Éditeur(s) : Université des Antilles Études caribéennes
Résumé : Le territoire d’Aysen, au sud du Chili, officiellement dénommé « Région XI », possède le charme discret d’une Patagonie oubliée. Cette région mythique n’a cessé de hanter l’imaginaire fécond des découvreurs et voyageurs en tout genre. Aujourd’hui, ces derniers sont autant des pêcheurs à la mouche fortunés que des routards européens ou israéliens, et de plus en plus des Chiliens venus des classes moyennes et du nord du pays. La Patagonie est un formidable terrain de jeu, et plus encore un vaste espace d’utopie, hier comme aujourd’hui, pour nombre de voyageurs et rêveurs.Le « charme » est indéniable, il suffit de contempler la nature qui domine ici la culture, et la région n’est pas un paradis pour les photographes par hasard ; quant au caractère « discret », il est également évident, comme en témoignent de nombreux touristes en quête de leur propre expérience “into the wild” et qui s’émerveillent en foulant ces sentiers non battus de la Patagonie. Terre de jeu pour aventuriers, lieu de science pour les chercheurs, espace de refuge pour de riches expatriés, territoire d’expérimentation sinon de rite de passage pour quelques jeunes et sportifs, marcheurs, cyclistes ou flâneurs, la Patagonie chilienne est désormais surtout devenue un enjeu, économique et donc politique, essentiel pour le pays.Cet article, fruit d’un travail en cours, apporte quelques éléments pour tenter de comprendre comment se fabrique et s’établit, dans le temps et dans l’espace, « une destination non touristique » qui, depuis ces dernières années, à la faveur des médias, mais pas seulement, a le vent en poupe. Avec ou sans le consentement des Patagons/Patagoniens ? C’est tout le véritable défi à venir.
The territory of Aysen in southern Chile, officially called "Region XI" has the discreet charm of a forgotten Patagonia. This legendary region has haunted the fertile imagination of explorers and travelers of all kinds. Today, they are so many rich fly fishermen that European or Israeli backpackers, and always more Chileans coming from the middle class and from the north of the country. Patagonia is a wonderful playground, and even more a vast space of utopia, then as now, for many travelers and dreamers.The "charm" is undeniable, simply contemplate the fabulous nature clearly dominating culture here, and the area is not a paradise for photographers by chance. As to the character "discrete", it is also clear, as evidenced by many tourists in search of their own experience "into the wild" and marvel treading the beaten path not of Patagonia. Playground for adventurers, place of science for researchers, refuge area for fortunate expatriates testing ground if not some rite of passage for young athletes, walkers, cyclists or loafers, Chilean Patagonia is now mostly become an issue, and therefore economic policy, rather essential for the country.This article, the first result of a work in progress, brings some elements to try to understand how to manufacture and settled in time and space, "a non-tourist destination", which, in recent years, the for the media but not only has the wind in its sails. With or without the consent of all the habitants of Patagonia? This is the real challenge ahead.
Chili

Droits : info:eu-repo/semantics/openAccess
urn:doi:10.4000/etudescaribeennes.7402
http://journals.openedition.org/etudescaribeennes/7402

Éditeur(s) : Elsevier
Résumé : The distribution and speciation of mercury (Hg) in the water column, the inputs (wet deposition and tributaries) and the outputs (atmospheric evasion and outlet) of an artificial partially anoxic tropical lake (Petit-Sa-Lit reservoir, French Guiana) were investigated oil a seasonal basis in order to appraise the cycling and transformations of this metal. The total mercury (HgT) concentrations in the oxygenated epilimnetic waters averaged 5 +/- 3 pmol L-1 in the unfiltered samples (HgTUNF) and 4 +/- 2 pmol L-1 in the dissolved (HgTD) phase (< 0.45 mu m). On average, the monomethylmercury (MMHg) constituted 8%, 40%, and 18% of the HgT in the dissolved phase, tile particulate suspended matter and in tile unfiltered samples, respectively. Covariant elevated concentrations of particulate MMHg and chlorophyll a in the epilimnion suggest that phytoplankton is ail active component for the MMHg transfer in tile lake. In the anoxic hypolimnion the HgTUNF averages 13 +/- 6 pmol L-1 and tile HgTD 8 +/- 4 pmol L-1. The averages of MMHgP and MMHgD in hypolimnetic waters were two and three times the corresponding values of the epilimnion, 170 +/- 90 pmol g(-1) and 0.9 +/- 0.5 pmol L-1, respectively. In the long dry and wet seasons, at the flooded forest and upstream dam sampling stations, the vertical profiles of MMHgD concentrations accounted for two distinct maxima: one just below the oxycline and the other near the benthic interface. Direct wet atmospheric deposition accounted for 14 moles yr(-1) HgTUNF, with 0.7 moles yr(-1) as MMHgUNF, while circa 76 moles yr(-1) of HgTUNF, with 4.7 moles yr(-1) as MMHgUNF, coming from tributaries. Circa 78 moles (similar to 17% as MMHg) are annually exported through tile dam, while 23 moles yr(-1) of Hg-0 evolve in the atmosphere. A mass balance calculation suggests that the endogenic production of MMHgUNF attained 8.1 moles yr(-1), corresponding to a methylation rate of 0.06% d(-1). As a result, tile Petit-Saut reservoir is a large man-made reactor that has extensively altered mercury speciation in favor of methylated species.
Applied Geochemistry (0883-2927) (Elsevier), 2008-05 , Vol. 23 , N. 5 , P. 1101-1126

Droits : 2008 Elsevier Ltd All rights reserved.
http://archimer.ifremer.fr/doc/2008/publication-4198.pdf
DOI:10.1016/j.apgeochem.2007.11.006
http://archimer.ifremer.fr/doc/00000/4198/

Éditeur(s) : Université de Bretagne Occidentale
Résumé : The negative impact of the man on the environment unquestionably increases. The coastal environment as a whole is the maritime environment which is the most exposed to man-made eutrophication. For instance, nitrate loads to coastal waters off Brittany (France) have increased 10 times (from 3 to s 30mg L-1NO3) during the four last decades. Eutrophication of this coastal zone is now a recurrent problem, more and more worrying. This eutrophication exhibits two main forms : " green tides ", which are caused by local proliferations and stranding of green macro-algae (particularly the Ulva species) in nitrogen-enriched areas ; phytoplanktonic blooms, which are responsible for coloured water events, toxic species can be present (Pseudo-Nitzschia, Alexandrium, Dinophysis), and induce banning of shellfish consumption. The objectives of this study are to assess the respective role of various rivers (especially the Loire and the Vilaine) in the eutrophication of the Brittany shelf ecosystem and test the impact of nitrogen enrichment in the triggering of Pseudo-Nitzchia toxicity. For these purposes, a coupled hydrodynamical/ biogeochemical 3D model has been developed and validated against past measured time-series and satellite images. After a brief analysis of primary production over the Brittany shelf under different conditions, we show a description of the real time adaptation of this model. Daily results are currently presented in real time on www.previmer.org web site. The inability of the model to correctly simulate near shore phytoplankton is worsened in this model by the fact that the turbidity field used is a climatological one, made by satellite images averaged on a decadal basis. First, near shore pixels of satellite images are scarcely reliable, secondly a climatological mean cannot represent the sudden bursts or drops of the real turbidity, highly dependent on the actual sea-state : this can explain also why the model at this moment fails to reproduce a sudden bloom occurring in a short period of sunny and calm weather. The simulated Pseudo-Nitzschia biomass and induced risk of toxicity in the water column cannot really be validated offshore, because monitoring measurements are available only near the coast, and deal only with toxicity in benthic filter feeders. To get temporarily rid of that problem, an interesting improvement would be to add to the operational model the bio-accumulation of toxin in the shellfishes : simulated concentrations in shellfish fresh would become directly comparable with usual measurements of the monitoring networks. Our model points out the important impact of Loire river loads on the primary production on the western and southern Brittany. This result is crucial for administrations in charge of reducing the terrestrial loadings responsible for eutrophication, because it can delay reduction programs on small tributaries until the main input from the Loire has been significantly reduced. A question arises, about the reliability of the haline stratification in the model, because the horizontal extent of the Loire plume will be enhanced by a stronger stratification.
L'eutrophisation des milieux marins côtiers, de plus en plus importante, représente un des impacts majeurs des activités humaines sur l'environnement. Les phénomènes d'eutrophisation sont en constante augmentation ; ces dernières décennies ont vu le nombre de sites touchés augmenter de par le monde. La bande côtière bretonne est particulièrement concernée par ce phénomène. L'eutrophisation s'y manifeste de deux façons : "Des phénomènes de marée vertes, très localisées, qui sont provoqués par la croissance excessive et l'échouage de macro-algues du genre Ulva dans ces zones riches en azote ; Des blooms de phytoplancton à l'origine des phénomènes d'eaux colorées, qui peuvent aussi provoquer des interdictions de consommation de coquillages lorsque les espèces mises en jeu sont toxiques (Pseudo-Nitzschia, Alexandrium, Dinophysis). L'objectif de ce travail est multiple : il vise à mettre en évidence et à comprendre l'impact et le rôle des apports en nutriments sur la production primaire et l'eutrophisation des milieux côtiers. Ce travail a aussi pour ambition l'identification et la compréhension des causes des phénomènes d'eutrophisation et permettre ainsi d'apporter des solutions ou des pistes d'amélioration. En n, il a aussi un objectif de prévision à court terme de l'état biologique sur la zone. Pour atteindre ces objectifs, un modèle en temps réel a été mis en oeuvre. Les résultats de simulations numériques et de mesures satellitaires sont présentés sur internet : www.previmer.org. L'outil principal de ce travail est un modèle couplé physique/biogéochimie. La partie hydrodynamique est fournie par le code Mars3D (3D hydrodynamical Model for Application at Regional Scale) développé à IFREMER. Au code hydrodynamique Mars3D est couplé le modèle des cycles de l'azote, du phosphore et du silicium d'IFREMER. Le modèle couplé permet de simuler en 3 dimensions et de manière dynamique les courants, le brassage horizontal et vertical, les champs de température et de salinité, mais aussi les principaux cycles de nutriments, reproduisant ainsi les conditions déterminantes de la production primaire. La croissance des algues est modélisée, et nous permet de voir l'influence des panaches de dilution des principales rivières bretonnes sur leur croissance. Les diffcultés du modèle à correctement simuler les concentrations en phytoplancton près des zones côtières, sont probablement dues à l'utilisation d'une climatologie de concentration en matière en suspension fondée sur des données satellitaires. Tout d'abord, les pixels côtiers des images satellitaires sont entachés d'erreurs, ensuite une climatologie n'est pas capable de représenter les apports soudains des fleuves lors des crues. Cela peut expliquer l'incapacité du modèle a représenter certains blooms liés à des périodes ensoleilées et calmes. A ce modèle de base nous avons ajouté un genre spécifique de phytoplancton : le genre Pseudo-Nitzschia. Certaines espèces de Pseudo-Nitzschia sont réputées toxiques. En effet, ce phytoplancton a la capacité de synthétiser une toxine : l'acide domoïque. Cette toxine est responsable du syndrome ASP (Amnesic Shellfish Poisoning). Le modèle reproduit globalement les mêmes zones de toxicité que les mesures du REPHY, et donne des résultats encourageants. L'étude montre que la Loire influence une large partie de la bande côtière bretonne ; son panache remonte jusqu'au nord de la mer d'Iroise, et contribue pour une grande part à l'enrichissement du sud et de l'ouest de la Bretagne. Le traçage de l'azote en provenance de la Loire au sein des cycles biogéochimiques nous a permis de quantifier cet enrichissement.

Droits : info:eu-repo/semantics/openAccess
http://archimer.ifremer.fr/doc/00015/12603/9481.pdf
http://archimer.ifremer.fr/doc/00015/12603/

Éditeur(s) : Wiley / Blackwell
Résumé : P>The distribution of the archaeal communities in deep subseafloor sediments [0-36 m below the seafloor (mbsf)] from the New Caledonia and Fairway Basins was investigated using DNA- and RNA-derived 16S rRNA clone libraries, functional genes and denaturing gradient gel electrophoresis (DGGE). A new method, Co-Migration DGGE (CM-DGGE), was developed to access selectively the active archaeal diversity. Prokaryotic cell abundances at the open-ocean sites were on average similar to 3.5 times lower than at a site under terrestrial influence. The sediment surface archaeal community (0-1.5 mbsf) was characterized by active Marine Group 1 (MG-1) Archaea that co-occurred with ammonia monooxygenase gene (amoA) sequences affiliated to a group of uncultured sedimentary Crenarchaeota. However, the anoxic subsurface methane-poor sediments (below 1.5 mbsf) were dominated by less active archaeal communities, such as the Thermoplasmatales, Marine Benthic Group D and other lineages probably involved in the methane cycle (Methanosarcinales, ANME-2 and DSAG/MBG-B). Moreover, the archaeal diversity of some sediment layers was restricted to only one lineage (Uncultured Euryarchaeota, DHVE6, MBG-B, MG-1 and SAGMEG). Sequences forming two clusters within the Thermococcales order were also present in these cold subseafloor sediments, suggesting that these uncultured putative thermophilic archaeal communities might have originated from a different environment. This study shows a transition between surface and subsurface sediment archaeal communities.
Environmental Microbiology (1462-2912) (Wiley / Blackwell), 2009-09 , Vol. 11 , N. 9 , P. 2446-2462

Droits : 2009 Society for Applied Microbiology and Wiley - Blackwell Publishing Ltd.
http://archimer.ifremer.fr/doc/2009/publication-6801.pdf
DOI:10.1111/j.1462-2920.2009.01976.x
http://archimer.ifremer.fr/doc/00000/6801/

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
Subduction processes play a major role in plate tectonics and the subsequent geological evolution of Earth. This special issue focuses on ongoing research in subduction dynamics to a large extent (oceanic subduction, continental subduction, obduction…) for both past and active subduction zones and into mountain building processes and the early evolution of orogens. It puts together various approaches combining geophysics (imaging of subduction zones), petrology/geochemistry (metamorphic analysis of HP-UHP rocks, fluid geochemistry and magmatic signal, geochronology), seismology and geodesy (present-day evolution of subduction zones, active tectonics), structural geology (structure and evolution of mountain belts), and numerical modelling to provide a full spectrum of tools that can be used to constrain the nature and evolution of subduction processes and orogeny. Studies presented in this special issue range from the long-term (orogenic cycle) to short-term (seismic cycle).
ISSN: 0264-3707

insu-01287985
https://hal-insu.archives-ouvertes.fr/insu-01287985
https://hal-insu.archives-ouvertes.fr/insu-01287985/document
https://hal-insu.archives-ouvertes.fr/insu-01287985/file/rolland-2016.pdf
DOI : 10.1016/j.jog.2016.03.006

Éditeur(s) : HAL CCSD American Geophysical Union (AGU)
Résumé : International audience
We studied the patterns, rates and evolution of fluvial terraces and fault system during the building process of an intracontinental transpressional mountain in the Gobi-Altay (Mongolia). By analyzing incisions and offsets of fluvial terraces and alluvial fans, we show that the massif has grown by outward migration of thrust faults through time. On the northern flank, the present bounding thrust fault began its activity ~600 ka ago, while a more internal sub-parallel fault was still active until ~200-100 ka. Vertical offset of an alluvial fan abandoned ~100 ka ago allows an estimate of 0.1 mm/yr Upper Pleistocene - Holocene uplift rate. The morphology of the catchment-piedmont system strongly suggests a periodical formation of the alluvial surfaces, controlled by the climatic pulses, at the beginning of the wet interglacial periods. The abandonment of the alluvial terraces lags by several thousand years the abandonment of the alluvial fans, showing a diachronous incision propagating upstream. The incision rate deduced from the different elevations of straths exceeds of one order of magnitude the rock uplift rate. This excess is mostly due to ongoing drainage network growth at the core of the massif, and incision due to alluvial apron entrenchment near the outlet. This implies that fluvial response is mainly controlled by drainage growth, interaction with piedmont and cyclic climatic variations, rather than by rock uplift.
ISSN: 0278-7407

hal-00323558
https://hal.archives-ouvertes.fr/hal-00323558
https://hal.archives-ouvertes.fr/hal-00323558v2/document
https://hal.archives-ouvertes.fr/hal-00323558/file/Vassallo2007.pdf
DOI : 10.1029/2006TC002081

Éditeur(s) : HAL CCSD Taylor & Francis
Résumé : International audience
This work evaluates the influence of three different intensities of refinement of sisal pulp and the effect of accelerated aging cycles on the behavior of composites. Fiber-cements were prepared by the slurry de-watering method and pressing as a crude simulation of the Hatschek process. Mechanical behavior of composites was evaluated by four-point bending test at 28 days, and after 50 and 100 wet/dry cycles. Refinement of pulp and aging have increased the strength and bulk density of composites and decreased the toughness and porosity. The best mechanical performance after aging was achieved for samples with highly refined fibers.
ISSN: 1042-6914

hal-00809817
https://hal.univ-antilles.fr/hal-00809817
DOI : 10.1080/10426910601062065

Éditeur(s) : HAL CCSD Oxford University Press (OUP)
Résumé : International audience
We carried out morphotectonic studies along the left-lateral strike-slip Bogd Fault, the principal structure involved in the Gobi-Altay earthquake of 1957 December 4 (published magnitudes range from 7.8 to 8.3). The Bogd Fault is 260 km long and can be subdivided into five main geometric segments, based on variation in strike direction. West to East these segments are, respectively: the West Ih Bogd (WIB), The North Ih Bogd (NIB), the West Ih Bogd (WIB), the West Baga Bogd (WBB) and the East Baga Bogd (EBB) segments. Morphological analysis of offset streams, ridges and alluvial fans-particularly well preserved in the arid environment of the Gobi region-allows evaluation of late Quaternary slip rates along the different faults segments. In this paper, we measure slip rates over the past 200 ka at four sites distributed across the three western segments of the Bogd Fault. Our results show that the left-lateral slip rate is similar to 1 mm yr(-1) along the WIB and EIB segments and similar to 0.5 mm yr(-1) along the NIB segment. These variations are consistent with the restraining bend geometry of the Bogd Fault.;Our study also provides additional estimates of the horizontal offset associated with the 1957 earthquake along the western part of the Bogd rupture, complementing previously published studies. We show that the mean horizontal offset associated with the 1957 earthquake decreases progressively from 5.2 m in the west to 2.0 m in the east, reflecting the progressive change of kinematic style from pure left-lateral strike-slip faulting to left-lateral-reverse faulting. Along the three western segments, we measure cumulative displacements that are multiples of the 1957 coseismic offset, which may be consistent with a characteristic slip. Moreover, using these data, we re-estimate the moment magnitude of the Gobi-Altay earthquake at M-w 7.78-7.95.;Combining our slip rate estimates and the slip distribution per event we also determined a mean recurrence interval of similar to 2500-5200 yr for past earthquakes along the different segments of the western Bogd Fault. This suggests that the three western segments of the Bogd Fault and the Gurvan Bulag thrust fault (a reverse fault bounding the southern side of the Ih Bogd range that ruptured during the 1957 earthquake) have similar average recurrence times, and therefore may have ruptured together in previous earthquakes as they did in 1957. These results suggest that the western part of the Bogd Fault system, including the Gurvan Bulag thrust fault, usually behaves in a 'characteristic earthquake' mode.
ISSN: 0956-540X

hal-00639467
https://hal.archives-ouvertes.fr/hal-00639467
https://hal.archives-ouvertes.fr/hal-00639467v2/document
https://hal.archives-ouvertes.fr/hal-00639467/file/rizzaGJI2011.pdf
DOI : 10.1111/j.1365-246X.2011.05075.x

Éditeur(s) : HAL CCSD International Aroid Society
Résumé : International audience
ISSN: 0197-4033

hal-01095862
https://hal-agroparistech.archives-ouvertes.fr/hal-01095862

Résumé : Arsenic levels of in the marine environment are high in comparison with other contaminants. Over the past twenty years, a large number of arsenic organic compounds have been identified in the water, sediments and living species. This document constitutes a synthesis of current knowledge on arsenic sources, and contamination levels, on its biogeochemical cycle as well as its toxic effects on human and marine fauna. This paper highlights in particular the effects of phosynthesis on arsenic speciation and its distribution throughout the marine environment. Problems of toxicity in the case of certain phyto- and zooplankton species are identified. Bioaccumulation in seaweeds, molluscs and fishes is documented as well, with special attention to the species encountered in the French coastal waters.
Les niveaux de présence de l'arsenic en milieu marin sont élevés comparativement à d'autres contaminants. Depuis une vingtaine d'années, de nombreux composés organiques de l'arsenic ont été identifiés dans l'eau, les sédiments et les espèces vivantes. Le présent document constitue une synthèse des connaissances sur les sources et les niveaux de contamination, le cycle biogéochimique, les effets toxiques pour l'homme et les espèces marines. L'accent est mis notamment sur les effets de la photosynthèse sur la spéciation de cet élément et sur sa distribution dans le milieu. Les problèmes de toxicité pour certaines espèces phyto- et zooplanctonniques sont identifiés. La bioaccumulation chez les algues, les mollusques et les poissons est bien documentée, avec une attention particulière pour les espèces présentes dans les eaux côtières françaises.

Droits : info:eu-repo/semantics/openAccess
http://archimer.ifremer.fr/doc/1993/rapport-1448.pdf
http://archimer.ifremer.fr/doc/00000/1448/

Éditeur(s) : HAL CCSD National Research Council Canada
Résumé : International audience
Spadix temperature was measured in three species of Philodendron: P. acutatum, P. pedatum and P.solimoesense. These species showed two different patterns of spadix temperature during their flowering cycle.In P. acutatum and P. pedatum (subgenus Philodendron), the spadix warmed up twice during the beginning ofeach flowering night with a temperature not significantly different from that of ambient air between the twopeaks. In P. solimoesense (subgenus Meconostigma), the spadix temperature rose up to 14oC above that ofambient air during the first night, then it progressively cooled down but remained 3-6oC above ambient airtemperature. We propose that the heat production and the spadix temperature patterns observed may reflectdifferent physiological processes and have a taxonomic significance in the genus Philodendron.
ISSN: 0008-4026

hal-01202714
https://hal.archives-ouvertes.fr/hal-01202714

Éditeur(s) : HAL CCSD Ecological Society of America
Résumé : Herbivory is viewed as a major driver of plant evolution and the mostimportant energy pathway from plants to higher trophic levels. Therefore, understandingpatterns of herbivory on plants remains a key focus in evolution and ecology. Theevolutionary impacts of leaf herbivory include altering plant fitness, local adaptation, theevolution of defenses, and the diversification of plants as well as natural enemies. Leafherbivory also impacts ecological processes such as plant productivity, communitycomposition, and ecosystem nutrient cycling. Understanding the impact of herbivory onthese ecological and evolutionary processes requires species-specific, as opposed tocommunity-level, measures of herbivory. In addition, species-specific data enables the use ofmodern comparative methods to account for phylogenetic non-independence. Althoughhundreds of studies have measured natural rates of leaf consumption, we are unaware of anyaccessible compilation of these data. We created such a data set to provide the raw dataneeded to test general hypotheses relating to plant–herbivore interactions and to test theinfluence of biotic and abiotic factors on herbivory rates across large spatial scales. A largerepository will make this endeavor more efficient and robust. In total, we compiled 2641population-level measures for either annual or daily rates of leaf herbivory across 1145 speciesof vascular plants collected from 189 studies. All damage measures represent naturaloccurrences of herbivory that span numerous angiosperm, gymnosperm, and fern species. Toenable researchers to explore the causes of variation in herbivory and how these mightinteract, we added information about the study sites including: geolocation, climateclassification, habitat descriptions (e.g., seashore, grassland, forest, agricultural fields), andplant trait information concerning growth form and duration (e.g., annual vs. perennial). Wealso included extensive details of the methodology used to measure leaf damage, includingseasons and months of sampling, age of leaves, and the method used to estimate percentagearea missing. We anticipate that these data will make it possible to test important hypothesesin the plant–herbivore literature, including the plant apparency hypothesis, the latitudinalherbivorydefense hypothesis, the resource availability hypothesis, and the macroevolutionaryescalation of defense hypothesis.
ISSN: 0012-9658

hal-01601627
https://hal.archives-ouvertes.fr/hal-01601627
DOI : 10.1890/13-1741.1
PRODINRA : 397136
PUBMED : 24870043

Éditeur(s) : HAL CCSD Wiley
Résumé : Tank bromeliads form a conspicuous, yet neglected freshwater habitat in Neotropical forests. Recent studies driven by interests in medical entomology, fundamental aspects of bromeliad ecology and experimental research on food webs have, however, prompted increasing interest in bromeliad aquatic ecosystems. As yet, there is nothing in the literature about the life histories and environmental drivers of invertebrate population dynamics in tank bromeliads. Based on fortnightly samples taken over oneyear, size frequency plots and individual dry masses allowed us to establish the life cycles and growth rates of the dominant aquatic invertebrates in a common bromeliad species of French Guiana. Linear mixed-effect models and Mantel tests were used to predict changes in density, biomass, and growth rates in relation to temperature, rainfall, humidity and detrital resources. Annual variations in invertebrate densities and biomasses could be described according to three types of distribution: unimodal, bimodal or almost constant. Despite seasonal variations, precipitation, temperature, relative humidity and detritus concentration accounted significantly for changes in density and biomass, but we found no significant responses in growth rates of most invertebrate species. Species rather displayed non-seasonal life cycles with overlapping cohorts throughout the year. There was also a trend for delayed abundance peaks among congeneric species sharing similar functional traits, suggesting temporal partitioning of available resources. Beyond novel knowledge, quantitative information on life histories is important to predict food-web dynamics under the influence of external forcing and self-organisation. Our results suggest that changes in species distribution that will affect population dynamics through biotic interactions in space and/or time could have greater effects on food webs and ecosystem functioning than changes in environmental factors per se.
ISSN: 0046-5070

hal-01607779
https://hal.archives-ouvertes.fr/hal-01607779
DOI : 10.1111/fwb.12862
PRODINRA : 407311

Éditeur(s) : American Geophysical Union
Résumé : [1] A multiproxy integrated chronological framework, based on oxygen and carbon stable isotope stratigraphy, biostratigraphy (foraminifera and nannoplankton bioevents and foraminifer assemblage-based climate cyclicity), magnetostratigraphy, sapropel stratigraphy, and C-14 AMS radiometric dates, has been achieved for borehole PRAD1-2, collected in 185.5 m water depth in the central Adriatic. This work was carried out within the European Community project Profiles across Mediterranean Sedimentary Systems (PROMESS1). The 71.2 m long borehole spans a time interval between late MIS 11 and MIS 1 (the last 370 ka), showing a chronological resolution of 500 and 250 years per cm during interglacial and glacial intervals, respectively. At present, this record is the most expanded and continuous marine record available for the Adriatic Basin. Several orbital cycles can be recognized in the PRAD1-2 record: the 100 ka glacial-interglacial fluctuations and the 23 ka precession-related cycles, which in turn control the deposition of sapropel layers. An integrated analysis of short-term oscillations within the Last Glaciation interval (MIS 4-MIS 2) allowed the identification of the Adriatic signature of Dansgaard-Oeschger events, showing the potential to achieve a more refined chronostratigraphic framework for the top part of the PRAD1-2 record. Finally, the age model obtained by this study allowed the chronological integration of the main foraminifera bioevents detected in the borehole as well as of the volcanoclastic layers present in the upper part of the record. Despite its proximal location, PRAD1-2 presents a continuous record and shows the potential to be consistently correlated both with deep-sea and continental records in the Mediterranean region and beyond.
Geochemistry Geophysics Geosystems (1525-2027) (American Geophysical Union), 2008 , Vol. 9 , P. NIL_107-NIL_127

Droits : 2008 American Geophysical Union
http://archimer.ifremer.fr/doc/2008/publication-3605.pdf
DOI:10.1029/2007GC001713
http://archimer.ifremer.fr/doc/00000/3605/

Éditeur(s) : HAL CCSD International Federation of Sports Medicine
Résumé : International audience
To study the exercise-induced arterial hypoxaemia (EIAH) kinetics in a world class Ironman triathlete at ventilatory threshold (TH vent), the authors simulated the cycle-run succession (CR, 20 min + 20 min) and a 20-min isolated run (R). Although 'moderate EIAH' was noted during CR, the SpO 2 kinetics of the isolated R reflected 'severe EIAH' from minutes 7 to 15 with a nadir of 85 % SpO 2 that stabilised at 90 % SpO 2 from minute 15 on. The physiological processes involved in these responses are discussed. These data indicate a systematic 'moderate EIAH' in a world class Ironman champion during CR and R at TH vent and a temporary 'severe EIAH' during R, which was attenuated when running was successive to cycling. The physiological significance of this phenomenon remains unclear, however, and further experiments are needed.
ISSN: 1528-3356

hal-01152346
https://hal.univ-antilles.fr/hal-01152346

Éditeur(s) : HAL CCSD Royal Society of Chemistry
Résumé : International audience
Abstract View references (60)Here we show the long term performance at high temperatures of a multi-tube module containing 8 membranes in 4 parallel lines with a total of 545 cm 2 area. The membranes were prepared via thin film dip coating of cobalt oxide silica (CoO xSi) sol-gel on tubular alumina supports. A preliminary study found that the sol-gel containing 20 mol% cobalt oxide formed the best microporous structure with the highest surface area and pore volume. All resulting membranes delivered permeances of ∼1 × 10 -7 mol m -2 s -1 Pa -1 at 500 °C, indicating a high repeatability for the membrane fabrication process. The permselectivities of helium (He) and hydrogen (H 2) over carbon dioxide (CO 2) and nitrogen (N 2) increased from 10-20 at 100 °C to values close to 1000 at 500 °C. Additionally, the apparent energies of activation (E act) for the smaller kinetic diameter gases He and H 2 at 12.2 and 19.5 kJ mol -1 were high and contrary to the negative values for larger gases N 2 and CO 2 at -1.8 and -7.4 kJ mol -1. These remarkable results were attributed to the molecular sieving mechanism of the microporous silica which was enhanced by the embedding of cobalt oxide into the matrix, delivering structural control with an average pore size of 3 Å. The E act for H 2 permeance was higher than that of He, indicating that the cobalt oxide played an important role in H 2 transport. Two membrane lines performed exceptionally well for binary gas mixture processing with H 2 purity reaching values close to 100% in the permeate stream for argon (Ar) concentrations of up to 80% in the retentate stream. A major finding here is that the binary gas selectivity was independent of temperature, contrary to the permselectivity observed for single gas permeance. Further, the H 2 flow rate was greatly affected by the concentration of Ar in the mixture, while the temperature dependency played only a marginal role. In particular, competitive adsorption in the percolative pathways containing pore constrictions or bottlenecks of the anisotropic CoO xSi matrix allowed Ar to impede H 2 diffusion. Finally, the CoO xSi membranes proved thermally stable and robust for 2000 h of testing for various thermal cycles up to 500 °C. © The Royal Society of Chemistry 2012.
Energy & Environmental Science

hal-01683199
https://hal.univ-antilles.fr/hal-01683199
DOI : 10.1039/c2ee03247c

Éditeur(s) : HAL CCSD Université des Antilles
Résumé : International audience
Within thirty years, the small island of Saint-Barthelemy (25 km²) is out of its secular isolation to be among major luxury tourism destinations in the world. In this study, the idea is to identify structural element and different cyclical factors that help to understand Saint-Barthelemy tourism situation. The small size of the territory itself can be seen as a fundamental handicap or, conversely, as a considerable asset. Everything depends on development project. It is necessary to know how to take advantage of specific characteristics of this type of territory. In Saint-Barthelemy case, scarcity is coveted; this coveted rarity is accessible only for rich people. The coveted rarity leads to luxury. Isolation is relative: this destination is not accessible to the jumbo jets. The airline market is controlled essentially by two small local companies and the airspace is open to charter flies and private aircrafts. Some other companies provide more or less regular flights from nearby airports of San Juan (Puerto Rico), Sint-Maarten and Guadeloupe. Luxury cannot be decreed, it is not planned. Luxury tourism is the election of a territory by elites who gather there to enjoy away from the rest of the world.
En l’espace de trente ans, la petite île de Saint-Barthélemy (25 km²) est sortie de son isolement séculaire pour s’imposer parmi les grandes destinations du tourisme de luxe dans le monde. Dans le cadre de cette étude, l’idée est d’identifier les éléments structurels et les différents facteurs conjoncturels qui permettent de comprendre la situation touristique de Saint-Barthélemy. L’exiguïté du territoire en lui-même peut être perçue comme un handicap fondamental ou, inversement, comme un atout considérable. Tout dépend du projet de développement. Il faut savoir tirer profit des spécificités du territoire considéré. Dans le cas de Saint-Barthélemy, l’exiguïté favorise la rareté et cette rareté convoitée n’est accessible qu’aux personnes les plus argentées. La rareté convoitée conduit au luxe. L’isolement est relatif : cette destination n’est pas accessible aux avions gros porteurs, l’essentiel du marché aérien est contrôlé par deux petites compagnies locales et l’espace aérien est ouvert aux petits avions privés. Le luxe ne se décrète pas, il ne se planifie pas. Le tourisme de luxe, c’est l’élection d’un territoire par des élites qui s’y retrouvent pour jouir de leur fortune à l’écart du monde.
ISSN: 1779-0980

Droits : http://creativecommons.org/licenses/by-nc/
hal-01364775
https://hal.univ-antilles.fr/hal-01364775
https://hal.univ-antilles.fr/hal-01364775/document
https://hal.univ-antilles.fr/hal-01364775/file/L%27%C3%AEle%20de%20Saint-Barth%C3%A9lemy%20une%20destination%20du%20tourisme%20de%20luxe.pdf
DOI : 10.4000/etudescaribeennes.6831

Résumé : Depuis octobre 1992 une étude est conduite par le laboratoire "Ressources Halieutiques" de l'IFREMER Cayenne pour analyser les mécanismes de recrutement du stock de crevettes pénéïdes (Penaeus subtilis) du plateau guyanais. En effet, le cycle de cette espèce étant très court, ces mécanismes conditionnent directement les rendements de la flottille industrielle crevettière guyanaise. Les variabilités intra et inter annuelles du recrutement sont considérées comme très fortes, aussi une optimisation de la gestion de cette pêcherie passe par une meilleure compréhension de ces mécanismes et notamment de leurs facteurs de variation. Cette étude s'intègre dans un programme de coopération régionale entre l'IFREMER et le Ministère de l'Agriculture, de l'Elevage et des Pêches du Surinam financé par des fonds FEDER et du FIC. Elle est respectivement menée par l'IFREMER et le laboratoire du Département des pêches du Surinam dans leurs Zones Economiques Exclusives. Ce programme prévoyait une série de huit campagnes en mer, précédées par une campagne commune de mise au point, qui devaient être conduites en parallèle par chacun des deux laboratoires français et surinamien sur les plateaux de Guyane (campagnes RESUBGUY) et du Surinam (campagnes RESUBSUR) afin d'analyser le phénomène de recrutement sur la plus large échelle possible d'observation (plateau guyano-surinamien). Deux campagnes annuelles ont été programmées pour chaque pays, en mai et en octobre, et ce sur deux années (1993 et 1994). Cette périodicité est fonction des résultats des travaux conduits par l'IFREMER et l'ORSTOM sur la phase pré-recrutée de Penaeus subtilis. Ceux-ci ont mis en évidence deux principales périodes annuelles distinctes de recrutement (avril-mai; septembre-octobre). Les résultats présentés ici proviennent de la cinquième et dernière campagne de la série initiée par l'IFREMER en octobre 1992. La première campagne avait servi de mise au point pour notamment standardiser la méthodologie entre les équipes de l'IFREMER et celle du Département des pêches du Surinam. L'étude ne s'est pas limitée à l'examen des seules captures de crevettes Penaeus subtilis, puisqu'elle a également inclue l'analyse de la composition des prises accessoires des crevettiers. Les "by-catches" considérées dans ce travail sont surtout représentées par la crevette "sea-bob", Xiphopenaeus kroyeri, ainsi que par les principales espèces de poissons dont certains d'intérêt commercial (ou ayant une forte probabilité de le devenir dans un futur proche). Enfin, une attention particulière a aussi été portée sur les captures accidentelles de tortues marines afin d'en estimer l'importance réelle.

Droits : 1995 Ifremer
http://archimer.ifremer.fr/doc/00076/18749/16320.pdf
http://archimer.ifremer.fr/doc/00076/18749/

Éditeur(s) : HAL CCSD European Geosciences Union (EGU)
Résumé : International audience
Storms and tsunamis, which may seriously endanger human society, are amongst the most devastating marine catastrophes that can occur in coastal areas. Many such events are known and have been reported for the Mediterranean, a region where high-frequency occurrences of these extreme events coincides with some of the most densely populated coastal areas in the world. In a sediment core from the Mar Menor (SE Spain), we discovered eight coarse-grained layers which document marine incursions during periods of intense storm activity or tsunami events. Based on radiocarbon dating, these extreme events occurred around 5250, 4000, 3600, 3010, 2300, 1350, 650, and 80 years cal BP. No comparable events have been observed during the 20th and 21st centuries. The results indicate little likelihood of a tsunami origin for these coarse-grained layers, although historical tsunami events are recorded in this region. These periods of surge events seem to coincide with the coldest periods in Europe during the late Holocene, suggesting a control by a climatic mechanism for periods of increased storm activity. Spectral analyses performed on the sand percentage revealed four major periodicities of 1228 ± 327, 732 ± 80, 562 ± 58, and 319 ± 16 years. Amongst the well-known proxies that have revealed a millennial-scale climate variability during the Holocene, the ice-rafted debris (IRD) indices in the North Atlantic developed by Bond et al. (1997, 2001) present a cyclicity of 1470 ± 500 years, which matches the 1228 ± 327-year periodicity evidenced in the Mar Menor, considering the respective uncertainties in the periodicities. Thus, an in-phase storm activity in the western Mediterranean is found with the coldest periods in Europe and with the North Atlantic thermohaline circulation. However, further investigations, such as additional coring and high-resolution coastal imagery, are needed to better constrain the main cause of these multiple events.
ISSN: 1814-9324

hal-01357199
https://hal.archives-ouvertes.fr/hal-01357199
https://hal.archives-ouvertes.fr/hal-01357199v2/document
https://hal.archives-ouvertes.fr/hal-01357199/file/cp-12-1389-2016.pdf
DOI : 10.5194/cp-12-1389-2016

Résumé : Depuis de nombreuses années, les biologistes étudiant des poissons d'eau douce, ont mis en évidence les relations existant entre le cycle de maturation et les facteurs environnementaux tels que la température et la photopériode (Bullough, 1940 ; Merinan & Schedl, 1941 ; Harrington 1957, Henderson, 1963...). En aquaculture, pour des espèces tempérées comme le loup, la dorade, le turbot, dès 1973, l'opportunité du décalage de la saison de ponte grâce au raccourcissement des cycles environnementaux naturels, est démontré (Girin & Devauchelle, 1978). Sur le loup (Dicentrarchus labrax), des pontes décalées ont pu être obtenues par manipulation du seuil facteur est également reprise par Suquet (1987) puis par Bouget (1988), sur la dorade (Sparus aurata). Devauchelle (1980) démontre que la maturation et la ponte du turbot (Scophthalmus maximus) se réalisent à température constante sans problème majeur. Bacon (1973) présente les plans d'un laboratoire à environnement contrôle utilisé par Kuo & al. (1974) pour des travaux sur le mullet (Mugil cephalus). D'autres travaux sont réalisés sur des espèces subtropicales comme Trachintous carolinus (Hoff & al. 1972, 1978). Pour une espèce tropicale telle que le milkfish Chanos chanos, Lee & al. (1987) concluent à une prépondérance du facteur photophase sur la température pour l'induction de la maturation. Chez Siganus guttatus, espèce tropicale à rythme de ponte mensuel, le facteur lumineux (cycle lunaire) semble être le plus important dans un milieu ou la température de l'eau est stade tout le long de l'année (plus ou moins 1 degré centigrade) (Soletchnik, non publié). Ainsi, chez les poissons tempérés, l'initiation de la maturation serait clairement déclenchée par l'augmentation de la photopériode (Bye & Htun Han, 1979). Harrington (1959), quant à lui, pense que l'influence de la température sur les poissons à longue saison de ponte est plus importante que celle de la photopériode. L'importance relative de l'un ou l'autre de ces deux facteurs, température et photopériode dans les processus physiologiques de maturation et de ponte de l'ombrine, sont actuellement à l'étude aux Etats Unis (Robert, Comm. pers.). L'opération envisagée en Martinique dès 987 est celle des transférer et d'adapter en conditions tropicales et dans un environnement insulaire une technologie développée dans différents états américains depuis le début des années 70. Les premiers cycles de maturation et ponte ont été initiés début 1989 avec la mise en fonctionnement des salles géniteurs à environnement contrôle. Les premiers résultats obtenus dans cette structure, et en cages flottantes sont décrits dans ce chapitre.

Droits : 1990 Ifremer
http://archimer.ifremer.fr/doc/00133/24408/22408.pdf
http://archimer.ifremer.fr/doc/00133/24408/