Snow depths of volcanic events and accumulation rates of firn cores from the IPY traverse, Antarctica

Volcanic signatures in ice-core records provide an excellent means to date the cores and obtain information about accumulation rates. From several ice cores it is thus possible to extract a spatio-temporal accumulation pattern. We show records of electrical conductivity and sulfur from 13 firn cores from the Norwegian-USA scientific traverse during the International Polar Year 2007-2009 (IPY) through East Antarctica. Major volcanic eruptions are identified and used to assess century-scale accumulation changes. The largest changes seem to occur in the most recent decades with accumulation over the period 1963-2007/08 being up to 25% different from the long-term record. There is no clear overall trend, some sites show an increase in accumulation over the period 1963 to present while others show a decrease. Almost all of the sites above 3200 m above sea level (asl) suggest a decrease. These sites also show a significantly lower accumulation value than large-scale assessments both for the period 1963 to present and for the long-term mean at the respective drill sites. The spatial accumulation distribution is influenced mainly by elevation and distance to the ocean (continentality), as expected. Ground-penetrating radar data around the drill sites show a spatial variability within 10-20% over several tens of kilometers, indicating that our drill sites are well representative for the area around them. Our results are important for large-scale assessments of Antarctic mass balance and model validation.

Biogeochemistry in acid sulphate soil landscapes and small urban centres in Western Finland

The overall purpose of this thesis was to increase the knowledge on the biogeochemistry of rural acid sulphate (AS) soil environments and urban forest ecosystems near small towns in Western Finland. In addition, the potential causal relationship between the distribution of AS soils and geographical occurence of multiple sclerosis (MS) disease was assessed based on a review of existing literature and data. Acid sulphate soils, which occupy an area of approximately 17–24 million hectare worldwide, are regarded as the nastiest soils in the world. Independent of the geographical locality of these soils, they pose a great threat to their surrounding environment if disturbed. The abundant metal-rich acid drainage from Finnish AS soils, which is a result of sulphide oxidation due to artificial farmland drainage, has significant but spatially and temporally variable ecotoxicological impacts on biodiversity and community structure of fish, benthic invertebrates and macrophytes. This has resulted in mass fish kills and even eradication of sensitive fish species in affected waters. Moreover, previous investigations demonstrated significantly enriched concentrations of Co, Ni, Mn and Al, metals which are abundantly mobilised in AS soils, in agricultural crops (timothy grass and oats) and approximately 50 times higher concentrations of Al in cow milk originating from AS soils in Western Finland. Nevertheless, the results presented here demonstrate, in general, relatively moderate metal concentrations in oats and cabbage grown on AS soils in Western Finland, although some of the studied fields showed anomalous values of metals (e.g. Co and Ni) in both the soil and target plants (especially oats), similar to that of the previous investigations. The results indicated that the concentrations of Co, Ni, Mn and Zn in oats and Co and Zn in cabbage were governed by soil geochemistry as these metals were correlated with corresponding concentrations extracted from the soil by NH4Ac-EDTA and NH4Ac, respectively. The concentrations of Cu and Fe in oats and cabbage were uncorrelated to that of the easily soluble concentrations in the soils, suggesting that biological processes (e.g. plant-root processes) overshadow geochemical variation. The concentrations of K and Mg in cabbage, which showed a low spread and were strongly correlated to the NH4Ac extractable contents in the soil, were governed by both the bioavailable fractions in the topsoil and plant-uptake mechanisms. The plant´s ability to regulate its uptake of Ca and P (e.g. through root exudates) seemed to be more important than the influence of soil geochemistry. The distribution of P, K, Ca, Mg, Mn and S within humus, moss and needles in and around small towns was to a high degree controlled by biological cycling, which was indicated by the low correlation coefficients for P, K, Ca, Mg and S between humus and moss, and the low spread of these nutrients in moss and needles. The concentration variations of elements in till are mainly due to natural processes (e.g. intrusions, weathering, mineralogical variations in the bedrock). There was a strong spatial pattern for B in humus, moss and needles, which was suggested to be associated with anthropogenic emissions from nearby town centres. Geogenic dust affected the spatial distribution of Fe and Cr in moss, while natural processes governed the Fe anomaly found in the needles. The spatial accumulation patterns of Zn, Cd, Cu, Ni and Pb in humus and moss were strong and diverse, and related to current industry, the former steel industry, coal combustion, and natural geochemical processes. An intriguing Cu anomaly was found in moss. Since it was located close to a main railway line and because the railway line´s electric cables are made of Cu, it was suggested that the reason for the Cu anomaly is corrosion of these cables. In Western Finland, where AS soils are particularly abundant and enrich the metal concentrations of stream waters, cow milk and to some extent crops, an environmental risk assessment would be motivated to elucidate if the metal dispersion affect human health. Within this context, a topic of concern is the distribution of multiple sclerosis as high MS prevalence rates are found in the main area of AS soils. Regionally, the AS soil type in the Seinäjoki area has been demonstrated to be very severe in terms of metal leaching, this area also shows one of the highest MS rates reported worldwide. On a local scale, these severe AS soil types coincide well with the corresponding MS clustering along the Kyrönjoki River in Seinäjoki. There are reasons to suspect that these spatial correlations are causal, as multiple sclerosis has been suggested to result from a combination of genetic and environmental factors.

Estado, industrialização e os espaços de acumulação das Multilatinas

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

Synchronisation of the EDML and EDC ice cores for the last 52 kyr by volcanic signature matching

A common time scale for the EPICA ice cores from Dome C (EDC) and Dronning Maud Land (EDML) has been established. Since the EDML core was not drilled on a dome, the development of the EDML1 time scale for the EPICA ice core drilled in Dronning Maud Land was based on the creation of a detailed stratigraphic link between EDML and EDC, which was dated by a simpler 1D ice-flow model. The synchronisation between the two EPICA ice cores was done through the identification of several common volcanic signatures. This paper describes the rigorous method, using the signature of volcanic sulfate, which was employed for the last 52 kyr of the record. We estimated the discrepancies between the modelled EDC and EDML glaciological age scales during the studied period, by evaluating the ratio R of the apparent duration of temporal intervals between pairs of isochrones. On average R ranges between 0.8 and 1.2 corresponding to an uncertainty of up to 20% in the estimate of the time duration in at least one of the two ice cores. Significant deviations of R up to 1.4–1.5 are observed between 18 and 28 kyr before present (BP), where present is defined as 1950. At this stage our approach does not allow us unequivocally to find out which of the models is affected by errors, but assuming that the thinning function at both sites and accumulation history at Dome C (which was drilled on a dome) are correct, this anomaly can be ascribed to a complex spatial accumulation variability (which may be different in the past compared to the present day) upstream of the EDML core.

El análisis regional en la Argentina : Enfoque teórico-metodológico y aportes para su profundización

El artículo presenta los principales núcleos del enfoque de análisis regional en la Argentina, realizando distintos aportes a su desarrollo sobre las dinámicas de acumulación y hegemonía. En ese sentido, retomamos a autores como Rofman, de Jong y Levín, para comprender la relación entre territorio y sociedad. Partimos del planteo de construcción de conocimiento sintético y holístico, tratando de integrar las distintas escalas del análisis espacial con sus particularidades y sus interpenetraciones. La relación espacio/modo de producción nos lleva a la pregunta por las transformaciones orgánicas del capital como relación social y, así, al estudio del proceso de reproducción ampliada del capital a partir de conceptos como el de régimen y modelo de acumulación, a diferentes escalas, alcances y niveles de abstracción. Vemos las relaciones de fuerzas a nivel internacional a la luz de la disputa por distintos monopolios estratégicos, que señala Amín, y del lugar de las corporaciones transnacionales como agentes centrales de los regímenes de acumulación actual. En ese punto, continuamos desarrollando el plan de análisis de relaciones de fuerzas gramsciano, desde su nivel estructural hasta el momento de la hegemonía. De esta manera, la construcción del territorio dentro de una formación social nacional lleva a indagar la dinámica del proceso productivo, sus agentes, fracciones y clases, así como el rol del Estado y de la disputa entre distintos proyectos societarios. Estas dimensiones aparecen, asimismo, conjugadas, en una escala menor, en el análisis de los subsistemas espaciales de acumulación y de los circuitos productivos regionales que los constituyen. La explicitación de diversas claves teórico-metodológicas aparece atravesada por el debate en torno a repensar la planificación del espacio social, preguntándonos ¿qué territorio para qué sociedad?

El análisis regional en la Argentina : Enfoque teórico-metodológico y aportes para su profundización

El artículo presenta los principales núcleos del enfoque de análisis regional en la Argentina, realizando distintos aportes a su desarrollo sobre las dinámicas de acumulación y hegemonía. En ese sentido, retomamos a autores como Rofman, de Jong y Levín, para comprender la relación entre territorio y sociedad. Partimos del planteo de construcción de conocimiento sintético y holístico, tratando de integrar las distintas escalas del análisis espacial con sus particularidades y sus interpenetraciones. La relación espacio/modo de producción nos lleva a la pregunta por las transformaciones orgánicas del capital como relación social y, así, al estudio del proceso de reproducción ampliada del capital a partir de conceptos como el de régimen y modelo de acumulación, a diferentes escalas, alcances y niveles de abstracción. Vemos las relaciones de fuerzas a nivel internacional a la luz de la disputa por distintos monopolios estratégicos, que señala Amín, y del lugar de las corporaciones transnacionales como agentes centrales de los regímenes de acumulación actual. En ese punto, continuamos desarrollando el plan de análisis de relaciones de fuerzas gramsciano, desde su nivel estructural hasta el momento de la hegemonía. De esta manera, la construcción del territorio dentro de una formación social nacional lleva a indagar la dinámica del proceso productivo, sus agentes, fracciones y clases, así como el rol del Estado y de la disputa entre distintos proyectos societarios. Estas dimensiones aparecen, asimismo, conjugadas, en una escala menor, en el análisis de los subsistemas espaciales de acumulación y de los circuitos productivos regionales que los constituyen. La explicitación de diversas claves teórico-metodológicas aparece atravesada por el debate en torno a repensar la planificación del espacio social, preguntándonos ¿qué territorio para qué sociedad?

El análisis regional en la Argentina : Enfoque teórico-metodológico y aportes para su profundización

El artículo presenta los principales núcleos del enfoque de análisis regional en la Argentina, realizando distintos aportes a su desarrollo sobre las dinámicas de acumulación y hegemonía. En ese sentido, retomamos a autores como Rofman, de Jong y Levín, para comprender la relación entre territorio y sociedad. Partimos del planteo de construcción de conocimiento sintético y holístico, tratando de integrar las distintas escalas del análisis espacial con sus particularidades y sus interpenetraciones. La relación espacio/modo de producción nos lleva a la pregunta por las transformaciones orgánicas del capital como relación social y, así, al estudio del proceso de reproducción ampliada del capital a partir de conceptos como el de régimen y modelo de acumulación, a diferentes escalas, alcances y niveles de abstracción. Vemos las relaciones de fuerzas a nivel internacional a la luz de la disputa por distintos monopolios estratégicos, que señala Amín, y del lugar de las corporaciones transnacionales como agentes centrales de los regímenes de acumulación actual. En ese punto, continuamos desarrollando el plan de análisis de relaciones de fuerzas gramsciano, desde su nivel estructural hasta el momento de la hegemonía. De esta manera, la construcción del territorio dentro de una formación social nacional lleva a indagar la dinámica del proceso productivo, sus agentes, fracciones y clases, así como el rol del Estado y de la disputa entre distintos proyectos societarios. Estas dimensiones aparecen, asimismo, conjugadas, en una escala menor, en el análisis de los subsistemas espaciales de acumulación y de los circuitos productivos regionales que los constituyen. La explicitación de diversas claves teórico-metodológicas aparece atravesada por el debate en torno a repensar la planificación del espacio social, preguntándonos ¿qué territorio para qué sociedad?

Spatial and temporal dynamics of jasmonate synthesis and accumulation in Arabidopsis in response to wounding.

A new metabolite profiling approach combined with an ultrarapid sample preparation procedure was used to study the temporal and spatial dynamics of the wound-induced accumulation of jasmonic acid (JA) and its oxygenated derivatives in Arabidopsis thaliana. In addition to well known jasmonates, including hydroxyjasmonates (HOJAs), jasmonoyl-isoleucine (JA-Ile), and its 12-hydroxy derivative (12-HOJA-Ile), a new wound-induced dicarboxyjasmonate, 12-carboxyjasmonoyl-l-isoleucine (12-HOOCJA-Ile) was discovered. HOJAs and 12-HOOCJA-Ile were enriched in the midveins of wounded leaves, strongly differentiating them from the other jasmonate metabolites studied. The polarity of these oxylipins at physiological pH correlated with their appearance in midveins. When the time points of accumulation of different jasmonates were determined, JA levels were found to increase within 2-5 min of wounding. Remarkably, these changes occurred throughout the plant and were not restricted to wounded leaves. The speed of the stimulus leading to JA accumulation in leaves distal to a wound is at least 3 cm/min. The data give new insights into the spatial and temporal accumulation of jasmonates and have implications in the understanding of long-distance wound signaling in plants.

Starch accumulation in cassava roots: spatial and temporal distribution

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

Spatial gradients of temperature, accumulation and delta18O-ice in Greenland over a series of Dansgaard-Oeschger events

Air and water stable isotope measurements from four Greenland deep ice cores (GRIP, GISP2, NGRIP and NEEM) are investigated over a series of Dansgaard–Oeschger events (DO 8, 9 and 10), which are representative of glacial millennial scale variability. Combined with firn modeling, air isotope data allow us to quantify abrupt temperature increases for each drill site (1σ = 0.6 °C for NEEM, GRIP and GISP2, 1.5 °C for NGRIP). Our data show that the magnitude of stadial–interstadial temperature increase is up to 2 °C larger in central and North Greenland than in northwest Greenland: i.e., for DO 8, a magnitude of +8.8 °C is inferred, which is significantly smaller than the +11.1 °C inferred at GISP2. The same spatial pattern is seen for accumulation increases. This pattern is coherent with climate simulations in response to reduced sea-ice extent in the Nordic seas. The temporal water isotope (δ18O)–temperature relationship varies between 0.3 and 0.6 (±0.08) ‰ °C−1 and is systematically larger at NEEM, possibly due to limited changes in precipitation seasonality compared to GISP2, GRIP or NGRIP. The gas age−ice age difference of warming events represented in water and air isotopes can only be modeled when assuming a 26% (NGRIP) to 40% (GRIP) lower accumulation than that derived from a Dansgaard–Johnsen ice flow model.

Temporal and Spatial Patterns of Accumulation of the Transcript of Myo-Inositol-1-Phosphate Synthase and Phytin-Containing Particles during Seed Development in Rice1

Myo-inositol-1-phosphate (I[1]P) synthase (EC 5.5.1.4) catalyzes the reaction from glucose 6-phosphate to I(1)P, the first step of myo-inositol biosynthesis. Among the metabolites of I(1)P is inositol hexakisphosphate, which forms a mixed salt called phytin or phytate, a storage form of phosphate and cations in seeds. We have isolated a rice (Oryza sativa L.) cDNA clone, pRINO1, that is highly homologous to the I(1)P synthase from yeast and plants. Northern analysis of total RNA showed that the transcript accumulated to high levels in embryos but was undetectable in shoots, roots, and flowers. In situ hybridization of developing seeds showed that the transcript first appeared in the apical region of globular-stage embryos 2 d after anthesis (DAA). Strong signals were detected in the scutellum and aleurone layer after 4 DAA. The level of the transcript in these cells increased until 7 DAA, after which time it gradually decreased. Phytin-containing particles called globoids appeared 4 DAA in the scutellum and aleurone layer, coinciding with the localization of the RINO1 transcript. The temporal and spatial patterns of accumulation of the RINO1 transcript and globoids suggest that I(1)P synthase directs phytin biosynthesis in rice seeds.

From ""Geography of Accumulation"" to ""Geography of Reproduction"": a dialogue with Harvey

This article aims to discuss the space, revealing its powerful in the comprehension of modem world, from the thesis which the geographic space consists itself as condition, medium and product of society reproduction in its totality, evolving several temporal-spatial scales and several levels of reality, that should prolong Marx's work, having in view the construction of a ""social theory of space"" in the sense of a radical critical geography. This argumentation allows to understand, in the limits of geography, the passage of the notion ""production of space"" as condition of the accumulation of capital to the notion ""production of space"" as condition of present reproduction in front of the accumulation crisis. As a starting point, a discussion about some David Harvey's works, who supports the thesis that accumulation crisis of capital would be solved, in the modem world, through the spatial fix.

Flood pulse and spatial dynamics of mercury in sediments in Puruzinho lake, Brazilian Amazon

The study was conducted in Puruzinho lake (Humaitá, AM) considering seasonal periods of rainy and dry in way to elucidate the flood pulse importance in the deposition, remobilization and distributions of mercury and organic matter in bottom sediments in the Madeira River Basin (Brazilian Amazon). Bottom sediments and soils samples were analyzed for total mercury and organic matter. Mercury concentrations obtained in bottom sediment were 32.20-146.40 ng g-1 and organic matter values were 3.5 - 18.0%. The main region for accumulation of mercury and organic matter was in the central and deepest lake area In the rainy season there was a greater distribution of Hg and organic matter, mainly controlled by means of income of the Madeira river water during flooding, while the predominant process in the dry season was the remobilization of total Hg due to the resuspension of bottom sediments.