Abstract

The photoautotrophic, unicellular N2-fixer, Cyanothece, is a model organism that has been widely used to study photosynthesis regulation, the structure of photosystems, and the temporal segregation of carbon (C) and nitrogen (N) fixation in light and dark phases of the diel cycle. Here, we present a simple quantitative model and experimental data that together, suggest external dissolved inorganic carbon (DIC) concentration as a major limiting factor for Cyanothece growth, due to its high C-storage requirement. Using experimental data from a parallel laboratory study as a basis, we show that after the onset of the light period, DIC was rapidly consumed by photosynthesis, leading to a sharp drop in the rate of photosynthesis and C accumulation. In N2-fixing cultures, high rates of photosynthesis in the morning enabled rapid conversion of DIC to intracellular C storage, hastening DIC consumption to levels that limited further uptake. The N2-fixing condition allows only a small fraction of fixed C for cellular growth since a large fraction was reserved in storage to fuel night-time N2 fixation. Our model provides a framework for resolving DIC limitation in aquatic ecosystem simulations, where DIC as a growth-limiting factor has rarely been considered, and importantly emphasizes the effect of intracellular C allocation on growth rate that varies depending on the growth environment.

Highlights

  • By reducing atmospheric CO2 into bioavailable carbon (C), photosynthesis is the driving process of global ecosystem productivity⇑ Corresponding author at: Graduate School of Oceanography, University of and biogeochemical cycles

  • We have developed a simple, cellular model of Cyanothece (CFM-Cyano) focusing on dissolved inorganic carbon (DIC) limitation

  • The model reproduced laboratory data both for N2-fixing and NO3À available conditions demonstrating that, under N2-fixing conditions, C storage is prioritized during the early photoperiod to accumulate C in storage for N2 fixation during the night, and later during the day, biosynthesis increases

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Summary

Introduction

By reducing atmospheric CO2 into bioavailable carbon (C), photosynthesis is the driving process of global ecosystem productivity⇑ Corresponding author at: Graduate School of Oceanography, University of and biogeochemical (nutrient) cycles. Phytoplanktonic organisms are responsible for most aquatic photosynthesis, and account for about half the primary production on earth [1]. A growing body of literature reveals prokaryotic, nitrogen-fixing organisms as key players in the dynamics of phytoplanktonic communities and the world ocean’s primary production.

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