In: Hydrogeology Journal, 2013, vol. 21, no. 2, p. 425-440
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In: International Journal of Earth Sciences, 2013, vol. 102, no. 4, p. 1111-1129
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In: Hydrogeology Journal, 2010, vol. 18, no. 5, p. 1173-1190
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In: Journal of Medical Entomology, 1999, vol. 36, no. 2, p. 216-218
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In: Microbial Pathogenesis, 2014, vol. 74, p. 20–24
Multidrug-resistant and difficult-to-treat Acinetobacter baumannii may be responsible for nosocomial infections. The production of carbapenem-hydrolyzing class D β-lactamases (CHDLs) and extended-spectrum β-lactamase (ESBLs) of the GES type possessing a carbapenemase activity has been increasingly reported worldwide in A. baumannii. The aim of this study was to analyze the...
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In: Bulletin de la Société Géologique de France, 2011, vol. 182, no. 6, p. 507-519
Near the Cenomanian-Turonian boundary, the filament event corresponds to the massive occurrence of thin elongate shells, probably bivalves which constitute, in the Bahloul Formation, about 40% of allochems. This biosedimentary event was described in several areas, such as in Tunisia, Algeria, Morocco, North America, Oman and Tibet. In Tunisia, filaments are well represented within well laminated...
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In: Cretaceous Research, 2010, vol. 31, no. 1, p. 1-15
In central Tunisia, the thickness of the Bahloul Formation varies generally between 20 to 40 m such as for example, respectively, at wadi Smara near Kalaat Senan and at wadi Bahloul near Maktar. The thickness is also of several tens metres at Koudiat el Azreg near Jerissa and at Tajerouine. In these sites where the thickness of the Bahloul Formation is dilated, in addition to five geochemical...
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