Ueber das Verhältniß verschiedener Religionsparteien zum Staate und über die Emancipation der Juden : noch ein dikäopolitischer Versuch

vom ... [Wilhelm Traugott] Krug

Climate and soil attributes determine plant species turnover in global drylands

Aim Geographical, climatic and soil factors are major drivers of plant beta diversity, but their importance for dryland plant communities is poorly known. The aim of this study was to: (1) characterize patterns of beta diversity in global drylands; (2) detect common environmental drivers of beta diversity; and (3) test for thresholds in environmental conditions driving potential shifts in plant species composition. Location Global. Methods Beta diversity was quantified in 224 dryland plant communities from 22 geographical regions on all continents except Antarctica using four complementary measures: the percentage of singletons (species occurring at only one site); Whittaker's beta diversity, β(W); a directional beta diversity metric based on the correlation in species occurrences among spatially contiguous sites, β(R2); and a multivariate abundance-based metric, β(MV). We used linear modelling to quantify the relationships between these metrics of beta diversity and geographical, climatic and soil variables. Results Soil fertility and variability in temperature and rainfall, and to a lesser extent latitude, were the most important environmental predictors of beta diversity. Metrics related to species identity percentage of singletons and β(W) were most sensitive to soil fertility, whereas those metrics related to environmental gradients and abundance (β(R2) and β(MV) were more associated with climate variability. Interactions among soil variables, climatic factors and plant cover were not important determinants of beta diversity. Sites receiving less than 178 mm of annual rainfall differed sharply in species composition from more mesic sites (> 200 mm). Main conclusions Soil fertility and variability in temperature and rainfall are the most important environmental predictors of variation in plant beta diversity in global drylands. Our results suggest that those sites annually receiving c. 178 mm of rainfall will be especially sensitive to future climate changes. These findings may help to define appropriate conservation strategies for mitigating effects of climate change on dryland vegetation.

Das Haus Rothschild : eine historisch-biographische Skizze

von Heinrich Döring

Human impacts and aridity differentially alter soil N availability in drylands worldwide

Aims Climate and human impacts are changing the nitrogen (N) inputs and losses in terrestrial ecosystems. However, it is largely unknown how these two major drivers of global change will simultaneously influence the N cycle in drylands, the largest terrestrial biome on the planet. We conducted a global observational study to evaluate how aridity and human impacts, together with biotic and abiotic factors, affect key soil variables of the N cycle. Location Two hundred and twenty-four dryland sites from all continents except Antarctica widely differing in their environmental conditions and human influence. Methods Using a standardized field survey, we measured aridity, human impacts (i.e. proxies of land uses and air pollution), key biophysical variables (i.e. soil pH and texture and total plant cover) and six important variables related to N cycling in soils: total N, organic N, ammonium, nitrate, dissolved organic:inorganic N and N mineralization rates. We used structural equation modelling to assess the direct and indirect effects of aridity, human impacts and key biophysical variables on the N cycle. Results Human impacts increased the concentration of total N, while aridity reduced it. The effects of aridity and human impacts on the N cycle were spatially disconnected, which may favour scarcity of N in the most arid areas and promote its accumulation in the least arid areas. Main conclusions We found that increasing aridity and anthropogenic pressure are spatially disconnected in drylands. This implies that while places with low aridity and high human impact accumulate N, most arid sites with the lowest human impacts lose N. Our analyses also provide evidence that both increasing aridity and human impacts may enhance the relative dominance of inorganic N in dryland soils, having a negative impact on key functions and services provided by these ecosystems.

Aceite esencial de tomillo como antioxidante y conservador de hamburguesas funcionales

Para determinar el poder antioxidante y conservante del aceite esencial de tomillo mendocino (Acantholippia seriphioides) en hamburguesas funcionales, conservadas a 4 ± 0.5 °C, se elaboraron medallones utilizando: 83 % carne vacuna 5 % grasa vacuna 5 % salvado de avena 5 % texturizado de soja 2 % sustituto graso 0.08 g NaCl/kg aceite esencial de tomillo (AET) 106 ufc/g Se estudió: • tipo de envasado: bolsas de poliamidapolietileno; atmósfera modificada: 70 % N 2 y 30 % CO2, y vacío; • tiempo de almacenamiento: 0, 1, 2, 3 y 4 semanas; • dosis de tomillo: 0 y 150 mg AET/kg Los datos se analizaron de acuerdo con un arreglo factorial 2 (tipo de envasado) x 5 (tiempos de almacenamiento) x 2 (dosis de AET) en un diseño de parcelas subdivididas, con 4 repeticiones. Se evaluaron TBA, pH, NBV, color, olor y carga microbiana. Las tres primeras variables se estudiaron mediante el ANOVA. Para color y olor se recurrió a un análisis sensorial descriptivo. La carga microbiana se representó gráficamente. El AET disminuyó el TBA, independientemente del tipo de envasado utilizado. El pH disminuyó en el tiempo siguiendo un modelo polinomial de 2° grado. El NBV resultó significativo para: envasamiento al vacío y 0 mg/kg AET. El AET mantiene los atributos sensoriales durante las dos primeras semanas pero no disminuye la carga microbiana. Conclusión: el AET tiene efecto antioxidante pero no conservante en hamburguesas funcionales de carne vacuna bajo las condiciones del ensayo.

El mercado de tierras en las fronteras interiores argentinas. La expansión territorial de Buenos Aires y Santiago del Estero en la segunda mitad del siglo XIX

En este trabajo proponemos una mirada comparativa de la expansión territorial de las provincias argentinas de Buenos Aires y Santiago del Estero entre las décadas de 1850 y 1890. Mediante la conjunción de estudios regionales verificamos los mecanismos de apropiación de las tierras públicas, la emergencia de un aparato legal que intentará regular las prácticas de ocupación y la incorporación de agentes económicos de alcance regional y nacional, en algunos casos invirtiendo en ambas provincias. Este proceso cobrará un fuerte impulso durante la segunda mitad del siglo xix, incorporando nuevos espacios al mercado mundial de tierras y bienes primarios. Estudiamos los mecanismos de conformación del mercado nacional de tierras, en qué momento y a ravés de qué tipo de transacciones algunos empresarios bonaerenses comenzaron a tomar tierras en los nuevos mercados que se brían en las alejadas fronteras internas del norte y quiénes fueron estos inversores

Biogeochemical investigation of the benthic nitrogen cycle in the Arabian Sea off Pakistan

A pronounced deficit of nitrogen (N) in the oxygen minimum zone (OMZ) of the Arabian Sea suggests the occurrence of heavy N-loss that is commonly attributed to pelagic processes. However, the OMZ water is in direct contact with sediments on three sides of the basin. Contribution from benthic N-loss to the total N-loss in the Arabian Sea remains largely unassessed. In October 2007, we sampled the water column and surface sediments along a transect cross-cutting the Arabian Sea OMZ at the Pakistan continental margin, covering a range of station depths from 360 to 1430 m. Benthic denitrification and anammox rates were determined by using 15N-stable isotope pairing experiments. Intact core incubations showed declining rates of total benthic N-loss with water depth from 0.55 to 0.18 mmol N m**-2 day**-1. While denitrification rates measured in slurry incubations decreased from 2.73 to 1.46 mmol N m**-2 day**-1 with water depth, anammox rates increased from 0.21 to 0.89 mmol N m**-2 day**-1. Hence, the contribution from anammox to total benthic N-loss increased from 7% at 360 m to 40% at 1430 m. This trend is further supported by the quantification of cd1-containing nitrite reductase (nirS), the biomarker functional gene encoding for cytochrome cd1-Nir of microorganisms involved in both N-loss processes. Anammox-like nirS genes within the sediments increased in proportion to total nirS gene copies with water depth. Moreover, phylogenetic analyses of NirS revealed different communities of both denitrifying and anammox bacteria between shallow and deep stations. Together, rate measurement and nirS analyses showed that anammox, determined for the first time in the Arabian Sea sediments, is an important benthic N-loss process at the continental margin off Pakistan, especially in the sediments at deeper water depths. Extrapolation from the measured benthic N-loss to all shelf sediments within the basin suggests that benthic N-loss may be responsible for about half of the overall N-loss in the Arabian Sea.

El mercado de tierras en las fronteras interiores argentinas. La expansión territorial de Buenos Aires y Santiago del Estero en la segunda mitad del siglo XIX

En este trabajo proponemos una mirada comparativa de la expansión territorial de las provincias argentinas de Buenos Aires y Santiago del Estero entre las décadas de 1850 y 1890. Mediante la conjunción de estudios regionales verificamos los mecanismos de apropiación de las tierras públicas, la emergencia de un aparato legal que intentará regular las prácticas de ocupación y la incorporación de agentes económicos de alcance regional y nacional, en algunos casos invirtiendo en ambas provincias. Este proceso cobrará un fuerte impulso durante la segunda mitad del siglo xix, incorporando nuevos espacios al mercado mundial de tierras y bienes primarios. Estudiamos los mecanismos de conformación del mercado nacional de tierras, en qué momento y a ravés de qué tipo de transacciones algunos empresarios bonaerenses comenzaron a tomar tierras en los nuevos mercados que se brían en las alejadas fronteras internas del norte y quiénes fueron estos inversores

El mercado de tierras en las fronteras interiores argentinas. La expansión territorial de Buenos Aires y Santiago del Estero en la segunda mitad del siglo XIX

En este trabajo proponemos una mirada comparativa de la expansión territorial de las provincias argentinas de Buenos Aires y Santiago del Estero entre las décadas de 1850 y 1890. Mediante la conjunción de estudios regionales verificamos los mecanismos de apropiación de las tierras públicas, la emergencia de un aparato legal que intentará regular las prácticas de ocupación y la incorporación de agentes económicos de alcance regional y nacional, en algunos casos invirtiendo en ambas provincias. Este proceso cobrará un fuerte impulso durante la segunda mitad del siglo xix, incorporando nuevos espacios al mercado mundial de tierras y bienes primarios. Estudiamos los mecanismos de conformación del mercado nacional de tierras, en qué momento y a ravés de qué tipo de transacciones algunos empresarios bonaerenses comenzaron a tomar tierras en los nuevos mercados que se brían en las alejadas fronteras internas del norte y quiénes fueron estos inversores

Collection of data on particulate and dissolved soil phosphorus in the Jena Experiment (Main Experiment, time series since 2002)

This data set contains two time series of measurements of dissolved phosphorus (organic, inorganic and total with a biweekly resolution) and dissolved inorganic phosphorus with a seasonal resolution. In addition, data on phosphorus from soil samples measured in 2007 and fractionated by different acid-extrations (Hedley fractions) are provided. All data measured at the main experiment plots of a large grassland biodiversity experiment (the Jena Experiment; see further details below). In the main experiment, 82 grassland plots of 20 x 20 m were established from a pool of 60 species belonging to four functional groups (grasses, legumes, tall and small herbs). In May 2002, varying numbers of plant species from this species pool were sown into the plots to create a gradient of plant species richness (1, 2, 4, 8, 16 and 60 species) and functional richness (1, 2, 3, 4 functional groups). Plots were maintained by bi-annual weeding and mowing. 1. Dissolved phosphorus in soil solution: Suction plates installed on the field site in 10, 20, 30 and 60 cm depth were used to sample soil pore water. Cumulatively extracted soil solution was collected every two weeks from October 2002 to May 2006. The biweekly samples from 2002, 2003 and 2004 were analyzed for dissolved organic phosphorus (DOP), dissolved inorganic phosphorus (PO4P) and dissolved total phosphorus (TDP) by Continuous Flow Analyzer (CFA SAN ++, SKALAR [Breda, The Netherlands]). 2. Seasonal values of dissolved inorganic phosphorus in soil solution were calculated as volume-weighted mean values of the biweekly measurements (spring = March to May, summer = June to August, fall = September to November, winter = December to February). 3. Phosphorus fractions in soil: Five independent soil samples per plot were taken in a depth of 0-15 cm using a soil corer with an inner diameter of 1 cm. The five samples per plot were combined to one composite sample per plot. A four-step sequential P fractionation (Hedley fractions) was applied and concentrations of P fractions in soil were measured photometrically (molybdenum blue-reactive P) with a Continuous Flow Analyzer (Bran&Luebbe, Germany).