Paleomagnetic measurements of 10 sediment profiles from the Antarctic continental slope

Die im Rahmen des zweijährigen Forschungsprojekts über paläomagnetisch-sedimentologische Analysen sedimentärer Zyklen in der Weddell See und ihre stratigraphische Interpretation durchgeführten Arbeiten lieferten Ergebnisse zur Geschichte glaziomariner Sedimentationsprozesse am antarktischen Kontinentalrand. So konnte für ein Kernprofil mit einer außergewöhnlichen Terassenstruktur eine fazielle Gliederung und stratigraphische Einordnung erreicht werden, die auch auf größere Areale in der Weddell See anwendbar sind. Aufgrund der stratigraphischen Randbedingungen konnten die gewonnenen paläo- und gesteinsmagnetischen Messungen in eine Altersstruktur integriert und zusammen mit den sedimentologischen Parametern im Hinblick auf lokale und regionale Umweltveränderungen interpretiert werden. Insbesondere die gesteinsmagnetischen Analysen haben gezeigt, daß die magnetische Kornfraktion als accessorischer Bestandteil im Gesamtsediment dennoch an die Sortierungsprozesse des terrigenen Sedimenteintrags gekoppelt ist. Die ungewöhnlich deutlichen Variationen korngrößenabhängiger Parameter zeigten weiterhin, daß in Verbindung mit einer hochauflösenden Stratigraphie die magnetische Detailanalyse und ein besseres Verständnis der Sedimentationsprozesse in der Nähe der Schelfeiskante und speziell bei Meeresspiegeltiefständen die Möglichkeit eröffnen, unmittelbar Aussagen über die Bewegungen der Schelfeise und die Qualität der Meereisbedeckungen zu machen. Die gezielte Fortsetzung dieser Arbeiten in anderen Arealen am antarktischen Kontinentalrand ist daher wünschenswert. Die verwendeten Verfahren lassen sich mit den derzeit verfügbaren Instrumenten noch erweitern und versprechen durch die sehr sensitive Methodik detaillierte Aussagen zu glaziomarinen Sedimentationsprozessen.

Induced thermo-mechanical stress in CPV receivers with cycled high intensity light

CPV receivers are made of materials with very different lineal expansion coefficients. Strong variations in DNI due to the passage of clouds can cause sudden temperature changes that creates mechanical stress. For common solder and metal filled polymers the plastic limit could be reached causing substantial fatigue. The best forecast of receiver reliability is therefore achieved by applying an intermittent light source with nominal irradiance level and a number of cycles equal to the expected cloud passages for a given site. The UPM has developed specialized equipment, dubbed the LYSS (Light cYcling Stressing Source), for carrying out such experiments. The small thermal capacity of receivers allows simulating more than 25000 cycles per week. The number of deep transients expected for Madrid in 30 years operation, based on available data, is about 45000. We are currently using the system to cycle a ?Ge/Ag Epoxy/aluminum? receiver, which shows no degradation after 20000 cycles. The equipment can cast up to 200 and 70 W/cm2 on 0.1 and 1 cm2 cells, respectively.

Analysis of thermo-mechanical stress effects on CPV receiver under high intensity light cycles

After construction of the LYSS (Light cYcling Stressing Source) in early 2014, several CPV receivers, with and without secondary optical element (SOE) have been aged under fast transient illumination cycling,. The test plan for Madrid consisted of 50000 cycles. Receivers with poor heat spreaders showed low reliability but those with thicker metal layers passed the test well. The operation of LYSS along 8 months, after more than 250000 cycles, did not show any significant failure, except lamp reposition every 120 hours, in average. The equipment seems valid for unveiling weak receiver designs with respect to intensive illumination, in steady and transient modes.

Signal changes in the spinal cord of the rat after injection of formalin into the hindpaw: Characterization using functional magnetic resonance imaging

Changes in metabolism and local circulation occur in the spinal cord during peripheral noxious stimulation. Evidence is presented that this stimulation also causes signal intensity alterations in functional magnetic resonance images of the spinal cord during formalin-induced pain. These results indicate the potential of functional magnetic resonance imaging in assessing noninvasively the extent and intensity of spinal cord excitation in this well characterized pain model. Therefore, the aim of this study was to establish functional magnetic resonance imaging as a noninvasive method to characterize temporal changes in the spinal cord after a single injection of 50 μl of formalin subcutaneously into the hindpaw of the anesthetized rat. This challenge produced a biphasic licking activity in the freely moving conscious animal. Images of the spinal cord were acquired within 2 min, enabling monitoring of the site and the temporal evolution of the signal changes during the development of formalin-induced hyperalgesia without the need of any surgical procedure. The time course of changes in the spinal cord functional image in the isoflurane-anesthetized animal was similar to that obtained from behavioral experiments. Also, comparable physiological data, control experiments, and the inhibition of a response through application of the local anesthetic agent lidocaine indicate that the signal changes observed after formalin injection were specifically related to excitability changes in the relevant segments of the lumbar spinal cord. This approach could be useful to characterize different models of pain and hyperalgesia and, more importantly, to evaluate effects of analgesic drugs.

Repair of x-ray-induced DNA double-strand breaks in specific Not I restriction fragments in human fibroblasts: joining of correct and incorrect ends.

An assay that allows measurement of absolute induction frequencies for DNA double-strand breaks (dsbs) in defined regions of the genome and that quantitates rejoining of correct DNA ends has been used to study repair of dsbs in normal human fibroblasts after x-irradiation. The approach involves hybridization of single-copy DNA probes to Not I restriction fragments separated according to size by pulsed-field gel electrophoresis. Induction of dsbs is quantitated from the decrease in the intensity of the hybridizing restriction fragment and an accumulation of a smear below the band. Rejoining of dsbs results in reconstitution of the intact restriction fragment only if correct DNA ends are joined. By comparing results from this technique with results from a conventional electrophoresis assay that detects all rejoining events, it is possible to quantitate the misrejoining frequency. Three Not I fragments on the long arm of chromosome 21 were investigated with regard to dsb induction, yielding an identical induction rate of 5.8 X 10(-3) break per megabase pair per Gy. Correct dsb rejoining was measured for two of these Not I fragments after initial doses of 80 and 160 Gy. The misrejoining frequency was about 25% for both fragments and was independent of dose. This result appears to be representative for the whole genome as shown by analysis of the entire Not I fragment distribution. The correct rejoining events primarily occurred within the first 2 h, while the misrejoining kinetics included a much slower component, with about half of the events occurring between 2 and 24 h. These misrejoining kinetics are similar to those previously reported for production of exchange aberrations in interphase chromosomes.

The War republics in the Donbas one year after the outbreak of the conflict. OSW Commentary Number 174, 17 June 2015

More than one year since the first pro-Russian moves in the Donbas, separatists have taken control of parts of the Donbas and Luhansk oblasts but are still unable to form truly functioning administrative structures. The exercise of power by the central administration of the so-called ‘Donetsk People’s Republic’ (DPR) and ‘Luhansk People’s Republic’ (LPR) is restricted to resolving problems as they arise, while administration proper is the prerogative of the local authorities reporting to them which had been performing this function before the conflict broke out. The way the situation is developing and the fact that access to information is restricted make it difficult to determine the structure of the separatist government in more detail, precisely how it is organised, and what the internal hierarchy is like. The overriding goal of the governments of the DPR and the LPR is to maintain and develop their military potential. In effect, the lives of the so-called republics are subordinate to military goals. The Donbas separatism is a conglomerate of different groups of interests, with Russia at the fulcrum. Its representatives set the main tactical and strategic goals and thus have a decisive influence on the development of the situation in the region. Individual separatist groupings come into conflict, and some oligarchs linked to the former Party of Regions circles have also been making attempts to maintain their influence. The struggle between individual groups of interest is intensifying as the situation on the war front becomes calmer. Since the situation has temporarily stabilised after the seizure of Debaltseve, the central governments of the DPR and the LPR have made attempts to expand their influence, combating armed criminals who are outside their control and that of Russia. The civilian population is taking the brunt of the devastation caused by the war and the increasing militarisation of the region. Despite the fact that the intensity of the fighting on the war front is falling, worsening humanitarian problems are causing refugees to continue their flight from the territories controlled by the separatists. 2 million people have fled the conflict zone since the beginning of the war: 1.3 million of them have found shelter in other regions of Ukraine, and more than 700,000 have left for Russia. The region has also sustained great economic losses – most mines have been either destroyed or closed, many industrial plants have restricted or completely discontinued their production, and many firms have been taken over by force. In effect, the region has seen an economic downturn.

Enriching plant diversity in grasslands by large-scale experimental sward disturbance and seed addition along gradients of land-use intensity

Aims The relationship between biodiversity and ecosystem functioning is among the most active areas of ecological research. Furthermore, enhancing the diversity of degraded ecosystems is a major goal in applied restoration ecology. In grasslands, many species may be locally absent due to dispersal or microsite limitation and may therefore profit from mechanical disturbance of the resident vegetation. We established a seed addition and disturbance experiment across several grassland sites of different land use to test whether plant diversity can be increased in these grasslands. Additionally, the experiment will allow us testing the consequences of increased plant diversity for ecosystem processes and for the diversity of other taxa in real-world ecosystems. Here we present details of the experimental design and report results from the first vegetation survey one year after disturbance and seed addition. Moreover, we tested whether the effects of seed addition and disturbance varied among grassland depending on their land use or pre-disturbance plant diversity. Methods A full-factorial experiment was installed in 73 grasslands in three regions across Germany. Grasslands were under regular agricultural use, but varied in the type and the intensity of management, thereby representing the range of management typical for large parts of Central Europe. The disturbance treatment consisted of disturbing the top 10 cm of the sward using a rotavator or rotary harrow. Seed addition consisted of sowing a high-diversity seed mixture of regional plant species. These species were all regionally present, but often locally absent, depending on the resident vegetation composition and richness of each grassland. Important findings One year after sward disturbance it had significantly increased cover of bare soil, seedling species richness and numbers of seedlings. Seed addition had increased plant species richness, but only in combination with sward disturbance. The increase in species richness, when both seed addition and disturbance was applied, was higher at high land-use intensity and low resident diversity. Thus, we show that at least the early recruitment of many species is possible also at high land-use intensity, indicating the potential to restore and enhance biodiversity of species-poor agricultural grasslands. Our newly established experiment provides a unique platform for broad-scale research on the land-use dependence of future trajectories of vegetation diversity and composition and their effects on ecosystem functioning.

Paleomagnetic and stable isotope measurements and distribution of benthic foraminifera in sediment core PS1388-3 from the Antarctic continental margin in the eastern Weddell Sea

A stable isotope record from the eastern Weddell Sea from 69°S is presented. For the first time, a 250,000-yr record from the Southern Ocean can be correlated in detail to the global isotope stratigraphy. Together with magnetostratigraphic, sedimentological and micropalaeontological data, the stratigraphic control of this record can be extended back to 910,000 yrs B.P. A time scale is constructed by linear interpolation between confirmed stratigraphic data points. The benthic d18O record (Epistominella exigua) reflects global continental ice volume changes during the Brunhes and late Matuyama chrons, whereas the planktonic isotopic record (Neogloboquadrina pachyderma) may be influenced by a meltwater lid caused by the nearby Antarctic ice shelf and icebergs. The worldwide climatic improvement during deglaciations is documented in the eastern Weddell Sea by an increase in production of siliceous plankton followed, with a time lag of approximately 10,000 yrs, by planktonic foraminifera production. Peak values in the difference between planktonic and benthic d13C records, which are 0.5 per mil higher during warm climatic periods than during times with expanded continental ice sheets, also suggest increased surface productivity during interglacials in the Southern Ocean.