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The responses of coastal microbial communities to nutrient inputs depend on the magnitude and nature of those inputs. To understand the response of prokaryote communities to contrasting levels of nutrient inputs from different sources, three nutrient addition experiments were performed in the Ría de Vigo in spring, summer, and autumn. The experiments consisted of controlled inorganic (nitrate, ammonium and phosphate), organic (glucose and a mix of 18 amino acids), and mixed (inorganic and organic); as well as natural (atmospheric and riverine) nutrient additions to surface water samples taken from the middle of the embayment and incubated for 48h, under in situ temperature and irradiance conditions. Prokaryote community DNA was collected and analyzed using high-throughput amplicon sequencing of the 16S rRNA gene. The joint addition of inorganic and organic nutrients provoked the most pronounced changes in community composition, systematically leading to great increases in the proportion of sequence reads belonging to Vibrionales, while natural amendments only caused subtle alterations. The proportion of reads assigned to the Planktomarina genus, bacteria belonging to the order Rhodobacterales, tended to increase when natural atmospheric nutrients were added. Overall, the fraction of reads belonging to the order Flavobacteriales did not show relevant changes, although the contribution of sequences affiliated to Polaribacter and Aurantivirga genera increased after atmospheric and riverine inputs in summer, and autumn. The proportion of Vibrionales reads also increased after controlled organic amendments in autumn, and to a lesser extent after riverine additions in spring and summer. In general, our findings suggest that an increasing input of nitrogenous organic matter from allochthonous sources into this coastal environment might promote the growth of potentially pathogenic bacteria belonging to the order Vibrionales. • Nutrient additions into coastal systems change communities of prokaryotic plankton. • The magnitude and nature of those inputs determine the extent and direction of the changes in prokaryotic composition. • Addition of organic nitrogen into coastal systems or estuaries can promote blooms of potentially pathogenic Vibrio bacteria. [ABSTRACT FROM AUTHOR]

Over the past decades, as a consequence of human activity, there was an increase in nutrient inputs to the ocean and they are expected to enhance even more in the future. Coastal areas, accounting for a significant proportion of marine primary productivity, are the most vulnerable zones to anthropogenic impacts. The response of phytoplankton communities to an increase in organic and inorganic nutrients levels from natural allochthonous sources was assessed in microcosm experiments conducted in a coastal system affected by intermittent upwelling events (Ría de Vigo, NW Iberia). Three nutrient addition experiments were performed in spring, summer and autumn, when surface water was supplemented with 5 and 10% of atmospheric and riverine matter. Pico-, nano- and microphytoplankton abundances, chlorophyll a concentration (Chl a ) and primary production rates (PP) were measured and compared with those in the control seawater sample (without additions) after 48 h of incubation. Simultaneous experiments with controlled additions of inorganic and organic nutrients were also performed in order to describe the limiting nutrient for phytoplankton growth at each experiment. The composition of the matter inputs and the structure of the phytoplankton communities determined the type of response observed. Phytoplankton responses varied among seasons, being positively correlated with dissolved inorganic nitrogen (DIN) concentrations. As expected, the phytoplankton responses to external nutrient inputs were stronger under low nutrient levels (summer) than when phytoplankton was already growing in nutrient replete conditions (spring). Null and negative responses to the natural inputs were observed in autumn, which suggests that the oceanic phytoplankton advected to this coastal system during downwelling events could be occasionally inhibited by these nutrient inputs. In a future global change scenario, characterized by enhanced nutrient inputs from riverine and atmospheric origin, the response of phytoplankton communities will strongly depend on the concentration and chemical composition of these inputs and on the structure of phytoplankton communities able to respond to them. [ABSTRACT FROM AUTHOR]