Éditeur(s) : ISTPM
Résumé : Shell is the basis of the distinction between the different species of molluscs. But the elements defining the shape and colour of the shell can vary according to the environmental conditions. So much so that, in numerous cases, a whole range of intermediates can be found between two species. Among molluscs, oysters are considered as a particularly confused group. Their shells are indeed extremely variable. All sorts of intermediates can be found. They usually attach themselves using their bottom valve, and, depending on the shape of the substrate, salinity conditions, temperature, outside environment, they present a wide range of individual variations. I had the opportunity to examine the larval shells of some of our coastal species. I noticed that each species had a specific prodissoconch, with a constant shape and no fundamental individual variations, an understandable fact given their planktonic life. The hinge and the position of the ligament in the hinge enable the definition of their genus. During the study of the collections of oysters from some of the world's most renowned museum (1), I tried to isolate the prodissoconches of the different species. I found them attached to the adult shells, making sure that all the prodissoconches attached to the top of the adult shells showed the same morphological characteristics. (unverified OCR)
LAMARCK, en 1806, dans l'ouverture de son Cours sur les «Animaux sans Vertèbres», s'exprimait ainsi : «En attendant, souvenons-nous que rien de tout cela n'est dans la nature, qu'elle ne connaît ni Classes, ni Ordres, ni Genres, ni Espèces, malgré le fondement que paraissent leur donner les portions de la série naturelle que nous offrent nos collections et que parmi les corps organisés, il n'y a réellement que des individus et des races diverses qui se nuancent dans tous les degrés de l'organisation. » Ainsi, pour LAMARCK, les cadres de la Classification zoologique seraient artificiels, ce seraient des créations de l'esprit, ayant seulement pour but de faciliter l'étude du monde vivant. Effectivement lorsqu'on consulte, comme je l'ai fait, les «Collections Lamarck» des Musées de Paris et de Genève. on s'aperçoit que, pour LAMARCK, le moindre caractère morphologique qui différencie une coquille de Mollusque d'une autre est une entité. Il multipliait le nombre des espèces et créait des variétés. Pour CUVIER (2) : «Le travail des nomenclatures, besogne facile, qui ne demande aucune intelligence a fait négliger la science véritable.» Et dit-il, ailleurs (:1) : «Après tout je n'ai pas jeté cette esquisse de division pour servir aux commençans à trouver les noms des espèces; qu'ils emploient pour cela tel système artificiel qu'ils trouveront le plus facile; cela est juste... » Les systèmes en question ne seraient donc que jeux de l'esprit, pour CUVIER également. Notre pensée a beaucoup évolué depuis cette époque. Nous pouvons dire maintenant que la Vie est la manière d'être des protéines et qu'il existe autant de protéines que d'espèces. Dès 1912, Jacques LOEB disait (4) : «Qu'en toute certitude, chaque animal a des substances germinatives spécifiques et que les substances germinatives diffèrent chimiquement d'un animal à l'autre, Les qualités chimiques d'un oeuf de poulet font qu'il ne peut donner naissance qu'à un poulet.» La notion d'espèce chimique vivante nous entraîne, par ailleurs, vers une nouvelle conception des autres groupes de la classification. L'individu porteur de caractères particuliers par lesquels il peut seulement être défini, est aussi porteur d'un noyau protoplasmique spécifique et enfin d'autres, propres successivement à la famille, à l'ordre, à la classe et à l'embranchement dont il fait partie. Cela est très important, car toutes ces catégories de la classification zoologique ne nous apparaissent plus alors comme de simples entités, subjectives, formelles, mais comme ayant effectivement une réalité précise dans le monde extérieur. La recherche et la définition correcte des espèces apparaissent alors comme un travail de première importance. Lorsqu'on poursuit des recherches embryologiques, physiologiques, biologiques ou autres sur un organisme, il est indispensable de savoir d'une manière précise en présence de quelle espèce on se trouve. Par ailleurs, comment parler de l'évolution des espèces si leur existence objective n'est pas admise et si elles ne sont pas correctement définies? Toute l'histoire de la Zoologie est marquée par l'effort constant de préciser les caractères de l'espèce et d'en faire une réalité objective. Chez les Mollusques, la coquille a servi de base essentielle pour la distinction des espèces. Mais les éléments de la forme et de la couleur de la coquille varient avec les conditions du milieu de telle sorte qu'on trouve dans de nombreux cas, tous les intermédiaires entre deux espèces. Parmi les Mollusques, les Huîtres constituaient un groupe particulièrement confus. En effet, leurs coquilles sont extrêmement variables. On rencontre tous les intermédiaires. Elles se fixent le plus souvent sur un support par la valve inférieure et là selon la forme du support, selon les conditions de la salinité, de la température, du milieu extérieur, elles présentent une immense gamme de variations individuelles. J'ai été amené à examiner les coquilles larvaires de quelques espèces de nos côtes. J'ai constaté que chaque espèce avait une prodissoconque particulière, d'une forme constante et sans variations individuelles fondamentales ce qui se conçoit aisément, étant donné leur vie planctonique. Leur charnière et la position du ligament par rapport à cette dernière, permettent de définir les genres, En étudiant les collections d'Huîtres des grands musées du monde (1), j'ai cherché à isoler les prodissoconques des diverses espèces. Je les ai trouvées sur les coquilles adultes où elles s'étaient fixées. m'assurant chaque fois que les prodissoconques conservées au sommet des coquilles adultes présentaient les mêmes caractéristiques morphologiques. J'ai microphotographié la plupart des coquilles larvaires étudiées. Ce sont les épreuves qui sont reproduites ici. J'en ai fait faire des dessins au trait et pour quelques-unes dont les microphotographies manquent, on trouvera les dessins au trait réalisé à la chambre claire. Chaque espèce est bien définie par sa coquille larvaire. La meilleure démonstration en est fournie par les deux espèces. si voisines par leurs coquilles adultes, Ostrea edulis et Ostrea chilensis; leurs prodissoconques sont spectaculairement différentes. Je remercie Monsieur le Directeur de l'Institut scientifique et technique des Pêches maritimes qui a bien voulu accepter de publier le résultat de ces recherches dans la belle Revue des Travaux de son Institut. (OCR non contrôlé)
Revue des Travaux de l'Institut des Pêches Maritimes (0035-2276) (ISTPM), 1967-06 , Vol. 31 , N. 2 , P. 127-199

Droits : Ifremer
http://archimer.ifremer.fr/doc/1967/publication-3761.pdf
http://archimer.ifremer.fr/doc/00000/3761/

Éditeur(s) : HAL CCSD Hong Kong : World Academic Publishing
Résumé : International audience
In automatic image analysis, when using natural images, it is important to select the elements in a scene that can lead to correct characterization. Extraneous elements can result in poor values in the parameter evaluation for recognition. Irrelevant elements also increase the processing time, because they can be used incorrectly by the algorithms for characterization or identification. The goal of this paper is to offer identification algorithms and characterizations that will allow effective recognition. We base our procedure on the photographer focus areas to identify those relevant elements in a scene. In this work, we propose a procedure to select the relevant shape from natural images. The treatment uses focal depth with edge detectors. The resulting points are combined with a region partition to obtain relevant shapes.
ISSN: 2309-0650

hal-01278550
https://hal.archives-ouvertes.fr/hal-01278550

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
The paper presents coastal structures design in the presence of waves by the minimization of a cost function. It aims to show that shape optimization can be efficiently applied to ocean engineering. This is an underlying guiding principle for the design of harbors or offshore breakwaters. We compute the solution of a specific simplified boundary value problem describing the short wave propagation toward a vertical sea cliff or vertical wall and modify accordingly the shape of defense structures in order to minimize a pre-defined cost function taking into account the strength (energy) of the water waves. The optimization procedure relies on a global semi-deterministic search algorithm able to escape from local minima.
ISSN: 0378-3839

hal-00411905
https://hal.archives-ouvertes.fr/hal-00411905
DOI : 10.1016/j.coastaleng.2007.06.006

Éditeur(s) : HAL CCSD
Résumé : In Taiwan , the subduction of the Chinese continental margin under the Luzon arc results in the progressive growth of an active orogenic wedge. It is one of the best places to study the complex relationships that occurs between the tectonic processes controlling deformation (plate rheology and kinematics, metamorphism and magmatism) and surface processes (erosion and sedimentation). In order to study the kinematics of the present day convergence of Philippine Sea plate to the Asian continent around Taiwan, we perform 2D and 3D sandbox modeling and we analyzed the models with PIV (Particle Image Velocimetry) software. In 2D experiments, a model Coulomb wedge is submitted to erosion and sedimentation under topography and flux steady state conditions. The 3D experiments are mainly used to study the escape tectonics occurring in the middle west and southwest Taiwan. A wedge shaped indenter and a basement relief were used to simulate the mechanical plate boundary between Philippine Sea plate and Eurasia plate and the basement topography to the west of Taiwan respectively. We examine the exhumation patterns, the mode of fault propagation and displacement patterns by strain partitioning of vertical vs. horizontal displacement and convergent parallel vs. orogen parallel components. The preliminary conclusions are: 1. The interactions between tectonics, erosion and sedimentation control geometry and kinematics of the doubly vergent transpressional orogen. 2. Exhumation processes are controlled by the balance between erosion, frontal accretion and underplating in different structural domains of the wedge. 3. Retrowedge erosion favorites backfolding and backthrusting, induces flower structures and fan shaped cleavage distribution. 4. Sedimentation promotes underplating and out-of sequences thrusting. 5. Continental subduction or subduction of topographic highs will enhance underthrusting/underplating, thick-skin tectonics and inversion of sedimentary basin.
Bolletino di Geofisica teorica ed applicata

hal-00411133
https://hal.archives-ouvertes.fr/hal-00411133

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
The nucleation and growth processes of spherulitic alkali feldspar have been investigated in this study through X-ray microtomography and electron backscatter diffraction (EBSD) data. Here we present the first data on Shape Preferred Orientation (SPO) and Crystal Preferred Orientation (CPO) of alkali feldspar within spherulites. The analysis of synchrotron X-ray microtomography and EBSD datasets allowed us to study the morphometric characteristics of spherulites in trachytic melts in quantitative fashion, highlighting the three-dimensional shape, preferred orientation, branching of lamellae and crystal twinning, providing insights about the nucleation mechanism involved in the crystallization of the spherulites. The nucleation starts with a heterogeneous nucleus (pre-existing crystal or bubble) and subsequently it evolves forming “bow tie” morphologies, reaching radially spherulitic shapes in few hours. Since each lamella within spherulite is also twinned, these synthetic spherulites cannot be considered as single nuclei but crystal aggregates originated by heterogeneous nucleation. A twin boundary may have a lower energy than general crystal–crystal boundaries and many of the twinned grains show evidence of strong local bending which, combined with twin plane, creates local sites for heterogeneous nucleation.This study shows that the growth rates of the lamellae (10− 6–10− 7 cm/s) in spherulites are either similar or slightly higher than that for single crystals by up to one order of magnitude. Furthermore, the highest volumetric growth rates (10− 11–10− 12 cm3/s) show that the alkali feldspar within spherulites can grow fast reaching a volumetric size of ~ 10 μm3 in 1 s.
ISSN: 0024-4937

hal-01172356
https://hal.archives-ouvertes.fr/hal-01172356
DOI : 10.1016/j.lithos.2014.12.003

Éditeur(s) : AGU
Résumé : Submarine canyons are narrow but deep submarine valleys that extend for hundreds of meters. They represent the most impressive structures that shape the present morphology of passive continental margins. They can occur off the mouth of rivers: the Tagus, Zaire, Amazon, and Orinoco in the Atlantic; the Indus in the Indian Ocean; and the Var, Rhone, and Ebro in the Mediterranean. Some are at times disconnected from any stream mouth such as the Nazare canyon, off Portugal, despite the fact that it is close to the coast. Some were connected to a river mouth during lowstands of sea level, such as the Wilmington canyon in the northwest Atlantic, or the Blackmud canyon in the northeast Atlantic.
EOS, Transactions American Geophysical Union (0096-3941) (AGU), 2004-07-06 , Vol. 85 , N. 27 , P. 257

Droits : 2004 AGU
http://archimer.ifremer.fr/doc/00071/18201/15769.pdf
DOI:10.1029/2004EO270001
http://archimer.ifremer.fr/doc/00071/18201/

Éditeur(s) : HAL CCSD Royal Society, The
Résumé : International audience
Many studies have focused on the impacts of climate change on biological assemblages, yet little is known about how climate interacts with other major anthropogenic influences on biodiversity, such as habitat disturbance. Using a unique global database of 1128 local ant assemblages , we examined whether climate mediates the effects of habitat disturbance on assemblage structure at a global scale. Species richness and evenness were associated positively with temperature, and negatively with disturbance. However, the interaction among temperature, precipitation and disturbance shaped species richness and evenness. The effect was manifested through a failure of species richness to increase substantially with temperature in transformed habitats at low precipitation. At low precipitation levels, evenness increased with temperature in undisturbed sites, peaked at medium temperatures in disturbed sites and remained low in transformed sites. In warmer climates with lower rainfall, the effects of increasing disturbance on species richness and evenness were akin to decreases in temperature of up to 98C. Anthropogenic disturbance and ongoing climate change may interact in complicated ways to shape the structure of assemblages, with hot, arid environments likely to be at greatest risk.
ISSN: 0962-8452

hal-01323255
https://hal.archives-ouvertes.fr/hal-01323255
DOI : 10.1098/rspb.2015.0418

Éditeur(s) : HAL CCSD Wiley
Résumé : International audience
Large-scale conical and saucer-shaped sand injectites have been identified in the Upper Miocene sediments of the Lower Congo Basin. These structures are evidenced on the 3D high-resolution seismic data at about 600 ms TWT (two-way traveltime) beneath the seabed. The conical and saucer-shaped anomalies range from 20 to 80 m in height, 50 to 300 m in diameter, and 10 to 20 ms TWT in thickness. They are located within a sedimentary interval of about 100 m in thickness and are aligned over 20 km in dip direction (NE-SW), above the NW margin of an underlying Upper Miocene submarine fan. We have interpreted the conical and saucer-shaped anomalies as upward-emplaced sand injectites sourced from the Upper Miocene fan because of their discordant character, the postsedimentary uplifting of the sediments overlying the cones and saucer-shaped bodies, the alignment with the lateral fringe of the Upper Miocene submarine fan, and the geological context. Sand injection dates from the Miocene-Pliocene transition (approximately 5.3 Ma). The prerequisite overpressure to the sand injection process may be due to the buoyancy effect of hydrocarbons accumulated in the margins of the fan. Additionally, overpressure could have been enhanced by the lateral transfer of fluids operating in the inclined margins of the lobe. The short duration of sand injection and the presence of many sandstone intrusions suggested that the process of injection was triggered by an event, likely due to a nearby fault displacement related to diapiric movements. This is the first time that sand injectites of seismic scale have been described from the Lower Congo Basin. The localized nature of these injectites has led to a change in the migration path of fluids through the sedimentary cover. Consequently, the sand intrusions are both evidence and vectors of fluid migration within the basin fill.
ISSN: 1468-8115

hal-00963594
https://hal.archives-ouvertes.fr/hal-00963594
DOI : 10.1111/gfl.12057

Éditeur(s) : Taylor & Francis Ltd
Résumé : A new benthic phototrophic dinoflagellate is described from sediments of a tropical marine cove at Martinique Island and its micromorphology is studied by means of light and electron microscopy. The cell contains small golden-brown chloroplasts and the oval nucleus is posterior. It is laterally compressed, almost circular in shape when viewed laterally. It consists of a small epitheca tilted toward the right lateral side and a larger hypotheca. In the left view, the cingulum is more anterior and the epitheca is reduced. The cingulum is displaced and left-handed. This organism is peculiar in having no apical pore and its thecal plate arrangement is 2 ' 1a 7 '' 5c 3s 5 ''' 1 ''''. The plates are smooth with small groups of pores scattered on their surface. An area with 60-80 densely arranged pores is found near the centre of the 2 ''' plate, on the left lateral side. Morphologically, these features are different from all other laterally compressed benthic genera. In addition, molecular genetic sequences of SSU and partial LSU form a distinct and well-supported clade among dinoflagellates and support the erection of a new genus. However, molecular phylogenies inferred from ribosomal genes failed to confirm any clear relationship with other benthic taxa and affinity with other laterally compressed dinoflagellates has not been demonstrated. Hence, the taxonomic affinity of Madanidinium loirii with a defined order and family is unclear at the moment.
European Journal Of Phycology (0967-0262) (Taylor & Francis Ltd), 2014-04 , Vol. 49 , N. 2 , P. 165-178

Droits : 2014 British Phycological Society
http://archimer.ifremer.fr/doc/00195/30622/29458.pdf
DOI:10.1080/09670262.2014.898797
http://archimer.ifremer.fr/doc/00195/30622/

Éditeur(s) : HAL CCSD Oxford University Press (OUP)
Résumé : International audience
The diffusion of titanium along with Ni, Co and Mn in pure synthetic forsterite has been studied as a function of temperature, oxygen fugacity, crystallographic orientation and chemical potentials in the four-component system MgO–SiO2–TiO2–TiO1·5. In over 100 different experimental conditions, no Ti diffusion profiles with the classical shape of the error function were observed. Instead, the profiles vary between ‘stepped’ at high fO2 (probably owing to diffusion on octahedral sites and trapping in tetrahedral sites), to hockey-stick shapes at low fO2 owing to concentration-dependent diffusion. The profile shapes vary systematically between these end-members according to oxygen fugacity. These profile shapes are also reproduced in experiments using natural San Carlos olivine. The change in profile shape is interpreted to be a function of valence-state change from Ti4+ to Ti3+, shown by a sigmoidal log fO2–diffusivity relationship. To distinguish between Ti4+ and Ti3+ in forsterite, a diffusion profile was also investigated using ‘hydroxylation spectroscopy’ whereby a crystal from a diffusion experiment was hydroxylated by annealing in an H2O-rich fluid at moderate pressure and temperature. The point defects associated with the added structural OH were then determined by infrared spectroscopy, providing evidence for the presence of Ti4+ and Ti3+ at intermediate oxygen fugacity. The transition from Ti4+ to Ti3+ occurs at considerably higher fO2 in these diffusion experiments than in equilibrium experiments in similar systems. Titanium diffusion, qualified using a mobility parameter (M), is fastest along the c-axis, at high activity of silica, low oxygen fugacity and high temperature. The rate of Ti diffusion is broadly similar to those of Mn, Ni and Co, and closer to published rates of Mg self-diffusion in olivine than Si self-diffusion. The observed Ti3+ and Ti4+ diffusion occurs on the M-sites. From statistical examination of the large Mn, Ni and Co diffusivity dataset, we determine that there is a 102/3 dependence of diffusion on aSiO2; the cations diffuse more rapidly at high aSiO2. In addition, diffusivity has a 10–1/8 dependence on fO2, suggested to be the result of increased concentration of loosely bound Ti3+–vacancy pairs, which enhance the mobility of other cations. This behaviour is likely to be present in natural systems where trivalent (e.g. Fe3+, Al3+, Cr3+) and divalent cations diffuse together. Consideration should be given to diffusive interference by highly charged, fast-moving cations when extracting time scales from frozen diffusion profiles.
ISSN: 0022-3530

hal-01531344
https://hal.archives-ouvertes.fr/hal-01531344
DOI : 10.1093/petrology/egw067

Éditeur(s) : HAL CCSD American Geophysical Union
Résumé : A differential effective medium (DEM) model is used to predict elastic properties for a set of porous and anisotropic aggregates, comprised of mixtures of calcite and muscovite. The DEM takes into consideration an anisotropic background medium with triclinic or higher symmetry, in which inclusions of idealized ellipsoidal shape are added incrementally. In general, the calculated elastic properties of a solid that contains inclusions representing "dry" pores/cracks are strongly dependent on the orientation and aspect ratio of the inclusions. Aspect ratios of inclusions in the synthetic aggregates, which consist of air-filled pores, are estimated from anisotropy of magnetic susceptibility (AMS) of samples whose pore space has been impregnated with a colloidal ferrofluid. The AMS derived pore shape geometry is used as an input value for inclusions in the DEM. Modeling results are compared with laboratory determined elastic properties, measured with ultrasonic waves. Calculated shear wave velocities agree in general well with laboratory measured S wave velocities, whereas calculated P wave velocities are typically 0.5-1.1 km/s higher than measured values. Differences between calculated and measured P wave velocities are attributed mainly to incomplete and biased ferrofluid saturation of pores. Spherical pores are preferably filled during imbibition, in comparison to thin cracks, which leads to overprediction of the calculated P wave velocities. The amount of ferrofluid that fills the pore space is dependent on the ratio of calcite to muscovite and the load used for compaction during sample synthesis. The permeability decreases with increasing muscovite content and increasing compaction load. Incomplete saturation of samples with high-muscovite content is confirmed by X-ray microtomography density contrast imaging of dry and ferrofluid saturated specimens.
ISSN: 0148-0227

hal-00617717
https://hal.archives-ouvertes.fr/hal-00617717
DOI : 10.1029/2010JB007750

Éditeur(s) : HAL CCSD American Institute of Mathematical Sciences
Résumé : International audience
In this paper, shape optimization tools are applied to coastal engineering. A barred beach protection study is described, using a new type of water wave attenuator device, namely geotextile tube, to reduce the mobilization of sediments. A global optimization algorithm, able to pursue beyond local minima, is used to search for the optimum properties of the geotextile tube. The optimal configuration is then post-validated for generated currents.
ISSN: 1531-3492

hal-00475636
https://hal.archives-ouvertes.fr/hal-00475636
DOI : 10.3934/dcdsb.2010.13.759

Résumé : Cette thèse traite de la problématique de l'analyse automatique de tracés manuscrits réalisés à mains levée, à caractère géométrique et acquis en ligne. Lorsque l'on analyse un tracé en ligne, on peut le faire selon plusieurs angles. Comme pour les tracés hors ligne, on peu s'atteler à reconnaitre la forme produite. Mais le caractère en ligne de l'acquisition permet également d'autres niveaux d'analyse, comme l'analyse de la procédure utilisée par le dessinateur lors de la production de son dessin. Nous avons dans le cadre de ce travail élaboré des outils permettant de telles analyses de la production de tracé. Dans une première partie nous traitons des pré traitements à effectuer sur le tracé afin de pouvoir procéder aux analyses spatio-graphique et procédurale. Ces pré traitements sont le filtrage, la segmentation mixte à base d'arcs de cercles et de segments de droite, la sélection des points d'intérêt ainsi que l'identification de la nature de ces points. La seconde partie concerne l'analyse visuo-spatiale. Nous abordons alors deux aspects: la question de la reconnaissance des formes et celle de l'évaluation automatique de leur qualité. Notre contribution consiste en une méthode de reconnaissance basée sur l'apparence utilisant des descripteurs locaux. La dernière partie traite de l'analyse procédurale. Nous proposons une méthode d'extraction et de modélisation de la procédure mise en œuvre lors du dessin d'une forme. Nous montrons comment en utilisant cette modélisation, nous pouvons non seulement déterminer la procédure favorite d'un utilisateur mais également reconnaitre un dessinateur par l'analyse de sa procédure.
This thesis handles the problem of the automatic analysis of online hand drawn geometric sketches. An online sketch can be analysed according to several points of view. As for offline sketching, we can try to recognize the produced shape. However, online sketching allows other levels of analysis. For example the analysis of the behavior of the drawer during the production of the sketch. In this thesis, we have tried to develop tools allowing a multi level analysis, including both shape and behavior analysis. The first part of our work deals with the pre treatments that must be performed on the sketch in order to allow upper level analysis. Those pre treatments are filtering, mixed segmentation and feature points detection and labelisation. In the second part, we approach shape analysis in two aspects: shape recognition and evaluation. We have developed a appearance based method which use local descriptors to allows both recognition and evaluation of the quality of a produced shape compared to the model . in the last part we propose a method for drawer's behavior extraction and modeling. Then we show how we can not only determine the favorite procedure of a drawer but also recognize the drawer by analyzing his behavior.

http://www.theses.fr/2010AGUY0394/document

Éditeur(s) : Gauthier-Villars
Résumé : The variability of ''yellow substance'' in waters of the Skagerrak and the Kattegat was studied during the international Skagex programme in 1990 and 1991. Data on attenuation of light and fluorescence of dissolved organic matter (DOM) in sea water were collected with a spectral transmissiometer and a submersible fluorometer within a depth range of 0-250 m at several stations. More than fifty-fold variations of fluorescence intensity over space and time were due to the combined action of different sources of DOM in the straits. The surface maximum of fluorescing DOM, related to river outflow, was spreading from Oslo fjord to the central Skagerrak in late spring. This maximum may be ecologically important because it diminishes shortwave PAR. In the autumn the brightest DOM fluorescence was found in the Kattegat and along the Norwegian coast in accordance with earlier studies. The local minima of DOM fluorescence are associated with the Jutland current. Both the instability of the current and a ten-fold difference in DOM content between deep layers of the Skagerrak and Kattegat resulted in strong synoptic variability of fluorescence in the transitional area between the straits. Seasonal and synoptic variabilities of ''yellow substance'' were minimal in the southern Kattegat. The vertical gradients of DOM fluorescence were mostly negative at the depth of the thermocline of the open Skagerrak in spring, reaching values of 40-50 % m-1. Fine structure and complex shape were inherent to fluorescence profiles from areas of intensive water mixing. DOM fluorescence closely covaried with attenuation of UV light: the correlation coefficient was + 0.9 for wavelength w <= 350 nm regardless of season. The inverse dependence between wavelength derivative and magnitude of UV attenuation in the straits did not change with season. DOM fluorescence and water salinity were negatively correlated at depths of 25-50 m but they varied independently in the upper 10 m. No significant correlation between fluorescence and nitrates has been found. Estimates of correlation with phosphates ranged from 0.7 to 0.8. In general, the changes of fluorescence were due to variations of DOM content in sea water but not to variability of DOM composition or state. The properties of DOM fluorescence in the Skagerrak-Kattegat area make it a useful natural tracer of water movements suitable for active remote sensing with airborne lidar.
Oceanologica Acta (0399-1784) (Gauthier-Villars), 1993 , Vol. 16 , N. 2 , P. 115-125

Droits : info:eu-repo/semantics/openAccess
http://archimer.ifremer.fr/doc/00099/21041/18667.pdf
http://archimer.ifremer.fr/doc/00099/21041/

Éditeur(s) : Elsevier
Résumé : During the Fanindien 2006 cruise of R/V 'Beautemps-Beaupre', high resolution multibeam bathymetry, sub-bottom profiling and sediment coring was carried out along the East African margin, offshore Tanzania and Mozambique (Indian Ocean). The newly acquired data reveal the presence of a giant deep-sea valley (the Tanzania channel) that is more than 10 km wide at 4000 m water depth, along the continental rise. The valley remains similar to 70 m deep and 7 km wide at 800 km from the Tanzania coast. Morphological comparison with worldwide submarine channels show that the Tanzania channel is one of the largest known submarine valleys. This discovery brings new light on development of submarine valleys that drain sediments originated from the East African Rift System (EARS) highlands (i.e. the Tanzania channel and its neighbor Zambezi channel located similar to 1000 km southward). Both of the systems have a morphology markedly different to the classical sinuous, V-shaped channels located at similar latitudes (e.g. the Zaire or Amazon channels). Their submarine drainage system consists of a downslope converging tributary canyons joining a central trunk channel in the continental rise. The presence of such giant deep-sea drainage systems is probably linked to a strong structural control on the sediment pathway, associated to a massive sediment transfer towards the Indian Ocean in relation with the tectonic activity of the East African Rift System (i.e. the uplift periods trough mid-Miocene and Plio-Pleistocene times) and its interplay with the East African equatorial climate changes.
Marine Geology (0025-3227) (Elsevier), 2008-12 , Vol. 255 , N. 3-4 , P. 179-185

Droits : 2008 Elsevier B.V. All rights reserved.
http://archimer.ifremer.fr/doc/00324/43491/42958.pdf
DOI:10.1016/j.margeo.2008.09.002
http://archimer.ifremer.fr/doc/00324/43491/

Éditeur(s) : Actes de colloques. Ifremer Brest [ACTES COLLOQ. IFREMER.]. 1986
Résumé : Bacterial density of the coelenteric fluid (CF) of some anthozoan species was determined in situ and under laboratory conditions. In all species examined bacterial density of the CF was higher in the gastral cavity than in ambient ranging from 10 super(5) up to 5 x 10 super(6) cells. ml super(-1). Incubation experiments with the CF indicate that a bacterial population within the coelenteron is efficiently controlled by the CF, favoring bacterial growth if bacterial densities are low in the CF and showing clearance activity at high bacterial densities. Feeding of pre-starved anthozoans caused a rapid response of coelenteric rod-shaped bacteria. Evidence is presented that coelenteric bacteria are digested periodically although they contribute 1% to the respiratory carbon losses of the antozoans tested. Therefore, it is more likely that the coelenteric bacterial population provide other substances which cannot be synthesized by the host.
La densité des bactéries du fluide gastrique de différents anthozoaires a été déterminée in situ et au laboratoire. Pour toutes les espèces étudiées, la densité des bactéries dans le fluide gastrique était plus élevée que dans l'eau ambiante et comprise entre 105et 106 cellules m"1. Des expériences d'incubation du fluide gastrique montrent que la population bactérienne est contrôlée efficacement par ce fluide gastrique, favorisant la croissance de bactéries lorsque la densité est faible mais révélant des activités de digestion lorsque la densité est élevée. En nourrissant des anthozoaires mis àjeun plusieurs jours, on provoque une réaction rapide des bactéries déforme bacillaire. Certaines observations montrent que les bactéries gastriques se développent et sont digérées par cycle dans le coelenteron. Néanmoins, la contribution en carbone de ces dernières, comparée aux pertes d'énergie par Sa respiration, représenterait moins de i ','-£. li est probable que cette population bactérienne fournisse des substances qui ne peuvent être synthétisées par i'hôte.

Droits : info:eu-repo/semantics/openAccess
http://archimer.ifremer.fr/doc/1984/acte-989.pdf
http://archimer.ifremer.fr/doc/00000/989/

Éditeur(s) : Université des Antilles Études caribéennes
Résumé : La question que pose cet article est : comment un individu cosmopolite, à partir du geste réflexif de s’éprouver dans le regard de l’autre, peut-il saisir et se représenter son appartenance à une commune humanité ? Nous proposons que la socialisation cosmopolite soit intimement liée à la nature du groupe d’accueil dans lequel se fait l’immersion dans un ailleurs. Or, cette rencontre ne peut se faire avec l’humanité en général, mais elle prend forme dans l’interrelation entre deux ou plusieurs entités culturelles spécifiques. Ce qui nous ouvre à d’autres questions : de quelle altérité parle-t-on ? Pour qui ? Pourquoi ? Pour quoi ? De ce fait, le sentiment d’appartenance à une commune humanité, s’il est, au moins dans une certaine mesure, partagé par tout individu cosmopolite, l’est à entendre d’un point de vue utopique. Si la socialisation cosmopolite dans des enclaves backpacker ou des dispositifs d’échanges universitaires est réalisée dans une logique d’intégration principalement dirigée vers une communauté occidentale cosmopolite, une autre forme de socialisation, par l’expérience de la grande itinérance, serait ainsi possible. Cette dernière serait immergée dans les cultures locales, elle serait éphémère, aléatoire, hétérogène et principalement réalisée dans le rite des hospitalités, et peut ainsi représenter une forme différente d’élaboration du sentiment cosmopolite. En effet, celle-ci ne serait pas élaborée dans la tension entre deux modèles (intégration), mais dans une réaction en chaine de multiples modèles, qui, par sérendipités, se travaillent les unes les autres, dans de multiples directions, sans pouvoir se fixer, ouvrant ainsi à la diversité de l’humanité. S’il faut ici parler de socialisation cosmopolite, elle serait plutôt à entendre sur le plan anthropologique qu’ethnologique.
The question raised by this article is: how a cosmopolitan individual, from the reflective gesture of experiencing himself in the gaze of the other, can grasp and represent his belonging to a common humanity. We propose that cosmopolitan socialization be intimately linked to the nature of the host group in which the immersion takes place. However, this encounter cannot be made with humanity in general, but it takes shape in the interrelationship between two or more specific cultural entities. What opens us to others questions: what kind of otherness are we talking about? For whom? Why? In which purpose? As a result, the feeling of belonging to a common humanity, if it is shared, at least to some extent, by each cosmopolitan individual, is to be understood from a utopian point of view. If cosmopolitan socialization in backpacker enclaves or academic exchanges is carried out in the logic of integration mainly directed towards a cosmopolitan Western community, then another form of socialization through the experience of itinerancy would be possible. The latter would be immersed in local cultures, it would be ephemeral, random and heterogeneous and mainly carried out in the rite of hospitalities, and may thus represent a different form of elaboration of cosmopolitan feeling. Indeed, this would not be elaborated in the tension between two models (integration), but in a chain reaction of multiple models, which by serendipities, work one another, in multiple directions, without being able to stabilized, opening to the diversity of humanity. If we speak here of cosmopolitan socialization, it would rather be understood on the anthropological level than on an ethnological one.

Droits : info:eu-repo/semantics/openAccess
urn:doi:10.4000/etudescaribeennes.11283
http://journals.openedition.org/etudescaribeennes/11283

Éditeur(s) : Taylor and Francis
Résumé : A new sand-dwelling dinoflagellate species, Cabra reticulata sp. nov., is described from sandy habitats in the south of Brittany (northwestern France). This new species possesses the characteristics of the 'unusual' genus, Cabra Murray et Patterson. The thecal plate formula is Po Pt 3' 1a 4'' 'x' 3c ?s 5''' 1'''' (or alternatively interpreted as Po Pt 4' 0a 4'' 'x' 3c ?s 5''' 1''''). Because of the strong lateral compression, cells of C. reticulata are frequently seen laterally and have a polygonal shape, with three prominent antapical pointed flanges and a dorsal spine in the anterior part of the hypotheca. The cingulum is ascending and incomplete. The thecal surface is ornamented with strong reticulations forming polygonal areolae, which differs from C. matta Murray et Patterson, the type species of the genus. In addition to their different size and shape, a detailed study of C. reticulata by scanning electron microscopy also revealed several different plate features. Plates of the cingulum, c1 and c3, have no reticulations and are ornamented with shallow round areolae, while c2 is only faintly reticulated. Plate 1'''' is also characteristic because dorsally it forms a prominent pointed flange and ventrally bears a peculiar small area of densely arranged pores or tiny areolae. A similar finding has previously been described in Roscoffia capitata Balech. In the description of the genus, it was suggested that Cabra is closely related to species of the genus Roscoffia, and our observations strengthen this hypothesis. Prior to this study, C. reticulata was probably observed in the Virgin Islands, Caribbean Sea, but was tentatively identified as Thecadinium sp. and not fully described. Thus, C. reticulata appears to be present on both sides of the Atlantic Ocean and to occupy benthic habitats in temperate and tropical areas.
European journal of phycology (0967-0262) (Taylor and Francis), 2009-08 , Vol. 44 , N. 3 , P. 415-423

Droits : 2009 Informa plc, Taylor & Francis
http://archimer.ifremer.fr/doc/2009/publication-6804.pdf
DOI:10.1080/09670260902883271
http://archimer.ifremer.fr/doc/00000/6804/

Éditeur(s) : Wiley / Blackwell
Résumé : A new marine benthic Prorocentrum species from sandy habitats of South Brittany (northwestern France), P. consutum sp. nov., is described using LM and SEM and molecular phylogenetic analyses. Cells have a subcircular to broadly ovoid shape and are plainly flattened. They are 57-61 lm long and 52-55 lm wide. A central pyrenoid is present, and the kidney-shaped nucleus is positioned in the posterior region. In right valve view, the periflagellar area is deeply excavated, and the left valve forms a prominent apical ridge. The periflagellar area consists of nine platelets, and a small narrow collar is present around the flagellar pore. The ornamentation of this new species is very peculiar and is characterized by a ring of round areolae located at the periphery of the valves, each areola containing three or four pores. Apart from this ring of areolae, the cell surface is smooth and with scattered pores. Pores are not present in the center of the right or left valve. The intercalary band is generally narrow and faintly striated horizontally. The molecular phylogenetic position of P. consutum sp. nov. was inferred using SSU and LSU rDNA. In both analyses, this species branched with high support in the clade comprising species with a symmetric shape and appeared to be a sister group to that formed by P. lima and other tropical benthic species, such as P. arenarium, P. belizeanum, P. hoffmannianum, and P. maculosum.
Journal of Phycology (0022-3646) (Wiley / Blackwell), 2010-02 , Vol. 46 , N. 1 , P. 183-194

Droits : 2010 Wiley Blackwell Publishing, Inc. Phycological Society of America
http://archimer.ifremer.fr/doc/2010/publication-7449.pdf
DOI:10.1111/j.1529-8817.2009.00774.x
http://archimer.ifremer.fr/doc/00000/7449/

Éditeur(s) : HAL CCSD Springer-Verlag
Résumé : International audience
With hull-mounted multibeam echosounder data, wereport for the first time along the active Ecuadorian margin,acoustic signatures of water column fluid emissions and seep-relatedstructures on the seafloor. In total 17 flare-shaped acousticanomalies were detected from the upper slope (1250 m) to the shelfbreak (140 m). Nearly half of the flare-shaped acoustic anomaliesrise 200–500 m above the seafloor. The base of the flares is generallyassociated with high-reflectivity backscatter patchescontrasting with the neighboring seafloor. We interpret these flaresas caused by fluid escape in the water column, most likely gases.High-resolution seismic profiles show that most flares occur closeto the surface expression of active faults, deformed areas, slopeinstabilities or diapiric structures. In two areas tectonic deformationdisrupts a Bottom Simulating Reflector (BSR), suggesting thatburied frozen gas hydrates are destabilized, thus supplying free gasemissions and related flares. This discovery is important as it opensthe way to determine the nature and origin of the emitted fluids andtheir potential link with the hydrocarbon system of the forearcbasins along the Ecuadorian margin.
ISSN: 0033-4533

insu-01267238
https://hal-insu.archives-ouvertes.fr/insu-01267238
DOI : 10.1007/s00024-015-1230-7