Libération : organe des Français libres

1943/11/16 (N155).

Libération : organe des Français libres

1943/11/02 (N153).

Libération : organe des Français libres

1943/10/08 (N149).

Libération : organe des Français libres

1943/10/12 (N150).

Libération : organe des Français libres

1943/09/28 (N148).

Libération : organe des Français libres

1943/09/21 (N147).

Bède, sur l'Apocalypse.

Catalogue de l'abbaye de Corbie (éd. d'E. Coyecque, Cat des mss des bibliothèques de France, XIX, p.XI-XLVIII) XIIe s.: n°66 ?; 1621: n°114 ? Ex-libris : pas de mention de provenance

Evangelia quattuor.

Ce ms. renferme la lettre de saint Jérôme au pape Damase, "Beato papae Damaso..." (1-3v), sa préface "Plures fuisse" (4-6r), les tables de concordances évangéliques (6v-14r), les textes des quatre Évangiles accompagnés des préfaces, prologues et sommaires (14v-213v), ainsi que le Capitulare evangeliorum ou liste des péricopes évangéliques (214-231v). En marge des Évangiles, numérotation des chapitres des sommaires à l'encre rouge et indication des concordances évangéliques à l'encre brune. Entre les ff. 61 et 66, 96- 101, 155-160v et 204v-208v (c'est-à-dire dans les passages correspondant à la Passion dans chacun des quatre Evangiles), de petites lettres à l'encre rouge orangé (a, c, m) introduisent les différents protagonistes du discours, le m désignant le Christ, le c Pilate et le a le narrateur. Au f. 155, le m est partiellement développé sous la forme "mans.". Ces indications nous renseignent sur les pratiques de la lecture liturgique, qui s'effectuait à plusieurs voix. Nombreuses corrections marginales ou interlinéaires à l'encre rouge ou noire, mots à corriger parfois surlignés en couleur (cf. "aliquid" f. 76v surligné en violet), mots réécrits par-dessus grattage aux ff. 115v-116 (par le copiste E).Dans le Capitulare evangeliorum, on remarquera, parmi un sanctoral à dominante romaine, la présence de deux saints mérovingiens du Hainaut, saint Ursmer, fêté le 18 avril (f. 226v), et sainte Amalberge, fêtée le 10 juillet (f. 228), ainsi que celle des saints Emerentienne et Macaire l'Egyptien, fêtés le 23 janvier (f. 225v), et des saints martyrs romains Pierre et Marcellin, fêtés le 2 juin (f. 227). Ursmer et Amalberge ont tous deux un lien avec l'abbaye bénédictine Saint-Pierre de Lobbes: le premier en est le véritable fondateur, la seconde y a été ensevelie, mais cela n'implique pas nécessairement que le ms. ait été exécuté à Lobbes, car le culte de ces deux saints jouissait d'une diffusion régionale. Quant aux autres saints, le culte de sainte Emerentienne et de saint Macaire était répandu en particulier dans les diocèses de Cambrai et Reims et celui des martyrs Pierre et Marcellin autour de Valenciennes, Gand et Soissons, où se trouvaient depuis le IXe siècles leurs reliques ; cf. sur le culte d'Amalberge, Pierre et Marcellin: F. Dolbeau, "La bibliothèque de l'abbaye d'Hasnon...", Revue des études augustiniennes 34 (1988), p. 237-246; sur celui d'Ursmer: F. Dolbeau, "La diffusion de la Vita S. Ursmari de Rathier de Vérone", Scribere sanctorum gesta. Recueil d'études d'hagiographie médiévale offert à Guy Philippart, Turnhout, 2005, p. 181-207.Au f. 231v ont été rajoutées diverses maximes et formules pieuses, par deux mains différentes, des XIIe-XIIIe siècles.

Feuillet d'une demi-Bible en français ayant appartenu à Jean de Berry

A l'exception des ex-libris et annotations de Jean Flamel, le manuscrit ne contient que la fin du Psautier sur une colonne (f. 4v) : « Sire, delivre nous en l'eure de la mort. / Sire, delivre (a exponctué) nous au jour du jugement ...-.... Sire, oy m'oroison / Et mon cri a toy viengne ». « Dex a qui propre chose est d'avoir merci ...-.... que la grant misericorde de ta pitié nous absoille. Par Crist nostre Seigneur. Ainsi soit il ». « Ci fine le Psautier en françois ». « Ci doit venir aprés le livre des paraboles Salemon ».

Supplément grec 1295

PORSON (Richard). papiers

Structural, stratigraphic and geochemical studies of the Horwood Peninsula - Gander Bay Area, Northeast Newfoundland /

The Horwood Peninsula - Gander Bay area is located at NE Newfoundland in the Botwood Zone (Williams et a1., 1974) or in the Dunnage Zone (Williams, 1979) of the Central Mobile Belt of the Newfoundland Appalachians. The area is underlain by Middle Ordovician to possible Lower Silurian rocks of the Davidsville and Indian Islands Groups, respectively. Three conformable formations named informally : the Mafic Volcanic Formation, the Greywacke and Siltstone Formation and the Black Slate Formation, have been recognized in the Davidsville Group. The Greywacke and the Black Slate Formations pass locally into a Melange Formation. From consideration of regional structure and abundant locally-derived mafic volcanic olisto- 1iths in the melange, it is considered to have originated by gravity sliding rather than thrusting. Four formations have been recognized in the Indian Islands Group. They mainly contain silty slate and phyllite, grey cherty siltstone, green to red micaceous siltstone and limestone horizons. Repetition of lithological units by F1 folding are well-demonstrated in one of formations in this Group. The major structure in this Group on the Horwood Peninsula is interpreted to be a synclinal complex. The lithology of this Group is different from the Botwood Group to the west and is probably Late Ordovician and/or Early Silurian in age. The effects of soft-sediment deformation can be seen from the lower part of the Davidsville Group to the middle part of the Indian Islands Group indicating continuous and/or episodic slumping and sliding activities throughout the whole area. However, no siginificant depOSitional and tectonic break that could be assigned to the Taconian Orogeny has been recognized in this study. Three periods of tectonic deformation were produced by the Acadian Orogeny. Double boudinage in thin dikes indicates a southeast-northwest sub-horizontal compression and main northeast-southwest sub-horizontal extension during the D1 deformation. A penetrative, axial planar slaty cleavage (Sl) and tight to isocJ.ina1 F1 folds are products of this deformation. The D2 and D3 deformations formed S2 and S3 fabrics associated with crenulations and kink bands which are well-shown in the slates and phyllites of the Indian Islands Group. The D2 and D3 deformations are the products of vertical and northeast-southwest horizontal shortening respectively. The inferred fault between the Ordovician slates (Davidsville Group) and the siltstones (Indian Islands Group) suggested by Williams (1963, 1964b, 1972, 1978) is absent. Formations can be followed without displacement across this inferred fault. Chemically, the pillow lavas, mafic agglomerates, tuff beds and diabase dikes are subdivided into three rock suites : (a) basaltic komatiite (Beaver Cove Assemblage), (b) tholeiitic basalt (diabase dikes), (c) alkaline basalt (Shoal Bay Assemblage). The high Ti02 , MgO, Ni contents and bimodal characteristic of the basaltic komatiite in the area are comparable to the Svartenhuk Peninsula at Baffin Bay and are interpreted to be the result of an abortive volcano-tectonic rift-zone in a rear-arc basin. Modal and chemical analyses of greywackes and siltstones show the trend of maturity of these rocks increasing from poorly sorted Ordovician greywackes to fairly well-sorted Silurian siltstones. Rock fragments in greywackes indicate source areas consisting of plagiogranite, low grade metamorphic rocks and ultramafic rocks. Rare sedimentary structures in both Groups indicate a southeasterly provenance. Trace element analyses of greywackes also reveal a possible island-arc affinity.

Brown Bess Socket Mount Bayonet

This original Brown Bess socket mount bayonet is vintage War of 1812. It was purchased in the Niagara area and likely has a long local provenance.

CENTRAL NORTH ATLANTIC PALEOCEANOGRAPHY DURING THE MIDDLE PLEISTOCENE (ca. 726–603 ka): INSIGHTS FROM THE DINOFLAGELLATE CYST RECORD

Integrated Ocean Drilling Program (IODP) Site U1313, located at the northern boundary of the subtropical gyre in the central North Atlantic, lies within the southern part of the ice-rafted debris belt. Seventy-three palynological samples were studied from an uninterrupted interval ca. 726–603 ka (upper Marine Isotope Stage [MIS] 18 through lower MIS 15) to resolve conflicting paleoceanographic interpretations. Glacial stages were characterized by high productivity surface waters reflecting a southward shift of the Arctic Front. Sea surface salinities (SSSs) and sea surface temperatures (SSTs) were obtained by transfer functions using the Modern Analogue Technique. The lowest SSTs of 9ºC (±1.3) and 10ºC (±1.3) were recorded in glacial MIS 16 and MIS 18 respectively. However, these reconstructions are influenced by abundant heterotrophic taxa and may reflect elevated nutrient levels rather than lowered temperatures. Reworked palynomorphs uniquely indicate a Cretaceous as well as Paleozoic provenance for the first Heinrich-like events.

Potential Urinary miRNA Biomarker Candidates for the Accurate Detection of Prostate Cancer among Benign Prostatic Hyperplasia Patients

MicroRNAs (miRNAs) are a class of short (similar to 22nt), single stranded RNA molecules that function as post-transcriptional regulators of gene expression. MiRNAs can regulate a variety of important biological pathways, including: cellular proliferation, differentiation and apoptosis. Profiling of miRNA expression patterns was shown to be more useful than the equivalent mRNA profiles for characterizing poorly differentiated tumours. As such, miRNA expression "signatures" are expected to offer serious potential for diagnosing and prognosing cancers of any provenance. The aim of this study was to investigate the potential of using deregulation of urinary miRNAs in order to detect Prostate Cancer (PCa) among Benign Prostatic Hyperplasia (BPH). To identify the miRNA signatures specific for PCa, miRNA expression profiling of 8 PCa patients, 12 BPH patients and 10 healthy males was carried out using whole genome expression profiling. Differential expression of two individual miRNAs between healthy males and BPH patients was detected and found to possibly target genes related to PCa development and progression. The sensitivity and specificity of miR-1825 for detecting PCa among BPH individuals was found to be 60% and 69%, respectively. Whereas, the sensitivity and specificity of miR-484 were 80% and 19%, respectively. Additionally, the sensitivity and specificity for miR-1825/484 in tandem were 45% and 75%, respectively. The proposed PCa miRNA signatures may therefore be of great value for the accurate diagnosis of PCa and BPH. This exploratory study has identified several possible targets that merit further investigation towards the development and validation of diagnostically useful, non-invasive, urine-based tests that might not only help diagnose PCa but also possibly help differentiate it from BPH.

Forum sur les métadonnées au Canada

Ce rapport résume trois conférences présentées dans le cadre du Forum sur les métadonnées au Canada tenu à Ottawa les 19 et 20 septembre 2003. Organisé par Bibliothèque et Archives Canada, ce forum de deux jours avait pour but de rassembler des participants en provenance de différentes communautés canadiennes de métadonnées afin d'améliorer la recherche d'information grâce aux métadonnées. Les conférences résumées traitent du Métrométa, des FRBR et du cadre de métadonnées du Gouvernement du Canada.