Soil properties of bare patches in rangelands of South African's grasslands

A loss of grassy cover accompanied by the development of bare soil patches, are the most notable forms of rangeland degradation in grasslands of South Africa. Concerns are growing over the threat of loss of nutritious perennial grass species and the lack of regrowth of the bare patches. Grazing and different rangeland tenure systems -communal and freehold, which is equal to continuous and rotational grazing system - are considered to be of major importance for rangeland degradation. The continuous grazing system is seen to be more affected, but the development of bare patches is not restricted to communal land. We hypothesized that (1) soil properties of bare patches in South Africa´s grasslands are not different in different tenure systems, and (2) soil properties differ with size of bare patches, where big patches are more degraded. To test this, we sampled soils at communal and commercial land in the Thaba Nchu area of South Africa with the following design: we selected three farms per tenure system, 6 randomly chosen plots (100x100m) per farm, and within these plots we sampled 5 bare patches of different sizes (0-10 cm) per plot, where the soil sample (3 replicates) were taken out of the middle of the bare patch. Additionally, soils of adjacent grass were sampled. The results showed that in total, there were more bare patches in continuous grazing systems, evaluated by aerial pictures, but we couldn´t find any differences in bulk density and carbon stocks, between the tenure systems. Additionally, and surprisingly, we found no significant differences in soil organic carbon stocks between bare soil samples and grass samples. There was no clear relationship between bare patch size and nutrient contents. Other nutrients like phosphor were significantly enlarged at the bare patch compared to the grass samples. According to our results, we conclude, that the bare patches seem to develop in different pathways: i) along tracks of grazing animals, (ii) around termite hills, where the termite construction seems to be an initial starting point of bare patches and (iii) on staying and lying places of the grazing animals, which aslo explain the higher nutrient contents at the bare patches

Reliability and usability of tourism climate indices.

Tourism climate indices (TCI) are commonly used to describe the climate conditions suitable for tourism activities, from the planning, investment or daily operations perspectives. A substantial amount of research has been carried out, in particular with respect to new indices formulae adapted to specific tourism products, and parameters and their weighting, taking into account surveys on the stated preferences of tourists, especially in terms of comfort. This paper illustrates another field of research, which seeks to better understand the different sources of uncertainty associated with indices. Indeed, slight differences in formula thresholds, variations in computation methods, and also the use of multimodel ensembles create nuances that affect the ways in which indices projections are usually presented. Firstly, we assess the impact of differences in preference surveys on the definition of indices thresholds, in particular for thermal comfort. Secondly, we compare computation methods for France, showing the need to better specify detailed data sources and their use to ensure the comparability of results. Thirdly, using multimodel ensembles for the Mediterranean basin, we assess the uncertainty inherent in long-term projections, which are used in modelling the economic impact of climate change. This paper argues in favour of a more cautious use of tourism comfort indices, with more consideration given to the robustness of data (validation, debiasing, uncertainty assessment, etc.) and users’ needs, from the climate services perspective.This paper was written by a team participating in the EU FP7 project CLIM-RUN “Climate Local Information in the Mediterranean region Responding Users Needs” (2011–2014)

Organic matter in termite mounds of an Amazonian rain forest.

This study investigates how termites alter the organic matter in rain forests near Manaus, Brazil. Samples were collected from the outer and inner parts of typical termite nests of Nasutitermes, Termes, Embiratermes, Cornitermes, Anoplotermes, and Constrictotermes genera, as well as from the surrounding topsoil (0cm-10cm) and potential wooden food. The termite nests were signficant sinks for organic matter and its associated nutrients. The organic C contents ranged between 100g kg-1 and 500g kg-1 in the nests, compared to 17g kg-1 to 42g kg-1 in the surrounding topsoils. As lignin contents of the mounds were higher than in wood, lignin may be accumulated in preference to other organic compounds. This findings also sugests that the interior part of the nests is a region of higher organic matter turnover and lignin degradation

The New Instantaneity: How Social Media are Helping us Privilege the (Politically) Correct over the True

The recent sacking of the eminent scientist Tim Hunt from one of the UK’s leading research institutions is only the latest in a series of cases where public individuals have been derided for comments made in jest on social media, with serious consequences for their professional and personal lives. This article discusses the case of Tim Hunt as an example of the extent to which the privileging of the correct over the true which has long pervaded media discourse is taken to the extreme by the instant-response culture of social media. It points to the emergence of a new form of instantaneity enabled by these networked forms of communication that serves to reinforce systemic inaction rather than the change widely associated with these technologies. It draws on philosophy and Critical Theory as useful conceptual frameworks for highlighting the ways in which Twitter & co. increasingly call us to action but crowd out thought, thereby passing over opportunities for real social change

Spatial distribution of organic carbon in the Atacama Desert, Chile

The Atacama Desert in northern Chile is known as the driest region on earth; however traces of life, can still be found. Soils are the habitat and reservoir for plants and microorganisms, which leave their fingerprints as organic residues. Here we identify and quantify organic carbon in soil profiles and along potential plant dispersal corridors in the Atacama Desert. We hypothesize that preferential pathways or barriers of the dispersal of life exist, which can be related to soil properties such as bulk density. We further assume that due to dust and salt accumulation at the surface, in particular the subsoils will reveal an unique though little explored archive of organic matter. The analytical assessment of Corg at very low levels is challenging. It was found that SOC in hyperarid soils ranged from 1.8 – 125 µg C per g soil for 0-1 m (1). We here present an improved Corg analysis, which is based on a temperature gradient method (DIN19539; Soli TOC cube, Elementar, Hanau). This allows combustion of samples with up to 5 g sample weight without the need to remove carbonate. This avoids loss and increases precision of Corg quantification at lowest concentrations. We can show that Corg contents decrease from 1.47 % to 0.1 % in the first 14 km of the gradient. However, first results suggest that within the hyper-arid core of the Atacama Corg contents increase. This gives first hints to the vegetation history of the desert and the dispersal of life

Der Austausch von Sauerstoffisotopen zwischen Phosphat und Wasser in Modellsystemen und Böden - neue Einblicke mit Raman Spektroskopie

Das Isotopenverhältnis (O-18/O-16) in Phosphat (PO43-) kann als Tracer von biogeochemischen Prozessen in terrestrischen und aquatischen Ökosystemen genutzt werden. Bei Temperaturen unter 70°C ist die Phosphoanhydridbindung stabil aber die Aktivität von Enzymen kann den Austausch von Sauerstoffisotopen zwischen Phosphat und Wasser katalysieren. Insbesondere die intrazelluläre Pyrophosphatase führt zu einem kompletten Austausch von Sauerstoff zwischen PO43- und H2O. Dieser biochemische Prozess ist sehr wichtig, da er in allen lebenden Zellen stattfindet und somit Aufschluss darüber geben kann, ob bodenbürtiges Phosphat Teil des biologischen Kreislaufs war oder nicht. Die Extraktion und Aufreinigung von anorganischem Phosphat aus Böden vor der Messung mit einem Isotopenmassenspektrometer (IRMS) ist allerdings teuer und sehr zeit- und arbeitsintensiv. Aus diesem Grund arbeiten wir an der Entwicklung einer alternativen Methode mit dem Einsatz von Raman-Spektroskopie. In einem Modellsystem konnten wir erfolgreich die Kinetik des enzym-katalysierten Sauerstoffisotopenaustausches bestimmen. Kleine Veränderungen der Protein- und Cofaktorkonzentrationen (MgCl2) hatten einen starken Einfluss auf die Reaktionsgeschwindigkeit. Zusätzlich präsentieren wir erste Resultate über die Anwendungsmöglichkeiten dieser Technologie in natürlichen Systemen, wie zum Beispiel in Fließgewässern oder in Böden

Sauerstoffisotopenaustausch an Oxiden - Raman Messungen mit Mischungen aus Nitrat, Sulfat und Phosphat

Der Austausch der Sauerstoffisotope O-16 und O-18 ist ein Indikator für biologische Kreisläufe wichtiger Nährstoffe wie Nitrat, Sulfat oder Phosphat im Boden. Dabei setzen sich die Austauschreaktionen in realen Systemen aus verschiedenen biotischen und abiotischen Einzelreaktionen zusammen (z.B. mit und ohne Beteiligung von Mikroorganismen). Um diese verschiedenen Mechanismen unterscheiden zu können, ist es nötig mit Modellsystemen einzelne Teilmechanismen zu beschreiben. In dem Poster stellen wir erste Messungen zum abiotischen Sauerstoffisotopenaustausch mittels Raman-Spektroskopie an einer Mischung aus Nitrat, Sulfat und Phosphat vor. Raman-Spektroskopie ist eine Lichtstreumethode, die Schwingungen symmetrischer Moleküle detektiert. Da diese Molekülschwingungen von den Massen der beteiligten Atome abhängen, verändern sich bei einem Isotopenaustausch die für die Schwingungen charakteristischen Wellenzahlen der Banden im Raman-Spektrum. Bei einem schrittweisen Austausch der 3 Sauerstoffatome im Nitrat (NO3-) sind während einer Zeitreihe 4 Banden für die symmetrische N-O Valenzschwingung zu beobachten, deren Intensität (≙ Fläche unter der Bande) sich mit der Zeit ändert. Bei Sulfat (SO42-) sind wegen der 4 Sauerstoffatome 5 Banden vorhanden. Beim Phosphat (PO43-) liegen die 5 Banden so dicht, dass nur eine Umhüllende erkennbar ist, deren Maximum sich mit der Zeit verschiebt. Für eine quantitative Bestimmung der Kinetik des Isotopenaustausches muss der relative Anteil jedes Isotopologs während der Austauschreaktion als Funktion der Zeit bestimmt werden. Dazu werden die Bandensignale integriert, bzw. bei überlappten Signalen entfaltet und integriert. Für jeden Isotopologen ergibt sich so eine charakteristische Zeitkurve, die dann mit den Geschwindigkeitsgesetzen der Reaktionskinetik beschrieben werden kann. Die in diesem Poster gezeigten Arbeiten beschäftigen sich mit dem abiotischen O-16 -> O-18 Austausch einer 3-fach Mischung aus KNO3, K2SO4 und KH2PO4 in O-18 angereichertem Wasser bei Temperaturen größer als 90°C. Bei niedrigeren Temperaturen konnte kein abiotischer Sauerstoffisotopenaustausch beobachtet werden. Die Geschwindigkeitsgesetze für die Isotopologen der drei Oxide werden vorgestellt

Intestinal motility distal of a deviating ileostomy after rectal resection with the construction of a primary anastomosis:results of the prospective COLO-MOVE study

Purpose No consensus exists regarding the use of preoperative bowel preparation for patients undergoing a low anterior resection (LAR). Several comparative studies show similar outcomes when a single time enema (STE) is compared with mechanical bowel preparation (MBP). It is hypothesized that STE is comparable with MBP due to a decrease in intestinal motility distal of a newly constructed diverting ileostomy (DI). Methods In this prospective single-centre cohort study, patients undergoing a LAR with primary anastomosis and DI construction were given a STE 2 h pre-operatively. Radio-opaque markers were inserted in the efferent loop of the DI during surgery, and plain abdominal X-rays were made during the first, third, fifth and seventh postoperative day to visualize intestinal motility. Results Thirty-nine patients were included. Radio-opaque markers were situated in the ileum or right colon in 100%, 100% and 97.1% of the patients during respectively the first, third and fifth postoperative day. One patient had its most distal marker situated in the left colon during day five. In none of the patients, the markers were seen distal of the anastomosis. Conclusion Intestinal motility distally of the DI is decreased in patients who undergo a LAR resection with the construction of an anastomosis and DI, while preoperatively receiving a STE