Abstract
Transfer and transformation processes of hydrocarbons between the surficial water and the sediment have been studied in the open Western Mediterranean Sea, by determining concentrations and distributions of non-volatile n-alkanes, isoprenoids, non-aromatic and aromatic hydrocarbons in the surficial sediment and in three fractions of the water column: dissolved matter, small-size and large-size particulates (> 63 μm). Hydrocarbons have been analysed by capillary gas liquid chromatography and HPLC/UV spectrophotometry. Hydrocarbons are present essentially in a dissolved form in the water column (for more than 90% for samples collected below 1,000m) and associated with small-size particles. The stock of hydrocarbons present in large-size, rapidly sinking particles accounts for less than 0.3%. Concentrations found in the water column are low, except for the surficial water in the Ligurian Sea (>20μg1−1). They decrease with depth to reach values less than 0.2 μg 1−1 below 1,000 m. The sediments are characterized by low concentrations (3.9–7.1 μgg−1). The nature of hydrocarbons is very different with respect to each pool: essentially petrogenic for the water column, derived from marine productivity and terrestrial higher plants waxes for large-size particles and sediments. Estimations of vertical flux of hydrocarbons are discussed in terms of mode of settling of hydrocarbons from the sea surface.