Climate and soil characteristics and soil arthropod abundance on Anchorage, Signy and Falkland Islands

Over a 2-year study, we investigated the effect of environmental change on the diversity and abundance of soil arthropod communities (Acari and Collembola) in the Maritime Antarctic and the Falkland Islands. Open Top Chambers (OTCs), as used extensively in the framework of the northern boreal International Tundra Experiment (ITEX), were used to increase the temperature in contrasting communities on three islands along a latitudinal temperature gradient, ranging from the Falkland Islands (51°S, mean annual temperature 7.5 °C) to Signy Island (60°S, -2.3°C) and Anchorage Island (67°S, -3.8°C). At each island an open and a closed plant community were studied: lichen vs. moss at the Antarctic sites, and grass vs. dwarf shrub at the Falkland Islands. The OTCs raised the soil surface temperature during most months of the year. During the summer the level of warming achieved was 1.7 °C at the Falkland Islands, 0.7 °C at Signy Island, and 1.1 °C at Anchorage Island. The native arthropod community diversity decreased with increasing latitude. In contrast with this pattern, Collembola abundance in the closed vegetation (dwarf shrub or moss) communities increased by at least an order of magnitude from the Falkland Islands (9.0 +/- 2 x 10**3 ind./m**2) to Signy (3.3 +/- 8.0 x 10**4 ind./m**2) and Anchorage Island (3.1 +/- 0.82 x 10**5 ind./m**2). The abundance of Acari did not show a latitudinal trend. Abundance and diversity of Acari and Collembola were unaffected by the warming treatment on the Falkland Islands and Anchorage Island. However, after two seasons of experimental warming, the total abundance of Collembola decreased (p < 0.05) in the lichen community on Signy Island as a result of the population decline of the isotomid Cryptopygus antarcticus. In the same lichen community there was also a decline (p < 0.05) of the mesostigmatid predatory mite Gamasellus racovitzai, and a significant increase in the total number of Prostigmata. Overall, our data suggest that the consequences of an experimental temperature increase of 1-2°C, comparable to the magnitude currently seen through recent climate change in the Antarctic Peninsula region, on soil arthropod communities in this region may not be similar for each location but is most likely to be small and initially slow to develop.

(Table 1) Organic geochemistry of ODP Hole 134-832B and Site 134-833

Ocean Drilling Program (ODP) Leg 134 was located in the central part of the New Hebrides Island Arc, in the Southwest Pacific. Here the d'Entrecasteaux Zone of ridges, the North d'Entrecasteaux Ridge and South d'Entrecasteaux Chain, is colliding with the arc. The region has a Neogene history of subduction polarity reversal, ridge-arc collision, and back-arc spreading. The reasons for drilling in this region included the following: (1) to determine the differences in the style and time scale of deformation associated with the two ridge-like features (a fairly continuous ridge and an irregularly topographic seamount chain) that are colliding with the central New Hebrides Island Arc; (2) to document the evolution of the magmatic arc in relation to the collision process and possible Neogene reversal of subduction; and (3) to understand the process of dewatering of a small accretionary wedge associated with ridge collision and subduction. Seven sites were occupied during the leg, five (Sites 827-831) were located in the d'Entrecasteaux Zone where collision is active. Three sites (Sites 827, 828, and 829) were located where the North d'Entrecasteaux Ridge is colliding, whereas two sites (Sites 830 and 831) were located in the South d'Entrecasteaux Chain collision zone. Sites 828 (on North d'Entrecasteaux Ridge) and 831 (on Bougainville Guyot) were located on the Pacific Plate, whereas all other sites were located on a microplate of the North Fiji Basin. Two sites (Sites 832 and 831) were located in the intra-arc North Aoba Basin. Results of Leg 134 drilling showed that forearc deformation associated with the North d'Entrecasteaux Ridge and South d'Entrecasteaux Chain collision is distinct and different. The d'Entrecasteaux Zone is an Eocene subduction/obduction complex with a distinct submerged island arc. Collision and subduction of the North d'Entrecasteaux Ridge results in off scraping of ridge material and plating of the forearc with thrust sheets (flakes) as well as distinct forearc uplift. Some offscraped sedimentary rocks and surficial volcanic basement rocks of the North d'Entrecasteaux Ridge are being underplated to the New Hebrides Island forearc. In contrast, the South d'Entrecasteaux Chain is a serrated feature resulting in intermittent collision and subduction of seamounts. The collision of the Bougainville Guyot has indented the forearc and appears to be causing shortening through thrust faulting. In addition, we found that the Quaternary relative convergence rate between the New Hebrides Island Arc at the latitude of Espiritu Santo Island is as high as 14 to 16 cm/yr. The northward migration rate of the d'Entrecasteaux Zone was found the be ~2 to 4 cm/yr based on the newly determined Quaternary relative convergence rate. Using these rates we established the timing of initial d'Entrecasteaux Zone collision with the arc at ~3 Ma at the latitude of Epi Island and fixed the impact of the North d'Entrecasteaux Ridge upon Espiritu Santo Island at early Pleistocene (between 1.89 and 1.58 Ma). Dewatering is occurring in the North d'Entrecasteaux Ridge accretionary wedge, and the wedge is dryer than other previously studied accretionary wedges, such as Barbados. This could be the result of less sediment being subducted at the New Hebrides compared to the Barbados.

Soil characteristics and Collembola and Acari abundance in control and warming plots at Abisco Research Station

Extreme weather events can have negative impacts on species survival and community structure when surpassing lethal thresholds. Extreme winter warming events in the Arctic rapidly melt snow and expose ecosystems to unseasonably warm air (2-10 °C for 2-14 days), but returning to cold winter climate exposes the ecosystem to lower temperatures by the loss of insulating snow. Soil animals, which play an integral part in soil processes, may be very susceptible to such events depending on the intensity of soil warming and low temperatures following these events. We simulated week-long extreme winter warming events - using infrared heating lamps, alone or with soil warming cables - for two consecutive years in a sub-Arctic dwarf shrub heathland. Minimum temperatures were lower and freeze-thaw cycles were 2-11 times more frequent in treatment plots compared with control plots. Following the second event, Acari populations decreased by 39%; primarily driven by declines of Prostigmata (69%) and the Mesostigmatic nymphs (74%). A community-weighted vertical stratification shift occurred from smaller soil dwelling (eu-edaphic) Collembola species dominance to larger litter dwelling (hemi-edaphic) species dominance in the canopy-with-soil warming plots compared with controls. The most susceptible groups to these winter warming events were the smallest individuals (Prostigmata and eu-edaphic Collembola). This was not apparent from abundance data at the Collembola taxon level, indicating that life forms and species traits play a major role in community assembly following extreme events. The observed shift in soil community can cascade down to the micro-flora affecting plant productivity and mineralization rates. Short-term extreme weather events have the potential to shift community composition through trait composition with potentially large consequences for ecosystem development.

Daily polynya area and ice production in the North Water polynya region

The North Water (NOW) Polynya is a regularly-forming area of open-water and thin-ice, located between northwestern Greenland and Ellesmere Island (Canada) at the northern tip of Baffin Bay. Due to its large spatial extent, it is of high importance for a variety of physical and biological processes, especially in wintertime. Here, we present a long-term remote sensing study for the winter seasons 1978/1979 to 2014/2015. Polynya characteristics are inferred from (1) sea ice concentrations and brightness temperatures from passive microwave satellite sensors (Advanced Microwave Scanning Radiometer (AMSR-E and AMSR2), Scanning Multichannel Microwave Radiometer (SMMR), Special Sensor Microwave Imager/Sounder (SSM/I-SSMIS)) and (2) thin-ice thickness distributions, which are calculated using MODIS ice-surface temperatures and European Center for Medium-Range Weather Forecasts (ECMWF) atmospheric reanalysis data in a 1D thermodynamic energy-balance model. Daily ice production rates are retrieved for each winter season from 2002/2003 to 2014/2015, assuming that all heat loss at the ice surface is balanced by ice growth. Two different cloud-cover correction schemes are applied on daily polynya area and ice production values to account for cloud gaps in the MODIS composites. Our results indicate that the NOW polynya experienced significant seasonal changes over the last three decades considering the overall frequency of polynya occurrences, as well as their spatial extent. In the 1980s, there were prolonged periods of a more or less closed ice cover in northern Baffin Bay in winter. This changed towards an average opening on more than 85% of the days between November and March during the last decade. Noticeably, the sea ice cover in the NOW polynya region shows signs of a later-appearing fall freeze-up, starting in the late 1990s. Different methods to obtain daily polynya area using passive microwave AMSR-E/AMSR2 data and SSM/I-SSMIS data were applied. A comparison with MODIS data (thin-ice thickness < 20 cm) shows that the wintertime polynya area estimates derived by MODIS are about 30 to 40% higher than those derived using the polynya signature simulation method (PSSM) with AMSR-E data. In turn, the difference in polynya area between PSSM and a sea ice concentration (SIC) threshold of 70% is fairly low (approximately 10%) when applied to AMSR-E data. For the coarse-resolution SSM/I-SSMIS data, this difference is much larger, particularly in November and December. Instead of a sea ice concentration threshold, the PSSM method should be used for SSM/I-SSMIS data. Depending on the type of cloud-cover correction, the calculated ice production based on MODIS data reaches an average value of 264.4 ± 65.1 km**3 to 275.7 ± 67.4 km**3 (2002/2003 to 2014/2015) and shows a high interannual variability. Our achieved long-term results underline the major importance of the NOW polynya considering its influence on Arctic ice production and associated atmosphere/ocean processes.

Actividad antioxidante de los compuestos fenólicos contenidos en las semillas de la vid (vitis vinifera l.)

El propósito de este trabajo es obtener un antioxidante natural a partir de las semillas de uva (Vitis vinifera L.), para emplear en alimentos. Para ello se compararon distintos solventes para la extracción de fenoles de las semillas de la uva, de modo de obtener el extracto más concentrado en compuestos activos con la mínima degradación de su poder antioxidante durante el proceso de obtención. La concentración de fenoles totales de los extractos se determinó por el método Folin Ciocalteu. El poder reductor de los extractos se midió empleando el método de Oyaizu. Una vez seleccionado el solvente más adecuado para la extracción, se analizó la cinética de extracción, optimizando el tiempo de tratamiento. El extracto fue concentrado al vacío, y se veríficó la conservación del poder reductor en el extracto concentrado, por el método de Oyaizu. El extracto de semillas concentrado y sin concentrar se empleó en un sistema real sujeto a oxidación, tal como el jugo de manzanas. El grado de oxidación del jugo se midió por el método de Özoglu. El extracto concentrado fue deshidratado por secado en lecho de espuma y por liofilizado. En ambos casos se verificó el efecto del tratamiento de secado sobre el poder reductor. Finalmente, se evaluó la actividad antioxidante del extracto líquido concentrado de semillas de vid, respecto de otros antioxidantes comerciales como ácido ascórbico y dióxido de azufre. El sustrato oxidable fue el jugo de manzanas, y el grado de oxidación se midió por el método de Özoglu. El análisis estadístico de los datos se realizó mediante el análisis de la varianza; cuando no fue posible emplear el mencionado análisis, debido a que no se verificaban los supuestos básicos para su aplicación, se empleó la prueba de Kruskal –Wallis. En todos los casos, se utilizó el programa Statgraphics plus ®4.0. Para obtener un extracto antioxidante a partir de semillas de vid se utilizó una ex-tracción con agua a 90ºC, durante 4 horas. La relación sólido- líquido empleada fue de 1g de semillas enteras por 10 ml de solvente. El extracto obtenido presentaba una concentración de 12,587 mg de fenoles totales por gramo de semillas de uva extractadas y un poder reductor de 1,290 unidades. Como consecuencia del análisis de la cinética de extracción, el tiempo de tratamiento se redujo de 4 horas a 3 horas. La concentración del extracto se realizó al vacío a 60ºC, verificándose un aumen-to del poder reductor en el extracto concentrado, comprobado sobre jugo de manzanas. Comparando el extracto concentrado y el extracto sin concentrar se observa que la concentración de fenoles totales aumentó 29,57 veces, mientras que el poder reductor aumentó 37,39 veces. El deshidratado del extracto por medio del lecho de espuma permitió conservar el poder reductor del mismo, no ocurrió lo mismo en el deshidratado por liofilizado, donde se produjo un deterioro del poder reductor. Para un mismo contenido de fenoles totales agregado al jugo de manzanas, el ex-tracto líquido sin concentrar produjo un 28,4% de inhibición de la oxidación, mientras que el de extracto líquido concentrado produjo un 51,5 % de inhibición de la oxidación del jugo de manzanas. El extracto de semillas de vid, aplicado como antioxidante en jugo de manzanas, inhibió el desarrollo de la oxidación en un 31,51%, considerando 24 horas el tiempo de tratamiento. Este desempeño supera al ácido ascórbico, que en iguales condiciones, inhibió el desarrollo de la oxidación en un 2,6%. Pero en las condiciones de tra-bajo, el dióxido de azufre resulta mejor antioxidante que ambos, ya que logró inhibir el desarrollo de la oxidación en un 97,40 %.

Desarrollo preliminar de descriptores para el análisis sensorial de ajos desecados y liofilizados

El polvo de ajo (Allium sativum L.) es una alternativa para conservar en el tiempo sus propiedades sensoriales y prolongar su vida útil como alimento procesado. En la actualidad, no existe una definición clara de las propiedades sensoriales que caracterizan el ajo ni de las técnicas más adecuadas para su análisis. Los objetivos del presente trabajo fueron estudiar diferentes vehículos y determinar el más apropiado para el análisis sensorial del polvo de ajo, y generar y definir los descriptores para las propiedades sensoriales de olor y flavor de diferentes cultivares deshidratados a través de dos métodos: en estufa a 50°C y por liofilización a -50°C, bajo vacío. Se pretende contribuir a la caracterización de este producto aportando un vocabulario específico y sus definiciones, como así también una metodología sensorial propia. Ocho evaluadores, seleccionados y entrenados de acuerdo con las normas internacionales y con experiencia en análisis sensorial, probaron diferentes vehículos y una vez determinado el más adecuado, desarrollaron el lenguaje descriptivo para los ajos desecados y liofilizados seleccionando por consenso los descriptores que mejor caracterizaban las cultivares, y se definió cada término. Se generaron 31 descriptores simples. Si bien, algunos de los descriptores coincidieron con los publicados en la guía ASTM DS 66 (1996) para ajos frescos, con esta investigación se aportó un amplio número de términos nuevos para la descripción del olor y el flavor de los ajos desecados y liofilizados, los cuales contribuyen a una mejor caracterización sensorial de este producto.

Extracto de semillas de vid (Vitis vinifera L.) con actividad antioxidante : concentración, deshidratación y comparación con antioxidantes de uso comercial

Los objetivos de este trabajo fueron: 1) Evaluar un proceso de concentración y deshidratación de un extracto polifenólico de semillas de vid (Vitis vinifera L.). El proceso debía conservar el poder reductor del extracto. 2) Valorar la eficiencia del antioxidante obtenido por comparación con antioxidantes de uso habitual en un producto vegetal susceptible de ser oxidado, tal como el jugo de manzanas. El extracto de semillas de vid fue concentrado a 60°C en un concentrador rotativo al vacío de laboratorio. La concentración de los compuestos fenólicos fue determinada por el método de Folin-Ciocalteu modificado. La actividad antioxidante se determinó midiendo el poder reductor, por el método de Oyaizu. La oxidación del jugo de manzanas se determinó por el método de Özoglu. El extracto concentrado obtenido fue deshidratado por dos métodos: liofilización y secado en lecho de espuma. A igual concentración fenólica, el extracto concentrado mostró mayor capacidad antioxidante que el extracto simple. El extracto secado en lecho de espuma conservó la misma capacidad antioxidante que el extracto concentrado. El extracto liofilizado experimentó una pérdida significativa de la actividad antioxidante. El extracto concentrado de semillas de vid inhibió la oxidación del jugo de manzanas en un 31,51%, el ácido ascórbico en un 2,60% y el dióxido de azufre en un 97,40%.

Vertical flux reconstruction for sediment cores off Chile

Biogenic opal and organic carbon vertical rain rates in sediment cores reveal a strong cyclicity in the productivity of the upwelling system off presently arid northern Chile during the last 100,000 years. Changes in productivity are found to be in phase with the precessional cycle (~20,000 years) and with inputs of iron from the continent. During austral summer insolation maxima, increased precipitation and river runoff in the region appear to have brought high inputs of iron, mainly from the Andes, to the coastal ocean enhancing primary productivity there. We interpret our results as providing evidence for iron control of past productivity in this upwelling system and for a tight link between productivity and orbital forcing at midlatitudes.