Tongass National Forest : hearing before the Subcommittee on Public Lands, National Parks, and Forests of the Committee on Energy and Natural Resources, United States Senate, One Hundred First Congress, first session, on S. 237 ... S. 346.

"February 28, 1989"--Pt. 1.

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.

Estimation of sea surface temperature from sediment core PS1768-8

The quantitative diatom analysis of 218 surface sediment samples recovered in the Atlantic and western Indian sector of the Southern Ocean is used to define a base of reference data for paleotemperature estimations from diatom assemblages using the Imbrie and Kipp transfer function method. The criteria which justify the exclusion of samples and species out of the raw data set in order to define a reference database are outlined and discussed. Sensitivity tests with eight data sets were achieved evaluating the effects of overall dominance of single species, different methods of species abundance ranking, and no-analog conditions (e.g., Eucampia Antarctica) on the estimated paleotemperatures. The defined transfer functions were applied on a sediment core from the northern Antarctic zone. Overall dominance of Fragilariopsis kerguelensis in the diatom assemblages resulted in a close affinity between paleotemperature curve and relative abundance pattern of this species downcore. Logarithmic conversion of counting data applied with other ranking methods in order to compensate the dominance of F. kerguelensis revealed the best statistical results. A reliable diatom transfer function for future paleotemperature estimations is presented.

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.

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.

Resolución 048 del 09 de enero de 2013: Por la cual se resuelve un recurso de apelación

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Resolución 048 del 30 de mayo de 2013: Por la cual se niega solicitud de impugnación de actas

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