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Díaz A., Poulin E. & A. Mansilla. (2016). Efecto de las glaciaciones del cuaternario en la historia evolutiva del caracol endémico del océano austral neobuccinum eatoni.
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Poulin E., González-Wevar C.A., Díaz A., Hüne M., Gérard K. & J. Naretto. (2016). Biogeografía en el Océano Austral: ¿es el frente polar una barrera efectiva entre las Provincias Antárticas y Subantárticas?.
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. (2014). Polar Front around the Kerguelen Islands: An up?to?date determination and associated circulation of surface/subsurface waters (Vol. 119).
Keywords: Kerguelen Polar Front Southern Ocean
Programme: 688
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Christopher S. Watson, Neil J. White, John A. Church, Matt A. King, Reed J. Burgette, Benoit Legresy. (2015). Unabated global mean sea-level rise over the satellite altimeter era (Vol. 5).
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Féral J-P, Saucède T & Améziane N. (2016). Un observatoire sous-marin des effets du changement global sur les communautés benthiques côtières de l’Archipel des Kerguelen. PROTEKER phase 1, l’installation.
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Koubbi P, Guinet C, Alloncle N, Ameziane N, Azam CS, Baudena A, Bost CA, Causse R, Chazeau C, Coste G, Cotté C, D'Ovidio F, Delord K, Duhamel G, Forget A, Gasco N, Hautecœur M, Lehodey P, Lo Monaco C, Marteau C, Martin A, Mignard C, Pruvost P, Saucède T, Sinegre R, Thellier T, Verdier AG, Weimerskirch H. (2016). Ecoregionalisation of the Kerguelen and Crozet islands oceanic zone. Part I: Introduction and Kerguelen oceanic zone.
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Saucède T & Marty G. (2016). Un observatoire des écosystèmes marins côtiers des Iles Kerguelen (Proteker).
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L. Testut, A.s. Unnikrishnan. (2015). Improving Modeling of Tides on the Continental Shelf off the West Coast of India.
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. (2016). Water cycle and salinity dynamics in the mangrove forests of Europa and Juan de Nova Islands, southwest Indian Ocean (Vol. 30).
Abstract: Rationale The functioning of mangrove forests found on small coralline islands is characterized by limited freshwater inputs. Here, we present data on the water cycling of such systems located on Europa and Juan de Nova Islands, Mozambique Channel. Methods In order to better understand the water cycle and mangrove growth conditions, we have analysed the hydrological and salinity dynamics of the systems by gauge pressure and isotopic tracing (?18O and ?2H values). Results Both islands have important seawater intrusion as measured by the water level change and the high salinities in the karstic ponds. Europa Island displays higher salinity stress, with its inner lagoon, but presents a pluri?specific mangrove species formation ranging from shrub to forest stands. No freshwater signal could be detected around the mangrove trees. On Juan de Nova Island, the presence of sand and detrital sediment allows the storage of some amount of rainfall to form a brackish groundwater. The mangrove surface area is very limited with only small mono?specific stands being present in karstic depression. Conclusions On the drier Europa Island, the salinity of all the water points is equal to or higher than that of the seawater, and on Juan de Nova the groundwater salinity is lower (5 to 20 PSU). This preliminary study shows that the karstic pothole mangroves exist due to the sea connection through the fractured coral and the high tidal dynamics. Copyright ? 2015 John Wiley & Sons, Ltd.
Programme: 688
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Boulinier, T. (2016). Infectious diseases as a threat to albatrosses and petrels: from basic immuno-ecology to perspectives for conservation..
Abstract: Oral communication at Labex CEMEB Workshop on the Ecology of Host-Microorganisms Interactions, Montpellier, November 2016
Programme: 1151
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