosaria .
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Allen Brain Atlas
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