Éditeur(s) : HAL CCSD BioMed Central
Résumé : International audience
Background: Neonatal infection constitutes one of Senegal’s most important public health problems, with amortality rate of 41 deaths per 1,000 live births.Methods: Between January 2007 and March 2008, 242 neonates with suspected infection were recruited at threeneonatal intensive care units in three major tertiary care centers in Dakar, the capital of Senegal. Neonatal infections wereconfirmed by positive bacterial blood or cerebrospinal fluid culture. The microbiological pattern of neonatal infectionsand the antibiotic susceptibility of the isolates were characterized. In addition, the genetic basis for antibiotic resistanceand the genetic background of third-generation cephalosporin-resistant (3GC-R) Enterobacteriaceae were studied.Results: A bacteriological infection was confirmed in 36.4 % (88/242) of neonates: 22.7 % (30/132) during the early-onsetand 52.7 % (58/110) during the late-onset periods (p > 0.20). Group B streptococci accounted for 6.8 % of the 88 collectedbacterial isolates, while most of them were Enterobacteriaceae (n = 69, 78.4 %). Of these, 55/69 (79.7 %) were 3GC-R. TheblaCTX-M-15 allele, the blaSHV and the blaTEM were highly prevalent (63.5, 65.4 and 53.8 %, respectively), usually associatedwith qnr genes (65.4 %). Clonally related strains of 3GC-R Klebsiella pneumoniae and 3GC-R Enterobacter cloacae, the twomost commonly recovered 3GC-R Enterobacteriaceae (48/55), were detected at the three hospitals, underlining the roleof cross-transmission in their spread. The overall case fatality rate was 18.6 %.Conclusions:Measures should be taken to prevent nosocomial infections and the selection of resistant bacteria
ISSN: 1471-2334

Droits : http://creativecommons.org/licenses/by/
hal-01473613
https://hal.archives-ouvertes.fr/hal-01473613
https://hal.archives-ouvertes.fr/hal-01473613/document
https://hal.archives-ouvertes.fr/hal-01473613/file/High%20third-generation%20cephalosporin%20resistant%20Enterobacteriaceae%20prevalence%20rate%20among%20neonatal%20infections%20in%20Dakar%2C%20Senegal.pdf
DOI : 10.1186/s12879-016-1935-y

Éditeur(s) : HAL CCSD BioMed Central
Résumé : International audience
BACKGROUND: The genetic diversity of Plasmodium falciparum has been extensively studied in various parts of the world. However, limited data are available from Mauritania. The present study examined and compared the genetic diversity of P. falciparum isolates in Mauritania. METHODS: Plasmodium falciparum isolates blood samples were collected from 113 patients attending health facilities in Nouakchott and Hodh El Gharbi regions. K1, Mad20 and RO33 allelic family of msp-1 gene were determined by nested PCR amplification. RESULTS: K1 family was the predominant allelic type carried alone or in association with Ro33 and Mad20 types (90%; 102/113). Out of the 113 P. falciparum samples, 93(82.3%) harboured more than one parasite genotype. The overall multiplicity of infection was 3.2 genotypes per infection. There was no significant correlation between multiplicity of infection and age of patients. A significant increase of multiplicity of infection was correlated with parasite densities. CONCLUSIONS: The polymorphism of P. falciparum populations from Mauritania was high. Infection with multiple P. falciparum clones was observed, as well as a high multiplicity of infection reflecting both the high endemicity level and malaria transmission in Mauritania.
ISSN: 1475-2875

inserm-00936407
http://www.hal.inserm.fr/inserm-00936407
http://www.hal.inserm.fr/inserm-00936407/document
http://www.hal.inserm.fr/inserm-00936407/file/1475-2875-13-26.pdf
DOI : 10.1186/1475-2875-13-26

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
Generation and emplacement of felsic magmas in the Paleoproterozoic Baoulé-Mossi domain, West African Craton does not match the apparent peaks of global crust generation identified between ca. 2900–2600, 1900–1600 and 1200–900 Ma. In contrast, across the Baoulé-Mossi domain, the emplacement of felsic intrusions ranges from ca. 2300 to 2000 Ma. It has proven difficult to place this magmatism within a robust geodynamic framework due to the lack of accurate geochronological data from across the West African Craton. The present study addresses this issue by presenting eighty-four new felsic intrusions zircon ion microprobe and LA-ICP-MS U-Pb ages from areas that up until now have not been targeted for geochronology. The new dataset, when fully integrated with existing age data, reveals a craton-wide diachronous geochronological pattern characterized by a magmatic front that migrated westward. This migration proceeded at a rate of 35 km per million years, with an apparent offset of the initiation and cessation of felsic magmatic activity between the east and west of approximately 50 million years. The new data also show that although the entire Baoulé-Mossi domain was subject to continuous magmatic activity for at least 150 million years, this magmatic activity displays a rather different record in the eastern and western portions of the domain. The differences are expressed as a westward migration of the magmatic activity, cessation of activity around ca. 2100 Ma (easternmost portion) and ca. 2050 Ma (westernmost portion) and a higher incidence of inherited ages in the westernmost portion when compared to the easternmost region. In addition, the new U-Pb data identify some of the oldest felsic intrusions in the region, including a granite from Burkina Faso (2265 ± 17 Ma) and a diorite porphyry (2216 ± 5 Ma) in southern Mali. This study also reveals inherited Archean zircon cores from across southern Mali. The combination of the new data presented here, along with previously published data, suggests that the Baoulé-Mossi domain formed from the accretion of two major crustal blocks. The Archean inherited ages open a window for further investigation of the interaction between the Archean Kénéma-Man and the Paleoproterozoic Baoulé-Mossi domains.
ISSN: 0301-9268

hal-01623272
https://hal.archives-ouvertes.fr/hal-01623272
DOI : 10.1016/j.precamres.2017.07.036

Éditeur(s) : HAL CCSD
Résumé : Les dossiers thématiques d'Agropolis, n° 11
Dans le contexte actuel de contraintes climatiques et socioéconomiques, les agricultures des zones sèches doivent évoluer afin de s’adapter et de répondre à un double défi : produire plus pour satisfaire les besoins alimentaires importants de populations en croissance, mais aussi produire mieux de façon viable et durable. Pour cela, les agricultures de ces zones doivent évoluer vers des modes de production à la fois plus productifs, économes en ressources naturelles et résistants aux aléas climatiques.Dans ce cadre, l’ingénierie écologique propose de nouvelles alternatives de gestion des systèmes agro-sylvo-pastoraux caractéristiques des régions arides et semi-arides d’Afrique subsaharienne. Ceci implique de maitriser la complexité des systèmes étudiés et de s’inspirer à la fois du fonctionnement des écosystèmes naturels de référence à la région agroécologique concernée — les savanes pour les zones sèches ouest-africaines — et des pratiques traditionnelles et savoir-faire locaux issus d’une longue adaptation face aux contraintes environnementales.À partir des expériences ouest-africaines notamment, différentes options pratiques sont exposées dans ce dossier. On pourra ainsi agir sur la biodiversité des organismes, que ce soit les plantes ou les microorganismes du sol par exemple, favoriser le recyclage des matières organiques et des éléments nutritifs pour les plantes qui sont associées, maitriser les cycles de l’eau et, enfin, agir sur l’organisation des paysages pour favoriser un meilleur contrôle des ravageurs de culture.Cependant, développer une telle approche demande une vision intégrée du fonctionnement et de l’évolution des systèmes agro-sylvo-pastoraux. Les questions sociales — le foncier, l’urbanisation et les migrations — et économiques — les marchés des denrées de première nécessité, la pauvreté, etc. — sont des déterminants essentiels qu’il convient de prendre en compte pour le développement durable des populations dans les zones sèches en Afrique subsaharienne.
https://hal.archives-ouvertes.fr/hal-01585038

hal-01585038
https://hal.archives-ouvertes.fr/hal-01585038