A comparison of the nitrogen metabolic networks of Kluyveromyces marxianus and Saccharomyces cerevisiae

In grape must, nitrogen is available as a complex mixture of various compounds (ammonium and amino acids). Wine yeasts assimilate these multiple sources in order to suitably fulfil their anabolic requirements during alcoholic fermentation. Nevertheless, the order of uptake and the intracellular fate of these sources are likely to differ between strains and species. Using a two-pronged strategy of isotopic filiation and RNA sequencing, the metabolic network of nitrogen utilization and its regulation in Kluyveromyces marxianus were described, in comparison with those of Saccharomyces cerevisiae. The data highlighted differences in the assimilation of ammonium and arginine between the two species. The data also revealed that the metabolic fate of certain nitrogen sources differed, thereby resulting in the production of various amounts of key wine aroma compounds. These observations were corroborated by the gene expression analysis.     

Neuronal Shot Noise and Brownian 1/f2 Behavior in the Local Field Potential

We demonstrate that human electrophysiological recordings of the local field potential (LFP) from intracranial electrodes, acquired from a variety of cerebral regions, show a ubiquitous 1/f² scaling within the power spectrum. We develop a quantitative model that treats the generation of these fields in an analogous way to that of electronic shot noise, and use this model to specifically address the cause of this 1/f² Brownian noise. The model gives way to two analytically tractable solutions, both displaying Brownian noise: 1) uncorrelated cells that display sharp initial activity, whose extracellular fields slowly decay in time and 2) rapidly firing, temporally correlated cells that generate UP-DOWN states.     

Mayday - integrative analytics for expression data

Background  

DNA Microarrays have become the standard method for large scale analyses of gene expression and epigenomics. The increasing complexity and inherent noisiness of the generated data makes visual data exploration ever more important. Fast deployment of new methods as well as a combination of predefined, easy to apply methods with programmer's access to the data are important requirements for any analysis framework. Mayday is an open source platform with emphasis on visual data exploration and analysis. Many built-in methods for clustering, machine learning and classification are provided for dissecting complex datasets. Plugins can easily be written to extend Mayday's functionality in a large number of ways. As Java program, Mayday is platform-independent and can be used as Java WebStart application without any installation. Mayday can import data from several file formats, database connectivity is included for efficient data organization. Numerous interactive visualization tools, including box plots, profile plots, principal component plots and a heatmap are available, can be enhanced with metadata and exported as publication quality vector files.     

Climate‐driven rampant speciation of the Cape flora

Aim To test whether the radiation of the extremely rich Cape flora is correlated with marine‐driven climate change. Location Middle to Late Miocene in the south‐east Atlantic and the Benguela Upwelling System (BUS) off the west coast of South Africa. Methods We studied the palynology of the thoroughly dated Middle to Late Miocene sediments of Ocean Drilling Program (ODP) Site 1085 retrieved from the Atlantic off the mouth of the Orange River. Both marine upwelling and terrestrial input are recorded at this site, which allows a direct correlation between changes in the terrestrial flora and the marine BUS in the south‐east Atlantic. Results Pollen types from plants of tropical affinity disappeared, and those from the Cape flora gradually increased, between 10 and 6 Ma. Our data corroborate the inferred dating of the diversification in Aizoaceae c. 8 Ma. Main conclusions Inferred vegetation changes for the Late Miocene south‐western African coast are the disappearance of Podocarpus‐dominated Afromontane forests, and a change in the vegetation of the coastal plain from tropical grassland and thicket to semi‐arid succulent vegetation. These changes are indicative of an increased summer drought, and are in step with the development of the southern BUS. They pre‐date the Pliocene uplift of the East African escarpment, suggesting that this did not play a role in stimulating vegetation change. Some Fynbos elements were present throughout the recorded period (from 11 Ma), suggesting that at least some elements of this vegetation were already in place during the onset of the BUS. This is consistent with a marine‐driven climate change in south‐western Africa triggering substantial radiation in the terrestrial flora, especially in the Aizoaceae.     

Seasonality in the altitude–diversity pattern of Alpine moths

Altitudinal gradients are frequently used to study environmental effects on species diversity. Recent quantitative studies on Lepidoptera focussed on tropical mountain systems and often reported unimodal diversity peaks at “mid-elevations”;, a pattern also often found in other taxa. Here we used methodologically comparable, nocturnal Macrolepidoptera samples from the Swiss Alps to analyze environmental correlates of diversity. Using seasonal data (monthly samples from April to November at altitudes between 600 and 2400 m a.s.l.) allowed to decouple altitude and some climate variables for analyses. We found that the altitude–diversity pattern changes with season. In spring and autumn, diversity decreased with increasing altitude, while we found a unimodal peak of diversity at mid-elevations during summer. This excluded all hypothetical causes of diversity variation that do not allow for seasonality. Temperature was an important correlate of diversity, whereas precipitation was not. These results were separately corroborated for the two most common families (Noctuidae and Geometridae). However, diversity patterns of the two families were not particularly close, and unexplained variance of climatic explanations was substantial in all cases. The patterns of faunal overlap did not explain the unimodal diversity pattern, and we claim that we lack a generally valid explanation for this common phenomenon.     

Effect of iron and/or vitamin A re-supplementation on vitamin A and iron status of rats after a dietary deficiency of both components

Iron and vitamin A deficiency are common nutritional problems in developing countries. From animal experiments and intervention studies, growing evidence is pointing to a possible influence of iron on vitamin A metabolism. We assessed the affects of an oral supplementation of vitamin A and/or iron on the recovery of rats from vitamin A and iron deficiency. Weanling male Wistar rats were kept for four weeks on an iron and vitamin A deficient diet. Thereafter, rats were repleted with iron 35 mg/kg feed, with vitamin A 4500 IU/kg feed both, or with iron 35 mg/kg and vitamin A 4500 IU/kg for five weeks. Retinol and retinyl esters in plasma and tissues were determined by HPLC. Iron was determined by atomic absorption spectrophotometry. The determination of haematological parameters showed that rats developed an anaemia during depletion. This was reversed by the re-supplementation with iron but not vitamin A alone. The simultaneous supplementation of vitamin A was of no additional benefit. When rats were resupplemented with iron alone a substantial further decrease in plasma retinol (P < 0.002) and liver vitamin A (P < 0.05) was observed. A similar but less pronounced decrease in plasma retinol was observed in the rats re-supplemented with vitamin A alone, despite a substantial increase in liver vitamin A (P < 0.002). Despite lower liver vitamin A levels compared to the group re-supplemented with vitamin A lone, the group re-supplemented with iron and vitamin A had substantial higher plasma levels compared to the one supplemented with iron alone (P < 0.002). In conclusion, the study supports an interaction of iron and vitamin A on the level of retinol transport in plasma. Despite a comparable availability of vitamin A as indicated by the comparable liver levels only the re-supplementation of both iron and vitamin A can normalize the retinol level in plasma. This might be of nutritional consequence in developing countries with regard to the supplementation regime of both nutrients iron and vitamin A to prevent a functional deficiency of vitamin A despite sufficient dietary availability.     

An expert system model for mapping tropical wetlands and peatlands reveals South America as the largest contributor

Wetlands are important providers of ecosystem services and key regulators of climate change. They positively contribute to global warming through their greenhouse gas emissions, and negatively through the accumulation of organic material in histosols, particularly in peatlands. Our understanding of wetlands’ services is currently constrained by limited knowledge on their distribution, extent, volume, interannual flood variability and disturbance levels. We present an expert system approach to estimate wetland and peatland areas, depths and volumes, which relies on three biophysical indices related to wetland and peat formation: (1) long‐term water supply exceeding atmospheric water demand; (2) annually or seasonally water‐logged soils; and (3) a geomorphological position where water is supplied and retained. Tropical and subtropical wetlands estimates reach 4.7 million km² (Mkm²). In line with current understanding, the American continent is the major contributor (45%), and Brazil, with its Amazonian interfluvial region, contains the largest tropical wetland area (800,720 km²). Our model suggests, however, unprecedented extents and volumes of peatland in the tropics (1.7 Mkm² and 7,268 (6,076–7,368) km³), which more than threefold current estimates. Unlike current understanding, our estimates suggest that South America and not Asia contributes the most to tropical peatland area and volume (ca. 44% for both) partly related to some yet unaccounted extended deep deposits but mainly to extended but shallow peat in the Amazon Basin. Brazil leads the peatland area and volume contribution. Asia hosts 38% of both tropical peat area and volume with Indonesia as the main regional contributor and still the holder of the deepest and most extended peat areas in the tropics. Africa hosts more peat than previously reported but climatic and topographic contexts leave it as the least peat‐forming continent. Our results suggest large biases in our current understanding of the distribution, area and volumes of tropical peat and their continental contributions.