Résumé : Arbol de 10 a 15 m o más, de copa densa, redondeada; corteza resinosa. Hojas alternas, oblongo-lanceoladas, agudas o acuminadas, subcoriáceas. Flores verdosas o amarillentas, fragantes, en grandes panículas; pétalos de 5 mm, glabros. Drupa elipsoidea a oblícuamente reniforme, de 5 a 15 cm, mesocarpo carnoso amarillo, agridulce.
Arbre de 10 à 15 m ou davantage, tête dense, arrondie; écorce résineuse. Feuilles alternes, oblongues-lancéolées, pointues ou acuminées, subcoriaces. Fleurs verdâtres ou jaunâtres, odorantes, en grandes panicules; pétales de 5 mm, glabres. Drupe ellipsoïdale à obliquement réniforme, de 5 à 15 cm, mésocarpe charnu, jaune, aigre-doux.
Tree evergreen, 10-15 m high with a dense, rounded crown of foliage, bark resinous.  Leaves alternate, simple, spirally arranged, lanceolate-elliptical, 10-25 cm x 2.5-8 cm; inflorescence a terminal panicle ca 30 cm long; flowers 5-8 mm in diameter, greenish or yellowish, fragrant; fruit a fleshy drupe, ellipsoid to obliquely reniform, 5-15 cm long.
Nativa del sureste asiático, cultivada en zonas tropicales y subtropicales de todo el mundo.
Originaire du sud-est asiatique, cultivée dans les zones tropicales et subtropicales du monde entier.
Native to Southeast Asia, cultivated in tropical and su

http://www.tramil.net/fototeca/plant220

Résumé : Arbol de hasta 15 m de alto con corteza blanquecina, suave y madera dura y pesada. Hojas obovadas o elípticas, obtusas, con venación finamente reticulada, corto pecioladas. Panículas con flores blancas, glandulosas; cáliz con 5 lóbulos. Fruto ovoide, negro al madurar.
Arbre pouvant atteindre 15 m de haut, écorce blanchâtre et douce, bois dur et lourd. Feuilles obovées ou elliptiques, obtuses, à nervation finement réticulée, avec un court pétiole. Panicules avec fleurs blanches glanduleuses; calice à 5 lobes. Fruit ovoïde, noir une fois parvenu à maturité.
Evergreen tree up to 15 m high with smooth, whitish, variegated and flaking bark, hard and heavy wood.  Leaves simple, entire, opposite in pairs, dark green, leathery, oblong to elliptic, obtuse at the tip, rounded at the base, 15-20 x 5-7 cm, prominent  venation, highly aromatic when crushed; inflorescence a compound panicle 5-10 cm long, flowers numerous 3-4 mm long, white; fruit a subglobose to ellipsoid berry, 8-10 mm long, thickly covered with small convex glands, black when ripe.
Nativa del norte de Sudamérica y las Antillas, cultivada en los trópicos.
Originaire du nord de l’;Amérique du Sud et des Antilles, cultivée sous les tropiques.
Native to northern South America and the Antilles, cultivated in the tropics.

http://www.tramil.net/fototeca/plant280

Éditeur(s) : HAL CCSD Springer Verlag
Résumé : International audience
Decomposition processes in tropical semi-evergreen forests are still poorly understood. The influence of soil properties and litter quality on decomposition rate was studied in two semi-evergreen forests of Guadeloupe, a forest plantation and a secondary forest, located on different soils. Leaf litter of four tree species was enclosed in litterbags for a 14-month period. Nonlinear correlations were calculated between mass loss and the concentration of major leaf components (soluble C, N, lignin, cellulose, tannins, total soluble phenols) in order to determine the best predictor of leaf litter decomposition. Soil physico-chemical properties and ratios between some of the above-mentioned litter quality parameters were also examined as mass loss predictors. In addition, non-linear correlations were calculated between mass loss and litter quality parameters, at successive periods. Litter quality was the main determinant of litter decomposition in the studied forests. Several litter quality parameters were correlated with leaf disappearance, varying according to stages of decomposition. Between 1 month and 2.5 months, the mass loss was correlated negatively with the initial phenol content and with initial lignin:N and (lignin+phenol):N ratios. From 2.5 to 5.5 months, the mass loss was correlated negatively with the initial phenol content and positively with the initial cellulose content. At later stages of decomposition (9-14 months), the mass loss was correlated negatively with the initial tannin content. Differences in soil characteristics and fauna did not seem to be enough to affect decomposition.
ISSN: 0178-2762

hal-00499535
https://hal.archives-ouvertes.fr/hal-00499535
https://hal.archives-ouvertes.fr/hal-00499535/document
https://hal.archives-ouvertes.fr/hal-00499535/file/Article_decomposition.pdf
DOI : 10.1007/s00374-002-0467-3

Éditeur(s) : HAL CCSD Springer Verlag
Résumé : International audience
The importance of secondary tropical forests regarding the maintenance of soil fauna abundance and diversity is poorly known. The aims of this study were (1) to describe soil fauna abundance and diversity and (2) to assess the determinants of soil fauna abundance and diversity in two stands of a tropical semi-evergreen secondary forest. Soil macrofauna and microarthropod abundance and soil macrofauna diversity were described at two sites developed on different soils and with different site histories: (1) a natural secondary stand (natural forest) under two dominant tree species, Pisonia subcordata and Bursera simaruba, and (2) a planted secondary forest (planted forest) under three tree species, B. simaruba, Swietenia macrophylla, and Tabebuia heterophylla. The effects of both soil and main tree species' litter quality were assessed to explain soil fauna abundance and diversity. The abundance of soil macrofauna was significantly higher in the soil under the planted forest, and soil fauna communities were contrasted between the two sites. In the planted forest, a soil-dwelling macrofauna community developed (mainly consisting of the anecic earthworm Polypheretima elongata). In the natural forest, soil macrofauna and microarthropod communities were located at the soil surface. The effect of plant litter quality varied according to each dominant tree species and was superimposed to soil effect. The lowest macrofauna abundance was associated with B. simaruba in the natural forest. T. heterophylla supported a much greater macrofauna community than the two other tree species studied at the same soil, and it appears likely that this is due to the palatability of its leaves compared with the other trees (low lignin, tannins, soluble phenols).
ISSN: 0178-2762

hal-00495371
https://hal.archives-ouvertes.fr/hal-00495371
https://hal.archives-ouvertes.fr/hal-00495371/document
https://hal.archives-ouvertes.fr/hal-00495371/file/Loranger-Merciris_et_al._2007.pdf
DOI : 10.1007/s00374-007-0199-5

Résumé : Arbol de hasta 10 m. Hojas lanceoladas u oblongo-lanceoladas, de 10 a 25 cm, acuminadas. Flores púrpura-pálidas, poco numerosas y en corimbos terminales; tubo del cáliz turbinado de 1 cm, lóbulos largos, redondeados; pétalos glandulosos de 1 a 1.5 cm. Fruto redondo u ovalado de 3 a 6 cm de largo, amarillo pálido.
Arbre pouvant atteindre 10 m. Feuilles lancéolées ou oblongues-lancéolées, de 10 à 25 cm, acuminées. Fleurs d’une couleur pourpre pâle, peu nombreuses et en corymbes terminaux; tube du calice turbiné de 1 cm, lobes longs, arrondis; pétales glanduleux de 1 à 1,5 cm. Fruit rond ou ovale de 3 à 6 cm de long, jaune pâle.
Evergreen tree up to 14 m high.  Leaves opposite, entire, glabrous, coriaceous, aromatic, pellucid dotted, petioles 2-3 cm long with swollen reddish base, blade elliptic, 7-13 x 3-6 cm, base cuneate, tip acuminate, mature leaves dark-green, shiny above, paler beneath; inflorescence terminal, 5 cm long of 3-20 flowers in paniculate cymes; flowers reddish; fruits a fleshy drupe 3 x 1.2cm, oblong-obovoid, dark red; seed oblong ca. 1.5 cm long. nb: angled peduncles and short pedicels ca 5 mm long constitute the clove stems of commerce.
Nativa de las islas Molucas, ampliamente cultivada.
Originaire des îles Moluques, cultivé dans de vastes zones.
Native to the Molucca Islands, widely cultivated.

http://www.tramil.net/fototeca/plant341

Résumé : La forêt tropicale humide guyanaise est située dans le grand ensemble Amazonien, qui est un point chaud des enjeux sur la biodiversité et la conservation des forêts tropicales. Une connaissance de l’âge et des taux d’accroissement des arbres est primordiale pour comprendre la dynamique de ces écosystèmes Cependant, l’absence de conditions hivernales sous les tropiques rend difficile la lecture de l’histoire dans les bois de ces forêts. En se plaçant dans le champ de l’anatomie fonctionnelle, cette thèse à caractère exploratoire avait pour but, à travers différentes approches, i) de suivre l’activité cambiale de quatre espèces ligneuses durant deux ans par prélèvements de micro-carottes, ii) de faire une étude dendrochronologique sur une espèce guyanaise, iii) d’utiliser la variation de la signature isotopique comme marqueur de croissance (ou d’histoire) et iv) de tester la pollution aérienne consécutive aux lancements de la fusée Ariane comme marqueurs de la croissance. L’examen bi-mensuel de l’activité cambiale a montré que tous les arbres présentent des alternances de quasi repos et de forte activité du cambium durant les deux années. Ces périodes de ralentissement ont été plus marquées chez Parkia nitida (décidue), Parkia velutina (décidue) et Schefflera morototoni (sempervirente). On observe donc des périodes de ralentissement de l’activité du cambium aussi bien chez deux espèces décidues que chez une espèce sempervirente. Il n’y a pas de patron universel de liaisons deux à deux entre pluviométrie intra-annuelle, phénologie de la feuillaison et activité cambiale même si des analogies fortes existent au cas par cas entre deux espèces pour une relation donnée. L’étude dendrochronologique chez Parkia nitida a mis en évidence la présence de cernes de croissance bien distincts et annuels. La limite de cerne se caractérise par une fine bande de parenchyme marginal renfermant de nombreux cristaux d’oxalate de calcium. A l’échelle de l’arbre, la croissance secondaire est homogène et elle est relativement synchrone au sein d’individus de cette espèce dans le même lieu. Cependant, l’influence des paramètres climatiques testés, comme la température et les précipitations, sur la croissance radiale annuelle est faible sur la période considérée. Ces deux premières études montrent que, dans le contexte de la Guyane française, la saisonnalité annuelle très marquée de la pluviométrie ne se traduit pas par un signal suffisamment fort pour synchroniser l’ensemble du fonctionnement des arbres. Néanmoins, elle influence clairement, au cas par cas soit la feuillaison, soit la floraison, soit la croissance cambiale. Les autres méthodes de marquage de la croissance (i.e. isotopie et chimie) entreprises demandent à être approfondies. Les bois des espèces de forêt tropicale humide se caractérisant en moyenne par un pourcentage élevé du plan ligneux occupé par les parenchymes axiaux, il serait important d’entreprendre une étude approfondie de leur rôle en tant qu’accumulateurs de substances potentiellement utiles pour la défense du bois dans l’arbre contre les xylophages. L’évolution dans le temps (périodicité, vieillissement chimique) des solutions de défense mises en place dans le bois est une piste intéressante pour la dendrochronologie
The rainforest of French Guiana is located in the Amazonian region, which is a hotspot of biodiversity, thus leading to several issues about conservation in tropical forests. Knowledge of the age and growth rate of trees is essential to understand the dynamics of these ecosystems. However, due to the lack of winter conditions it is difficult to read the story in the wood of these tropical forests. In the topic of functional anatomy, this thesis intends through different approaches i) to monitor the cambial activity of four tree species during two years sampling micro-cores, ii) to make a dendrochronological study on a Guyanese species iii) to use the variation of the isotopic signature as a marker of growth (or history) and iv) to test air pollution following launches of the Ariane rocket as markers of growth. The bi-monthly review of cambial activity showed that all trees have almost alternating rest and high activity of cambium in both years. These downturns have been more pronounced in Parkia nitida (deciduous), Parkia velutina (deciduous) and Schefflera morototoni (evergreen). We observe periods of cambial activity downturn in two deciduous species as well as in an evergreen species. There is no universal pattern of connections in pairs between rainfall intra-annual phenology of leafing and cambial activity although strong similarities exist in each case between two species for a given association. The dendrochronological study in Parkia nitida highlights the presence of distinct annual growth rings. The limit is characterized by a thin band of marginal parenchyma containing numerous crystals of calcium oxalate. At tree scale, secondary growth is homogeneous and relatively synchronous within individuals of this species in the same location. However, the influence of tested climatic parameters, such as temperature and precipitation on the annual radial growth, is low over the considered period. The first two studies showed that, in the environment of French Guiana, marked annual seasonality of rainfall does not affect in a strong way the behavior of the trees. Nevertheless, those rainfalls have an influence either on leafing, flowering or cambial growth. Other methods of marking growth (i.e. isotopic and chemical) intended require further investigations. Axial parenchyma represents a high average percentage in the wood of rainforest species: it could be important to investigate more precisely its role as accumulators of potentially useful substances involved in wood defense against borers. The evolution throughout time (periodicity, chemical aging) of defense mechanisms in woods is an interesting way for dendrochronology.

http://www.theses.fr/2013AGUY0605/document

Éditeur(s) : HAL CCSD Elsevier
Résumé : This study analyzes the records of several trace metals sensitive to redox conditions in continental shelf sediments off Concepcion, Chile (36 degrees S). The continental margin off Concepcion (36 S; 73 W) lies beneath an important upwelling center characterized by high primary production rates and, consequently, high fluxes of organic matter. In spring and summer, this material settles to the seafloor where it decays, producing periods of very low oxygen content in bottom waters (<1 mL L-1). In addition, an oxygen minimum zone develops at similar to 100-400 m water depth, where dissolved oxygen levels are <0.5 mL L-1. This situation changes during strong El Nino events, when dissolved oxygen at the bottom increases drastically (>1 mL L-1).;The goals of this study were to determine the input of trace metals to the sediment and to decipher how this information can be used to reveal variations in primary productivity or bottom oxygenation. Gravity cores collected at two stations - VG06-2 over the mid-shelf station (88 m water depth, upper boundary of the oxygen minimum zone) and VG06-3 over the outer shelf (120 m water depth, within the oxygen minimum zone) - were sampled for high resolution profiles (1 cm) of trace metals, biogenic opal, stable isotopes, and total organic carbon. The results suggest that the variability in the trace metal distribution on the continental shelf off Concepcion is determined by redox conditions and the organic carbon flux to the bottom. Some sections of the sediment cores from the outer shelf showed appreciable authigenic enrichment of U, Cd, and Mo (EF: 5-10, 2-5, and 10-16 respectively) along with heavier values of delta N-15, suggesting periods of suboxic conditions. During these periods, fluxes of organic material to the bottom were higher, as indicated by elevated TOC and opal contents. Alternating periods of higher and lower trace metal contents were not observed mid-shelf as they were on the outer shelf. Rather, the mid-shelf samples showed authigenic enrichment of U, Cd, and Mo (EF: 1-6, 4-5, and 10-20, respectively) throughout the core except in a 10-cm-thick gray layer. In general, authigenic enrichment of U. Mo, and Cd occurred at both sites, coincident with olive green layers in the cores. These layers were associated with periods of elevated primary productivity and suboxic conditions. Such periods did not seem to last as long as the oxygenated periods, which had higher inputs of refractive detrital material, coincident with the occurrence of distinct gray sediment layers.
ISSN: 0079-6611

hal-00682159
https://hal.archives-ouvertes.fr/hal-00682159
DOI : 10.1016/j.pocean.2011.07.010