Éditeur(s) : Université des Antilles Études caribéennes
Résumé : La petite île antillaise de Saint-Martin (90 km²) a vu sa population pratiquement tripler ces deux dernières décennies, passant de 25 000 à 70 000 insulaires environ. Les migrations intra-caribéennes sont la cause essentielle du sensible accroissement démographique de cette île mi-française, mi-hollandaise au niveau de vie comparable à celui de l’Europe occidentale, mais située dans une aire géographique moins privilégiée. L’article tend à interroger le lien de causalité entre l’afflux massif de populations allochtones et la partition de l’île, ce dernier facteur paraissant déterminant pour la compréhension du phénomène migratoire vers Saint-Martin. L’île serait rendue plus encore attractive par l’existence de cette frontière qui, d’une part, favorise un dynamisme économique particulier et, d’autre part, rend le contrôle des flux migratoires plus difficile en raison du différentiel législatif entre ses deux parties.
The small Caribbean island of St. Martin (90 km ²) saw its population nearly tripled in the last two decades, from 25 000 to about 70 000 islanders. The intra-Caribbean migrations are the main cause of significant population growth of the mid-French, mid-Dutch island where standard of living is comparable to that of Western Europe but located in a geographical area less privileged. The article tends to question the causal link between the massive influx of immigrants populations and the partition of the island, the latter factor appearing crucial for understanding the phenomenon of migration to Saint-Martin. The island would be made more attractive by the existence of this border which, on the one hand, promotes a particular economic dynamism and, on the other hand, gives the control of migration flows more difficult because of the legislative differential between its two parties.

Droits : info:eu-repo/semantics/openAccess
urn:doi:10.4000/etudescaribeennes.962
http://journals.openedition.org/etudescaribeennes/962

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
The thermal evolution of sediments in the shallowest part of sedimentary basins is challenging to investigate as most of the geothermometers are at their application limits. This is typically the case of the Callovian-Oxfordian claystones at the eastern border of the Paris Basin. A recent 2000 m deep well penetrated the entire Jurassic and Triassic sedimentary series and permitted coring of sediments never reached by previous drilling in this part of the basin. Thanks to the use of several independent geothermometers (apatite fission track thermochronology, fluid inclusion microthermometry, clay mineralogy and sedimentary organic matter evolution) the burial history of the Mesozoic series has been reconstructed, modeled and calibrated using kinetic algorithms relevant to the various paleothermometers used. In addition to these conventional methods, an innovative approach was developed using the temperature-dependence of the magnetic mineral assemblage within clay-rich sediments ("MagEval"). Thermal modeling indicates that the Callovian-Oxfordian and the Lower Triassic experienced maximum burial temperatures of 50 +/- 5 C-circle and 90 +/- 10 C-circle respectively, i.e., about 25 C higher than present-day. This temperature offset implies the erosion of several hundred meters of sediments which, depending on the thermal flux and conductivity considered, most likely constituted Upper Cretaceous chalk deposits. Falling sea level resulted in the exposure and subsequent dismantling of the chalk cover at the beginning of Cenozoic times. The eastern border of the basin was then subjected to slow erosion and discrete tectonic deformation.
ISSN: 0264-8172

hal-01313142
https://hal.archives-ouvertes.fr/hal-01313142
DOI : 10.1016/j.marpetgeo.2013.08.019

Éditeur(s) : HAL CCSD Wiley
Résumé :  
The lack of information on the ways seasonal drought modifies the CO2 exchange between Neotropical rainforest ecosystems and the atmosphere and the resulting carbon balance hinders our ability to precisely predict how these ecosystems will respond as global environmental changes force them to face increasingly contrasting conditions in the future. To address this issue, seasonal variations in daily net ecosystem productivity (NEPd) and two main components of this productivity, daily total ecosystem respiration (REd) and daily gross ecosystem productivity (GEPd), were estimated over 2 years at a flux tower site in French Guiana, South America (511605400N, 5215404400W). We compared seasonal variations between wet and dry periods and between dry periods of contrasting levels of intensity (i.e. mild vs. severe) during equivalent 93-day periods. During the wet periods, the ecosystem was almost in balance with the atmosphere (storage of 9.0 gCm_2). Seasonal dry periods, regardless of their severity, are associated with higher incident radiation and lower REd combined with reduced soil respiration associated with low soil water availability. During the mild dry period, as is normally the case in this region, the amount of carbon stored in the ecosystem was 32.7 gCm_2. Severe drought conditions resulted in even lower REd, whereas the photosynthetic activity was only moderately reduced and no change in canopy structure was observed. Thus, the severe dry period was characterized by greater carbon storage (64.6 gCm_2), emphasizing that environmental conditions, such as during a severe drought, modify the CO2 exchange between Neotropical rainforest ecosystems and the atmosphere and potentially the resulting carbon balance.
ISSN: 1354-1013

hal-01032067
https://hal.archives-ouvertes.fr/hal-01032067
DOI : 10.1111/j.1365-2486.2008.01610.x

Éditeur(s) : HAL CCSD Oxford University Press (OUP)
Résumé : International audience
Island arc picrites and boninites are magnesian magmatic rocks believed to be generated by high degrees of melting of depleted mantle sources fluxed by subduction-derived, volatile-rich components. These magmas can be probes of both the mantle wedge protoliths and subduction components, but are rare among other, usually more evolved, types of arc lavas. Furthermore, many arc picrites and boninites show evidence for late-stage differentiation prior to or during eruption, masking their primary, mantle-derived geochemical signatures. We report textural and chemical data on spinel-hosted melt inclusions of mantle origin in amphibole-bearing websterite veins cross-cutting spinel harzburgite xenoliths from the active andesitic Avacha volcano (south Kamchatka, Russia). The data are used to constrain the composition and origin of melts that formed the websterite veins in the sub-arc lithospheric mantle. The melt inclusions typically contain euhedral orthopyroxene and clinopyroxene and occasionally minor amphibole in silicate glass. The melt inclusions were homogenized using heating stages and gas-mixing furnaces. The homogenized glasses range from subalkaline primitive silica-rich picrite and high-Ca boninite (>15 wt % MgO, 48–54 wt % SiO2) to rhyolite. High-Ca boninite glasses have moderate volatile and low heavy rare earth element contents and elevated Cs, Rb, Ba, U, Sr, and Li abundances, with extremely high U/Th. In turn, the glasses display no negative spikes in the high field strength elements Nb, Ta, Zr, Hf, and Ti. We show that the silica-rich picrite and high-Ca boninite liquids in this study formed by high degrees of melting (>25%), at volatile under-saturation, of hybrid melt-depleted but silica-rich mantle sources at ≥1·5 GPa. The hybrid sources formed in two stages: first, by extraction of ∼15% melt from the convecting mantle to form a refractory protolith, which was subsequently enriched in silica via interaction with subduction-derived components prior to or during remelting in the mantle wedge. The subduction-derived components were enriched in fluid-mobile elements and probably oxidized. Overall, our results suggest that silica-rich picrites and high-Ca boninites can be primary melts in mature subduction zones and differentiate within the mantle wedge and the deep arc crust to form more evolved andesite magmas.
ISSN: 0022-3530

hal-01553676
https://hal.archives-ouvertes.fr/hal-01553676
DOI : 10.1093/petrology/egw066

Éditeur(s) : HAL CCSD MDPI
Résumé : International audience
AbstractThis review provides a global overview of microporous silica based membranes for desalination via pervaporation with a focus on membrane synthesis and processing, transport mechanisms and current state of the art membrane performance. Most importantly, the recent development and novel concepts for improving the hydro-stability and separating performance of silica membranes for desalination are critically examined. Research into silica based membranes for desalination has focussed on three primary methods for improving the hydro-stability. These include incorporating carbon templates into the microporous silica both as surfactants and hybrid organic-inorganic structures and incorporation of metal oxide nanoparticles into the silica matrix. The literature examined identified that only metal oxide silica membranes have demonstrated high salt rejections under a variety of feed concentrations, reasonable fluxes and unaltered performance over long-term operation. As this is an embryonic field of research several target areas for researchers were discussed including further improvement of the membrane materials, but also regarding the necessity of integrating waste or solar heat sources into the final process design to ensure cost competitiveness with conventional reverse osmosis processes. © 2012 by the authors.
ISSN: 2073-4441

hal-01683200
https://hal.univ-antilles.fr/hal-01683200
DOI : 10.3390/w4030629

Résumé : L'utilisation de l'énergie thermique des mers constitue une des formes de captation de l'énergie solaire. Le flux thermique apporté par le rayonnement du soleil aux limites supérieures de l'atmosphère est, en moyenne, d'environ 140 mW par centimètre carré de la surface perpendiculaire au rayonnement (constante solaire). Défalcation faite de l'absorption dans l'atmosphère des réflexions et dispersions par les nuages et par la surface de l'eau, il reste environ 16. mW/ cm2 absorbés par la mer. [OCR NON CONTRÔLE]

Droits : 1974 CNEXO
http://archimer.ifremer.fr/doc/00001/11260/7806.pdf
http://archimer.ifremer.fr/doc/00001/11260/

Résumé : Les océans qui couvrent les deux tiers de la planète sont susceptibles d'offrir deux types d'énergie. D'une part des énergies utilisables à faible niveau de puissance et capables d'apporter une solution pratique à certains problèmes particuliers : ce sont essentiellement les énergies de la houle et du vent. D'autre part, une énergie qui ne se révèle intéressante qu'à partir d'un certain niveau de puissance: c'est l'énergie thermique des mers (E.T.M.) encore appelée énergie maréthermique (l'énergie marémotrice qui relève de ce dernier type est un cas assez particulier car elle ne concerne qu'un nombre de sites très restreint). Les énergies de la mer sont un sous produit direct de l'énergie solaire ; en effet, en raison de la valeur du flux d'énergie solaire, le globe terrestre intercepte une puissance équivalente à 200 milliards de mégawatts, mais en raison de la réflexion diffuse sur l'atmosphère, sur les nuages, sur la mer et sur la terre, près de la moitié de cette énergie incidente est renvoyée vers l'espace. La plus grande partie du rayonnement solaire converti en chaleur sert à chauffer la mer qui, du fait de son faible coefficient de réflexion, absorbe une quantité importante de lumière. Comme la chaleur spécifique de l'eau est très grande, et que le volume d'eau échauffée est important, les couches superficielles de l'océan vont jouer le rôle d'un immense réservoir de chaleur. On sait par ailleurs que les eaux profondes des océans. qui prennent naissance dans la région des pôles, s'écoulent lentement sur le fond des bassins océaniques et que leur température est voisine de 0°. Il est donc théoriquement possible. en utilisant les différences de température qui existent entre les eaux de surface et celles du fond. de concevoir une machine thermique capable de fournir de l'énergie mécanique transformée en énergie électrique. Il s'agit là d'une technologie douce qui constitue certainement un progrès par rapport aux technologies dures et brutales mises en œuvre jusqu'à présent.

Droits : 1978 Ifremer
http://archimer.ifremer.fr/doc/00039/14975/12302.pdf
http://archimer.ifremer.fr/doc/00039/14975/

Éditeur(s) : Springer
Résumé : The Håkon Mosby mud volcano is a 1.5-km-diameter geological structure located on the Southwest Barents Sea slope at a water depth of 1,270 m. High-definition seabed mapping of the mud volcano has been carried out in 2003 and 2006. A comparative analysis of the bathymetry and backscatter maps produced from the two surveys shows subtle morphological changes over the entire crater of the mud volcano, interpreted to be the consequence of mud eruption events. Mud temperature measurements point to a persistently warm mud at shallow depth in the crater. This is explained by upward fluid advection, rather than conductive cooling of mud flows. The small-scale spatial variability in the temperature distribution may be related to mud outflows or changes in the fluid flow regime. Furthermore, the locations of free gas venting observed in 2006 were found to differ from those of 2003. Our observations of overall similar topographic profiles across the mud volcano in 2003 and 2006 suggest that eruption events would have been modest. Nevertheless, the data bring evidence of significant change in activity even over short time intervals of only 3 years. This may be a characteristic shared by other submarine mud volcanoes, notably those considered to be in a quiescent stage.
Geo-marine Letters (0276-0460) (Springer), 2010-06 , Vol. 30 , N. 3-4 , P. 157-167

Droits : Springer-Verlag 2010
http://archimer.ifremer.fr/doc/00004/11527/10261.pdf
DOI:10.1007/s00367-010-0193-z
http://archimer.ifremer.fr/doc/00004/11527/

Éditeur(s) : HAL CCSD
Résumé : Processes that occur within and across the oceanic crust–in particular along mid-ocean ridges and oceanic spreading centers—play a huge role in the dynamics of the Earth. The largest fluxes of heat and material between the Earth's mantle, crust, and seawater occur via magmatic, tectonic, and hydrothermal processes along oceanic spreading centers and their vast flanks. Roughly two thirds of the Earth's surface is accreted through magmatic and tectonic processes along mid-ocean ridges, and subduction of this ocean crust in turn influences mantle compositions. Exchange of elements between ocean crust and seawater strongly influences seawater compositions and leaves a geologic record of fluid-rock reactions in altered ocean crust. Some of these reactions contribute energy to microbial activity of a largely unexplored biosphere. The dynamics of ridge and ocean crustal processes therefore have enormous implications for thermal, chemical, and biological exchanges between the solid Earth and the hydrosphere.
EOS

hal-00564842
https://hal.archives-ouvertes.fr/hal-00564842
DOI : 10.1029/2010EO150001

Éditeur(s) : HAL CCSD
Résumé : Carbon isotopic signature has been measured at the different stages of the soil CO2 efflux production in trenched and control plots to improve the knowledge about the physical and biochemical processes of the soil respiration. All the measurements of _13C have been performed using a mass-spectrometer.We have compared the isotopic signatures of the CO2 going out of the soil, the CO2 of the soil atmosphere, the organic carbon in the material that could be considered as the main soil respiration sources (live and dead roots, soil organic matter, aerial litter) and the CO2 produced by these sources in incubation jars. The aims of this study were to evaluate the possibilities to combine these different data sets to estimate the partitioning of soil respiration between its autotrophic and heterotrophic components, and to get more insight into potential fractionation during biochemical or diffusion processes. Measurements were conducted in a beech forest located at Hesse in the North East of France (site equipped with a flux tower and belonging to the CarboEurope network) and in a neotropical primary rainforest located at Paracou (French Guiana). Preliminary results show first a very tenuous difference between CO2 isotopic signatures of efflux coming from the trenched and control plots and, secondly, _13C significant divergences between bulk organic material and CO2 produced in the corresponding incubation jars. Our ability to use this kind of data for partitioning soil respiration into its main components will be discussed.
Geophysical Research Abstracts

hal-01031785
https://hal.archives-ouvertes.fr/hal-01031785

Éditeur(s) : Academic Press Ltd- Elsevier Science Ltd
Résumé : The high heterogeneity of silica cycling in coastal margins and the lack of silica data (compared to nitrogen and phosphorus) prevent the estimation of global silica retention in estuaries. In this study, the spatial and temporal variability of porewater silicic acid (Si(OH)4) profiles e that integrate benthic transport and reaction processes e was investigated at different spatial (metre, longitudinal and crosssection, intra-estuary) and temporal (tidal, seasonal) scales in two macrotidal estuaries, very close geographically but essentially differing in their shape. Studying the spatial and temporal variability of Si(OH)4 concentrations in porewaters provided evidence for the importance of transport processes, e.g. bio-irrigation, tidal pumping, resuspension and any combination of these processes, in affecting Si(OH)4 concentrations and fluxes and therefore temporary or permanent retention along the landeocean continuum. We confirm that aSiO2 (amorphous silicate) transported by rivers and estuaries clearly needs to be better characterized as it provides an important source of reactive aSiO2 to sediments. This study allows us to: (1) interrogate spatial and temporal scales, although both are most often in complete interaction; (2) design the most appropriate sampling schemes to be representative of any given system and to extrapolate at the scale of the whole estuary; (3) quantify uncertainty associated to the estimations of Si(OH)4 stocks and fluxes in this type of ecosystem, essential for budget calculations. We showed that two adjacent small macrotidal estuaries, may exhibit different behaviours regarding Si retention. Temporary retention has been observed in the meanders of the Aulne Estuary and not along the more linear Elorn Estuary, demonstrating the importance of the morphology and hydrodynamic components of the estuarine filter. Research is needed in other systems and climatic zones, but our study suggests that the typology should not only account for the different types of landeocean continuum (fjord, delta, mangrove.), but also incorporate the physical or biological attributes of the estuarine filter.
Estuarine Coastal And Shelf Science (0272-7714) (Academic Press Ltd- Elsevier Science Ltd), 2013-03 , Vol. 119 , P. 31-43

Droits : 2013 Elsevier Ltd. All rights reserved.
http://archimer.ifremer.fr/doc/00124/23529/22370.pdf
DOI:10.1016/j.ecss.2012.12.008
http://archimer.ifremer.fr/doc/00124/23529/

Éditeur(s) : Elsevier Science Bv
Résumé : The timing, routing and processes of sediment transfer from the continents to the oceans at millennial time-scale are still largely unknown. The potential of turbidite systems (dominantly deposited during sea-level lowstands) to record global or regional environmental fluctuations is usually under-exploited because of the difficulty to obtain robust chronostratigraphic constraints in turbiditic deposits, and therefore to tie changes in sedimentary processes to environmental fluctuations. We were able to obtain a millennial-scale chronostratigraphy based on oxygen isotopes of the scarce foraminifera preserved in turbiditic deposits of the Rhone Turbidite System within the Western Mediterranean. Our results show that 1) objective criteria can be defined for the selection of foraminifera preserved within the pelagic intervals between the turbiditic sequences, in order to obtain a reliable isotope stratigraphy; 2) Turbidites triggered by hyperpycnal currents are described for the first time within the Rhone Turbidite System. They are related to the periods of direct fluvial connection with the canyon head (during the sea-level lowstand and early rise), and to a period of high sediment flux in relation with the massive recession of the Rhone glaciers in the Alps; 3) The lithofacies change passing from hyperpycnal to “Bouma-type” is dated at ca 19 cal. ka BP, which might correspond to an acceleration of sea-level rise (19-ka Meltwater Pulse,).
Sedimentary Geology (0037-0738) (Elsevier Science Bv), 2015-06 , Vol. 323 , P. 148-166

Droits : 2015 Elsevier B.V. All rights reserved.
http://archimer.ifremer.fr/doc/00266/37712/35730.pdf
DOI:10.1016/j.sedgeo.2015.04.009
http://archimer.ifremer.fr/doc/00266/37712/

Éditeur(s) : HAL CCSD Ecological Society of America
Résumé : CABI:20153174020
Understanding how plants are constructed - i.e., how key size dimensions and the amount of mass invested in different tissues varies among individuals - is essential for modeling plant growth, carbon stocks, and energy fluxes in the terrestrial biosphere. Allocation patterns can differ through ontogeny, but also among coexisting species and among species adapted to different environments. While a variety of models dealing with biomass allocation exist, we lack a synthetic understanding of the underlying processes. This is partly due to the lack of suitable data sets for validating and parameterizing models. To that end, we present the Biomass And Allometry Database (BAAD) for woody plants. The BAAD contains 259634 measurements collected in 176 different studies, from 21084 individuals across 678 species. Most of these data come from existing publications. However, raw data were rarely made public at the time of publication. Thus, the BAAD contains data from different studies, transformed into standard units and variable names. The transformations were achieved using a common workflow for all raw data files. Other features that distinguish the BAAD are: (i) measurements were for individual plants rather than stand averages; (ii) individuals spanning a range of sizes were measured; (iii) plants from 0.01-100 m in height were included; and (iv) biomass was estimated directly, i.e., not indirectly via allometric equations (except in very large trees where biomass was estimated from detailed sub-sampling). We included both wild and artificially grown plants. The data set contains the following size metrics: total leaf area; area of stem cross-section including sapwood, heartwood, and bark; height of plant and crown base, crown area, and surface area; and the dry mass of leaf, stem, branches, sapwood, heartwood, bark, coarse roots, and fine root tissues. We also report other properties of individuals (age, leaf size, leaf mass per area, wood density, nitrogen content of leaves and wood), as well as information about the growing environment (location, light, experimental treatment, vegetation type) where available. It is our hope that making these data available will improve our ability to understand plant growth, ecosystem dynamics, and carbon cycling in the world's vegetation.
ISSN: 0012-9658

hal-01535227
https://hal.archives-ouvertes.fr/hal-01535227
DOI : 10.1890/14-1889.1
PRODINRA : 306122

Résumé : Penaeus stylirostris shrimp imported from Hawaii for a genetic program and kept at the Saint-Vincent research facility had progressively developed a high sensitivity to IHHNV, the etiological agent of the Infectious, Hypodermic, and Hematopoietic Necrosis. Fears were that the virus could not only be transferred to their offspring, but also that the New Caledonian strain of Penaeus stylirostris, so far considered as resistant, could become sensitive by an off balance of its hosts/pathogen equilibrium. In October 2008, a joint decision between Uprac (shimp owner), Davar (New Caledonian Animal Health Authority) and Ifremer (scientific partner) was taken to terminate all pure breed and hybrid Hawaiian populations remaining in the ponds, and to implement an intensive fallowing protocol, and controlled restocking. IHHNV was also suspected to trouble experiments carried out in the research facility (mortalities, deformities, slow growth), thus affecting research programs. Difficulties pointed out by IHHNV have triggered since 2008 some awareness on biosecurity issues at some level of the New Caledonian shrimp industry. At the St-Vincent research station, it led to a risk assessment and implementation of biosecurity procedures (fallowing, propagation, grow out and use of screened animals) which minimizes the risk of expression of IHHNV. The use of a brand new hatchery building on site also helped in resetting routine hygiene procedures during production and in controlling incoming and outgoing items (shrimp, water, feed, personnel, equipment, pests and wastes). IHHNV has not been detected on analysed samples since then nor have any symptoms been found during experimental or broodstock growout. Keeping this control alive is considered as a useful tool to lower the risk of potential health threats, to get a better understanding in case of an outbreak, and to increase the reliability of experimental results.
Les crevettes originaires d’Hawaii et conservées au LEAD St-Vincent, dans le cadre du programme d’introduction de variabilité génétique dans le cheptel Calédonien, ont progressivement montré une sensibilité importante au virus IHHNV, agent de la Nécrose Hypodermale et Hématopoïétique Infectieuse (mortalité, croissance ralentie, déformations). Les risques d’une transmission génétique de cette sensibilité à leur descendance à moyen terme, et de son développement par rupture de l’équilibre hôte/pathogène sur la souche dite « Calédonienne » jusqu’alors considérée comme résistante à l’IHHN, ont conduit à partir d’octobre 2008, avec l’accord et l’appui de l’UPRAC et de la DAVAR, à la suppression des animaux hawaiiens ou hybrides encore présents dans les bassins de terre du LEAD St-Vincent, au vide sanitaire de ces derniers, et au repeuplement contrôlé du site. D’autre part, le virus IHHN est soupçonné d’avoir pu affecter les animaux utilisés dans les expérimentations menées au LEAD-St-Vincent (mortalités, déformations, croissance réduite), influençant donc potentiellement leur bon déroulement et celui des programmes de recherches. Les obstacles soulevés par l’expression du virus IHHN ont donc initié depuis 2008 une prise de conscience et la mise en place de démarches de biosécurité dans certains points de la filière. A la station de St-Vincent, cette démarche s’est traduite par une identification/évaluation des risques et l’application de mesures (vide sanitaire, reproduction, élevage et utilisation des animaux contrôlés) chacune dotée de procédures qui regroupées, minimisent le risque d’introduction et de dissémination de l’IHHNV. La prise en main de la nouvelle structure d’écloserie sur le site de la SASV a également été mise à profit pour revoir les procédures d’hygiène de routine dans la conduite des productions et dans le contrôle des flux intrants et sortants (animaux, eau, aliments, personnel, équipement, nuisibles, déchets). Aucune détection d’IHHNV sur les échantillons prélevés n’a depuis été observée, de même qu’aucun symptôme de l’expression de cette maladie sur les animaux en élevage sur le site de Saint-Vincent. La poursuite de ces mesures est envisagée comme un outil d’aide à la minimisation des problèmes potentiels, à leur compréhension en cas d’apparition, et à la fiabilisation des résultats.

Droits : 2010 Ifremer
http://archimer.ifremer.fr/doc/00118/22949/20776.pdf
http://archimer.ifremer.fr/doc/00118/22949/

Éditeur(s) : HAL CCSD Springer Verlag/EDP Sciences
Résumé : Key messageWe review the recent findings on the influence of drought on tree mortality, growth or ecosystem functioning in tropical rainforests. Drought plays a major role in shaping tropical rainforests and the response mechanisms are highly diverse and complex. The numerous gaps identified here require the international scientific community to combine efforts in order to conduct comprehensive studies in tropical rainforests on the three continents. These results are essential to simulate the future of these ecosystems under diverse climate scenarios and to predict the future of the global earth carbon balance.[br/]ContextTropical rainforest ecosystems are characterized by high annual rainfall. Nevertheless, rainfall regularly fluctuates during the year and seasonal soil droughts do occur. Over the past decades, a number of extreme droughts have hit tropical rainforests, not only in Amazonia but also in Asia and Africa. The influence of drought events on tree mortality and growth or on ecosystem functioning (carbon and water fluxes) in tropical rainforest ecosystems has been studied intensively, but the response mechanisms are complex.[br/]AimsHerein, we review the recent findings related to the response of tropical forest ecosystems to seasonal and extreme droughts and the current knowledge about the future of these ecosystems.[br/]ResultsThis review emphasizes the progress made over recent years and the importance of the studies conducted under extreme drought conditions or in through-fall exclusion experiments in understanding the response of these ecosystems. It also points to the great diversity and complexity of the response of tropical rainforest ecosystems to drought.[br/]ConclusionThe numerous gaps identified here require the international scientific community to combine efforts in order to conduct comprehensive studies in tropical forest regions. These results are essential to simulate the future of these ecosystems under diverse climate scenarios and to predict the future of the global earth carbon balance.
ISSN: 1286-4560

hal-01269438
https://hal.archives-ouvertes.fr/hal-01269438
DOI : 10.1007/s13595-015-0522-5
PRODINRA : 338568

Éditeur(s) : HAL CCSD Landes Bioscience
Résumé : International audience
In 2008 we published the first set of guidelines for standardizing research in autophagy. Since then, research on this topic has continued to accelerate, and many new scientists have entered the field. Our knowledge base and relevant new technologies have also been expanding. Accordingly, it is important to update these guidelines for monitoring autophagy in different organisms. Various reviews have described the range of assays that have been used for this purpose. Nevertheless, there continues to be confusion regarding acceptable methods to measure autophagy, especially in multicellular eukaryotes. A key point that needs to be emphasized is that there is a difference between measurements that monitor the numbers or volume of autophagic elements (e.g., autophagosomes or autolysosomes) at any stage of the autophagic process vs. those that measure flux through the autophagy pathway (i.e., the complete process); thus, a block in macroautophagy that results in autophagosome accumulation needs to be differentiated from stimuli that result in increased autophagic activity, defined as increased autophagy induction coupled with increased delivery to, and degradation within, lysosomes (in most higher eukaryotes and some protists such as Dictyostelium) or the vacuole (in plants and fungi). In other words, it is especially important that investigators new to the field understand that the appearance of more autophagosomes does not necessarily equate with more autophagy. In fact, in many cases, autophagosomes accumulate because of a block in trafficking to lysosomes without a concomitant change in autophagosome biogenesis, whereas an increase in autolysosomes may reflect a reduction in degradative activity. Here, we present a set of guidelines for the selection and interpretation of methods for use by investigators who aim to examine macroautophagy and related processes, as well as for reviewers who need to provide realistic and reasonable critiques of papers that are focused on these processes. These guidelines are not meant to be a formulaic set of rules, because the appropriate assays depend in part on the question being asked and the system being used. In addition, we emphasize that no individual assay is guaranteed to be the most appropriate one in every situation, and we strongly recommend the use of multiple assays to monitor autophagy. In these guidelines, we consider these various methods of assessing autophagy and what information can, or cannot, be obtained from them. Finally, by discussing the merits and limits of particular autophagy assays, we hope to encourage technical innovation in the field.
Autophagy

hal-00735751
https://hal.archives-ouvertes.fr/hal-00735751
PUBMED : 22966490

Éditeur(s) : HAL CCSD
Résumé : International audience
The Cenozoic weathering of peninsular India has been advocated as a major driver of globalcooling, however, its timing remains virtually unconstrained such that proposed links betweentropical weathering of the Deccan Traps, regional monsoonal intensity and global climate remainsspeculative. To solve this conundrum we present here a revised weathering chronologybased on the identification of lateritic paleosurfaces and their dating using 40Ar/39Ar on supergeneK-rich manganese oxides. We focus on the Indian western passive margin where theWestern Ghats Escarpment (WGE) – a ~1000 m high topographic barrier resulting from thecontinental break up of Greater India – exposes exceptionally preserved weathering profilesfrom the western coastal lowlands to the eastern highland plateaus above the WGE. Four mainlateritic paleosurfaces have been identified: Three in the highland; a high landsurface (Al-Femostly bauxite) at elevation 1200-1000 m asl, an intermediate landsurface covered by a Feduricrustat 1000-900 m asl and a lower pediment landsurface at 850-600 m asl; and one inthe coastal lowland underneath a pediment landsurface at 150-50 m asl. The 40Ar/39Ar agesdocument three major weathering periods over the Cenozoic. The oldest weathering period(W1) is recorded between 53 Ma to 45 Ma both in the highland and the lowland. This correlatesto the Global Eocene climatic Optimum, and allows defining a bauxitic paleolandsurface acrossthe escarpment. Intense bauxitic weathering between ~ 45 and 47 Ma in the lowland indicatethat the WGE was stabilized before ~ 47 Ma on its margin and also implies low denudation rateat the foot of the WGE (<5 m Ma-1) since that time. The second weathering period between37 Ma to 19 Ma (W2) occurred in two distinctive stages (W2a and W2b). From 37 to 26 (W2a),weathering is only recorded in the highland and affect intermediate surfaces. The intensityof chemical weathering decreased sensibly between 32 and 29 Ma – potentially linked to theEarly Oligocene cooling – and resulted in the formation of the lower pediment surface. From~26 Ma to 19 Ma (W2b), only the western coastal lowland weathered while the highland surfacesare mostly dissected. This change and the highland/lowland weathering mitigation after~26 Ma documents a change in climatic patterns over peninsular India that signs the onset ofmodern-like monsoon regime. These results are being interpolated to the Deccan Traps basaltsto quantify their weathering and ultimately estimate of the contribution to CO2 fluxes of thesethree weathering periods and their potential link to Asian Monsoons and global cooling.
Source to Sink: a long term perspective of sediment budgets and sources characterization, Abstracts
Rennes, France

insu-01406455
https://hal-insu.archives-ouvertes.fr/insu-01406455

Éditeur(s) : Université de Montpellier II
Résumé : The sea bass, Dicentrarchus labrax, has been subjected to intensive aquaculture on the Mediterranean cost for ten years. Marine fish hatcheries are key factors in the aquaculture field, and face different pathologies, especially one of viral origin (nodavirus) that could challenge their feasibility. Consequently, we have tried to provide some data on larvae and spawning stocks. Firstly, we have studied the immunoglobulins, components of the specific humoral immunity, and their role as antibodies. On adult basses, these immunoglobulins are tetrameric molecules with high molecular weight (850 kD), made of heavy (H) - 80 kD and light (L) - 26 kD chains. In the eggs, simplest forms such as monomeric or dimeric are brought to the fore; they are located under the chorionic membrane. Secondly, we have studied the development of the immunity system on larvae, preparing IgM assays with ELISA method, the study on the organogenesis of the main lymphoid organs, and using flow cytometry for the ontogenesis of IgM producing cell. Based on this experience, we can propose a date for the immunocompetence onset of the bar, i.e. from the 54th day of the hatchery phase. Finally, we made the most of these different results to study a viral pathology (nodavirus) in spawners and larvae. We defined an experimental contamination model for larvae and eggs, and we highlighted that eggs born from vaccinated hen fishes were protected against the nodavirus.
Le bar, Dicentrarchus labrax, fait l'objet d'une aquaculture intensive sur le littoral Méditerranéen depuis une dizaine d'années. Les écloseries marines représentent un des maillons clefs de cette filière aquacole, et sont confrontées à différentes pathologies, dont une d'origine virale (nodavirus), pouvant remettre en cause leur faisabilité. Aussi, nous avons tenté d'apporter quelques données concernant la protection des larves et des géniteurs reproducteurs. Dans un premier temps, nous avons étudié les immunoglobulines, éléments de l'immunité spécifique humorale ainsi que leur rôle anticorps. Chez les bars adultes ces immunoglobulines sont des molécules tétramériques de haut poids moléculaire (850 kD), composées de chaînes lourdes (H) de 80 kD et légères (L) de 26 kD. Dans les oeufs, des formes plus simples, monomériques ou dimériques, sont mises en évidence et sont localisées sous la membrane chorionique. Dans un second temps, nous avons étudié la mise en place du système immunitaire spécifique chez les larves, en effectuant le dosage des IgM par ELISA, l'étude de l'organogenèse des principaux organes lymphoïdes, puis celle de l'ontogenèse des cellules productrices d'IgM par cytométrie de flux. L'ensemble de cette étude nous permet de proposer une date d'acquisition de l'immunocompétence à partir du 54ème jour d'élevage chez le bar. Enfin, ces différents résultats ont été mis à profit dans le cadre d'une pathologie virale (nodavirus) touchant les reproducteurs et les larves. Après avoir défini un modèle de contamination expérimental des larves et des oeufs, nous avons mis en évidence une protection des oeufs lorsque ceux-ci proviennent d'une femelle vaccinée (vaccin expérimental) contre le nodavirus.

Droits : info:eu-repo/semantics/openAccess
http://archimer.ifremer.fr/doc/1997/these-1265.pdf
http://archimer.ifremer.fr/doc/00000/1265/

Éditeur(s) : Pergamon-elsevier Science Ltd
Résumé : We report rare earth element (REE) and neodymium (Nd) isotope data for the organic fraction of sediments collected from various depositional environments, i.e. rivers (n=25), estuaries (n=18), open-ocean settings (n=15), and cold seeps (n=12). Sedimentary Organic Matter (SOM) was extracted using a mixed hydrogen peroxide/nitric acid solution (20%-H2O2 – 0.02M-HNO3), after removal of carbonate and oxy-hydroxide phases with dilute hydrochloric acid (0.25M-HCl). A series of experimental tests indicate that extraction of sedimentary organic compounds using H202 may be complicated occasionally by partial dissolution of sulphide minerals and residual carbonates. However, this contamination is expected to be minor for REE because measured concentrations in H2O2 leachates are about two-orders of magnitude higher than in the above mentioned phases. The mean REE concentrations determined in the H2O2 leachates for samples from rivers, estuaries, coastal seas and open-ocean settings yield relatively similar levels, with ΣREE = 109 ± 86 ppm (mean ± s; n=58). The organic fractions leached from cold seep sediments display even higher concentration levels (285 ± 150 ppm; mean ± s; n=12). The H2O2 leachates for most sediments exhibit remarkably similar shale-normalized REE patterns, all characterized by a mid-REE enrichment compared to the other REE. This suggests that the distribution of REE in leached sedimentary organic phases is controlled primarily by biogeochemical processes, rather than by the composition of the source from which they derive (e.g. pore, river or sea- water). The Nd isotopic compositions for organic phases leached from river sediments are very similar to those for the corresponding detrital fractions. In contrast, the SOM extracted from marine sediments display εNd values that typically range between the εNd signatures for terrestrial organic matter (inferred from the analysis of the sedimentary detrital fractions) and marine organic matter (inferred from the analysis of local surface seawater). A notable exception is the case of organic matter (OM) fractions leached from cold seep sediment samples, which sometimes exhibit εNd values markedly different from both terrigenous and surface seawater signatures. This suggests that a significant fraction of organic compounds in these sediments may be derived from chemosynthetic processes, recycling pore water REE characterized by a distinct isotopic composition. Overall, our results confirm that organic matter probably plays an important role in the oceanic REE budget, through direct scavenging and remineralization within the water column. Both the high REE abundances and the shape of shale-normalized patterns for leached SOM also suggest that OM degradation in sub-surface marine sediments during early diagenesis could control, to a large extent, the distribution of REE in pore waters. Benthic fluxes of organic-bound REE could hence substantially contribute to the exchange processes between particulates and seawater that take place at ocean margins. Neodymium isotopes could provide useful information for tracing the origin (terrestrial versus marine) and geographical provenance of organic matter, with potential applications in paleoceanography. In particular, future studies should further investigate the potential of Nd isotopes in organic compounds preserved in sedimentary records for reconstructing past variations of surface ocean circulation.
Geochimica Et Cosmochimica Acta (0016-7037) (Pergamon-elsevier Science Ltd), 2014-09 , Vol. 140 , P. 177-198

Droits : 2014 Elsevier Ltd. All rights reserved.
http://archimer.ifremer.fr/doc/00191/30250/28682.pdf
DOI:10.1016/j.gca.2014.05.016
http://archimer.ifremer.fr/doc/00191/30250/

Éditeur(s) : Université de Rennes 1
Résumé : Le devenir des bactéries entériques rejetées en mer a été étudié sur cinq zones côtières du littoral français : la côte Ouest du Cotentin, la rade de Brest, l'estuaire de Morlaix, la rade de Toulon et la Baie de Fort de France. Sur chaque site, une étude a permis de déterminer les concentrations en coli formes thermotolérants et en streptocoques fécaux dans les principaux apports. Les salmonelles ont également été recherchées sur trois de ces secteurs. Un calcul de flux permet d'apprécier l'importance des rejets urbains. Dans ces eaux généralement très chargées en contamination fécale, la présence de salmonelles a presque toujours été détectée. La qualité des eaux littorales et des sédiments côtiers a ensuite fait l'objet d'observations. Les caractéristiques des sites et des eaux rejetées déterminent les niveaux de contamination : nature des rejets (rivière ou rejets urbains), géométrie du site (côte ouverte, estuaire ou baie), hydrodynamisme. (mer à marée ou sans marée), présence de vasières, conditions climatiques, tous ces facteurs jouent un rôle important sur le devenir des bactéries. Ainsi, la variation des temps de survie d'Escherichia coli est due à la qualité du milieu récepteur: dans les eaux oligotrophes bien ensoleillées, l'effet de la lumière visible provoque une décroissance rapide des numérations bactériennes. Le T90 -temps nécessaire pour que 90 % des bactéries ne cultivent plus -est alors inférieur à deux ou trois heures. ln vitro, il a été démontré que la lumière visible agissait sur E. coli en présence d'oxygène par la production endogène d'espèces toxiques (principalement le peroxyde d'hydrogène et l'anion superoxyde). Cependant, la perte de cultivabilité des entérobactéries ne s'accompagne pas toujours d'une perte de la viabilité. De plus, il semblerait que le pouvoir pathogène puisse alors être conservé. Le rôle majeur de la lumière est atténué, voire annulé, par la présence de matières en suspension. Ces dernières jouent un rôle très important, en arrêtant les rayons lumineux, elles protègent les bactéries de l'effet bactéricide de certaines longueurs d'onde. Les T90 peuvent alors atteindre plu ieurs dizaines d'heures voire quelques jours. (...)

Droits : 1995 The author, Univ. Rennes 1
http://archimer.ifremer.fr/doc/00052/16319/13822.pdf
http://archimer.ifremer.fr/doc/00052/16319/