Diel variations of nutrient retention and metabolism are coupled for ammonium but not for phosphorus in a lowland stream

EUGENIA MARTI; CLAUDIA FEIJOÓ; CAROLINA VILCHES; NICOLÁS FERREIRO; PATRICIA GANTES; CONSTANZA RANIERI; ANA TORREMORELL; CAROLINA RODRÍGUEZ CASTRO; MARÍA GULTEMIRIAM; ADONIS GIORGI; FRANCESC SABATER

Freshwater Science

The University of Chicago Press

Lugar: Chicago; Año: 2020

2161-9549

In-stream nutrient retention is an important ecosystem function because it can regulate nutrient fate and export to downstream ecosystems. Temporal variation in nutrient retention in streams has been studied extensively at the annual and seasonal scale but less thoroughly at the diel scale. However, understanding temporal variability in nutrient uptake at the diel scale can increase understanding of the role of photoautotrophic primary production on nutrient uptake in streams, especially open-canopy streams. We hypothesized that nutrient retention mostly depends on autotrophic demand in open-canopy streams and that it varies following the diel pattern of gross primary production (GPP). We therefore evaluated the temporal variation in phosphate (PO4 32) and ammonium (NH4 1) uptake at a daily scale in a highly-productive Pampean stream that is dominated by a dense assemblage of macrophytes and filamentous algae. We conducted 6 slug additions of PO4 32 and NH4 1 over a 24-h period and quantified reach scale nutrient uptake concurrently with measurements of whole-stream metabolism and chemical variables during additions (including nitrates and nitrites). The study stream had extremely high uptake of PO4 32 and NH41 (>90 and >75% retention of the P andNmass added, respectively). Uptake of PO432 did not vary throughout the day. Estimated PO432 uptake from GPP accounted for only a small fraction of observed PO4 32 uptake. Thus, another mechanism, such as heterotrophic demand by microbial assemblages or adsorption onto sediments, could also have contributed to PO432 uptake in the study stream. In contrast, NH41 uptake clearly varied throughout the day. Up to 48% of the observed NH41 uptake rate could be explained by NH41 estimated from GPP, and NH41 demand was positively associated with GPP, indicating a high dependence on photoautotrophic demand. An increase of nitrite (NO22) concentration during additions (representing up to 70% of the added mass of NH41) suggests that nitrification contributed to the diel pattern of NH41 uptake. Our results indicate that nutrient uptake does not always rely on autotrophic demand in open-canopy streams and that other abiotic and dissimilatory mechanisms may explain the diel patterns of nutrient retention. In addition, our study highlights the need tomeasure uptake metrics throughout the day to obtain an accurate estimate of nutrient retention on a daily scale.