Éditeur(s) : Société des sciences naturelles de la Charente-Maritime
Résumé : During 1975, a number of rare fishes or caught out of their distr:ibution area were observed in La Rochelle, especially Chlamycloselachus anguineus Garman, 1884 (one specimen) Mitsukurina sp. (three specimens), Pseudotriakis microdon Capello, 1868 (five specimens), Somniosus sp. (one specimen), probably a new species, Zenopsis cO/1chîfer (Lowe, 1852) (one specimen) recorded for the first time from the French Atlantic coast, Puntazzo puntazzo (Gmelin, 1789) (one specimen), Hyperoglyphe percifonnîs (Mitchill, 1818) (one specimen), Glyptocephalus cynoglossus (Linné, 1758) (one specimen) caught off the coast of Vendée and Lima11da limanda (Linné, 1758) (one specimen) caught off the coast of Landes. On the other hand, the authors found two albino fishes and five specimens remarkable for their large size. They also observed nine species of fishes from the Bay of Biscay belonging to a colder fauna and eight species of fishes from the Bay of Biscay belonging to a hotter fauna. Not controlled OCR
En 1975, les auteurs ont observé à la Rochelle un certain nombre de poissons «rares» ou capturés en dehors de leur aire de répartition et plus particulièrement un exemplaire de Chlamycloselachus anguineus Garman, 1884, trois exemplaires de Mitsukurina sp., cinq exemplaires de Pseuclotriakis microdon Capello, 1868, un exemplaire de Somniosus sp., cette espèce étant probablement nouvelle, un exemplaire de Zenopsis conchifer (Lowe, 1852) signalé pour la première fois au large des côtes françaises de l'Atlantique, un exemplaire de Puntazzo plmtazzo (Gmelin, 1789), un exemplaire d'Hyperoglyphe percîformis (Mitchill, 1818), un exemplaire de Glyptocephalus cynoglossus (Linné, 1758) pêché au large de la Vendée et un exemplaire de Limanda limanda (Linné, 1758) pris au large de la côte des Landes. D'autre part, ils ont observé deux cas d'albinisme ainsi que cinq exemplaires remarquables par leur grande taille. Ils ont aussi noté la présence dans le golfe de Gascogne de neuf espèces de poissons appartenant à une faune plus froide et de huit à une faune plus chaude. OCR non contrôlé
Annales de la Société des Sciences Naturelles de la Charente-Maritime (Société des sciences naturelles de la Charente-Maritime), 1976 , Vol. 6 , N. 3 , P. 177-190

Droits : 1976 Société des sciences naturelles de la Charente-Maritime
http://archimer.ifremer.fr/doc/1976/publication-3645.pdf
http://archimer.ifremer.fr/doc/00000/3645/

Éditeur(s) : Inter-research
Résumé : Marine protected areas (MPAs) have the potential to enhance the long-term sustainability of coastal resources, and the artisanal fisheries which depend on them. However, recreational fisheries, which are increasing their impacts on coastal resources worldwide, may reduce the benefits that MPAs provide to declining artisanal fisheries. Here we used the Bonifacio Straits Natural Reserve (BSNR) Corsica as a study case to simulate the combined effects on coastal resources of artisanal and recreational fishing efforts. The BSNR ecosystem was modelled using mass-balance modelling of trophic interactions. This model was compared to another built on a non-protected area from the same region. We aggregated fishing fleets into artisanal and recreational categories, and we simulated various combinations of fishing effort over a 20 yr dynamic simulation using Ecosim. We showed that fishing activities have an additional top-down effect on the food web and that they decrease the targeted group's biomass, such as piscivorous species. We found, for some trophic groups, non-trivial patterns of biomass variation through trophic cascades. Our trophic approach revealed that some groups may suffer a biomass decrease when MPAs are set or enforced, due to the combined effect of artisanal and recreational fisheries. Overall, our results illustrate the value of modelling to manage MPAs, as a complementary tool to surveys. Models provide the opportunity to anticipate the potential consequences, at the ecosystem level, of socio-political decisions that aim to sustain coastal resources while managing artisanal and recreational fisheries.
Marine Ecology-progress Series (0171-8630) (Inter-research), 2010-08 , Vol. 412 , P. 207-221

Droits : Inter-Research 2010
http://archimer.ifremer.fr/doc/00013/12436/9246.pdf
http://archimer.ifremer.fr/doc/00013/12436/9247.pdf
DOI:10.3354/meps08679
http://archimer.ifremer.fr/doc/00013/12436/

Éditeur(s) : Université des Antilles Études caribéennes
Résumé : Le tourisme balnéaire joue un rôle fondamental dans le développement économique des pays des deux rives du bassin méditerranéen. Climat tempéré, plages sablonneuses et beauté du paysage naturel côtier représentent le support à cette nouvelle activité. Si dans beaucoup de pays, comme l’Espagne, le Maroc, la Tunisie, la France, etc., une large surface du littoral est mise en tourisme, les aménagements touristiques restent en Algérie très ponctuels et en décalage avec la demande réelle de la population. La volonté de l’Etat algérien de faire du tourisme balnéaire une activité génératrice de richesse dans l’objectif d’atténuer la dépendance de l’économie au secteur des hydrocarbures, rencontre beaucoup de difficultés telles la question des enjeux fonciers et les dysfonctionnements entre les outils d’aménagement et ceux de protection de la nature. Dans cet article, l’objectif est, à travers le cas du littoral mostaganemois, d’analyser l’évolution des dispositions institutionnelles en matière du tourisme balnéaire et de leurs mises en œuvre sur le terrain toute en analysant les spécificités du contexte socioéconomique et naturel à une échelle locale.
The seaside tourism plays a fundamental role in the economic development of the Mediterranean countries. Temperate climate, sandy beaches and natural coastal landscape are the support to this new activity. If in many countries such as Spain, Morocco, Tunisia and France, etc., the tourism development is diffused over a wide area of the coast, it remains very limited phenomenon in Algeria and out of step with real request of the population. The will of the Algerian state to make of the seaside tourism a generative financial activity with the objective to limit the dependence of the energy income, faced many difficulties such land issues and dysfunctions between development tools and those of nature protection.In this article, the objective is, through the case of the Mostaganem coast, to discuss the evolution of the institutional capacities regarding the seaside tourism and his implementation on the ground while analyzing the specifities of socioeconomic and natural context in a local scale.
Algérie
Monstaganem

Droits : info:eu-repo/semantics/openAccess
urn:doi:10.4000/etudescaribeennes.9305
http://journals.openedition.org/etudescaribeennes/9305

Éditeur(s) : Amer Geophysical Union
Résumé : Seismic noise is an indirect source of information on ocean waves. Using a model of noise generation and propagation, seismic stations can be separated into those that are mostly sensitive to local sea states, and those that integrate sources from a large oceanic area. The model also provides a classification of noise-generating sea states into three classes. The analysis of Central California seismic noise data, well correlated with local waves, reveals that class I events dominate in summer, caused by a single wind-sea system, and for which ocean wave spectral levels are proportional to seismic spectral levels to an exponent b similar or equal to 0.9. In winter, noise is dominated by class II generation, for which coastal reflection is important, with a wave spectral density roughly proportional to the seismic spectral density to an exponent b similar or equal to 0.7. Sporadic events of class III probably produce some of the strongest noise events in Central California and need to be properly screened. These events are caused by opposed wave systems that are usually the wind-sea and a swell. This noise classification can be used to improve on the correlation between measured and estimated wave heights(up to r = 0.93 for daily averages). For other locations, where remote oceanic sources are recorded, a significant wave height estimated from the seismic noise compares well with area-averaged satellite data or wave model results(r > 0.85 for daily averages). These analyses pave the way for quantitative uses of seismic records, including the reconstruction of past wave climates, and the calibration of wave hindcasts.
Journal Of Geophysical Research-oceans (0148-0227) (Amer Geophysical Union), 2012-05 , Vol. 117 , N. C05002 , P. 19 pp.

Droits : 2012 AGU
http://archimer.ifremer.fr/doc/00083/19443/17051.pdf
DOI:10.1029/2011JC007449
http://archimer.ifremer.fr/doc/00083/19443/

Éditeur(s) : Elsevier
Résumé : The study, which is based on repetitive bathymetric surveys, assesses changes and effects of one of the most important floods recorded in the Rhone Delta area: bottom morphology and sediment distribution in the Rhone outlet after the December 2003 flood are discussed by comparison between Digital Terrain maps (DTMs) of November 2003 and January 2004. The post-flood morphology shows that the whole of the system is active, mainly in the east. The channel of the Rhbne has been hollowed out on the left bank by more than 5 m, the eastern coast of the mouth has retreated 400 m, the mouth-bar has prograded 200 m and the slope of the delta front has increased by 0.19. The overlay of pre- and post-flood DTMs makes it possible to estimate the total volume deposited in the [0 to -20 m] zone as +7.8 X 10(6) m(3) (i.e. 0.88 m(3) m(-2)), which corresponds to 4 X 10(6) t of sediment. These values are compared with the average annual volume of 0.47 X 10(6) m(3) yr(-1) of sediment deposited in this zone between 1995 and 2003, as well as the average sediment load estimated at the Arles station (50 km upstream) for this flood event (3.1 x 10(6) t to 5.3 x 10(6) t). The acquisition of bathymetric measurements immediately before and after a major flood allows more than a simple morphological description; in addition, an analysis of the solid load transfer processes towards the prodelta is achievable. Three mechanisms are highlighted. Most of the material eroded in the channel and supplied to the delta front corresponds to fine sediment that drape homogeneously over the pre-flood morphology of the delta front. The transit of the coarsest sediment (primarily sand) is slowed down in the channel of the Rh6ne: this sediment builds up in relatively small areas, leading to the formation of gullies on the prodelta slope. The gullies have fixed positions and disappear gradually towards the west, following the progressive migration of the active band towards the east. These old features are not reactivated by floods occurring after their formation. During the flood, only a small volume of coarse sediment bypasses through the gullies, and the fine deposits are remobilised rapidly or compacted. Flood input concerns essentially the delta front, which traps 90% of the fluvial solid discharge between 0 and 20 m depth. The coarse prodelta supply is then due mainly to mass movements of unconsolidated material deposited beforehand on the top of the delta front. Consequently, the main nourishment of the prodelta does not occur directly during and/or immediately after a flood event, but is delayed by sediment being temporarily trapped on the delta front.
Marine Geology (0025-3227) (Elsevier), 2006-12 , Vol. 234 , N. 1-4 , P. 159-177

Droits : 2006 Elsevier B.V. All rights reserved
http://archimer.ifremer.fr/doc/2006/publication-2304.pdf
DOI:10.1016/j.margeo.2006.09.025
http://archimer.ifremer.fr/doc/00000/2304/

Éditeur(s) : HAL CCSD
Résumé : International audience
Understand the dynamics of the fresh-salt water interface in aquifers is a key issue to comprehend mixing processand to quantity the discharge of nutrients in to coastal areas. In order to go beyond the current knowledge inthis issue an experimental site has been set up at the alluvial aquifer Riera Argentona (Barcelona – Spain). Thesite comprises 16 shallow piezometers installed between 30 and 90 m from the seashore, with depths rangingbetween 15 and 25 meters. The seawater interface is being monitored using several techniques, the combinationof which will help us to understand the spatial and temporal behaviour of the mixing zone and the geochemicalprocesses occurring there. Specially the deepest piezometers are equipped with electrodes in order to performcross-hole electrical resistivity tomography (CHERT). In addition, all piezometers are also equipped with FiberOptic cable to perform distributed temperature measurements. Two single steel armoured fibre optic cable lines ofaround 600m length were installed in all boreholes. The objective is to use the cable both as passive and activetemperature sensor. The first is being done for the continuous monitoring of temperature whereas; the secondprovides a higher temperature resolution used to monitor field experiments.Periodic CHERT measurements are carried out between the piezometer equipped with electrodes, resultingin parallel and perpendicular vertical cross sections of the site resistivity. The position of the fresh-salt waterinterface can be identified due to the resistivity contrast between the saline and fresh water. Preliminary resultsof periodic distributed temperature measurements will be also be used to monitor the position of the mixing zonethanks to the contrast and seasonal temperature changes. Periodic down-hole EC profiles will be used to validatethe method.AcknowledgementsThis work was funded by the projects CGL2013-48869-C2-1 y CGL2013-48869-C2-2-R of the Spanish Government.We would like to thank SIMMAR (Serveis Integrals de Manteniment del Maresme) and the ConsellComarcal del Maresme in the construction of the research site
European Geosciences Union General Assembly 2016
Vienne, Austria

insu-01308757
https://hal-insu.archives-ouvertes.fr/insu-01308757

Éditeur(s) : Université des Antilles Études caribéennes
Résumé : L’article présente les différences de perception entre les touristes et les résidents en matière de protection de l’environnement marin et côtier. Il s’appuie sur les résultats des études menées à l’échelle de la Martinique en 2010 dans le cadre de l’évaluation de la valeur économique et sociale des récifs coralliens et écosystèmes associés et à celle de la commune du Prêcheur en 2011 dans le cadre de la mise en place de la réserve marine régionale. Il met en exergue les éléments qui composent les disparités de perception et de souhaits quant aux mesures de gestion des espaces littoraux. Il montre toutefois que la création d’une aire marine protégée dans la commune du Prêcheur emporte l’adhésion de tous.
The article presents the differences in perception between the tourists and residents regarding the protection of the marine and coastal environment. It is based on the results of studies conducted across Martinique in 2010, in the framework of the evaluation of the economic and social value of coral reefs and associated ecosystems, and at the level of the rural community of le Prêcheur in 2011, in the context of the implementation of the regional marine reserve. It highlights the elements that compose the disparities of perception and wishes with respect to coastal areas management measures. It shows, however, that the creation of a marine protected area in the commune of le Prêcheur has the unanimous support of all.
Martinique
Prêcheur

Droits : info:eu-repo/semantics/openAccess
urn:doi:10.4000/etudescaribeennes.9351
http://journals.openedition.org/etudescaribeennes/9351

Éditeur(s) : Observatoire Océanologique de Banyuls sur mer
Résumé : Among a small collection of Annelida Polychaeta collected in the Banyuls-sur-Mer area which I was sent to for identification by M. Amouroux (Arago Laboratory, 66-Banyuls-sur-Mer) were three specimens of a recently described species of Paraonidae from the Breton coast, Paradoneis armata Glémarec, 1967. Two years later, this species was found in the eastern Mediterranean Sea, on the Cretan coasts (Kalo-Limmiones) in the endofauna of a Halophila stipulacea prairie by Harmelin (1969), who described and figured the main distinctive characters of this Paraonidae (the reference to the original description is erroneous, Glémarec linking this specimen to the genus Paradoneis Hartman, 1965, and not to the genus Paraonides Cerruti sensu Hartman, 1965). The discovery of P. armata in Banyuls-sur-Mer demonstrates the probable continuity of this species' distribution area, from Crete to the coasts of Finistère. I had the opportunity to compare the three eastern Mediterranean specimens to some Breton ones, provided by M. Glemarec, and this comparison drove me to examine again a relative form, Cirrophorus branchiatus Ehlers, 1908, discovered in the Mediterranean Sea a few years ago (Laubier 1966).
Parmi une petite collection d'Annélides Polychètes recueillie dans la région de Banyuls-sur-Mer qui m'a été envoyée pour identification par M. AMOUROUX (La boratoire Arago, 66-Banyuls-sur-Mer) figuraient trois spécimens d'une espèce de Paraonidae décrite récemment des côtes de Bretagne, Paradoneis armata Glémarec, 1967. Deux ans plus tard, l'espèce est retrouvée en Méditerranee orientale sur les côtes de Crète (Kalo-Limmiones) dans l'endofaune d'une prairie à Halophila stipulacea par HARMELIN (1969), qui décrit et figure les principaux caractères distinctifs de ce Paraonidae (la référence à la description originale est erronée, GLÉMAREC ayant rapporté cette forme au genre Paradoneis Hartman, 1965, et non au genre Paraonides Cerruti sensu Hartman, 1965). La découverte de P. armata à Banyuls-sur-Mer témoigne donc de la continuité probable de l'aire de répartition de cette espèce, depuis la Crète jusqu'aux côtes du Finistère. J'ai pu comparer les trois individus de Méditerranée occidentale avec des spécimens de Bretagne qui m'ont été aimablement confiés par M. GLEMAREC, et cette comparaison m'a conduit à reprendre également l'examen d'une forme voisine, Cirrophorus branchiatus Ehlers, 1908, découverte en Méditerranée depuis quelques années (LAUBIER 1966). [OCR NON CONTRÔLE]
Vie et milieu (Observatoire Océanologique de Banyuls sur mer), 1971 , Vol. 22 , N. 2A , P. 259-262

Droits : Observatoire Océanologique de Banyuls sur mer
http://archimer.ifremer.fr/doc/1971/publication-5030.pdf
http://archimer.ifremer.fr/doc/00000/5030/

Résumé : Le mérou géant, Epinephelus itajara, espèce en danger critique d’extinction au niveau mondial, est présent dans les eaux turbides et saumâtres de la Guyane française où l’espèce est exploitée par une pêcherie côtière. Dans la partie est du plateau continental guyanais, les mérous géants se localisent autour de tous les sites rocheux marins où ils se répartissent en fonction de la profondeur et du faciès (éboulis ou tombant). Les analyses des isotopes stables du carbone et de l’azote suggèrent qu’environ 30 % des mérous géants < 115 cm présents sur ces sites rocheux, proviendraient des mangroves alentours. Les analyses de contenus stomacaux révèlent un changement ontogénétique du régime alimentaire. Les petits individus (< 90 cm) s’alimentent principalement de Crustacés puis intègrent progressivement les poissons à leur alimentation jusqu’à devenir essentiellement piscivores au-delà de 140 cm. La population de Guyane est principalement composée d’individus juvéniles : seulement 8,5 % des individus capturés en Guyane a plus de 6 ans. Ces jeunes mérous sont très territoriaux durant les 4-5 premières années de leur vie puis ne sont plus retrouvés sur les sites rocheux. Le devenir de ces juvéniles est incertain, soit ils sont pêchés, soit ils migrent vers d’autres sites ou vers les agrégations de reproduction. Cependant, les mérous géants ne semblent pas se reproduire en Guyane. Il est possible que les conditions environnementales (forte turbidité et température) ne favorisent pas le développement gonadique, ce qui engendrerait une omission totale de reproduction. Le suivi par tags satellite suggère que les mérous géants migrent dans le sens des courants marins vers Trinidad-et-Tobago, potentiellement pour la reproduction. Aucun mouvement vers le Brésil n’a été mis en évidence bien que les stocks de mérous géants du Brésil et de Guyane semblent liés. En effet, ces deux stocks évoluent conjointement avec un déclin des populations au début des années 90. Le maintien de la population de mérou géant en Guyane se ferait grâce à l’apport de larves des sites d’agrégation du Brésil par le courant marin. La mortalité totale des mérous géants (0,65) est aussi élevée au sein de la réserve marine ainsi que sur les sites de pêche. Cela suggère que l’interdiction de pêche à la réserve n’est pas respectée et que les grands individus quittent la réserve pour des sites plus spacieux. En supposant que la population de mérous géants adultes a été réduite à cause de la pêche, une protection régionale des individus > 150 cm doit être instaurée afin de régénérer le stock d’individus matures. Il semble nécessaire de développer une politique de gestion internationale de l’espèce, surtout entre la Guyane et le Brésil, afin de conserver les populations de mérous géants d’Amérique du Sud.
The critically endangered Goliath Grouper, Epinephelus itajara, is found in the turbid and brackish waters of French Guiana, where the species is subject to a coastal fishery. Goliath Grouper populations inhabit all rocky habitats and exhibit increasing abundance with depth. Around 30% of individuals less than 115 cm may derive from the abundant mangrove habitat along the french Guiana coast. There is a ontogenetic shift of the diet, primarily crustacivorous, individuals >140 cm become piscivorous. The Goliath Grouper population in French Guiana is composed primarily og juvelines. The fate of the juvelines is unknonw, some may be caught in the fishery, others may move to other habitat. No evidence of spawning or gonadal readiness was found in french Guiana. it is possible that environmental conditions (high turbidity and temperature) are not conducive to reproductive activity. Goliath Grouper may migrate down current from French Guiana to Trinidad and Tobago or further. No movement of Goliath Grouper was found against the current toward Brazil. French Guiana juveniles may be derived from spawns occuring off Brazil. Calculated total mortality of Goliath Grouper off French Guiana is high (0.65) in both fished and protected areas suggesting that illegal fishing is occuring within the protected area, or that emigration rates are high. Assuming that the adult population of Goliath Grouper in French Guiana has been reduced due to fishing, protection of spawning-size adults (larger than about 150 cm TL) should be instated.

http://www.theses.fr/2014AGUY0721/document

Éditeur(s) : Elsevier
Résumé : The accumulation of nine heavy metals in fine-grained sediments from the mangrove fringed coast of French Guiana is evaluated. The dynamic features of the South American tropical coastline, from the Amazon to the Orinoco Rivers, result in mangrove sediments being alternately submitted to phases of erosion and net sedimentation a few tens of years long. This process influences the distribution of the heavy metals associated with these frequently re-mobilized deposits. Sedimentary cores and mangrove plant samples were collected, at different seasons, in various swamps characterized by different properties (content of sedimentary organic matter, distance from sea water and fresh water). The ranges of measured concentrations expressed in mu mol g(-1) were the following: Cu (0.06 to 0.61), Co (0.12 to 0.68), Pb (0.08 to 0.18), Ni (0.32 to 0.76), Cr (0.61 to 1.40), Zn (1.25 to 5.94), Mn (4.36 to 45.4) and Fe (441 to 1128). No differences were found between sediments from mangroves developing upstream and downstream of urban areas, i.e. Cayenne and Kourou. This suggests that the content of mangrove sediments in heavy metals along the coastline of French Guiana is essentially the result of the continuous alternation of accumulation and transport phases occurring upstream after departing from the Amazon watershed. The sources of this heavy metals content are thus difficult to identify. However it is well known that the alluvium produced by the natural erosion of the Amazonian soils is naturally enriched in mercury. Also, the run-off from gold mining activities is known to contribute to mercury pollution. Ranges in total Hg were between 0.15 and 2.57 nmol g(-1), with mean values close to 0.41 nmol g(-1), and were clearly correlated with total organic carbon except for some outstanding high values, which may be a result of rapid geochemical changes. Heavy metal concentrations showed variations with depth. The redox conditions and the decay processes affecting the organic matter control the cycling of iron and manganese, which in turn control the concentrations and associations of heavy metals. These preliminary results suggest that the variations in heavy metal content with depth or between mangrove areas result largely from diagenetic processes rather than changes in metal input resulting from local human activities. (c) 2005 Elsevier B.V. All rights reserved.
Marine Chemistry (0304-4203) (Elsevier), 2006 , Vol. 98 , N. 1 , P. 1-17

Droits : 2005 Elsevier B.V. All rights reserved
http://archimer.ifremer.fr/doc/2006/publication-1041.pdf
DOI:10.1016/j.marchem.2005.06.001
http://archimer.ifremer.fr/doc/00000/1041/

Éditeur(s) : Université de Bretagne Occidentale
Résumé : Study of mineral suspended particulate matter (SPM) is essential to understand ecosystem dynamics. SPM influences light penetration which is closely related to primary production and carries pollutants and nutrients within the water masses. This work aims to study near-surface mineral SPM dynamics in the English Channel using two complementary methods: remote-sensing by satellites and numerical modelling. Firstly, MODIS and MERIS satellite images processed by the IFREMER semi-analytical algorithm and describing non-algal SPM, are analysed to build three statistical models which are able to estimate near-surface SPM using simple variables, e.g., tidal coefficient, significant wave height and mean chlorophyll-a concentration. Secondly, the three-dimensional hydrosedimentary model ROMS (Regional Ocean Modeling System) is applied in the English Channel. It considers tidal forcing along open boundaries, wind stress at the sea-surface, wave-current interactions in the bottom boundary layer and realistic heterogeneous bottom sediments. Results of the more sophisticated statistical model is also used to impose SPM concentrations at open boundaries. Sensitivity tests on SPM boundary conditions show the importance of prescribing realistic sediment concentrations to improve the model predictions. Biological influences on mineral SPM are also tested using settling velocity and critical shear stress for erosion which vary with seasons. Both statistical and numerical models highlight and locate respective influences of tide, waves and biology on mineral SPM. Numerical predictions indicate that near-surface SPM is mainly composed of silts (>70%). Near-surface suspended silts come largely from seabed resuspension alongshore in the Eastern Channel and from the open boundaries of our limited-area coastal model at the West of Cotentin Peninsula and offshore. Near-surface SPM variations are investigated at semi-diurnal, neap-spring tidal cycle time scales and during a wave event. Finally, dynamics of sediments in the turbidity maximum zone around the Isle of Wight is examined depending on hydrodynamical conditions in order to distinguish the role played by advection and local erosion/settling processes in this area. Keywords: Suspended particulate matter, satellite, remote-sensing, modelling, English Channel, sediments, turbidity, tide, wave
L'étude des matières en suspension (MES) minérales est essentielle pour comprendre le fonctionnement des écosystèmes en Manche : les MES influencent la pénétration de la lumière dans la colonne d'eau, paramètre clé pour la production biologique, et sont susceptibles de transporter des polluants et nutriments. Lors de ce travail, la dynamique des MES minérales de surface en Manche est étudiée à l'aide de deux méthodes complémentaires : l'observation par satellite et la modélisation numérique tridimensionnelle. Dans un premier temps, les images satellite MODIS et MERIS, traitées par l'algorithme semi-analytique développé par l'IFREMER et représentant les MES non-algales de surface, sont analysées afin d'élaborer trois modèles statistiques permettant d'estimer la MES de surface en fonction de variables basiques telles que le coefficient de marée, la hauteur significative des vagues et la concentration moyenne en chlorophylle-a. Dans un deuxième temps, le modèle hydrosédimentaire multiclasse tridimensionnel ROMS (Regional Ocean Modeling System) est implémenté en Manche. Il prend en considération le forçage par la marée aux frontières ouvertes, la contrainte exercée par le vent à la surface de la mer, l'interaction houle-courant en couche limite de fond et l’hétérogénéité spatiale réaliste du lit sédimentaire. Les résultats du modèle statistique le plus sophistiqué sont également utilisés pour forcer la concentration en MES aux frontières ouvertes du domaine de calcul. Des tests de sensibilité sur les conditions limites montrent l'importance de considérer de manière réaliste les sédiments entrant en Manche par les frontières ouvertes lors de la modélisation numérique. L'influence de la biologie sur les MES minérales est testée en utilisant une formulation de la vitesse de chute et de la contrainte critique d'érosion variant saisonnièrement. Grâce à ces deux outils associés, les influences respectives de la marée, de la houle et de la biologie sur les MES minérales sont mises en avant et localisées en Manche. Le modèle numérique prédit que les MES de surface sont composées principalement de silts (>70%). Les silts en suspension en surface proviennent majoritairement du lit sédimentaire près des côtes en Manche orientale et des frontières ouvertes du domaine de calcul à l'ouest de la presqu'île du Cotentin et au large en Manche centrale et orientale. Les variations des MES de surface sont ensuite étudiées aux échelles des cycles de marée semi-diurnes, vive-eau/morte-eau et autour d'un épisode de houles. Enfin, l'évolution de la concentration de sédiments dans la zone de forte turbidité autour de l'île de Wight peut être analysée suivant les conditions hydrodynamiques afin d'évaluer les rôles respectifs des processus locaux d'érosion/dépot et d'advection dans la génération de ces turbidités remarquables. Mots-clés : Matière en suspension, télédétection, satellite, modélisation, Manche, sédiments, turbidité, marée, houle

Droits : 2013 UBO
http://archimer.ifremer.fr/doc/00157/26783/24884.pdf
http://archimer.ifremer.fr/doc/00157/26783/

Éditeur(s) : HAL CCSD
Résumé : International audience
In the analysis of coastal hazards, the features of extreme waves are determining information to question the impact of storms to the coast. The spatial behaviour of extreme waves is even more valuable especially since it is sparsely provided. Regarding recent applications in other contexts, a kind of statistical models called max-stable processes is relevant for modelling spatial extreme events. Max-stable processes are extensions of the well-known Generalised Extreme Value (GEV) distribution. Unlike univariate approaches, max-stable processes consider spatial dependence of a phenomenon. Such a modelling also overtakes a standard multivariate approach by providing information continuously over the area studied, even where no observation is available. Relying on such a stochastic modelling, the aim of this study is to discuss the extreme waves hazards in the Gulf of Lions, focusing on their spatial behaviour.
34th Conference on Coastal Engineering
Seoul, South Korea

lirmm-01382568
https://hal-lirmm.ccsd.cnrs.fr/lirmm-01382568
https://hal-lirmm.ccsd.cnrs.fr/lirmm-01382568/document
https://hal-lirmm.ccsd.cnrs.fr/lirmm-01382568/file/7553-31212-1-PB.pdf
DOI : 10.9753/icce.v34.management.17

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
We analyze in this study a new set of marine data including 3D local tomography, 1992-2008 relocated earthquakes and two recent multichannel seismic lines to characterize the deformation style in the collision area offshore east Taiwan. We have mapped in detail the Mohos of the converging plates as well as the subduction interface with a resolution never reached before. We show that the sharp continental subduction of the Eurasia plate, beneath the middle part of the Central Range, indents the Philippine Sea plate (PSP) as attested by intra-oceanic slicing and incipient subduction of the PSP beneath the east coast of Taiwan. The westernmost part of the PSP slab is probably experiencing a beginning of break-off as attested by NW-trending en-échelon shear zones beneath the southern slope of the southern Ryukyu arc (SRA). These en-échelon shear zones have a sinistral component favored by the "collision-free" subduction of the PSP north of 24°30′N. The down-faulting of the subduction interface forms ramps along which earthquakes clusterize. Three M7 subduction earthquakes occurred offshore Suao city along these ramps with a recurrence interval of about 40 years: 1920 Mw7.7, 1963 Mw7.2 and 2002 Mw7.1 events. The 1966 Mw6.0-7.5 earthquakes sequence likely outlines a WNW-ESE left-lateral intra-slab shear zone. The SRA upper plate accommodates the complex geometry and deformation of the subducting PSP through seismic deformation. Shallow high velocities fringing the Luzon volcanic arc (LVA) beneath the Longitudinal Valley and north of the southernmost Ryukyu forearc basins are interpreted as relics of the LVA forearc basement squeezed in the collision zone. Based on the accommodation of a large part of the convergence through shortening within the PSP and the subsequent segmentation of the shallow subduction interface, we consider that the nucleation of a Mw ≥ 8 earthquake along the southernmost Ryukyu megathrust is unlikely.
ISSN: 0040-1951

hal-00853365
https://hal.archives-ouvertes.fr/hal-00853365
https://hal.archives-ouvertes.fr/hal-00853365/document
https://hal.archives-ouvertes.fr/hal-00853365/file/publallemandifremer.pdf
DOI : 10.1016/j.tecto.2013.03.020

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
The marine Messinian deposits of Tunisia cover a narrow littoral strip some 300 km long between the northern Bizerte and Cap Bon areas and the central-eastern Sahel region. Litho- and biofacies analysis of six stratigraphic sections reveals the distinctive features of these deposits.;The lower Messinian deposits are characterized by ubiquitous siliciclastics and abundant oolitic/bioclastic limestones organized in an eastward facing ramp. Westward (landward), this ramp changes into coastal lagoons, sometimes containing evaporites. Eastward, the ramp passes to the reefal Pelagian Platform extending as far as Lampedusa.;Two main sedimentary cycles are distinguished: 1) an early Messinian siliciclastic retrogradational then oolitic/bioclastic progradational cycle (Beni Khiar Formation and lower Oued bel Khedim Formation): 2) a late Messinian brackish to continental cycle that probably accumulated in rapidly subsiding lagoons (Cued el Bir Formation and upper Oued bel Khedim Formation). The Tunisian early Messinian cycle is partly eustatically controlled, but the late Messinian cycle cannot be confidently correlated to other well-known Messinian series because of tectonic movements.;The lower Messinian deposits of Tunisia are also characterized by abundant suspension-feeding organisms (molluscs and bryozoans) and rare corals, calcareous algae, echinoids, and larger benthic foraminifers. The proposed palaeoenvironmental model shows that the lower Messinian ramp of Tunisia was located on a current-protected margin and subjected to continent-derived sediment and nutrient supply. Eastward, nutrient influx diminished and a shallow-water isolated carbonate platform with coralgal facies developed between the western and the eastern Mediterranean basins. The main hydrological connection between these two basins occurred through a narrow seaway situated to the northeast of the Pelagian Platform, south of Sicily and Malta.
ISSN: 0031-0182

hal-00475583
https://hal.archives-ouvertes.fr/hal-00475583
DOI : 10.1016/j.palaeo.2009.10.028

Éditeur(s) : IEEE
Résumé : Bathymetric estimation using remote sensing images has previously been applied to high spatial resolution imagery such as CASI, Ikonos, or SPOT but not on medium spatial resolution images (i.e., MERIS). This choice can be justified when there is a need to map the bathymetry on large areas. In this letter, we present the results of the bathymetry estimation over a large known area, the Gulf of Lion (France), expanding over 270 x 180 km.
Geoscience and Remote Sensing Letters, IEEE (1545-598X) (IEEE), 2007-04 , Vol. 4 , N. 2 , P. 274-277

Droits : 2007 IEEE
http://archimer.ifremer.fr/doc/2007/publication-2597.pdf
DOI:10.1109/LGRS.2007.890548
http://archimer.ifremer.fr/doc/00000/2597/

Éditeur(s) : Office Int Epizooties
Résumé : The tremendous development of penaeid shrimp culture across the world over the past twenty years has led to international trade in eggs, larvae and spawners of the best shrimp species for aquaculture. Trade has involved, in particular, the following species: - Penaeus japonicus from Japan to Europe, the Pacific Islands and South America - P. monodon from South-East Asia to almost all tropical countries - P. vannamei and P. stylirostris from countries along the Pacific coast of South and Central America to the United States of America, the islands of the South Pacific, countries along the Atlantic coast of the Americas and certain countries in Africa. In the 1980s, research conducted by American and French teams enabled the breeding of stocks of spawners in captivity. This resulted in the establishment of lines of captive broodstock outside natural areas of distribution, and the development of new breeding farms in previously unproductive regions. Trade related to movements of these species is facilitated by the absence of legislation in most countries; even when such legislation does exist, it is not always applied These practices have led to the rapid development of world shrimp production, but have also contributed to the dissemination of pathogens. In recent years, the occurrence of serious epizootics - occasioning heavy losses world-wide - has led to a more cautious approach involving trade of post-larvae obtained from captive broodstock in which thorough control measures have been implemented for known diseases. Trade in wild shrimp will probably be abandoned progressively, to avoid the risk of introducing new pathogens. The main challenges for research in the near future are the development of diagnostic tools, to enable continuous control of captive broodstock, and the selection of strains which are resistant to the principal pathogens affecting these species.
Revue Scientifique Et Technique-office International Des Epizooties (0253-1933) (Office Int Epizooties), 1996-06 , Vol. 15 , N. 2 , P. 499-515

Droits : info:eu-repo/semantics/openAccess
http://archimer.ifremer.fr/doc/00091/20231/17883.pdf
http://archimer.ifremer.fr/doc/00091/20231/

Éditeur(s) : Université des Antilles et de la Guyane
Résumé : Cette étude permet une approche distincte de la réflexion sur les ressources marines dans le cadre d'une aire protégée. En effet, les écosystèmes marins sont essentiels, d’autant plus, qu’ils présentent en Nouvelle-Calédonie une grande richesse, notamment en termes de patrimoine culturel. Ce sont majoritairement les Kanak qui habitent sur la Côte Est de la Province Nord, où la Collectivité et le WWF collaborent à la mise en place de plusieurs aires marines protégées (AMP). Jusqu’à présent, la gestion coutumière Kanak a permis une relative préservation de ces écosystèmes dans un secteur littoral non soumis aux pressions de l’urbanisation, du tourisme ou de la navigation. L’étude s’attache à souligner les enjeux autour de la mise en place des AMP et des perspectives de développement local, sur le milieu marin et les populations locales. Il s’agit de voir comment cette expérimentation est envisagée par les différents acteurs (État, Province Nord, associations, coutumiers etc.) et de s’interroger sur les mécanismes de gouvernance.
This study allows a distinct approach to thinking about the marine resources in a protected area. Indeed, marine ecosystems are essential, especially as they are in New Caledonia, particularly in terms of cultural heritage. It is mainly Kanak who live on the East Coast of the North Province, where the Community and WWF collaborate on the installation of several marine protected areas (MPAs). So far, the Kanak customary management allowed a relative preservation of these ecosystems in a coastal area not subject to the pressures of urbanization, tourism and navigation. The study aims to highlight the issues surrounding the establishment of MPAs and opportunities for local development on the marine environment and local populations. This is to see how this experiment is considered by the various actors (State, Northern Province, associations, etc. customary.) And to consider the mechanisms of governance.

urn:doi:10.4000/etudescaribeennes.4513
http://etudescaribeennes.revues.org/4513

Éditeur(s) : HAL CCSD Copernicus Publications on behalf of the European Geosciences Union
Résumé : International audience
The main goal of this study is to give the preliminary estimates of the tsunami risks for the Lesser Antilles. We investigated the available data of the tsunamis in the French West Indies using the historical data and catalogue of the tsunamis in the Lesser Antilles. In total, twenty-four (24) tsunamis were recorded in this area for last 400 years; sixteen (16) events of the seismic origin, five (5) events of volcanic origin and three (3) events of unknown source. Most of the tsunamigenic earthquakes (13) occurred in the Caribbean, and three tsunamis were generated during far away earthquakes (near the coasts of Portugal and Costa Rica). The estimates of tsunami risk are based on a preliminary analysis of the seismicity of the Caribbean area and the historical data of tsunamis. In particular, we investigate the occurrence of historical extreme runup tsunami data on Guadeloupe, and these data are revised after a survey in Guadeloupe.
Natural Hazards and Earth System Science

Droits : info:eu-repo/semantics/OpenAccess
hal-00330894
https://hal.archives-ouvertes.fr/hal-00330894
https://hal.archives-ouvertes.fr/hal-00330894/document
https://hal.archives-ouvertes.fr/hal-00330894/file/nhess-1-221-2001.pdf

Éditeur(s) : HAL CCSD Taylor & Francis
Résumé : International audience
Overfishing and habitat destruction due to local and global threats are undermining fisheries, biodiversity, and the long-term sustainability of tropical marine ecosystems worldwide, including in the Coral Triangle. Well-designed and effectively managed marine reserve networks can reduce local threats, and contribute to achieving multiple objectives regarding fisheries management, biodiversity conservation and adaptation to changes in climate and ocean chemistry. Previous studies provided advice regarding ecological guidelines for designing marine reserves to achieve one or two of these objectives. While there are many similarities in these guidelines, there are key differences that provide conflicting advice. Thus, there is a need to provide integrated guidelines for practitioners who wish to design marine reserves to achieve all three objectives simultaneously. Scientific advances regarding fish connectivity and recovery rates, and climate and ocean change vulnerability, also necessitate refining advice for marine reserve design. Here we review ecological considerations for marine reserve design, and provide guidelines to achieve all three objectives simultaneously regarding: habitat representation; risk spreading; protecting critical, special and unique areas; reserve size, spacing, location, and duration; protecting climate resilient areas; and minimizing and avoiding threats. In addition to applying ecological guidelines, reserves must be designed to address social and governance considerations, and be integrated within broader fisheries and coastal management regimes.
ISSN: 0892-0753

hal-01333534
https://hal-univ-perp.archives-ouvertes.fr/hal-01333534
DOI : 10.1080/08920753.2014.877763

Éditeur(s) : Pergamon-elsevier Science Ltd
Résumé : The environment is impacted by natural and anthropogenic disturbances that occur at different spatial and temporal scales, and that lead to major changes and even disequilibria when exceeding the resiliency capacities of the ecosystem. With an annual mean flow of 1700 m(3) s(-1), the Rhone River is the largest of the western Mediterranean basin. Its annual solid discharges vary between 2 and 20 Mt, with flood events responsible for more than 70% of these amounts. In the marine coastal area, close to the mouth, both flocculation and aggregation lead to the formation of fine-grained deposits, i.e. the prodelta. This area is characterized by sediment accumulation rates up to 20-50 cm yr(-1) and high accumulations of particle reactive contaminants such as various man-made radionuclides released into the river by nuclear facilities or arising form prior atmospheric nuclear tests (1954-1980) and the Chernobyl accident (April 1986). This prodelta, however, cannot be considered as a permanent repository for particle reactive pollutants since it is subjected to reworking processes. Sediment dynamics had to be linked to the influences of hydrodynamic and atmospheric events such as high flow rates or storms close to the Rhone River mouth. An experiment was carried out during the winter 2006 based on the deployment of two ADCPs and six altimeters at the Grand Rhone mouth for several months. This type of installation has never been used before in this area because of the hard meteorological conditions and the strong fishing activities. However, results showed pluricentimetric rises of the sedimentary level just after river flood events and decreases during storms, generated by southeast winds. Radiotracers and grain size depth profiles helped to characterise the studied events and to establish inventories of sediments and radionuclides. A cruise (CARMEX) was carried out during this same period to collect water samples, suspended particles and sediment cores. The results enabled us to link both river flow and wind characteristics to events recorded on the sea floor, i.e. resuspension, accumulation, consolidation, etc. Deposits of 11 cm of sediments were estimated during flood periods and bottom shear stresses up to 5 N m(-2) were calculated during sediment erosion phases. (C) 2010 Elsevier Ltd. All rights reserved.
Continental Shelf Research (0278-4343) (Pergamon-elsevier Science Ltd), 2010-05 , Vol. 30 , N. 9 , P. 1095-1107

Droits : 2010 Elsevier B.V. All rights reserved.
http://archimer.ifremer.fr/doc/00006/11695/8479.pdf
DOI:10.1016/j.csr.2010.02.015
http://archimer.ifremer.fr/doc/00006/11695/