Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
A subject of continuing debate is how the Earth's lithospheric portion of the upper mantle has remained the thickest (> 200 km) and oldest (> 3 Gy) beneath cratons and is yet surrounded by a vigorously convecting asthenosphere. It is generally admitted that water is a key parameter in the strength and longevity of cratonic roots, because olivine, the main phase of the lithospheric mantle, becomes stronger if its water content decreases. Expanding upon the work presented in Novella et al. (2015) and Taylor et al. (2016), we report new water contents for additional olivine inclusions in diamonds together with the trace-element composition for all olivine inclusions, as well as for mantle xenoliths from various kimberlite pipes located on the Siberian craton. The olivine diamond inclusions from this study have systematically low-water contents (< 50 ppmw H2O), moderate to high forsterite (e.g., Fo91–94) contents and low Ni, Co, and Zn ppm contents (e.g., < 2848, < 108, and < 47 ppm, respectively). In contrast, olivines from Siberian craton mantle xenoliths have a wide range of water contents (6–323 ppmw H2O) and extend to lower-Fo (91–92), Ni, Co, and Zn-rich compositions, compared to the diamond inclusions. Depleted incompatible trace-element concentrations in olivine (0.1–0.001 × Primitive Mantle) advance our hypothesis for the protogenetic origins for the majority of Siberian diamond inclusions. These observations are consistent with the peridotite xenoliths as representing a part of the cratonic lithosphere that has experienced melt re-fertilization, which has also transported water. The olivine diamond inclusions, on the other hand, preserve “micro-samples” of an initial, dry cratonic lithosphere, mostly resulting from melting events. These inclusions are likely sourced from the initial cratonic mantle lithosphere, which thereby, resisted delamination over time, due to its buoyancy and strength, imparted from melt and water depletion, respectively. And thus, our data provides a major argument that the kimberlite-hosted mantle xenoliths may be more metasomatized than common rocks at the base of the Siberian and other cratonic roots away from kimberlite fields.
ISSN: 0024-4937

hal-01467731
https://hal.archives-ouvertes.fr/hal-01467731
DOI : 10.1016/j.lithos.2016.07.023

Éditeur(s) : Université des Antilles Études caribéennes
Résumé : This paper will analyze the tourism image the municipal and state tourism offices of Guanajuato, Mexico, a World Heritage site, aim to project through their promotional materials: a small, colonial city, whose streets are shown as empty, cobble-stoned, and set in romantic light. The "city of Cervantes in the Americas" (a title bestowed by UNESCO in 2005 to honor the theatrical tradition of Cervantes plays in Guanajuato) appears to want to set forth an image of tranquility and spaciousness, while the reality is much different: Guanajuato's mainly narrow and windy streets typically bustle, plazas and gardens are full of activity, in short, the town is alive, yet its projected image lacks liveliness. Furthermore, although it is a World Heritage site, Guanajuato has thus far not used that brand to its advantage; instead, Guanajuato has recently had a variety of slogans to promote itself, seemingly at the whim of officials. Through interviews with tourism officials and a selection of collected tourism materials, I show how the city has yet to establish a “coherent” brand, and is going through various phases of place marketing at once.
Cette étude analyse l'image touristique et le projet touristique des municipalités et des offices de tourisme de l'État de Guanajuato, au Mexique. La «ville de Cervantès dans les Amériques" (un titre décerné par l'UNESCO en 2005 pour honorer la tradition théâtrale de Cervantès joue dans Guanajuato) semble vouloir assoir une image de tranquillité et d'espace, alors que la réalité est bien différente: l’image projetée de la ville de Guanajuato est loin de refléter la vie animée des places et jardins, des ruelles étroites coloniales. Force est de constater que la ville n’a pas encore su tirer profit de sa reconnaissance en tant que site du patrimoine mondial. Les slogans évoluent au gré des fonctionnaires qui organisent en charge de ce secteur. Par le biais d'entrevues avec des fonctionnaires du tourisme et une sélection de matériaux recueillis tourisme, l’auteure montre comment la ville passe par différentes phases marketing sans avoir établie une image cohérente de la destination.
Guanajuato
Mexique

Droits : info:eu-repo/semantics/openAccess
urn:doi:10.4000/etudescaribeennes.3882
http://journals.openedition.org/etudescaribeennes/3882

Résumé : This book represents a two year study by a team of French biologists to collect, summarise and present the experience and knowledge gained in the rearing of the giant freshwater prawn, not only in the French overseas territories but also in the main countries which are developing this culture. This document comprises four parts : - The first describes the world market. The prawn rearing is already an economic reality in the tropical world, the United States and in Europe. - The second on shows that, although the culture techniques are quite complex, production systems can be adapted to local conditions and markets. - The third part is a practical guide, both for investors and farmers, giving all necessary data to start-up and monitor a project in the best conditions. - The final part summarises the main elements of the biology of this species, in order that people interested in its development may have a better understanding of its life history. The authors were based at the aquaculture laboratory of the Ifremer station of French Guiana from 1989 to 1990 and had 15 years previous experience of this culture in Tahiti and the Caribbean. Regarding this initial complete French synthesis on this species in a special care has been given to balance accurate scientific reporting with the objective of reaching a wider audience.
Quinze années d'expérience sur l'élevage de la crevette d'eau douce tropicale, à Tahiti, aux Antilles et en Guyane, comme dans les principaux pays qui pratiquent cet élevage, sont rassemblées et synthétisées dans cet ouvrage. - Où en est le marché mondial ? Cet élevage est déjà une réalité économique dans le monde tropical, comme sur les marchés américain ou européen. - L'exploitation du cheptel est complexe, mais des schémas de production peuvent être adaptés aux conditions locales d'élevage et de marché. - Ce guide pratique donne toutes les informations nécessaires pour monter un projet et le mettre en oeuvre dans de bonnes conditions. - Pour élever la crevette, il faut mieux la connaître. On trouve ici les éléments essentiels de la biologie de cette espèce. L'ouvrage a été rédigé par l'équipe du laboratoire d'aquaculture de la station Ifremer de Guyane en 1989 et 1990. Ce guide, première synthèse en langue française, est unique en son genre. Il équilibre rigueur scientifique et esprit de vulgarisation pour s'adresser aussi bien aux scientifiques et techniciens qu'aux éleveurs ou aux décideurs du développement.

Droits : info:eu-repo/semantics/openAccess
http://archimer.ifremer.fr/doc/1991/rapport-639.pdf
http://archimer.ifremer.fr/doc/00000/639/

Éditeur(s) : Université des Antilles Études caribéennes
Résumé : La Patagonie a longtemps été considérée comme une Terra Australis res Nillius : les terres du sud sans maître. Depuis la Conquista espagnole cet espace a été l’objet de nombreuses utopies, collectives, celles des découvreurs, des militaires et des missionnaires, et individuelles, celles des marchands et des aventuriers et sportifs, avides de richesses et de gloires. Vers la fin des années 1980, une nouvelle idéalisation de la nature, le wilderness, fait de la Patagonie un « must » à découvrir puis à sauvegarder, face à la pression des usages industriels, agricoles, miniers, forestiers, hydroélectriques, et halieutiques. L’utopie éco-philanthropique du milliardaire étasunien Douglas Tompkins puise ses origines dans une expédition au Fitzroy en 1968, mais s’inscrit dans une tradition nord-américaine du xixe siècle. Convaincu de l’impérieuse nécessité de sauvegarder la biodiversité sud-américaine, il propose une Nouvelle Économie, basée sur les principes de la Deep Ecology. Il achète des terres pour « la valeur de la beauté et de l’harmonie » et façonne ses parcs pour « le bien de l’humanité » (Tompkins, 2012).Par une approche biogéographique, cet article montre comment un parcours individuel a instauré un nouvel imaginaire, culturel et touristique. Une œuvre dessine une nouvelle géographie, esthétique, utopique et individualiste qui fait débat, au-delà des enjeux territoriaux et politiques liés à la conservation et à la création de parcs privés. Écrits, films et affiches en faveur de l’écologie et contre l’industrialisation et la technologie changent le regard des acteurs sur ces terres de confins. Les activistes verts et acteurs écotouristiques louent son apport aux luttes socio-environnementales. Le monde rural, les entrepreneurs et les défenseurs de l’esprit des pionniers, défricheurs de terres vierges, critiquent son opposition au développement et son manque de respect pour leur mode de vie. Mais ils vendent leurs terres aux riches occidentaux et chiliens, qui veulent posséder leurs propres parcs du bout du monde et espèrent que le tourisme leur assurera leur futur.
Patagonia has long been considered a Terra Australis res Nillius: the lands of the south with no master. Since the Spanish Conquista this space has been the object of many collective utopias, those of discoverers, soldiers and missionaries, and individual ones, those of merchants and adventurers and sportsmen, eager for wealth and glory. Towards the end of the 1980’s a new idealization of nature, the wilderness, changed Patagonia into a “must” to discover and then to safeguard against the pressure of industrial, agricultural, mining, forestry, hydroelectric, and fisheries exploitation. The eco-philanthropic utopia of the American millionaire Douglas Tompkins finds draws its origins from an expedition to Mount Fitzroy in 1968 but is part of a North American tradition of the nineteenth century. Convinced of the imperious need to safeguard South American biodiversity, he proposes the “Next Economy”, based on the Deep Ecology ideals. He buys land for “the value of beauty and harmony” and shapes his parks for “the good of humanity” (Tompkins, 2012).Through a biogeographic approach, this article shows how an individual project has created a new imaginary, both cultural and touristic. The work of an artist defines a new geography, aesthetic, utopian and individualistic, that questions us, beyond the territorial and political issues associated with the conservation and creation of private parks. Books, films and graphic works in favor of ecology and against industrialization and technology, change views actors have on these remote lands. Eco activists and ecotourism actors praise his contribution to tackle socio-environmental issues. The rural world, entrepreneurs and defenders of the spirit of the pioneers, clearers of virgin lands, criticize his opposition to development and lack of respect for their way of life. Nevertheless they sell their land to rich westerners and Chileans who want to posses their own private parks at world’s end while hopping that tourism will ensure their future.
La Patagonia ha sido considerada por mucho tiempo como una Terra Australis res Nillius : las tierras austral de nadie. Desde la Conquista española este espacio ha sido objeto de numerosas utopías, colectivas e individuales, las de los descubridores, de los militares, misioneros, mercantes, aventureros y deportistas, en búsqueda de riquezas y glorias. Hacia el final de los años 80, una nueva idealización de la naturaleza, el wilderness, transforma la Patagonia en un lugar para conocer y preservar de las codicias industriales, agrícolas, mineras, forestales, hidroeléctricas o pesqueras. La utopía eco-filantrópica del millonario norte americano Douglas Tompkins nace en una expedición al Cerro Fitzroy en 1968, pero se enmarca en una tradición de los Estados Unidos del siglo xix. Convencido de la necesidad de salvaguardar la biodiversidad sur americana, el propone una Nueva Economia, basada en los principios de la Ecología Profunda. Compra tierras por el valor de su belleza y harmonía y planea sus parques por el bien de la humanidad.A través de una metodología llamada biogeográfica, esta comunicación muestra como un proceso personal ha instalado un nuevo imaginario cultural y turístico. Una obra moldea una nueva geografía, estética, utópica y personal, que genera debates, mas allá de los desafíos territoriales y políticos que conllevan la conservación y creación de parques privados. Escritos, películas y afiches a favor de la ecología y en contra de la industrialización y la tecnologización de la sociedad, cambian la mirada de los actores locales de estas zonas australes. Los activistas verdes y los emprendedores eco-turísticos alaban su contribución en las luchas socio-ambientales. El mundo rural, empresarios y defensores del espíritu de los colonos, critican sur oposición al desarrollo y su falta de afinidad con sus modos de vida. Pero ellos venden sus tierras a los ricos norte americanos, europeos y chilenos, deseosos de poseer sus propios parques del fin del mundo, esperando, sin embargo, que el turismo les asegure su futuro.
Patagonie

Droits : info:eu-repo/semantics/openAccess
urn:doi:10.4000/etudescaribeennes.11150
http://journals.openedition.org/etudescaribeennes/11150

Éditeur(s) : HAL CCSD Elsevier
Résumé : The Erro-Tobbio peridotites (Voltri Massif, Ligurian Alps) represent subcontinental lithospheric mantle tectonically exhumed during Permo-Mesozoic extension of the Europe-Adria lithosphere. Previous studies have shown that exhumation started during Permian times, and occurred along kilometer-scale lithospheric shear zones which enhanced progressive deformation and recrystallization from spinel- to plagioclase-facies conditions. Ongoing field and petrologic investigations have revealed that the peridotites experienced, during uplift, a composite history of diffuse melt migration and multiple episodes of ultramafic-mafic intrusions. In this paper we present the results of field, structural and petrologic-geochemical investigations into a sector of the Erro-Tobbio peridotite unit that preserves well this multiple intrusion history. Melt impregnation in the peridotites is evidenced by significant plagioclase enrichment and crystallization of unstrained orthopyroxene replacing kinked mantle olivine and clinopyroxene; impregnating melts were thus opx-saturated. Melt-rock interaction caused chemical changes in mantle minerals (e.g. Al decrease and REE increase in cpx; Ti and Cr# enrichment in spinel). Nevertheless, clinopyroxenes still exhibit LREE depletion (Ce;N;/Sm;N; = 0.006-0.011), indicating a depleted signature for the percolating melts. Melt impregnation was thus related to diffuse porous flow migration of depleted MORB-type melt fractions that modified their compositions towards opx saturation by mantle-melt interaction during ascent. The impregnated peridotites are intruded by a hectometer-scale stratified cumulate body, mostly consisting of troctolites and plagioclase wehrlites, showing gradational, interfingered contacts with the host mantle rocks. Subsequent intrusion events are revealed by the occurrence of olivine gabbros as decameter-wide lenses, variably thick (centimeter- to meter-scale) dykes and thin dykelets, which crosscut both the peridotite foliation and the magmatic layering in the cumulates. Overall, major and trace element compositions of minerals in the intrusives indicate that they represent variably differentiated cumulus products crystallized from rather primitive N-MORB-type aggregated melts. Slightly more evolved compositions are shown by olivine gabbros, relative to the troctolites and plagioclase wehrlites of the cumulate body. Mineral chemistry features (e.g. the Fo-An correlation and high Na, Ti, Mg# in cpx) indicate that the studied intrusive rocks crystallized at moderate pressure conditions (3-5 kbar, i.e. 9-15 km depth). Our study thus points to a progressive transition from porous flow melt migration to emplacement of magmas in fractures, presumably related to progressive change of lithospheric mantle rheology during extension-related uplift and cooling.
ISSN: 0024-4937

hal-00407669
https://hal.archives-ouvertes.fr/hal-00407669
DOI : 10.1016/j.lithos.2006.06.014

Éditeur(s) : American Geophysical Union
Résumé : Microwave Sea Surface Salinity (SSS) measurements can be performed by isolating the emissivity response to salinity changes from numerous geophysical effects, including surface temperature and wind waves. At L-band frequencies (1 to 2 GHz), the sensitivity to SSS is sufficient but it falls off quickly as frequency is increased. Nevertheless, methods using higher microwave frequencies with much lower SSS sensitivity than at L band, can already be tested. In particular, combining 6 and 10 GHz data in vertical polarization efficiently minimizes sea surface roughness and thermal impacts. Using AMSR-E data, the retrieved bi-monthly maps of SSS at 0.5 degrees resolution over the region of the Amazon plume show relative accuracy in-line with the future L-band dedicated mission objectives. Citation: Reul, N., S. Saux-Picart, B. Chapron, D. Vandemark, J. Tournadre, and J. Salisbury (2009), Demonstration of ocean surface salinity microwave measurements from space using AMSR-E data over the Amazon plume, Geophys. Res. Lett., 36, L13607, doi:10.1029/2009GL038860.
Geophysical Research Letters ( GRL ) (0094-8276) (American Geophysical Union), 2009-07 , Vol. 36 , P. 1-5

Droits : 2009. American Geophysical Union. All Rights Reserved
http://archimer.ifremer.fr/doc/2009/publication-6620.pdf
DOI:10.1029/2009GL038860
http://archimer.ifremer.fr/doc/00000/6620/

Résumé : Les objectifs de développement de systèmes de culture durables imposent aux acteurs du développement rural une reconception de ces systèmes. Les méthodes de conception actuelles conduisent souvent les chercheurs à être seuls concepteurs alors que parallèlement l'appropriation des innovations dépend fortement de l'implication des autres acteurs. En réponse, des approches participatives sont de plus en plus fréquentes pour pallier à cette difficulté d'appropriation. La méthode développée dans cette thèse -nommée DISCS pour 're-Design and assessment of Innovative Sustainable Cropping Systems' - met en oeuvre un processus de reconception des systèmes de culture par une approche participative tout en développant des outils d'évaluation multicritère. La méthode DISCS s'inscrit dans la lignée de la méthodologie du prototypage mais se différencie par une démarche itérative à trois échelles d'étude (parcelle, exploitation et territoire) afin de s'assurer que les innovations répondent bien aux attentes des acteurs. A chaque étape du processus une évaluation est réalisée à l'aide d'un jeu d'indicateurs. DISCS a été testée sur le système de culture agrumicole en Guadeloupe dans un but de réduire l'utilisation des pesticides. Cinq prototypes de gestion de l'enherbement ont été conçus collectivement puis testés selon les principes d'une approche systémique. Dans cette thèse, nous présentons les premières étapes de reconception du système agrumicole guadeloupéen basée sur la méthode DISCS. Notre travail nous permet de recommander des techniques de gestion de l'enherbement en jeunes vergers d'agrumes répondant aux contraintes actuelles de développement de systèmes de culture durable.
Re-designing sustainable cropping systems has become a major challenge for agricultural researchers and farmers. In most designing methods, researchers are the main, or sometimes the only designers. However, more and more attempts for involving different kinds of stakeholders in participatory approaches have been accounted for. The new method described in this thesis (DISCS for 're-Design and assessment of Innovative Sustainable Cropping Systems') implements a participatory re-designing process. Though founded on the common structure of prototyping methods, this five-step-method differs first by implementing three progress loops, at experimental field, farm then regional scale. Besides, an ongoing progress dynamic is set between research at the experimental station and crop management in farms, in order to ensure that innovative techniques actually match the farmers' expectations. Assessment at each step is performed using a scale-specific set of indicators. The DISCS method was tested on citrus production in Guadeloupe, to develop lower-pesticide sustainable cropping systems. Five weed management prototypes were collectively designed then tested at an experimental station based on the principles of a systematic approach. In this thesis, we present the first stages of citrus cropping system redesigning based on DISCS method. Our work enables us to recommend sustainable weed management techniques for young orchards that correspond to the current constraints facing orchards in Guadeloupe

http://www.theses.fr/2011AGUY0449/document

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
Most of the plate boundaries are activated obliquely with respect to the direction of far field stresses, as roughly only 8% of the plate boundaries total length shows a very low obliquity (ranging from 0 to 10°, sub-orthogonal to the plate displacement). The obliquity along plate boundaries is controlled by (i) lateral rheological variations within the lithosphere and (ii) consistency with the global plate circuit. Indeed, plate tectonics and magmatism drive rheological changes within the lithosphere and consequently influence strain localization. Geodynamical evolution controls large-scale mantle convection and plate formation, consumption, and re-organization, thus triggering plate kinematics variations, and the adjustment and re-orientation of far field stresses. These geological processes may thus result in plate boundaries that are not perpendicular but oblique to the direction of far field stresses. This paper reviews the global patterns of obliquity along plate boundaries. Using GPlate, we provide a statistical analysis of present-day obliquity along plate boundaries. Within this framework, by comparing natural examples and geological models, we discuss deformation patterns and kinematics recorded along oblique plate boundaries.
ISSN: 0040-1951

hal-01467188
https://hal.archives-ouvertes.fr/hal-01467188
DOI : 10.1016/j.tecto.2016.05.033

Éditeur(s) : Institut océanographie
Résumé : The aim of this paper is to present in a practical fashion the status of the use of remote sensing for the study of coral reef environments through the analysis of work published in the years 1980-2000. We review the scales of the potential work and of that actually conducted, the principal applications and their limiting factors. We detail these limitations which are of a technological nature (spatial and spectral resolution of sensors), as well as often of a conceptual (role of remote sensing in the study) or methodological (image processing) nature. The understanding of these limitations, in relation to the reality of the field, allows identification of work which could be undertaken in the years 2000.
Cet article présente, de façon pragmatique, le bilan de l’usage de la télédétection pour l’étude des milieux coralliens, à travers l’analyse des travaux publiés dans les vingt dernières années. Nous exposons les échelles de travail potentielles et celles réellement pratiquées, les principales applications et leurs facteurs limitants. Nous détaillons ces limites qui sont d’ordre technologique (résolutions spatiales et spectrales des capteurs), mais aussi bien souvent d’ordre conceptuel (place de la télédétection dans l’étude), ou méthodologique (traitement des images). La compréhension de ces limites, confrontées à la réalité du terrain, permet de cadrer les travaux qui pourront être menés au début du troisième millénaire.
Océanis (0182-0745) (Institut océanographie), 2000 , Vol. 26 , N. 3 , P. 311 349

Droits : info:eu-repo/semantics/openAccess
http://archimer.ifremer.fr/doc/00089/20044/17685.pdf
http://archimer.ifremer.fr/doc/00089/20044/

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
Cratons represent the oldest preserved lithospheric domains. Their lithosphere (lithospheric mantle welded to overlying Precambrian crystalline basement) is considered to be particularly robust and long-lived due to the protecting presence of buoyant and rigid “keels” made up of residual harzburgites. Although the cratons are mostly assumed to form in the Archaean, the timing of their formation remains poorly constrained. In particular, there are very few datasets describing concurrently the age of both the crustal and mantle portions of the lithosphere. In this study, we report new U–Pb ages and Hf isotope compositions for zircons in crustal xenoliths from the Udachnaya kimberlite in the central Siberian craton; this dataset includes samples from both the upper and lower portions of the crust. The zircon ages agree well with model melt-extraction Re–Os ages on refractory peridotite xenoliths from the same pipe; taken together they allow an integrated view of lithosphere formation. Our data reveal that the present day upper crust is Archaean, whereas both the lower crust and the lithospheric mantle yield Paleoproterozoic ages. We infer that the deep lithosphere beneath the Siberian craton was not formed in a single Archaean event, but grew in at least two distinct events, one in the late Archaean and the other in the Paleoproterozoic. Importantly, a complete or large-scale delamination and rejuvenation of the Archaean lower lithosphere (lower crust and lithospheric mantle) took place in the Paleoproterozoic. This further demonstrates that craton formation can be a protracted, multi-stage process, and that the present day crust and mantle may not represent complementary reservoirs formed through the same tectono-magmatic event. Further, deep cratonic lithosphere may be less robust and long living than often assumed, with rejuvenation and replacement events throughout its history.
ISSN: 0012-821X

hal-01467648
https://hal.archives-ouvertes.fr/hal-01467648
DOI : 10.1016/j.epsl.2016.09.046

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
Melting experiments were performed on a silica-rich peridotite composition at 10-17 GPa to determine majoritic garnet-melt partition coefficients (D) for major and trace elements. Our results show that D for many elements, including Na, Sc, Y and rare earth elements (REE), varies significantly with increasing pressure or proportion of majorite component. Lu and Sc become incompatible at 17 GPa, with D decreasing from 1.5 at 10 GPa to 0.9 at 17 GPa. As predicted from lattice strain, log D for isovalent cations entering the large site of majoritic garnet exhibits a near-parabolic dependence on ionic radius. Our data are used to refine a previously published predictive model for garnet-melt partitioning of trivalent cations, which suffered from a lack of calibration in the 10-20 GPa range. Our results suggest that Archean Al-depleted komatiites from Barberton (South Africa) may have been generated by partial melting of dry peridotite at depths between 200 and 400 km. We also speculate that transition zone diamonds from Kankan (Guinea), which contain inclusions of majoritic garnet, may have formed from the partial reduction of CO2-rich magmas that subsequently transported them to the surface. This hypothesis would provide an explanation for the REE patterns of majoritic garnet trapped within these diamonds, including Eu anomalies. Finally, we show that segregation of majoritic garnet-bearing cumulates during crystallisation of a deep Martian magma ocean could lead to a variety of Lu/Hf and Sm/Nd ratios depending on pressure, leading to a range of ε143Nd and ε176Hf isotope signatures for potential mantle sources of Martian rocks.
ISSN: 0024-4937

hal-00767567
https://hal.archives-ouvertes.fr/hal-00767567
DOI : 10.1016/j.lithos.2012.06.013

Éditeur(s) : HAL CCSD American Geophysical Union
Résumé : International audience
Rheological properties of mantle minerals and rocks at temperatures (T) appropriate to much of Earth's lithosphere have remained poorly constrained, even though past experimental studies on olivine single crystals and polycrystalline aggregates have quantified the high-temperature creep mechanisms (T > 1200 degrees C). Consequently, we have performed deformation experiments on crystals of San Carlos olivine at lower temperatures, from 900 degrees to 1200 degrees C, in triaxial compression along the [101](c) direction. The experiments were carried out at a confining pressure of 300 MPa in a high-resolution gas-medium mechanical testing apparatus at differential stresses of 100 to 500 MPa. Several samples were deformed at constant displacement rate and others at constant load, in order to provide insight into possible effects of work-hardening. Under the deformation conditions investigated, little evidence of work-hardening was observed. The data follow a power-law dependence on stress, as in previous high-temperature deformation studies. The samples were, however, considerably weaker than predicted by the experimentally determined high-temperature constitutive equation for olivine crystals of this orientation from the study of Bai et al. (1991). The mechanical behavior correlates instead with the weaker of the two mechanisms (flow laws) that contribute to the high-temperature constitutive equation. Thus, our experiments demonstrate that published high-temperature constitutive equations overestimate the strength of lithospheric mantle and that the transition to low-temperature creep occurs at lower temperatures than previously inferred. Citation: Demouchy, S., S. E. Schneider, S. J. Mackwell, M. E. Zimmerman, and D. L. Kohlstedt (2009), Experimental deformation of olivine single crystals at lithospheric temperatures, Geophys. Res. Lett., 36, L04304, doi: 10.1029/2008GL036611.
ISSN: 0094-8276

hal-00420070
https://hal.archives-ouvertes.fr/hal-00420070
DOI : 10.1029/2008GL036611

Éditeur(s) : Université des Antilles Études caribéennes
Résumé : Le bassin du fleuve Sixaola est un bassin transfrontalier partagé entre le Costa Rica et le Panama. Localisé sur la façade caraïbe de l’isthme centraméricain, il est depuis une vingtaine d’années considérées par les organismes de coopération et les organisations non gouvernementales comme un espace privilégié pour la coopération en matière environnementale. Ce bassin concentre en effet d’importantes richesses naturelles et culturelles propres à cette façade caraïbe. Dans le même temps, on y constate une importante vulnérabilité sociale et des dégradations environnementales croissantes, d’autant plus qu’on trouve autour de ce bassin des activités productives polluantes (monocultures, tourisme, etc.), ainsi que les villages les plus pauvres des deux pays.Cet article cherche à analyser comment, à côté des mécanismes d’intégration et des initiatives appuyées par les États, cet espace connaît aussi de nombreux projets et programmes de coopération menés par des organismes internationaux et des organisations non gouvernementales (ONG). Ces projets visent principalement à accroître la coopération transfrontalière pour la conservation et la gestion environnementale.En revanche, leur rôle est de plus en plus remis en cause par des acteurs locaux qui affirment que ces organismes « transnationaux » déplacent les États et imposent des projets qui ne prennent pas en compte les réalités et les besoins locaux tout en développant des discours « hégémoniques » sur la gestion intégrée des bassins transfrontaliers, le changement climatique, entre autres.
The Sixaola River basin is shared by Costa Rica and Panama. On the Caribbean side of the Central American Isthmus, it has been considered by cooperation organisms and non-governmental organizations as a privileged space for environmental cooperation for the past 20 years. This basin in fact concentrates an important amount of natural and cultural heritage that is endemic to this side of the Caribbean. At the same time, one can observe increasing social vulnerability and environmental degradation related to the presence of the poorest communities of both Panama and Costa Rica within the basin, and to polluting activities (monoculture, tourism, etc.) carried out around it.This article analyzes how this space is the locus of State integration mechanisms and other initiatives, at the same time that it harbors international organism and non-governmental cooperation programs. These latter projects claim to increase trans-border cooperation for conservation and environmental management.But their role is increasingly being contested by local stakeholders, who more and more claim that these “transnational” organisms displace States and impose projects that do not take into account local realities and needs, while developing “hegemonic” discourses on integrated management of trans-border basins and climate change, among other issues.
Amérique centrale
Costa Rica
Panama

Droits : info:eu-repo/semantics/openAccess
urn:doi:10.4000/etudescaribeennes.5747
http://journals.openedition.org/etudescaribeennes/5747

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
The growth of relief in active tectonic areas is mainly controlled by the interactions between tectonics and surface processes (erosion and sedimentation). The study of long-lived morphologic markers formed by these interactions can help in quantifying the competing effects of tectonics, erosion and sedimentation. In regions experiencing active extension, river-long profiles and faceted spurs (triangular facets) can help in un- derstanding the development of mountainous topography along normal fault scarps. In this study, we devel- oped analogue experiments that simulate the morphologic evolution of a mountain range bounded by a normal fault. This paper focuses on the effect of the fault slip rate on the morphologic evolution of the foot- wall by performing three analogue experiments with different fault slip rates under a constant rainfall rate. A morphometric analysis of the modelled catchments allows comparing with a natural case (Tunka half- graben, Siberia). After a certain amount of fault slip, the modelled footwall topographies of our models reaches a dynamic equilibrium (i.e., erosion balances tectonic uplift relative to the base level) close to the fault, whereas the topography farther from the fault is still being dissected due to regressive erosion. We show that the rates of vertical erosion in the area where dynamic equilibrium is reached and the rate of re- gressive erosion are linearly correlated with the fault throw rate. Facet morphology seems to depend on the fault slip rate except for the fastest experiment where faceted spurs are degraded due to mass wasting. A stream-power law is computed for the area wherein rivers reach a topographic equilibrium. We show that the erosional capacity of the system depends on the fault slip rate. Finally, our results demonstrate the pos- sibility of preserving convex river-long profiles on the long-term under steady external (tectonic uplift and rainfall) conditions.
ISSN: 0040-1951

hal-00646966
https://hal.archives-ouvertes.fr/hal-00646966
https://hal.archives-ouvertes.fr/hal-00646966/document
https://hal.archives-ouvertes.fr/hal-00646966/file/preprint_Strak_2011.pdf
DOI : 10.1016/j.tecto.2011.10.005

Éditeur(s) : HAL CCSD
Résumé : 12 pages, in French. Colloque international et interdisciplinaire pour les enjeux et usages des technologies de l'information et de la communication, 2015 (EUTIC 2015)
International audience
The emergence of new communication media such as blogs, online newspapers and social networks allow us to go further in the understanding of human behavior. Indeed, these public exchange spaces are now firmly planted in our modern society and appear to be powerful sensors of social behavior and opinion movements. In this paper, we focus on information spreading and attempt to understand what are the conditions in which a person decides to speak on a subject. For this purpose, we propose a set of measures that aim to characterize the diffusion behavior. Our measures have been used on messages related to two events that took place in January 2015: presentation by Microsoft of a new virtual reality headset and the election of a political party of radical left in Greece.
Colloque international et interdisciplinaire pour les enjeux et usages des technologies de l'information et de la communication, 2015 (EUTIC 2015)
Schoelcher, France

hal-01514258
https://hal.archives-ouvertes.fr/hal-01514258
ARXIV : 1602.00252

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
Located on the margin of the west Alboran basin, the Gibraltar Arc (Betic-Rif mountain belt) displays post-Pliocene vertical movements evidenced by uplifted marine sedimentary basins and marine terraces. Quantification of vertical movements is an important clue to understand the origin of present-day relief generation in the Betic-Rif mountain chain together with the causes of the Messinian Salinity Crisis. In this paper, we present the results of a pluridisciplinary study combining an analysis of low temperature thermochronology and Pliocene basins evolution to constrain the exhumation history and surface uplift of internals units of the Rif belt (Northern Morocco). The mean (U-Th)/He apatite ages obtained from 11 samples are comprised between 14.1 and 17.8 Ma and display a wide dispersion, which could be explained by a great variability of apatite chemistries in the analyzed samples. No correlations between altitude and age have been found along altitudinal profile suggesting a rapid exhumation during this period. Thermal modeling using our (U-Th)/He apatite ages and geochronological data previously obtained in the same area (40Ar/39Ar and K/Ar data on biotite, zircon and apatite fission track) allow us to propose a cooling history. The rocks suffered a rapid cooling at 60-100 °C/Ma between 22.5 and 19 Ma, then cooled to temperatures around 40 °C between 19 and 18 Ma. They were re-heated at around 110 °C between 18 and 15 Ma then rapidly cooled and exhumed to reach the surface temperature at around 13 Ma. The re-heating could be related to a renewal in thrusting and burying of the inner zones. Between 15 and 13 Ma the cooling resumed at a rate of 50 °C/Ma indicating an exhumation rate of 0.8 mm/y considering an average 40 °C/km geothermal gradient. This exhumation may be linked to the extension in the Alboran Sea. Otherwise biostratigraphic and sedimentological analysis of Pliocene basins of the internal Rif provided informations on the more recent events and vertical movements. Pliocene deposits of the Rifian coast represent the passive infilling of palaeo-rias between 5.33 and 3.8 Ma. The whole coastal area was uplifted at slow average rates (0.01-0.03 mm/y) in relation with a northeastward tilting of 0.2-0.3° since the Lower-Pliocene. A late Pliocene to present extensional tectonics associated to uplift has been identified all along the coastal ranges of the Internal Zone of the Rif chain. This extension was coeval with the major late Pliocene to Pleistocene extensional episode of the Alboran Sea and appears to be still active nowadays. No significant late Messinian uplift was evidenced, thus calling into question the geodynamic models relating the closure of the marine gateways and the MSC to slab roll back.
ISSN: 0264-3707

hal-01053531
https://hal.archives-ouvertes.fr/hal-01053531
DOI : 10.1016/j.jog.2014.01.006

Résumé : With resolution 3 067 (XXVIII), November 16th, 1973, the UN General Assembly decided the organization of a 3rd Conference on marine legislation which first session, "organization and proceedings", was held in New York City from December 3rd to December 14th, 1973 and whose second session, "in-depth questions", will be held in Caracas for 10 weeks between June 20th and August 29th, 1974. In reality, the decision dates back to a resolution 2 750 C (XXV), November 17th, 1970, and stems from a number of consultations carried out by the Secretary-General demonstrating that "the idea of a general-interest conference on marine legislation was largely supported". Why did it appear necessary to totally review marine legislation, 15 years after the Geneva Conferences of 1958 and 1960? This is what we will try to explain in analysing the causes of such an evolution and drawing its general tendencies, before focusing on the current situation at the opening of the conference and the future perspectives.
Par une résolution 3067 (XXVIII) du 16 Novembre 1973, l'Assemblée Générale des Nations Unies décidait la convocation d'une 3ème Conférence sur le droit de la mer dont la première session d'organisation et de procédure a eu lieu à New York du 3 au 14 Décembre 1973 et dont la deuxième session, "aux fins de traiter des questions de fond", se tiendra à Caracas pendant 10 semaines du 20 Juin au 29 Août 1974. En réalité, la décision de principe remonte B une résolution 2750 C (XXV) du 17 Décembre 1970, et résulte de consultations entreprises par le Secrétaire Général indiquant que "l'idée de convoquer une Conférence de portée générale sur le droit de la mer recueillait un large appui". Pourquoi est-il apparu nécessaire de procéder à une révision totale du droit de la mer, 15 ans après les Conférences de Genève de 1958 et 1960 ? C'est ce que nous allons essayer d'expliquer en analysant les causes d'une telle évolution et en dégageant les tendances qui se manifestent avant d'examiner la situation telle quel le se présente à l'ouverture de la Conférence et les perspectives d'avenir. [OCR NON CONTRÔLE]

Droits : info:eu-repo/semantics/openAccess
http://archimer.ifremer.fr/doc/1974/rapport-4794.PDF
http://archimer.ifremer.fr/doc/00000/4794/

Éditeur(s) : HAL CCSD
Résumé : The Neogene geodynamics evolution of the south-Alboran realm in western Mediterranean has been clarified, based on sedimentological and chronostratigraphical studies. This work focuses on three main themes of research, the first is to establish the moments for the opening and closing of the North Rifian Corridor by studying two Neogene basins of the southern edge of the Alboran sea. The second, aims to understand the behavior of these two basins face a major event in the history of the Mediterranean: The Messinian Salinity Crisis. Finally, the third theme aims to understand the modalities Post-MSC reflooding in the southern part of the Alboran realm.The late Miocene evolution of the North Rifian Corridor is clarified on the basis of chronostratigraphic studies of the Neogene Boudinar and Arbaa Taourirt basins (northeastern Morocco). The marine sediments deposited in the Boudinar basin between the early Tortonian and the late early Messinian (10 Ma to 6.1 Ma) and in the late Tortonian-earliest Messinian interval in the Arbaa Taourirt basin. Palaeoenvironmental data record a major drowning in association with extensive tectonics in the Boudinar basin during the early Messinian at ~7.2 Ma. At the same time, prograding conglomerates and sandstones developed over the late Tortonian marls in the Arbaa Taourirt basin. During the late-early Messinian, a shallowing trend occurred in the Boudinar basin. Thus, the North Rifian Corridor opened at ~7.2 Ma ensuring Atlantic-Mediterranean connections, then was progressively restricted during the late-early Messinian and totally closed at ~6.1 Ma. New sedimentological and paleontological studies of the late Messinian-early Pliocene deposits in the Boudinar basin provide new information on the Messinian Salinity Crisis (« MSC ») and the Zanclean reflooding in the Alboran sea. The Messinian erosional surface « MES » is of late Messinian age and was emplaced in subaerial settings. It is polygenic, its original geometry is locally preserved and was re-shaped by the Pliocene transgressive surface. Above the « MES », the Boudinar basin infill is characterized by a wide variety of facies from continental settings to lower offshore conditions. Two major sets are recognized: a latest Messinian-Zanclean set that constitutes a transgressive-regressive megasequence interrupted at the top by a tectonic unconformity, and an Plio-Quaternary regressive set. During the late Messinian Zanclean interval, four successive depositional models were documented. They record major changes in palaeoflow and paleogeography related to base-level fluctuations. No Gilbert-type delta has ben identified at Boudinar. the beginning of base-level rise is marked by normal regressions and by the formation of several lacs and fan-delta complexes on the margins of the basin in the late Messinian and befor the marine reefloding in the early Zanclean. The marine reflooding of the basin appears later, with a transgressive surface of ravinment and a thick package of transgressive deposits. These transgressive deposits onlap over all previous deposits. The major part of the basin infill did not issue from an inner landward position (south of the basin) but from the northwestern side of the basin, i.e. near the Mediterranean. Sediments were subsequently reworked by storms and transported by longshore-drift towards the south. a maximum flooding surface is found several tens of metres above the « MES ». This fiding is consistent with a progressive and not a catastrophic early Zanclean flooding of the westernMediterranean after the Mediterranean base-level fall.
Sur la base d’études sédimentologiques et chronostratigraphiques dans les bassins de Boudinar et d’Arbaa Taourirt (Rif oriental, Maroc), l’évolution géodynamique néogène du domaine sud-Alboran en Méditerranée occidentale a été clarifiée. Ce travail est axé sur trois grandes thématiques de recherche. La première vise à l’établissement d’un cadre chronostratigraphique pour l’ouverture et la fermeture du Couloir Nord Rifain, par l’étude de deux bassins nèogènes de la bordure sud de la mer d’Alboran. La deuxième, vise à comprendre le comportement de ces deux bassins face à un événement majeur de l’histoire de la Mediterranée : la Crise de salinité messinienne. Finalement, la troisième vise à comprendre les modalités de remise en eau de la Méditerranée après la Crise : le reenoiement pliocène. L'évolution du Couloir Nord Rifain au Miocène supérieur est clarifiée sur la base des études chronostratigraphiques des bassins néogènes de Boudinar et d'Arbaa Taourirt (Maroc Nord oriental). Les sédiments marins miocènes se sont déposés entre le Tortonien inférieur et le Messinien inférieur (10 à 6.1 Ma) dans le bassin de Boudinar et entre le Tortonien supérieur et le Messinien inférieur dans le bassin d'Arbaa Taourirt. Les données paléoenvironnementales enregistrent un ennoyage important du bassin de Boudinar en relation avec une tectonique extensive pendant le Messinien inférieur (~7.2 Ma). En même temps, des conglomérats et de grès progradants se sont développés au-dessus des marnes tortoniennes dans le bassin d’Arbaa Taourirt. Le bassin de Boudinar a subi un désapprofondissement au Messinien inférieur. Ces résultats indiquent que le Couloir Nord Rifain s’est ouvert à ~7.2 Ma assurant les communications entre l’Atlantique et la Méditerranée, puis a subi une restriction progressive pendant le Messinien inférieur avant d’être totalement fermé à ~6.1 Ma.De nouvelles études sédimentologiques et paléontologiques des dépôts Messinien supérieur-Pliocène inférieur dans le bassin de Boudinar fournissent des informations sur la Crise de salinité messinienne (« MSC ») et le réennoiement zancléen dans la Mer d'Alboran. L’un des marqueurs majeurs de la Crise est identifié : la surface d’érosion messinienne « MES ». Elle est d'âge Messinien supérieur et a été mise en place dans des conditions subaériennes. Sa géométrie originale n’est préservée que localement et a été remodelée par la surface transgressive du Pliocène inférieur. Au dessus de la « MES » le remplissage sédimentaire du bassin de Boudinar est caractérisé par une grande variété de faciès allant des conditions de dépôts continentales jusqu’à des conditions d’offshore inférieur. Deux ensembles majeurs sont reconnus : un ensemble messinien terminal-zancléen qui constitue une mégaséquence transgressive-regressive, interrompue au sommet par une discordance tectonique, et un ensemble plio-quaternaire regressif. Durant l’intervalle Messinien terminal-Zancléen, quatre modèles de dépôts successifs ont été documentés enregistrant des changements majeurs de paléocourants et de paléogéographies, liés aux fluctuations de niveau de base. Nous n’avons pas identifié de Gilbert delta à Boudinar. La remontée du niveau de base est marquée par une régression normale et par le développement des lacs et de complexes de fan-deltas sur les marges du bassin pendant le Messinien supérieur, avant l’inondation marine au Zancléen basal. Le réennoiement marin du bassin apparait plus tard avec une surface de transgression ravinante et par d’épais dépôts transgressifs, en onlap sur tous les dépôts précédents. La majeure partie du remplissage sédimentaire du bassin n’est pas reçue des reliefs de la bordure sud du bassin, mais du côté Nord-Ouset au bord de la Méditerranée. Les sédiments sont alors remaniés par les tempêtes et transportés vers le sud par la dérive littorale. Une surface d’inondation maximale a été identifiée à plusieurs dizaines de mètres au-dessus de la « MES ». Ceci suggère un ennoiement progressif et non catastrophique, après la chute du niveau de base méditerranéen.
https://tel.archives-ouvertes.fr/tel-01473572

Droits : http://hal.archives-ouvertes.fr/licences/copyright/
tel-01473572
https://tel.archives-ouvertes.fr/tel-01473572
https://tel.archives-ouvertes.fr/tel-01473572/document
https://tel.archives-ouvertes.fr/tel-01473572/file/Th%C3%A8se-achalhi.pdf

Éditeur(s) : Université des Antilles Études caribéennes
Résumé : La prostitution est une problématique très intéressante d’une part parce qu’elle est transversale à tous les temps, à toutes les classes sociales, à tous les espaces, et d’autre part parce qu’il s’agit d’un fléau qui se conjugue le plus souvent au féminin. Il s’agit à mon sens du versant spécifique d’une problématique universelle dont personne ne peut s’affranchir sans mettre en jeu l’ensemble de la condition humaine. En effet, la prostitution est le lieu où convergent et se concentrent de façon exacerbée tous les maux d’une société. La femme est malgré elle au centre de ce système dans lequel on retrouve les frustrations, les rapports de domination, de pouvoir, la violence, la misère, la corruption, l’aliénation… La prostitution, tout comme le concept de genre, est une construction sociale, dans laquelle les femmes sont enfermées réellement et symboliquement.D’autre part, si les maux d’une société sont décuplés dans le système de la prostitution, nulle part ailleurs n’existe un tel abîme entre fantasme et réalité. C’est le lieu des fausses représentations et des euphémismes comme le montrent ces deux expressions édulcorées « zones de tolérance » et « femmes publiques ». A Cuba, malgré les tentatives d’éradication de la prostitution dans les premières décennies qui suivirent le triomphe de la Révolution de 1959, la chute du bloc soviétique et la période de pénurie qui s’ensuivit donnèrent lieu à un retour de cette prostitution, sous de nouvelles formes qui persistent aujourd’hui. Cependant, il fut une époque, celle de la première République (1902-1958) durant laquelle Cuba, rongée par un système néocolonial, connût une recrudescence de ce phénomène, dans des proportions jamais égalées. Une époque somme toute récente où les zones de tolérance, espaces où étaient regroupées les maisons closes, occupaient une grande partie de La Havane coloniale ainsi que des quartiers entiers à travers l’île. A l’intérieur de ces zones très lucratives dont profitaient à la fois les proxénètes, policiers, politiques et hommes d’affaires, les femmes cubaines, mais également, dans une grande proportion des Françaises victimes de la traite des Blanches, se trouvaient au cœur d’un système qui étaient à lui seul le symptôme de la frustration néocoloniale, mais également de l’exacerbation du patriarcat.Cette problématique, on ne peut plus actuelle, convoque la pluridisciplinarité, c’est pourquoi j’ai eu recours à des témoignages de prostituées depuis le début du siècle jusqu’à la Révolution, recueillis et publiés à Cuba. Je me suis penchée sur les différents discours sur la prostitution de l’époque, discours politiques et féministes. Les rapports de police, les plaintes déposées par des femmes, les comptes rendus de procès, et les descriptions des médecins-hygiénistes sont autant de sources qui viennent corroborer les témoignages.
The republican era in Cuba is a complex and difficult one for the Cuban population. 1898 remains engraved in people’s memories as being a time of great disillusion for a population who, having freed itself from Spanish colonial domination, was deprived of independence by the United States of America. Three years of American intervention sufficed to put power bases into place, guarantee maximal exploitation conditions and organize the legal framework of the American domination over Cuba by means of the Platt Amendment in 1901. The protectorate set up by the United States, followed by a neocolonial system in 1934, relies upon the collaboration of presidents and corrupt governments succeeding each other in power. Corruption, nepotism and violence are put in place in a society in which inequality is dramatically worsening and all moral values are disintegrating. In this context and in a Cuban society governed with patriarchal rules, women are the first victims of the system. After the wars of independence, the only options they have are marriage, work or prostitution. Legitimate marriage is only available to a privileged few. With regards to employment, only 9.8% of women have the opportunity to work and this percentage didn’t change until 1959. It was at this time that prostitution reached unprecedented levels. It wasn’t just the case of a few marginalized women but of thousands of mothers, wives, widows and working women who were trapped in this alienating condition, forced to sell their bodies. Legislation and violence are used to control and restrict the work space for prostitutes, removing these ‘streetwalkers’ from the public eye, grouping them together in tolerance zones with very strict rules, which are in reality in the hands of Cuban and French procurers, and subjecting them to constant inspections carried out by hygienists who physically and symbolically assault women’s bodies. What is more, speeches about prostitution, whether made by politicians, feminists, journalists, doctors or mere observers, contribute significantly to a certain representation of these women. While debates about prostitution have recently shaken public opinion, this work refers back to an episode of Cuba’s history which brings us to reflect upon the evolution of the phenomenon and on its protean nature.
Cuba

Droits : info:eu-repo/semantics/openAccess
urn:doi:10.4000/etudescaribeennes.6945
http://journals.openedition.org/etudescaribeennes/6945

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
Almost all Red Sea deeps contain metal-rich sediments covered by brine pools. It is generally agreed that these metal-rich deposits precipitated from overlying metal-rich brines that originated from migrating hydrothermal fluids. No brine pool has ever been reported in Thetis Deep, inciting us to evaluate if such a brine layer ever occurred in the deep during the past. In order to address that questioning, a study combining mineralogical, geochemical (major-, minor-, rare-earth elements) and isotopic (Sr. Nd. Pb) approaches was completed on cored sediments and extracted interstitial waters from inside and outside the deep.;The sediments have an overall hydrothermal origin, as shown by the REE concentrations and patterns, metal contents, and Pb-Nd isotopic data, all pointing to a mantle signature. The intensity of the hydrothermal activity varied with time in the deep; the most intense episode resulting in an almost pure Fe-oxi-hydroxide layer. Varied chemical arguments, especially the Zr and REE data of the sediments, favor the fact that the whole sedimentation in Thetis Deep occurred in the absence of a stable, salt-rich and mineralized brine pool, and that no brine layer ever existed. This conclusion is supported by the constant Sr isotope composition of the sediment and its interstitial waters that are almost identical to that of the Red Sea seawater. The study also suggests that hydrothermal activity monitored fluid supplies that interacted differently with seawater in the different Red Sea deeps, resulting in an overall formation of metal-rich sediments, but along varied local conditions. (C) 2009 Elsevier B.V. All rights reserved.
ISSN: 0375-6742

hal-00475646
https://hal.archives-ouvertes.fr/hal-00475646
DOI : 10.1016/j.gexplo.2009.10.001