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Background: Occupational demands of educators are not very well researched. Nevertheless their work is subject to several requirements. Whether these demands have an effect on the work ability and the health status of employees has also not been examined. Furthermore it is unclear if the ownership type of day care centres have an influence on job satisfaction and work ability of the pedagogical staff and what kind of resources do exist. Previous studies were mainly based on questionnaire data. Objective data does not exist. Therefore the aim of this investigation is to collect precise data relating to work of educators.
Methods: Effects of different types of ownership of day care centres on job satisfaction and work ability of educators will be assessed with the help of objective real time studies in combination with multi-level psycho diagnostic measurements.
Discussion: The present study is the first of its kind. Up to now there are no computer-based real time studies on workflow of pedagogical staff with regard to assess their work-related stress. Following an exhaustive documentation of educators work processes the day-to-day task can be estimated and approaches for prevention can be developed. This can substantially contribute to an overall improvement of child care in Germany.
Background: Due to constantly rising air pollution levels as well as an increasing awareness of the hazardousness of air pollutants, new laws and rules have recently been passed. Although there has been a large amount of research on this topic, bibliometric data is still to be collected. Thus this study provides a scientometric approach to the material published on this subject so far.
Methods: For this purpose, data retrieved from the "Web of Science" provided by the Thomson Scientific Institute was analyzed and visualized both with density-equalizing methods and classic data-processing methods such as tables and charts.
Results: For the time span between 1955 and 2006, 26,253 items were listed and related to the topic of air pollution, published by 124 countries in 24 different languages. General citation activity has been constantly increasing since the beginning of the examined period. However, beginning with the year 1991, citation levels have been rising exponentially each year, reaching 39,220 citations in the year 2006. The United States, the UK and Germany were the three most productive countries in the area, with English and German ranked first and second in publishing languages, followed by French. An article published by Dockery, Pope, Xu et al. was both the most cited in total numbers and in average citation rate. J. Schwartz was able to claim the highest total number of citations on his publications, while D.W. Dockery has the highest citation rate per publication. As to the subject areas the items are assigned with, the most item were published in Environmental Sciences, followed by Meteorology & Atmospheric Sciences and Public, Environmental & Occupational Health. Nine out of the ten publishing journals with more than 300 entries dealt with environmental interests and one dealt with epidemiology.
Conclusions: Using the method of density-equalizing mapping and further common data processing procedures, it can be concluded that scientific work concerning air pollution and related topics enjoys unbrokenly growing scientific interest. This can be observed both in publication numbers and in citation activity.
Background: Leishmaniasis is a chronic disease that is found in various countries of the world. The aim of the current study was to investigate the impact of leishmaniasis on the world's research output. The present study assessed benchmarking of research output for the period between 1957 and 2006. Using large database analyses, research in the field of leishmaniasis was evaluated. Furthermore, cooperation between different countries was identified.
Results: The number of publications increased with time. Most publications came from Western countries such as the US, UK or Germany. Interestingly, countries like Brazil and India had a high research output. We found a substantial amount of cooperation between countries.
Conclusion: Although leishmaniasis is of limited geographic distribution it attracts a wide research interest. The central hub of research cooperation is the USA.
Soil biogenic NO emissions (SNOx) play important direct and indirect roles in chemical processes of the troposphere. The most widely applied algorithm to calculate SNOx in global models was published 15 years ago by Yienger and Levy (1995), was based on very few measurements. Since then numerous new measurements have been published, which we used to build up a atabase of field measurements conducted world wide covering the period from 1978 to 2009, including 108 publications with 560 measurements.
Recently, several satellite based top-down approaches, which recalculated the different sources of NOx (fossil fuel, biomass burning, soil and lightning), have shown an underestimation of SNOx by the algorithm of Yienger and Levy (1995). Nevertheless, to our knowledge no general improvements of this algorithm have yet been published.
Here we present major improvements to the algorithm, which should help to optimize the representation of SNOx in atmospheric-chemistry global climate models, without modifying the underlying principal or mathematical equations. The changes include: 1) Using a new up to date land cover map, with twice the number of land cover classes, and using annually varying fertilizer application rates; 2) Adopting the fraction of SNOx induced by fertilizer application based on our database; 3) Switching from soil water column to volumetric soil moisture, to distinguish between the wet and dry state; 4) Tuning the emission factors to reproduce the measured emissions in our database and calculate the emissions based on their mean value. These steps lead us to increased global yearly SNOx, and our total SNOx source ends up being close to one of the top-down approaches. In some geographical regions the new results agree better with the top-down approach, but there are also distinct differences in other regions. This suggests that a ombination of both top-down and bottom-up approaches could be combined in a future attempt to provide an even better calculation of SNOx.
Residual circulation trajectories and transit times into the extratropical lowermost stratosphere
(2010)
Transport into the extratropical lowermost stratosphere (LMS) can be divided into a slow part (time-scale of several months to years) associated with the global-scale stratospheric residual circulation and a fast part (time-scale of days to a few months) associated with (mostly quasi-horizontal) mixing (i.e. two-way irreversible transport, including stratosphere-troposphere exchange). The stratospheric residual circulation can be considered to consist of two branches: a deep branch more strongly associated with planetary waves breaking in the middle to upper stratosphere, and a shallow branch more strongly associated with synoptic-scale waves breaking in the subtropical lower stratosphere. In this study the contribution due to the stratospheric residual circulation alone to transport into the LMS is quantified using residual circulation trajectories, i.e. trajectories driven by the (time-dependent) residual mean meridional and vertical velocities. This contribution represents the advective part of the overall transport into the LMS and can be viewed as providing a background onto which the effect of mixing has to be added. Residual mean velocities are obtained from a comprehensive chemistry-climate model as well as from reanalysis data. Transit times of air traveling from the tropical tropopause to the LMS along the residual circulation streamfunction are evaluated and compared to recent mean age of air estimates. A clear time-scale separation with much smaller transit times into the mid-latitudinal LMS than into polar LMS is found that is indicative of a clear separation of the shallow from the deep branch of the residual circulation. This separation between the shallow and the deep circulation branch is further manifested in a clear distinction in the aspect ratio of the vertical to meridional extent of the trajectories as well as the integrated mass flux along the residual circulation trajectories. The residual transit time distribution reproduces qualitatively the observed seasonal cycle of youngest air in the extratropical LMS in fall and oldest air in spring.
Tubular carbonate concretions of up to 1 m in length and perpendicular to bedding, occur abundantly in the Upper Pliensbachian (upper Amaltheus margaritatus Zone, Gibbosus Subzone) in outcrops (Fontaneilles section) in the vicinity of Rivière-sûr-Tarn, southern France. Stable isotope analyses of these concretions show negative δ13C values that decrease from the rim to the center from −18.8‰ to −25.7‰ (V-PDB), but normal marine δ18O values (−1.8‰). Carbon isotope analyses of Late Pliensbachian bulk carbonate (matrix) samples from the Fontaneilles section show clearly decreasing C-isotope values across the A. margaritatus Zone, from +1‰ to −3‰ (V-PDB). Isotope analyses of coeval belemnite rostra do not document such a negative C-isotope trend with values remaining stable around +2‰ (V-PDB). Computer tomographic (CT) scanning of the tubular concretions show multiple canals that are lined or filled entirely with pyrite. Previously, the formation of these concretions with one, two, or more central tubes, has been ascribed to the activity of an enigmatic organism, possibly with annelid or arthropod affinities, known as Tisoa siphonalis. Our results suggest tisoan structures are abiogenic. Based on our geochemical analyses and sedimentological observations we suggest that these concretions formed as a combination of the anaerobic oxidation of methane (AOM) and sulfate reduction within the sediment. Fluids rich in methane and/or hydrocarbons likely altered local bulk rock carbon isotope records, but did not affect the global carbon cycle. Interestingly, Tisoa siphonalis has been described from many locations in the Grands Causses Basin in southern France, and from northern France and Luxemburg, always occurring at the same stratigraphic level. Upper Pliensbachian authigenic carbonates thus possibly cover an area of many thousand square kilometers. Greatly reduced sedimentation rates are needed to explain the stabilization of the sulfate-methane transition zone in the sedimentary column in order for the tubular concretions to form. Late Pliensbachian cooling, reducing run-off, and/or the influx of colder water and more vigorous circulation could be responsible for a halt in sedimentation. At the same time (thermogenic) methane may have destabilized during a major phase of Late Pliensbachian sea level fall. As such Tisoa siphonalis is more than a geological curiosity, and its further study could prove pivotal in understanding Early Jurassic paleoenvironmental change.
Floodplains play an important role in the terrestrial water cycle and are very important for biodiversity. Therefore, an improved representation of the dynamics of floodplain water flows and storage in global hydrological and land surface models is required. To support model validation, we combined monthly time series of satellite-derived inundation areas (Papa et al., 2010) with data on irrigated rice areas (Portmann et al., 2010). In this way, we obtained global-scale time series of naturally inundated areas (NIA), with monthly values of inundation extent during 1993–2004 and a spatial resolution of 0.5°. For most grid cells (0.5°×0.5°), the mean annual maximum of NIA agrees well with the static open water extent of the Global Lakes and Wetlands database (GLWD) (Lehner and Döll, 2004), but in 16% of the cells NIA is larger than GLWD. In some regions, like Northwestern Europe, NIA clearly overestimates inundated areas, probably because of confounding very wet soils with inundated areas. In other areas, such as South Asia, it is likely that NIA can help to enhance GLWD. NIA data will be very useful for developing and validating a floodplain modeling algorithm for the global hydrological model WGHM. For example, we found that monthly NIAs correlate with observed river discharges.
Introduction: Researchers experience increasing pressures to connect with bodies that finance their projects. In this climate, critical scholars face many obstacles as they seek to navigate the treacherous waters of securing external funds. To debate these challenges, the ACME Editorial Collective organized a panel for the 2009 Annual Meeting of the Association of American Geographers in Las Vegas. This intervention represents a follow-up discussion and collective writing process among some of the panelists and members of the audience who attended the panel.
Below, we examine the neoliberalization of the current funding systems, discuss the implications for research practice, and make suggestions for critical engagement and transformation. Our suggestions, however, will not be easy to implement, as we can infer from the experience of the radical scholars of the post-1968 generation whose ascension into the upper echelons of North American and European university systems was also associated with the neoliberalization of the funding systems. This intervention represents a modest contribution in the tradition of critical research practice of creating the possibilities for progressive change.
The KADoNiS (Karlsruhe Astrophysical Database of Nucleosynthesis in Stars) project is an online
database (www.kadonis.org) for cross sections relevant to the s-process and the p-process.
The first version was an updated sequel to the previous Bao et al. [1] compilations from 1987
and 2000 for (n; g) cross sections relevant to Big Bang and s-process nucleosynthesis. The first
update, KADoNiS v0.2, was published in 2006 [2]. It contained mainly Maxwellian averaged
(n; g) cross sections relevant to the s-process, and some experimental charged particle induced
reaction relevant to the p-process. After that a second update was presented in 2009 [3].
Recently, we started to collect and review all existing experimental data relevant for p-process
nucleosynthesis and to provide a user-friendly database based on the KADoNiS framework. The
p-process part of the KADoNiS database is currently being extended and will include all available
experimental data from (p; g), (p;n), (p;a), (a,g), (a;n) and (a; p) reactions in or close to the
respective Gamow window.
Tumor hypoxia and nutrient starvation are common phenomena in cancerous tissue. Cells that resist this hostile environment are selected for a more aggressive phenotype, usually accompanied by therapy resistance. The hypoxia inducible factors HIF-1a and HIF-2a play a key role in the adaptive homeostatic responses to these challenging conditions inducing a number of target genes that are involved in the regulation of a variety of cellular processes such as angiogenesis, proliferation, metabolism, self-renewal and cell death/cycle arrest. Thus, the HIF pathway encompasses opposing adaptive responses on tumor growthgrowth promoting abilities on the one hand and growth inhibiting on the other. A recent study in our lab uncovered that this switch between cell death and cell survival critically depends on HIF-2a protein levels. Since PHDs (HIF prolyl hydroxylases) are the main regulators of HIF protein abundance and hypoxia drives the malignant phenotype of tumors, we wanted to characterize HIF regulatory functions of PHDs under hypoxic conditions. Our intention was to reveal the importance of PHD contribution to the opposing functions of HIFs under hypoxia. Characterization of PHD1-4 mRNA and protein expression levels under normoxic and hypoxic conditions in glioblastoma cell lines led to the identification of PHD2 and PHD3 as hypoxia inducible PHD isoforms and highlighted their predominant function under hypoxia. Mechanistically, we demonstrated that HIF mediates the hypoxic induction of PHD2 and 3 within a negative feedback loop, promoting its own degradation during prolonged hypoxia. The functional impact of PHD2 and 3 abundance on cell viability under hypoxic conditions was analyzed by disrupting PHD2 and PHD3 function either through a siRNA mediated approach or by application of the PHD inhibitor DMOG. These experiments uncovered that PHD2 and 3 are protective under hypoxic conditions and that PHD inhibition expedites cell death. Combined HIF and PHD suppression under hypoxic conditions abrogated this increased susceptibility to cell death, clearly showing that PHD2 and 3 act in a negative feedback regulatory loop to limit the HIF response under prolonged hypoxia. With respect to possible future therapeutical applications we co-treated cells with a PHD inhibitor and pro-apoptotic agents staurosporine or TRAIL. Co-challenging tumor cells even potentiated the cell death response, indicating a more widespread protective function of PHD. Taken together PHD2 and 3 protect tumor cells from cell death induction, functioning in a negative feedback regulatory loop to constrain the HIF dependent cell death responses under hypoxia. Interestingly, however, when assessing the role of PHD2 and PHD3 in in vivo tumor growth using an intracranial tumor model, we identified an exclusive tumor suppressor function for PHD3. Loss of PHD3 function enhanced tumor growth whereas increased PHD3 expression diminished the tumor burden. The accelerated tumor growth following PHD3 loss could be attributed to a decrease in the induction of apoptosis and an increase in proliferation. Tumor cells are frequently exposed to temporary and spatial depletion of nutrients. Interestingly, PHD3 loss conferred a growth advantage under growth factor deprivation. The growth regulatory function of PHD3 was isoform specific, HIF independent and importantly, did not require the hydroxylase function of PHD3. Previous reports have uncovered a regulatory function of the PHD system in NF-kB signaling. However, our results demonstrated that NF- kB signaling remained unaffected by alteration in the PHD3 status of the cell. Additionally, the PHD3 tumor suppressor function proved to be independent of two putative PHD3 downstream effectors, ATF4 and KIF1Bb. Mechanistically, PHD3 suppression reduced EGFR internalization, enhancing the amount of EGFR expressed on the cell surface. We further showed that the impaired EGFR internalization during PHD3 loss resulted in receptor hyperactivation under stimulated and growth factor deprived conditions. Importantly, PHD3 physcially associated with the EGFR complex as evidenced by co-immunoprecpitation. Consequently, this extended EGFR activation in PHD3 deficient cells resulted in enhanced downstream activation of EGFR signaling and increased proliferation. Consistent with the interpretation that PHD3 loss is beneficial for tumor growth, we found PHD3 promoter methylation in glioblastoma cell lines, hinting at a epigenetic mechanism to finetune PHD3 expression on top of the hypoxic driven gene regulation. Finally, we demonstrated that PHD3 tumor suppressor function is not restricted to glioblastomas since PHD3 suppression in lung adenocarcinoma accelerated subcutaneous tumor growth. With these findings, we expand the knowledge of PHD3 action from its oxygen sensing role to a regulatory function in growth factor signaling. This clearly discriminates PHD3 from the other isoforms and supports the exclusive tumor suppressor function in glioblastoma. Taken together our results identify a complex role of PHD signaling in cancer and delineate HIF dependent and HIF independent functions of the PHD system. We think that the HIF dependent protective effect of PHD2 and 3 and the HIF independent PHD3 tumor suppressor function are not mutually exclusive, but might be activated according to the heterogeneous intra-tumoral conditions. However, PHD3 hydroxylase activity is dispensable for its HIFindependent tumor suppressor function in glioma. This uncouples PHD3 function from co-factor and co-substrate requirements and allows it to act over a broader physiological range, since its influence on cellular processes is not constrained by the availability of rate limiting factors. It might explain, why the enzymatic independent functions of PHD3 predominate in vivo. Thus, therapeutic modulation of the PHD system to inhibit tumor growth has to be based on these contrasting functions of the PHD system. However, their differential dependence on the hydroxylase activity may facilitate a therapeutic strategy to specifically inhibit or promote the protective versus suppressive functions of the PHD system.