Modificazioni soggettive del rapporto obbligatorio e garanzie reali

Lo studio del lato soggettivo del rapporto è centrale nella teoria dell’obbligazione. Ci si chiede se la modificazione di una o anche di entrambe le parti del rapporto determini sempre la sua estinzione o se, invece, si conservi la sua unitarietà oggettiva. La risposta a questo interrogativo è stata diversa a seconda delle diverse epoche storiche. Nel diritto romano si riteneva che la variazione di qualunque soggetto determinasse l’estinzione del rapporto e la costituzione di una nuova obbligazione (novazione soggettiva). Tale soluzione è stata osteggiata dai codificatori moderni per i quali, in caso di modifica delle personae non si ha estinzione del rapporto, ma solo il mutamento di uno dei suoi elementi. Quanto ai diritti di garanzia, in particolare l’ipoteca, i principi generali essenzali sono la specialità e l’accessorietà. Quest’ultima caratteristica è dirimente in caso di modificazione soggettiva del rapporto e ciò emerge in sede di trattazione delle singole fattispecie del Codice Civile che la determinano, sia quanto al creditore sia quanto al debitore. Per velocizzare il subentro nel credito, nel 2007 è stato approvato il decreto Bersani (sulla portabilità del mutuo) che ha consentito di rimuovere vincoli a tale circolazione, nell’ambito dei rapporti bancari. Le caratteristiche della modificazione del rapporto obbligatorio, tuttavia, possono minare l’efficacia della riforma Bersani. Questo è il motivo per il quale taluni studiosi ritengono necessario procedere a un’ampia rivisitazione dell’intero diritto ipotecario, eliminando, sulla scia di quanto accaduto in altri ordinamenti europei, il requisito dell’accessorietà del vincolo. Nonostante ciò, a causa dei rischi connessi a questa riforma, si ritiene preferibile affinare il meccanismo di perfezionamento della portabilità, eliminandone le criticità, senza però pregiudicare le sicurezze dell’attuale sistema giuridico, di cui l’accessorietà dell’ipoteca rispetto al credito costituisce un importante caposaldo.

Fauna associated with Bathymodiolus azoricus mussel beds within hydrothermal fields of the Mid-Atlantic Ridge

Structure of assemblages associated with mussel aggregations of Bathymodiolus azoricus was investigated. Mussel beds were found on hydrothermal vent fields on the Mid-Atlantic Ridge (Menez Gwen, Lucky Strike, and Rainbow) at depths 850-2400 m. The community structure of the mussel bed assemblages varied between studied areas. Large number of species was unique to mussel beds of the Menez Gwen field; the most observed taxa were not specialized hydrothermal species. All other nonunique species were found within the Lucky Strike region. The lowest mussel assemblage structure evenness was observed in the shallowest Menez Gwen area (850 m depth). We assume that two types of mussel assemblages (nematode-dominated and copepod-dominated) exist within the Lucky Strike field. The assemblages of B. azoricus differ significantly from assemblages of B. thermophilus inhabiting Pacific hydrothermal vents.

Abundance of benthic Foraminifera in the Kara Sea

Taxonomic composition and structure of assemblages of the present-day benthic Foraminifera in the Kara Sea has been studied on the base of 37 samples of surface sediments. Three assemblages have been distinguished by composition of dominant species. The assemblage Cribrostomoides subglobosus-Tritaxis nana with prevalence of agglutinating forms, typical for abyssal areas of the World Ocean, occurs in brown oozes in the deep western part of the sea at depths 70-375 m under conditions of considerable bottom stratification. The assemblage Elphidium clavatum-Cassidulina reniforme consists predominantly of species with calcareous shells and is characterized by a wide range of species; this assemblage occurs in the eastern part of the sea at depths 30-90 m in a well-aerated area. Species typical for sublittoral areas of polar regions are dominant. The assemblage Elphidium clavatum-Haynesina orbiculare occupies the littoral estuarine part of the sea. This assemblage is poor in species and not abundant, and it occurs under influence of freshened water masses undersaturated with dissolved carbonaceous matter.

Benthic fauna associated with mussel beds and shrimp swarms within hydrothermal fields on the Mid-Atlantic Ridge

Macrofaunal assemblages with prevalence of Bresiliidae shrimps and Mytilidae mussels are abundant in at hydrothermal vents along the Mid-Atlantic Ridge. Mussels inhabit zones of diffuse seeps of hydrothermal fluids with temperature abnormalities up to several degrees. Shrimps inhabit an extreme biotope in a mixed interface between seawater and hydrothermal fluids at temperature up to 20-30°C. We studied the mussel and shrimp assemblages in three hydrothermal vent fields: Rainbow, Broken Spur, and Snake Pit. Species richness of the mussel assemblages within at least two fields (Broken Spur and Snake Pit) is higher as compared with shrimps from the same hydrothermal vent fields. Fauna inhibiting shrimp swarms lack almost any taxa specific for particular assemblages: almost all the taxa are also present in the mussel beds. Structure of the shrimp assemblage is less homogeneous as compared with that of the mussel assemblage. Population prevalence of one taxon (Copepoda) in the shrimp assemblage is most likely connected with extreme and unstable conditions of the biotope occupied by the shrimps in a hydrothermal field. Taxonomic similarity between the mussel and shrimp assemblages within one hydrothermal vent field is higher as compared with similarity between the mussel (or shrimp) assemblages from different fields.

Speciation of metals in bottom sediments from the south Kara Sea and Ob and Yenisei estuarine zones

Speciation of Fe, Mn, Zn, Cu, Co, Ni, Cr, Pb, and Cd was studied in 52 samples of bottom sediments collected during Cruise 49 of the R/V "Dmitry Mendeleev" to the estuaries of the Ob and Yenisei rivers and to the southwest Kara Sea. Immediately after sampling the samples were subjected to on-board consecutive extraction to separate metal species according to their modes of occurrence in the sediments: (1) adsorbed, (2) amorphous Fe-Mn hydroxides and related metals, (3) organic + sulfide, and (4) residual, or lithogenic. Atomic absorption spectroscopy of the extracts was carried out at a stationary laboratory. Distribution of Fe, Zn, Cu, Co, Ni, Cr, Pb, and Cd species is characterized by predominance of lithogenic or geochemically inert modes (70-95% of bulk contents), in which the metals are bound in terrigenous and clastic mineral particles and organic detritus. About half of total Mn amount and 15-30% of Zn and Cu are contained in geochemically mobile modes. Spatiotemporal variations in proportions of the metal species in the surface layer of sediments along sub-meridional sections and through vertical sections of bottom sediment cores testify that Mn and, to a lesser extent, Cu are the most sensitive to changes in sedimentation environment. The role of their geochemically mobile species notably increases under reducing conditions.