We investigated the effect of benthic substratum type (sand and rocks) and nutrient supply (N and P) on biofilm structure and heterotrophic metabolism in a field experiment in a forested Mediterranean stream (Fuirosos). Rock and sand colonization and biofilm formation was intensively studied for 44 d at two stream reaches: control and experimental (continuous addition of phosphate, ammonia, and nitrate). Structural (C, N, and polysaccharide content and bacterial and chlorophyll density) and metabolic biofilm parameters (-glucosidase, peptidase, and phosphatase enzyme activities) were analyzed throughout the colonization process. The epilithic biofilm (grown on rocks) had a higher peptidase activity at the impacted reach, together with a higher algal and bacterial biomass. The positive relationship between the peptidase activity per cell and the N content of the epilithic biofilm suggested that heterotrophic utilization of proteinaceous compounds from within the biofilm was occurring. In contrast, nutrient addition caused the epipsammic biofilm (grown on sand) to exhibit lower -glucosidase and phosphatase activities, without a significant increase in bacterial and algal biomass. The differential response to nutrient addition was related to different structural characteristics within each biofilm. The epipsammic biofilm had a constant and high C : N ratio (22.7) throughout the colonization. The epilithic biofilm had a higher C : N ratio at the beginning of the colonization (43.2) and evolved toward a more complex structure (high polysaccharide content and low C : N ratio) during later stages. The epipsammic biofilm was a site for the accumulation and degradation of organic matter: polysaccharides and organic phosphorus compounds had higher degradation activities.Microorganisms play a key role in the degradation of organic matter and the associated release of energy in stream ecosystems (Meyer 1994). Microbial communities feed on allochthonous (dissolved and particulate plant and animal materials) and/or autochthonous organic matter (algal detritus and exudates) and are the main factor responsible for river C cycling (Allan 1995). In low-order streams, the benthic community is the most important site for organic matter cycling. In most cases, rock, cobbles, sand, and wood coexist in a stream reach, and all of these substrata host biofilms with differing structural characteristics (Lock 1993). In association with these structural differences, there are also significant differences in photosynthetic activity, biofilm thick-
AcknowledgmentsWe thank two anonymous reviewers for their helpful suggestions about the manuscript. Comments by E. Garcia Berthou and C. Freeman are very much appreciated.