Journal cover Journal topic
Biogeosciences An interactive open-access journal of the European Geosciences Union
Journal topic
Volume 14, issue 9
Biogeosciences, 14, 2469–2480, 2017
https://doi.org/10.5194/bg-14-2469-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
Biogeosciences, 14, 2469–2480, 2017
https://doi.org/10.5194/bg-14-2469-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 16 May 2017

Research article | 16 May 2017

Sequential nutrient uptake as a potential mechanism for phytoplankton to maintain high primary productivity and balanced nutrient stoichiometry

Kedong Yin1,2, Hao Liu1,2, and Paul J. Harrison3,† Kedong Yin et al.
  • 1School of Marine Sciences, Sun Yat-sen University, Guangzhou, China
  • 2Key Laboratory of Marine Resources and Coastal Engineering in Guangdong Province, Guangzhou, China
  • 3Department of Earth and Ocean Sciences, University of British Columbia, Vancouver BC V6T 1Z4, Canada
  • deceased

Abstract. We hypothesize that phytoplankton have the sequential nutrient uptake strategy to maintain nutrient stoichiometry and high primary productivity in the water column. According to this hypothesis, phytoplankton take up the most limiting nutrient first until depletion, continue to draw down non-limiting nutrients and then take up the most limiting nutrient rapidly when it is available. These processes would result in the variation of ambient nutrient ratios in the water column around the Redfield ratio. We used high-resolution continuous vertical profiles of nutrients, nutrient ratios and on-board ship incubation experiments to test this hypothesis in the Strait of Georgia. At the surface in summer, ambient NO3 was depleted with excess PO43− and SiO4 remaining, and as a result, both N : P and N : Si ratios were low. The two ratios increased to about 10 : 1 and 0. 45 : 1, respectively, at 20 m. Time series of vertical profiles showed that the leftover PO43− continued to be removed, resulting in additional phosphorus storage by phytoplankton. The N : P ratios at the nutricline in vertical profiles responded differently to mixing events. Field incubation of seawater samples also demonstrated the sequential uptake of NO3 (the most limiting nutrient) and then PO43− and SiO4 (the non-limiting nutrients). This sequential uptake strategy allows phytoplankton to acquire additional cellular phosphorus and silicon when they are available and wait for nitrogen to become available through frequent mixing of NO3 (or pulsed regenerated NH4). Thus, phytoplankton are able to maintain high productivity and balance nutrient stoichiometry by taking advantage of vigorous mixing regimes with the capacity of the stoichiometric plasticity. To our knowledge, this is the first study to show the in situ dynamics of continuous vertical profiles of N : P and N : Si ratios, which can provide insight into the in situ dynamics of nutrient stoichiometry in the water column and the inference of the transient status of phytoplankton nutrient stoichiometry in the coastal ocean.

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Short summary
Nutrient-limited phytoplankton are capable of first taking up the limiting nutrient and continuing to take up non-limiting nutrients after the exhaustion of the limiting nutrient, and then taking up the limiting nutrient rapidly when it is available due to mixing of the water column. We refer to this process as phytoplankton sequential nutrient uptake. Our results showed the sequential nutrient uptake, a process to maintain the phytoplankton nutrient stoichiometry and high primary productivity.
Nutrient-limited phytoplankton are capable of first taking up the limiting nutrient and...
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