17 research outputs found

    Frequency of female worms as a function of the proportion of degenerating microfilariae in their uteri.

    No full text
    <p>These frequencies were plotted before and 80 days after ivermectin treatment for the control and frequently ( = multiply) treated groups. The proportion of degenerating microfilariae was assessed from 15 µl of the homogenized suspension resulting from the crushing of each female worm.</p

    Composition of the nodules and distribution of female worms according to their uterine contents.

    No full text
    <p>The evaluation of the uterine content was done from 15 µl of the homogenized suspension resulting from the crushing of each female worm. We expressed the numbers of embryos using this volume (15 µl) as arbitrary unit; sd: standard deviation; mf: microfilariae; max: maximum.</p

    Mean number of embryos per female worm before and 80 days after ivermectin treatment.

    No full text
    <p>These data are presented separately for all female worms (a) and only for productive female worms (b) and are compared between the control and the frequently ( = multiply) treated groups. The mean number of embryos was assessed from 15 µl of the homogenized suspension resulting from the crushing of each female worm.</p

    Mapping of Bancroftian Filariasis in Cameroon: Prospects for Elimination

    No full text
    <div><p>Background</p><p>Lymphatic filariasis (LF) is one of the most debilitating neglected tropical diseases (NTDs). It still presents as an important public health problem in many countries in the tropics. In Cameroon, where many NTDs are endemic, only scant data describing the situation regarding LF epidemiology was available. The aim of this study was to describe the current situation regarding LF infection in Cameroon, and to map this infection and accurately delineate areas where mass drug administration (MDA) was required.</p><p>Methodology</p><p>The endemicity status and distribution of LF was assessed in eight of the ten Regions of Cameroon by a rapid-format card test for detection of <i>W</i>. <i>bancrofti</i> antigen (immunochromatographic test, ICT). The baseline data required to monitor the effectiveness of MDA was collected by assessing microfilariaemia in nocturnal calibrated thick blood smears in sentinel sites selected in the health districts where ICT positivity rate was ≥ 1%.</p><p>Principal findings</p><p>Among the 120 health districts visited in the eight Regions during ICT survey, 106 (88.3%) were found to be endemic for LF (i.e. had ICT positivity rate ≥ 1%), with infection rate from 1.0% (95% CI: 0.2–5.5) to 20.0% (95% CI: 10–30). The overall infection rate during the night blood survey was 0.11% (95% CI: 0.08–0.16) in 11 health districts out of the 106 surveyed; the arithmetic mean for microfilaria density was 1.19 mf/ml (95% CI: 0.13–2.26) for the total population examined.</p><p>Conclusion/significance</p><p>ICT card test results showed that LF was endemic in all the Regions and in about 90% of the health districts surveyed. All of these health districts qualified for MDA (i.e. ICT positivity rate ≥ 1%). Microfilariaemia data collected as part of this study provided the national program with baseline data (sentinel sites) necessary to measure the impact of MDA on the endemicity level and transmission of LF important for the 2020 deadline for global elimination.</p></div

    Distribution of female worms according to the density of oocytes in their uteri.

    No full text
    <p>A semi-quantitative approach was used to classify the density of oocytes into four categories: absence, rare (less than one PSC), few (1–10 oocytes PSC) and numerous (more than 10 oocytes PSC). The density of oocytes was assessed from 15 µl of the homogenized suspension resulting from the crushing of each female worm.</p

    Salt-bearing fumarole deposits in the summit crater of Oldoinyo Langai, Northern Tanzania: Interaractions between natrocarbonatite lava and meteoric water

    No full text
    Oldoinyo Lengai in the Northern Tanzania rift is the only active nephelinite-carbonatite stratovolcano. We report the discovery of thermonatrite, aphthitalite, halite and sylvite fumarole deposits on recent natrocarbonatite lava flows erupted in the summit crater during the wet season. These salt deposits occur as delicate, concave fringes or tubes that line the cooling cracks in the lava flows and consist of intergrowths of euhedral crystals. The presence of a dark altered zone, depleted in halides and alkalies, adjacent to cooling cracks and observations of steam fumaroles emanating from the fractures suggest that the salts are formed by sublimation from saturated vapours generated by the extrusion of lavas over meteoric water. The crystallisation sequence recorded in the salts suggests that mixing between meteoric steam and magmatic CO2 and H2S occurs at high temperatures resulting in the sublimation of carbonates and sulphates. At lower temperatures the vapours are dominated by meteoric steam and sublimate halides. The high solubility of the fumarole salts within meteoric water and their formation only during the wet season implies that these are ephemeral deposits that are unlikely to be preserved in the geological record. © 2001 Elsevier Science B.V. All rights reserved
    corecore