Éditeur(s) : American Geophysical Union
Résumé : Lagrangian analyses of a global ocean circulation model quantify the salinity changes experienced by the warm limb of the thermohaline circulation during the northward flow to the Atlantic deep convection regions. 6 Sv out of the estimated 10-Sv transfer from 45 degrees S to 47 degrees N flow through regions of prevailing surface evaporation: the southern and northern formation regions of Salinity Maximum Water and the Gulf of Cadiz/Mediterranean Sea domain. The remaining transport gains salinity through mixing with adjacent waters. As much as 6 Sv flow through the low-salinity surface mixed layer at the latitudes of the ITCZ whose effect annihilates that of the southern region of Salinity Maximum Water. Most of the salinity increase corresponds to the transformation of South to North Atlantic Central Water, with strong diapycnal transfers for the water that intersects the high and low salinity regions, and nearly isopycnal modifications for the water that avoids these regions.
Geophysical Research Letters ( GRL ) (0094-8276) (American Geophysical Union), 2006-03 , Vol. 33 , N. 6 , P. NIL_44-NIL_47

Droits : 2006 by the American Geophysical Union
http://archimer.ifremer.fr/doc/2006/publication-1213.pdf
DOI:10.1029/2005GL024938
http://archimer.ifremer.fr/doc/00000/1213/

Éditeur(s) : HAL CCSD Oxford University Press (OUP)
Résumé : International audience
STUDY QUESTION: Can protein biomarkers of the male genital tract be identified in human seminal plasma? SUMMARY ANSWER: We identified potential biomarkers for each of the organs participating in the secretions of the human seminal plasma. WHAT IS KNOWN ALREADY: The seminal plasma fulfills critical functions for fertility by providing spermatozoa with a protective milieu, promoting their final maturation and modulating the immune responsiveness of the female reproductive tract. It is also considered to be a promising source of biomarkers of male infertility and/or pathologies of the male genital tract. STUDY DESIGN, SIZE, DURATION: This study combines proteomic analyses of normal seminal plasma together with transcriptomic gene expression profiling of human healthy tissues. MATERIALS, SETTING, METHODS: Non-liquefied seminal plasma proteins from a healthy donor were prefractionated using two sequential Proteominer™ libraries. Eight subproteome fractions were collected, trypsin digested and subjected to three successive mass spectrometry analyses for peptide characterization. The list of identified proteins was compared with and merged with other available data sets of the human seminal plasma proteome. The expression of corresponding genes was then investigated using tissue transcriptome profiles to determine where, along the male reproductive tract, these proteins were produced. Finally, tissue specificity of a selected subset of biomarker candidates was validated on human tissues. MAIN RESULTS AND THE ROLE OF CHANCE: We first performed a proteomic analysis of the human seminal plasma and identified 699 proteins. By comparing our protein list with other previous proteomic data sets, we found that 2545 unique proteins have been described so far in the human seminal plasma. We then profiled their expression at the gene level and identified 83 testis, 42 epididymis, 7 seminal vesicle and 17 prostate candidate protein markers. For a subset of testis-specific candidates, i.e. TKTL1, LDHC and PGK2, we further validated their germ cell expression and demonstrated that such markers could distinguish between semen from fertile and infertile men. LIMITATIONS, REASONS FOR CAUTION: While some of the markers we identified are well-known tissue-specific products, further dedicated studies to validate the biomarker status of new candidates will be required. Additionally, whether or not the abundance of these proteins is indeed decreased in some specific pathological situations remains to be determined. WIDER IMPLICATIONS OF THE FINDINGS: Using an integrative genomics approach, we identified biomarker candidates for each of the organs participating in the seminal plasma production. In this study, we essentially focused on germ cell markers and their potential application for the diagnosis of male infertility. Other types of markers also deserve a focused attention given their potential predictive value for various reproductive disorders, notably for prostate cancers. STUDY FUNDING/COMPETING INTEREST(S): This work was supported by the Proteomics Core Facility at Biogenouest and was funded by Conseil Régional de Bretagne, IBiSA and Agence de la Biomédecine grants. The authors declare that there exists a competing financial interest in this work that is related to a patent application on the use of identified germ cell-specific proteins in an antibody-based assay (Fertichip™) to predict the successful testicular biopsy outcomes in human non-obstructive azoospermia.
ISSN: 0268-1161

inserm-00814146
http://www.hal.inserm.fr/inserm-00814146
DOI : 10.1093/humrep/des360
PUBMED : 23024119

Éditeur(s) : HAL CCSD Taylor & Francis: SSH Journals
Résumé : International audience
We analysed stroke phases and arm and leg coordination during front crawl swimming with and without a wet suit. Twelve nationally and internationally ranked French male triathletes performed three swim trials in randomized order using the front crawl stroke with and without a wet suit. All triathletes swam at three different swim velocities, corresponding to the paces appropriate for the 800 m (V800), 100 m (V100) and 50 m (V50) events. The different stroke phases and arm and leg coordination were identified by video analysis. Arm coordination was quantified using a new index of coordination, which expresses the three major modalities of opposition, catch-up and superposition in swimming. At all swim velocities, no significant differences in leg movements with or without the wet suit were noted. However, the wearing of the wet suit was associated with a significantly greater stroke length at the paces appropriate for the 100 and 50 m events (+3.46% and +3.10% at V100 and V50, respectively; P<0.01); a significantly greater stroke index at all three velocities (+5.18%, +5.21% and +5.91% at V800, V100 and V50, respectively; P<0.01); a significantly shorter pulling phase (-10.97%; P<0.05) and lower index of coordination (-21.87%; P<0.01) at the pace appropriate for the 800 m; and a significantly greater entry and catch phase (+9.81%; P<0.05) at the pace appropriate for the 100 m. We conclude that the wet suit amplified the coordination mode of the triathletes (i.e. catch-up coordination) without modifying stroke rate, recovery phase or leg movements.
ISSN: 0264-0414

hal-00720724
https://hal.univ-antilles.fr/hal-00720724

Éditeur(s) : HAL CCSD Borntraeger Science Publishers
Résumé : This study characterizes the stratigraphical context as well as the palaeoenvironmental and sealevel trends during the Late Frasnian and Famennian in the Buschteich section (Thuringia, Germany). An integrated approach combines conodont biostratigraphy, chemostratigraphy based on carbon and oxygen isotopes, conodont biofacies analyses and investigations of the morphotypes of foraminifera that occur in the section was applied. Conodonts provided a fine-scale biostratigraphical framework. All the Famennian conodont biozones were identified, with the exception of the three lowest. The Frasnian – Famennian transition was further identified by a positive carbon isotope excursion. This continuous Famennian record is developed in a condensed limestone succession. The reddish Griotte facies, typical of strata of this period, were not documented. Black shales were not developed except for an interval of dark colored mud rocks corresponding to the Hangenberg event at the top of the section. The carbonate succession of Buschteich was deposited in an outer ramp environment, pelagic organisms are the dominant fauna. This is corroborated by the overall dominance of the deep-water conodont genus Palmatolepis. Microfacies, conodont biofacies and foramini fera indicated a deepening trend from the Lower crepida to the Lower rhomboidea Zone, followed by a shallowing trend from the Upper rhomboidea to the praesulcata Zone. This sequence overall matches the sea level reference curve for Euramerica. The timing of maximum water depth at Buschteich, as well as the general sea-level reference record, differs from the Col des Tribes (Montagne Noire, France). Differential uplift or overprinting of the long-term eustatic changes may be the cause of the discrepancy in the local sea-level records.
ISSN: 0078-0421

hal-01623111
https://hal.archives-ouvertes.fr/hal-01623111
DOI : 10.1127/nos/2016/0318

Éditeur(s) : HAL CCSD Wiley
Résumé :  
The forests in Cat Tien National Park, appear as a mosaic of different communities, distinct from each other with respect to their floristic and structural parameters. The objectives of this study are (1) to characterize the different formations occurring in the lowland part and (2) to identify the main successional trends in the area. Understanding forest succession is important for silviculture and restoration of forests and land rehabilitation, as adequate information on the ecological role of local species in the functioning of the forests is not available in Vietnam. Five plots (1 ha each) were established in the lowland part of Cat Tien National Park, where all the trees ≥ 10 cm d.b.h. (diameter at breast height) were located, measured and identified. A systematic sampling was made to assess the regeneration. Three plots (A, C and D) can be considered as secondary forests on the basis of their structural parameters. Plots A and C are dominated by Lagerstrmia calyculata and plot D by Dipterocarpus alatus. The other two plots can be regarded as mature forests. Plot B corresponds to a semideciduous formation dominated by Lagerstrmia calyculata and Fabaceae species, and plot E to an evergreen one dominated by dipterocarp species. The floristic composition of plots A and C will change in the future because dominant canopy species are rare or absent in regeneration. A correspondence analysis performed on the number of trees per species shows two kinds of successional trends: one from A to B on shallow and drier soils, and another from C to E on deeper and wetter soils.
ISSN: 0305-0270

hal-01032094
https://hal.archives-ouvertes.fr/hal-01032094
DOI : 10.1046/j.1365-2699.2000.00347.x

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
In orogenic systems, thrust faults play a major role in stacking different tectonic units and may act as conduits for the expulsion of large amounts of fluid of different origins (metamorphic, diagenetic, meteoric). This study focuses on the Monte Perdido thrust unit emplaced in the Paleogene Jaca thrust-sheet-top basin, in the SW-central Pyrenees. We aim to decipher the mechanisms and P-T conditions of deformation in fault zones and characterize the related fluid involvement, through combined microstructural, geochemical and microthermometry analyses. Two thrust faults cutting platform limestones, marls and siliciclastic turbidites of the lower part of the basin-fill (Paleocene-lower Eocene) have been studied. The fault zones are characterized by metre-thick shear zones with highly deformed, foliated clay-rich sediments. Foliation is underlined by preferentially oriented phyllosilicates. Several generations of shear and extension calcite, quartz and chlorite-bearing veins attest to fluid-rock interactions during a multi-stage deformation. Microstructural observations and stable isotope analyses on calcite from veins and host sediments suggest that deformation was aseismic and dominated by diffusive mass transfer from pressure solution sites along cleavage and stylolites to the precipitation sites in veins, with mineralizing fluids in equilibrium with the host sediments. Our results suggest an essentially closed hydrologic system, and imply the absence of significant fluid flow along the studied fault zones. Microthermometric study on fluid inclusions present in calcite and quartz veins, and calcite-quartz oxygen isotopic fractionation determined for the first generation shear veins, allow a geothermal gradient of 34 degrees C/km to be estimated. Analytical results demonstrate an evolution of the fault zones in three stages. The first stage was related to the emplacement of the Monte Perdido thrust unit during the middle Eocene at a temperature of similar to 208 degrees C and a burial depth of similar to 5.7 km. The second stage corresponds to a fault reactivation at a temperature of similar to 240 degrees C and a burial depth of similar to 6.5 km. The latter deformation may have been related to folding of the Monte Perdido thrust unit during the emplacement of the underlying Gavarnie thrust unit during the late Eocene-early Oligocene, with deeper burial resulting from aggradation of the thrust-sheet-top basin-fill. The last event corresponds to the formation of a dilatant vein system likely related to the exhumation of the massif.
ISSN: 0191-8141

hal-00644828
https://hal.archives-ouvertes.fr/hal-00644828
DOI : 10.1016/j.jsg.2011.06.006

Éditeur(s) : HAL CCSD
Résumé :   Diplôme : DEA
il s'agit d'un type de produit dont les métadonnées ne correspondent pas aux métadonnées attendues dans les autres types de produit : DISSERTATION
Eperua falcata Aublet est une espèce très abondante en forêt tropicale humide guyanaise. Elle présente une structure spatiale particulière, en agrégats se développant autour des bas-fonds. L'étude des peuplements sur le dispositif de Paracou et sur les placettes permanentes (ONF-Cirad) a permis de caractériser cette structure spatiale et sa dynamique et d'évaluer l'influence des conditions édaphiques sur la structuration spatiale. Ces analyses permettront ainsi de caractériser le tempérament et la stratégie d'Eperua falcata pour se maintenir dans ce milieu très compétitif qu'est la forêt tropicale humide. Eperua falcata est plus densément installé en engorgement moyen de bas de pente, ses performances sont elles aussi plus élevées dans cette zone. Cette espèce présente donc une préférence pour certaines conditions édaphiques. Ses performances (croissance, diamètre moyen et maximum, etc.) dans l'ensemble bonnes partout n'indiquent pas de limitation à l'expansion des agrégats. Cependant certains semblent limités par des sols à drainage vertical qui présenterait une disponibilité hydrique insuffisante en saison sèche. Cette contrainte agirait a priori sur les jeunes stades de développement des arbres. La structure spatiale agrégée d'Eperua falcata serait conditionnée essentiellement par la faible distance de dissémination de ses graines et par les conditions édaphiques. Les peuplements d'Eperua falcata avanceraient le long du réseau de bas-fonds en multiples digitations qui s'échapperaient progressivement de ces zones hydromorphes jusqu'à atteindre des sols à drainage vertical situés sur les plateaux qui stopperaient leur propagation.
https://hal.archives-ouvertes.fr/hal-01189221

hal-01189221
https://hal.archives-ouvertes.fr/hal-01189221
PRODINRA : 16384

Éditeur(s) : HAL CCSD Public Library of Science
Résumé : International audience
Little is known of how linkage patterns between species change along environmental gradients. The small, spatially discrete food webs inhabiting tank-bromeliads provide an excellent opportunity to analyse patterns of community diversity and food-web topology (connectance, linkage density, nestedness) in relation to key environmental variables (habitat size, detrital resource, incident radiation) and predators: prey ratios. We sampled 365 bromeliads in a wide range of understorey environments in French Guiana and used gut contents of invertebrates to draw the corresponding 365 connectance webs. At the bromeliad scale, habitat size (water volume) determined the number of species that constitute food-web nodes, the proportion of predators, and food-web topology. The number of species as well as the proportion of predators within bromeliads declined from open to forested habitats, where the volume of water collected by bromeliads was generally lower because of rainfall interception by the canopy. A core group of microorganisms and generalist detritivores remained relatively constant across environments. This suggests that (i) a highly-connected core ensures food-web stability and key ecosystem functions across environments, and (ii) larger deviations in food-web structures can be expected following disturbance if detritivores share traits that determine responses to environmental changes. While linkage density and nestedness were lower in bromeliads in the forest than in open areas, experiments are needed to confirm a trend for lower food-web stability in the understorey of primary forests.
PLoS ONE

hal-00913931
https://hal.archives-ouvertes.fr/hal-00913931
https://hal.archives-ouvertes.fr/hal-00913931/document
DOI : 10.1371/journal.pone.0071735
OATAO : 10204

Éditeur(s) : HAL CCSD
Résumé :   Diplôme : DEA
il s'agit d'un type de produit dont les métadonnées ne correspondent pas aux métadonnées attendues dans les autres types de produit : DISSERTATION
L'étude de la répartition géographique de la diversité génétique résultant de l'histoire des populations apparaît comme fondamentale pour la conservation des espèces. Ainsi, la mise en évidence des relations phylo-géographiques au court du Quaternaire récent, au sein d'une espèce modèle Vouacapoua americana (Caesalpiniaceae), en Guyane française apporte des informations importantes sur la dynamique des populations naturelles. Dans cette étude les loci trn Q-trn S et trn Sa-trn fM sont utilisés afin de déterminer l'histoire évolutive des populations issues des refuges forestiers tropicaux. Le but principal est l'obtention des séquences après amplification PCR. L'analyse de ces séquences chez cinq populations testées a permis de mettre en évidence leur caractère hypervariable, ainsi que des régions présentant des motifs conservés répétés plusieurs fois. Les constructions phylogéographiques obtenues à partir de celles-ci accentuent la régionalisation des différents chlorotypes, existant en Guyane pour cette espèce, mise en évidence au cours de travaux précédents. Ainsi, les informations apportées par cette approche apparaissent comme complémentaires aux résultats obtenus par d'autres techniques d'analyse moléculaire.
https://hal.archives-ouvertes.fr/hal-01189224

hal-01189224
https://hal.archives-ouvertes.fr/hal-01189224
PRODINRA : 16622

Résumé : Bycatch of marine turtles, vulnerable or endangered species, is a growing issue of all fisheries, including Oceanic purse-seine fishery. The present paper seeks to assess marine turtle bycatch at a spatial and temporal level in the European purse seine fishery operating in the Atlantic and Indian Oceans. The study was based on data collected through French and Spanish observer programs from 1995 to 2011, a period where more than 230 000 fishing sets were realized by the UE fleets in both Oceans. A total of 15 913 fishing sets were observed, including 6 515 on drifting Fish Aggregate Devices (FAD) and 9 398 on Free Swimming Schools (FSC). Over the study period, 597 turtles were caught, 86% being released alive at sea. At the same time, from 2003 to 2011, 14 124 specific observations were carried out on floating objects whether they ended in a set or not. 354 marine turtles were observed upon which 80% were already free or entangled alive and therefore released alive. At the temporal and spatial level, data were organized and analysed by Ocean, fishing mode (FAD vs. FSC) as well as by year, quarter and statistical square of 1°. In order to evaluate the impact if this fishery in both Oceans, bycatch distribution was compared to the total fishing effort of the UE fleet, as well as to the known marine turtle post nesting migration routes, nesting population abundances and known feeding areas. The species composition, the size and sex structure of bycatch are also discussed here. At last, an attempt to raise the data to the total fishing effort was carried out. Based on observation of marine turtle by-catches on sets, we estimated that, globally, 3500 marine turtles were accidentally captured by the EU-PS fleet in the Atlantic Ocean from 1995 to 2010, and around 2000 in the Indian Ocean from 2003 to 2010, with a corresponding annual bycatch rate of 218 (SD=150; survival rate =91%) and 250 (SD=157; survival rate =77%) respectively in the Atlantic and Indian Ocean. However, because of important uncertainties mainly due to the low observation coverage and the scarcity of marine turtle bycatch events, it was impossible to produce solid and reliable global estimates of marine turtle bycatch and mortality due to PS activity.

Droits : 2012 IOTC
http://archimer.ifremer.fr/doc/00149/25991/24087.pdf
http://archimer.ifremer.fr/doc/00149/25991/

Éditeur(s) : HAL CCSD European Geosciences Union
Résumé : International audience
During the GWADASEIS cruise (Lesser Antilles volcanic arc, February-March 2009) a very high resolution (VHR) seismic-reflection survey was performed in order to constrain Late Quaternary to Present faulting. The profiles we obtained evidence frequent "ponding" of reworked sediments in the deepest areas, similar to the deposition of Mediterranean "homogenites". These bodies are acoustically transparent (few ms t.w.t. thick) and are often deposited on the hanging walls of dominantly normal faults, at the base of scarps. Their thickness appears sufficient to compensate (i.e. bury) co-seismic scarps between successive earthquakes, resulting in a flat and horizontal sea floor through time. In a selected area (offshore Montserrat and Nevis islands), piston coring (4 to 7 m long) was dedicated to a sedimentological analysis of the most recent of these particular layers. It corresponds to non-stratified homogenous calcareous silty sand (reworked calcareous plankton and minor volcanoclastics). This layer can be up to 2 m thick, and overlies finegrained hemipelagites. The upper centimeters of the latter represent the normal RedOx water/sediment interface. 210Pb and 137Cs activities lack in the massive sands, while a normal profile of unsupported 210Pb decrease is observed in the hemipelagite below, together with a 137Cs peak correspond- ing to the Atmospheric Nuclear Experiments (1962). The RedOx level was thus capped by a recent instantaneous major sedimentary event considered as post-1970 AD; candidate seismic events to explain this sedimentary deposits are either the 16 March 1985 earthquake or the 8 October 1974 one (Mw=6.3 and Mw=7.4, respectively). This leads to consider that the syntectonic sedimentation in this area is not continuous but results from accumulation of thick homogenites deposited after the earthquakes (as observed in the following weeks after Haiti January 2010 event, McHugh et al., 2011). The existence of such deposits suggests that, in the area of study, vertical throw likely results from cumulated effects of separated earthquakes rather than from aseismic creep. Examination of VHR profiles shows that all major co-seismic offsets are recorded in the fault growth sequence and that co-seismic offsets can be precisely estimated. By using a sedimentation rate deduced from 210Pb decrease curve (0.5 mm yr−1) and taking into account minor reworking events detected in cores, we show that the Redonda system may have been responsible for five >M6 events during the last 34 000 yr. The approach presented in this work differs from fault activity analyses using displaced sets of isochronous surfaces and postulating co-seismic offsets. Combining VHR seismic imagery and coring we can decipher co-seismic vs. slow continuous displacement, and thus actually estimate the amplitude and the time distribution of major co-seismic offsets.
ISSN: 1561-8633

insu-00844581
https://hal-insu.archives-ouvertes.fr/insu-00844581
https://hal-insu.archives-ouvertes.fr/insu-00844581/document
https://hal-insu.archives-ouvertes.fr/insu-00844581/file/nhess-12-1755-2012.pdf
DOI : 10.5194/nhess-12-1755-2012

Éditeur(s) : HAL CCSD
Résumé : International audience
The "South-Dominica" archaeological mission of the French ministry of foreign affairs has started work in 2005. Designed to enlighten the archaeological terra incognita dominicana, this research has essentially been dedicated to the early ceramic occupation of the island. Our work has been based on the analysis of the few collections already existing, on systematic survey campaigns and on an important test pit program. This lecture will be concentrating on the presentation of the Soufrière site excavation. The Soufriere site, found in the seventies, is composed of an important early cedrosan saladoid occupation covered by volcanic deposits. The data obtained during this excavation, associated with other results of the "South Dominica" archaeological mission, incites us to think about a revision of the territories associated to the complexes in the Lesser Antilles.
La mission archéologique "Sud-Dominique" du ministère français des affaires étrangères a débuté ses travaux en 2005. Destinées à en finir avec la terra incognita dominicana archéologique, ces recherches sont essentiellement consacrées à l'étude du premier peuplement agro-céramique de l'île. Le travail de la mission archéologique repose sur l'étude de séries anciennes, des campagnes de prospections systématiques et un important programme de sondages. Notre présentation se concentrera sur la fouille que nous avons menée du site de Soufrière dans le sud de la Dominique. Ce gisement identifié dans les années 1970 correspond à une importante occupation saladoïde cedrosane ancienne qui a été recouverte par des dépôts volcaniques. Les données obtenues lors de cette fouille associées à l'ensemble des résultats obtenus en 3 années par la mission archéologique Sud-Dominique nous incitent à nous interroger sur la nécessité d'une révision des territoires associés à la notion de complexe dans les Petites Antilles.
XXII Conference of the International Association of Caribbean Archaeology
Kingston, Jamaica

Droits : info:eu-repo/semantics/OpenAccess
hal-00961335
https://hal.univ-antilles.fr/hal-00961335
https://hal.univ-antilles.fr/hal-00961335/document
https://hal.univ-antilles.fr/hal-00961335/file/soufriA_repaperfinal.pdf

Résumé : La présente synthèse fait un historique des activités thonières en Nouvelle-Calédonie et dresse un bilan des données disponibles dans ce domaine. Ces données sont d'origines diverses (Agences des Pêches des pays étrangers pratiquant la pêche hauturière, Commission du Pacifique Sud, ORSTOM, Service Territorial de la Marine Marchande et des Pêches Maritimes, Services des Pêches des Provinces, ...). Certaines sont incomplètes et de mauvaise qualité. Elles se présentent sous forme disparate (données historiques informatisées des armements étrangers agrégées par mois et par carré de 5° de côté, fiches de pêche manuscrites, rapports scientifiques, rapports de mission, ... ). Elles ne sont donc pas directement accessibles et utilisables par les professionnels de la pêche thonière. Après informatisation, le recueil de l'ensemble de ces données a été transféré à l'ORSTOM et à la Structure de Gestion et de Valorisation Locale (SGVL) du programme ZoNéCo pour analyse. Cette analyse a permis de situer la production thonière en Nouvelle-Calédonie dans son contexte régional et de décrire son évolution depuis 1962. Les données de pêche postérieures à la mise en place de la ZE, et notamment celles qui correspondent à la période 1983-1994, ont été analysées en détail de façon à faire ressortir les fluctuations interannuelles, saisonnières et géographiques des prises et des rendements pour les principales espèces. Cette analyse a mis en évidence l'existence de zones et de saisons préférentielles de capture en tentant de les relier aux fluctuations des caractéristiques hydrologiques (structures thermique et haline). Les principaux résultats de cette synthèse sont récapitulés dans la conclusion.

Droits : info:eu-repo/semantics/openAccess
http://archimer.ifremer.fr/doc/00105/21639/19220.pdf
http://archimer.ifremer.fr/doc/00105/21639/

Éditeur(s) : HAL CCSD Taylor & Francis
Résumé : Modern geochronology has moved beyond the acquisition of dates: the goal is to understand the significance of these numbers for the geodynamic evolution of Earth at all scales. The coupling of the laser-ablation microprobe (LAM) to inductively coupled plasma mass spectrometers (ICPMS, multicollector (MC)-ICPMS) has revolutionised geochronology and geochemistry over the last 10 years. These systems enable the rapid and precise in situ analysis of trace-element patterns and isotopic systems, while adding information related to microstructural context and major-element composition. The integration of these multiple sources of data is crucial in constraining the origin of the sample and the processes leading to its formation, so that we can understand the meaning of a date in terms of geological events. LAM-ICPMS measurement of U-Pb ages and trace-element patterns in zircon, coupled with LAM-MC-ICPMS analysis of Hf isotopes in the same grains, gives new insights into the processes of magma genesis. Applied to detrital zircons from modern drainages or sedimentary rocks (the TerraneChron approach), it becomes a powerful tool to investigate problems of crustal evolution on scales ranging from single terranes to continents. The in situ analysis (LAM-MC-ICPMS) of Re-Os systematics in single grains of sulfides in mantle-derived peridotites has demonstrated that most mantle rocks contain several generations of Os-bearing sulfides; whole-rock analyses are mixtures reflecting multiple melting and metasomatic events in the lithospheric mantle. These deep-seated events are commonly mirrored in the crust; Os model-age spectra from xenolith suites show age 'peaks' that correspond to the ages of thermal/tectonic events in the overlying crust, suggesting strong linkages between crust and mantle. Integrated studies of the timing and nature of crustal and mantle events, using these techniques, will be important for understanding the large-scale dynamics of the Earth.
ISSN: 0812-0099

hal-00411328
https://hal.archives-ouvertes.fr/hal-00411328
DOI : 10.1080/08120090802097450

Éditeur(s) : HAL CCSD l'Harmattan
Résumé : International audience
Combien y a-t-il de saisons ? Sont-elles chaudes, froides, humides ou sèches ? La lune dans le ciel apparaît-elle verticale ou penchée ? Ces questions qui paraissent scientifiquement simples sont liées à de multiples contextes et, en particulier, au lieu d’observation. Elles ont été posées par questionnaire à l’ensemble d’une promotion d’étudiants scientifiques de Guadeloupe. Les réponses sont-elles plus pertinentes sur la description des saisons de métropole que sur celles des Antilles ? Confrontés à des photographies, les étudiants se réfèrent-ils plus à leurs observations de la lune ou à des images et modèles ? Ces questions renvoient toutes au rapport entre observation de la nature et transmission des connaissances formelles dans les apprentissages de sciences expérimentales. Ce travail vise principalement à estimer les conceptions d’étudiants scientifiques guadeloupéens de première année universitaire vis-à-vis de deux observations courantes : la forme apparente de la lune, et en particulier son orientation par rapport à la verticale, et les caractéristiques climatiques des saisons. Ces deux objets d’observation astronomique peuvent être réunis par trois caractéristiques communes :•Ils correspondent à des observations directes et fréquentes de la nature. Elles ne nécessitent pas de matériel d’observation complexe ni de protocole élaboré. Elles ne sont pas rares, et chacun, en zone intertropicale, est confronté quotidiennement à la météorologie (précipitation et température) et très fréquemment à l’observation de la lune. •Ils sont traités en cours de sciences dans l’enseignement secondaire français. En Sciences de la Vie et de la Terre (SVT dans la suite de ce texte) pour les saisons, et en Physique Chimie pour l’observation de la lune. Ces programmes sont nationaux et les manuels utilisés sont les mêmes dans les Antilles françaises que dans le reste du pays. •De nombreuses représentations des saisons situées en zones tempérées et de lune verticale sont utilisées en zone caraïbe. Elles sont liées aux arts (littératures, cinéma, musique,…) comme à des symboles divers (dessin de lune dans les agendas par exemple). Pour ces deux exemples une contradiction est notable entre le premier point, lié à l’observation locale, et les deux autres qui correspondent à des observations de zone tempérée. Cet article a pour objet d’estimer l’impact relatif de ces facteurs sur les conceptions des étudiants à l’issue de leurs cursus secondaire. En d’autres termes, notre objectif est d’observer, sur un échantillon représentatif d’étudiants de première année scientifique, si leurs descriptions des saisons tempérées est plus précises que celle des saisons des Antilles, et si leur conception de l’aspect de la lune est en lien avec l’observation de la nature.Le premier objectif de l’enseignement des sciences dans le secondaire est particulièrement clairement défini ainsi dans les programmes scolaires du collège :À l’issue de ses études au collège, l’élève doit s’être construit une première représentation globale et cohérente du monde dans lequel il vit. Il doit pouvoir apporter des éléments de réponse simples mais cohérents aux questions : « Comment est constitué le monde dans lequel je vis ? », « Quelle y est ma place ? », « Quelles sont les responsabilités individuelles et collectives ? ».Introduction générale des programmes de SVT du collège (BO du 28août 2008)Une rapide analyse scientifique et didactique sera présentée à la suite de la partie théorique afin de rappeler au lecteur les connaissances en jeu comme elles peuvent apparaître dans la littérature et dans les prescrits du secondaire. Cette analyse vise à mettre en perspective les résultats présentés et discutés dans les parties suivantes.
Apprentissages, éducation, socialisation et contextualisation didactique, approche plurielles

ISBN : 978-2-343-07837-3
hal-01536021
https://hal.univ-antilles.fr/hal-01536021

Éditeur(s) : HAL CCSD American Geophysical Union (AGU)
Résumé : International audience
This paper presents a new balanced structural cross-section of the Jaca thrust-sheet-top basin of the southern Pyrenees combined with paleo-thermometry and apatite fission track (AFT) thermochronology data. The cross-section, based on field data and interpretation of industrial seismic reflection profiles, allows refinement of previous interpretations of the south-directed thrust system, involving the identification of new thrust faults, and of the kinematic relationships between basement and cover thrusts from the middle Eocene to the early Miocene. AFT analysis shows a southward decrease in the level of fission track resetting, from totally reset Paleozoic rocks and lower Eocene turbidites (indicative of heating to Tmax > ~120 °C), to partially reset middle Eocene turbidites and no/very weak resetting in the upper Eocene-lower Oligocene molasse (Tmax < ~60 °C). AFT results indicate a late Oligocene-early Miocene cooling event throughout the Axial Zone and Jaca Basin. Paleo-maximum temperatures determined by vitrinite reflectance measurements and Raman spectroscopy of carbonaceous material reach up to ~240 °C at the base of the turbidite succession. Inverse modelling of AFT and vitrinite reflectance data with the QTQt software for key samples show compatibility between vitrinite-derived Tmax and the AFT reset level for most of the samples. However, they also suggest that the highest temperatures determined in the lowermost turbidites correspond to a thermal anomaly rather than burial heating, possibly due to fluid circulation during thrust activity. From these results, we propose a new sequential restoration of the south Pyrenean thrust system propagation and related basin evolution.
ISSN: 0278-7407

insu-01312746
https://hal-insu.archives-ouvertes.fr/insu-01312746
https://hal-insu.archives-ouvertes.fr/insu-01312746/document
https://hal-insu.archives-ouvertes.fr/insu-01312746/file/Labaume_et_al-2016-Tectonics.pdf
DOI : 10.1002/2016TC004192

Résumé : The dynamism of small-scale fishing since the end of the sixties was able to slow the fall in employment observed since after the war in the fishing sector. If changes in the number of small-scale fishermen correspond to those of the entire primary sector, two contrasted examples, that of Martinique's small-scale fishing and that of the Boulonnais sole trammel netters, will bring out the influence of the peculiarities of this sector as well as that of the general economic environment on employment. After the first section devoted to the general evolution of employment in the fishing sector, the second section will focus on studying the influence of public assistance on the situation of Martinique's fishing industry. The third section will be devoted to the growth of coastal fishing in the Boulogne region with the sole trammel netters. The conclusion will place these two examples side by side in order to emphasize the whole of the factors to be taken into account to analyse employment in this business sector.
Le dynamisme de la pêche artisanale depuis la fin des années soixante-dix a permis de ralentir la chute de l'emploi observée depuis l'après-guerre dans le secteur de la pêche. Si l'évolution du nombre de pêcheurs artisans correspond à celle de l'ensemble du secteur primaire, deux exemples contrastés, celui de la pêche artisanale martiniquaise et celui des trémailleurs à sole boulonnais, permettront de mettre en relief l'influence des particularités de ce secteur ainsi que celle de l'environnement économique général sur l'emploi. Après une première section consacrée à l'évolution générale de l'emploi dans le secteur de la pêche, la seconde section s'attachera à étudier l'influence des aides publiques sur la situation de la pêche martiniquaise. La troisième section sera consacrée au développement de la petite pêche dans la région de Boulogne avec les trémailleurs à sole. La conclusion mettra en parallèle ces deux exemples afin de souligner l'ensemble des éléments à prendre en compte pour analyser l'emploi dans ce secteur d'activité.

Droits : info:eu-repo/semantics/openAccess
http://archimer.ifremer.fr/doc/1989/rapport-2482.pdf
http://archimer.ifremer.fr/doc/00000/2482/

Éditeur(s) : Institut national agronomique Paris Grignon
Résumé : The flat oyster Ostrea edulis L. is the indigenous oyster of the Atlantic as well as the Mediterranean coasts of Europe. Its commercial exploitation dates back to Antiquity but its breeding is now threatened by two parasitic protozoa, among which Bonamia ostreae. Various aspects of the genetics of this species' natural and farmed populations have been studied with the aid of microsatellite markers. At first, the implementation and the screening of two partial genomic libraries made it possible to identify 28 new microsatellite loci. Analysis of the segregation of 12 of these loci and of two enzymatic loci shows that most microsatellite loci are transmitted in a Mendelian way, but some loci have significant segregation distortions. Moreover, seven linkage groups, of which four contain at least two markers, were identified in Ostrea edulis. The genetic variability of three populations selected for one or two generations for resistance to Bonamia ostreae was analysed with the aid of 5 microsatellite loci. In spite of the absence of genealogical data, we have shown that these selected populations were descended from a very low number of founding genitors (from 3 to 15 depending on the population) and for two populations, we were able to reconstruct the genealogy and the relationships between the individuals were identified. These selected populations have, in addition to a very low genetic variability, real and at times high levels of consanguinity. These results have a significant implication for the continuation of the selection programme (consanguinity management, augmentation of genetic variability by introducing wild genitors). The geographical structuring of the genetic variability of natural populations of Ostrea edulis has been analysed with the aid of 5 microsatellite loci on a sampling covering almost the entire distribution area of the species (from Norway to the Adriatic Sea). The results are consistent with those published in the literature and using enzymatic markers. The populations show a low level of differentiation that could correspond to a model of isolation by distance. The Atlantic populations, which have a reduced polymorphism, could be descended from post-glacial recolonisation from Mediterranean populations that had survived the glaciations of the Quaternary Period. The current distribution of flat oyster populations is surely also subject to anthropogenic activities. Finally, the genetic bases of the heterozygosis-growth correlation were studied in a natural population with the aid of enzymatic and microsatellite markers. Although leads favouring the direct contribution of enzymatic loci have been found, biases in the sampling design make it impossible to come to a formal conclusion. However, this study has made it possible to show that the capture of individuals over a short period (around ten days) leads to a sampling of a population descended from a very low number of founding genitors, in contradiction with the generally accepted idea that marine bivalve populations are large panmictic populations with significant, efficient numbers. These results confirm in a natural population the observations of a significant reduction of efficient sizes in hatchery populations.
L'huître plate Ostrea edulis L. est l'huître indigène des côtes européennes aussi bien atlantiques que méditerranéennes. Son exploitation commerciale remonte à l'Antiquité mais son élevage est aujourd'hui menacé par deux protozoaires parasites dont Bonamia ostreae. Différents aspects de la génétique des populations naturelles et cultivées de cette espèce ont été étudiés à l'aide de marqueurs microsatellites. Dans un premier temps, la réalisation et le criblage de deux banques génomiques partielles ont permis l'identification de 28 nouveaux locus microsatellites. L'analyse de la ségrégation de 12 de ces locus et de deux locus enzymatiques montre que la plupart des locus microsatellites sont transmis de façon mendélienne, mais certains locus présentent des distorsions de ségrégation importantes. Par ailleurs, sept groupes de liaison dont quatre contiennent au moins deux marqueurs ont été identifiés chez Ostrea edulis. La variabilité génétique de trois populations sélectionnées depuis une ou deux générations pour une résistance à Bonamia ostreae a été analysée à l'aide de 5 locus microsatellites. Malgré l'absence de données généalogiques, nous avons montré que ces populations sélectionnées étaient issues d'un très faible nombre de géniteurs fondateurs (de 3 à 15 selon les populations) et pour deux populations, la généalogie a pu être reconstituée et les liens de parenté entre les individus ont été identifiés. Ces populations sélectionnées présentent, outre une très faible variabilité génétique, des niveaux de consanguinité réels et parfois élevés. Ces résultats ont une implication importante pour la continuation du programme de sélection (gestion de la consanguinité, augmentation de la variabilité génétique par introduction de géniteurs sauvages). La structuration géographique de la variabilité génétique des populations naturelles d'Ostrea edulis a été analysée à l'aide de 5 locus microsatellites sur un échantillonnage couvrant presque toute l'aire de répartition de l'espèce (de la Norvège à la Mer Adriatique). Les résultats sont cohérents avec ceux publiés dans la littérature et utilisant des marqueurs enzymatiques. Les populations montrent un niveau de différenciation faible qui pourrait correspondre à un modèle d'isolement par la distance. Les populations atlantiques, qui présentent un polymorphisme réduit, pourraient être issues de recolonisation post-glaciaire à partir de populations méditerranéennes ayant survécu aux glaciations du Quaternaire. La répartition actuelle des populations d'huître plate est certainement aussi soumise aux actions anthropiques. Enfin, les bases génétiques de la corrélation hétérozygotie-croissance ont été étudiées dans une population naturelle à l'aide de marqueurs enzymatiques et microsatellites. Bien que des pistes en faveur de la contribution directe des locus enzymatiques aient été trouvées, des biais dans le dispositif expérimental ne permettent pas de conclure de façon formelle. Cependant, cette étude a permis de montrer que le captage d'individus sur une faible période (une dizaine de jours) conduit à l'échantillonnage d'une population issue d'un nombre très réduit de géniteurs fondateurs, en contradiction avec l'idée reçue que les populations de bivalves marins sont de larges populations panmictiques à effectif efficace important. Ces résultats confirment dans une population naturelle les observations de réduction importante des tailles efficaces dans des populations d'écloserie.

Droits : info:eu-repo/semantics/openAccess
http://archimer.ifremer.fr/doc/1998/these-1919.pdf
http://archimer.ifremer.fr/doc/00000/1919/

Éditeur(s) : HAL CCSD
Résumé : International audience
Since long years, the archaeologists have analyzed the migrations link to the pre-Columbian settlement of the Antillean archipelago. On an other hand, the researches about the origins of the raw materials have demonstrated the importance of the inter-insular exchanges, exchanges not only of material elements but even of concepts and persons. This is those relations who permitted the development of real Antillean civilizations. Sadly, the off shore canoe, real civilizational tool, and the different aspects link to is utilization have been frequently absent of the discussion or only analyzed from a theoretical point of view by the meaning of modelization tries. The "Ioumoúlicou" project we will present now is an experimental archaeological program dedicated to the study of the pre-Columbian navigation conditions and techniques. Those works realized in a scientifically controlled frame completed by a canoe hydrostatic parameters analysis, gave us the possibility to obtain totally original data. Those data give us an opportunity to refund our vision of the relation of the pre-Columbian peoples with the archipelagic Antillean space.
Depuis plusieurs décennies, les recherches archéologiques ont mis en évidence plusieurs mouvements migratoires à l'origine du peuplement précolombien de l'archipel antillais. D'autre part, les travaux réalisés sur l'origine des matières premières ont permis de souligner l'importance des échanges inter-insulaires, des échanges de biens matériels mais aussi d'idées et de personnes. Ce sont ces relations qui ont permis le développement de véritables civilisations antillaises. Malheureusement, le canot de haute mer, véritable outil civilisationnel, et les différents aspects liés à son utilisation ont trop souvent été les grands absents du débat ou approchés uniquement d'une point de vue théorique au travers de tentatives de modélisation. Le projet "Ioumoúlicou" que nous allons vous présenter ici correspond à un programme d'archéologie expérimentale sur les techniques et les conditions de navigation précolombiennes dans les Antilles. Ces travaux réalisés dans un cadre scientifique contrôlé et complétés par une analyse des caractéristiques hydrostatiques du canot, nous ont ainsi permis d'obtenir un ensemble de données tout à fait inédites. Elles nous permettent de refonder notre approche de la relation des populations précolombiennes à l'espace archipélique antillais.
The Proceedings of the XXIII Congress of the International Association for Caribbean Archaeology, Antigua, 29 june-3 july 2009

hal-00966520
https://hal.univ-antilles.fr/hal-00966520
https://hal.univ-antilles.fr/hal-00966520/document
https://hal.univ-antilles.fr/hal-00966520/file/ioumoulicou.pdf

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
The Hengshan–Wutaishan area forms part of the Trans-North-China Belt developed in response to the final amalgamation of the North China Craton. The Hengshan–Wutaishan domain and the adjacent Fuping massif constitute the largest and the most representative rock exposure of the belt. A structural study allows us to redefine the lithological and tectonic units that compose the architecture of the Hengshan–Wutaishan domain and to propose that the Trans-North-China Belt was built up through a polyphase tectonic evolution within the period 1900–1800 Ma. The first event (D1) corresponds to the emplacement of lower and upper nappes herein called the Orthogneiss and Volcanites Unit (OVU) and the Low Grade Mafic Unit (LGMU), respectively. The OVU mainly consists of rocks formed in an arc system and metamorphosed under amphibolite facies conditions whereas the LGMU represents oceanic crust rocks with an arc component that underwent greenschist facies metamorphism. The syn-metamorphic D1 deformation is characterized by a NW–SE stretching and mineral lineation with a top-to-the SE sense of shear that corresponds to the sense of nappe motion. U–Th–Pb EPM chemical dating on monazite from three metapelites of the OVU gives isochron ages of 1884 ± 11 Ma, 1886 ± 5 Ma and 1887 ± 4 Ma interpreted as the age of the prograde amphibolite facies metamorphism coeval with nappe stacking during the D1 event. The D2 event corresponds to a widespread crustal melting of the OVU and underlying basement rocks in Hengshan related to the exhumation of deep structures about 20–30 Ma after nappe emplacement. The migmatite contains blocks of retrograded eclogite or HP-granulitic restites, and is characterized by the development of a pervasive foliation and lineation. A late D2 event represents the folding stage of the migmatitic foliation during the completion of a dome. The Orthogneiss and Volcanics Unit and the Low Grade Mafic Unit are unconformably covered by weakly metamorphosed to unmetamorphosed sediments belonging to the Hutuo Supergroup. These rocks were deformed by a ductile D3 event, characterized by a NW–SE trending stretching lineation, south verging folds associated with an axial planar slaty cleavage and an E–W crenulation lineation. Lastly, a left-lateral wrenching along the Zhujiafang Shear Zone separates the northern and southern parts of Hengshan. Our structural study shows that there is no significant difference between the southern part of Hengshan and the lower part of Wutaishan, both areas belong to OVU and show a structural continuity. We suggest that this polyphase deformation developed in response to a north-westward subduction of an old ocean, named the Lüliang Ocean, beneath the Western Block, followed by collision with a micro-continent named the Fuping Block at not, vert, similar1890–1880 Ma.
ISSN: 0301-9268

insu-00151594
https://hal-insu.archives-ouvertes.fr/insu-00151594
https://hal-insu.archives-ouvertes.fr/insu-00151594/document
https://hal-insu.archives-ouvertes.fr/insu-00151594/file/Trap-PrecambrainResearch-2007.pdf
DOI : 10.1016/j.precamres.2007.03.001