Quilliet A.S. (2005). Etude spatiale des euphausiacés Euphausia crystallorophias et thysanoessa macrura dans la zone côtière de Terre Adélie. MASTER « Environnement Naturel + Qualité de l’Air »-2ème année. Université du Littoral et de la Côte d’Opale.
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Jaeger A. (2006). Caractérisation de l'environnement océanographique des zones d'alimentation d'un prédateur marin: le manchot adélie. Master 2 'mention sciences de l'univers, environnement, écologie – spécialité océanographie et environnement marin. Université Paris VI..
Abstract: en codirection avec le CEBC
Programme: 281
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Ceyssat D.
. (2005). Expression génique des systèmes protéolytiques musculaires lors du jeûne prolongé chez le manchot Adélie : possible implication dans le signal de réalimentation..
Abstract: Master II "physiologie intégrée en conditions extrêmes" – Année 2004-2005 – Université Claude
Programme: 137
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Santin-Janin H. (2006). Rapport de recherche du Master “Ecologie, Evolution, Biométrie”. Université C. Bernard Lyon1, 55 pages..
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Duneau, D. (2006). Effets en cascades dans les systèmes à vecteurs: le cas de la bactérie Borrelia burdgorferi sensu lato chez les oiseaux marins. Rapport de Master 2 BEE, Université Montpellier II..
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GLOBALVIEW-CO2: Cooperative Atmospheric Data Integration Project - CarbonDioxide. (2005). GLOBALVIEW-CO2: Cooperative Atmospheric Data Integration Project – CarbonDioxide..
Abstract: CD-ROM, NOAA CMDL, Boulder, Colorado [Also available on
Internet via anonymous FTP to ftp.cmdl.noaa.gov, Path:
ccg/co2/GLOBALVIEW]
Programme: 439
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D. Delille, A. Duval, E. Pelletier. (2008). Highly efficient pilot biopiles for on-site fertilization treatment of diesel oil-contaminated sub-Antarctic soil (Vol. 54).
Abstract: In order to determine the efficiency of on-site bioremediation of diesel contaminated subAntarctic soils, a pilot biopiles study was initiated in January 2006 with a selected soil of The Grande Terre (Kerguelen Archipelago, 69° 42′E–49° 19′S). Each 4 kg biopile received 180 g of diesel fuel and several of them were submitted to different treatments. All biopiles were sampled on a regular basis over a one-year period. A highly efficient biodegradation was observed in all piles. Analytical results show that less than 7% of total petroleum hydrocarbons (TPH) remained after one year in biopiles not treated with fertilizers. This proportion decreases to less than 0.2% in biopiles treated with fish compost. These biopiles revealed to be 100 times more efficient than previously reported in situ bioremediation study conducted under similar weather conditions with the same concentrations of similar fertilizers. After one year, a significantly larger amount of polycyclic aromatic hydrocarbons (PAH) was present in fertilized biopiles without a physical treatment compared to ventilated or agitated ones. Although biopiles were highly efficient to reduce TPH concentrations well below the target concentration of 100 ppm, a residual toxicity determined with Microtox assay was observed in a number of biopiles treated with fish compost.
Keywords: Bioremediation agent Diesel fuel Sub-Antarctic soils Toxicity
Programme: 193
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Alexis Chaigneau, Rosemary A. Morrow, Stephen R. Rintoul. (2004). Seasonal and interannual evolution of the mixed layer in the Antarctic Zone south of Tasmania (Vol. 51).
Abstract: Seasonal and interannual variations of the mixed layer properties in the Antarctic Zone (AZ) south of Tasmania are described using 7 WOCE/SR3 CTD sections and 8 years of summertime SURVOSTRAL XBT and thermosalinograph measurements between Tasmania and Antarctica. The AZ, which extends from the Polar Front (PF) to the Southern Antarctic Circumpolar Current Front (SACCF), is characterized by a 150m deep layer of cold Winter Water (WW) overlayed in summer by warmer, fresher water mass known as Antarctic Surface Water (AASW). South of Tasmania, two branches of the PF divide the AZ into northern and southern zones with distinct water properties and variability. In the northern AZ (between the northern and southern branches of the PF), the mixed layer depth (MLD) is fairly constant in latitude, being 150m deep in winter and around 40–60m in summer. In the southern AZ, the winter MLD decreases from 150m at the S-PF to 80m at the SACCF and from 60 to 35m in summer. Shallower mixed layers in the AZ-S are due to the decrease in the wind speed and stronger upwelling near the Antarctic Divergence. The WW MLD oscillates by ±15m around its mean value and modest interannual changes are driven by winter wind stress anomalies. The mixed layer is on annual average 1.7°C warmer, 0.06 fresher and 0.2kgm−3 lighter in the northern AZ than in the southern AZ. The Levitus (1998) climatology is in agreement with the observed mean summer mixed layer temperature and salinity along the SURVOSTRAL line but underestimates the MLD by 10–20m. The winter MLD in the climatology is also closed to that observed, but is 0.15 saltier than the observations along the AZ-N of the SR3 line. MLD, temperature and density show a strong seasonal cycle through the AZ while the mixed layer salinity is nearly constant throughout the year. During winter, the AZ MLD is associated with a halocline while during summer it coincides with a thermocline. Interannual variability of the AZ summer mixed layer is partly influenced by large scale processes such as the circumpolar wave which produces a warm anomaly during the summer 1996–1997, and partly by local mechanisms such as the retroflection of the S-PF which introduces cold water across the AZ-N.
Keywords: Antarctic zone Surface and subsurface water masses Surface mixed layer Temporal variations
Programme: 694
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Bailleul F. (2006). Deux mille mètres sous les mers – Stratégies d'acquisition des ressources et réponses comportementales des éléphants de mer de Kerguelen aux structures physiques de l'Océan Austral. Thèse de doctorat, Université La Rochelle..
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Silvia Galli. (2007). Bolometric interferometry demonstrator to measure the Cosmic Microwave Background Polarization.
Abstract: report of a Master degree, advisor Michel Piat
Programme: 915
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