Organic carbon in waters, suspended matter, and upper layer bottom sediments of the Kara Sea and Obskay Guba

Along three sections in the Kara Sea and Obskaya Guba concentrations of dissolved and particulate organic carbon (DOC and POC, respectively) in waters , as well as of organic carbon in bottom sediments (Corg) in September-October 2007 were determined. DOC varied from 6.3 to 2400 µg/l, POC - from 0.84 to 12.2 mg/l. For all samples the average DOC was 200 µg/l (n = 78; sigma = 368), the average POC - 2.7 mg/l (n = 92; sigma = 2.7). Concentrations of Corg in dried samples of upper layer bottom sediments varied from 0.13 to 2.10% (aver. = 0.9%; n = 21; sigma = 0.49%). It is shown that distribution of different forms of organic matter (OM) is an indicator of supply and scattering of particulate matter in the Kara Sea and that DOC and POC of the Kara Sea are formed under impact of runoff of the Ob and Yenisei Rivers. It is found that distribution of OM in bottom sediments is closely related to their grain size composition and to the structure of currents in the area. Variations in Corg concentration in bottom sediment cores from the zone of riverine and sea water mixing represent variability of OM burial.

Sea ice cover, and bottom water and sediment characteristics at stations in the Amundsen Gulf, Canada

Seasonal dynamics in the activity of Arctic shelf benthos have been the subject of few local studies, and the pronounced among-site variability characterizing their results makes it difficult to upscale and generalize their conclusions. In a regional study encompassing five sites at 100-595 m water depth in the southeastern Beaufort Sea, we found that total pigment concentrations in surficial sediments, used as proxies of general food supply to the benthos, rose significantly after the transition from ice-covered conditions in spring (March-June 2008) to open-water conditions in summer (June-August 2008), whereas sediment Chl a concentrations, typical markers of fresh food input, did not. Macrobenthic biomass (including agglutinated foraminifera >500 µm) varied significantly among sites (1.2-6.4 g C/m**2 in spring, 1.1-12.6 g C/m**2 in summer), whereas a general spring-to-summer increase was not detected. Benthic carbon remineralisation also ranged significantly among sites (11.9-33.2 mg C/m**2/day in spring, 11.6-44.4 mg C/m**2/day in summer) and did in addition exhibit a general significant increase from spring-to-summer. Multiple regression analysis suggests that in both spring and summer, sediment Chl a concentration is the prime determinant of benthic carbon remineralisation, but other factors have a significant secondary influence, such as foraminiferan biomass (negative in both seasons), water depth (in spring) and infaunal biomass (in summer). Our findings indicate the importance of the combined and dynamic effects of food supply and benthic community patterns on the carbon remineralisation of the polar shelf benthos in seasonally ice-covered seas.

Clay minerals in bottom sediments of the St. Anna Trough

This paper is devoted to studies of clay minerals from two cores collected in the northern and central regions of the St. Anna Trough, the largest trough of the Kara Sea. Upper Quaternary glacial, glaciomarine, and marine deposits are characterized by various contents of kaolinite, chlorite, illite, and smectite. It is established that, from older to younger deposits, amounts of kaolinite and chlorite generally decrease, while those of illite and smectite, on the contrary, increase. A joint analysis of distributions of clay and heavy minerals over the section allowed us to refine position of sources for terrigenous matter and their temporal variability. It is shown changes in sources of supply were directly related to climate changes that occurred when passing from glacial to marine sedimentation environments.

Living benthic foraminifers in bottom sediments of the southeastern Kandalaksha Bay (White Sea)

Analysis of composition and distribution of benthic foraminifers in six samples of bottom sediments obtained in the southeast Kandalaksha Bay of the White Sea at water depths of 20 to 155 m revealed their dependence on lithology and different hydrological characteristics. It is shown that living foraminifers populating relatively shallow areas of the bay (20-60 m), which are bathed by seasonally warmed intermediate water with temperature 0.7-1.5°C and salinity 26 per mil, are characterized by high abundance (250-750 specimens/10 ccm of wet sediment) and prevalence of agglutinated species (Eggerella advena, Recurvoides turbinatus, and others). Deeper (155 m) where cold and relatively saline deep water occurs (-1.4°C, 29.5 per mil), abundance is an order lower (30 specimens/10 ccm) and is dominated by calcareous taxa Cassidulina reniforme, an Arctic cold resistant species.

Antropología de las relaciones transnacionales en las regiones de frontera. El caso de la Triple Frontera entre Argentina, Brasil, Paraguay. 16H363

La triple frontera entre Argentina, Brasil y Paraguay, concebida como una amplia región con epicentro en la red urbana Puerto Iguazú, Foz do Iguazú y Ciudad del Este y otras localidades satélites, y que reconoce, además, dos puntos de gran importancia como Posadas/Encarnación y Bernardo de Irigoyen/Dionisio Cerqueira, comprende en realidad, un territorio muchos más vasto que abarca la provincia argentina de Misiones, la zona occidentalde los estados del sur de Brasil y el sur de Mato Grosso do Sul y el este de Paraguay. En este espacio tienen lugar múltiples relaciones transnacionales: económicas, políticas, sociales, culturales, etcétera que poseen una dilatada historia pero que, a partir de la integración y el MERCOSUR adquirieron una complejidad y densidad en permanente crecimiento y además, el surgimiento de procesos emergentes cuyo conocimiento supone un imperativo ineludible. Hemos investigado en los proyectos anteriores, ocho en total, los dos niveles en los que consideramos deben estudiarse estos procesos. Un nivel de escala mayor que trata de comprender la complejidad de una formación socioeconómica y espacial transnacional y su lugar en el ajedrez nacional e internacional del sistema imperial y, otro nivel, consistente en la profundización de problemas específicos de la región fronteriza como: redes sociales, mercado de trabajo, migraciones, exilio, solidaridad y lucha, movimientos sociales, gestión de ecosistemas compartidos, proyectos de desarrollo comunes, foros de esclarecimiento y defensa regionales, e integración del conocimiento.

Antropología de los procesos transfronterizos. La Triple Frontera en el sistema mundo. Complejidad y resistencia regional. (HANUIN VII) 2008-2009. 16H245

La presente investigación forma parte de un ciclo integrado por seis investigaciones precedentes, cuyas referencias están incluidas en el apartado de antecedentes. Su objetivo principal es conocer y describir la complejidad de la región de fronteras estudiada (triple frontera), las zonas de influencia directa y las acciones propias, que desde la región, protagonizan organizaciones y movimientos sociales en relación a las cada vez mas intensas amenazas de intervención militar por parte del poder hegemónico de Estados Unidos y la intensificación de los controles estatales nacionales que responden a las presiones internacionales. Qué lugar ocupa en las estrategias de la hegemonía imperial esta región y cuales son las respuestas locales tanto en acciones como en representaciones