Éditeur(s) : CARDI : Caribbean Agricultural Rechearch and Development Institute Université des Antilles. Service commun de la documentation
Extrait de : 52e congrès annuel de la Société caribéenne des plantes alimentaires / 52nd annual meeting of the Caribbean food crops society (CFCS), du 10 au 16 juillet 2016. INRA, CFCS
Description : Banana and plantain (Musa spp) are important foreign exchange earners in Guyana and the Windward Islands of the Caribbean. Black Sigatoka Disease (BSD) also referred to as black leaf streak disease is one of the most destructive diseases of banana and plantain and is present within the region. In Guyana within two years following its introduction in 2008, the industry was totally decimated, recording a 100% decline, turning the country to a net banana importer. Also, from 2009 ? 2012 the disease spread in the Windward Islands causing as much as 100% decrease in the export of banana. The disease is caused by the ascomycete fungus, Mycosphaerella fijiensis (anamorph Pseudocercospora fijiensis) and is aggressive, challenging to control and results in enormous crop damage if left uncontrolled. In an effort to develop an integrated management approach to the disease the Caribbean Agricultural Research and Development Institute (CARDI) with financial assistance from the Caribbean Development Bank (CDB) is evaluating five FHIA banana and plantain accessions and eight IITA plantain accessions for tolerance to BSD. The evaluation is presently conducted in four Caribbean countries, Dominica, Guyana, St Lucia and St Vincent and the Grenadines. In each country, four distinct agro- ecological zones were selected for the trial evaluation blocks and using a randomized block design, four blocks were established in each country. Five FHIA accessions: FHIA-01, FHIA-03, FHIA-18, FHIA-21 and FHIA-23 are being evaluated in Dominica, St Lucia and St Vincent and the Grenadines whereas, plantain accessions: PITA-17, PITA-21, PITA-22, PITA-23, PITA-24 and PITA-26 are to be evaluated in Guyana for tolerance to the disease. Cavendish are used as regional controls and as borders rows to increase disease pressure. The disease parameters evaluated are youngest leaf spotted (YLS), disease development time (DDT), leaf emission rate (LER), disease severity at 6 months, bunch emergence and harvest, and index of standing leaves. Agronomic data; days from planting to flowering, bunch weight, number of hands in bunch, average weight of hands and average number of fingers per hand and bunch, as well as organoleptic characteristics of both cooked and ripe fruits are also evaluated. The early data collection, of the FHIA only accessions, show trends in the disease tolerance and agronomic performance as well as their adaptability in the different agro-ecological zone. The trends indicate better disease tolerance of FHIA varieties with higher leaf counts before, at bunching and at harvest. The organoleptic test shows a preference to FHIA 03 and FHIA 21. La banane et le plantain (espèces de Musa) sont les acquéreurs de devises étrangères importants en Guyane et en Îles du Vent des Caraïbe. La maladie noire de Sigatoka (schéma) également désignée sous le nom de la maladie noire de filet de feuille est l'une des maladies les plus destructives de la banane et du plantain et est présente dans la région. En Guyane dans un délai de deux ans après son introduction en 2008, l'industrie a été totalement décimée, enregistrant une baisse de 100%, tournant le pays à un importateur net de banane. En outre, à partir de 2009-2012 la propagation de maladie en Îles du Vent causant pas moins de la diminution de 100% de l'exportation de la banane. La maladie est provoquée par le champignon d'ascomycète, fijiensis de Mycosphaerella (fijiensis anamorph de Pseudocercospora) et est agressive, contestant pour commander et les résultats dans l'énorme culture endommagent si laissé incontrôlé. Dans un effort de développer une approche intégrée de gestion à la maladie l'institut agricole des Caraïbes de recherche et développement (CARDI) avec l'aide financière de la banque de développement des Caraïbes (BDC) évalue des adhésions de banane et de plantain de cinq FHIA et huit adhésions de plantain d'IITA pour la tolérance au schéma. L'évaluation est actuellement effectuée quatre pays des Caraïbes, Dominique, Guyane, St Lucia et Saint-Vincent-et-les Grenadines. Dans chaque pays, quatre agro zones écologiques distinctes ont été sélectionnées pour les blocs d'essai d'évaluation et employant une conception de bloc randomisé, quatre blocs ont été établis dans chaque pays. Cinq adhésions de FHIA : FHIA-01, FHIA-03, FHIA-18, FHIA-21 et FHIA-23 sont évalués en Dominique, au St Lucia et au Saint-Vincent-et-les Grenadines tandis que, des adhésions de plantain : PITA-17, PITA-21, PITA-22, PITA-23, PITA-24 et PITA-26 doivent être évalués en Guyane pour la tolérance à la maladie. Cavendish sont employés en tant que contrôles régionaux et comme rangées de frontières pour augmenter la pression de la maladie. Les paramètres de la maladie évalués sont la plus jeune feuille repérée (YLS), le temps d'élaboration de la maladie (DDT), le taux d'émission de feuille (LER), la sévérité de la maladie à 6 mois, émergences et récoltes de groupe, et index des feuilles debout. Données agronomiques ; des jours de la plantation à la floraison, du poids de groupe, nombre de mains dans le poids de groupe et moyen des mains et du nombre moyen de doigts par main et groupe, aussi bien que les caractéristiques organoleptiques des fruits cuits et mûrs sont également évalués. La collecte de données tôt, des adhésions de FHIA seulement, exposition tend dans la tolérance de maladie et la représentation agronomique aussi bien que leur adaptabilité dans la zone agro-écologique différente. Les tendances indiquent qu'une meilleure tolérance de maladie des variétés de FHIA avec une plus haute feuille compte avant, à se rassembler et à la récolte. L'essai organoleptique montre une préférence à FHIA 03 et à FHIA 21.
Siècle(s) traité(s) : 21
Droits : CC-BY-NC-ND - Attribution - Pas d'utilisation commerciale - Pas de modification
Permalien : http://www.manioc.org/fichiers/V16266
V16266

Éditeur(s) : Université des Antilles AREBio Groupe de recherche BIOSPHERES : BIOlogie, Sciences Physiques & Humaines pour les énergies Renouvelables, l
Extrait de : 1er colloque international BIOSPHERES, du 18 au 20 juin 2019. Université des Antilles
Description : Drosophila often offers many advantages as an experimental organism. The dead ringer (dri) gene of drosophila melanogaster is a member of the recently discovered ARID-box family of eukaryotic genes that encodes proteins with a conserved DNA-binding domain. dri itself is highly well conserved with specific orthologs from human to yeast genomes. This family include ARID3A, 3B and 3C with have role in embryonic pattening, cell lineage gene regulation, cell cycle control, transcriptional regulation and chromatin structure modification. We first showed that the gene encoding ARID3A also known as Bright (B cell regulator of immunoglobulin heavy chain transcription) play critical roles in B-cell development and SATB1 in T-cell transcription regulation. In this international workshops we will expose a comprehensive understanding of these molecules and better knowledge of their specific targets and function-interactions in controlling cell fate decisions and development. In addition, dri have homology with the Aedes aegypti mosquitoes which had ability to carry and spread disease to human. More than half of the world?s population live in areas where this mosquito species is present, including Martinique. Sustained mosquito control efforts are important to prevent outbreaks from Dengue, Chikungunya, malaria, zika diseases. Discovering the functions of AT-rich genes in preventing illness from mosquito is the central goal for raising working progress hypothesis.

Droits : CC-BY-NC-ND - Attribution - Pas d'utilisation commerciale - Pas de modification
Permalien : http://www.manioc.org/fichiers/V19077
V19077

Résumé : The slides were taken on collecting trips sponsored by the William L. Bryant Foundation, where books, music and art indigenous to the regions were gathered. The are organized by geographical location.
Devon House was built in 1881 by Jamaica’s first black millionaire George Stiebel. The land was first assigned to Reverend John Zellers by King George II in May 1667 to aid in the Anglican Church’s efforts to spread Christianity on the island. The house’s architectural style is a mix of Jamaican and English Georgian style architecture and is located at the corner of Trafalgar Road and Hope Road, in what later became known as Millionaire’s corner. In 1967, the house was purchased by the Jamaica National Heritage Trust and was later declared a national monument in 1990 after winning the American Express Historic Preservation Award. Devon House is a Jamaica Heritage Site owned by the Jamaican government. Slide labeled Jam. in Kingston Devon House.
Jamaica -- Caribbean region -- Saint Andrew

Droits : All rights to images are held by the respective holding institution. This image is posted publicly for non-profit educational uses, excluding printed publication. For permission to reproduce images and/or for copyright information contact Special Collections & University Archives, University of Central Florida Libraries, Orlando, FL 32816 phone (407) 823-2576, email: speccoll@mail.ucf.edu
CFM1972_01a
Sheet 58:15
http://ufdc.ufl.edu/AA00030138/00001

Éditeur(s) : Gauthier-villars
Résumé : Seismic, Seabeam, magnetic and gravimetrie surveys in the southern part of the N-Fiji basin were conducted during the SEAPSO LEG III Cruise. The active spreading axis was recognized between 17°30'S and 21°S. It consists of a continuous N-S Ridge cross-cut by transverse directions oriented N25 and N45. North of 17°30'S, the spreading System is more complex due to the existence of a possible triple junction located around 15° S. The eastern part of the N-Fiji basin, west of Viti Levu is mostly characterized by alternating highs and deeps (<4,000 m). This area must be regarded no more as a spreading center, but as complex boundary suffering transverse tectonics.
La mission SEAPSO III a permis de localiser une zone d'accrétion active, d'orientation méridienne et pratiquement continue entre 17°30'S et 21° S. Des accidents transverses, qui encadrent ou recoupent cette dorsale, s'orientent autour de deux directions principales N25 et N45. Au Nord de 17 30'S le système d'accrétion, beaucoup plus complexe, annonce la triple jonction reconnue aux alentours de 15" S. La partie orientale du bassin Nord-Fidjien (à l'Ouest de l'île de Viti Levu) est caractérisée par l'alternance de zones hautes et de dépressions dont certaines dépassent 4000 m de profondeur. Il s'agit d'une zone complexe de déformations liées à des accidents cisaillants transverses.
Comptes Rendus de l'Academie des Sciences Serie II (1251-8069) (Gauthier-villars), 1986-06 , Vol. 303 , N. 1 , P. 93-98

Droits : Académie des Sciences
http://archimer.ifremer.fr/doc/00184/29492/27835.pdf
http://archimer.ifremer.fr/doc/00184/29492/

Résumé : The slides were taken on collecting trips sponsored by the William L. Bryant Foundation, where books, music and art indigenous to the regions were gathered. The are organized by geographical location.
In Trinidad and Tobago, cocoa production is monitored by the Cocoa and Coffee Industry Board, which was established in 1961. Cocoa, used to make chocolate, is a traditional export crop in the country. Buildings like those pictured would be used for processing, drying, sorting, and storing cocoa beans. In this image, several children and adults can be found in the yard near buildings on the cocoa plantation. The buildings are made with wood and have zinc paneled roofs, some of the steps are made of concrete. The level flat area between the buildings on the far right would be used to dry cocoa beans. The beans would be spread out evenly on this area, then raked and turned so that beans were exposed to the sun for adequate drying. Slide labeled Cocoa Plantation Trinidad.
Trinidad and Tobago -- South America -- Trinidad
Trinidad and Tobago -- Caribbean region -- Trinidad

Droits : All rights to images are held by the respective holding institution. This image is posted publicly for non-profit educational uses, excluding printed publication. For permission to reproduce images and/or for copyright information contact Special Collections & University Archives, University of Central Florida Libraries, Orlando, FL 32816 phone (407) 823-2576, email: speccoll@mail.ucf.edu
CFM1972_01a
http://ufdc.ufl.edu/AA00031228/00001

Éditeur(s) : C. Hingray Brockhaus et Avenarius C. Hingray ( Paris ) Brockhaus et Avenarius ( Leipzig )
Résumé : Title from PDF t.p. (LLMC Digital, viewed on Nov. 27, 2010)
"Ouvrage contenant le texte des codes 1⁰ Napoléon, 2⁰ des Deux-Siciles, 3⁰ de la Louisiane, 4⁰ Sarde, 5⁰ du Canton de Vaud, 6⁰ Hollandais, 7⁰ Bavarois, 8⁰ Autrichien, 9⁰ Prussien, 10⁰ Suédois, 11⁰ de Berne, 12⁰ de Fribourg, 13⁰ d'Argovie, 14⁰ de Bade, 15⁰ d'Haïti, et les lois hypothécaires de 1⁰ Suède, 2⁰ Wurtemberg, 3⁰ Genève, 4⁰ Fribourg, 5⁰ Saint-Gall, 6⁰ la Grèce."
First section paged in duplicate and arranged in parallel columns spread across two pages.
(Statement of Responsibility) par M. Anthoine de Saint-Joseph.
Europe
France
Haiti
Europe
France
Haïti

685212440

Résumé : The slides were taken on collecting trips sponsored by the William L. Bryant Foundation, where books, music and art indigenous to the regions were gathered. The are organized by geographical location.
Montego Bay, Saint James, Jamaica became popular as a sea bathing destination when in 1906 Doctor Alexander James McCatty donated the land to the community and rumors spread that the waters off this beach had health benefits. The beach received its name from Doctor McCatty and his physician friends and because the original entrance was through a cave, which was destroyed in a 1932 hurricane. The image is of tourists sea bathing in the Caribbean Sea while children play in the sand of Doctor's Cave Beach.
Jamaica -- Caribbean region -- Montego Bay, Saint James

Droits : All rights to images are held by the respective holding institution. This image is posted publicly for non-profit educational uses, excluding printed publication. For permission to reproduce images and/or for copyright information contact Special Collections & University Archives, University of Central Florida Libraries, Orlando, FL 32816 phone (407) 823-2576, email: speccoll@mail.ucf.edu
CFM1972_01a
http://ufdc.ufl.edu/AA00031050/00001

Résumé : At the outbreak of war with Spain in 1898, the U.S. Army was very small in numbers. This situation necessitated an immediate call for volunteers. President McKinley's appeal was overwhelmingly answered by a generation that had grown up in the shadow of their elders' Civil War glory. One group answering the call was the First Regiment of the U.S. Cavalry Volunteers, headed by Colonel Leonard Wood, a distinguished army doctor and Medal of Honor recipient. The regiment was actually the brainchild of Theodore Roosevelt, assistant secretary of the navy and Wood's friend. Roosevelt, realizing his own lack of military experience, suggested Wood for the command. The Rough Riders, as the regiment was soon known, comprised 1,250 men, including cowboys, Native Americans and eastern college athletes. Despite their dissimilarities, they were in excellent physical condition'a stark contrast to most of the other volunteer contingents. The Rough Riders departed from Tampa in mid-June without their horses. They landed at Daiquiri on June 22 and two days later served with distinction in a battle at Las Guásimas. Immediately prior to the conflict at San Juan, Colonel Wood was promoted to another field command, enabling Roosevelt as a full colonel to take command of the Rough Riders. On July 1, Roosevelt, having secured a horse, led his forces in a charge up Kettle Hill outside of Santiago. They achieved their goal and later in the day participated in the victory at San Juan Hill. By seizing these heights, American guns commanded the harbor at Santiago. The Spanish position was imperiled and an abortive attempt by the Spanish navy to escape from the harbor was halted with devastating results. Spanish land forces surrendered shortly thereafter. Roosevelt urged the Rough Riders' swift evacuation, fearing the continuing spread of disease. They returned to Montauk, Long Island, where they were held in quarantine before being mustered out in September. More than one-third of the Rough Riders were casualties in the Spanish-American War, a fact that has led some observers to criticize Roosevelt for unnecessary risk-taking. Nevertheless, the Rough Riders became heroes to the American public and Roosevelt emerged as a major national figure.
(Funding) Funded in part by the Institute for Museum and Library Services (IMLS), Ephemeral Cities Project.
Tampa |z 1271000 |2 ceeus
Hillsborough County |z 12057 |2 ceeus
United States of America -- Florida -- Hillsborough County -- Tampa
United States

Droits : All rights reserved. 2005.
D20-012

Éditeur(s) : Gauthier-Villars
Résumé : The three main sources of organic matter in oceanic basins are marine plankton, terrestrial higher plants and undifferentiated residual organic matter which has been highly degraded in subaerial environments. The time and areal distribution of marine organic matter is mainly controlled by the conditions of preservation. In deep oceans accumulation occurs mainly in confined anoxic basins, and also in open ocean, where local conditions generate a surplus of supply over bacterial degradation. Moderately degraded terrestrial organic matter is derived from land plants and carried away by rivers and currents. It is mainly deposited in sediments of the river fans. Residual organic matter has been highly degraded in subaerial conditions prior to transportation, and may consist of contemporaneous and/or recycled material. It cannot be degraded any more and may be spread over wide areas, regardless of the local environments.
Oceanologica Acta, Special issue (0399-1784) (Gauthier-Villars), 1981

Droits : info:eu-repo/semantics/openAccess
http://archimer.ifremer.fr/doc/00246/35680/34188.pdf
http://archimer.ifremer.fr/doc/00246/35680/

Éditeur(s) : EDP Sciences
Résumé : A population of the invasive slipper limpet (Crepidula fornicata) has been spreading in the Bay of Mont-Saint-Michel (Western English Channel) for 40 years. Sidescan sonar, underwater video and quantitative sampling were conducted in 1996 and 2004 to document the widening geographic spread of the species over the bay. The limpet population grew by 50% during this period, to reach a fresh biomass of about 150 000 t. This local study analyses causes and effects of the spread and provides a typical example of the limpet spreading process. This population increase has significant effects on the environment in the most densely colonized area (modification to the sediment and biodiversity), leading to the emergence of a new benthic community. Anthropic dredging activities are among the causative factors of the spread but are also adversely affected by the invasion.
Depuis 40 ans, la population de crépidules (Crepidula fornicata) prolifère en baie du Mont Saint-Michel (Manche Ouest). Deux études réalisées en 1996 et 2004 ont permis de cartographier et d'estimer le stock de la population grâce à des moyens similaires : sonar à balayage latéral, vidéo sous-marine et prélèvements quantitatifs à la benne. Durant cet intervalle de temps, la biomasse a augmenté de 50 % pour atteindre 150 000 t dans la baie en 2004. Cette étude comparative a permis d'analyser les causes et les effets d'une telle prolifération et d'en montrer le processus général. Dans les secteurs fortement colonisés, les effets sur l'environnement sont particulièrement néfastes (modification du sédiment et de la biodiversité) et aboutissent à une nouvelle communauté benthique. Les activités de pêche aux engins traînants (dragues et chaluts) sont à la fois les principales responsables et les victimes de cette prolifération.
Aquatic Living Resources (0990-7440) (EDP Sciences), 2009 , Vol. 22 , N. 1 , P. 11-19

Droits : 2009 EDP Sciences
http://archimer.ifremer.fr/doc/2009/publication-6351.pdf
DOI:10.1051/alr/2009004
http://archimer.ifremer.fr/doc/00000/6351/

Éditeur(s) : HAL CCSD
Résumé : International audience
Structure and evolution of networks have been areas of growing interest in recent years, especially with the emergence of Social Network Analysis (SNA) and its application in numerous fields. Researches on diffusion are focusing on network modeling for studying spreading phenomena. While the impact of network properties on spreading is now widely studied, involvement of network dynamicity is very little known. In this paper, we address the epidemiology context and study the consequences of network evolutions on spread of diseases. Experiments are conducted by comparing incidence curves obtained by evolution strategies applied on two generated and two real networks. Results are then analyzed by investigating network properties and discussed in order to explain how network evolution influences the spread. We present the MIDEN framework, an approach to measure impact of basic changes in network structure, and DynSpread, a 2D simulation tool designed to replay infections scenarios on evolving networks.
Database and Expert Systems Applications - 22nd International Conference, DEXA 2011, Toulouse, France, August 29 - September 2, 2011, Proceedings, Part II
Toulouse, France

hal-00614925
https://hal.archives-ouvertes.fr/hal-00614925
DOI : 10.1007/978-3-642-23091-2_49

Éditeur(s) : HAL CCSD American Geophysical Union - AGU
Résumé : IODP Expedition 335 "Superfast Spreading Rate Crust 4" returned to ODP Hole 1256D with the intent of deepening this reference penetration of intact ocean crust several hundred meters into cumulate gabbros. This was the fourth cruise of the superfast campaign to understand the formation of oceanic crust accreted at fast spreading ridges, by exploiting the inverse relationship between spreading rate and the depth to low velocity zones seismically imaged at active mid-ocean zones, thought to be magma chambers. Site 1256 is located on 15-million-year-old crust formed at the East Pacific Rise during an episode of superfast ocean spreading (>200 mm/yr full rate). Three earlier cruises to Hole 1256D have drilled through the sediments, lavas and dikes and 100 m into a complex dike-gabbro transition zone. The specific objectives of IODP Expedition 335 were to: (1) test models of magmatic accretion at fast spreading ocean ridges; (2) quantify the vigor of hydrothermal cooling of the lower crust; (3) establish the geological meaning of the seismic Layer 2-3 boundary at Site 1256; and (4) estimate the contribution of lower crustal gabbros to marine magnetic anomalies. It was anticipated that even a shortened IODP Expedition could deepen Hole 1256D a significant distance (300 m) into cumulate gabbros. Operations on IODP Expedition 335 proved challenging from the outset with almost three weeks spent re-opening and securing unstable sections of the Hole. When coring commenced, the destruction of a hard-formation C9 rotary coring bit at the bottom of the hole required further remedial operations to remove junk and huge volumes of accumulated drill cuttings. Hole-cleaning operations using junk baskets returned large samples of a contact-metamorphic aureole between the sheeted dikes and a major heat source below. These large (up to 3.5 kg) irregular samples preserve magmatic, hydrothermal and structural relationships hitherto unseen because of the narrow diameter of drill core and previous poor core recovery. Including the ~60 m-thick zone of granoblastic dikes overlying the uppermost gabbro, the dike-gabbro transition zone at Site 1256 is over 170 m thick, of which more than 100 m are recrystallized granoblastic basalts. This zone records a dynamically evolving thermal boundary layer between the principally hydrothermal domain of the upper crust and a deeper zone of intrusive magmatism. The recovered samples document a sequence of evolving geological conditions and the intimate coupling between temporally and spatially intercalated intrusive, hydrothermal, contact-metamorphic, partial melting and retrogressive processes. Despite the operational challenges, we achieved a minor depth advance to 1522 m, but this was insufficient penetration to complete any of the primary objectives. However, Hole 1256D has been thoroughly cleared of junk and drill cuttings that have hampered operations during this and previous Expeditions. At the end of Expedition 335, we briefly resumed coring and stabilized problematic intervals with cement. Hole 1256D is open to its full depth and ready for further deepening in the near future.
InterRidge News

hal-00688821
https://hal.archives-ouvertes.fr/hal-00688821

Éditeur(s) : Gauthier-Villars
Résumé : Over 400,000 km of low level aeromagnetic data were collected by US Navy research organization over the Arctic Basin and Greenland-Norwegian Sea during the years 1972 to 1978. These data provide new constraints on the crustal structure and tectonic evolution of this vast region. Magnetic anomalies over continental fragments (Lomonosov Ridge and Chukchi Borderland) are irregular, with local short-wavelength features indicating relatively shallow basement. Sea-floor spreading between Scandinavia and Greenland commenced about 58 m.y.b.p. during the reversed period preceding anomaly 24. Spreading between the Lomonosov Ridge and Eurasia also began at this time or possibly somewhat earlier. An extinct spreading axis in the Canada Basin is indicated by gravity and magnetic data.
Oceanologica Acta, Special issue (0399-1784) (Gauthier-Villars), 1981

Droits : info:eu-repo/semantics/openAccess
http://archimer.ifremer.fr/doc/00245/35663/34171.pdf
http://archimer.ifremer.fr/doc/00245/35663/

Éditeur(s) : American Geophysical Union
Résumé : We present four companion digital models of the age, age uncertainty, spreading rates, and spreading asymmetries of the world's ocean basins as geographic and Mercator grids with 2 arc min resolution. The grids include data from all the major ocean basins as well as detailed reconstructions of back-arc basins. The age, spreading rate, and asymmetry at each grid node are determined by linear interpolation between adjacent seafloor isochrons in the direction of spreading. Ages for ocean floor between the oldest identified magnetic anomalies and continental crust are interpolated by geological estimates of the ages of passive continental margin segments. The age uncertainties for grid cells coinciding with marine magnetic anomaly identifications, observed or rotated to their conjugate ridge flanks, are based on the difference between gridded age and observed age. The uncertainties are also a function of the distance of a given grid cell to the nearest age observation and the proximity to fracture zones or other age discontinuities. Asymmetries in crustal accretion appear to be frequently related to asthenospheric flow from mantle plumes to spreading ridges, resulting in ridge jumps toward hot spots. We also use the new age grid to compute global residual basement depth grids from the difference between observed oceanic basement depth and predicted depth using three alternative age-depth relationships. The new set of grids helps to investigate prominent negative depth anomalies, which may be alternatively related to subducted slab material descending in the mantle or to asthenospheric flow. A combination of our digital grids and the associated relative and absolute plate motion model with seismic tomography and mantle convection model outputs represents a valuable set of tools to investigate geodynamic problems.
Geochemistry Geophysics Geosystems - G3 (1525-2027) (American Geophysical Union), 2008-04 , Vol. 9 , P. NIL_18-NIL_36

Droits : 2008 American Geophysical Union
http://archimer.ifremer.fr/doc/2008/publication-3900.pdf
DOI:10.1029/2007GC001743
http://archimer.ifremer.fr/doc/00000/3900/

Éditeur(s) : HAL CCSD
Résumé : This thesis compiles two distinct studies that both document the control of microstructures on rock seismic properties. The first part deals with the development of crystallographic preferred orientations (CPO) in the uppermost mantle associated with melt/fluid-rock interactions, recorded in peridotites xenoliths from the Japan sea back-arc basin. The microstructural and geochemical characteristics of the studied samples reveal that active spreading is associated to uppermost mantle deformation similar to that observed in the Oman ophiolite. At the onset of back-arc spreading, there are no strong interactions between melt percolation and deformation in comparison to continental rift zones, probably due to the relatively small size and short duration of the spreading event. The second part presents a unique database of plagioclase CPO from variously deformed mafic rocks. CPO are grouped in three main types; their characteristics as a function of deformation regime (magmatic or crystal-plastic) are outlined and discussed. Calculated seismic properties of gabbroic rocks show that anisotropy tends to increase as a function of fabric strength, although it is generally weak, due to the competing effect of olivine/clinopyroxene and plagioclase.
Cette thèse regroupe deux études distinctes, qui documentent le contrôle des microstructures sur les propriétés sismiques des roches. La première partie traite du développement des orientations préférentielles cristallographiques (OPC) dans le manteau supérieur, associé aux interactions liquide/magma-roche, enregistré dans des xénolites de péridotites du bassin d'arrière-arc de la mer du Japon. Les caractéristiques microstucturales et géochimiques des échantillons étudiés montrent que l'ouverture arrière-arc active est associée à une déformation du manteau supérieure similaire à celle observée dans l'ophiolite d'Oman. L'initiation de l'extension d'arrière-arc n'est pas associée à de fortes interactions entre percolation magmatique et déformation, en comparaison avec les zones de rifting continentales, probablement en raison des taille et durée relativement petites de l'épisode d'ouverture. La seconde partie présente une base de données unique d'OPC de plagioclase de roches mafiques plus ou moins déformées. Les OPC sont classées en 3 types principaux; leurs caractéristiques en fonction du régime de déformation (magmatique ou plastique) sont présentées et discutées. Les propriétés sismiques calculées des roches gabbroiques montrent que l'anisotropie tend à croitre avec l'intensité des fabriques, bien qu'elle soit généralement faible, en raison des effets opposés des olivines/clinopyroxènes et du plagioclase.
https://tel.archives-ouvertes.fr/tel-00795505

tel-00795505
https://tel.archives-ouvertes.fr/tel-00795505
https://tel.archives-ouvertes.fr/tel-00795505/document
https://tel.archives-ouvertes.fr/tel-00795505/file/Satsukawa_thesis_UM2.pdf

Éditeur(s) : HAL CCSD AGU and the Geochemical Society
Résumé : International audience
In the Oman ophiolite crustal section, a contact zone between the gabbro unit and the volcanics and diabase sheeted dikes, called the root zone of the sheeted dike complex, has been recently mapped at a fine scale in a selected area. The Oman ophiolite is derived from a fast spreading ridge which had a melt lens located between the main gabbro unit and the root zone of the sheeted dike complex. With a few exceptions accounted for, this horizon has a fairly constant thickness, similar to 100 m, and a crude internal pseudo-stratigraphy. At the base of the root zone are isotropic ophitic gabbros interpreted as a thermal boundary layer. This layer is transitional between the magmatic system of the melt lens, convecting at 1200 degrees C, and a high-temperature (< 1100 degrees C) hydrothermal system, convecting within the root zone. Above this level, the isotropic gabbros have been, locally, largely molten due to an influx of seawater, at similar to 1100 degrees C, thus generating varitextured ophitic and pegmatitic gabbros. These latter gabbros constitute the upper part of the root zone and are associated with trondjhemitic intrusions as screens in the lower sheeted dikes. Diorites and trondjhemites were also generated by hydrous melting, at temperatures below 1000 degrees C. The whole root zone is a domain of very sharp average thermal gradient (similar to 7 degrees C/m). At the top of the root zone, a new thermal boundary layer, with diabase dikes hydrated in amphibolite facies conditions, separates the preceding high- temperature convective system from the well-known greenschist facies (< 450 degrees C) hydrothermal system operating throughout the sheeted dike complex, up to the seafloor. The isotropic gabbros near the base of the root zone are intruded by protodikes with distinctive microgranular margins and an ophitic center. Protodike swarms are exceptional because, intruding a medium at similar to 1100 degrees C, they are largely destroyed by dike-in-dike intrusions and by hydrous melting. However, they demonstrate that this zone was generated by melt conduits issued from the underlying melt lens. Each dike of the sheeted dike complex is thus fed by one protodike. As this zone has been recently drilled by IODP in the eastern Pacific Ocean, a brief comparison is proposed.
ISSN: 1525-2027

hal-00411331
https://hal.archives-ouvertes.fr/hal-00411331
DOI : 10.1029/2007GC001918

Résumé : Arbusto o árbol de hasta 20 m. Hojas oblongas a anchamente aovadas, de 3 a 15 cm, agudas a acuminadas, aserradas, estrellado-tomentosas, marcadamente asimétricas. Flores amarillentas, fragantes, en cimas axilares pequeñas, con 5 pétalos de 3 mm. Fruto leñoso, globoso u oval, de 2 a 4 cm, con tubérculos duros.
Arbuste ou arbre pouvant atteindre 20 m. Feuilles oblongues à largement ovées, de 3 à 15 cm, aiguës à acuminées, dentées, en forme d&rsquo;étoile, tomenteuses, très asymétriques. Fleurs jaunâtres, odorantes, sur de petites tiges axillaires, avec 5 pétales de 3 mm. Fruit ligneux, arrondi ou ovale, de 2 à 4 cm, avec tubercules fermes.
Tree deciduous up to 16 m tall with spreading branches. Leaves alternate 20 cm x 7 cm, lanceolate to ovate, unequal at the base, margins crenate-dentate, hairy from sub-glabrous to tomentose; inflorescence axillary in panicles, flowers 3 mm with five yellow-green petals, fragrant; fruit black, woody, warty, sub-globose 1-2 cm in diameter with the faint smell of molasses, seeds numerous.
Regiones tropicales del continente americano.
Régions tropicales du continent américain.
Tropical and sub-tropicalregions of the American continent.

http://www.tramil.net/fototeca/plant179

Résumé : Arbusto o arbolito de hasta 12 m, ramas armadas con espinas rectas. Hojas pecioladas, compuestas, glabras; 1 a 3 pares de pinas; con folíolos de 12 a 20 pares por pinna, sésiles, linear-oblongos. Flores verde-amarillentas, sésiles, en espigas cilíndricas, densas, de 5 a 10 cm de longitud, pedunculadas. Vaina comprimida, falcada, coriácea indehiscente; semillas aplanadas, ovales de color café.
Arbuste ou petit arbre pouvant atteindre 12 m, branches armées d&rsquo;épines droites. Feuilles pétiolées glabres, bipennées ou tripennées, dont chaque élément porte 12 à 20 paires de folioles, sessiles, linéaires-oblongues.Fleurs vert-jaunâtres, sessiles, en épis cylindriques, denses, de 5 à 10 cm de longueur, pédonculées. Gousse comprimée, en forme de lame de faucille, coriace indéhiscente; graines plates, ovales, couleur café.
Shrub or small tree, up to 12 m high with spreading branches armed with straight spines 0.6-2.5 cm.  Leaves, petiolate 1-4 cm, bipinnate with glands between pairs of pinnae, pinnae 1 pair rarely 2, leaflets 12-20 pairs linear-oblong, 7-16 x 1.5-3.2 mm, apex obtuse or short abrupt point; inflorescence axillary in spikelike racemes, 5-10 cm long; flowers densely packed with pale yellow corolla 2.5 mm long; pod compressed, 7-20 cm x 1-1.6 cm, slightly curved, pale yellow; seeds brown 6 mm embedded in white sweet pulp.
Nativa de América tropical.
Originaire d’;Amérique tropicale.
Native to tropical America.

http://www.tramil.net/fototeca/plant259

Résumé : Arbol de 4-5 (raras veces 8) metros de altura, tronco de hasta 20 cm de diámetro y ramas extendidas. Hojas corto-pecioladas, espatuladas, fasciculadas, de 5 a 20 cm. Flores solitarias, amarillentas con venas de color púrpura, de 5 a 6 cm; lóbulos lacerados. Fruto globoso o elipsoideo, liso, lustroso, de 10 a 30 cm de diámetro, de cáscara dura.
Petit arbre de 8 m ou moins, tronc pouvant avoir jusqu&rsquo;à 20 cm de diamètre et branches allongées. Feuilles à court pétiole, spatulées, fasciculées, de 5 à 20 cm. Fleurs solitaires, jaunâtres avec des veines pourpres, de 5 à 6 cm; lobes très découpés. Fruit arrondi ou ellipsoïdal, lisse, brillant, de 10 à 30 cm de diamètre, à l&rsquo;écorce dure.
Small tree, up to 8 m tall with shorttrunk up to 20 cm in diameter with long spreading branches; leaves short-petiolate, spatulate, fasciculate, 5-20 cm long; flowers bell-shaped, born on the trunk in clusters, 5-6 cm long, greenish- white to greenish-yellowish with purple markings, foul smelling; fruit globose to ellipsoid, smooth, shiny, 10-30 cm in diameter, with hard shell.
Nativa de América tropical continental, cultivada y naturalizada en los trópicos.
Originaire de l’;Amérique tropicale continentale, cultivée et acclimatée sous les tropiques.
Native to tropical continental America, cultivated and naturalized

http://www.tramil.net/fototeca/plant150

Résumé : Hierba perenne, glabra, de hasta 60 cm. Hojas lanceoladas a oblanceoladas de hasta 30 cm de largo, crenadas a finamente espinuloso serradas, adelgazadas en la base formando un pecíolo corto, alado. Inflorescencias en dicasios, ampliamente ramificados con capítulos verde-amarillentos; brácteas involucrales, lanceoladas foliáceas, excediendo los capítulos. Fruto globoso, comprimido lateralmente, densamente escamoso.
Herbe perenne, glabre, pouvant atteindre 60 cm. Feuilles lancéolées à oblongues-lancéolées pouvant atteindre 30 cm de long, crénelées à finement denticulées, minces à la base, laquelle forme un pétiole court, en forme d&rsquo;aile. Inflorescences caractérisées par une fleur terminale, et deux autres situées sur des tiges latérales opposées, amplement ramifiées avec capitules vert-jaunes; bractées en forme de collerette, lancéolées-foliacées, dépassant les capitules. Fruit arrondi, comprimé sur les côtés, abondamment recouvert d&rsquo;écailles.
Biennial, tap-rooted, pungent herb. Leaves forming a basal rosette, oblanceolate, serrate-dentate, 30 cm x 4 cm; inflorescence widely spreading from the main shoot; flower heads cylindrical ca 1.5 cm long, green, subtended by a whorl of 5- 6 unequal bracts; fruits scaly, ca 2 mm long.
Originaria de América tropical, introducida y naturalizada en Africa tropical.
Originaire d&rsquo;Amérique tropicale, introduite et naturalisée en Afrique tropicale.
Native to tropical America, introduced and naturalized in tropical Africa

http://www.tramil.net/fototeca/plant168