Éditeur(s) : HAL CCSD Public Library of Science
Résumé : International audience
Growth series of Palaeozoic fishes are rare because of the fragility of larval and juvenile specimens owing to their weak mineralisation and the scarcity of articulated specimens. This rarity makes it difficult to describe early vertebrate growth patterns and processes in extinct taxa. Indeed, only a few growth series of complete Palaeozoic fishes are available; however, they allow the growth of isolated elements to be described and individual growth from these isolated elements to be inferred. In addition, isolated and in situ scales are generally abundant and well-preserved, and bring information on (1) their morphology and structure relevant to phylogenetic relationships and (2) individual growth patterns and processes relative to species ontogeny. The Late Devonian acanthodian Triazeugacanthus affinis from the Miguasha Fossil-Lagerstä tte preserves one of the best known fossilised ontogenies of early vertebrates because of the exceptional preservation, the large size range, and the abundance of complete specimens. Here, we present morphological, histological, and chemical data on scales from juvenile and adult specimens (scales not being formed in lar-vae). Histologically, Triazeugacanthus scales are composed of a basal layer of acellular bone housing Sharpey's fibers, a mid-layer of mesodentine, and a superficial layer of ganoine. Developmentally, scales grow first through concentric addition of mesodentine and bone around a central primordium and then through superposition of ganoine layers. Onto-genetically, scales form first in the region below the dorsal fin spine, then squamation spreads anteriorly and posteriorly, and on fin webs. Phylogenetically, Triazeugacanthus scales show similarities with acanthodians (e.g. " box-in-box " growth), chondrichthyans (e.g. squamation pattern), and actinopterygians (e.g. ganoine). Scale histology and growth are interpreted in the light of a new phylogenetic analysis of gnathostomes supporting acantho-dians as stem chondrichthyans.
ISSN: 1932-6203

Droits : http://creativecommons.org/licenses/by/
hal-01526367
http://hal.upmc.fr/hal-01526367
http://hal.upmc.fr/hal-01526367/document
http://hal.upmc.fr/hal-01526367/file/journal.pone.0174655.pdf
DOI : 10.1371/journal.pone.0174655

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) : Blackwell science
Résumé : Peneid shrimp are commonly reared in clear-water aquaria or tanks for short-term studies of 4-6 weeks during controlled experiments, such as nutrition studies to estimate dietary nutrient requirements. Recently, in line with the genetic program at Centre Oceanologique du Pacifique (COP), experimental clear-water facilities were tested for the first time over a longer rearing period. Environmental conditions used to maintain animal growth in clear-water system using a well-balanced diet were defined. After 100 days, shrimp growth rates tended to decrease and only by adjusting the diet could shrimp complete their life cycle and reach maturation size of around 40 g. This paper presents information on stocking density, diet quality and husbandry linked to reproduction that must be considered to successfully rear animals from PL's to breeder size in clear water. By following these protocols a minimum amount of breeders can be used to meet production goals. Moreover, by isolating a small group of individuals, genetic diversity can be preserved, thereby allowing specific crosses for selective breeding purposes. Length of trials, amount of feed, composition of feed, growth performances and maturation success are reported and should encourage further studies to optimize rearing conditions in clear-water rearing.
Aquaculture Research (1355-557X) (Blackwell science), 2004-11 , Vol. 35 , N. 13 , P. 1244-1252

Droits : 2004 Blackwell Synergy
http://archimer.ifremer.fr/doc/2004/publication-619.pdf
DOI:10.1111/j.1365-2109.2004.01145.x
http://archimer.ifremer.fr/doc/00000/619/

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

Résumé : En occupant un espace social privilégié, la médecine traditionnelle et les diverses pratiques qui y sont liées, sont de moins en moins marginalisées, de plus en plus admises comme ressources et la société leur devient du même coup permissive. La tolérance sociale est relativement forte ». Cette lecture de la situation de la médecine traditionnelle et de sa réception dans la société est celle de l’anthropologue et médecine martiniquais M. Yoyo. Elle évoque la réalité de la médecine créole dans l’espace antillais et dit l’intérêt que lui portent ceux qui en font usage.L’objectif de cette recherche est de poser la question de la transmission du savoir médicinal en contexte martiniquais : transmission des tradipraticiens vers les profanes ; transmission entre professionnels de cette médecine. Autrement dit comment se fait l’apprentissage si apprentissage il y a, de ce savoir traditionnel, jalousement gardé par ceux qui l’exercent ? La dimension magico-religieuse de ce savoir influe-t-elle sur sa transmission ? Quel est le rôle de la famille dans l’éducation et la transmission de ces pratiques ? Quelle est la connaissance profane accessible à tous et que détiennent certaines familles ? Celle-ci répond-elle aux attentes de la médecine traditionnelle et comment les familles procèdent-elles à sa transmission ? Quelle contribution l’institution scolaire apporte-t-elle à la sauvegarde de ce patrimoine ? Ce questionnement nous amène à nous interroger sur les pratiques en matière de médecine des Martiniquais et à considérer la coexistence entre savoir traditionnel et savoir rationnel dit moderne.On ne peut faire l’économie de ces analyses si on veut appréhender de façon objective le problème de la transmission de la médecine créole, de sa sauvegarde par – et pour – les générations montantes, en raison de l’aspect mémoriel de cette pratique thérapeutique mais également en raison de son efficacité et du potentiel important qu’elle représente pour la santé dans les années qui viennent.
By occupying a privileged social space, traditional medicine and the diverses practices related to the field are less and less marginalized, more and more accepted as resources, thus society is gradually becoming more tolerant towards those practices. The social tolerance is relatively strong”. This perception of the present situation of traditional medicine and of its reception in society is proposed by M. Yoyo, French anthropologist and physician from Martinique. It speaks of the reality of traditional medicine in the west Indians context and highlights the positive affects on those who make use of it. The objective of this research is to explore the question of the transmission of medicinal knowledge within the confines of Martinique: transmission by traditionalists towards nonprofessionals as well as transmission among professionals in the fields of medicine. In other words, what learning, if any, still exists of this traditional knowledge faithfully kept by those practiced it? To what extent does the magical-religious experience influence the transmission of this knowledge? What is the role of the family in the education and the transmission of those practices? How much of this profane knowledge is accessible to all and to what extent is it practiced by families? Does the latter respond to the demands of traditional medicine? How do families proceed with the process of transmission. What contribution does the school make towards preserving this tradition ? The above questions provoke reflection on the medicinal practices of the people of Martinique and of the possible coexistence of traditional knowledge and modern or rational knowledge. These questions are inevitable if we want to progress with objectivity in the transmission of Creole medicine and of its preservation for future generations, as a form of safeguarding the memory of this therapeutic practice. However, they also help to focus on the level of its effectiveness and the potential importance that it represents in ensuring a healthy environment in the coming years.

http://www.theses.fr/2015AGUY0865/document

Éditeur(s) : HAL CCSD Oxford University Press (OUP)
Résumé : International audience
Upper-mantle flow beneath the South Pacific is investigated by analysing shear wave splitting parameters at eight permanent long-period and broad-band seismic stations and 10 broad-band stations deployed in French Polynesia from 2001 to 2005 in the framework of the Polynesian Lithosphere and Upper Mantle Experiment (PLUME). Despite the small number of eventsand the rather poor backazimuthal coverage due to the geographical distribution of the natural seismicity, upper-mantle seismic anisotropy has been detected at all stations except at Tahiti where two permanent stations with 15 yr of data show an apparent isotropy. The median value of fast polarization azimuths (N67.5°W) is parallel to the present Pacific absolute platemotion direction in French Polynesia (APM: N67°W). This suggests that the observed SKS fast polarization directions result mainly from olivine crystal preferred orientations produced by deformation in the sublithospheric mantle due to viscous entrainment by the moving Pacific Plate and preserved in the lithosphere as the plate cools. However, analysis of individualmeasurements highlights variations of splitting parameters with event backazimuth that imply an actual upper-mantle structure more complex than a single anisotropic layer with horizontal fast axis. A forward approach shows that a two-layer structure of anisotropy beneath French Polynesia better explains the splitting observations than a single anisotropic layer. Second ordervariations in the measurements may also indicate the presence of small-scale lateral heterogeneities. The influence of plumes or fracture zones within the studied area does not appear to dominate the large-scale anisotropy pattern but may explain these second-order splitting variations across the network.
ISSN: 0956-540X

hal-01249275
https://hal.archives-ouvertes.fr/hal-01249275
https://hal.archives-ouvertes.fr/hal-01249275/document
https://hal.archives-ouvertes.fr/hal-01249275/file/GJI2007SKS.pdf
DOI : 10.1111/j.1365-246X.2007.03475.x

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
The Chalkidiki block is a major domain in the North Aegean that, contrary to other domains in the region, largely escaped thermal perturbations during Tertiary extension. As a result, the Chalkidiki block is an ideal candidate to glean information related to the timing of Mesozoic thermal events using appropriate geochronological techniques. We have undertaken a laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS) study (U-Th-Pb on monazites and U-Pb on zircons) coupled with 40Ar/39Ar dating on nine samples from various structural levels within the thrust system of the Chalkidiki block. The eastern, and structurally lower part of the system revealed a complete isotopic reset of Carboniferous – Early Triassic monazites coeval with partial monazite destruction, REE-mobilisation and formation of apatite-allanite-epidote coronas at ~ 132 Ma, a reaction that is commonly observed in amphibolite-facies rocks. These coronas formed after crystallisation of garnet (i.e., at T > 580 °C) and, in all probability, either close to the peak-temperature conditions (~ 620 °C) on a prograde path or during retrogression between the peak-temperature and the low-temperature boundary of the amphibolite facies. Cooling of these rocks and arrival at mid-crustal levels occurred at 95–100 Ma. By contrast, the western, and structurally uppermost part of the system went through the same event by 120–125 Ma. Further structural considerations with respect to medium-temperature geochronology data imply that syn-metamorphic thrusting must have ceased by early Late Cretaceous. We emphasize that, with the sole exception of the Chalkidiki block, no pre-45 Ma medium-temperature geochronology data are preserved in other North Aegean domains, a feature that is clearly related to the extension-induced thermal perturbation of the region during the Tertiary.
ISSN: 0040-1951

insu-01329472
https://hal-insu.archives-ouvertes.fr/insu-01329472
https://hal-insu.archives-ouvertes.fr/insu-01329472/document
https://hal-insu.archives-ouvertes.fr/insu-01329472/file/kydonakis-tectono-2016.pdf
DOI : 10.1016/j.tecto.2016.06.006

Éditeur(s) : HAL CCSD
Résumé : International audience
Continental erosion and weathering destroy parts of the stratigraphic record. Analyses of the sedimentary filling of paleokarsts help completing the geological record of regions that have been submitted to post-depositional, long-term, continental evolution. Jurassic carbonate platform of Languedoc (South of France) has undergone several karstification phases from Cretaceous to Neogene. Later incision of canyons through the carbonate massifs allows to observe paleokarsts over 400m depth, within the massifs. Paleokarsts are partly filled with sediments. Some have yielded marine bioclasts (echinoderms, radiolars), foraminifera and nannofossils; others are composed of polygenic detrital sediments, including sources from the upstream Paleozoic basement (Cevennes). The age of the filling of successive paleokarsts can be constrained by structural relationships and by biostratigraphy. These findings suggests 1) the marine elements of the karstic filling relate to a Late Cretaceous to Early Paleocene interval, while 2) the Paleozoic basement-sourced-sediments were trapped in the karst during Miocene to Present. Karstic sediment containing Early Paleocene foraminifera and nannofossils are found in paleokarsts cavities distributed across the entire thickness of the carbonate massif (≥350m). This requires base-level lowering and associated karstification, followed by base-level rise and karst filling of at least 350 m amplitude, respectively. The time interval corresponding to the occurrence of foraminifera and nannofossils in karsts covers 10 Myrs ; surprisingly, no equivalent marine sediments are preserved on the surface. In addition, analyses of the different forams species suggests several (up to 3) distinct karstification and marine filling cycles. Finally, sedimentological facies analysis of the karst filling reveals the following succession of processes: low energy settling of mudstone, high energy reworking, transport and deposition of silts and sandstones within the karst system. Integration of geological, paleontological and sedimentological data, leads to a polyphase scenario in response to repeated base-level variations, more than 350m amplitude. Such an amplitude excludes eustacy, and the improbable repeated sequence of uplift and subsidence rules out tectonics, as driving forces for base-level change, respectively. We propose that the high-amplitude base-level changes results from a succession of desiccation-flooding events of an endorheic, silled, basin during Early Paleogene. The later detrital assemblage sourced in the Cevennes occurs on perched paleosurfaces and in karst cavities across the whole 350m-deep canyon walls. When found on paleosurfaces, they correspond to the south-flowing Early Miocene fluvial drainage, and can be correlated downstream with the marine, well dated, Early Miocene, sediments. When found within the karst cavities, they correspond to successive base-level surfaces connected to the progressive incision of the canyon. This canyon incision is coeval with a Late Miocene uplift of the hinterland.
24th International Karstological School "Classical karst" : Paleokarst
Postojna, Slovenia

hal-01306683
https://hal-brgm.archives-ouvertes.fr/hal-01306683
https://hal-brgm.archives-ouvertes.fr/hal-01306683/document
https://hal-brgm.archives-ouvertes.fr/hal-01306683/file/Abstract_IKS.pdf

Éditeur(s) : HAL CCSD Integrated Ocean Drilling Program
Résumé : Integrated Ocean Drilling Program (IODP) Expedition 325, designed to investigate the fossil reefs on the shelf edge of the Great Barrier Reef, was the fourth expedition to utilize a mission-specific platform and was conducted by the European Consortium for Ocean Research Drilling (ECORD) Science Operator (ESO). The objectives of Expedition 325 were to establish the course of sea level change, define sea-surface temperature variations, and analyze the impact of these environmental changes on reef growth and geometry for the region over the period of 20-10 ka. To meet these objectives, a succession of fossil reef structures preserved on the shelf edge seaward of the modern barrier reef were cored from a dynamically positioned vessel in February-April 2010. A total of 34 boreholes across 17 sites were cored in depths ranging from 42.27 to 167.14 meters below sea level (lowest astronomical tide taken from corrected EM300 multibeam bathymetry data). Borehole logging operations in four boreholes provided continuous geophysical information about the drilled strata. The cores were described during the Onshore Science Party (OSP) at the IODP Bremen Core Repository (Germany) in July 2010, where minimum and some standard measurements were made. Preliminary postcruise dating of core catcher samples and initial observations of the cores made during the OSP confirm that coral reef material ranging in age from >30,000 to 9,000 calendar years before present (years before 1950 AD) was recovered during Expedition 325. Further postcruise research on samples taken during the OSP is expected to fulfill the objectives of the expedition.
ISSN: 1930-1014

hal-00855800
https://hal.archives-ouvertes.fr/hal-00855800

Éditeur(s) : HAL CCSD Wiley-Blackwell
Résumé : International audience
Garnet growth in high-pressure, mafic garnet granulites formed by dehydration melting of hornblende-gabbronorite protoliths in the Jijal complex (Kohistan palaeo-island arc complex, north Pakistan) was investigated through a microstructural EBSD-SEM and HRTEM study. Composite samples preserve a sharp transition in which the low-pressure precursor is replaced by garnet through a millimetre-sized reaction front. A magmatic foliation in the gabbronorite is defined by mafic-rich layering, with an associated magmatic lineation defined by the shape-preferred orientation (SPO) of mafic clusters composed of orthopyroxene (Opx), clinopyroxene (Cpx), amphibole (Amp) and oxides. The shape of the reaction front is convoluted and oblique to the magmatic layering. Opx, Amp and, to a lesser extent, Cpx show a strong lattice-preferred orientation (LPO) characterized by an alignment of [001] axes parallel to the magmatic lineation in the precursor hornblende-gabbronorite. Product garnet (Grt) also displays a strong LPO. Two of the four < 111 > axes are within the magmatic foliation plane and the density maximum is subparallel to the precursor magmatic lineation. The crystallographic relationship < 111 >(Grt)//[001](Opx,Cpx,Amp) deduced from the LPO was confirmed by TEM observations. The sharp and discontinuous modal and compositional variations observed at the reaction front attest to the kinetic inhibition of prograde solid-state reactions predicted by equilibrium-phase diagrams. The P-T field for the equilibration of Jijal garnet granulites shows that the reaction affinities are 5-10 kJ mol.(-1) for the Grt-in reaction and 0-5 kJ mol.(-1) for the Opx-out reaction. Petrographic and textural observations indicate that garnet first nucleated on amphibole at the rims of mafic clusters; this topotactic replacement resulted in a strong LPO of garnet. Once the amphibole was consumed in the reaction, the parallelism of [001] axes of the mafic-phase reactants favoured the growth of garnet crystals with similar orientations over a pyroxene substrate. These aggregates eventually sintered into single-crystal garnet. In the absence of deformation, the orientation of mafic precursor phases conditioned the nucleation site and the crystallographic orientation of garnet because of topotaxial transformation reactions and homoepitaxial growth of garnet during the formation of high-pressure, mafic garnet-granulite after low-pressure mafic protoliths.
ISSN: 0263-4929

hal-00411323
https://hal.archives-ouvertes.fr/hal-00411323
DOI : 10.1111/J.1525-1314.2008.00789.x

Éditeur(s) : HAL CCSD
Résumé : International audience
In the southern part of the Armorican Massif, a Carboniferous continental sedimentation is preserved in two basins located along a dextral fault (the Nort-sur-Erdre Fault). The first one called the Ancenis Basin is Early Carboniferous in age. The second, Namurian in age (i.e. Early to Late Carboniferous), consists of coal-bearing basins (Basse-Loire Unit) and is supposed to be synchronous with the dextral displacement along the North-sur-Erdre Fault. The Carboniferous series of the Ancenis Basin presents intrusive rocks (granite, microgranites) and volcanic rocks (rhyolites). Chemical analyses indicate that they all belong to the same magmatic high-K calc-alkaline association of peraluminous composition. For the first time, this magmatic event has been dated using the LA-ICPMS U-Pb method on zircons. The obtained age is of 319.3 3.1 Ma and constrains both the maximum age of end of the sedimentation and the northward tilting of the sediments in the Ancenis Basin. This magmatic event is coeval with the sedimentation of the coal-bearing Namurian basins. These intrusions are interpreted as the feeding conduits of the volcano-sedimentary layers encountered in these basins. The present-day distance between the intrusive rocks in the Ancenis basin and their extrusive products would imply a minimal dextral displacement of nearly 20-25 km along the Nort-sur-Erdre Fault.
Geophysical Research Abstracts
Vienne, Austria

insu-00673907
https://hal-insu.archives-ouvertes.fr/insu-00673907

Éditeur(s) : Gauthier-Villars
Résumé : The mangroves of Senegal are limited to the inlet of the Casamance - a river with very low discharge - and to the Sine-Saloum. The mineralogical and geochemical analysis of sediments (derived from 30 deep bore-holes) shows the thickness of the mangrove substrate, which overlies the continental terminal formation. Kaolinite and smectite account for over 90% of the clay fraction. The former is derived from the continental terminal whereas the latter is of marine origin. The chemical composition of the mangrove sediments is remarkably stable and clays play an overwhelming role in the preservation of organic matter and pyrite. Since 1968, a drought in Senegal has caused an important increase in the salinity levels of streams and water-tables; a considerable modification of vegetation zones in the Casamance, especially manifest in the extension of bare flats locally known as "tannes" at the expense of mangroves and marked changes in the morphology and geochemistry of mangrove soils. Compared to most mangrove areas in the humid tropics, mangroves in Senegal are characterized by a very fragile equilibrium.
Oceanologica Acta, Special issue (0399-1784) (Gauthier-Villars), 1982

Droits : info:eu-repo/semantics/openAccess
http://archimer.ifremer.fr/doc/00246/35744/34252.pdf
http://archimer.ifremer.fr/doc/00246/35744/

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

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

Éditeur(s) : HAL CCSD
Résumé : International audience
The fusion of regions from segmentation is often a required step in order to analyze objects in the scene. It allows to group under a same closure property the partitions of an image, which denote the same object. In this way, several studies have been made. Most of the algorithms are based on global information to evaluate the relevance of region combinations and fusion. In this paper, we propose a merging process based on Gestalt vision's theory. The particularity of our method is to preserve photographer's region of interest thanks to the definition of a new criterion based on Di Zenzo gradient. Thus, region fusion preserves photographer's relevant objects of the scene. The performance of the proposed method is evaluated using various natural images, including Berkeley image database and its accuracy is shown.
Color and Imaging Conference
San Jose, CA, United States

hal-00637144
https://hal.archives-ouvertes.fr/hal-00637144

Éditeur(s) : HAL CCSD American Geophysical Union
Résumé : International audience
Past earthquake slips on faults are commonly determined by measuring morphological offsets at current ground surface. Because those offsets might not always be well preserved, we examine whether the first 10 m below ground surface contains relevant information to complement them. We focus on the Te Marua site, New Zealand, where 11 alluvial terraces have been dextrally offset by the Wellington fault. We investigated the site using pseudo-3D Ground Penetrating Radar and also produced a high-resolution digital elevation model (DEM) of the zone to constrain the surface slip record. The GPR data reveal additional information: (1) they image the 3D stratigraphic architecture of the seven youngest terraces and show that they are strath terraces carved into graywacke bedrock. Each strath surface is overlain by 3-5 m of horizontally bedded gravel sheets, including two pronounced and traceable reflectors; (2) thanks to the multilayer architecture, terrace risers and channels are imaged at three depths and their lateral offsets can be measured three to four times, constraining respective offsets and their uncertainties more reliably; and (3) the offsets are better preserved in the subsurface than at the ground surface, likely due to subsequent erosion-deposition on the latter. From surface and subsurface data, we infer that Te Marua has recorded six cumulative offsets of 2.9, 7.6, 18, 23.2, 26, and 31 m (± 1-2 m). Large earthquakes on southern Wellington fault might produce 3-5 m of slip, slightly less than previously proposed. Pseudo-3D GPR thus provides a novel paleoseismological tool to complement and refine surface investigations
ISSN: 2169-9313

hal-00873350
https://hal.archives-ouvertes.fr/hal-00873350
DOI : 10.1002/jgrb.50317

Éditeur(s) : Springer
Résumé : Large benthic foraminifers are considered to be good indicators of shallow marine carbonate environments in fossil series. Over the last 50 years, the palaeoenvironment of Tertiary Nummulites accumulations has been a matter of debate, particularly because of difficulties in interpreting these deposits, and in this way, the absence of analogues in present-day seas does not help. The aim of this paper is to insight the different ways Nummulites tests and clasts may accumulate according to their hydrodynamic behaviour. Based on experimental measurements and on SEM observations, it appears that the high primary skeletal porosity of Nummulites made them easily transportable. The calculated threshold shear velocities confirm that large-sized Nummulites can be moved by weak wave-driven currents. This peculiar hydrodynamic behaviour of Nummulites could explain the diversity of depositional models. Depending on local hydrodynamic conditions, autochthonous Nummulites deposits can be preserved as in situ winnowed bioaccumulations or be accumulated offshore, onshore or alongshore, away from the original biotope.
Facies (0172-9179) (Springer), 2006-05 , Vol. 52 , N. 2 , P. 221-235

Droits : Springer-Verlag 2005
http://archimer.ifremer.fr/doc/00085/19597/17234.pdf
DOI:10.1007/s10347-005-0035-z
http://archimer.ifremer.fr/doc/00085/19597/

Résumé : The tropical seabass Lates calcarifer was introduced in Tahiti in 1984 and then was domesticated without other introduction. Three successive generations have been obtained in captivity. Tissue samples of the 38 animaIs which represent the total Tahitian broodstock were preserved in alcohol to be genotyped with four microsatellite markers (Yue et al., 2001). Three of four described markers were successfully transferred to the laboratory of genetics of Tahiti (marker LcaM01, LcaM02, LcaM03), as the revelation technology available locally did not allow the use of LcaM04 in routine. The results show that the genetic diversity of the tahitian broodstock is not equivalent of the one of the species, which could be explained by the small size of the founder population, which is consistant with the history of the Tahitian population. The structuration of the 4th generation into several batches obtained from different parents appears to be the minimum management procedure to limit inbreeding.
Le loup tropical Lates calcarifer a été introduit à Tahiti en 1984 puis domestiqué sans apport d'animaux extérieurs. Trois générations successives ont été obtenues en captivité. Des prélèvements de tissus sur les 38 géniteurs qui constituent l'intégralité du stock de reproducteurs tahitiens sont conservés dans l'alcool pour être génotypés à l'aide de quatre marqueurs microsatellites (Yue et al., 2001). Trois des quatre marqueurs décrits ont pu être transférés avec succès au laboratoire de génétique de Tahiti (marqueurs LcaM01, LcaM02, LcaM03), la technique de révélation disponible localement ne permettant pas d'utiliser LcaM04 en routine. Les résultats montrent qu'on ne dispose pas à Tahiti de toute la variabilité génétique de l'espèce, ce qui pourrait s'expliquer, compte tenu de l'histoire de cette population, par un faible nombre de géniteurs fondateurs. La structuration de la 4ème génération en plusieurs lots issus de parents différents apparaît comme la mesure de gestion minimale pour limiter la consanguinité au sein de cette population.

Droits : 2003 Ifremer
http://archimer.ifremer.fr/doc/00142/25300/23372.pdf
http://archimer.ifremer.fr/doc/00142/25300/

Éditeur(s) : HAL CCSD Taylor & Francis (Routledge)
Résumé : International audience
The influences of task difficulty (index difficulty: 2-4), input device of different length, range of motion and mode of resistance (joystick or rotorcraft stick), and directions of movement (leftward rightward) on motor patterns in a realistic control situation were examined with a multilevel analysis (joint kinematics and muscular variables, and global task performance). Eight subjects controlled the displacements of a virtual object during a slalom task characterized by a realistic inertial model. Pilots adapted the endpoint kinematic organization to increasing accuracy constraints to preserve task success whatever the device and the direction. However, the rotorcraft stick manipulation remains highly complex in comparison to the joystick due to poorer proprioceptive information, higher inertial constraints, and an asymmetrical muscle control.
ISSN: 0022-2895

hal-01442056
https://hal.archives-ouvertes.fr/hal-01442056
https://hal.archives-ouvertes.fr/hal-01442056/document
https://hal.archives-ouvertes.fr/hal-01442056/file/Fuente%20-%20J%20Motor%20Behav%20-%202013.pdf
DOI : 10.1080/00222895.2013.837424

Éditeur(s) : IEEE Geoscience and Remote Sensing Society
Résumé : The Medium Resolution Imaging Spectrometer (MERIS) launched in March 2002 and has been providing images since June 2002. Before its launch, we had implemented a method to improve its resolution by merging its images with Landsat Enhanced Thematic Mapper images in order to preserve the best characteristics of the two images (spatial, spectral, temporal). We now present the results of this method for real MERIS images (level 1b and 2) in a coastal area. The robustness of the method is studied as well as the influence of the delay between the acquisitions of the two images.
IEEE Geoscience and Remote Sensing Letters (1545-598X) (IEEE Geoscience and Remote Sensing Society), 2006-04 , Vol. 3 , N. 2 , P. 227-231

Droits : 2006 IEEE
http://archimer.ifremer.fr/doc/2006/publication-2119.pdf
DOI:10.1109/LGRS.2005.861699
http://archimer.ifremer.fr/doc/00000/2119/

Éditeur(s) : HAL CCSD Museum National d'Histoire Naturelle Paris
Résumé : Au Burdigalien supérieur, des récifs coralliens se sont développés dans la Formation de Cala di Labra, aux alentours de Bonifacio (Corse-du-Sud, France). Ils sont organisés en trois épisodes successifs R1, R2 et R3. La faune corallienne comprenant 16 espèces récifales, est décrite pour la première fois. Deux associations coralliennes sont distinguées. Les principaux genres constructeurs sont Porites Link, 1807, Tarbellastraea Alloiteau, 1950 et Thegioastraea Sismonda, 1871. La diversité corallienne est maximale avec 15 espèces (8 genres) dans l'épisode R1, puis réduite (4 espèces appartenant à 3 genres) pour l'épisode R2, l'épisode R3 renfermant des coraux mal préservés pour être identifiés. Les formes de croissance sont en grande majorité massives étalées et superposées, associées à des conditions paléoenvironnementales de haute à moyenne énergie (rides de courant, bioclastes usés, peu de formes branchues), sous apports terrigènes réguliers. Les récifs, pour la plupart frangeants et à zonation récifale discrète, se sont développés en domaine de plate-forme peu profonde. Cette étude reprend également toutes les citations d'espèces dans la littérature pour cette région et replace ces épisodes coralliens remarquables dans l'évolution plus générale du Bassin Liguro-Provençal.
ISSN: 1280-9659

hal-01236095
https://hal.archives-ouvertes.fr/hal-01236095
DOI : 10.5252/g2015n3a5