The input of continental organic matter (OM) was studied in the trophodynamic system of a shelf area (NW Mediterranean).
Stable isotopic composition and biochemical components of sedimentary OM were used as input proxies.
The highest continental influence was observed within the 50-m isobaths (3–4 km from the coast).
Allochthonous carbohydrates were recycled by microbiota, allowing terrigenous OM entrance in the lower food web.
Macrofaunal organisms consumed allochthonous OM, but also selected autochthonous OM and prey.