Mineralogy of sea-floor surface sediments, Sonne cruise SO202/1 to the North Pacific and Bering Sea

During expedition 202 of research vessel SONNE in 2009, 39 sea-floor surface sediments were sampled over a wide area across the North Pacific and the Bering Sea, which are well suited as reference archives of modern environmental processes. In this study, we used the samples to infer the documentation of land-ocean linkages of terrigenous sediment supply. We followed an integrated approach of grain-size analysis, bulk mineralogy, and clay mineralogy in combination with statistical data evaluation (end-member modelling of grain-size data, fuzzy-cluster analysis of mineralogical data), in order to identify the significant sources and modes of sediment transport in an overregional context. We also compiled literature data on clay mineralogy and updated those with the new data. Today, two processes of terrigenous sediment supply prevail in the study area: far-distant aeolian sediment supply to the pelagic North Pacific as well as hemipelagic sediment dispersal from nearby land sources by ocean currents along the continental margins and island arcs of the study area. The aeolian particles show the finest grain sizes (clay and fine silt), while the hemipelagic sediments have high abundances of sortable silt, particles >10 microns.

A critical review of both the synthesis approach and the receptor profile of the 8-chloro-1-(2′,4′-dichlorophenyl)-N-piperidin-1-yl-1,4,5,6-tetrahydrobenzo[6,7]cyclohepta[1,2-c]pyrazole-3-carboxamide and analogue derivatives

We thank European Commission (project “PET BRAIN: Mapping the brain with PET radiolabeled cannabinoid CB1 ligands”; FP7-People-2009-IAPP; Grant Agreement N.25142).

(Table 1) Peak intensity of minerals in ODP Hole 126-793B

Sediments and rocks recovered during Ocean Drilling Program Leg 126 at Sites 792 and 793 in the Izu-Bonin forearc basin are described with a primary focus on clay mineralogy. Evidence for diagenetic hydrothermal alteration processes is present in the upper Oligocene to lower Miocene sediments at these sites. The vitric and pumiceous sand/sandstone and pumiceous gravel contain high concentrations of smectites, zeolites, and gypsum. Microscopic observations show that the volcanic glass and feldspars have been altered to smectites and zeolites. The authigenic mineral assemblages indicate that these minerals resulted from precipitation from circulating fluids, as well as from the alteration of glass and feldspar under temperature conditions that may have reached 200°-300°C. Mineral assemblages in microfractures display thermal gradients that possibly reflect cooling effects.

(Table 1) Stable isotope record of Middle Cretaceous benthic foraminifera

Preservation of planktic foraminiferal calcite has received widespread attention in recent years, but the taphonomy of benthic foraminiferal calcite and its influence on the deep-sea palaeotemperature record have gone comparatively unreported. Numerical modeling indicates that the carbonate recrystallization histories of deep-sea sections are dominated by events in their early burial history, meaning that the degree of exchange between sediments and pore fluids during the early postburial phase holds the key to determining the palaeotemperature significance of diagenetic alteration of benthic foraminifera. Postburial sedimentation rate and lithology are likely to be important determinants of the paleoceanographic significance of this sediment-pore fluid interaction. Here we report an investigation of the impact of extreme change in sedimentation rate (a prolonged and widespread Upper Cretaceous hiatus in the North Atlantic Ocean) on the preservation and d18O of benthic foraminifera of Middle Cretaceous age (nannofossil zone NC10, uppermost Albian/lowermost Cenomanian, ~99 Ma ago) from multiple drill sites. At sites where this hiatus immediately overlies NC10, benthic foraminifera appear to display at least moderate preservation of the whole test. However, on closer inspection, these tests are shown to be extremely poorly preserved internally and yield d18O values substantially higher than those from contemporaneous better preserved benthic foraminifera at sites without an immediately overlying hiatus. These high d18O values are interpreted to indicate alteration close to the seafloor in cooler waters during the Late Cretaceous hiatus. Intersite differences in lithology modulate the diagenetic impact of this extreme change in sedimentation rate. Our results highlight the importance of thorough examination of benthic foraminiferal wall structures and lend support to the view that sedimentation rate and lithology are key factors controlling the paleoceanographic significance of diagenetic alteration of biogenic carbonates.

Magnetic and petrographic properties of ODP Site 120-747 (Table 1)

Carbonate sediments from the Kerguelen Plateau (ODP Leg 120) of Eocene to Pliocene age were investigated with rock magnetic, petrographic and geochemical methods to determine the carriers of remanent magnetization. Magnetic methods showed that the major magnetic minerals were titanomagnetites slightly larger than single domain particles. Submicrometre to micrometre-size grains of titanomagnetite were identified as inclusions in volcanic glass particles or as crystals in lithic clasts. Volcanic fallout ash particles formed the major fraction of the magnetic extract from each sediment sample. Three groups of volcanic ashes were identified: trachytic ashes, basaltic ashes with sideromelane and tachylite shards, and palagonitic ashes. These three groups could be equally well defined based on their magnetic hysteresis properties and alternating field demagnetization curves. The highest coercivities of all samples were found for the tachylite, due to the submicrometre-size titanomagnetite inclusions in the matrix. Trachytic ashes had intermediate magnetic properties between the single-domain-type tachylites and the palagonitic (altered) basaltic ashes with low coercivities. Samples which contained mixtures of these different volcanic ashes could be distinguished from the three types of ashes based on their magnetic characteristics. There was neither evidence of biogenic magnetofossils in the transmission electron micrographs nor did we find magnetic particles derived from continental Antarctica. The presence of dispersed volcanic fallout ashes between visible ash layers suggests continuous explosive volcanic activity on the Kerguelen Plateau in the South Indian Ocean since the early Eocene. The continuous fallout of volcanic ash from explosive volcanism on the Kerguelen Archipelago is the source of the magnetic particles and thus responsible for the magnetostratigraphy of the nannofossil oozes drilled during Leg 120.

(Table 1) Age determination of sediment cores F2-92-P3 and F2-92-P40

Although climate records from several locations around the world show nearly synchronous and abrupt changes, the nature of the inferred teleconnection is still poorly understood. On the basis of preserved laminations and molybdenum enrichments in open margin sediments we demonstrate that the oxygen content of northeast Pacific waters at 800 m depth during the Bölling-Alleröd warm period (15-13 kyr) was greatly reduced. Existing oxygen isotopic records of benthic and planktonic foraminifera suggest that this was probably due to suppressed ventilation at higher latitudes of the North Pacific. Comparison with ventilation records for the North Atlantic indicates an antiphased pattern of convection relative to the North Pacific over the past 22 kyr, perhaps due to variations in water vapor transport across Central America.

Preparation and characterization of Pr0.6Sr0.4FeO3-δ-Ce0.9Pr0.1O2-δ nanofiber structured composite cathode for IT-SOFCs

In this work, Pr_0.6Sr_0.4FeO_3-δ -Ce_0.9Pr_0.1O_2-δ (PSFO-CPO) nanofibers were synthesized by a one-step electrospin technique for use in intermediate-temperature solid oxide fuel cell (IT-SOFC) applications. PSFO-CPO nanofibers were produced with a diameter of about 100nm and lengths exceeding tens of microns. The thermal expansion coefficient (TEC) matches with standard GDC electrolytes and the resulting conductivity also satisfies the needs of IT-SOFCs cathodes. EIS analysis of the nanofiber structured electrode gives a polarization resistance of 0.072Ωcm² at 800°C, smaller than that from the powdered cathode with the same composition. The excellent electrochemical performance can be attributed to the well-constructed microstructure of the nanofiber structured cathode, which promotes surface oxygen diffusion and charge transfer processes. All the results imply that the one-step electrospin method is a facile and practical way of improving the cathode properties and that PSFO-CPO is a promising cathode material for IT-SOFCs.

Phiêu sinh vat trong vinh Nha Trang 1: Khuê tào: Bacillariales

This paper deals with the work performed at the Department of Zoology of the Faculty of Sciences in Saigon on planktonic material, collected in the Bay of Nhatrang, Central Vietnam. After preliminary considerations on the physical factors relating to plankton life in the Bay, the materials and methods are described. Follows a list of the planktonic organisms studied and identified, and the descriptions of 154 species of diatoms, containing mostly planktonic species mixed with a few benthic species. This is the first of a series of papers dealing with plankton organisms recorded in the Bay of Nhatrang. As it is intended to be a tool for Marine Biology students as well as interested, beginners, the systematic and descriptive characteristics have been reduced to a minimum. Stress was on making detailed and clear illustrations of the organisms described.

Le traitement nutritionnel des épisodes d'hypoglycémie dans le diabète de type 1

Les patients atteints de diabète de type 1 (DbT1) semblent sur-traiter leurs hypoglycémies par rapport aux recommandations des Lignes directrices Canadiennes en diabète. Objectifs : 1) Décrire les habitudes des patients DbT1 pour le traitement des hypoglycémies et estimer les impacts sur le profil de risque cardio-métabolique et 2) explorer les excursions glycémiques suite à un traitement d’hypoglycémie qui respecte les recommandations. Méthodologie (analyses secondaires) : Objectif 1 : 121 patients DbT1 ont complété un journal alimentaire et de glycémies de 48 h. Des variables cardio-métaboliques ont été mesurées et un questionnaire sur la peur des hypoglycémies a été complété. Objectif 2 : 57 patients DbT1 ont complété les bras contrôles de notre programme sur le pancréas artificiel (traitement des hypoglycémies standardisé). Les valeurs de glycémie étaient disponibles aux 5 minutes. Résultats : Projet 1 : Les patients ont fait en moyenne 1,45 hypoglycémies/jour et 73% sur-traitaient avec une consommation moyenne de glucides de 32 ± 24 g. Ce sur-traitement est associé avec un plus jeune âge et une peur des hypoglycémies plus importante, mais pas avec un profil de risque cardio-métabolique plus défavorable. Projet 2 : Dans 20% des cas, traiter une hypoglycémie avec 15 g de glucides était efficace pour ramener la glycémie ≥ 4,0 mmol/L en 15 minutes, le temps moyen étant de 24 ± 12 minutes. La proportion d’insuline basale, le temps depuis le dernier repas et la pratique d’activité physique sont les éléments qui semblent avoir le plus d’impact sur l’efficacité du traitement. Conclusion : L’éducation entourant le traitement des hypoglycémies a besoin d’être renforcée et d’autres études sont nécessaires afin de valider les recommandations.

Le traitement nutritionnel des épisodes d'hypoglycémie dans le diabète de type 1

Les patients atteints de diabète de type 1 (DbT1) semblent sur-traiter leurs hypoglycémies par rapport aux recommandations des Lignes directrices Canadiennes en diabète. Objectifs : 1) Décrire les habitudes des patients DbT1 pour le traitement des hypoglycémies et estimer les impacts sur le profil de risque cardio-métabolique et 2) explorer les excursions glycémiques suite à un traitement d’hypoglycémie qui respecte les recommandations. Méthodologie (analyses secondaires) : Objectif 1 : 121 patients DbT1 ont complété un journal alimentaire et de glycémies de 48 h. Des variables cardio-métaboliques ont été mesurées et un questionnaire sur la peur des hypoglycémies a été complété. Objectif 2 : 57 patients DbT1 ont complété les bras contrôles de notre programme sur le pancréas artificiel (traitement des hypoglycémies standardisé). Les valeurs de glycémie étaient disponibles aux 5 minutes. Résultats : Projet 1 : Les patients ont fait en moyenne 1,45 hypoglycémies/jour et 73% sur-traitaient avec une consommation moyenne de glucides de 32 ± 24 g. Ce sur-traitement est associé avec un plus jeune âge et une peur des hypoglycémies plus importante, mais pas avec un profil de risque cardio-métabolique plus défavorable. Projet 2 : Dans 20% des cas, traiter une hypoglycémie avec 15 g de glucides était efficace pour ramener la glycémie ≥ 4,0 mmol/L en 15 minutes, le temps moyen étant de 24 ± 12 minutes. La proportion d’insuline basale, le temps depuis le dernier repas et la pratique d’activité physique sont les éléments qui semblent avoir le plus d’impact sur l’efficacité du traitement. Conclusion : L’éducation entourant le traitement des hypoglycémies a besoin d’être renforcée et d’autres études sont nécessaires afin de valider les recommandations.

DNA 93-1

Combined media on photographic paper. 40" x 30"