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Springer (part of Springer Nature), Aquatic Sciences - Research Across Boundaries, 4(77), p. 695-707

DOI: 10.1007/s00027-015-0412-9

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Biofilm growth and nitrogen uptake responses to increases in nitrate and ammonium availability

Journal article published in 2015 by Miquel Ribot ORCID, Daniel von Schiller, Francesc Sabater, Eugènia Martí
This paper is available in a repository.
This paper is available in a repository.

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Abstract

13 páginas, 4 tablas, 5 figuras ; Nitrate (NO3 -) and ammonium (NH4 +) are the two major dissolved inorganic nitrogen (DIN) species available in streams. Human activities increase stream DIN concentrations and modify the NO3 -:NH4 + ratio. However, few studies have examined biofilm responses to enrichment of both DIN species. We examined biofilm responses to variation in ambient concentrations and enrichments in either NO3 - or NH4 +. We incubated nutrient diffusing substrata (NDS) bioassays with three treatments (DIN-free, +NO3 - and +NH4 +) in five streams. Biomass-specific uptake rates (Uspec) of NO3 - and NH4 + were then measured using in situ additions of 15N-labeled NO3 - and NH4 +. Biomass (estimated from changes in carbon content) and algal accrual rates, as well as Uspec- NO3 - of biofilms in DIN-free treatments varied among the streams in which the NDS had been incubated. Higher ambient DIN concentrations were only correlated with enhanced biofilm growth rates. Uspec-NO3 - was one order of magnitude greater and more variable than Uspec-NH4 +, however similar relative preference index (RPI) suggested that biofilms did not show a clear preference for either DIN species. Biofilm growth and DIN uptake in DIN-amended NDS (i.e., +NO3 - and +NH4 +) were consistently lower than in DIN-free NDS (i.e., control). Lower values in controls with respect to amended NDS were consistently more pronounced for algal accrual rates and Uspec-NO3 - and for the +NH4 + than for the +NO3 - treatments. In particular, enrichment with NH4 + reduced biofilm Uspec- NO3 - uptake, which has important implications for N cycling in high NH4 + streams. ; This study was funded by the Spanish Ministry of Education and Science through NICON project (ref: CGL2005-7362). MR was supported by a contract with the Spanish Ministry of Science and Innovation through the MED_FORSTREAM project (CGL2011-30590-C02-02). DvS’s work was also funded by a Juan de la Cierva postdoctoral contract (JCI-2010-06397) from the Spanish Ministry of Science and Innovation. ; Peer reviewed