Éditeur(s) : HAL CCSD E Schweizerbart Science Publishers
Résumé : The occurrence and preservation of aragonite in eclogite-facies rocks of north-eastern Corsica is linked to an uncommon microtexture. Aragonite exclusively occurs as oriented fibres in garnet crystals of a graphitic, more or less siliceous marble that immediately overlies a serpentinite body of the meta-ophiolitic unit. The arrangement of the fibres is grossly radial, but more clearly sectoral in subhedral garnet, the fibres growing perpendicular to the garnet/matrix interface. Raman mapping reveals that the carbonate is calcite in the matrix and in poikiloblastic garnet cores, and that the fibres in the garnet mantle are aragonite alone in the case of a carbonate matrix, and both aragonite and quartz (in distinct fibres) in a quartz–carbonate matrix. These features are interpreted as prograde intergrowths, the result of garnet nucleation and growth in a calcite and then aragonite matrix (±quartz). Upon further heating and/or decompression, the aragonite matrix transformed back to calcite while the carbonates included in garnet retained their original structure, in spite of the relatively high temperature attained (ca. 500 °C). These aragonite relics are one more example of the preservation of a high-pressure polymorph through mechanical shielding of inclusions in a rigid host. The aragonite–garnet intergrowths are similar to quartz–garnet intergrowths described in amphibolite-facies graphitic schists. They are evidence that oriented inclusions in garnet are not necessarily precipitates (‘exsolutions'). Unlike precipitates, their orientation is controlled more by the shape of the garnet growth front than by symmetry constraints.
ISSN: 0935-1221

hal-00411136
https://hal.archives-ouvertes.fr/hal-00411136
DOI : 10.1127/0935-1221/2008/0020-1892

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
In this paper, we propose a benchmarking of supervised machine learning techniques (neural networks, Gaussian processes and support vector machines) in order to forecast the Global Horizontal solar Irradiance (GHI). We also include in this benchmark a simple linear autoregressive (AR) model as well as two naive models based on persistence of the GHI and persistence of the clear sky index (denoted herein scaled persistence model). The models are calibrated and validated with data from three French islands: Corsica (41.91°N; 8.73°E), Guadeloupe (16.26°N; 61.51°W) and Reunion (21.34°S ; 55.49°E). The main findings of this work are, that for hour ahead solar forecasting, the machine learning techniques slightly improve the performances exhibited by the linear AR and the scaled persistence model. However, the improvement appears to be more pronounced in case of unstable sky conditions. These nonlinear techniques start to outperform their simple counterparts for forecasting horizons greater than one hour.
ISSN: 0038-092X

Droits : info:eu-repo/semantics/OpenAccess
hal-01101564
https://hal.archives-ouvertes.fr/hal-01101564
https://hal.archives-ouvertes.fr/hal-01101564/document
https://hal.archives-ouvertes.fr/hal-01101564/file/Manuscript_Lauretetal_Rev_unmarked.pdf
DOI : 10.1016/j.solener.2014.12.014

Éditeur(s) : HAL CCSD Université des Antilles
Résumé : International audience
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 des 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.
ISSN: 1779-0980

hal-00830509
https://hal.archives-ouvertes.fr/hal-00830509
https://hal.archives-ouvertes.fr/hal-00830509/document
https://hal.archives-ouvertes.fr/hal-00830509/file/Eco-tourisme-un-modele-de-tourisme-alternatif-pour-les-territoires-insulaires-touristiques-francais-discussion-a-partir-d-experiences-croisees-corse-martinique.pdf
DOI : 10.4000/etudescaribeennes.5303

Éditeur(s) : HAL CCSD Société géologique de France
Résumé : In the western Mediterranean Sea, the Liguro-Provençal Basin (LPB) is a key area for studying passive margins because of its recent formation and abundance of onshore and offshore data. The Nerthe area located in the northern margin of LPB provides the unique continuous Oligo-Miocene deposits contemporaneous of the transition rifting to drifting. However, the age of the deposits remains debated and the link between outcrops and offshore seismic data is poorly constrained. The purpose of this paper is double. First, we intend to propose a new chronostratigraphic frame based on bio- (planktonic foraminifera, calcareous nannofossils) and magneto-stratigraphy. Second, we aim to make, through the integration of new highly time-resolved seismic data and field works, a coherent onshore-offshore link concretized by a 3D geological model. The new temporal and spatial data presented in this paper allow correlating the Oligo-Miocene sequences, defining their geometry and specifying precisely the timing of syn- and post-rift stages. The first marine transgression is now precisely dated latest Chattian within the syn-rift deposits and appears to be synchronous with the first marine deposits in the offshore wells and other marginal basins. The transition from syn-rift to post-rift appears to last 3.3 Ma at maximum, between 21.8 and 18.5 Ma (late Aquitanian to early Burdigalian). It is underlined by two major erosional unconformities bearing a hiatus of around 1 Ma. The post-rift started with a major marine transgression that is now dated from middle Burdigalian, at around 18.5 Ma, as elsewhere in the LPB. Contrarily to recent proposals, the post-rift deposits are widely represented on the northeastern margin of the "Golfe du Lion". There, the subsidence of the margin was low during the syn-rift and the transitional periods and high during the post-rift. The onset of this high post-rift subsidence appears to be synchronous with the slowdown of the Corsica-Sardinia block (CSb) motion.
EISSN: 1777-5817

hal-00558497
https://hal.archives-ouvertes.fr/hal-00558497
DOI : 10.2113/gssgfbull.181.6.591

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
The analysis of field relationships between allochthonous crystalline slivers, ultramafic units and associated sedimentary cover in the high-pressure Schistes Lustrés units of northern Corsica allows reconstruction of the pre-orogenic architecture of a fossil Mesozoic Ocean-Continent Transition (OCT) of the Tethys basin. The studied area, encompassing the Serra di Pigno and Col de Téghime areas (Cap Corse) is composed of an assemblage of prealpine basement sheets made up of serpentinized mantle rocks, Permian gabbros and gneisses, locally associated with Paleozoic metabasites and micaschists. The sedimentary cover includes numerous intervals of calc-schists, marbles, quartzites, micaschists and dolomitic metabreccias yielding a great variety of lithostratigraphical successions. The metasedimentary sequences do not show affinities with the typical cover series of the Prépiémontais margin domains. This implies an origin from a more internal domain (oceanward) for the studied units. In addition, the sedimentary cover of the ultramafic basement units do not display the characters of the classical Alpine ophiolites but bear lithological features showing affinities with both continental and oceanic environments. We assume that the high variability of the sedimentary successions as well as the presence of a basement composed of continental and upper-mantle rocks is consistent with an origin at an OCT. The acidic basement slivers are regarded as former extensional allochthons of continental crust abandoned during breakup on a newly exhumed seafloor of peridotite composition. Such extensional allochthons, will then logically constitute the most internal continental slices buried at great depth during Alpine subduction. This work shows that a lot has to be expected from a revision of the Schistes Lustrés lithostratigraphy in the light of the new concepts of the evolution of the OCT domains.
ISSN: 0040-1951

hal-00795578
https://hal.archives-ouvertes.fr/hal-00795578
DOI : 10.1016/j.tecto.2012.06.013

Éditeur(s) : HAL CCSD Museum National d'Histoire Naturelle Paris
Résumé : Au Burdigalien supérieur, des récifs coralliens se sont développés dans la Formation de Cala di Labra, aux alentours de Bonifacio (Corse-du-Sud, France). Ils sont organisés en trois épisodes successifs R1, R2 et R3. La faune corallienne comprenant 16 espèces récifales, est décrite pour la première fois. Deux associations coralliennes sont distinguées. Les principaux genres constructeurs sont Porites Link, 1807, Tarbellastraea Alloiteau, 1950 et Thegioastraea Sismonda, 1871. La diversité corallienne est maximale avec 15 espèces (8 genres) dans l'épisode R1, puis réduite (4 espèces appartenant à 3 genres) pour l'épisode R2, l'épisode R3 renfermant des coraux mal préservés pour être identifiés. Les formes de croissance sont en grande majorité massives étalées et superposées, associées à des conditions paléoenvironnementales de haute à moyenne énergie (rides de courant, bioclastes usés, peu de formes branchues), sous apports terrigènes réguliers. Les récifs, pour la plupart frangeants et à zonation récifale discrète, se sont développés en domaine de plate-forme peu profonde. Cette étude reprend également toutes les citations d'espèces dans la littérature pour cette région et replace ces épisodes coralliens remarquables dans l'évolution plus générale du Bassin Liguro-Provençal.
ISSN: 1280-9659

hal-01236095
https://hal.archives-ouvertes.fr/hal-01236095
DOI : 10.5252/g2015n3a5

Éditeur(s) : HAL CCSD Wiley-Blackwell
Résumé : International audience
In Alpine Corsica (France), deeply subducted metabasalts are well preserved as lawsonite-bearing eclogite (Law-Ecl), occurrence of which is restricted to similar to 10 localities worldwide. The Corsican Law-Ecl, consisting of omphacite + lawsonite + garnet + phengite + titanite, occurs as both single undeformed metabasaltic pillows surrounded by lawsonite blueschist (Law-Bs), and carbonate-bearing eclogitic veins. Law-Bs are found as variably deformed metabasaltic pillows locally cross-cut by eclogitic veins and consist of glaucophane + actinolite + lawsonite + garnet + phengite + titanite. Field evidence and microstructures reveal that both Law-Ecl and Law-Bs are stable at the metamorphic peak in the lawsonite-eclogite stability field. Isochemical phase diagrams (pseudosections) calculated for representative Law-Ecl and Law-Bs samples indicate that both lithologies equilibrated at the same conditions of similar to 520 +/- 20 degrees C and 2.3 +/- 0.1 GPa. Therefore, the coexistence at the same peak metamorphic conditions of Law-Ecl and Law-Bs implies that different portions of deeply subducted oceanic crust may store significantly different H2O contents, depending on bulk-rock chemical composition. In addition, thermodynamic modelling of phase equilibria indicates that the occurring progressive dehydration reactions, which are significantly depending on bulk-rock chemical composition, strongly influence rock densification and eclogite formation in subducting slabs.
ISSN: 0263-4929

hal-00617768
https://hal.archives-ouvertes.fr/hal-00617768
DOI : 10.1111/j.1525-1314.2011.00931.x

Éditeur(s) : ISTPM
Résumé : Investigations carried out in both Corsica lagoons Diana and Urbino during the period from January to August 1985, permitted to define the main characteristics of microplankton cycle. Two phytoplanktonic blooms have been observed, first in winter, second less important in July-August. Any correlation cannot be observed between phytoplanktonic cycle or one its main components, and both environmental variables temperature and salinity. However dissolved oxygen ratio may be subject to large summer variations, drifting towards until ecological desequilibrious.
Les investigations menées dans les étangs corses de Diana et Urbino pour la période de janvier à août 1985, ont permis de définir les principales caractéristiques du cycle microplanctonique. Deux efflorescences phytoplanctoniques ont été observées, la première en hiver avec Skeletonema costatum, Nitzschia delicatissima, Prorocentrum micans, Scrippsiella trochoidea et entre 13,2.106 et 28,7.106 cellules par dm3, la seconde moins importante en juillet-août : 5,3.10e à 10,7.106 cellules par dm3 avec comme espèces principales à Diana Leptocylindrus danicus, L. minimus, diverses dinophycées, et à Urbino Chaetoceros diuersus et Nitzschia sp. Aucune corrélation nette n'a pu être dégagée entre le cycle phytoplanctonique ou l'un de ses principaux composants et les deux variables de l'environnement température et salinité. Toutefois dans ces milieux relativement confinés, le taux d'oxygène dissous peut être sujet à de grandes variations estivales, pouvant aller jusqu'au déséquilibre écologique. Par ailleurs l'évolution des valeurs de l'indice de diversité spécifique de Gieason et surtout l'analyse des valeurs de l'indice de similitude de Sorensen confirment les observations antérieures relatives au particularisme des deux étangs.
Revue des Travaux de l'Institut des Pêches Maritimes (0035-2276) (ISTPM), 1984-06 , Vol. 48 , N. 3-4 , P. 161-175

Droits : Ifremer
http://archimer.ifremer.fr/doc/1984/publication-1800.pdf
http://archimer.ifremer.fr/doc/00000/1800/

Éditeur(s) : Elsevier
Résumé : Foraminifera and ostracods have been quantitatively studied in core MD01-2472, from the upper continental slope (at water depth of 501 m), to evaluate their relationship with bottom water condition variability and decipher the control of the Levantine Intermediate Water (LIW) current on benthic faunas. The occurrence of reworked ostracod species (originating from the continental shelf) and, the presence of shallow water Elphidium/Ammonia benthic foraminifera are used to estimate the degree of along-slope transport at the core site. This has revealed two intervals of along-slope transport also associated with coarse-grained contourite deposits, deposited during the YD and HS2 episodes. Planktonic-benthic foraminiferal and ostracod assemblages reflect climate oscillations. Peaks of the polar planktonic Neogloboquadrina pachyderma (left-coiling S) may be used to identify Heinrich Events. Interstadials are marked by abundant ostracod species such as Paracypris sp., Argilloecia acuminata, and Cytheropteron alatum and the presence of benthic foraminifera like Bulimina marginata, Bulimina costata and Gyroidina altiformis. The B–A and Holocene are characterized by abundant warm water species of planktonic foraminifera and by the ostracod species Polycope sp. We hypothesize that there is relationship between LIW intensification during cold rapid climate events and benthic fauna assemblage variations due to changes in: 1) bottom water ventilation; and 2) the export of nutrients and/or sediment particles by bottom currents.
Quaternary International (1040-6182) (Elsevier), 2015-01 , Vol. 357 , P. 295-313

Droits : 2014 Elsevier Ltd and INQUA. All rights reserved.
http://archimer.ifremer.fr/doc/00245/35648/34208.pdf
DOI:10.1016/j.quaint.2014.11.038
http://archimer.ifremer.fr/doc/00245/35648/

Éditeur(s) : Université des Antilles Études caribéennes
Résumé : Certaines villes corses comme Bastia, Bonifacio, Calvi ou Corte possèdent des centres anciens enchâssés dans des ouvrages d’art militaire, aux fonctions défensives à l’origine : les citadelles. Cet article invite à interroger le patrimoine des citadelles urbaines insulaires, non pas en lui-même, mais en tant qu’objet de construction sociale et symbolique pris dans des processus de patrimonialisation qui engagent diverses logiques d’actions et modalités d’interventions, différents acteurs et usages. C’est donc cette pluralité instable des usages et des représentations du patrimonial qui a été privilégiée pour appréhender les enjeux sociaux, culturels, politiques et symboliques liés localement à ces processus. Cette communication s’appuie en particulier d’éléments extraits d’une enquête de terrain réalisée à Calvi, dans la microrégion de Balagne située dans l’ouest de la Corse.
Some Corsican cities like Bastia, Bonifacio, Calvi or Corte have old centers enshrined in military engineering works build originally for defensive functions: the citadels. This article invited to question the patrimony of insular urban citadels not for itself, but like the object of social and symbolic system, taken in patrimonialization process who engaged various logics of actions and conditions of operations, many actors and uses. So, it’s this unstable pluralism of patrimonial uses and representations that had been prioritized to grasp the social, cultural, politic and symbolic stakes bounded locally at these processes. This paper is based on field’s works realized in Calvi, in Balagna area, located in west Corsica.
Corse

Droits : info:eu-repo/semantics/openAccess
urn:doi:10.4000/etudescaribeennes.6714
http://journals.openedition.org/etudescaribeennes/6714

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 Elsevier
Résumé : International audience
The chronostratigraphy of the lower Miocene deposits of northwestern Sardinia is refined in the Castelsardo Basin. The combination of new 40Ar/39Ar isotopic datings, 19 micropalaeontological datings (calcareous nannofossils, planktonic and large benthic foraminifers) and 16 palaeomagnetic polarity measurements led to a new chronostratigraphic framework. The continental deposits of the first megasequence (Valledoria and Casteldoria members) are possibly Aquitanian. The overlying marine sediments are early Burdigalian (Vaginella depressa Molasse). The marine transgression can be dated to around 19.7 Ma. Marine conditions ceased 18.83 ± 0.13 Ma, the age of the index aerial τ2 ignimbrite. The continental part of the second megasequence (“Lacustre” unit) is early–middle Burdigalian, between 18.8 and 18 Ma. The overlying marine part (Campulandu and Sedini members) is middle–late Burdigalian. The second marine transgression began in the earliest–late Burdigalian, during the Chron C5Dr reversal, at the time of the eustatic Bur 4 event. The Castelsardo basin went through two main extensional tectonic episodes. The first one occurred as the Valledoria Member was deposited and possibly dates back to the Aquitanian. The second one occurred as the uppermost part of the Vaginella depressa Molasse was deposited during the early Burdigalian. The second extensional episode is related to a rapid rotation of Sardinia. Palaeomagnetic results confirm that Corsica and Sardinia acted as a single block which suffered a 28 ± 17° ccw rotation after 19.2 Ma. The Castelsardo basin is held to be an Aquitanian–early Burdigalian intra-arc rift basin that later evolved in a thermally controlled subsident margin of the Ligurian-Provençal Basin during the middle–late Burdigalian.
ISSN: 0031-0182

hal-00498288
https://hal.archives-ouvertes.fr/hal-00498288
DOI : 10.1016/j.palaeo.2010.06.007

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
Diamond-bearing UHP metamorphic rocks witness for subduction of lithospheric slabs into the mantle and their return to shallow levels. In this study we present U–Pb and trace elements analyses of zircon and rutile inclusions from a diamond-bearing garnet megacryst collected in a mélange unit exposed on the northern margin of Africa (Edough Massif, NE Algeria). Large rutile crystals (up to 300 μm in size) analyzed in situ provide a U–Pb age of interpreted as dating the prograde to peak subduction stage of the mafic protolith. Trace element analyses of minute zircons (≤30 μm) indicate that they formed in equilibrium with the garnet megacryst at a temperature of 740–810 °C, most likely during HP retrograde metamorphism. U–Pb analyses provide a significantly younger age of attributed to exhumation of the UHP units. This study allows bracketing the age of UHP metamorphism in the Western Mediterranean Orogen to the Oligocene/early Miocene, thus unambiguously relating UHP metamorphism to the Alpine history. Exhumation of these UHP units is coeval with the counterclockwise rotation of the Corsica–Sardinia block and most likely resulted from subduction rollback that was driven by slab pull.
ISSN: 0012-821X

hal-01622789
https://hal.archives-ouvertes.fr/hal-01622789
DOI : 10.1016/j.epsl.2017.06.043

Éditeur(s) : HAL CCSD Elsevier
Résumé : Upper mantle flow beneath the French Massif Central is investigated using teleseismic shear wave splitting induced by seismic anisotropy. About 25 three component stations (short period, intermediate and broad-band) were installed during the period 1998-1999 in the southern Massif Central, from the Clermont Ferrand volcanic area to the Mediterranean sea. Teleseismic shear waves (SKS, SKKS and PKS) were used to determine the splitting parameters: the fast polarization direction and the delay time. Delay times ranging between 0.7 and 1.5 s have been observed at most of the sites. The azimuths of the fast split shear waves trend homogeneously NW-SE in the southern Massif Central suggesting a homogeneous mantle flow beneath this area. The observed NW-SE direction differs from the N100°E Pyrenean anisotropy further South. It does not appear to be correlated to Hercynian structures nor to the present-day motion of the plate but is well correlated to the Tertiary extension direction. We propose that the opening of the western Mediterranean induced by the rotation of the Corsica-Sardinia lithospheric bloc and the roll-back to the SE of the Tethys slab may have generated a large asthenospheric mantle flow beneath the southern Massif Central and a deflection of the up going plume centered beneath the northern Massif Central toward the SE.
ISSN: 0012-821X

insu-00150214
https://hal-insu.archives-ouvertes.fr/insu-00150214
https://hal-insu.archives-ouvertes.fr/insu-00150214/document
https://hal-insu.archives-ouvertes.fr/insu-00150214/file/Barruol_Granet_EPSL2002_hal.pdf
DOI : 10.1016/S0012-821X(02)00752-5

Éditeur(s) : HAL CCSD Wiley-Blackwell
Résumé : International audience
Although lawsonite-bearing rocks are rare in exhumed high-pressure (HP) terranes, they are considered to exert a primary role in subduction dynamics. Recent observations in natural settings have shown that fluid–rock interaction at HP conditions, including metasomatism, may lead to unusually high lawsonite amounts even in rocks that originally contained little or no lawsonite. This process may therefore bear important implications for element recycling in subduction zones. A detailed characterization of the geochemical fingerprints associated with lawsonite metasomatism is presented in this contribution. The studied rocks belong to the HP terranes of Alpine Corsica (France), which is the largest documented exposure for lawsonite metasomatism. Metasomatic lawsonite displays complex compositional zoning, including high trace element, Cr and Ti content. The trace element content is much higher compared with the average of non-metasomatic lawsonite, and is in line with the re-incorporation of large amounts of trace elements (e.g. REE, Sr, Pb, Th) in the rock during metasomatism, as shown by mass transfer calculations. Our data suggest that serpentinites represented the main fluid source for the metasomatism, with concurrent contribution of other, possibly Ca-rich lithologies, such as mafic or meta-sedimentary rocks. We propose that the breakdown of metasomatic lawsonite may contribute to the genesis of magmas and their characteristic geochemical signatures.
ISSN: 0263-4929

hal-01107395
https://hal.archives-ouvertes.fr/hal-01107395
DOI : 10.1111/jmg.12074

Éditeur(s) : Université des Antilles Études caribéennes
Résumé : Les auteurs interrogent les systèmes d’indicateurs destinés à évaluer les impacts économiques, écologiques et sociaux du tourisme sur la destination. Le questionnement porte sur la capacité des systèmes d’indicateurs actuels à prendre en compte l’impact du tourisme sur la vie des populations résidentes des destinations insulaires où l’emprise touristique est importante. Au-delà des considérations économiques et écologiques, il s’agit de prendre la mesure de l’impact touristique sur la qualité de vie des résidents (QVR). S’appuyant sur l’expérience de la Corse, il apparaît évident que les indicateurs doivent prendre en compte les dimensions de l’espace, des temporalités et des ressources.
The authors question indicators systems to assess economic, ecological and social of tourism impacts on destination. Questioning focuses on the ability of existing indicator systems which can take into account the impact of tourism in the life of island resident. Beyond economic and ecological considerations, it must ponder tourism impacts on the quality of residents’ life. Relying on the Corsica experience, it is clear that indicators should take into account space, temporalities and resources dimensions.
Corse

Droits : info:eu-repo/semantics/openAccess
urn:doi:10.4000/etudescaribeennes.6277
http://journals.openedition.org/etudescaribeennes/6277

Éditeur(s) : Université des Antilles Études caribéennes
Résumé : Tandis que l’agriculture et le tourisme sont en concurrence pour l’accès au foncier, comment penser, soutenir et promouvoir les complémentarités entre ces deux activités pour développer un tourisme rural intégré socialement, économiquement et spatialement ? Cette question trouve un écho particulier dans les territoires insulaires où les enjeux pour les communautés locales sont d’autant plus cruciaux que les conflits sont aigus. Compte tenu de ce contexte problématique, cet article propose une grille d’indicateurs évaluant les complémentarités entre les deux activités. Outil d’accompagnement du développement durable, cette grille est mise à l’épreuve du territoire de Balagne en Corse : les résultats de l’expérimentation conduite sur cette île méditerranéenne en 2010 conduisent à discuter la portée des indicateurs sélectionnés.
On coastal areas and in islands in particular, the tourism sustainability is still at stake: whereas agriculture and tourism are competing for land, how can we think and promote the complementarities between both activities for a sustainable territorial development? This paper deals with this question. For instance, a grid of indicators for the complementarities between farming systems and tourism is set as a tool for local development. The results of a survey lead in the Mediterranean island of Corsica in 2010 are used to discuss the scope of such a grid.
Corse

Droits : info:eu-repo/semantics/openAccess
urn:doi:10.4000/etudescaribeennes.6249
http://journals.openedition.org/etudescaribeennes/6249

Éditeur(s) : Inter-research
Résumé : Marine protected areas (MPAs) have the potential to enhance the long-term sustainability of coastal resources, and the artisanal fisheries which depend on them. However, recreational fisheries, which are increasing their impacts on coastal resources worldwide, may reduce the benefits that MPAs provide to declining artisanal fisheries. Here we used the Bonifacio Straits Natural Reserve (BSNR) Corsica as a study case to simulate the combined effects on coastal resources of artisanal and recreational fishing efforts. The BSNR ecosystem was modelled using mass-balance modelling of trophic interactions. This model was compared to another built on a non-protected area from the same region. We aggregated fishing fleets into artisanal and recreational categories, and we simulated various combinations of fishing effort over a 20 yr dynamic simulation using Ecosim. We showed that fishing activities have an additional top-down effect on the food web and that they decrease the targeted group's biomass, such as piscivorous species. We found, for some trophic groups, non-trivial patterns of biomass variation through trophic cascades. Our trophic approach revealed that some groups may suffer a biomass decrease when MPAs are set or enforced, due to the combined effect of artisanal and recreational fisheries. Overall, our results illustrate the value of modelling to manage MPAs, as a complementary tool to surveys. Models provide the opportunity to anticipate the potential consequences, at the ecosystem level, of socio-political decisions that aim to sustain coastal resources while managing artisanal and recreational fisheries.
Marine Ecology-progress Series (0171-8630) (Inter-research), 2010-08 , Vol. 412 , P. 207-221

Droits : Inter-Research 2010
http://archimer.ifremer.fr/doc/00013/12436/9246.pdf
http://archimer.ifremer.fr/doc/00013/12436/9247.pdf
DOI:10.3354/meps08679
http://archimer.ifremer.fr/doc/00013/12436/

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
In this paper, we propose a benchmarking of supervised machine learning techniques (neural networks, Gaussian processes and support vector machines) in order to forecast the Global Horizontal solar Irradiance (GHI). We also include in this benchmark a simple linear autoregressive (AR) model as well as two naive models based on persistence of the GHI and persistence of the clear sky index (denoted herein scaled persistence model). The models are calibrated and validatedwith data from three French islands: Corsica (41.91°N; 8.73°E), Guadeloupe (16.26°N; 61.51°W) and Reunion (21.34°S ; 55.49°E). The main findings of this work are, that for hour ahead solar forecasting,the machine learning techniques slightly improve the performances exhibited by the linear AR and the scaled persistence model. However, the improvement appears to be more pronounced in case of unstable sky conditions.These nonlinear techniques start to outperform their simple counterparts for forecasting horizons greater than one hour.
ISSN: 0038-092X

Droits : info:eu-repo/semantics/OpenAccess
hal-01099211
https://hal.archives-ouvertes.fr/hal-01099211
https://hal.archives-ouvertes.fr/hal-01099211/document
https://hal.archives-ouvertes.fr/hal-01099211/file/Manuscript_Lauretetal_Rev_unmarked.pdf