Éditeur(s) : HAL CCSD springer Link
Résumé : International audience
Experimental Astronomy

hal-01094521
https://hal.archives-ouvertes.fr/hal-01094521
BIBCODE : 2014ExA...tmp...41R
DOI : 10.1007/s10686-014-9383-4
ARXIV : 1310.0696

Éditeur(s) : HAL CCSD European Geosciences Union
Résumé : Xylem density is a physical property of wood that varies between individuals, species and environments. It reflects the physiological strategies of trees that lead to growth, survival and reproduction. Measurements of branch xylem density, ρx, were made for 1653 trees representing 598 species, sampled from 87 sites across the Amazon basin. Measured values ranged from 218 kg m−3 for a Cordia sagotii (Boraginaceae) from Mountagne de Tortue, French Guiana to 1130 kg m−3 for an Aiouea sp. (Lauraceae) from Caxiuana, Central Pará, Brazil. Analysis of variance showed significant differences in average ρx across regions and sampled plots as well as significant differences between families, genera and species. A partitioning of the total variance in the dataset showed that species identity (family, genera and species) accounted for 33% with environment (geographic location and plot) accounting for an additional 26%; the remaining "residual" variance accounted for 41% of the total variance. Variations in plot means, were, however, not only accountable by differences in species composition because xylem density of the most widely distributed species in our dataset varied systematically from plot to plot. Thus, as well as having a genetic component, branch xylem density is a plastic trait that, for any given species, varies according to where the tree is growing in a predictable manner. Within the analysed taxa, exceptions to this general rule seem to be pioneer species belonging for example to the Urticaceae whose branch xylem density is more constrained than most species sampled in this study. These patterns of variation of branch xylem density across Amazonia suggest a large functional diversity amongst Amazonian trees which is not well understood.
ISSN: 1726-4170

hal-01032137
https://hal.archives-ouvertes.fr/hal-01032137

Éditeur(s) : Gauthier-Villars
Oceanologica Acta (0399-1784) (Gauthier-Villars), 1990 , Vol. 13 , N. 4 , P. 513-524

Droits : info:eu-repo/semantics/openAccess
http://archimer.ifremer.fr/doc/00103/21421/18998.pdf
http://archimer.ifremer.fr/doc/00103/21421/

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

Droits : 2008 Elsevier B.V. All rights reserved.
http://archimer.ifremer.fr/doc/2008/publication-6855.pdf
DOI:10.1016/j.margeo.2008.09.002

Éditeur(s) : Gauthier-villars
Résumé : The aim of the HYFIFLUX-SONNE 99 cruise was the geological, biological and chemical study of the 2 triple-junctions characterizing the oceanic accretion in the North Fiji Basin. Multibeam bathymetric coverage, in situ observations and sampling confirmed the existence of an active spreading ridge immediately west of the Fiji islands (WFR), and gave an evaluation of the magmatic and hydrothermal activity of the central ridge (CSR). New hydrothermal sites have been discovered and sampled.
La campagne HYFIFLUX-SONNE 99 a eu pour objectif l'étude géologique, biologique et chimique des 2 triples jonctions qui caractérisent l'accrétion océanique dans le bassin nord fidjien. La couverture bathymétrique multifaisceaux, l'observation in situ et l'échantillonnage ont permis de confirmer l'existence d'un axe d'accrétion actif immédiatement à l'Ouest des îles Fidji (WFR), et d'évaluer l'activité magmatique et hydrothermale à l'extrémité nord de l'axe central (CSR). De nouveaux sites hydrothermaux ont été découverts et échantillonnés.
Comptes Rendus de l'Academie des Sciences Serie II Fascicule A-Sciences de la Terre et des Planetes (Gauthier-villars), 1995-08 , Vol. 321 , N. 3 , P. 239-246

Droits : Académie des Sciences
http://archimer.ifremer.fr/doc/00183/29453/27843.pdf
http://archimer.ifremer.fr/doc/00183/29453/

Éditeur(s) : HAL CCSD American Geophysical Union (AGU)
Résumé : Structural, metamorphic, and geochronologic work shows that the Ampelos/Dilek nappe of the Cycladic blueschist unit in the eastern Aegean constitutes a wedge of high-pressure rocks extruded during early stages of orogeny. The extrusion wedge formed during the incipient collision of the Anatolian microcontinent with Eurasia when subduction and deep underthrusting ceased and the Ampelos/Dilek nappe was thrust southward over the greenschist-facies Menderes nappes along its lower tectonic contact, the Cycladic-Menderes thrust, effectively cutting out a ∼30- to 40-km-thick section of crust. The upper contact of the Ampelos/Dilek extrusion wedge is the top-to-the-NE Selçuk normal shear zone, along which the Ampelos/Dilek nappe was exhumed by ∼30–40 km. Detailed Rb-Sr and 40Ar/39Ar dating of mylonites demonstrates that both shear zones operated between 42 and 32 Ma. There is no evidence for episodic motion during the ∼10 Myr life span of the shear zones, suggesting that both shear zones operated in a steady, nonepisodic fashion. Our data provide supporting evidence that simultaneous thrust-type and normal sense shearing can accomplish the early exhumation of deep-seated rocks
ISSN: 0278-7407

hal-00405013
https://hal.archives-ouvertes.fr/hal-00405013
DOI : 10.1029/2005TC001872

Éditeur(s) : Station Biologique de Roscoff
Résumé : The hydrothermal vent shrimp genus Mirocaris is reviewed. Morphological comparison between the two nominal species in the genus, M. fortunata and M. keldyshi, was made based on the re-examination of the holotype and paratypes of Mirocarisfortunata and the paratypes of M. keldyshi. Samples newly collected from various sites on the Mid-Atlantic Ridge were also examined. The validity of the genus Mirocaris has been confirmed. However, our study has revealed that the supposed morphological characters distinguishing M. fortunata and M. keldyshi do not provide significant taxonomic differences and further comparison failed to detect morphological differences between the two taxa. Thus M. keldyshi is synonymized with M. fortunata, and so there is only one single species in the genus Mirocaris. This supports the suggestion by Shank et al. (1999), based on a molecular study, that the two taxa might be conspecific. A redescription of M. fortunata is provided to better establish the morphology of the species. The clarification led us to improve the morphological descriptions of the caridean species associated with vent or seep environments and to reassess the relationships among Mirocaris and the other shrimp taxa in the superfamily Bresilioidea. The generic diagnosis of Mirocaris is emended. Because a number of presumably apomorphic characters are shared by Mirocaris and other alvinocaridid genera, the genus Mirocaris is now assigned to the family Alvinocarididae. The family Mirocarididae is synonymized with the Alvinocarididae and the diagnosis of this family is emended.
Révision du genre Mirocaris, crevette des sources hydrothermales océaniques, redescription de M. fortunata et réexamen du statut de la famille des Alvinocarididae. Le genre Mirocaris, créé pour des crevettes hydrothermales, est révisé. Une étude morphologique comparative des deux espèces Mirocaris fortunata et M. keldyshi, basée sur le réexamen des holo-types et paratypes et sur l'étude de nombreux échantillons provenant de divers sites hydrothermaux de la dorsale médio-atlantique, a été effectuée. La validité du genre Mirocaris est confirmée. Il apparaît que les caractères qui distinguent M. keldyshi et M.fortunata ne sont pas des critères taxonomiques suffisants et une étude morphologique plus poussée n'a pas révélé de différences morphologiques entre les deux taxa. Ceci est en accord avec l'interprétation de Shank et al. (1999) qui, à la suite d'une étude moléculaire, suggèrent la synonymie des deux espèces. Une redescription détaillée de M. fortunata est donnée et les relations entre Mirocaris et les autres genres de la superfamille des Bresilioidea sont discutées. La diagnose générique de Mirocaris est modifiée. Comme plusieurs caractères apomorphes sont partagés par Mirocaris et les autres genres de la famille des Alvinocarididae, le genre Mirocaris est maintenant affecté à cette famille. La famille des Mirocarididae est mise en synonymie avec celle des Alvinocarididae dont la diagnose est modifiée.
CBM - Cahiers de Biologie Marine (0007-9723) (Station Biologique de Roscoff), 2003-03 , Vol. 44 , N. 2 , P. 199-215

Droits : 2003 Station Biologique de Roscoff
http://archimer.ifremer.fr/doc/2003/publication-883.pdf
http://archimer.ifremer.fr/doc/00000/883/

Éditeur(s) : Caribbean Volunteer Expeditions Caribbean Volunteer Expeditions ( Corning, NY )

Droits : All rights reserved by the source institution.

Éditeur(s) : HAL CCSD AGU and the Geochemical Society
Résumé : International audience
The South Pacific region is characterized by a broadly elevated seafloor known as the South Pacific superswell. This region has a concentration of midplate volcanoes that experienced massive eruptions in the mid-Cretaceous period (90-120 Ma). These characteristics suggest the presence of a large-scale mantle plume beneath the South Pacific, called the South Pacific superplume. The geometry, origin depth, temperature, and composition of the superplume remain controversial, however, mainly due to the lack of seismological data that documents the mantle structure beneath the South Pacific. Seismic stations are sparse in the area due to its remote ocean environment. To obtain a better seismic image of the superplume, we deployed temporary broadband seismographs on oceanic islands and the seafloor in the South Pacific, which made possible the highest spatial resolution that has ever been achieved for the mantle structure beneath the region. The seismic image obtained from this new seismic data indicates that large-scale low-velocity anomalies (on the order of 1000 km in diameter), indicative of the superplume, are located from the bottom of the mantle to a depth of 1000 km, and small-scale low-velocity anomalies (on the order of 100 km in diameter) are present above it. A comparison of the seismic image with recent mantle convection studies based upon laboratory and numerical experiments suggests that the superplume may be a hot and chemically distinct mantle dome, and that the small-scale anomalies may be narrow plumes generated from the top of the dome. This model may explain various characteristics of hot spots in the South Pacific, such as the seafloor swell, short-lived hot spot chains, and the periodicity of massive eruptions.
ISSN: 1525-2027

hal-00443845
https://hal.archives-ouvertes.fr/hal-00443845
https://hal.archives-ouvertes.fr/hal-00443845/document
https://hal.archives-ouvertes.fr/hal-00443845/file/Suetsugu_PLUME_tomo_G32009_hal.pdf
DOI : 10.1029/2009GC002533

Éditeur(s) : F. Lucas, Jr. ( [Baltimore )
Résumé : (Citation/Reference) Phillips,
From: A general atlas, map # 82
Relief shown by hachures.
Prime meridian: London.
(Funding) Funded in part by the University of Florida, the Florida Heritage Project of the State University Libraries of Florida, the Institute for Museum and Library Services, and the U.S. Department of Education's TICFIA granting program.
(Statement of Responsibility) drawn and published by F. Lucas, Jr. ; B.T. Welch & Co., sc.
Jamaica

Droits : This item is presumed to be in the public domain. The University of Florida George A. Smathers Libraries respect the intellectual property rights of others and do not claim any copyright interest in this item. Users of this work have responsibility for determining copyright status prior to reusing, publishing or reproducing this item for purposes other than what is allowed by fair use or other copyright exemptions. Any reuse of this item in excess of fair use or other copyright exemptions may require permission of the copyright holder. The Smathers Libraries would like to learn more about this item and invite individuals or organizations to contact Digital Services (UFDC@uflib.ufl.edu) with any additional information they can provide.
002357153
ALW1590
174120078
http://ufdc.ufl.edu/UF90000461/00001

Éditeur(s) : HAL CCSD
Résumé : 38 pages
Rapport
The Chicxulub impact crater, México, is unique. It is the only known terrestrial impact structure that has been directly linked to a mass extinction event and the only terrestrial impact with a global ejecta layer. Of the three largest impact structures on Earth, Chicxulub is the best preserved. Chicxulub is also the only known terrestrial impact structure with an intact, unequivocal topographic peak ring. Chicxulub’s role in the Cretaceous/Paleogene (K-Pg) mass extinction and its exceptional state of preservation make it an important natural laboratory for the study of both large impact crater formation on Earth and other planets and the effects of large impacts on the Earth’s environment and ecology. Our understanding of the impact process is far from complete, and despite more than 30 years of intense debate, we are still striving to answer the question as to why this impact was so catastrophic.During International Ocean Discovery Program (IODP) Expedition 364, Paleogene sediments and lithologies that make up the Chicxulub peak ring were cored to investigate (1) the nature and formational mechanism of peak rings, (2) how rocks are weakened during large impacts, (3) the nature and extent of post-impact hydrothermal circulation, (4) the deep biosphere and habitability of the peak ring, and (5) the recovery of life in a sterile zone. Other key targets included sampling the transition through a rare midlatitude section that might include Eocene and Paleocene hyperthermals and/or the Paleocene/Eocene Thermal Maximum (PETM); the composition and character of the impact breccias, melt rocks, and peak-ring rocks; the sedimentology and stratigraphy of the Paleocene–Eocene Chicxulub impact basin infill; the chronology of the peak-ring rocks; and any observations from the core that may help us constrain the volume of dust and climatically active gases released into the stratosphere by this impact. Petrophysical property measurements on the core and wireline logs acquired during Expedition 364 will be used to calibrate geophysical models, including seismic reflection and potential field data, and the integration of all the data will calibrate impact crater models for crater formation and environmental effects. The proposed drilling directly contributes to IODP Science Plan goals:Climate and Ocean Change: How resilient is the ocean to chemical perturbations? The Chicxulub impact represents an external forcing event that caused a 75% level mass extinction. The impact basin may also record key hyperthermals within the Paleogene.Biosphere Frontiers: What are the origin, composition, and global significance of subseafloor communities? What are the limits of life in the subseafloor? How sensitive are ecosystems and biodiversity to environmental change? Impact craters can create habitats for subsurface life, and Chicxulub may provide information on potential habitats for life, including extremophiles, on the early Earth and other planetary bodies. Paleontological and geochemical studies at ground zero will document how large impacts affect ecosystems and effects on biodiversity.Earth Connections/Earth in Motion: What are the composition, structure and dynamics of Earth’s upper mantle? What mechanisms control the occurrence of destructive earthquakes, landslides, and tsunami? Mantle uplift in response to impacts provides insight into dynamics that differ between Earth and other rocky planets. Impacts generate earthquakes, landslides, and tsunami, and scales that generally exceed plate tectonic processes yield insight into effects, the geologic record, and potential hazards.IODP Expedition 364 was a Mission Specific Platform expedition to obtain subseabed samples and downhole logging measurements from the sedimentary cover sequence and peak ring of the Chicxulub impact crater. A single borehole was drilled into the Chicxulub impact crater on the Yucatán continental shelf, recovering core from 505.7 to 1334.73 m below seafloor with ~99% core recovery and acquiring downhole logs for the entire depth.
International Ocean Discovery Program

hal-01639520
https://hal.archives-ouvertes.fr/hal-01639520
DOI : 10.14379/iodp.pr.364.2017

Résumé : (Funding) Support for the development of the technical infrastructure and partner training provided by the United States Department of Education TICFIA program.
Saint Thomas (V.I.)
Caribbean

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
The chemical investigations of Dicorynia guianensis heartwood led to the isolation of four new indole alkaloids for the first time in this plant. Compound (1) identified as spiroindolone 20,30,40,90-tetrahydrospiro [indoline-3,10pyrido[3,4-b]-indol]-2-one, and compound (3) described as nitrone 1-methyl-4,9-dihydro-3H-pyrido [3,4-b] indole 2-oxide and were isolated for the first time as natural products. ABTS antioxidant activity guided their isolation.
ISSN: 1874-3900

hal-01138910
https://hal.archives-ouvertes.fr/hal-01138910
DOI : 10.1016/j.phytol.2015.03

Éditeur(s) : HAL CCSD Publisher : Paris : Baillière [1980-. Latest Publisher : Paris : Elsevier
Résumé : National audience
Introduction Les monocytes sont constitués de populations cellulaires hétérogènes aux propriétés distinctes. Il est retrouvé une sur-représentation de la population monocytaire CD14+/CD16+ pro-inflammatoire au cours de certaines connectivites. Cette population monocytaire s’oppose aux monocytes CD14+/CD16– qui jouent un moindre rôle dans l’amplification de la réponse inflammatoire. Les monocytes et les macrophages pourraient jouer un rôle central dans les mécanismes de fibrose au cours de la sclérodermie systémique. L’association entre les manifestations cliniques de la sclérodermie systémique et les différentes populations monocytaires reste à préciser. L’objectif de cette étude « proof of concept »est d’évaluer l’association entre la population monocytaire CD14+/CD16+ et les manifestations cliniques de fibrose chez les patients sclérodermiques. Patients et méthodes Cinquante-cinq patients répondant aux critères ACR 2013 de sclérodermie systémique ont été inclus de manière consécutive de mars à juillet 2015. Les atteintes fibrosantes ont été évaluées simultanément selon les données du bilan viscéral annuel en centre de compétence : l’atteinte cutanée était évaluée cliniquement selon le score de Rodnan modifié, les patients étaient classés selon la classification de Leroy (atteinte cutanée diffuse, atteinte cutanée limitée, sine scleroderma). La présence d’une pneumopathie interstitielle diffuse était évaluée par TDM thoracique, son retentissement sur la fonction respiratoire était précisé par les épreuves fonctionnelles respiratoires (capacité pulmonaire totale, capacité vitale forcée, DLCO). La NFS réalisée le jour du bilan viscéral était traitée en hématoflow permettant de préciser les sous populations monocytaires en fonction de leur statut CD16+ ou CD16–. Les données cliniques étaient relevées en aveugle vis-à-vis des données de cytométrie en flux. Résultats 55 patients sclérodermiques ont été inclus. Le taux moyen de monocytes CD16+ était de 0,054 G/L (SD = 0,029). Les patients avec une atteinte cutanée diffuse avaient des taux significativement plus élevés de monocytes CD16+ (p = 0,021), alors que les taux de monocytes CD16–ne différaient pas entre les patients avec atteinte cutanée diffuse et cutanée limitée. Le score de Rodnan modifié était corrélé de manière significative avec le taux de monocytes CD16+ (R = 0,513, p < 0,001). Il existait une tendance à l’association entre des taux élevés de CD16+ et la présence d’une pneumopathie interstitielle diffuse détectée par TDM (p = 0,113). Il existait une corrélation négative significative (p < 0,05) entre les taux de CD16+ et les résultats des épreuves fonctionnelles respiratoires (capacité pulmonaire totale et DLCO), attestant d’une fonction respiratoire moins bonne chez les patients à taux plus élevés de monocytes CD16+. Il n’était pas retrouvé d’association entre les taux de CD16+ et les autres paramètres cliniques ou immunologiques. Discussion Cette étude « proof of concept » semble montrer une association entre des taux élevés de monocytes CD16+ et certains paramètres de gravité des atteintes fibrosantes de la maladie. En plus de leur association à la gravité des atteintes fibrosantes de la sclérodermie systémique, les taux de monocytes CD16+ pourraient également avoir un intérêt pronostique qui reste à évaluer. Des travaux in vitro ont montré que l’ajout de TGFb au milieu de culture cellulaire de monocytes induisait une augmentation de l’expression du CD16+ par ces monocytes. Les monocytes CD16+ sont également une source de production d’IL-1 bêta et de TNF alpha pro-inflammatoires. D’autres travaux in vitro ont très récemment démontré la plus grande capacité des monocytes CD16+ à se différencier préférentiellement en macrophages ayant également des propriétés pro-inflammatoires. La sous-population monocytaire CD16+ peut également être hiérarchisée en fonction de l’intensité d’expression du CD16. La place précise de ces différentes populations monocytaires dans la physiopathologie de la sclérodermie systémique reste encore à déterminer. Les liens ténus entre monocytes et macrophages, dont l’implication est maintenant reconnue au cours de la sclérodermie invitent à investiguer davantage le rôle possible du monocyte dans le cadre de cette maladie inflammatoire et fibrosante afin d’identifier d’éventuelles nouvelles cibles thérapeutiques ou marqueurs pronostiques. Conclusion Dans cette étude « proof of concept », sur un nombre restreint de patients atteints de sclérodermie systémique répondants aux critères ACR 2013, le taux de monocytes CD16+ semble corrélé avec les atteintes fibrosantes de la maladie, laissant supposer une implication possible de cette sous-population monocytaire dans la physiopathologie de cette connectivite
ISSN: 0248-8663

hal-01321851
https://hal-univ-rennes1.archives-ouvertes.fr/hal-01321851
DOI : 10.1016/j.revmed.2016.04.253

Éditeur(s) : HAL CCSD
Résumé : International audience
Objective Macrophages may play a significant role in the initiating stages leading to chronic inflammation/infection in cystic fibrosis (CF), via an inability to act as a suppressor cell. In a previous study demonstrating impaired function of CF macrophage, we have shown high production of soluble CD14 (sCD14). The aim of the present work is to determine origin and function of sCD14 in blood monocyte-derived macrophages from stable adult CF patients. Methods To study origin, sCD14 is measured by ELISA in supernatant of macrophages from healthy subjects (non-CF) treated with PI-PLC or cholesterol. The involvement of sCD14 in inflammation, was investigated by analysis of NF-kB and caspase 1 pathways in non-CF macrophages treated by sCD14. Measurement of gene expression was done by qPCR and proteins were quantified by ELISA and Western blot. Results Treatment with PI-PLC increased sCD14 level in the supernatant of non-CF macrophages whereas cholesterol did not modified it. Furthermore high secretion of sCD14 from CF macrophages was decreased by an inhibitor of PI-PLC. Treatment with sCD14 increased pro-IL-1β, IL-8 and TNF-α expression resulting from NF-kB activation through IkBa phosphorylation, this effect was inhibited by NF-kB inhibitors. Also, activation of caspase 1 by cleavage of pro-caspase 1 allowed the secretion of mature IL-1β, inhibited by an inhibitor of caspase 1. However, inflammasome complex involved in caspase 1 activation remains to be determined. Conclusion This data show that origin of sCD14 is partly due to the action of lipases cutting the GPI tail that serves as a membrane anchor to CD14. Furthermore sCD14 have a role in chronic inflammation in CF
the 38th European Cystic Fibrosis Conference
Vienne, Austria

hal-01162773
https://hal-univ-rennes1.archives-ouvertes.fr/hal-01162773
DOI : 10.1016/S1569-1993(15)30203-4

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
ISSN: 0006-3207

hal-01090646
https://hal-agroparistech.archives-ouvertes.fr/hal-01090646
DOI : 10.1016/j.biocon.2010.07.034

Éditeur(s) : HAL CCSD Oldendorf/Luhe
Résumé : International audience
Large filamentous sulfur-oxidizing bacteria belonging to the Beggiatoacae family can cover large portions of shallow marine sediments surrounding mangroves in Guadeloupe (French West Indies). In order to assess the importance of Beggiatoa mats as an infaunal food source, observations were conducted of the area within mats and at increasing distances from mats. We used natural isotopic compositions and a C-13 enrichment study. Both revealed an ingestion of bacterial mats by associated meiofauna, dominated by rotifers and to a smaller extent by small polychaetes and nematodes. Compared to adjacent sites, sediment covered by bacterial mats presented a higher abundance of diatoms, whereas the total biomass of bacteria did not vary. This constant bacterial abundance suggests that the proportion of organic matter represented by sulfur bacteria is limited compared to the fraction of total bacteria. There was no significant difference in infaunal abundance in mats, suggesting that the availability of this chemosynthetic food resource had a limited local effect. Grazers presented a delta C-13 value increasing with distance from the mat. However, isotopic composition of phospholipid-derived fatty acids specific for diatoms and bacteria revealed that this change is related to modifications of delta C-13 dietary components rather than to changes in diet composition. These complementary methods revealed that the occurrence of sulfur-oxidizing bacterial mats does not necessarily affect grazer abundance and importance of bacteria in their diet. Despite its wide occurrence, Beggiatoa mats would consequently have a minor influence on the structure of the mangrove food web.
ISSN: 0171-8630

hal-01545912
https://hal.archives-ouvertes.fr/hal-01545912
DOI : 10.3354/meps11035

Éditeur(s) : HAL CCSD Wiley
Résumé : International audience
ISSN: 1354-1013

hal-01080954
https://hal-agroparistech.archives-ouvertes.fr/hal-01080954
DOI : 10.1111/j.1365-2486.2007.01439.x

Éditeur(s) : HAL CCSD European Geosciences Union (EGU)
Résumé : International audience
The transformation of nonlinear long internal waves in a two-layer fluid is studied in the Boussinesq and rigid-lid approximation. Explicit analytic formulation of the evolution equation in terms of the Riemann invariants allows us to obtain analytical results characterizing strongly nonlinear wave steepening, including the spectral evolution. Effects manifesting the action of high nonlinear corrections of the model are highlighted. It is shown, in particular, that the breaking points on the wave profile may shift from the zero-crossing level. The wave steepening happens in a different way if the density jump is placed near the middle of the water bulk: then the wave deformation is almost symmetrical and two phases appear where the wave breaks.
ISSN: 1023-5809

hal-00331099
https://hal.archives-ouvertes.fr/hal-00331099
https://hal.archives-ouvertes.fr/hal-00331099/document
https://hal.archives-ouvertes.fr/hal-00331099/file/npg-14-247-2007.pdf

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
Laboratory models have been conducted to improve our understanding of the role that the resistance of the slab to bending and its coupling to the ambient mantle play in subduction dynamics over geological time scales. Our models are set up with a viscous plate of silicone (lithosphere) subducting under negative buoyancy in a viscous layer of glucose syrup (mantle). For our study, the lithosphere/upper mantle viscosity contrast has been systematically varied, from similar to 10 to similar to 10(5) in order to explore the parameter space between weak and strong slab dynamics. We found that subduction is characterized by a retreating mode for viscosity ratios > 10(4), by the coexistence of a retreating mode and an advancing mode for viscosity ratios between similar to 10(4) and similar to 10(2), and quasi-stationary, Rayleigh-Taylor like behaviour for ratios < 10(2). By combining our experimental results and kinematic data from current subduction zones in four reference frames which differ in the amount of net rotation, we infer that a lithosphere/upper mantle viscosity contrast of 150-500 is necessary to obtain realistic trench/subducting plate velocity ratios as well as the variability of subduction styles observed in nature.
ISSN: 0012-821X

hal-00412008
https://hal.archives-ouvertes.fr/hal-00412008
DOI : 10.1016/j.epsl.2008.04.006