Riverine and wet atmospheric inputs of materials to a North Africa coastal site (Annaba Bay, Algeria)

Abstract This study simultaneously assesses for the first time the relative contributions of riverine and wet atmospheric inputs of materials into the Algerian Annaba Bay on the Mediterranean coast of North Africa. Surface water sampling and water discharge estimates were performed weekly in 2014 at the outlets of the Mafragh River (MR) and Seybouse River (SR). Riverine samples were analyzed for dissolved nutrients and particulate matter (suspended particulate matter: SPM; particulate organic carbon: POC; biogenic silica: BSi; chlorophyll a : Chl a ; particulate organic nitrogen: PON and particulate organic phosphorus (POP). Rainwater samples were jointly collected at a close weather station on a daily basis and analyzed for dissolved nutrients. The rainwater from the Annaba region was characterized by high concentrations of phosphate (PO 4 ) and silicic acid (Si(OH) 4 ) that are several times the average Mediterranean values, and by strong deposition fluxes. Conversely, the levels of dissolved inorganic nitrogen (DIN) and dissolved organic nitrogen (DON) and associated fluxes were remarkably low. The dissolved nutrient fluxes for the two catchments were low following the lowering of the river flows, but those of particulate matter (POC, Chl a , BSi) displayed significant amounts, especially for the MR catchment. BSi and POP represented approximately a third of the total silicon and total phosphorus fluxes, respectively. The levels of dissolved N and P in the MR water were comparable to those in rainwater. MR appeared to be a nearly pristine ecosystem with low nutrient levels and almost balanced N:P and Si:N ratios. SR water had low Si(OH) 4 levels but was highly charged with NH 4 and PO 4 and showed unbalanced N:P and Si:N ratios in almost all samples. These conditions have resulted in large phytoplankton biomasses, which may lead to eutrophication. More importantly, the rainwater was identified as a relevant source of fertilizers for marine waters and agricultural land in the Annaba area and can partially balance the loss of Si(OH) 4 from rivers to the bay due to dam retention.