1,722,008 research outputs found
L'histoire de la Goutelle
Adnet , Rogissart . L'histoire de la Goutelle. In: L'information géographique, volume 5, n°4, 1941. p. 85
L'histoire de la Goutelle
Adnet , Rogissart . L'histoire de la Goutelle. In: L'information géographique, volume 5, n°4, 1941. p. 85
ADNeT Neuropsychology Norming Tool
The Australian Dementia Network (ADNeT) Neuropsychology Norming Tool app is a web application designed for clinical neuropsychologists to enter patient cognitive assessment data. The app will summarise the cognitive assessment results and provide a benchmark with respect to normalisation values found in literature.\nLineage: The app was written using R statistical software, and implemented using the R Shiny package
Oromobula dakhlaensis Adnet & Cappetta & Guinot & Sciara 2012, SP. NOV.
OROMOBULA DAKHLAENSIS SP. NOV. (FIG. 6) <p> <i>Type locality:</i> DAK3. Unit 2, level B2; from two sites south of Ad Dakhla (35.5 km and 41.5 km), southwestern Morocco (Adnet <i>et al</i>., 2010).</p> <p> <i>Type horizon:</i> Samlat Formation, Gerran member (Ratschiller, 1967) – late Middle Eocene/Late Eocene.</p> <p> <i>Synonymy:</i> <i>Mobula</i> sp. (Adnet <i>et al</i>., 2010) in text only.</p> <p> <i>Etymology:</i> Species named after the peninsula of Dakhla, south-western Morocco.</p> <p> <i>Holotype:</i> DAK 2B-5 (Fig. 6E–H).</p> <p> <i>Diagnosis:</i> Same as the genus.</p> <p> <i>Description:</i> Crown is three or more times higher than root. Its lateral extremities are flared as in holotype (Fig. 6E) to convex (Fig. 6A) in labial or lingual view. Strongly labiolingually flattened, its lingual face is concave between a basal transversal roll of enameloid, overlapping the root/crown boundary, toward the transversal crest. Labial face is however, principally convex with a curve that follows those of lingual face in profile (Fig. 6B). Labial visor is only visible on the smallest tooth (Fig. 6N) but disappears in larger ones (Fig. 6B, F) and root is totally overhung in labial view (Fig. 6C, G). Nearly all the labial surface (visor included) is ragged by numerous deep vertical folds that form partially anastomosing lamellae around the mid part of labial face. The basal part is devoid of grooves, especially on the small teeth (Fig. 6M–P) considered as the youngest specimen. The apical part of the labial face that edges the transversal crest (making an occlusal surface) is flat, nearly horizontal, and smooth (except on the smallest elements, Fig. 6M–P) because of scouring by functional wear. Occlusal contour is chaotic (Fig. 6D, H, L), with no geometric structure indicating possible interlocking columns of teeth, even weakly. The transversal crest is irregular and largely overlaps the lingual face. The lingual face is relatively smooth except under the transversal crest where a few pronounced vertical folds extend below the transversal crest (Fig. 6E, M). Root is extremely reduced in size, both in height and depth. Except on some of the youngest specimens of the type series (Fig. 6M, N), root is principally at the polyaulacorhize state. Root lobes are lamella-like and are well-spaced, except on the youngest specimens (Fig. 6M, N), in which the root shows a more compact shape. Small scattered foramina are sometimes visible on the labial and lingual faces of root, as in holotype (Fig. 6E, G).</p> <p> <i>Discussion:</i> Teeth of † <i>O. dakhlaensis</i> gen. et sp. nov. come only from the level B2 (see Adnet <i>et al</i>., 2010 for geological details) and have never been found together with those of <i>A. barbei</i> gen. et sp. nov. from the underlying level B1. Distinct in time, these two taxa are also distinct in morphology with the youngest († <i>O. dakhlaensis</i> gen. et sp. nov.) having more strongly labiolingually compressed teeth with a higher crown without well-marked bulge on the labial face, a non-ornamented lingual face and a higher root strongly compressed labiolingually compared to the crown with well-spaced short lamellae.</p> <p> Neither sexual nor monognathic heterodonty are seen in our limited sample. However, ontogenetic heterodonty is substantial within the smallest specimens (Fig. 6I–P), which display teeth showing more morphological affinities with those of <i>Mobula</i> (e.g. holaulacorhize to polyaulacorhize root, labial face partially ornamented, presence of an individualized labial visor). The labiolingual flattening as well as the enameloid ornamentation is moreover only slightly marked on the smallest teeth. Affinities with the Oligocene † <i>E. kowaldi</i> and † <i>P. kruibekensis</i> are marked as they share a number of similar characters such as a reduced labial visor combined with a concave lingual face in large teeth and a flat occlusal surface with a transversal crest often ragged (contrary to † <i>Plinthicus</i>). However, the enameloid layer on the lingual face is globally smooth (except some scattered folds) as in † <i>Eomanta</i> and contrary to † <i>Plinthicus.</i> The teeth are strongly constricted labiolingually with a high crown/root ratio and the root possesses thin regular lamellae as in † <i>Plinthicus</i> and contrary to † <i>Eomanta</i>. Indeed, this genus represents an intermediate form with a mixed suite of characters existing in both enigmatic genera. Comparisons may be extended with care to † <i>P. stenodon</i>, as some small specimens of this species with large teeth recovered from the mid Miocene of North Carolina, USA (H. Cappetta, unpubl. data), resemble those of † <i>O. dakhlaensis</i> gen. et sp. nov. However, we remain unsure whether these unstudied and unfigured teeth really represent juvenile specimens of † <i>P. stenodon</i> or a different lineage.</p>Published as part of <i>Adnet, Sylvain, Cappetta, Henri, Guinot, Guillaume & Sciara, Giuseppe Notarbartolo Di, 2012, Evolutionary history of the devilrays (Chondrichthyes: Myliobatiformes) from fossil and morphological inference, pp. 132-159 in Zoological Journal of the Linnean Society 166 (1)</i> on page 145, DOI: 10.1111/j.1096-3642.2012.00844.x, <a href="http://zenodo.org/record/5408589">http://zenodo.org/record/5408589</a>
The Australian Dementia Network (ADNeT): Bringing together Australia’s dementia stakeholders
The Australian Dementia Network (ADNeT) will bring together Australia’s leading dementia researchers and clinicians in an effort to prevent or effectively treat dementia. We will develop strong linkages with consumers, community groups, service providers, charities and industry bodies. ADNeT will work to improve care, expand access to specialist services and advanced diagnostic methods, and speed the development of effective therapies and disease prevention strategies for all Australians.$18,000,000.00Boosting Dementia Research InitiativeNational Dementia Networ
ADnet - Un network regionale per i pazienti Alzheimer
<p>Presentazione del caso d'uso "ADnet".</p>
Catalogue général n° 19 de verrerie, chimie, bactériologie comprenant : l\u27aménagement du laboratoire, porcelaine terre et grès, verrerie, produits chimiques, appareils d\u27analyse, étuves, appareils de stérilisation, microscopes, microtomes, cages et appareils à contention, centrifugeurs, instruments pour vaccins et sérums, laboratoire sans gaz, outillage
1 vol. (895 p.-1 f.) : ill. ; 25 c
Galeorhinus louisi Adnet & Cappetta 2008
Galeorhinus louisi Adnet & Cappetta, 2008 Fig. 23 G–J Galeorhinus louisi Adnet & Cappetta, 2008: 438, fig. 4. Material examined UNITED STATES OF AMERICA – Alabama • 2 isolated teeth; Claiborne Group; MSC 37353.1 – 2. Description Teeth small, not exceeding 2.2 mm in mesiodistal width; distal-most extent of main cusp in line with, or slightly exceeding, distal extent of heel. Mesial cutting edge elongate, ranges from straight to slightly sinuous; distal edge much shorter, slightly convex, forms triangular and distally inclined cusp with mesial edge. Prominent distal heel bears one or two cusplets, which are not well differentiated from the heel itself. Lingual crown face smooth, strongly convex. Labial face with bulbous base that overhangs the root; very short folds and wrinkles at base that coalesce apically to form a transverse ridge (easily seen in profile view). Root high and thick, with highly diverging and rounded lobes; lobes separated by shallow and triangular interlobe area. Lingual root face bisected by deep nutritive groove. Remarks The teeth in our sample appear conspecific to the holotype of G. louisi Adnet & Cappetta, 2008 in that they have extensive folds and notches present along the entire width of the labial crown base. This ornamentation is indistinct or absent on the teeth of G. minutissimus, present only beneath the heels on the teeth of G. mesetaensis, and is much less extensive on the teeth of G. duchaussoisi (see above) and G. ypresiensis (see below). Stratigraphic and geographic range in Alabama The specimens in our sample were collected from the Tallahatta Formation at site AMo-8. Lower Lutetian, Zone NP14.Published as part of Ebersole, Jun A., Cicimurri, David J. & Stringer, Gary L., 2019, Taxonomy and biostratigraphy of the elasmobranchs and bony fishes (Chondrichthyes and Osteichthyes) of the lower-to-middle Eocene (Ypresian to Bartonian) Claiborne Group in Alabama, USA, including an analysis of otoliths, pp. 1-274 in European Journal of Taxonomy 585 on pages 63-64, DOI: 10.5852/ejt.2019.585, http://zenodo.org/record/366025
Ouverture du colloque
Adnet Jean-Jacques. Ouverture du colloque. In: Le Fablier. Revue des Amis de Jean de La Fontaine, n°10, 1998. La Fontaine et le Moyen Âge (actes de Reims, 5-6 juin 1998) pp. 11-13
Aturobatis Adnet 2006
Aturobatis aff. A. aquensis Adnet, 2006 Fig. 41 Aturobatis aquensis Adnet, 2006: 111, pl. 39, figs 3a–5b. Material examined UNITED STATES OF AMERICA – Alabama • 2 isolated teeth; Claiborne Group; MSC 37687, MSC 38464. Description Large teeth approaching 4.0 mm in mesiodistal width. Occlusal outline of crown is rhomboidal, wider than long, with sharp labial, lingual and lateral angles. Oral surface flat and diamond-shaped, subparallel to basal plane of crown. Sharp medial vertical ridge of labial face flanked by concave faces, with indistinct transverse ridge near the crown foot. Crown is weakly concave on each side of the vertical ridge. Lingual crown face slightly higher than labial face, inclined, straight, weakly concave on either side of lingual angle. Lingual crown foot developed into distinctive shelf-like projection, forming acute angle with lingual face. All crown faces smooth. Base of crown overhangs root labially and laterally. Root narrow, distally located under lingual part of crown, bilobed with a shallow medial nutritive groove. Root lobes rather elongate, with oblique labial face, extending just past lingual crown foot. Remarks The gross morphology of MSC 37687 and MSC 38464 is similar to other the Dasyatidae teeth in our sample, but the teeth are much larger and lack crown ornamentation.These teeth are also morphologically similar to the lateral teeth of members of the Myliobatidae, however, the lack of labial and lingual ornament on vertical crown faces and narrow, distally located root are inconsistent with our observations of Lisbon Formation Myliobatidae (see below). Teeth of Aturobatis are not to be confused with Hypolophodon, which has a weakly convex occlusal surface, much less angular appearance in occlusal and profile views, and a wide, centrally located root (Dartevelle & Casier 1959; Murray et al. 2010: figs 2c–d; Cappetta 2012: fig. 412). Adnet et al. (2010) and Cappetta (2012) mentioned the occurrence of Aturobatis in Ypresian strata in the Atlantic Coastal Plain of the USA, and a younger, potentially new species has been noted from the Priabonian of Morocco (Adnet et al. 2010). Only the type species, A. aquensis, has been described and illustrated, and the two teeth in our Lisbon Formation sample, although much larger, are comparable to the Lutetian teeth reported by Adnet (2006). However, as A. aquensis is based on only four teeth and the range of variation is not known, we tentatively assign our two teeth to this species. Discovery of additional specimens will help determine if the Lisbon taxon is distinct or conspecific with A. aquensis. Stratigraphic and geographic range in Alabama The two specimens in our sample were collected from the basal Lisbon Formation at site ACov-11. Lower Lutetian, Zone NP15.Published as part of Ebersole, Jun A., Cicimurri, David J. & Stringer, Gary L., 2019, Taxonomy and biostratigraphy of the elasmobranchs and bony fishes (Chondrichthyes and Osteichthyes) of the lower-to-middle Eocene (Ypresian to Bartonian) Claiborne Group in Alabama, USA, including an analysis of otoliths, pp. 1-274 in European Journal of Taxonomy 585 on pages 116-117, DOI: 10.5852/ejt.2019.585, http://zenodo.org/record/366025
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