Français 1532

Contient : 1° « Hystoire des glorieuses Maries, filles madame sainte Anne, et de ses.III. maris », par « Frere JEHAN, dis DE VENETTE, nommé FILLOUS » ; 2° « L'Oroison de PIERRE DE NANTES, evesque de Saint Pol de Leon en Bretaigne » ; 3° « Lettres de pardons » de « l'evesque de Paris FOULQUES »

Français 1533

Contient : 1° « La Vie Nostre Dame » ; 2° « Les.XV. Signes du definement du monde » ; 3° « Les Miracles de Nostre Dame », par « GAUTIER DE COINSI » ; Prologue ; Chansons ; « Amors qui set bien enchanter... » ; « Qui que face rotruange ne chançon... » ; « D'esforcier m'esteut ma voiz... » ; « Quant ces floretes florir voi... » ; « Pour conforter mon cuer et mon corage... » ; « Haute pucele pure et monde... » ; Miracles ; « Pour cels esbatre et deporter... » ; « Un archevesque out à Tolete... » ; « A Boorges, ce truis lisant... » ; « Un biau miracle vos recite... » ; « Un miracle truis d'un provoire... » ; « A Chartres fu, ce truis,.I. clers... » ; « Un moines fu d'une abeïe... » ; « Pour plusors cuers plus enflamer... » ; « Un haut miracle mult piteus... » ; « Tuit li miracle Nostre Dame... » ; « Une abeesse fu jadis... » ; « Tenez scilence, bele genz... » ; « Entendez tuit, fetes scilence... » ; « Un brief miracle mult aoigne... » ; « Si con mes livres le tesmoigne... » ; « Un biau miracle vos voil dire... » ; « Mes livres me dit et revele... » ; « En escrit truis qu'en l'abaïe... » ; « A ceus qui aiment doucement... » ; « De la loenge de la Virge... » ; « Ici apres voil metre en brief... » ; « Se pres de moi vos volez traire... » ; « Queque d'oïr estes engrant... » ; « Queque talent aves d'oïr... » ; « En escrit truis que pres d'Oliens... » ; « Entendez tuit, et cler et lai... » ; « Queque volentez me semont... » ; « Un miracle voil reciter... » ; « Pour ce c'oiseuse est mort à l'ame... » ; « Bien est que nos le bien dions... » ; « Il fu, ce truis, uns chevaliers... » ; « Cele en qui prist humanité... » ; « A la gloire la glorieuse... » ; « Qui que devine ne dechaie... » ; « Li seconz livres des Miracles Nostre Dame... » ; Prologue ; Chansons ; « Pour la pucele en chantant me deport... » ; « Mere Dieu, virge senée... » ; « L'amor dont sui espris... » ; « D'une amour coie et ferme chanter voil seriement... » ; « Hui matin à l'ains jornée... » ; « Entendez tuit ensenble et li clerc et li lai... » ; « Hui enfantez fu li Filz Dieu... » ; Miracles ; « A sages dit et fet savoir... » ; « Vos, damoiseles, et vos, dames... » ; « Un miracle trop merveilleus... » ; « Au tens que de la cité noble... » ; « Sainte Escriture nos esclaire... » ; « Assez savez c'assez lo on... » ; « Queque li clerc entr'eus disoient... » ; « Mestre Buisarz et si chanoine... » ; « Le bon borjois qui por sa fame... » ; « Or entendez ça en cest foil... » ; « Tanttruis escrit, foi que doi m'ame... » ; « Qui bons livres velt encerchier... » ; « Conter vos voil sanz nul delai... » ; « La douce mere au criator... » ; « Se Diex m'aït hui et demain... » ; « Ici apres voil remoller... » ; « Ançois que fors del livre issons... » ; « Qui velt oïr vers moi se traie... » ; « Cele qui est de tel maniere... » ; « Mes livres conte et narraz... » ; « Qui velt oïr, qui velt entendre... » ; « A le loenge de la dame... » ; « Vos qui amez de cuer entier... » ; « A Bissance la riche et noble... » ; « Prologue de l'epistre que le prieur envoie à ses amis ; Épilogue ; 4° « Les Avez de Nostre Dame », par le même ; 5° Diverses Oraisons à Notre-Dame, par le même

Français 1768

Contient : 1° « Li Apochalisse » de « saint JEHAN » ; 2° L'« Ymaige dou monde » [par GAUTIER DE METZ] ; 3° « Li Passions Nostre Seignour Jhesu Crist selonc saint MATHEU » ; 4° « Les Paroles que sainz BERNARS disoit en oroison à la douce dame de paradis » ; 5° « Ansoignemanz » du père à son fils ; 6° « C'est l'Omelie de ORIGINES de sainte Marie Magdelaine » ; 7° Vie de Notre-Seigneur Jésus-Christ

Français 2000

Contient : 1° « Le Jeu des eschas moralisé », par « JAQUES DE COSSOLES », traduction par « JEHAN FERRON, de l'ordre des Freres Prescheurs » ; 2° « Le Compte des.LXIIII. poins de l'escequier double... translaté de latin en françois... par ROBERT DU HERLIN »

Français 2464

Contient : 1° La Légende de St Denis ; 2° « La Vie St Eustace » ; 3° La Chronique de TURPIN ; 4° Chronologie des rois de France ; 5° Chronologie tirée de l'Écriture sainte ; 6° Description de la Terre sainte ; 7° La Pénitence d'Adam

Recueil de copies de pièces concernant les finances et le domaine. De 1428 à 1488.

Contient : 1 à 7 Sept ordonnances de CHARLES VII : Saumur, 25 septembre et 25 novembre 1443 ; Nancy, 10 février 1445; Bourges, 26 novembre 1447; Mehun-sur-Yèvre, 23 décembre 1454; Bouchet, près Saint-Pourçain, 30 janvier 1456; Les Roches Tranchelion, 21 avril 1460. De ces ordonnances deux seulement, la seconde et la dernière, ne figurent pas dans le Recueil imprimé ; 8 Procès-verbal d'ordonnance concernant les officiers comptables. 16 février 1460 ; 9 « Instructions... faictes par le conseil du roy [Charles VII], sur les finances que l'en peut raisonnablement demander pour le roy aux gens d'Eglise, pour le temps passé qu'ilz ont tenu possession sans l'assentement du roy ». 1463 ; 10 Ordonnance de « HENRY [VI], roy de France et d'Angleterre », concernant le rachat des rentes constituées sur les maisons de Paris. « Donné à Paris, le derrenier jour de juillet 1428 » ; 11 Table de comptes faits pour les revenus d'une année ; 12 « Ordonnance du feu roy CHARLES VIII sur la deffence de n'acheter le demaine par les officiers du roy... Donné à Paris, le 10... de jung... 1488 »

Geology of the Gander Group, Gander River Ultramafic Belt and Davidsville Group in the Jonathan's Pond - Weir's Pond Area, northeast Newfoundland /

The study area is situated in NE Newfoundland between Gander Lake and the north coast and on the boundary between the Gander and Botwood tectonostratigraphic zones (Williams et al., 1974). The area is underlain by three NE trending units; the Gander Group, the Gander River Ultramafic Belt (the GRUB) and the Davidsville Group. The easternmost Gander Group consists of a thick, psammitic unit composed predominantly of psammitic schist and a thinner, mixed unit of semipelitic and pelitic schist with minor psammite. The mixed unit may stratigraphically overlie the psammitic unit or be a lateral facies equivalent of the latter. No fossils have been recovered from the Gander Group. The GRUB is a terrain of mafic and ultramafic plutonic rocks with minor pillow lava and plagiogranite. It is interpreted to be a dismembered ophiolite in thrust contact with the Gander Group. The westernmost Davidsville Group consists of a basal conglomerate, believed deposited unconformably upon the GRUB from which it was derived, and an upper unit of greywacke and slate, mostly of turbidite origin, with minor limestone and calcareous sandstone. The limestone, which lies near the base of the unit, contains Upper Llanvirn to Lower Llandeilo fossils. The Gander and Davidsville Groups display distinctly different sedimentological , structural and metamorphic histories. The Gander Group consists of quartz-rich, relatively mature sediment. It has suffered three pre-Llanvirn deformations, of which the main deformation, Dp produced a major, NE-N-facing recumbent anticline in the southern part of the study area. Middle greenschist conditions existed from D^ to D- with growth of metamorphic minerals during each dynamic and static phase. In contrast, the mineralogically immature Davidsville Group sediment contains abundant mafic and ultramafic detritus which is absent from the Gander Group. The Davidsville Group displays the effects of a single penetrative deformation with localized D_ and D_ features, all of which can be shown to postdate D_ in the Gander Group. Rotation of the flat Gander S- into a subvertical orientation near the contact with the GRUB and the Davidsville Group is believed to be a Davidsville D^ feature. Regional metamorphism in the Davidsville Group is lower greenschist with a single growth phase, MS . These sedimentological, structural and metamorphic differences between the Gander and Davidsville Groups persist even where the GRUB is absent and the two units are in contact, indicating that the tectonic histories of the Gander and Davidsville Groups are distinctly different. Structural features in the GRUB, locally the result of multiple deformations, may be the result of Gander and/or Davidsville deformations. Metamorphism is in the greenschist facies. Geochemical analyses of the pillow lava suggest that these rocks were formed in a back-arc basin. Mafic intrusives in the Gander Group appear to be the result of magraatism separate from that producing the pillow lava. The Gander Group is interpreted to be a continental rise prism deposited on the eastern margin of the Late Precambrian-Lower Paleozoic lapetus Ocean. The GRUB, oceanic crust possibly formed in a marginal basin to the west, is believed to have been thrust eastward over the Gander Group, deforming the latter, during the pre-Llanvirnian, possibly Precambrian, Ganderian Orogeny. The Middle Ordovician and younger Davidsville Group was derived from, and deposited unconformably on, this deformed terrain. Deformation of the Davidsville Group occurred during the Middle Devonian Acadian Orogeny.

Mermithid (nematoa: mermithidae) infections of black flies (Diptera: Simuliidae) : seasonal variation and developmental characteristics /

Mermithid nematodes (Nematoda: Mermithidae) parasitize larval, pupal and adult black flies (Diptera: Simuliidae), oftentimes resulting in partial or complete host feminization. This study was designed to characterize parasite-host seasonal variation and to estabUsh the developmental life stage at which feminization is initiated. Data indicate that the total adult population of black flies collected from Algonquin Provincial Park throughout the spring of 2004 was comprised of 31.8% female, 67.8% male and 0.4% intersex individuals. Of the total population, 0.6% was infected by mermithid nematodes (69.0% female, 3.5% male and 27.6% intersex). Seasonal infection trends established over a 12-month period revealed that black flies with different life histories host the same mermithid subfamilies, while black flies with similar life histories host mermithids from different subfamilies. If a simuliid species simultaneously hosts two mermithid species, these parasites are from different subfamilies. Molecular mermithid identification revealed two mermithid subfamilies, Me.somermithinae and Gastromermithinae, present in the simuliid hosts. Mermithid colour variation was not found to be a reliable species indicator. The developmental stage at which feminization is initiated was determined by examining gonad morphology and meiotic chromosomal condition. Results indicate that mermithid-infected black flies exhibit feminization prior to larval histoblast formation. Larvae can be morphologically male (testes present) or female (ovaries present), with morphological males exhibiting either male (achiasmate) or female (chiasmate) meiotic chromosomes; morphological females were only genetically female. Additionally, mermithid infection inhibits simuliid gonad development.

Agrarian revolution in Central America : a comparison of Nicaragua and Honduras using Jeffery Paige's theory of Agrarian revolution

ABSTRACT In 1979 Nicaragua, under the Sandinistas, experienced a genuine, socialist, full scale, agrarian revolution. This thesis examines whether Jeffery Paige's theory of agrarian revolutions would have been successful in predicting this revolution and ln predicting non-revolution in the neighboring country of Honduras. The thesis begins by setting Paige's theory in the tradition of radical theories of revolution. It then derives four propositions from Paige's theory which suggest the patterns of export crops, land tenure changes and class configurations which are necessary for an agrarian and socialist revolution. These propositions are tested against evidence from the twentieth century histories of economic, social and political change in Nicaragua and Honduras. The thesis concludes that Paige's theory does help to explain the occurrence of agrarian revolution in Nicaragua and non-revolution in Honduras. A fifth proposition derived from Paige's theory proved less useful in explaining the specific areas within Nicaragua that were most receptive to Sandinista revolutionary activity.

Career paths of educational administrators

Ten superintendents~ 5 male and 5 female~ were randomly selected from a possible 33 males and 9 females in the Niagara and Hamilton regions. The participants were interviewed through a guided interview process coupled with an accounting of their educational and career histories. They were asked to discuss significant aspects of their careers such as the support they had received from families, from mentors and from involvement in networks. The data collected were then analyzed for similarities and differences both within and between the two gender cohorts. Upon analysis, it was found that the female and male administrators possessed differences in their personal backgrounds as well as their career and educational histories. Differences were also found in the perceived role of mentors, and networks. The ways in which the female administrators experienced their careers were found to be quite different from the ways in which the male administrators experienced their careers.

Sinister creativity: a phenomenological exploration of some of the experiences and perceptions of six lefthanded visual artists

Six lefthanded artist-educators were interviewed to attempt to discover any patterns t6 their perceptions and experiences. Artists have their own culture and priorities. According to the literature, lefthanded people appear more likely to suffer from dyslexia, allergies, asthma and other auto-immune diseases as well as machinery and equipment injuries. Patterns emerging suggested that lefthanded people indeed suffer more from dyslexia. More startling was the distinct possibility that many artists have traumatic childhood histories. This would commonly include negative school experiences, and for a significant number sexual assault, perceived or actual abandonment by parents, and/or consistently low selfesteem. The researcher discovered possible reasons why creative people frequently have problems at school, why they tend to be rebellious and anti-establishment oriented, how many of them perceive societal rules, and why they are more likely to be lefthanded. These characteristics all have significant implications for art school administrators.

The utility of sedimentary diatoms as a measure of historical lake ph

As a result of increased acid precipitation, the pH of a large number of Canadian Shield lakes has been falling. Prior to this study there was no documentation available to explain the history of lake acidification for the Algoma area lakes. In order to obtain this information the diatom inferred pH technique was developed in this study. During two field seasons, July 1981 and July 1982, short sediment cores (circa 25-30 cm) were collected from 28 study lakes located north of Lake Superior, District Algoma, Ontario. The surface sediment diatoms (0-1 cm) from each of these lakes were carefully identified, enumerated, and classified in terms of their pH indicator status. The surface sediment diatom analysis indicated that lake pH is one of the most important factors affecting the species composition and relative abundance of diatom populations. Thus diatom assemblages can be sensitive indicators of lake acidification. When Nygaard's index alpha was plotted against observed lake pH, a statistically significant relationship resulted (r=-0.89; p=histories of 4 lakes (lakes X4, CS, U3, and WI). The repeatability of this technique was confirmed by comparing two downcore paleo-pH profiles of Lake WI. These two paleo-pH profiles represented almost identical paleo-pH patterns for Lake WI. The paleo-pH study of Lake X4 revealed that the lake has been rather acidic (pH <5.6) for the last 200 years. It appears that the recent increase in acid precipitation 3 over the last 30 years has not altered the water pH compared to the lake's pH history. However, the paleo-pH study of another acidic lake (Lake CS) indicated that its pH has significantl}* dropped over the last 30 years . During this time the Lake CS pH has dropped almost 2 pH units (7.1 to 5.2). The other two lakes studied for downcore pH were circumneutral in nature . One of these lakes (Lake U3) displayed a relatively stable pH history while the other lake (Lake WI) displayed significant pH fluctuations over post-Ambrosia time. The variable pH history of Lake WI was probably associated with the Algoma sintering plant plume and forest fires. A significant relationship between surface sediment diatoms and observed lake pH and secondly a statistically significant relationship between index alpha and observed pH suggested that diatoms are one of the best indicators of lake pH. Thus diatom inferred pH technique has great potential in explaining the rate of lake acidification.

Vegetational history and geochronology of several sites in South Southwestern Ontario with discussion on mastodon extinction in Southern Ontario /

This study has three purposes: to establish a chronologically controlled vegetational history for a number of sites in south Southwestern Ontario; to utilize the resulting data to support and/or add to the current understanding of Quaternary geology and stratigraphy, and the glacial and postglacial history of the Great Lakes in south Southwestern Ontario; and to attempt to propose a possible explanation for the extinction of the mastodon in Southern Ontario. Palynological and geochronological analyses were conducted on material collected from eleven sites (east to west): Verbeke Mastodon Site, Woloshko Mastodon Site, Walker Pond II, Pond Mills I, Lake Hunger Bog, Bouckaert Site. Mabee Site, Cornell Bog. Colles Lake I, Folden Mastodon Site and Forest Pond. Individual geochronologically controlled (where possible) vegetational histories were reconstructed for each of the sites investigated. The results of the individual studies, when considered in overview. indicated the existance of an established closed boreal forest throughout south Southwestern Ontario by 10,000 years B.P. This evidence for a significant climatic change coincident throughout south Southwestern Ontario supports the proposed age of 10,000 years B.P. for the Pleistocene/Holocene Boundary (Terasmae, 1972). Remnant patches of 'open spruce parkland' persisted in small local 'wet' areas. It was in these areas that the mastodon was restricted during early Holocene time. With continued encroachment by the surrounding boreal forest, possibly speeded up by this browser's destructive feeding habits, the spruce enclaves shrank and the mastodon became extinct in south Southwestern Ontario. The results of this thesis basically support Dreimanis' (1967, 1968) proposed 'Environmental-Climatic' theory for mastodon extinction. It is suggested that increased dryness during the present interglacial compared to the climate of earlier interglacials may be the key to unravelling the problem of mastodon extinction in eastern North America.

Understanding the polyvocality of autism discourse : a critical autoethnographic approach

Currently, much of the autism literature supports the notion that Pervasive Developmental Disorder (PDD) is a deviation from what is considered "normal" and, accordingly, that it is in need of early remediation. This thesis explored alternative constructions of autism and pathology by drawing on theorists from other disciplines, such as cultural studies (Deleuze & Guattari, 1987, 1965, 1972, 1975,1980, 2003), critical psychology (Parker, 1995, 2002, 2005, 2007), disability studies (Danforth,1997, 1999, 2000; Skrtic, 1995, 1996) and anti-psychiatry (Basaglia, 1987). In an attempt to show how our accounts of the world encompass constructions rooted in language and our own histories of thinking about topics that interest us, this research took an autoethnographic approach to understanding autism discourse. Instead of denying the researcher's existence and personal investment in the research, the author attempted to implicate "the self in the research by acknowledging her own assumptions, biases and ideologies about autism discourse and practice. Thus, tensions between the self and other, personal and political become woven into the fabric, creating a personal, subjective, and partial account of the phenomenon. This research was intended to explicate and interrogate some of the taken-for-granted Truths which guide our practices with people with autism. This alternative critical framework focused on understanding autism as a discourse and explored the way these dominant autism constructions function in society. Furthermore, positioning "the self in the research was meant to illustrate the fundamental need for self-reflective practice in the social sciences.

Geochemistry and petrogenesis of the McElroy and Larder Lake assemblages, Abitibi Greenstone Belt, Northeastern Ontario

The McElroy and Larder Lake assemblages, located in the southern Abitibi Greenstone Belt are two late Archean metavolcanic sequences having markedly contrasting physical characteristics arid are separated from one another by a regional fault. An assemblage is an informal term which describes stratified volcanic and/or sedimentary rock units built during a specific time period in a similar depositional or volcanic setting and are commonly bounded by faults, unconformities or intrusions. The petrology and petrogenesis of these assemblages have been investigated to determine if a genetic link exists between the two adjacent assemblages. The McElroy assemblage is homoclinal sequence of evolved massive and pillowed fl.ows, which except for the basal unit represents a progressively fractionated volcanic pile. From the base to the top of the assemblage the lithologies include Fe-tholeiitic, dendritic flows; komatiite basaltic, ultramafic flows; Mg-tholeiitic, leucogabbro; Mg-tholeiitic, massive flows and Fe-tholeiitic, pillowed flows. Massive flows range from coarse grained to aphanitic and are commonly plagioclase glomerophyric. The Larder Lake assemblage consists of komatiitic, Mg-rich and Fe-rich tholeiitic basalts, structurally disrupted by folds and faults. Tholeiitic rocks in the Larder Lake assemblage range from aphanitic to coarse grained massive and pillowed flows. Komatiitic flows contain both spinifex and massive textures. Geochemical variability within both assemblages is attributed to different petrogenetic histories. The lithologies of the McElroy assemblage were derived by partial melting of a primitive mantle source followed by various degrees of crystal fractionation. Partial melting of a primitive mantle source generated the ultramafic flows and possibly other flows in the assemblage. Fractionation of ultramafic flows may have also produced the more evolved McElroy lithologies. The highly evolved, basal, dendritic flow may represent the upper unit 3 of a missing volcanic pile in which continued magmatism generated the remaining McElroy lithologies. Alternatively, the dendritic flows may represent a primary lava derived from a low degree (10-15%) partial melt of a primitive mantle source which was followed by continued partial melting to generate the ultramafic flows. The Larder Lake lithologies were derived by partial melting of a komatiitic source followed by gabbroic fractionation. The tectonic environment for both assemblages is interpreted to be an oceanic arc setting. The McElroy assemblage lavas were generated in a mature back arc setting whereas the Larder Lake lithologies were produced during the early stages of komatiitc crust subduction. This setting is consistent with previous models involving plate tectonic processes for the generation of other metavolcanic assemblages in the Abitibi Greenstone Belt.