Éditeur(s) : HAL CCSD Oxford University Press (OUP)
Résumé : International audience
STUDY QUESTION: Is there evidence at the population level of associations between different male genital disorders, outside Scandinavian countries? SUMMARY ANSWER: At an international scale, there is evidence for a number of correlations between rates of four male reproductive disorders (hypospadias, cryptorchidism, testicular cancer and low sperm concentration). WHAT IS KNOWN ALREADY: Some associations between these outcomes have been shown in studies focusing on individuals and mainly in Nordic European countries. These associations, together with histological evidence of a dysgenesis pattern in testicular tissue specimens, have generated the concept of the existence of a 'testicular dysgenesis syndrome' originating in utero. STUDY DESIGN, SIZE, DURATION: This is a geographical correlation study using cancer, malformations rates and sperm quality data collected between the years 1998 and 2005. PARTICIPANTS/MATERIALS, SETTING, METHODS: Incidence rates of testicular cancer were extracted from International Agency for Research on Cancer registries and Globocan, while cryptorchidism and hypospadias prevalence rates were obtained from EUROCAT and International Clearinghouse for Birth Defects Surveillance and Research registries. Sperm concentration data were extracted from recent studies using standardized methodology. A total of 39 registries and 9 sperm studies were selected. Non-parametric Spearman correlation tests were used to test the association between these four disorders. Correlations were computed for all registries together, for registries with high-quality matching coverage only and by continents. Sensitivity analyses were also conducted using data from prospective clinical studies to take into account potential bias related mainly to ascertainment of malformation rates. MAIN RESULTS AND THE ROLE OF CHANCE: We found positive correlations between testicular cancer and hypospadias (r = 0.32, P = 0.05) and between hypospadias and cryptorchidism (r = 0.70, P = 0.008). Stronger correlations were observed when using registries with high-quality matching coverage. Among these registries, differences between Europe and the rest of the world appeared (the positive correlation between testicular cancer and cryptorchidism was stronger outside Europe, r = 0.83, P = 0.01 compared with 0.40, P = 0.60 for European registries). A negative correlation between testicular cancer and sperm concentration was observed (r = -0.88, P = 0.002). These correlations support our initial hypothesis but remain only suggestive due to the intrinsic limitations in the study design (i.e. geographical correlation study) and do not allow causal inference. LIMITATIONS, REASONS FOR CAUTION: Differences in the ascertainment of malformations rates (definition, length of follow-up) make the international comparison difficult. The small number of registries for some conditions (cryptorchidism) or of studies (for sperm quality) and the absence of information about major risk factors such as ethnicity and socioeconomic status in the registries are also limitations. WIDER IMPLICATIONS OF THE FINDINGS: Our findings are in agreement with results of studies focusing on individuals and suggest that shared risk factors are present in the populations studied.
ISSN: 0268-1161

inserm-00863412
http://www.hal.inserm.fr/inserm-00863412
DOI : 10.1093/humrep/det111
PUBMED : 23670171

Résumé : Le rapport "Production d'énergie à partir de la houle" comme créneau possible de développement pour les houlomotrices, les sites isolés où l'énergie est chère, situés dans des zones où la houle est, sinon très importante, du moins assez régulière. Les îles situées au milieu des océans, loin des continents ont, en général, des marées d'amplitude assez faible, ce qui est un élément favorable. Nous avons donc recherché, parmi les DOM/TOM, quels seraient les sites à priori favorables à l 'implantation de houlomotrices. Nous avons éliminé à priori les TAAF en raison de leur environnement trop hostile, Saint-Pierre et Miquelon, dont la ressource houle doit être faible et irrégulière vu leurs positions. Tous les DOM/TOM que nous avons examinés sont donc situés à des latitudes où soufflent les alizés. [OCR NON CONTRÔLE]

Droits : 1981 CNEXO -COB
http://archimer.ifremer.fr/doc/00001/11263/7809.pdf
http://archimer.ifremer.fr/doc/00001/11263/

Éditeur(s) : HAL CCSD Vuibert
Résumé : Depuis l'origine des temps géologiques, la surface de la Terre est en perpétuel bouleversement. Après les avoir fait apparaître, la tectonique des plaques promène les continents d'un bout à l'autre de la Terre dans une danse qui ne doit rien au hasard. Tremblements de Terre, éruptions volcaniques, tsunamis... les manifestations les plus visibles des colères actuelles de la Terre font peur. Toutes sont dues à la dynamique du manteau de la Terre dont les couches les plus profondes sont continuellement brassées avec les plus superficielles. Dans l'histoire de la Terre, les lents mouvements du manteau terrestre ont quelquefois été pris dans des événements d'avalanches catastrophiques qui ont successivement créé et détruit les supercontinents. Les conséquences de ces événements se mesurent à l'échelle de la planète entière qu'ils ont modelée de manière irréversible par des phénomènes volcaniques et tectoniques dont l'ampleur n'a rien a voir avec ceux que nous connaissons aujourd'hui.
https://hal.archives-ouvertes.fr/hal-00525570

hal-00525570
https://hal.archives-ouvertes.fr/hal-00525570

Éditeur(s) : HAL CCSD Elsevier Masson
Résumé : National audience
Les leishmanioses sont des maladies parasitaires à transmission vectorielle observées sur tous les continents, à l’exception de l’Amérique du Nord et de l’Australie. Nous focaliserons ici sur la leishmaniose viscérale méditerranéenne due à Leishmania infantum et dont l’incidence annuelle est estimée entre 1200 et 2000 cas. Son cycle biologique est zoonotique avec un réservoir animal essentiellement canin. Les récentes observations épidémiologiques sont rapportées ici, notamment la mise en évidence du portage humain asymptomatique et l’extension de la zone endémique de la leishmaniose canine. La prise en charge thérapeutique de la leishmaniose viscérale méditerranéenne du patient immunocompétent fait essentiellement appel à l’amphotéricine B liposomale. Le débat existe toujours sur la pertinence d’une prophylaxie secondaire ou des traitements itératifs à chaque rechute chez le patient co-infecté par le VIH. Summary Leishmaniasis are protozoan infections transmitted by the bite of the sandflies, widely reported except in North-America and Australia. Here, we focus on mediterranean visceral leishmaniasis due to Leishmania infantum, with an estimated annual incidence of 1200–2000 cases. Its biological cycle is zoonotic and mainly involves the canine reservoir. The recent epidemiological observations are reported here, particularly the asymptomatic carriage but also the extension of the canine enzooty. Regarding treatment of immunocompetent patients, the drug of choice for mediterranean visceral leishmaniasis is liposomal amphotericin B. In case of HIV-Leishmania co-infection, the interest of secondary prophylaxis is still in debate
ISSN: 2210-6545

hal-01225489
https://hal-univ-rennes1.archives-ouvertes.fr/hal-01225489
https://hal-univ-rennes1.archives-ouvertes.fr/hal-01225489/document
https://hal-univ-rennes1.archives-ouvertes.fr/hal-01225489/file/Mise%20au%20point%20et%20actualit%C3%A9s%20sur%20la%20leishmaniose%20visc%C3%A9rale%20m%C3%A9diterran%C3%A9enne.pdf
DOI : 10.1016/j.antinf.2014.12.005

Éditeur(s) : HAL CCSD American Society for Microbiology
Résumé : International audience
Human leishmaniasis are widely spread diseases with different clinical forms caused by about 20 species within the Leishmania genus. Leishmania species identification is relevant for therapeutic management and prognosis, especially for cutaneous and muco-cutaneous forms. Several methods are available to identify Leishmania species from culture, but they have not been standardized for the majority of the currently described species, with the exception of MultiLocus Enzyme Electrophoresis. Moreover, these techniques are expensive, time-consuming and not available in all laboratories. Within the last decade, mass spectrometry (MS) has been adapted for microorganism identification, including Leishmania However, no commercial reference mass spectral database is available. In this study, a reference mass spectral library (MSL) for Leishmania isolates, accessible through a free web-based application (mass spectral identification, MSI), was constructed and tested. It includes mass spectral data for 33 different Leishmania species, including species that infect humans, animals and phlebotomine vectors. Four laboratories on two continents evaluated MSI performance using 268 samples of which 231 were Leishmania strains. All Leishmania strains, but one, were correctly identified at least at the complex level. A risk of species misidentification within the L. donovani, L. guyanensis and L. braziliensis complexes was observed, as already reported with other techniques. The tested application was reliable, with identification results comparable to those obtained with reference methods, but with a more favorable cost-efficiency ratio. This free online identification system relies on a scalable database and can be implemented directly in the user's computers.
ISSN: 0095-1137

hal-01571305
https://hal.archives-ouvertes.fr/hal-01571305
DOI : 10.1128/JCM.00845-17
PUBMED : 28724559

Éditeur(s) : HAL CCSD
Résumé : International audience
Understanding subduction rheology in both space and time has been a challenge since the advent of plate tectonics.We herein focus on "subduction infancy", which corresponds to the first 0-2 My immediately following subductionnucleation, when a newly born slab penetrates into the overriding plate mantle and heats up.The only remnants of this critical, yet elusive, geodynamic step are thin metamorphic soles, commonly found beneathpristine, 100-1000 km long portions of oceanic lithosphere emplaced on top of continents (i.e. ophiolites).In this study, we show how, during subduction infancy, transient mechanical properties of both the mantle and crustacross the subduction plate interface (during 100s ky) control and hinder the penetration of tectonic plates intothe mantle, and how this results in strong peaks of resistance and even slicing of their surface — leaving behindthin, chopped-off metamorphic slivers (i.e. metamorphic soles).These findings constrain the mechanical behaviour of the subduction plate interface (with implications for couplingprocesses and earthquake generation) as well as the properties of the crust and mantle. They also highlight the roleof fluids in enabling subduction to overcome this early resistance.
Geophysical Research Abstracts
Vienne, Austria

insu-01309386
https://hal-insu.archives-ouvertes.fr/insu-01309386

Éditeur(s) : Elsevier Science Bv
Résumé : The timing, routing and processes of sediment transfer from the continents to the oceans at millennial time-scale are still largely unknown. The potential of turbidite systems (dominantly deposited during sea-level lowstands) to record global or regional environmental fluctuations is usually under-exploited because of the difficulty to obtain robust chronostratigraphic constraints in turbiditic deposits, and therefore to tie changes in sedimentary processes to environmental fluctuations. We were able to obtain a millennial-scale chronostratigraphy based on oxygen isotopes of the scarce foraminifera preserved in turbiditic deposits of the Rhone Turbidite System within the Western Mediterranean. Our results show that 1) objective criteria can be defined for the selection of foraminifera preserved within the pelagic intervals between the turbiditic sequences, in order to obtain a reliable isotope stratigraphy; 2) Turbidites triggered by hyperpycnal currents are described for the first time within the Rhone Turbidite System. They are related to the periods of direct fluvial connection with the canyon head (during the sea-level lowstand and early rise), and to a period of high sediment flux in relation with the massive recession of the Rhone glaciers in the Alps; 3) The lithofacies change passing from hyperpycnal to “Bouma-type” is dated at ca 19 cal. ka BP, which might correspond to an acceleration of sea-level rise (19-ka Meltwater Pulse,).
Sedimentary Geology (0037-0738) (Elsevier Science Bv), 2015-06 , Vol. 323 , P. 148-166

Droits : 2015 Elsevier B.V. All rights reserved.
http://archimer.ifremer.fr/doc/00266/37712/35730.pdf
DOI:10.1016/j.sedgeo.2015.04.009
http://archimer.ifremer.fr/doc/00266/37712/

Éditeur(s) : HAL CCSD
Résumé : International audience
Understanding subduction rheology in both space and time has been a challenge since the advent of plate tectonics. We herein focus on "subduction infancy", that is the first ~1-5 My immediately following subduction nucleation, when a newly born slab penetrates into the upper plate mantle and heats up. The only remnants of this critical yet elusive geodynamic step are thin metamorphic soles, commonly found beneath pristine, 100-1000 km long portions of oceanic lithosphere emplaced on continents (i.e., ophiolites).Through the (i) worldwide compilation of pressure-temperature conditions of metamorphic sole formation augmented by pseudosection thermodynamic modeling, (ii) calculations of the viscosity of materials along the plate interface and (iii) generic numerical thermal models, we provide a conceptual model of dynamic plate interface processes during subduction infancy (and initiation s.l.).We show in particular how major rheological switches across the subduction interface control slab penetration, and the formation of metamorphic soles. Due to the downward progression of hydration and weakening of the mantle wedge with cooling, the lower plate (basalt, sediment) and the upper plate (mantle wedge) rheologies equalize and switch over a restricted temperature-time-depth interval (e.g., at ~800°C and ~1 GPa, during 0.1-2 My, for high-temperature metamorphic sole formation). These switches result in episodes of maximum interplate mechanical coupling, thereby slicing the top of the slab and welding pieces (basalt, sediment) to the base of the mantle wedge. Similar mechanical processes likely apply for the later, deeper accretion and exhumation of high-temperature oceanic eclogites in serpentinite mélanges, or for the accretion of larger tectonic slices.This model provides constraints on the effective rheologies of the crust and mantle and general understanding, at both rock and plate scale, for accretion processes and early slab dynamics.
AGU Fall Meeting 2015
San Francisco, United States

insu-01242103
https://hal-insu.archives-ouvertes.fr/insu-01242103

Éditeur(s) : HAL CCSD Société géologique de France
Résumé : International audience
New geodynamical data from West Africa bring consistent informations on the pre-Mesozoic reconstruction within a large area running from the western Sahara to the Colombian cordillera. These new data support a Neoproterozoic Ocean (WANO) between the Amazonian (AMC) and West African (WAC) cratons previously to the Iapetus and Rheic oceans. We delineate 31 blocs detached from the surrounding three continents: NAC (North American Craton), AMC and WAC. 7 came from the WAC margin, 7 from the NAC, 6 from the AMC and 11 from an intermediate volcano sedimentary domain (COB) built on a 1200-1000 Ma oceanic crust. These imbricated blocks formed a tight mosaic by the Hercynian/Alleghanian tectonic event which gave way to the Pangea super-continent. But, during the Atlantic Ocean opening these blocks began to move. They were separated by new oceanic basins. However, previously to the Pangea, blocks from the COB domain formed two sets of garlands located on the northwestern Gondwana margin. The northern one moved to the North until the Silurian to collide the NAC (Taconic tectonic event) meanwhile the southern one remains on the Gondwana margin. All together were gathered by the Carboniferous/Permian time. Then, the framework for the opening of the Atlantic Ocean was not totally disconnected from the "Variscan" collage and many variscan weakness zones were re-used as initial breaking zones. Beyond this tectonic impact, the pre-mesozoic assemblage allows us to compare this "Caribbean" island arc with another one: the Indonesian "Banda" arc. Thus, West Africa is a geological key area for correlations between the Caribbean, the Appalachian, the Brazilian "Nordeste" and the West European domains and for the understanding of the Atlantic Ocean opening process.
EISSN: 1777-5817

hal-00842747
https://hal.archives-ouvertes.fr/hal-00842747
DOI : 10.2113/gssgfbull.184.1-2.5

Résumé : Les marges continentales passives représentent la zone de transition entre le plateau continental et les domaines océaniques profonds. Elles sont typiquement caractérisées par d'épais bassins sédimentaires où les produits détritiques des continents s'accumulent et subissent une longue histoire d'enfouissement et de mouvements verticaux (subsidence/surrection). Dans ces bassins reposent de vastes ressources naturelles (surtout les hydrocarbures) et ils ont ainsi un grand intérêt économique.

Droits : 2008 Ifremer
http://archimer.ifremer.fr/doc/00034/14510/11843.pdf
http://archimer.ifremer.fr/doc/00034/14510/

Éditeur(s) : HAL CCSD
Résumé : International audience
Seismic anisotropy is a ubiquitous feature of the subcontinental mantle. This can be inferred both from direct seismic observations of shear wave splitting from teleseismic shear waves, as well as the petrofabric analyses of mantle nodules from kimberlite pipes. The anisotropy is principally due to the strain-induced lattice preferred orientation (LPO) of olivine. The combined use of these mantle samples, deformation experiments on olivine, and numerical modeling of LPO, provides a critical framework for making inferences about mantle deformation from observed seismic anisotropy. In most cases there is a close correspondence between mantle deformation derived from seismic observations of anisotropy, and crustal deformation, from the Archean to the present. This implies that the mantle plays a major, if not dominant role in continental deformation. No clear evidence is found for a continental asthenospheric decoupling zone, suggesting that continents are probably coupled to general mantle circulation.
Mantle Petrology: Field Observations and high Pressure experimentations: a Tribute to Francis R. (Joe) Boyd

hal-01391514
http://hal.univ-reunion.fr/hal-01391514
http://hal.univ-reunion.fr/hal-01391514/document
http://hal.univ-reunion.fr/hal-01391514/file/Silver_et_al_BoydVolume 1999_hal.pdf

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
The interseismic velocity field provided by geodetic methods is generally interpreted in the framework of a thick elastic lithosphere with a slipping fault at depth. Because lateral variations of lithospheric rheology play a key role in determining the geological strain distribution, I examine the idea that interseismic strain rate variations also occur in response to lateral variations in the elastic thickness of the lithosphere. Using a stress balance principle and some simplifying assumptions, I show using a 1D model that elastic thickness is inversely proportional to strain rate for the simple case of pure strike-slip faulting. Elastic thickness computed on three profiles crossing the San Andreas fault system (SAFS) suggests that the distribution of interseismic strain rate is compatible with a thick elastic lithosphere in the Great Basin-Sierra Nevada province and on the Pacific plate. Conversely, a thin plate with a shallow asthenosphere is needed on the SAFS to explain its high strain rate. A 2.5D Finite Element model of interseismic strain in the Carrizo Plain region in Central California shows how known vertical and horizontal variations of elastic properties refine 1D model predictions. In a case of a multiple fault system, I point out that the interseismic velocity is not causally tied to faults slip rate. Therefore, analysing the velocity field across the SAFS cannot reliably provide faults slip rate distribution as previously claimed. Rather, the apparent correlation between geologic slip rate and interseismic strain may only indicate that the elastic thickness plays a dominant role in controlling fault strength. Finally, I suggest that interseismic geodetic strain could be a new way to infer effective elastic plate thickness on the continents.
ISSN: 0012-821X

hal-00412155
https://hal.archives-ouvertes.fr/hal-00412155
DOI : 10.1016/j.epsl.2008.01.046

Éditeur(s) : Université de Bretagne Occidentale
Résumé : Le plateau des Açores est une région volcanique située à 38°N-30°W dans l'océan Atlantique nord. Il se trouve à une profondeur d'eau moyenne comprise entre 1000 et 2000 mètres et se caractérise par la présence de 8 îles volcaniques, d'une dizaine de petits segments de dorsale et par une activité hydrothermale. Il constitue une triple limite de plaque entre l'Amérique, l'Europe et l'Afrique. L'éloignement des continents et sa localisation dans le gyre subtropical en font, vis à vis de l'Atlantique nord, une région à faibles apports terrigènes et biogènes. Il se situe également au sud de limite d'extension du front polaire (42°N) lors des époques glaciaires, et n'est pas soumis à la forte variabilité climatique de l'Atlantique nord.

Droits : UBO
http://archimer.ifremer.fr/doc/00034/14505/11847.pdf
http://archimer.ifremer.fr/doc/00034/14505/

Éditeur(s) : HAL CCSD Wiley-Blackwell
Résumé : The Oman-Emirates is the largest and best-exposed ophiolite; consequently, it has attracted significant interest among scientists, together with serious conflicts. Most geologists regard this ophiolite as having formed in an intra-oceanic subduction zone before being accreted to the Arabian continent. Here, we propose an alternative scenario, supported by detailed field observations and integrated geophysics. The smaller Emirates part of the ophiolite was forced into a nearby continent, in the pre-collision stage of Tethyan closure. The contraction led to the exhumation of the mantle floor of segmented basins accreted in a rifted system similar to the present-day Gulf of California. The implied high temperature–high pressure metamorphism and the range of geochemical signatures were introduced during the process of rifting, whereas the larger Oman ophiolite was emplaced by obduction onto and along the subducting continental shore. This Ridge–Trench–Transform system might call for a new process to obduct over continents in particular Tethyan ophiolites.
ISSN: 0954-4879

hal-01526919
https://hal.archives-ouvertes.fr/hal-01526919
DOI : 10.1111/ter.12256

Résumé : Three species of man.-rove oysters, Crassostrea rhizophorae, C. brasiliana, and C. gasar, have been described along the Atlantic shores of South America and Africa. Because the distribution of these molluscs is of great biological and commercial interest, their taxonomy and distribution deserve further clarification. Therefore, 15 populations were sampled from both continents. Their 16S mitochondrial polymorphism was studied by sequencing and PCR-RFLP analysis. Two haplotypes were identified. Haplotype a was the only one observed in Africa, but it was also observed in South America together with haplotype b. Because C. gasar is the only mangrove oyster identified on the west coast of Africa, haplotype a was attributed to this species, which has thus been shown to occur in South America. Haplotype b is attributed to C. rhizophorae. The karyotypes of specimens of C. gasar, from Africa and from South America, were very similar, and both species were observed at the same location in Brazil. The occurrence of C. gasar in South America adds a third species-in addition to C rhizophorae and C. brasiliana-to the list of species present along these coasts. The predominant surface circulation patterns in this part of the Atlantic Ocean favor the hypothesis that C. gasar was transported from Africa to America. Finally, a phylogenetic tree built with seven 16S sequences from Crassostrea and Saccostrea species showed that C. gasar is intermediate between the American Crassostrea species (C virginica and C. rhizophorae) and the Asian species (C. gigas and C ariakensis).
Biological Bulletin (0006-3185), 2002-06 , Vol. 202 , N. 3 , P. 232-242

Droits : Marine Biological Laboratory.
http://archimer.ifremer.fr/doc/2002/publication-2790.pdf
http://archimer.ifremer.fr/doc/00000/2790/

Éditeur(s) : The American Asscoiation of Petroleum Geologists
Résumé : A plate tectonic model of the early opening of the south atlantic is used to des cibe the structural framework of the continental margins and adjacent oceanic and coastal areas on both sides of the ocean. It is proposed that major offsets of the continental margins necessarily induce the subsidence of coastal basins where fracture zones intersect the continents. The configuration of the accreting plate-margin boundary gradually developed throughout the opening of the ocean after Late Jurassic time. [NOT CONTROLLED OCR]
The American Asscoiation of Petroleum Geologists Bulletin (The American Asscoiation of Petroleum Geologists), 1972 , Vol. 56 , N. 6 , P. 991-1007

Droits : The American Asscoiation of Petroleum Geologists
http://archimer.ifremer.fr/doc/1972/publication-5033.pdf
http://archimer.ifremer.fr/doc/00000/5033/

Éditeur(s) : HAL CCSD Springer Verlag/EDP Sciences
Résumé : Key messageWe review the recent findings on the influence of drought on tree mortality, growth or ecosystem functioning in tropical rainforests. Drought plays a major role in shaping tropical rainforests and the response mechanisms are highly diverse and complex. The numerous gaps identified here require the international scientific community to combine efforts in order to conduct comprehensive studies in tropical rainforests on the three continents. These results are essential to simulate the future of these ecosystems under diverse climate scenarios and to predict the future of the global earth carbon balance.[br/]ContextTropical rainforest ecosystems are characterized by high annual rainfall. Nevertheless, rainfall regularly fluctuates during the year and seasonal soil droughts do occur. Over the past decades, a number of extreme droughts have hit tropical rainforests, not only in Amazonia but also in Asia and Africa. The influence of drought events on tree mortality and growth or on ecosystem functioning (carbon and water fluxes) in tropical rainforest ecosystems has been studied intensively, but the response mechanisms are complex.[br/]AimsHerein, we review the recent findings related to the response of tropical forest ecosystems to seasonal and extreme droughts and the current knowledge about the future of these ecosystems.[br/]ResultsThis review emphasizes the progress made over recent years and the importance of the studies conducted under extreme drought conditions or in through-fall exclusion experiments in understanding the response of these ecosystems. It also points to the great diversity and complexity of the response of tropical rainforest ecosystems to drought.[br/]ConclusionThe numerous gaps identified here require the international scientific community to combine efforts in order to conduct comprehensive studies in tropical forest regions. These results are essential to simulate the future of these ecosystems under diverse climate scenarios and to predict the future of the global earth carbon balance.
ISSN: 1286-4560

hal-01269438
https://hal.archives-ouvertes.fr/hal-01269438
DOI : 10.1007/s13595-015-0522-5
PRODINRA : 338568

Éditeur(s) : HAL CCSD
Résumé : International audience
È in un clima di contestazione che il presidente Chirac ha celebrato il 10 maggio 2006-data dell'approvazione della legge Taubira- la Giornata della memoria delle vittime della schiavitù, con il pieno consenso del " Comitato per la difesa della memoria degli schiavi " che, istituito il 5 gennaio 2004, sostiene la necessità di promuovere anche nelle scuole le conoscenze sulla tratta, la schiavitù e la sua abolizione, per farle uscire da una sostanziale " amnesia ". Le recenti polemiche francesi intorno alla storia della schiavitù e al suo riconoscimento come crimine contro l'umanità hanno nei fatti rivelato l'esistenza di un malessere, sia storico che sociale. L'esito controverso di questi dibattiti dimostra l'insufficienza delle conoscenze su questo fenomeno e le difficoltà, ancora oggi, di riflettere " serenamente " su tre secoli di storia, di analizzare la complessità del fenomeno e le sue ripercussioni nei diversi continenti (Africa, Europa, America e Asia) e nella società francese.
Passato e Presente

hal-01673495
https://hal.univ-antilles.fr/hal-01673495
https://hal.univ-antilles.fr/hal-01673495/document
https://hal.univ-antilles.fr/hal-01673495/file/Storia%2C%20memoria%20e%20politica.pdf

Éditeur(s) : Elsevier
Résumé : The combined use of Lu-Hf and Sm-Nd isotope systems potentially offers a unique perspective for investigating continental erosion, but little is known about whether, and to what extent, the Hf-Nd isotope composition of sediments is related to silicate weathering intensity. In this study, Hf and Nd elemental and isotope data are reported for marine muds, leached Fe-oxide fractions and zircon-rich turbidite sands collected off the Congo River mouth, and from other parts of the SE Atlantic Ocean. All studied samples from the Congo fan (muds, Fe-hydroxides, sands) exhibit indistinguishable Nd isotopic composition (epsilon(Nd)similar to - 16), indicating that Fe-hydroxides leached from these sediments correspond to continental oxides precipitated within the Congo basin. In marked contrast, Hf isotope compositions for the same samples exhibit significant variations. Leached Fe-hydroxide fractions are characterized by epsilon(Hf) values (from -1.1 to +13) far more radiogenic than associated sediments (from -7.1 to -12.0) and turbidite sands (from -27.2 to -31.6). epsilon(Hf) values for Congo fan sediments correlate very well with Al/K (i.e. a well-known index for the intensity of chemical weathering in Central Africa). Taken together, these results indicate that (1) silicate weathering on continents leads to erosion products having very distinctive Hf isotope signatures, and (2) a direct relationship exists between epsilon(Hf) of secondary clay minerals and chemical weathering intensity. These results combined with data from the literature have global implications for understanding the Hf-Nd isotope variability in marine precipitates and sediments. Leached Fe-hydroxides from Congo fan sediments plot remarkably well on an extension of the 'seawater array' (i.e. the correlation defined by deep-sea Fe-Mn precipitates), providing additional support to the suggestion that the ocean Hf budget is dominated by continental inputs. Fine-grained sediments define a diffuse trend, between that for igneous rocks and the,seawater array', which we refer to as the 'zircon-free sediment array' (epsilon(Hf)=0-91 epsilon(Nd)+3.10). Finally, we show that the Hf-Nd arrays for seawater, unweathered igneous rocks, zircon-free and zircon-bearing sediments (epsilon(Hf)= 1.80 epsilon(Nd)+2.35) can all be reconciled, using Monte Carlo simulations, with a simple weathering model of the continental crust. (C) 2008 Elsevier B.V. All rights reserved.
Earth and Planetary Science Letters (0012-821X) (Elsevier), 2009 , Vol. 277 , N. 3-4 , P. 318-326

Droits : 2009 Elsevier B.V. All rights reserved.
http://archimer.ifremer.fr/doc/2009/publication-6451.pdf
DOI:10.1016/j.epsl.2008.10.028
http://archimer.ifremer.fr/doc/00000/6451/

Éditeur(s) : Douay : François Fabri
Résumé : "Titre dans un encadrement gravé - La 1ère partie correspondant aux Indes occidentales est la traduction de "Descriptionis Ptolemaicae augmentum" de Wytfliet. - La 2e partie est de G.A. Magini Première édition en français, après l'édition originale en latin de 1597. - Approbation du 24 octobre 1604. - Dédicace à Philippe de Caverel. - Reliure parchemin souple, 17e siècle. - Ex dono manuscrit au titre : "Ex dono dom. Praesidis Barbot". - Cachet de l'Académie de Bordeaux. - Cachet de la bibliothèque de la Ville de Bordeaux Burden 102. - Koeman III, 219. - Phillips 4459. Liste complète des cartes : Utriusque Hemispherii Delineato. - Chica sive Patagonica et Australis Terra 1597. - Chili Provincia Amplissima. - Plata Americae Provincia. - Brasilia. - Peruani Regni Descriptio, 1597. - Castilia Aurifera cum Vicinis Provinciis. - Residuum Continentis cum Adiadentibus Insulis Hispaniola Insula. - Cuba Insula et Jamaica. - Iucatana Regio et Fondura. - Hispania Nova. - Granata Nova et California. - Limes Occidentis Quivira et Anian 1597. - Conibas Regio cum Vicinis Gentibus. - Florida et Apalche. - Norumbega et Virginia 1597. - Nova France et Canada 1597. - Estotilandia et Laboratoris Terra India Orientalis. - Japaniae Regnum. - Chinae Regnum. - Insulae Philippinae"
Siècle(s) traité(s) : 16
Droits : Domaine public
Provenance : Ville de Bordeaux. Bibliothèque municipale
Permalien : http://www.manioc.org/patrimon/BBX17003
BBX17003