295 research outputs found

    Mortality salience in an offline and online setting

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    The current study aims to examine the effects of mortality salience effects on worldview defense in an offline and online setting. Participants were 146 (66 offline and 80 online) Singaporeans. Participants were randomly assigned to either the mortality salience condition or the control condition and after a delay completed a Worldview Defense Assessment. No significant mortality salience effects on worldview defense occurred in either setting. The results might be explained by the Asian sample, Singapore's culture of tolerance, and data collection during the Coronavirus Disease 2019 (COVID-19) pandemic. Future research directions include examining the effects of COVID-19 in activating worldview defense

    COVID-19-related knowledge, attitudes, and practices among decisionmakers of indigenous municipalities in Guatemala: Study description

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    Indigenous communities are often socially and economically marginalized which makes them particularly vulnerable to the impact of COVID-19. The Population Council has a longstanding partnership with indigenous communities in Guatemala through the Abriendo Oportunidades program. To understand the knowledge, perspectives, and needs related to the COVID-19 pandemic, we will conduct key informant interviews with indigenous community leaders and frontline workers. Phone-based surveys will be carried out with approximately 130 key informants in the municipalities of Chisec, Patzún, San Andrés Semetabaj, San Juan Ostuncalco, San Juan Sacatepéquez, San Pedro Carchá, Santa María Chiquimula, Totonicapán, Uspantán and Sololá in April 2020. These individual profiles will include heads of household, former girl-program mentors, community health workers and providers, education officers, traditional birth attendants, and municipal officers. We anticipate this effort will provide initial baseline information and subsequent interviews may be conducted throughout 2020. Results from this study will help inform national and municipal prevention and mitigation strategies for indigenous communities and identify government resources that may be prioritized to meet the needs of these communities. Findings will also help decisionmakers understand the effects that COVID-19 is having on girls, girls’ education, and sexual and reproductive health under these rapidly changing conditions

    Complex patterns of the HIV-1 epidemic in Kuala Lumpur, Malaysia: Evidence for expansion of circulating recombinant form CRF33_01B and detection of multiple other recombinants

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    AbstractThe HIV protease-reverse transcriptase (PR-RT) (1047 bp), gp120-env (891 bp) and gp41-env (547 bp) regions from the plasma of 115 HIV-1-infected patients in Kuala Lumpur (KL), Malaysia were sequenced. Detailed phylogenetic and bootscanning analyses were performed to determine the mosaic structure of the HIV-1 strains and their recombination breakpoint(s). Among the 50 patient samples in which all three regions could be amplified, the HIV-1 CRF01_AE subtype (46%) was predominant followed by subtypes B (10%) and B′ (6%). A total of 9/50 (18%) patients were infected with a CRF01_AE/B inter-subtype recombinant, displaying a recombinant form (RF)PR-RT, CRF01_AEgp120-env and CRF01_AEgp41-env. This RF was derived from the Thai variants of CRF01_AE and B′ subtype, with two distinct B′ subtype segments in the backbone of CRF01_AE, similar to the newly identified CRF33_01B. In addition, one sample demonstrated a close structural relationship with the new CRF33_01B in the PR-RT region but displayed B′ segment in part of the env region (RFPR-RT, CRF01_AE/B′gp120-env and B′gp41-env) indicating continuing evolution of CRF33_01B. The remaining 18% of samples were identified as unique recombinant forms (URFs)

    Age and geochemistry of the Charlestown Group, Ireland:Implications for the Grampian orogeny, its mineral potential and the Ordovician timescale

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    Accurately reconstructing the growth of continental margins during episodes of ocean closure has important implications for understanding the formation, preservation and location of mineral deposits in ancient orogens. The Charlestown Group of county Mayo, Ireland, forms an important yet understudied link in the Caledonian-Appalachian orogenic belt located between the well documented sectors of western Ireland and Northern Ireland. We have reassessed its role in the Ordovician Grampian orogeny, based on new fieldwork, high-resolution airborne geophysics, graptolite biostratigraphy, U–Pb zircon dating, whole rock geochemistry, and an examination of historic drillcore from across the volcanic inlier. The Charlestown Group can be divided into three formations: Horan, Carracastle, and Tawnyinah. The Horan Formation comprises a mixed sequence of tholeiitic to calc-alkaline basalt, crystal tuff and sedimentary rocks (e.g. black shale, chert), forming within an evolving peri-Laurentian affinity island arc. The presence of graptolites Pseudisograptus of the manubriatus group and the discovery of Exigraptus uniformis and Skiagraptus gnomonicus favour a latest Dapingian (i.e. Yapeenian Ya 2/late Arenig) age for the Horan Formation (equivalent to c. 471.2–470.5 Ma according to the timescale of Sadler et al., 2009). Together with three new U–Pb zircon ages of 471.95–470.82 Ma from enclosing felsic tuffs and volcanic breccias, this fauna provides an important new constraint for calibrating the Middle Ordovician timescale. Overlying deposits of the Carracastle and Tawnyinah formations are dominated by LILE- and LREE-enriched calc-alkaline andesitic tuffs and flows, coarse volcanic breccias and quartz-feldspar porphyritic intrusive rocks, overlain by more silicic tuffs and volcanic breccias with rare occurrences of sedimentary rocks. The relatively young age for the Charlestown Group in the Grampian orogeny, coupled with high Th/Yb and zircon inheritance (c. 2.7 Ga) in intrusive rocks indicate that the arc was founded upon continental crust (either composite Laurentian margin or microcontinental block). Regional correlation is best fitted to an association with the post-subduction flip volcanic/intrusive rocks of the Irish Caledonides, specifically the late-stage development of the Tyrone Igneous Complex, intrusive rocks of Connemara (western Ireland) and the Slishwood Division (Co. Sligo). Examination of breccia textures and mineralization across the volcanic inlier questions the previous porphyry hypothesis for the genesis of the Charlestown Cu deposit, which are more consistent with a volcanogenic massive sulfide (VMS) deposit.</p
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