Global compilation of benthic data sets I

Approaches to quantify the organic carbon accumulation on a global scale generally do not consider the small-scale variability of sedimentary and oceanographic boundary conditions along continental margins. In this study, we present a new approach to regionalize the total organic carbon (TOC) content in surface sediments (<5 cm sediment depth). It is based on a compilation of more than 5500 single measurements from various sources. Global TOC distribution was determined by the application of a combined qualitative and quantitative-geostatistical method. Overall, 33 benthic TOC-based provinces were defined and used to process the global distribution pattern of the TOC content in surface sediments in a 1°x1° grid resolution. Regional dependencies of data points within each single province are expressed by modeled semi-variograms. Measured and estimated TOC values show good correlation, emphasizing the reasonable applicability of the method. The accumulation of organic carbon in marine surface sediments is a key parameter in the control of mineralization processes and the material exchange between the sediment and the ocean water. Our approach will help to improve global budgets of nutrient and carbon cycles.

Implication du glutamate 346 de NHE1 dans le transport du Na⁺ et l'interaction avec les inhibiteurs

Thèse numérisée par la Direction des bibliothèques de l'Université de Montréal.

Implication du glutamate 346 de NHE1 dans le transport du Na⁺ et l'interaction avec les inhibiteurs

Thèse numérisée par la Direction des bibliothèques de l'Université de Montréal.

Clay mineralogy of South Atlantic surface sediments

Surface samples, mostly from abyssal sediments of the South Atlantic, from parts of the equatorial Atlantic, and of the Antarctic Ocean, were investigated for clay content and clay mineral composition. Maps of relative clay mineral content were compiled, which improve previous maps by showing more details, especially at high latitudes. Large-scale relations regarding the origin and transport paths of detrital clay are revealed. High smectite concentrations are observed in abyssal regions, primarily derived from southernmost South America and from minor sources in Southwest Africa. Near submarine volcanoes of the Antarctic Ocean (South Sandwich, Bouvet Island) smectite contents exhibit distinct maxima, which is ascribed to the weathering of altered basalts and volcanic glasses. The illite distribution can be subdivided into five major zones including two maxima revealing both South African and Antarctic sources. A particularly high amount of Mg- and Fe-rich illites are observed close to East Antarctica. They are derived from biotite-bearing crystalline rocks and transported to the west by the East Antarctic Coastal Current. Chiorite and well-crystallized dioctaedral illite are typical minerals enriched within the Subantarctic and Polarfrontal-Zone but of minor importance off East Antarctica. Kaolinite dominates the clay mineral assemblage at low latitudes, where the continental source rocks (West Africa, Brazil) are mainly affected by intensive chemical weathering. Surprisingly, a slight increase of kaolinite is observed in the Enderby Basin and near the Filchner-Ronne Ice shelf. The investigated area can be subdivided into ten, large-scale clay facies zones with characteristic possible source regions and transport paths. Clay mineral assemblages of the largest part of the South Atlantic, especially of the western basins are dominated by chlorite and illite derived from the Antarctic Peninsula and southernmost South America and supported by advection within the Circumantarctic Deep Water flow. In contrast, the East Antarctic provinces are relatively small. Assemblages of the eastern basins north of 30°S are strongly influenced by African sources, controlled by weathering regimes on land and by a complex interaction of wind, river and deep ocean transport. The strong gradient in clay mineral composition at the Brazilian slope indicate a relatively low contribution of tropically derived assemblages to the western basins.

Calcium carbonate content in surface sediments and benthic fauna on Antarctic shelves

We analyzed 214 new core-top samples for their CaCO3 content from shelves all around Antarctica in order to understand their distribution and contribution to the marine carbon cycle. The distribution of sedimentary CaCO3 on the Antarctic shelves is connected to environmental parameters where we considered water depth, width of the shelf, sea-ice coverage and primary production. While CaCO3 contents of surface sediments are usually low, high(> 15%) CaCO3 contents occur at shallow water depths (150-200 m) on narrow shelves of the eastern Weddell Sea and at a depth range of 600-900 m on the broader and deeper shelves of the Amundsen, Bellingshausen and western Weddell Seas. Regions with high primary production, such as the Ross Sea and the western Antarctic Peninsula region, have generally low CaCO3 contents in the surface sediments. The predominant mineral phase of CaCO3 on the Antarctic shelves is low-magnesium calcite. With respect to ocean acidification, our findings suggest that dissolution of carbonates in Antarctic shelf sediments may be an important negative feedback only after the onset of calcite undersaturation on the Antarctic shelves. Macrozoobenthic CaCO3 standing stocks do not increase the CaCO3 budget significantly as they are two orders of magnitude lower than the budget of the sediments. This first circumpolar compilation of Antarctic shelf carbonate data does not claim to be complete. Future studies are encouraged and needed to fill data gaps especially in the under-sampled southwest Pacific and Indian Ocean sectors of the Southern Ocean.

Understandings of transnational families in debates on Migration and development

International migration sets in motion a range of significant transnational processes that connect countries and people. How migration interacts with development and how policies might promote and enhance such interactions have, since the turn of the millennium, gained attention on the international agenda. The recognition that transnational practices connect migrants and their families across sending and receiving societies forms part of this debate. The ways in which policy debate employs and understands transnational family ties nevertheless remain underexplored. This article sets out to discern the understandings of the family in two (often intermingled) debates concerned with transnational interactions: The largely state and policydriven discourse on the potential benefits of migration on economic development, and the largely academic transnational family literature focusing on issues of care and the micro-politics of gender and generation. Emphasizing the relation between diverse migration-development dynamics and specific family positions, we ask whether an analytical point of departure in respective transnational motherhood, fatherhood or childhood is linked to emphasizing certain outcomes. We conclude by sketching important strands of inclusions and exclusions of family matters in policy discourse and suggest ways to better integrate a transnational family perspective in global migration-development policy.

Utilização de minhocas (Eisenia fetida Savigny, 1826) na alimentação de achigãs (Micropterus salmoides, Lacépède, 1802) - resultados preliminares

A minhoca (Eisenia fetida Savigny, 1826) é uma boa fonte de proteína. O elevado teor em humidade (82,80% ±2,128) e cinzas (10,70% ±2,345), principalmente terra, poderão ser um fator limitante à sua utilização como alimento para peixes. Com o objetivo de avaliar o interesse da utilização de E. fetida na alimentação de peixes, em 23 setembro 2014 foram capturados 22 juvenis de achigã (Micropterus salmoides Lacépède, 1802) (0+ anos) numa pequena barragem de rega Os achigãs foram colocados em três aquários para habituação a um alimentos compostos comercial. Três semanas depois 86,4% já ingeriam o alimento. A taxa de sobrevivência foi de 100%. Em 13 outubro 2014 foram escolhidos aleatoriamente 16 achigãs e colocados em dois aquários (8 peixes/aquário; 0,048 m3 de água). Os valores médios iniciais de peso, comprimento, fator K e densidade foram semelhantes nosdois aquários. No aquário G1 (minhocas) e aquário G2 (alimento composto) o peso, o comprimento, o fator K e a densidade iniciais foram, respetivamente, 13,62 g (±3,171) e 13,40 g (±3,002) (P>0,05); 10,49 cm (±0,757) e 10,39 cm (±0,649) (P>0,05); 1,160 (±0,043) e 1,179 (±0,082) (P>0,05); 2,27 kg/m3 e 2,23 kg/m3. No nosso estudo laboratorial a temperatura média da água variou entre 19,9ºC e 16,8ºC. Como em Portugal não se produzem alimentos específicos para achigãs foi utilizado um alimento composto comercial formulado para douradas (Sparus aurata L., 1758) e robalos (Dicentrarchus labrax L., 1758) (proteína 49,74%MS; gordura 18,07%MS; cinzas 11,57%MS; fibra bruta 0,84%MS; humidade 6,55%). No dia 88 do estudo (09 janeiro 2015) os valores médios de peso, comprimento, fator K e densidade nos aquários G1 e G2 foram, respetivamente, 17,57 g (±4,071) e 19,19 g (±4.811) (P<0,05); 10,88 cm (±0,875) e 11,29 cm (±0,871) (P<0,05); 1,346 (±0,051) e 1,311 (±0,061) (P>0,05); 2,93 kg/m3 e 3,20 kg/m3). Os resultados obtidos até agora parecem indicar que a E. fetida pode ser utilizada na alimentação de achigãs.

The effectiveness of using a simple ARIA based geographical classification to identify road crash patterns in rural and urban areas of Queensland

Research has noted a ‘pronounced pattern of increase with increasing remoteness' of death rates in road crashes. However, crash characteristics by remoteness are not commonly or consistently reported, with definitions of rural and urban often relying on proxy representations such as prevailing speed limit. The current paper seeks to evaluate the efficacy of the Accessibility / Remoteness Index of Australia (ARIA+) to identifying trends in road crashes. ARIA+ does not rely on road-specific measures and uses distances to populated centres to attribute a score to an area, which can in turn be grouped into 5 classifications of increasing remoteness. The current paper uses applications of these classifications at the broad level of Australian Bureau of Statistics' Statistical Local Areas, thus avoiding precise crash locating or dedicated mapping software. Analyses used Queensland road crash database details for all 31,346 crashes resulting in a fatality or hospitalisation occurring between 1st July, 2001 and 30th June 2006 inclusive. Results showed that this simplified application of ARIA+ aligned with previous definitions such as speed limit, while also providing further delineation. Differences in crash contributing factors were noted with increasing remoteness such as a greater representation of alcohol and ‘excessive speed for circumstances.' Other factors such as the predominance of younger drivers in crashes differed little by remoteness classification. The results are discussed in terms of the utility of remoteness as a graduated rather than binary (rural/urban) construct and the potential for combining ARIA crash data with census and hospital datasets.