4,513 research outputs found

    SLIDES: Public Funding Sources in MT: State Funding Sources, 3 Partnerships Examples

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    Presenter: Alan Wood, MT Department of Fish, Wildlife and Parks, Helena, MT 12 slide

    SLIDES: Public Funding Sources in MT: State Funding Sources, 3 Partnerships Examples

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    Presenter: Alan Wood, MT Department of Fish, Wildlife and Parks, Helena, MT 12 slide

    Structure, paleolimnology and basin history of the East Kivu Graben, Lake Kivu, Rwanda from offshore seismic reflection data

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    Lake Kivu, located at the topographic high point of the western branch of Africa\u27s Great Rift Valley, is regularly subjected to large-magnitude seismic events, violent volcanic discharges, and possible limnic eruptions which pose substantial geohazards to the ~two million Congolese and Rwandan people living around its basin. Although most of the western branch of Africa\u27s Great Rift Valley is amagmatic, Lake Kivu is bordered to the north and south by two volcanic provinces. Subaqueous springs, charged by the active Virunga Magmatic Complex at the north end of the lake, currently inject gas into the deep- hypolimnion, where it remains in solution at high concentrations. Rapid expulsion of these gases into the atmosphere, possibly induced by seismic, meteorologic, or volcanic events, would be devastating to the local population. To assess the potential danger, it is critical to understand the basin\u27s structure, and the effects of magmatism and climate changes on the lake. Information about past basin structural, and lake surface elevation changes are preserved in the sediments under the lake; these provide information about the region\u27s tectonic and climatic past. Between 2010 and 2013, Syracuse University\u27s Department of Earth Sciences acquired ~1100 km of marine seismic reflection data and six Kullenberg sediment cores from the eastern basin of the lake. Interpretation of these seismic data show that the eastern basin of Lake Kivu is a half-graben, bounded by east-dipping normal faults. Most subsidence is accommodated at the west side of the basin by slip along two north striking, offset growth faults which are located east of Idjwi and Iwawa Islands. Strain between these faults is accommodated by oblique strike-slip along a northeast striking, transfer fault. Oblique slip along other northeast-striking faults may accommodate extension between more recent, north striking fault segments. This could account for the irregular shape of Lake Kivu\u27s basin, islands, and shoreline. The \u3e1.5 km sedimentary section observed in the marine seismic reflection data records extreme climate changes through the late Pleistocene and Holocene. Truncated surfaces indicate that the lake has experienced at least three periods of desiccation. Two of these events correlate to prolonged times of aridity interpreted within the sedimentary records of other African Great Lakes. Between these desiccation periods, the maximum lake surface has varied over a range of \u3e400 m, controlled at different times by climate or the basin\u27s structural configuration. At ~12 ka, there was a transgression from a lowstand of ~370 m below the current lake level, to a level above the current water position. This transgression is reported as induced by a sudden, rapid expansion of the Virunga Volcanic Complex which blocked the northern outlet of the lake, forcing it to a higher, southern spill point through Bukavu Bay; however data presented herein show that it was likely caused by a change in the regional climate. Sediment core data indicate that the transgression occurred over a time span of ~100 years which was likely too short of a period for such a large magmatic expansion. Seismic data show that for most of the lake\u27s past, prior to this -370 m lowstand, the lake level was at ~310 m below the modern lake level, indicating that the lowstand underfilled the lake basin. In this circumstance, the basinal spill point did not control the lake level. Other East African Lakes also transgressed from low stands at approximately the same time, indicating that there was a regional change to wetter climate conditions. Inflation of the Virunga Volcanic Complex, which likely occurred gradually before, or during the lowstand, raised the topographic threshold to the north forcing the lake to spill out of the southern, Bukavu Basin when the transgression occurred

    What Does It Mean to Be Human? Education for World Citizenship

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    What is the purpose of education in a democracy? What is the meaning of freedom? These questions are explored in depth in this essay as the author attempts to expand the conversation between private and public education. Without reference to religious purposes or Gospel mandates, the article explores possible responses to ultimate questions of meaning by mining language, history, biology, and technology for answers

    Tunnelling

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    Tunnelling has become a fragmented process, excessively influenced by lawyers'notions of confrontational contractual bases. This prevents the pooling of skills, essential to the achievement of the promoters' objectives. Tunnelling: Management by Design seeks the reversal of this trend. After a brief historical treatment of selected developments, t

    Human Endothelial Progenitor Cells: A Novel and Promising Cellular Therapy For Regenerative Medicine

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    Endothelial progenitor cells represent a novel and promising therapy for a myriad of tissues and conditions including diseases and disorders of the liver and small intestine. Cirrhosis and other diseases have created a need for a readily available supply of hepatocytes and supporting cells in diseased and scarred liver. Following chemo/radiation therapy and inflammatory bowel disease, the cell populations of the small intestine are diminished and a cell therapy for the replenishment of these populations is needed. Additionally, the cellular makers to identify both EPCs and mesenchymal stem cells (MSCs) have been defined in the literature but a debate remains as to the heterogenic vs. homogenic nature of the cell populations. This dissertation investigates the engraftment potential of EPCs in the liver when transplanted (Tx) In Utero into the pre-immune sheep model via two routes of injection, Intra-hepatic (IH) and Intra-peritoneal (IP). Upon finding engraftment, the contribution of these cells to vasculature and parenchymal tissue as well as their differentiative potential in contribution to the developing liver was investigated. Tx EPCs engraft albeit at low levels but preferentially associate with vasculature. In addition to their association with vasculature, the EPCs maintain the expression of endothelial markers in addition to expressing markers raging from fully differentiated hepatic cells to liver stem cells. In addition to their contribution to the liver, EPCs not only engraft into the small intestine but do so in a preferential manner in the area containing the crypts of Lieberkühn (above the muscularis mucosa and below the crypt-villus junction). Upon transplantation, these cells actively engraft and differentiate into both intestinal stem cells (ISCs) and into the supporting cell types of the ISC niche as well as mature cells of the intestinal parenchyma. Finally, LAM-PCR and LM-PCR were employed to identify vector integration sites in both MSCs and EPCs transfected with a variety of retroviruses. These experiments are designed to address the existence of a heterogeneous or homogenous population in both the EPC and MSC populations. Further testing on an experimental sample reveals the presence of chimeric DNA in the sample and successful amplification of integration sites in this sample is pending further investigation

    Additions to the rust fungi of South Africa

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    This paper presents new species, combinations, national reports and host records for the South African rust fungi (Uredinales/Pucciniales). Endophyllum mpenjatiense on cf. Hibiscus sp. (Malvaceae), Phakopsora combretorum (anamorph Uredo combreticola) on the new host Combretum apiculatum (Combretaceae) and Uredo sekhukhunensis on Ziziphus mucronata (Rhamnaceae) are described as new species. Dietelia cardiospermi and E. metalasiae are proposed as new combinations to replace Aecidium cardiospermi on Cardiospermum halicacabum (Sapindaceae) and A. metalasiae on Metalasia spp. (Asteraceae), respectively. Four species are new records for South Africa: Crossopsora antidesmae-dioicae on Antidesma venosum (Euphorbiaceae), Phakopsora ziziphi-vulgaris on Z. mucronata, and Uromyces cypericola and Puccinia subcoronata, both on a new host, Cyperus albostriatus (Cyperaceae). The record of P. subcoronata is the first one from outside the New World. Puccinia scirpi is reported as a possible addition to the South African rust fungi. New host records and observations are presented for Pucciniastrum agrimoniae that is recorded on two new host genera and species, Cliffortia odorata and Leucosidea sericea (Rosaceae), Uromyces cypericola whose urediniospores are described for the first time, Phakopsora stratosa in that spermogonia and Uredo-like aecia were discovered, and for Sphaerophragmium dalbergiae in that characters of the urediniospores are re-evaluated. A lectotype is selected for Aecidium garckeanum and spermogonia are reported for this rust for the first time. The rust fungi of Ehrharta (Poaceae) are discussed and critically evaluated in the light of spore morphology and host specie
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