“…In natural nutrient-plankton systems, waters flowing into the system bring input of fluxes of nutrients and outflows also carry out nutrients [4,10,32,33]. The rate of waters flowing in and out of the system is a constant and denoted by D. However, unlike the study in [19], we assume that the input nutrient concentration N 0 (t) is varied periodically around N 0 with N 0 (t) = N 0 + ar(t), where N 0 > 0, 0 < a < N 0 , and r(t) is τ -periodic with mean value zero and |r(t)| ≤ 1 for t ≥ 0. The consideration of periodic input of nutrients is motivated by the tidal, day/night, or seasonal cycles occurring in nature.…”