Transport of Inorganic Phosphate in the Marine Seagrass Posidonia Oceanica By 32P-Phosphate As Tracer

Uptake and loss of inorganic phosphate by Posidonia oceanica leaf tissue has been studied in in vitro experiments. Experimental data have shown that a steady state of inorganic phosphate uptake (about 40 nmol mg^-1 dry wt.) is attained after 48 hours. in particular high accumulation (over 1000-fold the natural level in sea water) and slow loss (biological half-life, 65 days) of inorganic phosphate has been evaluated. Moreover the effect of three different metabolic inhibitors (sodium monovanadate, sodium azide, 2, 4-dinitrophenol) have been tested. Results of this effect and the high degree of inorganic phosphate accumulation in leaf tissue have demonstrated that inorganic phosphate carrier is energy dependent. Furthermore, the inorganic phosphate uptake is probably influenced by bivalent cations (Ca⁺², Mg⁺²) but the mechanism is still uncertain.

Preliminary kinetic study has shown interesting results. in particular, k_m estimated value (2.8 μmol 1^-1) has demonstrated the existence of a relatively high uptake rate (V_max) at low DIP concentration while the kinetic study of inorganic phosphate loss from leaf tissues has shown a low value of the biological half life (about 60-70 days). This evidence could be significant for the existence of a complex distribution of inorganic phosphate in the leaf tissues.     

Use of remote sensing for the characterization of the Mediterranean coastal environment—the case ofPosidonia oceanica

The beds ofPosidonia oceanica, a marine vascular plant species endemic to the Mediterranean, form a major Mediterranean marine ecosystem. These beds are well-developed along the sandy east coast of Corsica, where the continental shelf is wide and extends for ca. 100 km. The upper limit of this ecosystem has been mapped by means of a computer image processing technique using 1/20 000 colour photographs. One of the major problems for image processing in the marine environment is the impact of the water layer (of variable thickness and quality), which can result in variations of the spectral signature for a particular vegetation or bottom type. In an attempt to reduce the impact of this artefact, a processing technique that takes into account bathymetric factors has been tested. Cartographical data obtained for an area extending from Bastia to Solenzara are presented. In the vicinity of the mouths of coastal rivers, a systematic indentation of the upper limit of the seagrass beds has been revealed. On the basis of these results, local variations in the quality of the marine environment can be detected, in particular with regard to salinity, turbidity and/or the impact of sedimentation. The overall surface area of thePosidonia oceanica beds has also been calculated.     

Influence of hydrodynamic conditions on the production and fate of Posidonia oceanica in a semi-enclosed shallow basin (Stagnone di Marsala,Western Sicily)

An integrated approach using hydrodynamic and transport numerical models, lepidochronology and stable isotope analysis was used to investigate how local hydrodynamic conditions influence the primary production and fate of the seagrass Posidonia oceanica in a Mediterranean semi-enclosed marine system (Stagnone di Marsala). The water mass exchange aptitude of different sectors of the basin was analysed, and data collected were used to select two sectors (colonized by Posidonia oceanica showing the lowest and highest water exchange values) for biological analyses. According to the mean dispersal coefficient differences simulated by the hydrodynamic model, growth rate and primary production of P. oceanica differed between sectors, with average values lower in the central sector where water exchange is lower than in the southern sector. Although P. oceanica coverage and primary production were higher in the southern sector, carbon and nitrogen stable isotope analysis suggests that the transfer of seagrass organic matter to higher trophic levels of the food web was higher in the central sector. The possibility of a link between hydrodynamism, production and fate of organic matter is proposed to explain the observed patterns.     

Trace metals in “ Posidonia oceanica ” seagrass from south-eastern Sicily

Heavy-metal concentrations were measured in sediments and tissues of Posidonia oceanica seagrass from south-eastern Sicily (Italy) in order to assess the degree of metal pollution in the coastal area. Seagrasses and sediments were collected at four sites along the south-eastern coast of Sicily. Flame atomic absorption spectrophotometry (FAAS) was used to measure concentrations of Cu, Zn, Cd and Pb. Standard statistical analyses were used to assess significant differences among the levels of the elements measured in different tissues and sediment and spatial distribution. The greatest values of potentially toxic metal concentrations were observed at the station near the industrial sites of Augusta and Priolo. Comparisons with the concentrations of the same metals in other sites of north and western Sicily and with data from surveys in other areas of the Mediterranean Sea are shown.