Sedimentological and clay mineralogical analysis of ODP sites in the central Fram Strait

This study presents the results of high-resolution sedimentological and clay mineralogical investigations on sediments from ODP Sites 908A and 909AlC located in the central Fram Strait. The objective was to reconstruct the paleoclimate and paleoceanography of the high northern latitudes since the middle Miocene. The sediments are characterised in particular by a distinctive input of ice-rafted material, which most probably occurs since 6 Ma and very likely since 15 Ma. A change in the source area at 1 1.2 Ma is clearly marked by variations within clay mineral composition and increasing accumulation rates. This is interpreted as a result of an increase in water mass exchange through the Fram Strait. A further period of increasing exchange between 4-3 Ma is identified by granulometric investigations and points to a synchronous intensification of deep water production in the North Atlantic during this time interval. A comparison of the components of coarse and clay fraction clearly shows that both are not delivered by the Same transport process. The input of the clay fraction can be related to transport mechanisms through sea ice and glaciers and very likely also through oceanic currents. A reconstruction of source areas for clay minerals is possible only with some restrictions. High smectite contents in middle and late Miocene sediments indicate a background signal produced by soil formation together with sediment input, possibly originating from the Greenland- Scotland Ridge. The applicability of clay mineral distribution as a climate proxy for the high northern latitudes can be confirmed. Based on a comparison of sediments from Site 909C, characterised by the smectite/illite and chlorite ratio, with regional and global climatic records (oxygen isotopes), a middle Miocene cooling phase between 14.8-14.6 Ma can be proposed. A further cooling phase between 10-9 Ma clearly shows similarities in its Progress toward drastic decrease in carbonate sedimentation and preservation in the eastern equatorial Pacific. The modification in sea water and atmosphere chemistry may represent a possible link due to the built-up of equatorial carbonate platforms. Between 4.8-4.6 Ma clay mineral distribution indicates a distinct cooling trend in the Fram Strait region. This is not accompanied by relevant glaciation, which would otherwise be indicated by the coarse fraction. The intensification of glaciation in the northern hemisphere is distinctly documented by a rapid increase of illite and chlorite starting from 3.3 Ma, which corresponds to oxygen isotope data trends from North Atlantic.

Sedimentological, physical, bulk geochemical, elemental and rock magnetic properties of the Middle to Late Pleistocene Rodderberg (Eifel/Germany)

The sediment record from Rodderberg potentially provides a climate and environmental record spanning at least the last ca 130 ka. Results from a low resolution pilot study reveal characteristic fluctuations that can be related to global climate variability as reflected in marine isotope stages and document the potential of this site for continuous and high-resolution investigations of the Middle to Late Pleistocene. Here we document the tentative lithology drilled, and show how the elemental composition can be interpreted with regard to lake level fluctuations, related redox conditions, but also to grain-size distribution and changes in lacustrine productivity. Finally, based on major lithological changes, a preliminary depth/age model is suggested that allows reassessing published luminescence ages from the same site.

Mid-Wisconsin to Holocene permafrost and landscape dynamics based on a drained lake basin core from the northern Seward Peninsula, Northwest Alaska

Permafrost-related processes drive regional landscape dynamics in the Arctic terrestrial system. A better understanding of past periods indicative of permafrost degradation and aggradation is important for predicting the future response of Arctic landscapes to climate change. Here, we used a multi-proxy approach to analyze a ~4 m long sediment core from a drained thermokarst lake basin on the northern Seward Peninsula in western Arctic Alaska (USA). Sedimentological, biogeochemistical, geochronological, micropaleontological (ostracoda, testate amoeba) and tephra analyses were used to determine the long-term environmental Early-Wisconsin to Holocene history preserved in our core for Central Beringia. Yedoma accumulation dominated throughout the Early to Late-Wisconsin but was interrupted by wetland formation from 44.5 to 41.5 ka BP. The latter was terminated by deposition of 1 m of volcanic tephra, most likely originating from the South Killeak Maar eruption at about 42 ka BP. Yedoma deposition continued until 22.5 ka BP and was followed by a depositional hiatus in the sediment core between 22.5 and 0.23 ka BP. We interpret this hiatus as due to intense thermokarst activity in the areas surrounding the site, which served as a sediment source during the Late-Wisconsin to Holocene climate transition. The lake forming the modern basin on the upland initiated around 0.23 ka BP, which drained catastrophically in spring 2005. The present study emphasizes that Arctic lake systems and periglacial landscapes are highly dynamic and permafrost formation as well as degradation in Central Beringia was controlled by regional to global climate patterns and as well as by local disturbances.

Factores que afectan la emisión de escapo floral y producción de bulbillos aéreos en ajo (Allium sativum L.)

El ajo constituye el principal producto agrícola no transformado destinado a la exportación en Mendoza. En la Argentina, la ausencia de cultivares específicas de ajo y producción de semilla fiscalizada han sido unas de las principales debilidades del sistema exportador. Para que los materiales provenientes de los planes de mejoramiento y saneados lleguen rápidamente al productor es necesario acelerar la tasa de multiplicación de los mismos. Con esta finalidad, los bulbillos aéreos que se forman en el extremo del escapo de ajo tipo “colorado" (Grupo IV, Argentina) libre de virus, pueden ser utilizados como propágulos en la producción de ajo “semilla". El objetivo general del presente trabajo fue establecer la influencia del: genotipo, liberación de virus (OYDV y LYSV), tamaño de “diente" empleado como propágulo, fertilización nitrogenada y conservación de los escapos luego de la cosecha, en la producción de bulbillos aéreos. En Mendoza, Argentina, se evaluaron durante el ciclo 1994, 32 introducciones de ajo tipo “colorado" de distinto origen, por su hábito de floración y producción de bulbillos aéreos. Se llevaron a cabo durante los años 1995 y 1996 dos ciclos de ensayos, en los que se evaluó en una población clonal de ajo “colorado criollo" (AR-I-051) y una de ajo “ruso" (AR-I-033) el efecto del saneamiento viral sobre la floración y producción de bulbillos aéreos, trabajando con material crónicamente enfermo y libre de OYDV y LYSV. En AR-I-051 además se estudió el efecto del tamaño de “diente" (2; 3,5 y 5 g ó 1,2; 3,2 y 5,2 g) e influencia de la fertilización nitrogenada (0, 50 y 100 kg.ha-1 de N como SO4(NH4)2). Entre 1995 y 1998, se compararon diversas métodos de “curado" de los escapos luego de la cosecha de las plantas (en planta entera, cortados de distintas longitudes, mantenidos en seco o con inmersión de sus bases en agua o en solución nutritiva con o sin el regulador del crecimiento CCC). Se concluye que la producción de bulbillos aéreos depende del genotipo considerado. En ajo “colorado" se distinguen 5 grupos por su modalidad de floración y potencialidad de producción de bulbillos. La producción de bulbillos aéreos útiles (>2,4 mm de diámetro) depende del tiempo transcurrido entre floración y cosecha y no entre plantación y floración. Se puede predecir la cantidad de bulbillos aéreos útiles (Numa) sobre la base del diámetro de espata (espa) y la longitud de escapo (long) al momento de cosecha, según la ecuación: Numa = - 81,62 + 4,79 espa + 1,05 long (r2 = 0,88). v La capacidad de cada genotipo de emitir escapos, disminuye con la liberación de OYDV y LYSV, por lo que la producción por hectárea de bulbillos aéreos útiles es menor en el material saneado. El empleo de material saneado, “dientes" grandes, como la fertilización con N producen plantas de mayor tamaño y con mayor área foliar, lo que se traduce en un mayor rendimiento en la producción de bulbos. Sin embargo, la producción de bulbillos aéreos por hectárea disminuye, debido al menor porcentaje de plantas que emiten escapos y no a la disminución del número de bulbillos por planta. En cambio, todas aquellas condiciones que favorecen menor expresión vegetativa de las plantas aumentan la emisión de escapos. El “curado" de los escapos separados de la planta madre se puede llevar a cabo sin necesidad de realizar la inmersión de la base de los mismos en agua o en solución nutritiva con o sin CCC. La longitud a la cual se deben cortar los escapos, de manera de no afectar la producción de bulbillos, depende del grado de crecimiento de los bulbillos en el campo. La longitud de corte del escapo en ajo “criollo", con escaso crecimiento de los bulbillos aéreos en el campo, no debe ser inferior a 50 cm. En ajo “ruso", que presenta al momento de cosecha de las plantas un desarrollo avanzado de los bulbillos aéreos, los escapos pueden cortarse de menor longitud, sin afectar la producción de bulbillos aéreos. La longitud del escapo, en planta o separado de ella, afecta la producción de bulbillos aéreos en forma directamente proporcional.

Científicos y políticas públicas : la incidencia de una red en el tratamiento de una Ley de Ordenamiento Territorial

Nuestro trabajo tiene como objetivo aplicar conceptos de la teoría de los sistemas complejos y herramientas del análisis de redes sociales para describir y analizar el surgimiento y la evolución de una red social conformada por científicos, docentes, graduados y funcionarios públicos de diferentes organismos científicos y académicos, que crearon y participaron de un equipo multidisciplinario que elaboró un informe sobre un proyecto de ley de Ordenamiento Territorial y Usos del Suelo de la provincia de Mendoza en el año 2006. Para la compresión de la evolución del proceso de elaboración del proyecto de ley de ordenamiento territorial y de usos del suelo, organizaremos la estructura del trabajo de la siguiente manera: - Primero aplicaremos aspectos teóricos y metodológicos, basados en la sistematización realizada por Rolando García en su libro “Sistemas Complejos. Conceptos, método y fundamentación epistemológica de la investigación interdisciplinaria", para realizar el recorte del sistema objeto de estudio. - En segundo lugar utilizaremos la Teoría de Análisis de Redes Sociales para describir la composición y estructura del sistema (nodos y vínculos) en cada momento. La estructura del sistema en cada momento significativo será graficada por medio el Software Ucinet 6 y NetDraw. - Por último, haremos referencia a las dificultades que tuvo el proceso desde el punto de vista de las condicionalidades que generaban los modelos mentales que portaban los participantes.

Geochemistry, clay mineralogy and grain size distribution in various sediment cores drilled during ODP Leg 119 on the Antarctic continental shelf off Prydz Bay

Drilling was undertaken at five sites (739-743) on ODP Leg 119 on a transect across the continental shelf of Prydz Bay, East Antarctica, to elucidate the long-term glacial history of the area and to examine the importance of the area with respect to the development of the East Antarctic ice sheet as a whole. In addition to providing a record of glaciation spanning 36 m.y. or more, Leg 119 has provided information concerning the development of a continental margin under the prolonged influence of a major ice sheet. This has allowed the development of a sedimentary model that may be applicable not only to other parts of the Antarctic continental margin, but also to northern high-latitude continental shelves. The cored glacial sedimentary record in Prydz Bay consists of three major sequences, dominated by diamictite: 1. An upper flat-lying sequence that ranges in thickness from a few meters in inner and western Prydz Bay to nearly 250 m in the outer or eastern parts of the bay. The uppermost few meters consist of Holocene diatom ooze and diatomaceous mud with a minor ice-rafted component overlying diamicton and diamictite of late Miocene to Quaternary age. The diamictite is mainly massive, but stratified varieties and minor mudstone and diatomite also occur. 2. An upper prograding sequence cored at Sites 739 and 743, unconformly below the flat-lying sequence. This consists of a relatively steep (4° inclination) prograding wedge with a number of discrete sedimentary packages. At Sites 739 and 743 the sequence is dominated by massive and stratified diamictite, some of which shows evidence of slumping and minor debris flowage. 3. A lower, more gently inclined, prograding sequence lies unconformably below the flat-lying sequence at Site 742 and the upper prograding sequence at Site 739. This extends to the base of both sites, to 316 and 487 mbsf, respectively. It is dominated by massive, relatively clast-poor diamictite which is kaolinite-rich, light in color, and contains sporadic carbonate-cemented layers. The lower part of Site 742 includes well-stratified diamictites and very poorly sorted mudstones. The base of this site has indications of large-scale soft-sediment deformation and probably represents proximity to the base of the glacial sequence. Facies analysis of the Prydz Bay glacial sequence indicates a range of depositional environments. Massive diamictite is interpreted largely as waterlain till, deposited close to the grounding line of a floating glacier margin, although basal till and debris flow facies are also present. Weakly stratified diamictite is interpreted as having formed close to or under the floating ice margin and influenced by the input of marine diatomaceous sediment (proximal glaciomarine setting). Well-stratified diamictite has a stronger marine input, being more diatom-rich, and probably represents a proximal-distal glaciomarine sediment with the glaciogenic component being supplied by icebergs. Other facies include a variety of mudstones and diatom-rich sediments of marine origin, in which an ice-rafted component is still significant. None of the recovered sediments are devoid of a glacial influence. The overall depositional setting of the prograding sequence is one in which the grounded ice margin is situated close to the shelf edge. Progradation was achieved primarily by deposition of waterlain till. The flat-lying sequence illustrates a complex sequence of advances and retreats across the outer part of the shelf, with intermittent phases of ice loading and erosion. The glacial chronology is based largely on diatom stratigraphy, which has limited resolution. It appears that ice reached the paleoshelf break by earliest Oligocene, suggesting full-scale development of the East Antarctic ice sheet by that time. The ice sheet probably dominated the continental margin for much of Oligocene to middle Miocene time. Retreat, but not total withdrawal of the ice sheet, took place in late Miocene to mid-Pliocene time. The late Pliocene to Pleistocene was characterized by further advances across, and progradation of, the continental shelf. Holocene time has been characterized by reduced glacial conditions and a limited influence of glacial processes on sedimentation.

Results of bulk sediment X-ray diffraction analysis and quantification of mineral phases based on the RockJock and on the QUAX quantitative analysis

We have performed quantitative X-ray diffraction (qXRD) analysis of 157 grab or core-top samples from the western Nordic Seas between (WNS) ~57°-75°N and 5° to 45° W. The RockJock Vs6 analysis includes non-clay (20) and clay (10) mineral species in the <2 mm size fraction that sum to 100 weight %. The data matrix was reduced to 9 and 6 variables respectively by excluding minerals with low weight% and by grouping into larger groups, such as the alkali and plagioclase feldspars. Because of its potential dual origins calcite was placed outside of the sum. We initially hypothesized that a combination of regional bedrock outcrops and transport associated with drift-ice, meltwater plumes, and bottom currents would result in 6 clusters defined by "similar" mineral compositions. The hypothesis was tested by use of a fuzzy k-mean clustering algorithm and key minerals were identified by step-wise Discriminant Function Analysis. Key minerals in defining the clusters include quartz, pyroxene, muscovite, and amphibole. With 5 clusters, 87.5% of the observations are correctly classified. The geographic distributions of the five k-mean clusters compares reasonably well with the original hypothesis. The close spatial relationship between bedrock geology and discrete cluster membership stresses the importance of this variable at both the WNS-scale and at a more local scale in NE Greenland.

Radiocarbon ages and clay minerals in sediment cores obtained during a 2009 Jan Mayen cruise to the Norwegian Sea

The origin of two acoustic sediment units has been studied based on lithological facies, chronology and benthic stable isotope values as well as on foraminifera and clay mineral assemblages in six marine sediment cores from Kveithola, a small trough west of Spitsbergenbanken on the western Barents Sea margin. We have identified four time slices with characteristic sedimentary environments. Before c. 14.2 cal. ka, rhythmically laminated muds indicate extensive sea ice cover in the area. From c. 13.9 to 14.2 cal. ka, muds rich in ice-rafted debris were deposited during the disintegration of grounded ice on Spitsbergenbanken. From c. 10.3 to 13.1 cal. ka, sediments with heterogeneous lithologies suggest a shifting influence of suspension settling and iceberg rafting, probably derived from a decaying Barents Sea Ice Sheet in the inner-fjord and land areas to the north of Kveithola. Holocene deposition was episodic and characterized by the deposition of calcareous sands and shell debris, indicative of strong bottom currents. We speculate that a marked erosional boundary at c. 8.2 cal. ka may have been caused by the Storegga tsunami. Whilst deposition was sparse during the Holocene, Kveithola acted as a sediment trap during the preceding deglaciation. Investigation of the deglacial sediments provides unprecedented details on the dynamics and timing of glacial retreat from Spitsbergenbanken.