Abstract

Hygrophila polysperma is a heterophyllous amphibious plant. The growth of H. polysperma in submerged conditions is challenging due to the low CO2 environment, increased resistance to gas diffusion, and bicarbonate ion (HCO3–) being the dominant dissolved inorganic carbon source. The submerged leaves of H. polysperma have significantly higher rates of underwater photosynthesis compared with the terrestrial leaves. 4,4′-Diisothiocyanatostilbene-2,2′-disulfonate (DIDS), an anion exchanger protein inhibitor, and ethoxyzolamide (EZ), an inhibitor of internal carbonic anhydrase, repressed underwater photosynthesis by the submerged leaves. These results suggested that H. polysperma acclimates to the submerged condition by using HCO3– for photosynthesis. H. polysperma transports HCO3– into the leaf by a DIDS-sensitive HCO3– transporter and converted to CO2 by carbonic anhydrase. Additionally, proteome analysis revealed that submerged leaves accumulated fewer proteins associated with C4 photosynthesis compared with terrestrial leaves. This finding suggested that H. polysperma is capable of C4 and C3 photosynthesis in the terrestrial and submerged leaves, respectively. The ratio of phosphoenol pyruvate carboxylase to ribulose 1,5-bisphosphate carboxylase/oxygenase (Rubisco) in the submerged leaves was less than that in the terrestrial leaves. Upon anatomical observation, the terrestrial leaves exhibited a phenotype similar to the Kranz anatomy found among C4 plants; however, chloroplasts in the bundle sheath cells were not located adjacent to the vascular bundles, and the typical Kranz anatomy was absent in submerged leaves. These results suggest that H. polysperma performs proto-Kranz type photosynthesis in a terrestrial environment and shifts from a proto-Kranz type in terrestrial leaves to a HCO3– use photosynthesis in the submerged environments.

Highlights

  • Carbon assimilation is essential for plant growth

  • Underwater photosynthetic O2 evolution rate (Pn) per unit leaf area responded to dissolved inorganic carbon (DIC) and light differently than underwater Pn expressed relative to the chlorophyll content

  • Terrestrial leaves had a larger underwater Pn on a per leaf area basis compared with submerged leaves at high DIC levels and high light intensities (Supplementary Figure 1)

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Summary

Introduction

Carbon assimilation is essential for plant growth. Higher plants evolved C4 photosynthesis and crassulacean acid metabolism (CAM) to maintain carbon assimilation rates under conditions limiting carbon acquisition. C4 photosynthesis and CAM concentrate CO2 around ribulose 1,5-bisphosphate carboxylase/oxygenase (Rubisco) to avoid limiting carbon assimilation condition such as when the stomata are closed. C4 photosynthesis concentrates CO2 by physically separating primary CO2 fixation by phosphoenol pyruvate carboxylase (PEPC) in mesophyll cells (MCs) from secondary fixation by Rubisco in bundle sheath cells (BSCs) (Hatch, 1971; Kanai and Edwards, 1973). CAM plants fix CO2 using PEPC during the night and conduct secondary fixation by Rubisco during the day (Black et al, 2003). C4 photosynthesis and CAM are adaptations allowing photosynthesis to continue in limiting CO2 conditions (Sage et al, 2012)

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