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.
Boats and ocean liners anchored in Saint George’s harbor, Grenada. A yacht with what appears to be the name Sans Souci is flying a United States of America and the Grenadan flag (1967-1974). In 1967 when Grenada became a British Associated State, it adopted a blue-yellow-green flag with a nutmeg in the center. The nutmeg represented Grenada’s position as the “Spice Isle” and is also featured on the Coat of Arms. This flag was used until 1974 when Grenada gained independence. Merchant Vessel (MV) Geestcape, partially pictured, entered service in 1966. In 1935, the Van Geest brothers in Spalding, United Kingdom started a horticultural business. The brothers later expanded their business to include a cargo service to carry horticultural produce, primarily bananas, from the Windward and Leeward Islands to Europe. MV Geestcape is also flying the flag of the British Merchant Navy, a red flag with the Union Jack in the upper left corner. Motor Ship (MS) Renaissance, behind MV Geestcape, was built in 1966. Until 1977, Renaissance operated primarily on the Marseille-Haifa route under Compagnie Navigation de Paquet (Croiseres Paquet), Marseille, France. The cruise liner had many subsequent owners throughout her history, until her disposal in 2010. She is pictured here flying the French flag. In the distance overlooking the harbor is Fort George, Grenada’s oldest fort which was built by the French in 1705. Fort George continues (2013) to function as the headquarters for the Royal Grenada Police Force, which it has housed since 1854 when the Colonial Government took over control of the fort. Slide labeled Grenada Harbor.
Grenada -- Caribbean region -- Saint George's, Saint George

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 44:9
http://ufdc.ufl.edu/AA00029627/00001

Résumé : Photo date stamped on back: April 11, 1980.
(Biographical) "34 true Cuban patriots ... are starving themselves as they say the thousands of their brothers and sisters trapped in the Peruvian Embassy in Havana are starving. ... 'I no work until I have an answer from the governments and from the world,' said 56-year-old Angel Urquiloa." -- Article by Jack Knarr in the Miami News, April 10, 1980, p. 4A.
(Biographical) In early April 1980, the Cuban government announced that anyone wishing to leave the country should go to the Peruvian Embassy. Within two days about 10,000 Cubans entered the grounds. On April 20, Castro announced that all who wished to leave could board boats at the port of Mariel. Thus began the Mariel Boatlift.
(Preferred Citation) Cite as Miami News Collection, HistoryMiami, 1995-277-3047.
Cuba

Droits : All rights reserved by the source institution.
1995-277-3047
http://ufdc.ufl.edu/AA00015765/00001

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.
View of a Jamaican coastal fishing village with board, zinc roofed houses on the shores of the Caribbean Sea. Numerous fishing nets have been hung to dry on bamboo poles. Various fishing boats can be seen moored to the docks. In the distance, a woman is entering a house while laundry dries in the sun. Slide labeled Jam. north Coast.
Jamaica -- Caribbean region

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/AA00030869/00001

Extrait de : La Guyane Française, souvenirs et impressions de voyage (p.241)
Siècle(s) traité(s) : 19
Droits : Domaine public
Permalien : http://www.manioc.org/images/FRA110900245i1
FRA110900245i1

Éditeur(s) : Gauthier-Villars
Résumé : The suspended matter transported by the Orinoco to the Orinoco delta originates mainly in the Colombian Andes. The four clayey minerals (kaolinite, chlorite, illite and smectite) are always present in the deltaic suspensions, the delta deposits and the gulf of Paria. Illite contents are always dominant except in those regions of the gulf of Paria situated far from the mouths of the Orinoco tributaries characterized by smectites. In the delta, illite contents which are minimal during the dry season increase noticeably during the wet season which is marked by a high Liquid and particulate matter discharge. In the delta, the clay mineralogy of the substrate is comparable to that of dry season suspensions (February), thus showing a sedimentation composed of particulate matter carried by the Orinoco and Amazon rivers. In the wet season, the high liquid and particulate discharges circulate through the delta, then enter and disperse in the Caribbean Sea and the near Atlantic. The clay mineralogy described in the gulf of Paria show that this allochthonous participation of the Amazon in the deltaic sedimentation of the Orinoco is much more pronounced there. In this region, the spatial variations in illite content show this mineral to be a good marker for circulation.
Oceanolica Acta (0399-1784) (Gauthier-Villars), 1997 , Vol. 20 , N. 6 , P. 799-809

Droits : info:eu-repo/semantics/openAccess
http://archimer.ifremer.fr/doc/00093/20435/18102.pdf
http://archimer.ifremer.fr/doc/00093/20435/

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.
Buildings near the harbor in Saint George’s, Saint George, Grenada. Many of the buildings’ architectural elements feature symmetrical designs. People can be seen walking along the harbor as automobiles pass by. Some of the retail establishments include “Jonas Browne & Hubbard Ltd.,” “The Royal Bank of Canada,” “The Nutmeg Bar & Restaurant,” “The Food Fair,” “BWIA,” and “Hankeys.” Jonas Browne and Hubbard Limited is a supermarket, which has been in business since the 1830s. Food Fair is also another supermarket chain. Trinidad and Tobago based BWIA, British West Indian Airways, was incorporated in 1943 by Lowell Yerex. The clock tower of Saint George's Anglican Church can be seen above the city. Saint George's Anglican Church was built in 1825 and suffered damage during Hurricane Ivan in 2004, losing its roof. The clock tower, constructed in 1904, still remains. Small boats can be seen in the harbor along with Merchant Vessel (MV) Geestcape, partially pictured, which entered service in 1966. In 1935, the Van Geest brothers in Spalding, United Kingdom started a horticultural business. The brothers later expanded their business to include a cargo service to carry horticultural produce, primarily bananas, from the Windward and Leeward Islands to Europe. Slide labeled Harbor + City Grenada.
Grenada -- Caribbean region -- Saint George's, Saint George

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 44:1
http://ufdc.ufl.edu/AA00029619/00001

Éditeur(s) : Musée départemental d'archéologie précolombienne et de préhistoire de la Martinique
2012.0.1.185
Gros-Morne
Avenue Madiana (Gors-Morne)

Droits : Reproduction soumise à autorisation du Musée départemental d’archéologie précolombienne et de préhistoire de la Martinique
http://www.patrimoines-martinique.org/ark:/35569/a011423604740OLShSl

Résumé : Bacteriological study of abyssal sediments: During the Demeraby mission of the N/O Jean Charcot in the western Atlantic Ocean, a study of the microflora of the digestive tracts of echinoderms (Holothuroidea of various genera, Asteroidea, Echinoidea) was compared with that of the surrounding sediment. The bacterial concentration observed in the digestive tracts of all the animals studied is higher than that in the surrounding sediments. The largest numbers were always found in the most anterior part of the digestive tracts of the holothurians. In some cases, the increase is considerable (7.10 versus 5.2. 10 cells per millilitre): It indicates a proliferation of bacterial cells in the anterior part of the digestive tract. As the sediment moves through the digestive tract, the bacterial level progressively decreases. In the most posterior part, the concentration is, however, always clearly greater than that in the surrounding sediment. In the case of the holothurian of the genus Deima, analysis according to the Adamsonian principle of comparison shows that the microflora isolated from the various parts of the digestive tract is composed of taxonomic groups showing little resemblance to those isolated from the sediment. In the case of the holothurian of the genus Pseudostichopus, no specialisation of the microflora from digestive tract contents appears with respect to that of the ingested sediment. Examination of metabolic activities suggests a juxtaposition of two types of communities: Free sediment - sediment in transit that complement one other in their enzymatic and nutritional behaviour Indeed, the strains of free sediment seem to be rather suitable for hydrolysing and using carbohydrates, while those of enteric communities prefer the hydrolysis of lipids and proteins and the assimilation of fatty acids, dicarboxylic acids, hydroxylic acids and certain amino acids. Moreover, the enteric microflorae possess a greater nutritional versatility that, linked with its total numbers, has a sizeable catabolic potential. .../... -2- Measurements of heterotrophic activity done by means of 14 C glucose tracers make it possible to show that the metabolic activities of the bacterial communities of superficial abyssal sediments vary according to zones. In the Amazon Cone, a clear glucose mineralization gradient over a distance of a few kilometres can be observed. In the abyssal plain of Demerara heterotrophic activities are slowed in relation to those of the superficial sediments of the Cone of the Amazon, even though the bacterial numbers and the depths are of the same order of magnitude in the two zones. The abundant microflorae associated with the various divisions of digestive tract contents of the Deima abyssal holothurian manifest little metabolic activity as regards the glucose. However, the bacterial communities of Pseudostichopus and Psychropotes manifest very strong heterotrophic activities, increasing from the oesophagus towards the cloaca. Current results are too fragmentary to allow us to observe possible physiological specialisation of enteric bacterial communities enabling the facilitation of digestion processes in the host. Conclusion: In the abyssal environment, characterised by poorly developed bacterial communities, microflorae associated with the digestive tract contents of echinoderms have considerably greater cellular concentrations. By means of their enzymatic equipment, these enteric communities, which complement those of the free microflorae of superficial sediments, can participate in the transformation of organic matter in the abyssal area. Study of the dynamics of microbial communities and their heterotrophic activities in shellfish farms: From experiments done on the water in the Arcachon basin, trials to quantify and describe the reactivity potential of bacterial communities were performed. Bacterial communities were defined by direct counts, counts after setting them up for cultivation, structure and diversity of these communities, dosage of AMP, ADP, ATP. Two opposite ecological conditions were considered: Autumn conditions (high temperature) and a winter conditions (low temperature). Tubs of sea water of 6 and 60 litres were enriched either with ammonium chloride or a mixture of amino acids, at about 500 uAtg N.L. The experiments lasted 24 hours, with sampling every 3 hours. The autumn community reacted rapidly (6 hours), the response to the enrichment in organic nitrogen being the highest. The structure of the community has unstable immature stages. On the contrary, during the winter experiment, no response could be perceived. This may mean that the latency phase is greater than 24 hours. The structure of this community has mature stages. In conclusion, bacterial communities react in the same way as macroscopic communities. Stable communities are diversified and correspond to mature stages of the ecosystem; the immature stages are unstable and less diversified. This type of experiment has made it possible to bring to light the rapidity of response of bacterial populations, and can be used to define the stability of a bacterial community in a precise biotope.
ETUDE BACTERIOLOGIQUE DES SEDIMENTS ABYSSAUX RESUME Au cours de la mission DEMERABY du n/o Jean CHARCOT en atlantique occidental , une étude de la microflore des tractus digestifs d'Echinodermes (Holothurides de différents genres, Astérides, Echinides) a été comparée à celle du sédiment environnant. La concentration bactérienne observée dans les tractus digestifs de tous les animaux étudiés est supérieure à celle des sédiments environnants. Les effectifs les plus importants sont toujours observés dans la partie la plus antérieure des tractus digestifs des holothuries. Dans certains cas, l'accroissement est considérable (7.10 contre 5,2. 10 cellules/ml) : il indique une prolifération des cellules bactériennes dans la partie antérieure du tractus digestif. Au.cours de la progression du sédiment dans le tractus digestif, la charge bactérienne décroit progressivement. Dans la partie la plus postérieure, la concentration est cependant toujours nettement supérieure à celle du sédiment environnant-. Dans le cas d'une holothurie du genre Deima, l'analyse selon le principe adansonien de comparaison montre que la microflore isolée des différentes parties du tractus digestif est constituée de groupes taxonomiques présentant peu de ressemblance avec ceux isolés du sédiment. Dans le cas d'une holothurie du genre Pseudostichopus il n'apparait pas de spécialisation de la microflore du contenu du tractus digestif par rapport à celle du sédiment ingéré. ¿ ¿ . L'étude des activités métaboliques suggère une juxtaposition de deux types de communautés : sédiment libre-sédiment en transit qui se complètent dans leur comportement enzymatique et nutritionnel. En effet les souches du sédiment libre semblent être plutôt aptes à hydrolyser et à utiliser les glucides, tandis que celles des communautés entériques portent leur préférence sur l'hydrolyse des lipides et protéines et 1'assimilation des acides gras, acides dicarboxyl iques, hydro'xy-acides et certains acides aminés. D'autre part les microflores entériques possèdent une versatilité nutritionnelle plus importante qui, liée à leurs effectifs, offre une potentialité catabolique non négligeable. .../... -2- Les mesures d'activité hétérotrophe effectuées au moyen de traceurs glucose 14 C permettent de montrer que les activités métaboliques des communautés bactériennes des sédiments abyssaux superficiels varient selon les zones. Dans le Cone de l'Amazone on observe un net gradient de minéralisation du glucose sur une distance de quelques kilomètres. Dans la plaine abyssale de Demerara les activités hétérotrophessont ralenties par rapport à celles des sédiments superficiels du Cone de l'Amazone, bien que les effectifs bactériens et les profondeurs soient du même ordre de grandeur dans ces deux zones. Les abondantes microflores associées aux différentes fractions du contenu du tractus digestif de l'holothurie abyssale Deima ne manifestent que peu d'activités métaboliques vis à vis du glucose. Par contre les communautés . bactériennes de Pseudostichopus et P syahropotes manifestent des activités hétérotrophes très fortes, croissant de 1'oesophage vers le cloaque. Les résultats actuels sont trop fragmentaires pour permettre d'observer une éventuelle spécialisation physiologique des communautés bactériennes entëriques permettant de faciliter les processus de digestion chez l'hôte. Conclusion: dans le milieu abyssal, caractérisé par des communautés bactériennes faiblement développées, les microflores associées aux contenus de tractus digestif des Echinodermes présentent des concentrations cellulaires considérablement plus importantes. Par leurs équipements enzymâtiques ces communautés entëriques complémentaires de ceux des microflores libres des sédiments superficiels, peuvent participer à la transformation des matières organiques du domaine abyssal. ETUDE DE LA DYNAMIQUE DES COMMUNAUTES MICROBIENNES ET DE LEURS ACTIVITES HETEROTROPHES DANS LES PARCS CONCHYLICOLES RESUME A partir d'expérimentations effectuées sur l'eau du bassin d'Arcachon, des essais de quantification et qualification du potentiel de réactivité des communautés bactériennes ont été effectuées. Les communautés bactériennes ont été définies par comptage directs, comptages après mise en culture, structure et diversité de ces communautés, dosage des AMP, ADP, ATP. Deux situations écologiques opposées ont étées considérées . Une situation automnale (température élevée) et une situation hivernale (température faible). Des bacs d'eau de mer de 6 et 60 litres ont été enrichis , soit avec du chlorure d'ammonium, soit avec un mélange d'acides aminés, à environ 500 uAtg N.l" . Les expériences ont duré 24 heures, avec des prélèvements toutes les 3 heures. La communauté automnale réagit rapidement (6 heures), la ' réponse à l'enrichissement en azote organique étant la plus importante. La structure de la communauté présente des stades immatures instables. Au contraire, au cours de l'expérimentation hivernale, aucune réponse n'a pu être perçue. Ceci peut signifier que la phase de latence est supérieure à 24 heures. La structure . de cette communauté présente des stades matures. En Conclusion, les communautés bactériennes réagissent de la même façon que les communautés macroscopiques. Les communautés stables sont diversifiées et correspondent à des stades matures de l'écosystème, les stades immatures sont instables et moins diversifiés. Ce type d'expérience a permi de mettre en évidence la rapidité de réponse des populations bactériennes, et peut être utilisé pour définir la stabilité d'une communauté bactérienne dans un biotope précis.

Droits : info:eu-repo/semantics/openAccess
http://archimer.ifremer.fr/doc/1981/rapport-1926.pdf
http://archimer.ifremer.fr/doc/00000/1926/

Éditeur(s) : John C. Winston Co.] John C. Winston Co.] ( [Chicago ;, Philadelphia ;, Toronto )
Résumé : (Statement of Responsibility) profusely illustrated with over 150 fine engravings.
Imprint inferred from copyright statement on t.p. verso: "Entered according to Act of Congress in the year 1898 by W.E. Scull," Scull was the vice president of John C. Winston Co.
United States -- Illinois -- Chicago
United States -- Pennsylvania -- Philadelphia
Canada -- Toronto

Droits : This item is presumed to be in the public domain. The University of Florida George A. Smathers Libraries respect the intellectual property rights of others and do not claim any copyright interest in this item. Users of this work have responsibility for determining copyright status prior to reusing, publishing or reproducing this item for purposes other than what is allowed by fair use or other copyright exemptions. Any reuse of this item in excess of fair use or other copyright exemptions may require permission of the copyright holder. The Smathers Libraries would like to learn more about this item and invite individuals or organizations to contact The Department of Special and Area Studies Collections (special@uflib.ufl.edu) with any additional information they can provide.
002223115
ALG3363
262616601

Résumé : Planta de 6 a 10 m, estolonífera. Hojas pecioladas, de hasta 2 m, arregladas en espiral, simples, enteras, ampliamente elípticas, penninervadas. Inflorescencias espiciformes que crecen desde el cormo a través del pseudo tallo, recurvo-colgantes; flores blanco-amarillentas, en cimas a lo largo del eje principal, cubiertas por brácteas grandes. Fruto cilíndrico de hasta 30 cm, amarillo o verdoso al madurar.
Plante de 6 à 10 m, stolonifère. Feuilles pétiolées, pouvant atteindre 2 m, disposées en spirale, simples, entières, largement elliptiques, penniformes. Inflorescences spiciformes sortant du pseudo-tronc, recourbées et pendantes; fleurs blanc-jaunâtres, disposées en cymes le long de l’axe principal, couvertes de grandes bractées, les supérieures femelles. Fruit cylindrique pouvant avoir 30 cm de long, jaune ou verdâtre au cours de la période de maturation.
Large perennial herb 2-9 m high with basal corm. Pseudostem composed of leaf sheaths forming the ‘trunk’ of the plant. Leaves blades oblong, entire 1.5-4 m x 0.7-1 m, petiole 30-90 cm long, rounded beneath, channeled above; inflorescences terminal, growing from the pseudostem, erect or drooping; flowers in flat clusters in the axils of spirally arranged broad, dark purple-coloured bracts, functionally unisexual, the lower female the upper male; mature fruit fleshy, cylindrical, 6-35 cm x 2.5-5 cm with greenish, yellow or reddish skin.
Nativa de los trópicos del Viejo Mundo, cultivada en las regiones tropicales de todo el mundo.
Originaire des tropiques de l’;Ancien Monde, cultivée dans les régions tropicales du monde entier.
Native to the tropics of the Old World, cultivated

http://www.tramil.net/fototeca/plant238

Résumé : Arbusto o arbolito de hasta 9 m, muy ramificado. Hojas alternas, aovadas, de 8 a 20 cm, acuminadas, cordadas en la base, enteras. Inflorescencia en panículas terminales; flores de 4 a 5.3 cm de diámetro; pétalos rosados o blancos, obovados a anchamente ovales. Cápsula (fruto) ovoidea a globoso-ovoidea, de 3 a 4 cm, usualmente con espinas blandas. Semillas con un arilo rojo.
Arbuste ou petit arbre pouvant atteindre 9 m, très ramifié. Feuilles alternes, ovalées, de 8 à 20 cm, acuminées, cordées à la base, entières. Inflorescence en panicules terminaux; fleurs de 4 à 5,3 cm de diamètre; pétales rosés ou blancs, courbes à largement ovales. Capsule ovalée à globuleuse-ovalée, de 3 à 4 cm, avec habituellement des épines molles. Graines avec un arille rouge.
Shrub or small tree, up to 9 m in height, with many branches.  Leaves alternate, ovate, 8 to 20 cm in length, cordate at the base, entire.  Inflorescence in terminal panicles; flowers 4 to 5.3 cm wide; pink or white petals, obovate to broadly oval.  Capsule (fruit), ovoid to globosely-ovoid, 3 to 4 cm in length, usually with soft thorns.  Seed with red aril.
Originaria del trópico americano, cultivada en las regiones tropicales.
Originaire du tropique américain, cultivée dans les régions tropicales.
Native from American tropic and cultivated in tropical regions.

http://www.tramil.net/fototeca/plant101

Résumé : Herbácea anual, erecta, de hasta 60 cm; las partes nuevas pubescentes. Hojas elípticas, ovadas u oblongas de 2 a 4 cm, agudas en el ápice, atenuadas en la base, dentadas o enteras, glabras. Inflorescencia verticilada de hasta 20 cm; pedicelos muy cortos, recurvados; cáliz largo-ciliado de 5 mm; corola blanca, de 4 a 5 mm; filamentos superiores con un apéndice dentiforme en la base.
Herbacée annuelle, dressée, pouvant atteindre 60 cm, dont les parties nouvelles sont pubescentes. Feuilles elliptiques, ovées ou oblongues de 2 à 4 cm, aiguës à la pointe, légèrement renflées à la base, dentées ou entières, glabres. Inflorescence verticillée pouvant atteindre 20 cm; pédicelles très courts, incurvés; calice long-cilié de 5 mm; corolle blanche, de 4 à 5 mm; filaments supérieurs avec un appendice denticulé à la base.
Erect annual herb 30-60 cm high. Stems pubescent, leaves elliptic, ovate or sub-rhombic, 2-4 cm x 1-2 cm, tip acute, base narrow, margins lightly dentate or entire, glabrous except on veins; inflorescence verticillate ca. 20 cm long; corolla white to mauve, 4-5 mm long; fruit an oblong, black, minutely verrucose, nutlet.
Originaria de Asia, cultivada en todo el mundo.
Originaire d’;Asie, cultivée dans le monde entier.
Native to Asia, cultivated throughout the world.

http://www.tramil.net/fototeca/plant247

Éditeur(s) : Gauthier-Villars
Résumé : Simple thermodynamics calculations are applied to processes of a rising plume within an environment of an upward directed gradient of viscosity in the uppermost mantle. Four stages of the development of passive margins are described. Following an initial regional uplift strong lateral movements are induced at asthenospheric levels, stretching the overlying lithosphere. In the second stage plume material also enters the low viscosity lower crust, replacing continental material and forming a new, higher crust-mantle boundary by gravitational differentiation. The inital phase lag between the laterally intruding plume material and the rest of the lithosphere disappears once the continent is rifted and sea floor spreading is established (= stage 3). Finally, at stage 4, quiet subsidence, controlled by contraction, sedimentation, and possible phase changes in the lower crust, is established. The sequence described is in accordance with many observations of geology and geophysics. Rising plumes and sinking slabs are considered equivalent expressions of the heat engine earth which determines global tectonics.
Oceanologica Acta, Special issue (0399-1784) (Gauthier-Villars), 1981

Droits : info:eu-repo/semantics/openAccess
http://archimer.ifremer.fr/doc/00245/35658/34167.pdf
http://archimer.ifremer.fr/doc/00245/35658/

Résumé : The boundaries of territorial waters are not as stable as boundaries on land. Nowadays, indeed they are characterised by their very mobility. No doubt the reason for this is political. A state which sought to further her own interests by enlarging her domain within her own waters would encounter no sovereign opposition. Additonally, with the collapse of the traditional "understanding" regarding the conception of -and the criteria governing -maritime boundaries. nations chose the most effective methods of appeasing their own needs and appetites. This was achieved with the maximum ingenuity. The natural boundary myth was shaken sometimes before and sometimes simultaneously with, the cultivation of negotiating skills or, from a position of strength. the imposition of "political limits". Fruitful sources of approximation were provided by phenomena such as low-water mark, the continental shelf. the Humboldt current and so on. As for accuracy. however. this was obtained by the application of geometrical methods such as calculation on a straight line basis or by equidistance or. again. by numeric evaluation : expression of distance in nautical miles. The general effect of this medley of arguments - or pretexts - has been to add to the fluctuating nature of sea boundaries rather than contribute to their stability. In fact. the only way stabilisation of these boundaries is usually achieved is by confrontation between two or more adjacent and competing sovereign states once the question of demarcation has been hammered out. The ocean, "man's common heritage", seems to have entered a phase of parcelling out, of sharing. [NOT CONTROLLED OCR]
Les frontières maritimes n'ont pas la stabilité des frontières terrestres. Dans la présente époque, au contraire, elles se caractérisent essentiellement par leur mobilité. La principale raison de ce phénomène est sans doute d'ordre politique : au large de sa mer territoriale, l'État ne rencontre pas d'autre souveraineté lorsque ses intérêts le portent à étendre son emprise. Aussi, lorsque le « consensus » international traditionnel sur la conception et le critère de la frontière maritime fut ruiné. les États laissèrent libre cours à leur ingéniosité pour choisir les techniques les plus adéquates à la pleine satisfaction de leurs besoins et de leurs appétits. Tour à tour, et, parfois. simultanément. fut agité le mythe de la « frontière naturelle » et cultivé l'art de négocier ou d'imposer, selon les rapports de force. des "limites politiques". La "laisse de basse mer", la "marge continentale ", le courant de Humboldt. etc. fournirent des approximations fécondes. Mais la certitude est venue des techniques géométriques (lignes de base droites, équidistance) ou des évaluations chiffrées (distance exprimée en milles marins). De façon générale. ces divers arguments, ou prétextes. ont puissamment alimenté le dynamisme des frontières maritimes et fort peu contribué à leur stabilisation. Celle-ci ne procède finalement que de la rencontre de deux ou plusieurs souverainetés voisines et concurrentes. une fois tranchées les querelles de "bornage". L'océan, "héritage commun de l'humanité", est entré, semble-t-il, dans une phase de liquidation et de partage... [OCR NON CONTRÔLE]

Droits : 1979 CNEXO
http://archimer.ifremer.fr/doc/1979/rapport-4798.PDF
http://archimer.ifremer.fr/doc/00000/4798/

Éditeur(s) : Amer Geophysical Union
Résumé : Large rivers are key hydrologic components in oceanography, particularly regarding air-sea and land-sea exchanges and biogeochemistry. We enter now in a new era of Sea Surface Salinity (SSS) observing system from Space with the recent launches of the ESA Soil Moisture and Ocean Salinity (SMOS) and the NASA Aquarius/Sac-D missions. With these new sensors, we are now in an excellent position to revisit SSS and ocean color investigations in the tropical northwest Atlantic using multi-year remote sensing time series and concurrent in situ observations. The Amazon is the world's largest river in terms of discharge. In its plume, SSS and upper water column optical properties such as the absorption coefficient of colored detrital matter (acdm) are strongly negatively correlated (<-0.7). Local quasi-linear relationships between SSS and acdm are derived for these plume waters over the period of 2010-2013 using new spaceborne SSS and ocean color measurements. Results allow unprecedented spatial and temporal resolution of this coupling. These relationships are then used to estimate SSS in the Amazon plume based on ocean color satellite data. This new product is validated against SMOS and in situ data and compared with previously developed SSS retrieval models. We demonstrate the potential to estimate tropical Atlantic SSS for the extended period from 1998 to 2010, prior to spaceborne SSS data collection.
Journal Of Geophysical Research-oceans (0148-0227) (Amer Geophysical Union), 2015-05 , Vol. 120 , N. 5 , P. 3177-3192

Droits : 2015. American Geophysical Union. All Rights Reserved.
http://archimer.ifremer.fr/doc/00255/36610/35742.pdf
DOI:10.1002/2014JC010109
http://archimer.ifremer.fr/doc/00255/36610/

Éditeur(s) : HAL CCSD Ocean Drilling Programm
Résumé : This paper provides a summary of postcruise scientific results from Ocean Drilling Program (ODP) Leg 209 available to date, building upon shipboard observations and syntheses summarized in the Leg 209 Initial Results volume. During Leg 209, 19 holes were drilled at 8 sites along the Mid-Atlantic Ridge from 14°43´ to 15°44´N, mainly in residual mantle peridotite intruded by gabbroic rocks, in order to understand the tectonic and structural processes responsible for formation of oceanic lithosphere with abundant residual peridotite exposed on the seafloor coupled with a relatively low proportion of volcanic rocks. Based on proportions of recovered lithologies, the entire area may be underlain by mantle peridotite with ~20%–40% gabbroic intrusions and impregnations. Impregnated peridotites with olivine + two pyroxenes + plagioclase + spinel that apparently formed in equilibrium probably record crystallization from primitive mid-ocean-ridge basalt at pressures of 0.5–0.6 GPa. Metamorphic equilibria record isobaric cooling to ~1100°C at this pressure. Thus, the conductively cooled thermal boundary layer beneath the Mid-Atlantic Ridge in this region is >15 km thick. Combined crystallization and reaction with residual peridotite formed a series of impregnated peridotites recording increasing Na content at nearly constant Mg#; this process could explain some of the variation in fractionation-corrected Na (e.g., Na = 8.0) observed in mid-ocean-ridge basalts. Clinopyroxene textures and compositions record such impregnation processes, and they are particularly well documented for Site 1274. Other Leg 209 gabbroic rocks formed from extensive crystallization of highly evolved melts, indicating that a substantial proportion of melt entering the thermal boundary layer crystallizes entirely beneath the seafloor, with no volcanic equivalent. Alteration of peridotites occurred over a range of temperatures and is the result of three distinct processes: rock-dominated serpentinization with formation of brucite in olivine-rich lithologies, fluid-dominated serpentinization with formation of magnetite and no brucite, and fluid-dominated talc alteration with addition of SiO2 as well as H2O and oxygen. The latter two processes also exhibit detectable trace element metasomatism that is distinct in its character from the igneous impregnation described in the previous paragraph. Microstructures show that most residual peridotites were not ductilely deformed at temperatures less than ~1200°C. Structural and paleomagnetic data require tectonic rotations of relatively undeformed blocks; some rotations probably exceeded 60° around nearly horizontal axes parallel to the rift axis. Rotations occurred along several generations of high-temperature mylonitic shear zones extending deeper than 15 km depth and numerous faults at lower temperature. Early formed shear zones and faults were passively rotated around later features; such a process could have produced low-angle fault surfaces without slip on low-angle faults. This region provides end-member examples of processes that are common at many or most slow-spreading ridges. Osmium isotope ratios indicate an ancient history of depletion for residual peridotites from the 14°–16°N region along the Mid-Atlantic Ridge. Though depleted Os isotope ratios in peridotite have been reported elsewhere along the global ridge system, the values from this region are among the most depleted. In general, Os isotope ratios from mid-ocean-ridge basalts are systematically more radiogenic than Os isotope ratios from ridge peridotite samples, suggesting a polygenetic heterogeneous source for mid-ocean-ridge basalts. Geochemical studies of zircons from Leg 209 gabbroic rocks and impregnated peridotites, together with other ridge and arc-related zircons, indicate that ridge zircons have systematically lower fractionation-corrected U and Th concentrations compared to arc zircons. This observation provides a tool for interpreting the tectonic provenance of ancient detrital zircons and indicates an arclike provenance for Hadean detrital zircons. Geobiological studies and aerobiological studies were also undertaken during Leg 209. The geobiological work found no measurable microbial enhancement of olivine dissolution rate, possibly because the samples from Leg 209 were sterile. The aerobiological study determined that dust from North Africa, collected from the derrick of the JOIDES Resolution during Leg 209, contains a variety of abundant microorganisms.
Proceedings ODP, scientific results, 209

hal-00407966
https://hal.archives-ouvertes.fr/hal-00407966
DOI : 10.2973/odp.proc.sr.209.001.2007

Résumé : Arbusto pequeño muy ramificado de hasta 30 cm de alto; ramas leñosas, rojas o purpúreas, puberulentas. Hojas fasciculadas, corto-pecioladas, elípticas a lineares, obtusas, agudas u obtusas en la base, enteras, conspicuamente glandular-punteadas. Verticilos con 3 a 6 flores, axilares; cáliz puberulento; corola lila, rosada o purpúrea. Nuececillas de 1 mm de longitud.
Petit arbuste très ramifié pouvant atteindre 30 cm de haut; branches ligneuses, rouges ou pourpres, pubérulentes. Feuilles fasciculées, à court pétiole, elliptiques à linéaires, obtuses, aiguës ou obtuses à la base, entières, pointe très nettement glandulaire. Verticilles de 3 à 6 fleurs, axillaires; calice pubérulent; corolle couleur lilas, rosée ou pourpre. Noisettes de 1 mm de longueur.
Densely branching, aromatic, shrub, 20-30 cm high.  Leaves lanceolate, entire, 0.5-1 cm x 0.2-0.5 cm, grayish-green, aromatic with glandular-dotted; flowers born in rounded or ovoid cluster, corolla 2-lipped, lilac, pink or purple; fruits tiny producing 4 nutlets.
Nativa de Europa, cultivada en otras partes del mundo.
Originaire d’;Europe, cultivée dans d’;autres parties du monde.
Native to Europe, cultivated in others parts of the world.

http://www.tramil.net/fototeca/plant350

Résumé : Preliminary analysis of the impact of an environmental change on ichtyologic fauna marinates and fishing in Guyanese water enter within the framework of the program CHALOUPE (dynamic Change of the exploited marine biodiversity and the viability of the Fisheries) coordinated by Ifremer Cayenne and financed by the ANR (National Agency of Research). The study focuses on: -analysis temporal variations of various environmental parameters (sea surface temperature and salinity, the phenomenon El Niño) -fish physical characteristics (tolerances of temperature and salinity, maximum height, distribution…) - analysis of the unloadings per unit of effort of the inshore fishing and an economic analysis of the selling price of fish Data are found on data bases and are given by scientists. The statistical studies and the cartographic representations show that there is an increase in temperature of water in Guiana since the end of the Nineties. The model AquaMaps® simulates the potential consequences of this reheating on the fish distribution. Certain stocks of fishing are weakened. For the moment, if the composition of the captures of inshore fishing changes, that seems more due to a change of fishing strategy than due to an impact of the climatic change. In addition, the average value of the capture increased for reason commercial.
Les analyses de l’impact d’un changement environnemental sur la faune ichtyologique marine et la pêche dans les eaux guyanaises entrent dans le cadre du programme CHALOUPE (CHAngement gLObal, dynamiqUe de la biodiversité marine exploitée et de la viabilité des Pêcheries) coordonné par l’Ifremer Cayenne et financé par l’ANR (Agence Nationale de la Recherche). L’étude porte sur : -l’analyse des variations temporelles de différents paramètres environnementaux (température et salinité de surface des eaux, le phénomène El Niño) à l’échelle de quelques décennies -les caractéristiques physiques des poissons (tolérances de températures et de salinité (taille maximum, répartition…) ; -l’analyse des débarquements par unité d’effort de la pêche côtière depuis les années 70 ; -une analyse économique de la pêche ; Les données sont récoltées à partir de bases de données et au près de différents chercheurs. Les études statistiques et les représentations cartographiques démontrent qu’il y a bien une augmentation de température des eaux en Guyane depuis la fin des années 90. Le modèle statistique sous AquaMaps® permet de simuler les conséquences potentielles de ce réchauffement sur la répartition des poissons. Dans un tel contexte, certains stocks de pêche sont fragilisés. Pour le moment, si la composition des captures de la pêche côtière se modifie dans le même temps, cela semble plus du fait de changement de stratégie de pêche que du fait de l’impact du changement climatique. Par ailleurs, la valeur moyenne de la capture a augmenté pour des raisons commerciales.

Droits : 2006 Ifremer
http://archimer.ifremer.fr/doc/00077/18855/16429.pdf
http://archimer.ifremer.fr/doc/00077/18855/

Résumé : Árbol o arbusto de 5 m o más; ramas erguidas, cuadrangulares. Hojas simples, opuestas, pubescentes, aovadas o elípticas, de 6 a 20 cm de largo, margen entero. Panículas piramidales terminales, de 10 a 40 cm de largo; flores azules o púrpuras, numerosas, de 10 a 12 cm de largo. Drupa azulada o negra, esférica, de 3 a 6 mm de diámetro.
Arbre ou arbuste de 5 m ou davantage; branches dressées, quadrangulaires. Feuilles simples, opposées, pubescentes, ovées ou elliptiques, de 6 à 20 cm de long, bord du limbe entier. Panicules terminales pyramidales, de 10 à 40 cm de longueur; fleurs bleues ou pourpres, nombreuses, de 10 à 12 cm de longueur. Drupe bleutée ou noire, sphérique, de 3 à 6 mm de diamètre.
Tree or shrub, at least 5 m in height, branches erect, square.  Leaves single, opposite, pubescent, ovate to elliptic, 6 to 20 cm in length, margin entire.  Panicles pyramidal, terminal, 10 to 40 cm in length; flowers blue or purple, numerous, 10 to 12 cm in length.  Drupe bluish to black, spherical, 3 to 6 mm in diameter.
Cuenca del Caribe y norte de Suramérica.
Bassin caraïbe et nord de l’;Amérique du Sud.
Caribbean basin and north of South America

http://www.tramil.net/fototeca/plant148

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
Serpentinites form by hydration of mantle peridotite and constitute the largest potential reservoir of fluid-mobile elements entering subduction zones. Isotope ratios of one such element, boron, distinguish fluid contributions from crustal versus serpentinite sources. Despite 85% of boron hosted within abyssal peridotite being lost at the onset of subduction at the lizardite-to-antigorite transition, a sufficient cargo of boron to account for the composition of island arc magma is retained (c. 7 μg g− 1, with a δ11B of + 22‰) until the down-going slab reaches the antigorite-out isograd. At this point a 11B-rich fluid, capable of providing the distinctive δ11B signature of island arc basalts, is released. Beyond the uniquely preserved antigorite-out isograd in serpentinites from Cerro del Almirez, Betic Cordillera, Spain, the prograde lithologies (antigorite–chlorite–orthopyroxene–olivine serpentinite, granofels-texture chlorite-harzburgite and spinifex-texture chlorite-harzburgite) have very different boron isotope signatures (δ11B = − 3 to + 6‰), but with no significant difference in boron concentration compared to the antigorite-serpentinite on the low P–T side of the isograd. 11B-rich fluid, which at least partly equilibrated with pelagic sediments, is implicated in the composition of these prograde lithologies, which dehydrated under open-system conditions. Serpentinite-hosted boron lost during the early stages of dehydration is readily incorporated into forearc peridotite. This, in turn, may be dragged to sub-arc depths as a result of subduction erosion and incorporated in a mélange comprising forearc serpentinite, altered oceanic crust and pelagic sediment. At the antigorite-out isograd it dehydrates, thus potentially providing an additional source of 11B-rich fluids.
ISSN: 0009-2541

hal-01172276
https://hal.archives-ouvertes.fr/hal-01172276
DOI : 10.1016/j.chemgeo.2014.03.015