FN Archimer Export Format PT J TI Nutrient Patchiness, Phytoplankton Surge-Uptake, and Turbulent History: A Theoretical Approach and Its Experimental Validation BT AF Schapira, Mathilde Seuront, Laurent AS 1:1;2:2,3,4; FF 1:PDG-ODE-LITTORAL-LERMPL;2:; C1 Ifremer, LITTORAL, F-44311 Nantes, France CNRS, Univ. Lille, Univ. Littoral Côte d’Opale, UMR 8187, LOG, Laboratoire d’Océanologie et de Géosciences, F-62930 Wimereux, France Department of Marine Resource and Energy, Tokyo University of Marine Science and Technology, 4-5-7 Konan, Minato-ku, Tokyo 108-8477, Japan Department of Zoology and Entomology, Rhodes University, Grahamstown 6140, South Africa C2 IFREMER, FRANCE CNRS, FRANCE UNIV TOKYO, JAPAN UNIV RHODES, SOUTH AFRICA SI NANTES SE PDG-ODE-LITTORAL-LERMPL IN WOS Ifremer UPR DOAJ copubli-france copubli-int-hors-europe copubli-sud TC 1 UR https://archimer.ifremer.fr/doc/00643/75527/76435.pdf LA English DT Article DE ;nutrient patchiness;turbulence;phytoplankton;surge uptake;nutrient depletion;turbulent history AB Despite ample evidence of micro- and small-scale (i.e., millimeter- to meter-scale) phytoplankton and zooplankton patchiness in the ocean, direct observations of nutrient distributions and the ecological importance of this phenomenon are still relatively scarce. In this context, we first describe a simple procedure to continuously sample nutrients in surface waters, and subsequently provide evidence of the existence of microscale distribution of ammonium in the ocean. We further show that ammonium is never homogeneously distributed, even under very high conditions of turbulence. Instead, turbulence intensity appears to control nutrient patchiness, with a more homogeneous or a more heterogeneous distribution observed under high and low turbulence intensities, respectively, under the same concentration in nutrient. Based on a modelling procedure taking into account the stochastic properties of intermittent nutrient distributions and observations carried out on natural phytoplankton communities, we introduce and verify the hypothesis that under nutrient limitation, the “turbulent history” of phytoplankton cells, i.e., the turbulent conditions they experienced in their natural environments, conditions their efficiency to uptake ephemeral inorganic nitrogen patches of different concentrations. Specifically, phytoplankton cells exposed to high turbulence intensities (i.e., more homogeneous nutrient distribution) were more efficient to uptake high concentration nitrogen pulses (2 µM). In contrast, under low turbulence conditions (i.e., more heterogeneous nutrient distribution), uptake rates were higher for low concentration nitrogen pulses (0.5 µM). These results suggest that under nutrient limitation, natural phytoplankton populations respond to high turbulence intensities through a decrease in affinity for nutrients and an increase in their transport rate, and vice versa. PY 2020 PD JUL SO Fluids SN 2311-5521 PU MDPI AG VL 5 IS 2 UT 000551761800001 DI 10.3390/fluids5020080 ID 75527 ER EF