Résumé : The slides were taken on collecting trips sponsored by the William L. Bryant Foundation, where books, music and art indigenous to the regions were gathered. The are organized by geographical location.
Devon House was built in 1881 by Jamaica’s first black millionaire George Stiebel. The land was first assigned to Reverend John Zellers by King George II in May 1667 to aid in the Anglican Church’s efforts to spread Christianity on the island. The house’s architectural style is a mix of Jamaican and English Georgian style architecture and is located at the corner of Trafalgar Road and Hope Road, in what later became known as Millionaire’s corner. In 1967, the house was purchased by the Jamaica National Heritage Trust and was later declared a national monument in 1990 after winning the American Express Historic Preservation Award. Devon House is a Jamaica Heritage Site owned by the Jamaican government. Slide labeled Jam. in Kingston Devon House.
Jamaica -- Caribbean region -- Saint Andrew

Droits : All rights to images are held by the respective holding institution. This image is posted publicly for non-profit educational uses, excluding printed publication. For permission to reproduce images and/or for copyright information contact Special Collections & University Archives, University of Central Florida Libraries, Orlando, FL 32816 phone (407) 823-2576, email: speccoll@mail.ucf.edu
CFM1972_01a
Sheet 58:15
http://ufdc.ufl.edu/AA00030138/00001

Éditeur(s) : ECMEA : Etudes Croisées des Mondes Européens et Américains CRILLASH : Centre de Recherches Interdisciplinaires en Lettres, Langues, Arts et Sciences Humaines ECMEA : Etudes Croisées des Mondes Européens et Américains CRILLASH : Centre de Recherches Interdisciplinaires en Lettres, Langues, Arts et Sciences Humaines
Extrait de : "Terres promises, représentations et imaginaires" : colloque, du 25 au 27 novembre 2015. Université des Antilles
Description : La promesse, selon la philosophe britannique J.L. Austin (Quand dire c'est faire, 1962), est un acte de langage qui s'engage et, à travers cet engagement, s'inscrit dans un futur, affirmant ainsi une félicité à venir et non immédiate. La notion de terre promise comporte une nature proleptique qui se projette dans un avenir que l'on veut certain. C'est la promesse d'accéder un jour à une terre, une nation, un pays rêvé. Lors de l'élection présidentielle de Barack Obama en 2008, les Amériques ont eu pour la première fois l'impression d'accéder à cette terre promise, c'est ce qu'on a appelé l'Amérique post-raciale. Un mois après l'investiture d'Obama, Edouard Glissant et Patrick Chamoiseau publiaient L'intraitable beauté du monde (2009), une ode à une créolisation enfin accomplie grâce à Obama. Glissant et Chamoiseau écrivaient alors « M. Barack Obama, nous pensons qu'il a entendu le cri du monde, la voix des peuples et le chant joyeux ou meurtri des pays ». De même, aux États-Unis, les intellectuels ont loué l'avènement de cette Amérique post-raciale qui aurait été nettoyée de son histoire de ségrégation raciale et dont les lois contre la discrimination raciale seraient ainsi devenues obsolètes. Il s'agira dans cette présentation, de penser à l'impossible, c'est-à-dire au lendemain de la terre promise, une terre qui se voulait pourtant toujours à venir et différée. Dans le cadre des événements autour du mouvement Black Lives Matter, les émeutes anti-racistes à Ferguson et à Baltimore qui rappellent le mouvement des droits civils des années 60, il est temps de soulever la question du post-racial en tant que promesse et idylle ; Comment devons-nous interpréter aujourd'hui cette créolisation qui se voulait enfin accomplie ? L'ère post-raciale, est-elle, ou fut elle, vraiment la terre promise des Amériques ?
Siècle(s) traité(s) : 20
Droits : CC-BY-NC-ND - Attribution - Pas d'utilisation commerciale - Pas de modification
Permalien : http://www.manioc.org/fichiers/V16225
V16225
V16225

Extrait de : Santo Domingo : past and present with a glance at Hayti (p.61)
Résumé : Portrait gravé de Sir Francis Drake, né en 1542 à Tavistock (Devon), mort le 28 janvier 1596, corsaire, explorateur et esclavagiste anglais. Il mena notamment un expédition contre les ports de Saint-Domingue et Carthagène.
Siècle(s) traité(s) : 16
Droits : Domaine public
Provenance : Université des Antilles et de la Guyane. Service commun de la documentation
Permalien : http://www.manioc.org/images/HASH015bdb9bb120f3b41f292eec
HASH015bdb9bb120f3b41f292eec

Éditeur(s) : HAL CCSD Cambridge University Press (CUP)
Résumé : We present detailed biostratigraphy based on conodonts and palaeoenvironmental trends deduced from microfacies and conodont abundance through the Famennian (Late Devonian) at Col des Tribes (Montagne Noire, France). The succession is characterized by micritic limestones deposited in settings oscillating between mid to outer ramp. Facies contain poor fauna, widely dominated by nektonic organisms. This section is complete and one of the most conodont-rich for the Famennian of the north Gondwana-related area. The Upper Kellwasser event (Frasnian–Famennian boundary) and the Hangenberg (Devonian–Carboniferous boundary) have been lithologically identified. They are characterized by decimetre-thick black dysoxic to anoxic argillaceous sediments. The Condroz and annulata events, although not materialized by lithological changes, have been positioned due to the precise stratigraphy. The first event occurred during the deposition of condensed ferruginous facies (griotte limestones) and the second event during the deposition of micrites barren of benthic fauna. The combination of information from both facies and conodont biofacies changes allows a general sea-level curve through the entire Famennian for north Gondwana to be proposed for the first time. At Col des Tribes, the general trend is a slight deepening upwards from triangularis to trachytera zones, then a pronounced shallowing-upwards trend from upper trachytera to praesulcata zones. This curve correlates with the well-known reference curve from Euramerica concerning the late Famennian (trachytera to praesulcata Zones). There are some discrepancies in minor cycles which can be explained by tectonical phenomena at the onset of the edification of the Variscan belt in Europe.
ISSN: 0016-7568

hal-01115222
https://hal.archives-ouvertes.fr/hal-01115222
DOI : 10.1017/S0016756813000927

Éditeur(s) : CRILLASH : Centre de Recherches Interdisciplinaires en Lettres, Langues, Arts et Sciences Humaines
Extrait de : "Intercompréhension des langues et des cultures dans la Caraïbe" : séminaire international, les 4 et 5 décembre 2013. Université des Antilles et de la Guyane
Description : Hubert St-Laurent Devonish réagit d'abord sur les réalités linguistiques caribéennes. Il met l'accent sur la lutte existant entre les langues indigènes de la Caraïbe et les langues officielles. Il fait également part du projet de création du concept de langue du territoire.
Siècle(s) traité(s) : 21
Droits : CC-BY-NC-ND - Attribution - Pas d'utilisation commerciale - Pas de modification
Permalien : http://www.manioc.org/fichiers/V14058
V14058

Éditeur(s) : Université des Antilles
Extrait de : "La Guadeloupe au sein de l'organisation des Etats de la Caraïbe orientale : une adhésion pour quoi faire ?" : journées d'étude, le 28 février et le 15 mars 2019. Université des Antilles
Description : La Guadeloupe veut mieux s?ancrer dans son environnement caribéen, avec pour objectif de développer des opportunités économiques, mais aussi la coopération scolaire et universitaire, la coopération dans les domaines de l?agriculture et du transport, de la transition agro-écologique et bio-économie, vers un renforcement des connections maritimes au sein de l?OECO. L?insertion de notre archipel dans notre aire re?gionale est une e?vidence : C?est sans conteste l?un de nos atouts, un atout sur lequel nous devons construire notre place dans le monde.
Siècle(s) traité(s) : 21
Droits : CC-BY-NC-ND - Attribution - Pas d'utilisation commerciale - Pas de modification
Permalien : http://www.manioc.org/fichiers/V19054
V19054

Éditeur(s) : HAL CCSD Société géologique de France
Résumé : International audience
Age constraints on the protoliths, deformation, metamorphism and melting events are key parameters when correlating different continental lithospheric remnants among each other and disentangling their evolution within large-scale orogens. In situ U-Th-Pb chemical dating on monazites using Electron Probe Micro-Analyser (EPMA) has been performed on eight samples throughout the Variscan Maures-Tanneron massif (SE France) in order to date the medium to high-tectonothermal events related to the Variscan orogeny.Results indicate a polyphased crustal evolution : (i) U-Th-Pb ages obtained in polygenetic monazite grain cores gave inherited Upper Ordovician (456 ± 11 Ma) age, highlighting the large scale occurrence of the Ordovician magmatic activity in the North Gondwanian margin. An Early Devonian (404 ± 10 Ma) age may date a protolith emplacement related to calc-alkaline supra-subduction magmatism or could be associated to an early medium-grade metamorphism, prior to collisional stage. (ii) The crustal thickening stage has been further recorded in prograde metamorphic monazites formed during the underthrusting and subsequent nappe stacking events, under amphibolite facies conditions. This stage is dated between 382 ± 11 (Middle Devonian) and 331 ± 5 Ma (Late Visean). (iii) An orogenic partial melting event took place during Middle Carboniferous and is accompanied by the crystallization of crustal peraluminous magmas (Plan-de-la-Tour granite, 329 ± 3 Ma).This contribution demonstrates the capacity of monazite to record the prograde path of rocks during increasing metamorphic conditions related to stages of crustal thickening, and the robustness of the U-Th-Pb chronometer in monazite despite the overprinting of high-grade thermal events, including partial melting. The age ranges of the different orogenic stages reported in this study are in good agreement with those reported in adjacent Variscan Corsica and Sardinia; while correlations with other nearest Variscan massifs like the Argentera massif in the southwestern Alps or the French Massif Central remain more hypothetic. The Internal Zone of the Maures-Tanneron massif, and more widely the Internal Zone of the Maures-Tanneron-Corsica-Sardinia segment, is part of the southern orogenic root system of the Variscan belt.
EISSN: 1777-5817

insu-01140973
https://hal-insu.archives-ouvertes.fr/insu-01140973
DOI : 10.2113/gssgfbull.186.2-3.145

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
Intraplate deformation is most often linked to major stress applied on plate margins. When such intraplate events are accompanied by magmatism, the use of several dating methods integrated within a multidisciplinary approach can bring constraints on the age, nature and source mobilized for generating the magma and in turn on the nature of the intraplate deformation. This study focuses on the large gabbro Arrikine sill (35 km in extension) emplaced within the Silurian sediments of the western margin of the Murzuq cratonic basin in southeastern Algeria. Its emplacement is dated during the early Devonian (415-400 Ma) through the determination of a reliable paleomagnetic pole by comparison with the Gondwana Apparent Polar Wander Path (APWP). This age can be correlated with deep phreatic eruptions before Pragian time thought to be at the origin of sand injections and associated circular structures in Algeria and Libya. For the sill, the K–Ar age of 325.6 ± 7.7 Ma is related to a K-rich aplitic phase that has K-enriched by more than 20% the Devonian gabbro. Laser-ICP-MS U–Pb method dates only inherited zircons mostly at c. 2030 Ma with additional ages at c. 2700 Ma and younger ones in the 766-598 Ma age range. The Arrikine sill is a high-Ti alkaline gabbro having the geochemical composition of a hawaiite akin to several intraplate continental and oceanic provinces, including the contemporaneous Aïr ring complexes province in Niger, but also to the Mauna Loa volcano in Hawaii. This peculiar composition akin to that of the contemporaneous Aïr province is in agreement with a lower Devonian age for the Arrikine sill.The lower Devonian Arrikine sill emplacement is related to a “Caledonian” transtensive reactivation of the western metacratonic boundary of the Murzuq craton. This event also generated in the Saharan platform the so-called “Caledonian unconformity” of regional extension, the Aïr ring complexes and magmatic rocks that produced sand injections. It could be related to rifting of the Hun terranes that occurred at the plate margin to the north (Stampfli and Borel, 2002, Blackey, 2008 and references therein). The mid-Carboniferous (c. 326 Ma) reactivation corresponds to Variscan compression on NW Africa generating aplitic fluids, but also to the major “Hercynian unconformity” of regional extension. The generation of the Arrikine magma is attributed to partial melting through adiabatic pressure release of uprising asthenosphere along tectonically reactivated mega-shear zones, here bordering the relictual Murzuq craton enclosed in the Saharan metacraton.
ISSN: 0899-5362

hal-01306637
https://hal.archives-ouvertes.fr/hal-01306637
DOI : 10.1016/j.jafrearsci.2015.11.019

Éditeur(s) : HAL CCSD Royal Society, The
Résumé : International audience
Since its original description as a chordate, the Late Devonian Scaumenella mesacanthi has been interpreted alternately as a prochordate, a larval ostracoderm and an immature acanthodian. For the past 30 years, these minute specimens were generally considered as decayed acanthodians, most of them belonging to Triazeugacanthus affinis. Among the abundant material of `Scaumenella', we identified a size series of 188 specimens of Triazeugacanthus based on otolith characteristics. Despite taphonomic alteration, we describe proportional growth and progressive appearance of skeletal elements through size increase. Three ontogenetic stages are identified based on squamation extent, ossification completion and allometric growth. We demonstrate that what has been interpreted previously as various degrees of decomposition corresponds to ontogenetic changes.
ISSN: 1744-9561

hal-01545474
https://hal.archives-ouvertes.fr/hal-01545474
DOI : 10.1098/rsbl.2014.0950

Éditeur(s) : HAL CCSD Geological Society of London
Résumé : International audience
The sediments of the Mauges Unit located in the internal zone provide an opportunity of studying the evolution of relief during Palaeozoic time. U-Pb dating on zircon and 39Ar/40Ar on white mica are used to constrain the age and nature of the sources. The first relief identified is marked by an Early Devonian unconformity interpreted as the opening of a northern back-arc basin. Detrital minerals are first reworked from underlying layers indicating a local supply. Magmatic zircons at c. 400 Ma then record the emergence of a magmatic arc. During the Middle Devonian, the gap in the sedimentary record is attributed to an emersion followed by the disappearance of the relief during the Late Devonian. At the Devonian-Carboniferous boundary, the main collision is followed by the onset of a relief. The continental sedimentation in the Ancenis Basin (late Tournaisian-Viséan) is a coarsening-upwards megasequence indicating an increasing and/or approaching relief. The detrital minerals record the progressive exhumation of Variscan metamorphic (mica at c. 350 Ma) and magmatic rocks (zircons at c. 390-340 Ma). The Serpukhovian-Bashkirian sedimentation records the erosion of a proximal metamorphic source (Champtoceaux with micas at c. 350-340 Ma) showing a much shorter drainage system
The Variscan Orogeny: Extent, Timescale and the Formation of the European Crust

ISBN : 978-1-86239-658-6
insu-01016985
https://hal-insu.archives-ouvertes.fr/insu-01016985
DOI : 10.1144/SP405.6

Éditeur(s) : HAL CCSD PeerJ
Résumé : International audience
The study of vertebrate ontogenies has the potential to inform us of shared developmental patterns and processes among organisms. However, fossilised ontogenies of early vertebrates are extremely rare during the Palaeozoic Era. A growth series of the Late Devonian ''acanthodian'' Triazeugacanthus affinis, from the Miguasha Fossil-Fish Lagerstätte, is identified as one of the best known early vertebrate fossilised ontogenies given the exceptional preservation, the large size range, and the abundance of specimens. Morphological, morphometric, histological and chemical data are gathered on a growth series of Triazeugacanthus ranging from 4 to 52 mm in total length. The developmental trajectory of this Devonian ''acanthodian'' is characteristic of fishes showing a direct development with alternating steps and thresholds. Larvae show no squamation but a progressive appearance of cartilaginous neurocranial and vertebral elements, and appendicular elements, whereas juveniles progress in terms of ossification and squamation. The presence of cartilaginous and bony tissues, discriminated on histological and chemical signatures, shows a progressive mineralisation of neurocranial and vertebral elements. Comparison among different body proportions for larvae, juveniles and adults suggest allometric growth in juveniles. Because of the phylogenetic position of ''acanthodians'', Triazeugacanthus ontogeny informs us about deep time developmental conditions in gnathostomes.
ISSN: 2167-8359

Droits : http://creativecommons.org/licenses/by/
hal-01633978
http://hal.upmc.fr/hal-01633978
http://hal.upmc.fr/hal-01633978/document
http://hal.upmc.fr/hal-01633978/file/peerj-3969.pdf
DOI : 10.7717/peerj.3969

Éditeur(s) : HAL CCSD Elsevier Masson
Résumé : In Vietnam, the Triassic Indosinian collision affected coevally the Truong Son belt and the Kontum Massif,which were not independent tectonic units, but parts of the same Gondwana-derived Indochina continental block. This thermotectonic event took place synchronously throughout Vietnam, during the Lower Triassic 250-240-Ma time interval, as demonstrated by numerous geochronological data, combining Ar-Ar and U-Pb dating methods. Structural and kinematic investigations, in the Indosinian metamorphic rocks, reveal that the collisional process resulted from a consistent northwest-striking convergence of Indochina with respect to the adjacent blocks. It is suggested that this motion was taken up by a pair of opposite subduction zones: to the north, beneath South China, and to the west, beneath western Indochina, along the Song Ma and Po Ko sutures, respectively. Tectonic markers, calc-alkaline subduction-related volcanism and granitic intrusions and the generation of high-pressure rocks that have been recently discovered support this geodynamic setting, at least along Po Ko. Along the northwest-trending Song Ma zone, the obliquity of the convergence during subduction and subsequent collision resulted in the development, within the Truong Son Belt, of a set of subparallel dextral mylonitic shear zones, under amphibolite-facies metamorphism. The intermediate segments remained weakly metamorphic or even almost devoid of metamorphism. Along Po Ko, the convergence was near-orthogonal, with a left-lateral strike-slip component; the ongoing continental subduction resulted in the reworking of the Kontum granulitic basement and the development of Indosinian HP granulitic conditions; the subsequent extension-related exhumation operated approximately in the same northwestwards direction. This Indosinian evolution, applied on a continental crust that had been probably affected, as in South China, by a Caledonian-related event, as judged by the general unconformity of the Lower Devonian sediments, the widespread occurrence of magmatic crystallisation ages of ca 450 Ma (Ordovician-Silurian), and by the approximately similar age of the primary granulitic episode in the Kontum Massif. The similarities of the Devonian facies over central, northern Vietnam and South China imply a land connection, possibly as a consequence of a Caledonian collision along Song Ma, but this does not preclude a further oceanic opening and a closure during the Indosinian.
ISSN: 1631-0713

hal-00411591
https://hal.archives-ouvertes.fr/hal-00411591
DOI : 10.1016/j.crte.2007.10.005

Éditeur(s) : HAL CCSD Borntraeger Science Publishers
Résumé : This study characterizes the stratigraphical context as well as the palaeoenvironmental and sealevel trends during the Late Frasnian and Famennian in the Buschteich section (Thuringia, Germany). An integrated approach combines conodont biostratigraphy, chemostratigraphy based on carbon and oxygen isotopes, conodont biofacies analyses and investigations of the morphotypes of foraminifera that occur in the section was applied. Conodonts provided a fine-scale biostratigraphical framework. All the Famennian conodont biozones were identified, with the exception of the three lowest. The Frasnian – Famennian transition was further identified by a positive carbon isotope excursion. This continuous Famennian record is developed in a condensed limestone succession. The reddish Griotte facies, typical of strata of this period, were not documented. Black shales were not developed except for an interval of dark colored mud rocks corresponding to the Hangenberg event at the top of the section. The carbonate succession of Buschteich was deposited in an outer ramp environment, pelagic organisms are the dominant fauna. This is corroborated by the overall dominance of the deep-water conodont genus Palmatolepis. Microfacies, conodont biofacies and foramini fera indicated a deepening trend from the Lower crepida to the Lower rhomboidea Zone, followed by a shallowing trend from the Upper rhomboidea to the praesulcata Zone. This sequence overall matches the sea level reference curve for Euramerica. The timing of maximum water depth at Buschteich, as well as the general sea-level reference record, differs from the Col des Tribes (Montagne Noire, France). Differential uplift or overprinting of the long-term eustatic changes may be the cause of the discrepancy in the local sea-level records.
ISSN: 0078-0421

hal-01623111
https://hal.archives-ouvertes.fr/hal-01623111
DOI : 10.1127/nos/2016/0318

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
The Paleozoic-early Mesozoic geology of Tibet was controlled by the rift-drift, seafloor spreading and subduction zone tectonics of a Paleo-Tethyan realm, which evolved between the West Cathaysides (WC) and the East Cimmerides (EC). Different suture zones with ophiolites and ophiolitic mélanges, high-pressure metamorphic belts, magmatic arcs and accretionary prism complexes separating different terranes mark multiple subduction-accretion systems within this Paleo-Tethyan domain, reminiscent of the modern Western Pacific Ocean. Discrete basins separated by different continental blocks and magmatic arcs constituted a complex paleogeography of Paleo-Tethys, and these oceanic strands were closed as a result of subduction with different polarities during the late Paleozoic-Triassic. The Longmu Tso Shuanghu-Changning Menglian Suture zone (LS-CMS) in Tibet represents the main tectonic boundary between the WC and EC that developed in the Devonian. The East Kunlun-A’nyemaqen oceanic slab was subducted northward beneath the East Kunlun terrane in northern Tibet, whereas the Sumdo oceanic slab was subducted northward beneath the South Qiangtang-North Lhasa terrane in southern Tibet. The Longmu Tso Shuanghu-Changning Menglian and Jinshajiang-Ailaoshan-Song Ma ophiolites were developed and emplaced in subduction-accretion systems with opposite polarities (westward and eastward) beneath the North Qiangtang-Qamdo-Simao-Indochina terrane in central Tibet. The Jinshajiang-Ailaoshan-Song Ma oceanic slab was subducted westward beneath the North Qiangtang-Simao-Indochina terrane along the Jinshajiang and Ailaoshan-Song Ma trenches in a trench-ridge-trench triple junction plate configuration. The Emeishan mantle plume produced a large Permian basaltic terrane, developed on the western passive margin of the South China block. The final closure of the Paleo-Tethyan oceanic branches resulted in continental collisions and development of a vast Indosinian orogenic collage in the latest Triassic-Jurassic.
ISSN: 0743-9547

insu-01119604
https://hal-insu.archives-ouvertes.fr/insu-01119604
https://hal-insu.archives-ouvertes.fr/insu-01119604/document
https://hal-insu.archives-ouvertes.fr/insu-01119604/file/Xu-JAES-2015.pdf
DOI : 10.1016/j.jseaes.2015.01.021

Éditeur(s) : ISTPM
Résumé : The dwindling of the stocks of some marine animals traditionally fished is driving the producers to consider the exploitation of species which were seen as of lesser interest up to now. Among the latter, cephalopods hold a specific position. In the first place, they are not a new resource so to speak, having been eaten in Asian and Mediterranean countries for a long time, and, above all, they've been the object of a growing interest for a few years now. It is encouraging to see that this tendency is very distinct in our country where it can be thought that producers and consumers are now aware of the value of this abounding species. The actions aimed at optimising their exploitation are thus facilitated but they suffer from the imprecision of the statistical data on the fisheries. This data is indeed necessary to evaluate the availability of the stocks and to direct the production through a rational management.
L'amenuisement des stocks de certains animaux marins traditionnellement pêchés amène les producteurs à envisager l'exploitation d'espèces jusqu'à présent considérées comme de moindre intérêt. Parmi ces dernières, les céphalopodes occupent une place particulière. En premier lieu, ils ne constituent pas à proprement parler une ressource nouvelle, ayant de tous temps été consommés dans les pays asiatiques et méditerranéens, et surtout, depuis quelques années, ils suscitent un intérêt croissant dans nombre de pays. II est encourageant de constater que cette tendance est particulièrement nette dans notre pays où tout porte à croire •que producteurs et consommateurs ont pris conscience de la valeur de cette ressource disponible en abondance. Les actions destinées à optimaliser l'exploitation en sont facilitées mais se heurtent à l'imprécision des données statistiques sur les pêcheries. Ces dernières deviennent indispensables si l'on veut évaluer la disponibilité des stocks et orienter la production par une gestion rationnelle. On observe de plus qu'une étendue de plus en plus importante du domaine maritime tombe inévitablement sous le coup de réglementations locales ou internationales qui s'appuient très largement sur les statistiques de pêche. Si nous voulons aider efficacement les producteurs, nous devons disposer de données complètes et objectives. Sans attendre que soit atteint ce degré de précision, nous avons voulu aborder une étape plus élémentaire en réunissant les informations relatives à l'état actuel de l'exploitation des céphalopodes et aux solutions pour la développer. [OCR NON CONTRÔLE]
Science et Pêche (0036-8350) (ISTPM), 1977 , Vol. 265

Droits : Ifremer
http://archimer.ifremer.fr/doc/1977/publication-6666.pdf
http://archimer.ifremer.fr/doc/00000/6666/

Résumé : Shouldn't Earth, the human planet, be called the algae planet? First appearing 3.5 billion years ago, algae have always been objective allies of life and humans. Brought about by algae, oxygen and the ozone layer allowed plant and animal life to develop in oceans and on continents. They offer spawning grounds and feeding grounds for marine fauna....
La Terre, dite planète des hommes, n'est-elle pas en réalité celle des algues? Présentes il y a 3,5 milliards d'années, elles ont toujours été les alliées objectives de la vie et des hommes. Nous leur devons l'oxygène et la couche d'ozone qui ont permis la vie végétale et animale en mer et sur les continents. Elles servent de frayères et de nourriceries à la faune marine. Les algues ont toujours été offertes à l'homme pour sa nourriture et les besoins les plus divers. Algues brunes, vertes, rouges fournissent les substances, alginates, carraghénanes, agars, que l'industrie adapte à des usages innombrables entrant de plus en plus dans la vie moderne, qu'il s'agisse de matériaux courants (textiles, papiers, films, peintures), de toutes sortes d'aliments pour l'homme ou les animaux d'élevage, de médicaments, de produits de beauté,... La transformation des algues est parmi les secteurs les plus performants et les plus innovants de l'industrie moderne. L'avenir est prometteur pour les antibiotiques, antivirus et anticoagulants qu'elles contiennent. / Mais, les peuplements naturels ne suffisent plus à satisfaire cette demande. Il a fallu recourir à la culture des algues. Plus de 530 000 hectares y sont consacrés, 900 000 algoculteurs y travaillent dans 200 000 entreprises familiales, 250 usines conditionnent les produits. L'algoculture est la branche la plus forte de l'aquaculture. Cet ouvrage fait l'inventaire des méthodes utilisées dans le monde, surtout en Extrême-Orient, au moment où l'on passe de la culture toute simple à celle gérée par ordinateur, en un temps où il apparaît de plus en plus que l'algoculture pourrait être une des sources de cette énergie propre dont l'humanité aura immanquablement besoin. Cette synthèse s'adresse non seulement aux scientifiques qui y trouveront un point des connaissances màis à tous ceux, algoculteurs, industriels, aménageurs, écologistes, qui tireront le meilleur parti de cette somme d'expériences. Qui s'intéresse aux algues y trouve un livre de base. [OCR NON CONTRÔLE]

Droits : info:eu-repo/semantics/openAccess
http://archimer.ifremer.fr/doc/1992/rapport-4402.pdf
http://archimer.ifremer.fr/doc/00000/4402/

Éditeur(s) : HAL CCSD Wiley-Blackwell
Résumé : International audience
New petrographic and microstructural observations, mineral equilibria modelling and U/Pb (monazite) geochronological studies were carried out to investigate the relationships between deformation and metamorphism across the Rehamna massif (Moroccan Variscan belt). In this area, typical Barrovian (muscovite to staurolite) zones developed in Cambrian to Carboniferous metasedimentary rocks that are distributed around a dome-like structure. First assemblages are characterized by the presence of locally preserved andalusite, followed by prograde evolution culminating at 6 kbar and 620 °C in the structurally deepest staurolite zone rocks. This Barrovian sequence was subsequently uplifted to supracrustal levels, heterogeneously reworked at greenschist facies conditions, which was followed locally by static growth of andalusite, indicating heating to 2.5–4 kbar and 530–570 °C. The 206Pb/238U monazite age of 298.3 ± 4.1 Ma is interpreted as minimum age of peak metamorphic conditions, whereas the ages of 275.8 ± 1.7 Ma and 277.0 ± 1.1 Ma date decompression and heating at low pressure, in agreement with previous dating of Permian granitoids intruding the Rehamna massif. The prograde metamorphism occurred during thickening and associated horizontal flow in the deeper crust (S1 horizontal schistosity). The horizontally disposed metamorphic zones were subsequently uplifted by a regional scale antiform during ongoing N–S compression. The re-heating of the massif follows late massive E–W shortening, refolding and retrograde shearing of all previous fabrics coevally with regionally important intrusions of Permian granitoids. We argue that metamorphic evolution of the Rehamna massif occurred several hundred kilometres from the convergent plate boundaries in the interior of continental Gondwanan plate. The tectonometamorphic history of the Rehamna massif is put into Palaeozoic plate tectonic perspective and Late Carboniferous reactivation of (Devonian)–Early Carboniferous basins formed during stretching of the north Gondwana margin and formation of the Palaeotethys Ocean. The inherited heat budget of these magma-rich basins plays a role in the preferential location of this intracontinental orogen. It is shown that rapid transition from lithospheric stretching to compression is characterized by specific HT type of Barrovian metamorphism, which markedly differs from similar Barrovian sequences along Palaeozoic plate boundaries reported from Variscan Europe.
ISSN: 0263-4929

hal-01468009
https://hal.archives-ouvertes.fr/hal-01468009
DOI : 10.1111/jmg.12214

Éditeur(s) : HAL CCSD La Garde : Faculté des lettres et sciences humaines - Université de Toulon et du Var
Résumé : International audience
Avec un protagoniste aux origines viles, héros de la marge, les récits picaresques nous invitent à repenser l’héroïcité et à interroger diverses tensions et ruptures, tant du point de vue du fond que de la forme. Devons-nous alors, comme le fait communément la critique, entériner le déterminisme de ces récits et faire fi de leur dimension prospective, utopique, et présenter les pícaros comme des anti-héros dont les échecs successifs confirmeraient l’ordre pré-établi de la société classique espagnole ? En somme, le pícaro est-il une figure de la norme ou une figure de la rupture, de la rupture-brèche ou bien de la rupture-fracture ? Induit-il une transgression ou plutôt une subversion ? Et y parvient-il par le biais du détour ou de manière frontale ? Dans ce conflit idéologique ou « tectonique des idéologies », le cas du Buscón s’individualise par sa double tension.
ISSN: 2263-4746

hal-01325010
https://hal-univ-tln.archives-ouvertes.fr/hal-01325010
DOI : 10.4000/babel.2488

Éditeur(s) : Cnexo
Résumé : Voici un an déjà le dépôt du Programme d'action à Moyen Terme que m'avaient demandé les Ministres, marquait le départ d'une réflexion intense au niveau gouvernemental sur l'océanologie. Témoignage d'un intérêt précieux pour la mise en valeur d'océans à la fois si proches et si lointains par la faiblesse de nos connaissances et de nos moyens d'investigation, cette réflexion a clarifié le cadre dans lequel nous devons travailler. Notre rôle, notre mission en ressortent mieux. Nous ne sommes pas un ensemble de recherche-développement comme les autres parce que nous sommes, parce que vous êtes d'abord au service de quatre missions nationales indissociables qui nous sont confiées: 1. animer, orienter, développer en liaison avec les utilisateurs finaux l'effort de recherche exploratoire national, c'est-à-dire cette recherche de pointe qui doit associer les finalités de connaissance et celles des applications sur des problématiques de portée générale et avec des visées qui peuvent être à relativement long terme; 2. permettre à la communauté scientifique de disposer des meilleurs outils, des meilleurs équipements lourds pour poursuivre un effort dont l'efficacité, la productivité scientifique doivent être accrues fortement en raison de son coût élevé pour la Nation. A cette mission se rattache celle de favoriser le développement des technologies de base utile à la pénétration, à la mesure et à la valorisation du milieu marin lato sensu; 3. être l'outil privilégié de la promotion d'une approche intégrée pluridisciplinaire et intersectorielle de l'effort océanologique; 4. S'assurer du meilleur transfert possible à l'économie des résultats de l'effort public de recherche en le facilitant en cas de besoin, notamment en encourageant l'effort privé et en s'y associant. [OCR NON CONTRÔLE]
La Lettre du Cnexo (Cnexo), 1980-04 , N. 1 , P. 1-6

Droits : Cnexo - Ifremer
http://archimer.ifremer.fr/doc/1980/publication-4776.pdf
http://archimer.ifremer.fr/doc/00000/4776/

Éditeur(s) : HAL CCSD Springer Verlag
Résumé : International audience
For the first time, an albite orthogneiss has been recognised and dated within the HP-LT blueschist facies metabasites and metapelites of the Ile de Groix. It is characterised by a peraluminous composition, high LILE, Th and U contents, MORB-like HREE abundances and moderate Nb and Y values. A U-Pb age of 480.8 ± 4.8 Ma was obtained by LA-ICP-MS dating of zircon and titanite. It is interpreted as the age of the magmatic emplacement during the Early Ordovician. Morphologically different zircon grains yield late Neoproterozoic ages of 546.6-647.4 Ma. Zircon and titanite U-Pb ages indicate that the felsic magmatism from the Ile de Groix is contemporaneous with the acid, pre-orogenic magmatism widely recognised in the internal zones of the Variscan belt, related to the Cambro-Ordovician continental rifting. The magmatic protolith probably inherited a specific chemical composition from a combination of orogenic, back-arc and anorogenic signatures because of partial melting of the Cadomian basement during magma emplacement. Besides, the late Devonian U-Pb age of 366 ± 33 Ma obtained for titanite from a blueschist facies metapelite corresponds to the age of the HP-LT peak metamorphism.
ISSN: 1437-3254

insu-00714570
https://hal-insu.archives-ouvertes.fr/insu-00714570
DOI : 10.1007/s00531-011-0732-5