Éditeur(s) : Pêche thonière et dispositifs de concentration de poissons, Caribbean-Martinique, 15-19 Oct 1999
Résumé : This paper discusses the hypothesis that small tunas and the various species found in association with drifting fads (such as "mahi-mahi", rainbow runner, wahoo, etc.) may be biologically trapped by such a strong association. Massive seeding of drifting artificial fads was observed worldwide during recent years. In this hypothesis, we suggest that fads may alter some biological characteristics of epipelagic populations associated with them: migration, growth, condition factors, predation and natural mortality. As fads are most often used in the equatorial currents, they tend to exhibit zonal drift. Therefore, the associated populations would be artificially transferred from one part of the ocean to another, when they would show different movement patterns in the absence of fads. Natural logs were probably beneficial in terms of ecology and evolution, because they tend to accumulate in convergence areas, most often considered as rich forage areas. Now, fads are seeded in offshore areas, which are not necessarily favourable for tuna feeding. This apparently strong association between fishes and drifting fads may then produce an unexpected biological impact on tuna populations and their associated fauna. The plan is to test this hypothesis in the Atlantic, developing an ad hoc research programme based on tagging, biological and physiological studies, in association to an analysis of high resolution fishery data before and after the development of the fad fishery.Original Abstract: Cet article discute l'hypothese selon laquelle les petits thons et les differentes especes associees a des DCP derivants (comme les coryphenes, elagatis, thazards, etc.) pourraient etre pris dans un piege biologique resultant de cette forte association. Le deploiement massif de DCP artificiels derivants a ete constate a l'echelle mondiale au cours des dernieres annees. Dans cette hypothese, ces DCP, colonises en permanence par de grandes fractions de populations epipelagiques, pourraient modifier les caracteristiques biologiques des especes concernees: leur migration, leur croissance, leurs facteurs de condition, la predation et la mortalite naturelle. Les DCP etant plus frequemment utilises dans les courants equatoriaux, ils tendent a deriver zonalement. Ainsi, les populations associees seraient artificiellement transferees d'un bord a l'autre de l'ocean, alors qu'elles manifesteraient d'autres types de deplacements en l'absence de DCP. Les debris naturels etaient probablement benefiques sur le plan de l'ecologie et de l'evolution car ils s'accumulent dans des zones de convergence le plus souvent considerees comme des zones riches en nourriture. Maintenant, les DCP sont mouilles au large, dans des zones qui peuvent ou non etre favorables a l'alimentation des thons. Cette association apparemment forte entre poissons et DCP derivants pourrait alors causer un impact biologique inattendu sur les populations pelagiques (thons et faune accompagnante). L'objectif est de tester cette hypothese dans l'Atlantique au moyen d'un programme de recherche s'appuyant sur du marquage et des etudes biologiques et physiologiques, parallelement a une analyse des donnees de peche (tailles et CPUE, avant et apres le deploiement des DCP derivants).

Droits : info:eu-repo/semantics/openAccess
http://archimer.ifremer.fr/doc/00042/15303/12636.pdf
http://archimer.ifremer.fr/doc/00042/15303/

Éditeur(s) : HAL CCSD Public Library of Science
Résumé : International audience
While the fire coral Millepora platyphylla is an important component of Indo-Pacific reefs,where it thrives in a wide range of environments, the ecological and biological processesdriving its distribution and population structure are not well understood. Here, we quantifiedthis species' population structure in five habitats with contrasting hydrodynamic regimes inMoorea, French Polynesia; two in the fore reef: mid and upper slopes, and three in thelagoon: back, fringing and patch reefs. A total of 3651 colonies of fire corals were mappedand measured over 45,000 m2 of surveyed reef. Due to the species' sensitivity to fragmentationin response to strong water movement, hydrodynamic conditions (e.g. waves, pass andlagoonal circulation) corresponded to marked differences in colony size distributions, morphologyand recruitment dynamics among habitats. The size structure varied among reefhabitats with higher proportions of larger colonies in calm nearshore reefs (fringing andpatch reefs), while populations were dominated by smaller colonies in the exposed forereefs. The highest densities of fire corals were recorded in fore reef habitats (0.12±0.20 n.m-2) where the proportion of recruits and juveniles was higher at mid slope populations(49.3%) than on the upper slope near where waves break (29.0%). In the latter habitat, mostcolonies grew as vertical sheets on encrusting bases making them more vulnerable to colonyfragmentation, whereas fire corals were encrusting or massive in all other habitats. Thelowest densities of M. platyphylla occurred in lagoonal habitats (0.02±0.04 n.m-2) characterizedby a combination of low water movement and other physical and biological stressors.This study reports the first evidence of population structure of fire corals
ISSN: 1932-6203

hal-01561659
https://hal-univ-perp.archives-ouvertes.fr/hal-01561659
https://hal-univ-perp.archives-ouvertes.fr/hal-01561659/document
https://hal-univ-perp.archives-ouvertes.fr/hal-01561659/file/millepora%20platyphylla.pdf
DOI : 10.1371/journal.pone.0173513

Éditeur(s) : HAL CCSD
Résumé : International audience
Coming from Crimea, the Black Death spread to Western Europe and North Africa during the 1340s. From 1346 to 1352, the plague killed an estimated 25-40% of Europeans of all age-groups [1] , i.e., 30 to 60% of Europe population. One of the earliest and most widely accepted explanations was that God was punishing humanity for their sins. One remedy for the curse was to do penitence. Thus in 1348 there rapidly arose a mass movement of flagellation [2]. In fact flagellation could not really help against such threat. The Black Death or Bubonic plague is caused by Yersinia pestis, a Eubacteria discovered in 1894 by Alexandre Yersin. It is transmitted by the bite of the flea Xenopsylla cheopsis. This flea lives by feeding the blood of many species besides man but its most preferred relationship is with the black rat (Rattus rattus). Fossilized remains of the plague flea have been found in large numbers in Amarna, Egypt [3, 4] about 1350 BC, and thus could be directly linked to the events described in the Book of Samuel [5, 6]. During the epidemic of Bubonic plague in London in 1665-1666, the known treatments were made use of, e.g. the so-famous Theriac or Venice Treacle which is used from the time of ancient Rome as a remedy against poison [7]. Since then, more specialized and novel treatments have been developed. However, since the characterization of Yersinia pestis, numerous drugs have been developed against it, e.g. gentamicin or doxycycline [8]. These researches had been carried out using more elaborated biochemical, biophysical and biological approaches.
Infectious disorders drug targets

Droits : info:eu-repo/semantics/OpenAccess
inserm-00395256
http://www.hal.inserm.fr/inserm-00395256
http://www.hal.inserm.fr/inserm-00395256/document
http://www.hal.inserm.fr/inserm-00395256/file/editorial.pdf
http://www.hal.inserm.fr/inserm-00395256/file/inserm-00395256_edited.pdf

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
The Tso Morari serpentinites in the Ladakh area, northwest Himalaya, originated from the forearc mantle overlying the northward subducting Neo-Tethys lithosphere and the margin of the Indian continent. The serpentinites are characterized by high concentration of fluid-mobile elements (FME: As, Sb, B, Li, and U) compared to ophiolitic or abyssal serpentinites. The Pb isotopic compositions of serpentinites show influence of the subducted Indian continental lithosphere. Trace element concentrations of antigorite determined in situ with Laser Ablation High Resolution Inductively Coupled Mass Spectrometer (LA-HR-ICP-MS) show high contents of FME including Pb, in contrast to the spatially associated iron oxides. Rare earth elements (REE) and compatible elements, such as Sc and Co, remained immobile during the hydration, allowing the identification of the primary minerals (olivine or orthopyroxene) from which serpentine formed. Serpentinized olivine displays higher Sb and As concentrations (up to 1000 x PM) than serpentinized orthopyroxenes that are enriched in Pb, Cs and Li (2 to up to 10 x PM).;We propose that the observed FME distribution in two types of serpentine reflect the differential incorporation of FME during the downward movement of the serpentinite along the subduction plane. At temperature lower than 400 degrees C, at shallow depths, olivine is preferentially serpentinized and incorporates elements that are fluid soluble at low temperatures, such as Sb and As. Above 400 degrees C, orthopyroxene is hydrated and incorporates Pb, Cs, Li and possibly Ba. Boron and U are incorporated in both types of serpentine suggesting that they are released from slabs at temperatures around 300-400 degrees C. The serpentine acts as a sink for water, but also for FME and transports them to deeper and hotter levels in the mantle, down to the isotherm 600-650 degrees C where dehydration occurs.
ISSN: 0009-2541

hal-00475565
https://hal.archives-ouvertes.fr/hal-00475565
DOI : 10.1016/j.chemgeo.2009.10.002

Éditeur(s) : HAL CCSD American Geophysical Union
Résumé : During the 2003 summer monsoon, the Hi-CLIMB seismological stations deployed across the Himalayan Range detected bursts of high-frequency seismic noise that lasted several hours to days. On the basis of the cross correlation of seismic envelopes recorded at 11 stations, we show that the largest transient event on 15 August was located nearby a village partially destroyed on that day by a devastating debris flow. This consistency in both space and time suggests that high-frequency seismic noise analysis can be used to monitor debris flow generation as well as the evacuation of the sediment. A systematic study of one year of seismic noise, focusing on the detection of similar events, provides information on the spatial and temporal occurrence of mass movements at the front of the Himalayas. With a 50% probability of occurrence of a daily event, a total of 46 debris flows are seismically detected. Most of them were generated in regions of steep slopes, large gullies, and loose soils during the 2003 summer monsoon storms. These events are compared to local meteorological data to determine rainfall thresholds for slope failures, including the cumulative rainfall needed to bring the soil moisture content to failure capacity. The inferred thresholds are consistent with previous estimates deduced from soil studies as well as sediment supply investigations in the area. These results point out the potential of using seismic noise as a dedicated tool for monitoring the spatiotemporal occurrence of landslides and debris flows on a regional scale.
ISSN: 0148-0227

hal-00464177
https://hal.archives-ouvertes.fr/hal-00464177
DOI : 10.1029/2008JF001198

Éditeur(s) : Université des Antilles Études caribéennes
Résumé : Au début de l’année 2009, la Guadeloupe a connu un mouvement social et politique d’ampleur : quarante-quatre jours de grève générale. Le but de cette recherche est de parvenir à classer cet événement récent en recourant à une méthode hétérotopologique, tout en reconnaissant sa qualité de mouvement contestataire dans la théorie des nouveaux mouvements sociaux. En saisissant l’épistémè du Lyinnaj Kont Pwofitasyon, il deviendra possible de mieux comprendre, outre les propos journalistiques, son sens et son essence. Mouvement de masses, syndicalisme révolutionnaire et appel à l’unité nationale, tels sont les outils dont use le collectif en vue de la lutte contre les « pwofitans » ; outils qui, contrairement à ce que l’on entend çà et là dans les médias et autres travaux de recherche, ne relève guère du jamais vu, mais bien du déjà vu et, sans doute, du reja vu. Il est donc question de relativiser ici l’impact idéologique du LKP, en saisissant la spécificité de son utopie régressive à contenu historique, tout en le resituant à la même hauteur que les autres mouvements du même type, dans de nombreux pays, que l’histoire a vu se développer au cours des xixe et xxe siècles.
At the beginning of 2009, a large social movement hit the island of Guadeloupe: a forty-four-day general strike. The point of this study is to historically position this recent event. It is suggested that identifying the episteme from which the LKP operates helps make sense of this social movement. Mass movements, nationalism, propaganda are the tools the group uses to fight the “pwofitans” – the capitalists. And these tools cannot be considered as jamais vu but indeed as déjà vu and, probably, reja vu. I propose here to reinsert the ideological impact of LKP in its own context and history and to compare it to many similar movements in the 19th and 20th centuries.
Guadeloupe

Droits : info:eu-repo/semantics/openAccess
urn:doi:10.4000/etudescaribeennes.7238
http://journals.openedition.org/etudescaribeennes/7238

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

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

Éditeur(s) : Université des Antilles Études caribéennes
Résumé : A partir d’une étude comparée originale qui met en perspective des expériences insulaires prises en Corse et en Martinique, cette communication interroge la portée de l’éco-tourisme comme alternative au tourisme de masse pour les territoires insulaires français. Les deux destinations touristiques sont tout d’abord présentées brièvement : l’examen du type de tourisme développé et de ses conséquences socio-spatiales amène à discuter, pour chacune des îles, l’existence d’une attente sociétale prégnante pour faire du tourisme autrement. Il est ensuite montré que le positionnement des pouvoirs publics en matière de tourisme alternatif, qui reste de l’ordre du discours, incite les acteurs locaux à mener leurs propres projets. Or, en matière de développement local, les retombées de ces initiatives locales, éparses et disjointes, sont somme toute très faibles. Ces constats conduisent à la présentation d’un modèle conceptuel d’écotourisme pour les territoires insulaires, qui cherche autant à clarifier la définition de l’écotourisme qu’à ouvrir la discussion sur des recommandations pour aller vers plus de durabilité.
From a comparative study of original that puts into perspective the experiences made in Corsica and Martinique islands, this paper questions the scope of eco-tourism as an alternative to mass tourism to the French islands. Both destinations are first presented briefly review the type of developed tourism and its socio-spatial causes discussed for each of the islands, there is a societal expectation pregnant for another type of tourism. It is then shown that the position of the government in terms of alternative tourism, which remains the order of discourse, encourages local actors to pursue their own projects. However, in terms of local development, the impact of these local initiatives, scattered and disjointed, are in fact very low. These observations lead to the presentation of a conceptual model for ecotourism island territories, which seeks both to clarify the definition of ecotourism is to open the discussion on recommendations for moving towards sustainability.
Corse
Martinique

Droits : info:eu-repo/semantics/openAccess
urn:doi:10.4000/etudescaribeennes.5303
http://journals.openedition.org/etudescaribeennes/5303

Éditeur(s) : HAL CCSD IWA Publishing
Résumé : International audience
The widely occurring degradation product aminomethylphosphonic acid (AMPA) is a result of glyphosate and amino-polyphosphonate degradation. Massive use of the parent compounds leads to the ubiquity of AMPA in the environment, and particularly in water. The purpose of this review is to summarize and discuss current insights into AMPA formation, transport, persistence and toxicity. In agricultural soils, AMPA is concentrated in the topsoil, and degrades slowly in most soils. It can reach shallow groundwater, but rarely managed to enter deep groundwater. AMPA is strongly adsorbed to soil particles and moves with the particles towards the stream in rainfall runoff. In urban areas, AMPA comes from phosphonates and glyphosate in wastewater. It is commonly found at the outlets of Wastewater Treatment Plants (WWTP). Sediments tend to accumulate AMPA, where it may be biodegraded. Airborne AMPA is not negligible, but does wash-out with heavy rainfall. AMPA is reported to be persistent and can be biologically degraded in soils and sediments. Limited photodegradation in waters exists. AMPA mainly has its sources in agricultural leachates, and urban wastewater effluents. The domestic contribution to urban loads is negligible. There is a critical lack of epidemiological data - especially on water exposure - to understand the toxicological effects, if any, of AMPA on humans. Fortunately, well operated water treatment plants remove a significant proportion of the AMPA from water, even though there are not sufficient regulatory limits for metabolites.
ISSN: 0043-1354

hal-01516026
https://hal-univ-rennes1.archives-ouvertes.fr/hal-01516026
https://hal-univ-rennes1.archives-ouvertes.fr/hal-01516026/document
https://hal-univ-rennes1.archives-ouvertes.fr/hal-01516026/file/Grandcoin%20et%20al.%20-%20AminoMethylPhosphonic%20acid%20%28AMPA%29%20in%20natural%20water.pdf
DOI : 10.1016/j.watres.2017.03.055

Éditeur(s) : HAL CCSD
Résumé : The Manche-à-Eau lagoon, brackish water ecosystem is subject to tide, trade winds and hurricanes. The 2004 map (IGN) is covered of a 90 m aside square, to place 37 spots in a GIS and to limit them on the field with a GPS. From aerial photos, the outlines drawing allows morphological follow up since 1950. Depth is measured at 1437 spots with bathymetric perch and prob. Stream direction is established during stream and ebb tide using ribbon fixed to the spot and a compass. Water volumes at low and high tide allow calculating the water renewal rate, at each tide. The mapping follow-up shows outlines and island stabilization because of the “shield effect” and soil (root peat), small islands aggregation/disaggregation depending of hurricanes passing. The present bathymetry shows the lagoon filling and the channels digging. General streams are subject to trade-winds (SSE-NNW) andthe tide movement to and fro. The up and down water generates a stream channel situated along the outlines and around dips and sandbanks. Water renewal volume (14.8 %) at each tide, combined with an active and various hydrodynamism tends to improve the water quality in this system.
Evolución Morfológica de la Laguna del Manglar Manche-à-EAU (Guadalupe, Antilles Francesas) de 1950 a 2004, y su batimetría eb 2007La laguna del Manche-à-Eau, ecosistema de agua salobre está sometido a la marea, a los alisios y a los huracanes. El mapa IGN de 2004 está dividido según una malla de 90 m para colocar 37 puntos en un SIG y limitarlos in situ con un GPS. Según las fotografías aéreas, el dibujo de los contornos hace posible el seguimiento morfológico desde 1950. La profundidad se mide en 1437 puntos con una pértiga y una sonda batimétrica. La orientación de las corrientes se establece en el mar y en el reflujo con catavientos fijados en los puntos, y una brújula. Las masas de agua entrantes y salientes permiten el cálculo del volumen de agua renovado durante cada marea. El seguimiento cartográfico muestra una estabilización de los contornos y de la isla debido al “efecto de escudo” y al suelo (turba de raíz), y una agregación/desagregación de los islotes según el paso de los huracanes. De acuerdo a la batimetría actual, se constatan el relleno de la laguna y la excavación de los canales. Las corrientes generales son controladas en superficie por los alisios, vientos de SSE-NNO y por el vaivén de la marea. Los movimientos ascendentes y descendentes de agua generan corrientes profundas a lo largo de los bordes y alrededor de depresiones y bajos. El volumen de agua renovado durante cada marea (14,8%) combinado al hidrodinamismo activo y variado tiende a vivificar este ecosistema.
La lagune de la Manche-à-Eau, écosystème d’eau saumâtre est soumis à la marée, aux alizés et aux ouragans. La carte IGN de 2004 est quadrillée selon une maille de 90 m pour placer 37 points dans un SIG et les borner sur le terrain avec un GPS. D’après les photographies aériennes, le dessin des contours rend possible le suivi morphologique depuis 1950. La profondeur est mesurée à 1437 points avec une perche et une sonde bathymétrique. L’orientation des courants est établie au flot et au jusant avec des penons fixés aux points, et une boussole. Les masses d’eau entrantes et sortantes permettent le calcul du volume d’eau renouvelé à chaque marée. Le suivi cartographique montre, une stabilisation des contours et de l’île due à « l’effet bouclier » et au sol (tourbe racinaire), et une agrégation/désagrégation des îlots selon le passage des ouragans. D’après la bathymétrie actuelle, le comblement de la lagune et le creusement des chenaux sont constatés. Les courants généraux sont gouvernés en surface par les alizés, vent de SSE-NNO et par le va-et-vient de la marée. Les descentes et remontées d’eau obligent ceux-ci à emprunter en profondeur les passages situés le long des berges et autour des dépressions et des hauts-fonds. Le volume d’eau renouvelé à chaque marée (14,8 %) combiné à l’hydrodynamisme actif et varié tend à vivifier cet écosystème.
Proceedings of the 61st Gulf and Caribbean fisheries institute
Le Gosier, Guadeloupe, France

hal-01600092
https://hal.archives-ouvertes.fr/hal-01600092
PRODINRA : 384819

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
This paper focuses on the analyses of the clastic sedimentary infill of the Coastal Plain of Eastern Mexico, which initiated synchronously with the Laramide orogeny in the vicinity of the Golden Lane. Results of these analyses are used as boundary conditions for calibrating/interpreting seismic profiles across more distal depocenters in the offshore of the Gulf of Mexico, from the sea shore and continental slope in the west to the abyssal plain in the east. The objective of the study is to better predict the reservoir distribution in the Deep offshore Basin of the Gulf of Mexico (DBGM), in order to explore for petroleum. The Coastal Plain is underlain by three morpho-tectonic domains: the tectonic front of the Sierra Madre Orientale (SMO), the Chicontepec deep water flexural basin, and the Tuxpan Platform (also known as the Golden Lane). Each domain is characterized by a distinct, dominantly siliciclastic Cenozoic lithostratigraphy. After a Jurassic rifting episode, followed by thermal subsidence, the oceanic basin and its western passive margin were deformed during the Upper Cretaceous and Paleogene, by far field stresses associated with the Cordilleran-Laramide Orogeny. Starting in the Late Cretaceous-Early Paleogene and during the Early Eocene, the tectonic load associated with the Laramide Orogen (Sierra Madre Oriental, SMO) caused flexural subsidence of the foreland located under the Coastal Plain. During this period, a massive transfer of siliciclastic sediments occurred from the Laramide foothills into the adjacent foreland. Sediments were eroded of the Sierra Madre tectonic wedge. Loading by these sediments pushed source units associated with the former passive margin down ward. The first syn-tectonic sediments of the Laramide orogeny were turbiditic silt layers in submarine fans which record also numerous collapse episodes and gravity slides. During the Late Eocene and Oligocene, the flexural subsidence stopped in the hinterland, whereas the subsidence of the passive margin resumed. This resulted in a change in the overall sedimentary architecture of the basin. Paleo-highs and reefs facies of the Golden Lane were flooded. Clastics by-passed the reefs and progradational clastic stratification formed as sediment moved towards the DBGM in the east. The final depositional environment of the continental platform/Coastal Plain became deltaic, marked by a succession of sand bars, levees and channels systems. From Miocene times onward, a system of gravitational listric faults developed near the platform to slope transition, resulting in a coeval compressional system at the transition between the slope and the abyssal plain. This system is driven by sediments charge. Because the sedimentation rate is larger than the subsidence, a large amount of clastics and slumped sediments are deposited in hangingwall basins.
ISSN: 0264-8172

hal-00424586
https://hal.archives-ouvertes.fr/hal-00424586
DOI : 10.1016/j.marpetgeo.2008.03.009

Éditeur(s) : HAL CCSD
Résumé : International audience
Debris avalanches derived from the flanks of volcanic islands are among the largest on Earth. Debris avalanches are rare, catastrophic destabilizations that still keep geologists debating about the mechanisms that initiate them and make them travel huge runout distances. To shed light on the trigger of such destabilizations, we studied the inland scar of a debris avalanche deposit cropping out at Piton des Neiges, a dormant and eroded basaltic volcano of La Réunion Island. The avalanche deposit rests on a pile of 50-70 sill intrusions with a shallow northward dip, i.e. toward the sea. We measured the anisotropy of magnetic susceptibility in a transect across the uppermost sill of the pile in contact with the avalanche deposit. This transect reveals a strongly asymmetric magnetic fabric, consistent with a north-directed shear movement of the upper intrusion wall. This suggests that the upper sill induced a co-intrusive shear displacement of the volcano flank toward the sea. The upper sill margin in contact with the avalanche is striated, showing that this intrusion is older than the avalanche. Striae indicate a northward direction of avalanche runout. The upper sill margin also displays a magmatic lineation consistent with a magma flow in the intrusion toward the north. There is thus a striking kinematic consistency between the directions of intrusion propagation and avalanche runout, both oriented toward the sea. From the above results, we propose that repeated sill intrusions, such as observed on Piton des Neiges, increase the instability of a volcanic edifice. Each injection induces an incremental slip of the overlying rock mass, which may eventually end up into a landslide. Sill intrusions associated with seaward displacements of volcano flank, such as inferred for the April 2007 eruption of Piton de la Fournaise (also in La Réunion), should therefore be considered as a potential trigger of debris avalanches.
Fall meeting
San Francisco, United States

hal-01387002
http://hal.univ-reunion.fr/hal-01387002