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The global-score likelihood peaks near ω = 0.18 in good agreement with the previous determinations, showing that it reproduces quite well the amino acid substitution patterns found in real sequences.
This suggests a non-synergistic effect, which is in line with the assumed mode of action of Qnr proteins as well as with earlier susceptibility determinations showing that isolates carrying two qnr genes do not display a superior resistance phenotype [ 24, 25].
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In addition, the MBC determination showed that B. melitensis NI failed to survive after being sub-cultured in media without the tested disinfectants, a blank space suggesting that the MICs and MBCs were equivalent (Table 2).> -wrap-foot> a P < 0.05 (significant) in comparison with the corresponding recommended concentration.
The structure determinations show that substituted group at the 4,4′-position of the this kind of Salen ligands are important factors influencing the crystalline array.
The results of the MIC determinations showed that the methanol extract and aristolochic acid I prevent the growth of all studied organisms.
Single-crystal X-ray molecular structure determinations show that both compounds have similar three-dimensional molecular structures; however, PDBS crystals are thin platelets and FPDBS crystals form hexagonal tube-like structures that are predominately hollow at one end.
The radiocarbon determinations show that the Upper Palaeolithic (Epigravettian) humans from Grotta di San Teodoro (15 232–14 126 cal. BP) and Grotta Addaura Caprara (16 060–15 007 cal. BP) date to the Late-glacial and were possibly contemporary.
X-ray crystal structure determinations show that 2 is a phenoxy-bridged dimer with the ortho-methyl groups making the beginning of a pocket about the terminal chloro ligand and 6 is a tetrahedral monomer in which the pocket is more well developed by the ortho-tert-butyl groups.
However, approximate determinations showed that mannose was consumed shortly after glucose was depleted from the medium.
Speciation determinations showed that, within analytical errors, all of the dissolved As was present as As V).
The epicenter determinations show that the first event in 04.01.1935 was located at 40.72N 27.72E, while the second one occurred at 40.61N 27.43E, indicating that both were located near the Marmara Island.
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