925 resultados para Theodore II, Negus of Ethiopia, d. 1868.


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A survey was conducted to generate holistic information on the production and utilization of local white lupin in two lupin growing districts, namely, Mecha and Sekela, representing mid and high altitude areas, respectively in North-western Ethiopia. During the survey, two types of participatory rural appraisal (PRA) techniques, namely, individual farmer interview (61 farmers from Mecha and 51 from Sekela) and group discussion (with 20 farmers from each district) were employed. There are significant differences (P<0.05) between the two study districts for the variables like total land holding, frequency of ploughing during lupin planting, days to maturity, lupin productivity, and number of days of soaking lupin in running water. However, there are no significant differences (P>0.05) between the two study districts for the variables like land allocated for lupin cultivation, lupin seed rate, lupin soaking at home, lupin consumption per family per week and proportion of lupin used for household consumption. The use of the crop as livestock feed is negligible due to its high alkaloid content. It is concluded that the local white lupin in Ethiopia is a valuable multipurpose crop which is being cultivated in the midst of very serious shortage of cropland. Its ability to maintain soil fertility and serve as a source of food in seasons of food scarcity makes it an important crop. However, its bitter taste due to its high alkaloid content remains to be a big challenge and any lupin improvement strategy has to focus on minimizing the alkaloid content of the crop.

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These guidelines are a working instrument for the assessment and documentation of existing and potential strategies for land and water conservation (prevention and mitigation strategies) in DESIRE study sites. DESIRE (Desertification Mitigation and Remediation of Land) is a European Integrated Project. The DESIRE WB 3 methodology was developed by CDE and is based on experiences from Learning for Sustainability (LforS) and WOCAT.

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In the present-day Ethiopia, glaciated landscapes do not exist, but paleoglaciated landscapes have been documented on a few mountain tops, which have altitudes higher than about 4,350 m asl in northern Ethiopia (Simen Mountains) and about 4,100 m asl in southern Ethiopia (Arsi and Bale Mountains). Glaciers were associated with the Late Pleistocene cold stages and reached as far down as 3,760 m asl in northern and 3,200 m asl in southern Ethiopia. Bale Mountains had the most extensive Late Pleistocene glaciation, covering over 190 km2, followed by Arsi Mountains (about 85 km2). In Simen, the Late Pleistocene glaciers covered merely 13 km2. In addition, paleo-periglacial slope deposits are found on all above-mentioned paleoglaciated mountains and in further mountain systems which did not host glaciers. This allows the reconstruction of the Late Pleistocene paleoclimate as being about 8 °C colder than at present (2014), much more dry, and probably without monsoon, at least in northern Ethiopia. Most probably in the Early Holocene, the re-emergence of monsoonal rains led to a strong erosion phase, which was followed by an extended stable phase with soil formation, building up about 70-cm-deep A-horizons (Andosol) on the paleo-periglacial slope deposits. These soils have been heavily degraded due to human-induced soil erosion up to about 3800 m asl since agriculture started several decades to millennia ago.

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A study was conducted on the highlands of Ethiopia to identify and analyse the factors determining the adoption of environmental management measures. In 1985, Ethiopia was classified into low –and high-potential areas based on the suitability of the natural environment for rain-fed agriculture. To address these objectives, case study areas were selected from low-potential and high-potential areas randomly. Data were collected through face-to-face interview and key informants, focus group discussion and field observation. In the low-potential areas, the physical environment ‒ particularly soil and forest environments have shown substantial recovery. Similarly, the water environment has improved. However, in the high-potential areas sampled, these resources are still being degraded. Clear understanding of the benefits of soil conservation structures by farmers, active involvement and technical support from the government and full and genuine participation of farmers in communal environmental resources management activities were found to be main factors in the adoption of environmental management measures.

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The majority of sensor network research deals with land-based networks, which are essentially two-dimensional, and thus the majority of simulation and animation tools also only handle such networks. Underwater sensor networks on the other hand, are essentially 3D networks because the depth at which a sensor node is located needs to be considered as well. Due to that additional dimension, specialized tools need to be used when conducting simulations for experimentation. The School of Engineering’s Underwater Sensor Network (UWSN) lab is conducting research on underwater sensor networks and requires simulation tools for 3D networks. The lab has extended NS-2, a widely used network simulator, so that it can simulate three-dimensional networks. However, NAM, a widely used network animator, currently only supports two-dimensional networks and no extensions have been implemented to give it three-dimensional capabilities. In this project, we develop a network visualization tool that functions similarly to NAM but is able to render network environments in full 3-D. It is able to take as input a NS-2 trace file (the same file taken as input by NAM), create the environment, position the sensor nodes, and animate the events of the simulation. Further, the visualization tool is easy to use, especially friendly to NAM users, as it is designed to follow the interfaces and functions similar to NAM. So far, the development has fulfilled the basic functionality. Future work includes fully functional capabilities for visualization and much improved user interfaces.

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Lymphocyte development requires the assembly of diversified antigen receptor complexes generated by the genetically programmed V(D)J recombination event. Because germline DNA is cut, introducing potentially dangerous double-stranded breaks (DSBs) and rearranged prior to repair, its activity is limited to the non-cycling stages of the cell cycle, G0/G1. The potential involvement of a key mediator, Ataxia Telangiectasia Mutated or ATM, in the DNA damage response (DDR) and cell cycle checkpoints has been implicated in recombination, but its role is not fully understood. Thymic lymphomas from ATM deficient mice contain clonal chromosomal translocations involving the T-cell antigen receptor (TCR). A previous report found ATM and its downstream target p53 associated with V(D)J intermediates, suggesting the DDR senses recombination. In this study, we sought to understand the role of ATM in V(D)J recombination. Developing thymocytes from ATM deficient mice were analyzed according to the cell cycle to detect V(D)J intermediates. Examination of all TCR loci in the non-cycling (G0/G1) and cycling (S/G2/M) fractions revealed the persistence of intermediates in ATM deficient thymocytes, contrary to the wild-type in which intermediates are found only during G0/G1. Further analysis found no defect in end-joining of intermediates, nor were they detected in developed T-cells. Based upon the presence of persisting intermediates, the recombination initiating nuclease Rag-2 was examined; strict regulation limits it to G 0/G1. Rag-2 regulation was not affected by an ATM deficiency as Rag-2 expression remained contained within G0/G 1, indicating recombination is not continuous. To determine if an ATM deficiency affects recognition of V(D)J breaks, sites of recombination identified by a TCR locus or Rag expression were analyzed according to co-localization with a DDR factor phosphorylated immediately after DNA damage, phosphorylated H2AX (γH2AX). No differences in co-localization were found between the wild-type and ATM deficiency, demonstrating ATM deficient lymphocytes retain the ability to recognize DSBs. Together, these results suggest ATM is necessary in the cell cycle regulation of recombination but not essential for the identification of V(D)J breaks. ATM ensures the containment of intermediates within G0/G1 and maintains genomic stability of developing lymphocytes, emphasizing its fundamental role in preventing tumorigenesis.^

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Results of studies of hydrothermal sulfide-sulfate rocks occurring in the Atlantis II Deep of the Red Sea are reported in the paper.