Structural studies and gabbro mylonitization within the Barton Bay Deformation Zone, Geraldton, Ontario /

Structures related to ductile siMple shear parallel to the Bankf ield-Tonbill Fault, define a 5km wide zone, the Barton Bay Deformation Zone. Structures present within this zone Include; simple shear fabrics S, C and C , asymmetric Z shaped folds with rotated axes, boudinage and pinch and swell structures and a subhorlzontal extension llneation. The most highly deformed rock is a gabbro mylonite which occurs in the fault zone. The deformation of this gabbro has been traced in stages from a protomylonite to an ultramylonite In which feldspar and chlorite grainslze has been reduced from over 100 microns to as little as 5 microns. Evidence from the mylonite and the surrounding structure indicates that deformation within the Barton Bay Deformation Zone is related to a regional simple shear zone, the Bankf ield-Tombill Fault. Movement along this shear zone was in a south over north oblique strike slip fashion with a dextral sense of displacement.

Regional variations of deformation mechanisms in the Lorrain Quartzite near Whitefish Falls, Ontario, Canada /

The quartzite microfabric found in the Lorrain Formation was studied across the La Cloche syncline, along a regional north-south transect along highway 6, near Whitefish Falls, Ontario. The complete stratigraphic sequence across the syncline is preserved, and is present on each fold limb. The lithostratigraphic units with the smallest grains size and lowest mica content are located close to the core of the fold, while coarser grained mica and feldspar rich units are situated at the northern and southern most extent of the transect. Deformation mechanisms vary with lithology and with position across the fold. Pressure solution appears to be the dominant deformation mechanism in the feldspathic, micaceous and ferruginous units. In the finer grained, mica poor white medium grained and cherty sandstone units, grain boundary migration (GBM) characteristics show dominance over those of pressure solution and show high amounts of fracturing which cut migrated boundaries and therefore post date GBM. All samples across the fold display a preferred orientation of quartz c-axes. The senses of asymmetry of fabrics are found to be similar across the syncline, with the exception of the ferruginous sandstone unit. Formation of these similar fabrics synmietries can not be the result of strain related to first order folding. The mica content appears to be related to the percentage of quartz lost due to pressure solution as a result of strain; the more mica present, the less quartz was lost. Calculations based on the shape of initial grains suggest that conservatively 30% of the quartz volume has been dissolved out of the Lorrain quartzite, and potentially migrated hundreds of meters to other members of the Huronian Supergroup as there was no meso or macroscopic evidence observed in outcrop.

Structural analysis of the Paint Lake Deformation Zone, Northern Ontario /

The Paint Lake Deformation Zone (PLDZ), located within the Superior Province of Canada, demarcates a major structural and lithological break between the Onaman-Tashota Terrane to the north and the Beardmore-Geraldton Belt to the south. The PLDZ is an east-west trending lineament, approximately 50 km in length and up to 1 km in width, comprised of an early ductile component termed the Paint Lake Shear Zone and a late brittle component known as the Paint Lake Fault. Structures associated with PLDZ development including S-, C- and C'-fabrics, stretching lineations, slickensides, C-C' intersection lineations, Z-folds and kinkbands indicate that simple shear deformation dominated during a NW-SE compressional event. Movement along the PLDZ was in a dextral sense consisting of an early differential motion with southside- down and a later strike-slip motion. Although the locus of the PLDZ may in part be lithologically controlled, mylonitization which accompanied shear zone development is not dependent on the lithological type. Conglomerate, intermediate and mafic volcanic units exhibit similar mesoscopic and microscopic structures where transected by the PLDZ. Field mapping, supported by thin section analysis, defines five strain domains increasing in intensity of deformation from shear zone boundary to centre. A change in the dominant microstructural deformation mechanism from dislocation creep to diffusion creep is observed with increasing strain during mylonitization. C'-fabric development is temporally associated with this change. A decrease in the angular relationship between C- and C'-fabrics is observed upon attaining maximum strain intensity. Strain profiling of the PLDZ demonstrates the presence of an outer primary strain gradient which exhibits a simple profile and an inner secondary strain gradient which exhibits a more complex profile. Regionally metamorphosed lithologies of lower greenschist facies outside the PLDZ were subjected to retrograde metamorphism during deformation within the PLDZ.

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.

Microstructural and geochemical investigation of North American lower-middle Paleozoic trilobites and recent arthropods

Trilobites ¥tere collected from Ordovician and Devonian formations of Ontario} New York} Ohio} Oklahoma} and Indiana. Diversity was generally low} but 19..?telllS and Ph..~tY>ps ¥tere the most abundant species from the Ordovician and Devonian} respectively. Recent marine arthropods ¥tere collected from the Atlantic shore of the middle Florida Keys} and from the Pacific and lagoonal waters at Cape Beale} B. C. Fresh-water arthropods were collected along the shore of the Severn River in northcentral Ontario. Cuticles ¥tere analyzed for major} minor and trace elements, 180 and 13C isotopes, as ¥tell as examined by scanning electron micr?scope to identify original and diagenetic fabrics. Examination of trilobite cuticles by scanning electron microscope revealed several microstructures consistent with those observed in Recent arthropods. Microstructures} such as setae and tegumental gland duct openings} in like sized Lim/IllS and Isoteline trilobites may indicate common ancestral origins for these organisms, or simply parallel cuticle evolutions. The dendritic microstructure, originally' thought to be a diagenetic indicator, was found in Recent specimens and therefore its presence in trilobites may be suggestive of the delicate nature of diagenesis in trilobites. The absence of other primary microstructures in trilobites may indicate alteration, taxonomic control} or that there is some inherent feature of S EM examination which may' not allow detection of some features} while others are apparently visit·le onl~1 under SH.·1. The region of the cuticle sampled for examination is also a major influence in detecting pristine microstructures, as not all areas of trilobite and Recent arthropod cuticles will have microstructures identifiable in a SEM study. Subtleties in the process of alteration, however} ma~·· leave pristine microstructures in cuticles that are partial~/ silicified or do 10m itized, and degree and type of alteration may vary stratigraphically and longitudinally within a unit. The presence of fused matrices, angular calcite rhombs, and pyrite in the cuticle are thought to be indicative of altered cuticles, although pyritization may not affect the entire cuticle. t-~atural processes in Recent arthropods, such as molting, lead to variations in cuticle chemistries, and are thought to reflect the area of concentration of the elements during calcification. The level of sodium in Recent arthropods was found to be higher than that in trilobites, but highly mobile when sUbjected to the actions of VY'€'athering. Less saline water produced lovy'€'r magnesium and higher calcium values in Recent specimens .. and metal variations in pristine Ordovician trilobite cuticle appears to follow the constraints outlined for Recent arthropods, of regulation due to the chemislry of the surrounding medium. In diagenetic analysis, sodium, strontium and magnesium proved most beneficial in separating altered from least altered trilobites. Using this criterion, specimens from shale show the least amount of geochemical alteration, and have an original mineralogy of 1.7 - 2.4 mole % MgC03 (8000 t(> 9500 ppm magnesium) for both /s>..?/e/11S lJA'i.riff!11S and PseIAit'11J17ites I..itmirpin..itl/~ and 2.8 - 3.3 mole % MgC03 (5000 to 7000 ppm magnesium) for Ph.i{).?PS This is Slightly lower than the mineralogy of Recent marine arthropods (4.43 - 12.1 mole % MgC03), and slightly higher than that of fresh-water crayfish (0.96 - 1.82 mole % MgC03). Geochemically pristine trilobites were also found to possess primary microstructures. Stable isotope values and trends support the assertion that marine-meteoriclburial fluids were responsible for the alteration observed in a number of the trilobite specimens. The results of this stUdy suggest that fossil material has to be evaluated separately along taxonomic and lithological lines to arrive at sensible diagenetic and e nvironmenta I interpretations.

Sedimentology and micromorphology of drumlin sediments at Chimney Bluffs State Park, New York, United States of America

The drumlin sediments at Chimney Bluffs, New York appear to represent a block-inmatrix style glacial melange. This melange comprises sand stringers, lenses and intraclasts juxtaposed in an apparently massive diamicton. Thin section examination of these glacigenic deposits has revealed microstructures indicative of autokinetic subglacial defonnation which are consistent with a deformable bed origin for the diamicton. These features include banding and. necking of matrix grains, oriented plasma fabrics and the formation of pressure shadows at the long axis ends of elongate clasts. Preservation of primary stratification within the sand intraclasts appears to suggest that these features were pre-existing up-ice deposits that were frozen, entrained, then deposited as part of a defonning till layer beneath an advancing ice sheet. Multi-directional micro-shearing within the sand blocks is thought to reflect the frozen nature of the sand units in such a high strain environment. It is also contended that dewatering of the sediment pile leading to the eventual immobilisation of the defonning till layer was responsible for opening sub-horizontal fissures within the diamicton. These features were subsequently infilled with mass flow poorly sorted sands and silts which were subjected to ductile defonnation during the waning stages of an actively deforming till layer. Microstructures indicative of the dewatering processes in the sand units include patches of fine-grained particles within a coarser-grained matrix and the presence of concentrated zones of translocated clays. However, these units were probably confined within an impermeable diamicton casing that prevented massive pore water influxes from the deforming till layer~ Hence, these microstructures probably reflect localised dewatering of the sand intraclasts. A layered subglacial shear zone model is proposed for the various features exhibited by the drumlin sediments. The complexity of these structures is explained in terms of ii superposing deformation styles in response to changing pore water pressures. Constructional glaciotectonics, as implied by the occurrence of sub-horizontal fissuring, is suggested as the mechanism for the stacking of the sand intraclast units within the diamicton. The usefulness of micromorphology in complimenting the traditional sedimentology of glacigenic deposits is emphasised by the current study. An otherwise massive diamicton was shown to contain microstructures indicative of the very high strain rates expected in a complexly deforming till layer. . It is quite obvious from this investigation that the classification of diamictons needs to be re-examined for evidence of microstructures that could lead to the re-interpretation of diamicton forming processes. RESUME Le pacquet de sediments drumlinaire de Chimney Bluffs, New York, represent un "bloc-en-matrice" genre de melange glaciale. Des structures microscopique comprennent l'evidence pour la defonnation intrinseque attribuee a l'origine lit non resistant du drumlin. PreselVation des structures primaires au coeur des blocs arenaces suggere que ceux sont des depots preexistant qui furent geles, entraines et par la suite sedimentes au milieu d'une couche de debris sous-glaciaires en voie de deformation. Des failles microscopiques a l'interieur des blocs arenaces appuient aussi l'idee d'un bloc cohesif (c'est-a-dire gele) au centre d'un till non resistant. Des implications significatives s'emergent de cette etude pour les conditions sous-glaciaire et les processus de la formation des drumlin.

Second Welland Canal - Book 1, Survey Map 11 - St. Catharines and Locks 3 and 4

Survey map of the Second Welland Canal created by the Welland Canal Company showing the Town of St. Catharines. Identified structures associated with the Canal include Lock 3 and its Lock House, Lock 4 and its Lock House, Hydraulic Race, and a floating tow path. The surveyors' measurements and notes can be seen in red and black ink and pencil. Local area landmarks are also identified and include streets and roads (ex. Geneva Street, Ontario Street, St. Paul Street, and Merritville Road), Lincoln Mills and its Store House, T. M. Merritt's Store House, Cooper Shop, L. Shickluna's Dry Dock, Peter McGill's Grist Mill, J. Flint's Saw Factory, T. Hosteter's Gristing Mill, J. Dougan Builder's shop or office, Norris and Nelson Mill, G. N. Oil Foundry and its Machine Shop and Boiler, a barrel shed, woolen factory, Estate of P. Nihen (or T. Nihan), Norris and Nelson's Wharf, the W. C. Office, and structures (possibly houses) or small properties belonging to T. Adams, and A. K. Boomer. Properties and property owners of note are: Concession 6 Lots 16, 17, and 18, Concession 7 Lots 16, 17, and 18, Alva Dittrick, James R. Benson, W. B. Robinson, and C. Phelps.

Elucidation of a mechanism of cell lysis by chorhexidine : a biophysical approach

Chlorhexidine is an effective antiseptic used widely in disinfecting products (hand soap), oral products (mouthwash), and is known to have potential applications in the textile industry. Chlorhexidine has been studied extensively through a biological and biochemical lens, showing evidence that it attacks the semipermeable membrane in bacterial cells. Although extremely lethal to bacterial cells, the present understanding of the exact mode of action of chlorhexidine is incomplete. A biophysical approach has been taken to investigate the potential location of chlorhexidine in the lipid bilayer. Deuterium nuclear magnetic resonance was used to characterize the molecular arrangement of mixed phospholipid/drug formulations. Powder spectra were analyzed using the de-Pake-ing technique, a method capable of extracting both the orientation distribution and the anisotropy distribution functions simultaneously. The results from samples of protonated phospholipids mixed with deuterium-labelled chlorhexidine are compared to those from samples of deuterated phospholipids and protonated chlorhexidine to determine its location in the lipid bilayer. A series of neutron scattering experiments were also conducted to study the biophysical interaction of chlorhexidine with a model phospholipid membrane of DMPC, a common saturated lipid found in bacterial cell membranes. The results found the hexamethylene linker to be located at the depth of the glycerol/phosphate region of the lipid bilayer. As drug concentration was increased in samples, a dramatic decrease in bilayer thickness was observed. Differential scanning calorimetry experiments have revealed a depression of the DMPC bilayer gel-to-lamellar phase transition temperature with an increasing drug concentration. The enthalpy of the transition remained the same for all drug concentrations, indicating a strictly drug/headgroup interaction, thus supporting the proposed location of chlorhexidine. In combination, these results lead to the hypothesis that the drug is folded approximately in half on its hexamethylene linker, with the hydrophobic linker at the depth of the glycerol/phosphate region of the lipid bilayer and the hydrophilic chlorophenyl groups located at the lipid headgroup. This arrangement seems to suggest that the drug molecule acts as a wedge to disrupt the bilayer. In vivo, this should make the cell membrane leaky, which is in agreement with a wide range of bacteriological observations.

James Corbin letter, October 2, 1813

James Corbin (1791-1860) lived in Williamstown, Berkshire County, Massachusetts. He is buried there is Southlawn cemetery. Pliny Moore (1759-1822) was the founder of the town of Champlain, New York. He served in the revolutionary war and after received the Smith and Graves patent, a parcel of land more than 11,000 acres in size. He served in several town offices in Champlain, including postmaster and judge, as well as operating sawmills and textile mills. Letter transcription: Dear Sir, The reason I did not come to tend your mill last spring was because the letter you wrote me dated 1 of March I didn’t receive it until the 12 of April and inform me that if I could be there in 2 or 3 weeks you would employ me as we agreed and therefore I concluded it would not do any good for me to come. It was a great disappointment to me because I was all ready to come whenever I got word. It is impossible for me to come now for I am in partnership with my brother in the farm and Mills and must take care our crops and settle our [bushels] this winter. I know nothing to the contrary but what I can come next spring I will let you know by uncle Corbin this winter. James Corbin

Glacial stratigraphy and micromorphology of the Pine Point Pb-­‐Zn mining district, Northwest Territories

This investigation aims to gain a better understanding of the glacial history of the Pine Point Mining district, Northwest Territories, by examining the sedimentological properties of the glacial sediments including, geochemical analysis, heavy mineral concentrate analysis, clast macro-­‐fabrics, pebble lithologies, and micromorphological investigation. Four till units were identified, and three were associated with identified erosional bedrock features and streamlined landforms in the area, indicating a minimum of three ice flow directions. Sedimentological properties suggest that these units were all Type-­B tectomict/mélange till, emplaced as part of a soft subglacial deformable bed. The lack of ice-­‐marginal advance and retreat sequences within the studied till, suggests the Middle Wisconsinan Laurentide Ice margin was likely north and west of the Pine Point area, as opposed to along the margin of the Canadian Shield and Western Sedimentary Basin where it has been suggested to have existed.

Letter to S.D. Woodruff from George C. Flint and Co.

Letter to S.D. Woodruff from George C. Flint and Co., Upholsterers and Furniture Manufacturers of New York regarding items such as mantle glass, cornices and fabrics. They have enclosed a handwritten price list with this letter (4 pages, handwritten), Sept. 13, 1876.

Crise du secteur manufacturier au Québec : ampleur et nature des restructurations impliquant des licenciements collectifs entre 2003 et 2008

Des données de Statistique Canada montrent que le Québec a perdu 86 700 emplois manufacturiers nets entre 2004 et 2008, ce qui représente un recul de 13,8% (Bernard, 2009). Un dollar canadien fort, la concurrence internationale, les délocalisations de la production et les consolidations globales d'opérations sont souvent mentionnés comme étant les causes des difficultés du secteur manufacturier canadien - principalement concentré au Québec et en Ontario. La crise financière amorcée à l’été 2007, a contribué à aggraver la crise propre au secteur manufacturier dont les origines remontent au début des années 2000 (Weir, 2007; AgirE, 2008; Pilat et al., 2006). Cette recherche examine le processus de restructuration du secteur manufacturier québécois de manière détaillée au niveau des établissements afin d’en évaluer l’ampleur et la nature entre 2003 et 2008. Les données colligées permettent de poser un regard unique et original sur les restructurations ayant impliqué des licenciements collectifs au Québec. Ces données sont issues de deux sources. D'abord, nous avons utilisé une liste d‘entreprises qui ont envoyé un avis de licenciement collectif au Ministère de l’Emploi et de la Solidarité sociale du Québec entre 2003 et 2008. En second lieu, nous avons eu recours aux archives en ligne des médias pour trouver d’autres évènements de restructuration non rapportés par le ministère ainsi que pour obtenir des informations complémentaires sur les évènements déjà compilés dans la liste du ministère. Notre méthodologie de recherche et notre typologie analytique des types de restructuration sont basées sur celles développées par l’European Monitoring Center on Change (EMCC) et reprises dans certaines études comme celles de Bronfenbrenner et Luce (2004) et Hickey et Schenk (soumis). Les résultats, présentés en termes d’événements de restructuration et d’emplois perdus, sont ventilés en fonction de quelques variables (année d’occurrence, taille de l’établissement, sous-secteur d’activité, intensité technologique, région administrative, types de restructuration). Les raisons données par l’entreprise afin de justifier la restructuration ont aussi été colligées. Au cours de la période étudiée, nous avons identifié au total 1 631 évènements de restructurations dans le secteur manufacturier à travers toutes les régions du Québec, qui ont entraîné la perte de 129 383 emplois. Ainsi, 78 246 emplois ont été perdus suite à la réduction des activités de l‘établissement et 51 137 emplois l’ont été suite à la fermeture de leur établissement. La forme la plus fréquente de restructuration est la restructuration interne, suivi par la faillite/fermeture. Les types de restructuration qui ont engendré le plus de pertes d’emplois en moyenne par évènement sont dans l’ordre, la délocalisation, la sous-traitance, la consolidation d’activités ainsi que la fusion-acquisition. L’année 2008 fut celle où il y a eu le plus grand nombre de restructurations. Montréal et la Montérégie sont les régions qui ont le plus été touchées par la restructuration, les pertes d’emplois et les fermetures d’établissements. Les industries à faible intensité technologique ont davantage été frappées par la crise manufacturière. C’est le sous-secteur du papier et du bois qui connu le plus grand nombre d’événements de restructurations. Ce sous-secteur a aussi subi les pertes d’emplois les plus importantes, suivi par le sous-secteur du textile et du vêtement. Ces deux industries se partagent plus de la moitié des fermetures d’établissements. L’insuffisance de la demande (22,1%), la concurrence internationale (14,3%), la hausse de la valeur du dollar canadien (11,2%), la réorganisation interne de l’entreprise (11,1%), la rationalisation des coûts visant une augmentation de la profitabilité (10,1%) ainsi que les difficultés financières (9,9%) sont les motifs principaux donnés par les employeurs. Nos résultats montrent qu’il y a eu deux temps dans l’évolution de la restructuration du secteur manufacturier au Québec. Un premier temps au début de la période où des changements structurels profonds ont été observés dans certaines industries (p.ex. le bois-papier et le textile-vêtement) et un second temps, en fin de période caractérisé par des changements davantage liés à la conjoncture en raison de la crise économique dont les effets commençaient à se faire sentir à ce moment (Institut de la statistique du Québec, 2009a).

Les licenciements collectifs au Québec : portée et efficacité de la règle de droit

Au cours des dernières années, le Québec fut durement touché par des vagues massives de licenciements collectifs. Après l’industrie du textile et du vêtement, c’est maintenant au tour de l’industrie forestière de subir, de plein fouet, les contrecoups d’une économie en pleine mutation. Les résultats des entrevues réalisées au printemps 2008, auprès des travailleurs de la Louisiana-Pacific de Saint-Michel-des-Saints, attestent de l’incapacité des dispositions sur le licenciement collectif à prendre adéquatement en charge les travailleurs victimes de ces fermetures d’usines. Pour évaluer le degré d’efficacité des dispositions sur le licenciement collectif, nous partons d’une étude empirique visant le processus de restructuration d’une grande entreprise papetière, qui conduit à la fermeture de son usine de traitement du bois à St-Michel-des-Saints. Des entretiens conduits auprès des travailleurs, des acteurs locaux comme des dirigeants du syndicat et de la communauté locale, et d’autres acteurs syndicaux et gouvernementaux permettent de reconstruire les étapes conduisant aux licenciements collectifs et à leur suite. Seule la mobilisation syndicale (blocus de l’usine) a permis de bonifier les faibles mesures palliatives prévues initialement par la loi. Cette mobilisation n’a toutefois pas empêché de constater des effets négatifs marqués (appauvrissement, sentiment d’exclusion, tensions familiales, etc.) chez les travailleurs victimes de ce licenciement massif.

Polyamides and polyesters made of bile acids in the main chain

La préparation de polymères à base d’acides biliaires, molécules biologiques, a attiré l'attention des chercheurs en raison des applications potentielles dans les domaines biomédicaux et pharmaceutiques. L’objectif de ce travail est de synthétiser de nouveaux biopolymères dont la chaîne principale est constituée d’unités d’acides biliaires. La polymérisation par étapes a été adoptée dans ce projet afin de préparer les deux principales classes de polymères utilisés en fibres textiles: les polyamides et les polyesters. Des monomères hétéro-fonctionnels à base d’acides biliaires ont été synthétisés et utilisés afin de surmonter le déséquilibre stoechiométrique lors de la polymérisation par étapes. Le dérivé de l’acide lithocholique modifié par une fonction amine et un groupement carboxylique protégé a été polymérisé en masse à températures élevées. Les polyamides obtenus sont très peu solubles dans les solvants organiques. Des polyamides et des polyesters solubles en milieu organique ont pu être obtenus dans des conditions modérées en utilisant l’acide cholique modifié par des groupements azide et alcyne. La polymérisation a été réalisée par cycloaddition azoture-alcyne catalysée par l'intermédiaire du cuivre(Ι) avec deux systèmes catalytiques différents, le bromure de cuivre(I) et le sulfate de cuivre(II). Seul le bromure de cuivre(Ι) s’est avéré être un catalyseur efficace pour le système, permettant la préparation des polymères avec un degré de polymérisation égale à 50 et une distribution monomodale de masse moléculaire (PDI ˂ 1.7). Les polymères synthétisés à base d'acide cholique sont thermiquement stables (307 °C ≤ Td ≤ 372 °C) avec des températures de transition vitreuse élevées (137 °C ≤ Tg ≤ 167 °C) et modules de Young au-dessus de 280 MPa, dépendamment de la nature chimique du lien.

New insights into the substrate specificities of microbial transglutaminase: a biocatalytic perspective

La transglutaminase microbienne (Microbial transglutaminase : MTG) est fortement exploitée dans l’industrie textile et alimentaire afin de modifier l’apparence et la texture de divers produits. Elle catalyse la formation de liaisons iso-peptidiques entre des protéines par l’entremise d’une réaction de transfert d’acyle entre le groupement γ-carboxamide d’une glutamine provenant d’un substrat donneur d’acyle, et le groupement ε-amino d’une lysine provenant d’un substrat accepteur d’acyle. La MTG est tolérante à un large éventail de conditions réactionnelles, ce qui rend propice le développement de cette enzyme en tant que biocatalyseur. Ayant pour but le développement de la MTG en tant qu’alternative plus soutenable à la synthèse d’amides, nous avons étudié la réactivité d’une gamme de substrats donneurs et accepteurs non-naturels. Des composés chimiquement diversifiés, de faible masse moléculaire, ont été testés en tant que substrats accepteurs alternatifs. Il fut démontré que la MTG accepte une large gamme de composés à cet effet. Nous avons démontré, pour la première fois, que des acides aminés non-ramifiés et courts, tels la glycine, peuvent servir de substrat accepteur. Les α-acides aminés estérifiés Thr, Ser, Cys et Trp, mais pas Ile, sont également réactifs. En étendant la recherche à des composés non-naturels, il fut observé qu’un cycle aromatique est bénéfique pour la réactivité, bien que les substituants réduisent l’activité. Fait notable, des amines de faible masse moléculaire, portant les groupements de forte densité électronique azidure ou alcyne, sont très réactives. La MTG catalyse donc efficacement la modification de peptides qui pourront ensuite être modifiés ou marqués par la chimie ‘click’. Ainsi, la MTG accepte une variété de substrats accepteurs naturels et non-naturels, élargissant la portée de modification des peptides contenant la glutamine. Afin de sonder le potentiel biocatalytique de la MTG par rapport aux substrats donneurs, des analogues plus petits du peptide modèle Z-Gln-Gly furent testés; aucun n’a réagi. Nous avons toutefois démontré, pour la première fois, la faible réactivité d’esters en tant que substrats donneurs de la MTG. L’éventuelle amélioration de cette réactivité permettrait de faire de la MTG un biocatalyseur plus général pour la synthèse d’amides. Mots clés: Lien amide, biocatalyse, biotransformation, transglutaminase, arrimage moléculaire, criblage de substrats, ingénierie de substrats.