Peripheral benzodiazepine receptor ligand-melphalan conjugates for potential selective drug delivery to brain tumors

To gain insight into the strategy to target PBR ligand-drug conjugates to brain tumors, novel N-imidazopyridinacetyl-melphalan conjugates and the corresponding ethyl esters have been prepared and evaluated for their cytotoxicity in melphalan-sensitive human (SF126, SF188) and rat (RG-2) glioma cell lines. These conjugates exhibited PBR binding affinity with IC(50) values ranging from 57 and 2614 nM. By a computational approach it can be predicted that these conjugates possess significant brain penetration. The stability of the conjugates in 0.05 M phosphate buffer at pH 7.4 and, in some cases, in dilute human serum solution was determined. All the ethyl ester derivatives were stable in 0.05 M phosphate buffer at pH 7.4 and their half-lives exceeded 28 h. Conversely, under the same conditions, the corresponding acids were found to undergo a fast cleavage within a few minutes. HPLC-MS analysis of the mixture from degradation in buffer and physiological medium of the representative cases allowed the identification of their main degradation products. A plausible degradation pathway accounting for the available experimental data is presented.     

Surface-bottom relationships in the Gulf of Salerno (Tyrrhenian Sea) over the last 34 kyr: Compositional data analysis of palaeontological proxies and geochemical evidence

The palaeontological, geochemical and mineralogical records of core GNS84-C106 were analysed in order to reconstruct palaeohydrological changes and palaeoproductivity patterns in the Gulf of Salerno for the last 34 kyr. This approach, including compositional analysis of planktonic and benthic assemblages, gave an insight into the relationships between continental, sea surface and bottom environmental changes. The main source of variability of planktonic and benthic assemblages is related respectively to sea surface temperature and palaeobathymetry. Interrelated changes in surface salinity, nutrients, density gradient in the water column and organic fluxes at the bottom act as a secondary factor controlling the composition of both planktonic and benthic assemblages. The highest palaeoproductivity rates were reached during an interval spanning from late glacial to Middle Holocene, in conditions of enhanced continental run-off. During the Early and Middle Holocene, reduced surface salinity and density stratification were also coupled with the development of a deep chlorophyll maximum and enhanced flux or organic matter at the bottom. From about 6.5 kyr B.P. onward, a sharp reduction in palaeoproductivity took place, coupled with an increase in surface salinities.