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      The nature of the CO2-concentrating mechanisms in a marine diatom,Thalassiosira pseudonana

      , , ,
      New Phytologist
      Wiley-Blackwell

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          Abstract

          Diatoms are widespread in aquatic ecosystems where they may be limited by the supply of inorganic carbon. Their carbon dioxide-concentrating mechanisms (CCMs) involving transporters and carbonic anhydrases (CAs) are well known, but the contribution of a biochemical CCM involving C4 metabolism is contentious. The CCM(s) present in the marine-centric diatom, Thalassiosira pseudonana, were studied in cells exposed to high or low concentrations of CO2 , using a range of approaches. At low CO2 , cells possessed a CCM based on active uptake of CO2 (70% contribution) and bicarbonate, while at high CO2 , cells were restricted to CO2 . CA was highly and rapidly activated on transfer to low CO2 and played a key role because inhibition of external CA produced uptake kinetics similar to cells grown at high CO2 . The activities of phosphoenolpyruvate (PEP) carboxylase (PEPC) and the PEP-regenerating enzyme, pyruvate phosphate dikinase (PPDK), were lower in cells grown at low than at high CO2 . The ratios of PEPC and PPDK to ribulose bisphosphate carboxylase were substantially lower than 1, even at low CO2 . Our data suggest that the kinetic properties of this species results from a biophysical CCM and not from C4 type metabolism.

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          Most cited references50

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          Carbon dioxide in water and seawater: the solubility of a non-ideal gas

          R.F. Weiss (1974)
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            The evolution of C4photosynthesis

            Rowan Sage (2004)
            C4 photosynthesis is a series of anatomical and biochemical modifications that concentrate CO2 around the carboxylating enzyme Rubisco, thereby increasing photosynthetic efficiency in conditions promoting high rates of photorespiration. The C4 pathway independently evolved over 45 times in 19 families of angiosperms, and thus represents one of the most convergent of evolutionary phenomena. Most origins of C4 photosynthesis occurred in the dicots, with at least 30 lineages. C4 photosynthesis first arose in grasses, probably during the Oligocene epoch (24-35 million yr ago). The earliest C4 dicots are likely members of the Chenopodiaceae dating back 15-21 million yr; however, most C4 dicot lineages are estimated to have appeared relatively recently, perhaps less than 5 million yr ago. C4 photosynthesis in the dicots originated in arid regions of low latitude, implicating combined effects of heat, drought and/or salinity as important conditions promoting C4 evolution. Low atmospheric CO2 is a significant contributing factor, because it is required for high rates of photorespiration. Consistently, the appearance of C4 plants in the evolutionary record coincides with periods of increasing global aridification and declining atmospheric CO2 . Gene duplication followed by neo- and nonfunctionalization are the leading mechanisms for creating C4 genomes, with selection for carbon conservation traits under conditions promoting high photorespiration being the ultimate factor behind the origin of C4 photosynthesis. Contents Summary 341 I. Introduction 342 II. What is C4 photosynthesis? 343 III. Why did C4 photosynthesis evolve? 347 IV. Evolutionary lineages of C4 photosynthesis 348 V. Where did C4 photosynthesis evolve? 350 VI. How did C4 photosynthesis evolve? 352 VII. Molecular evolution of C4 photosynthesis 361 VIII. When did C4 photosynthesis evolve 362 IX. The rise of C4 photosynthesis in relation to climate and CO2 363 X. Final thoughts: the future evolution of C4 photosynthesis 365 Acknowledgements 365 References 365.
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              Efficiency of the CO2-concentrating mechanism of diatoms.

              Diatoms are responsible for a large fraction of CO(2) export to deep seawater, a process responsible for low modern-day CO(2) concentrations in surface seawater and the atmosphere. Like other photosynthetic organisms, diatoms have adapted to these low ambient concentrations by operating a CO(2) concentrating mechanism (CCM) to elevate the concentration of CO(2) at the site of fixation. We used mass spectrometric measurements of passive and active cellular carbon fluxes and model simulations of these fluxes to better understand the stoichiometric and energetic efficiency and the physiological architecture of the diatom CCM. The membranes of diatoms are highly permeable to CO(2), resulting in a large diffusive exchange of CO(2) between the cell and external milieu. An active transport of carbon from the cytoplasm into the chloroplast is the main driver of the diatom CCM. Only one-third of this carbon flux is fixed photosynthetically, and the rest is lost by CO(2) diffusion back to the cytoplasm. Both the passive influx of CO(2) from the external medium and the recycling of the CO(2) leaking out of the chloroplast are achieved by the activity of a carbonic anhydrase enzyme combined with the maintenance of a low concentration of HCO(3)(-) in the cytoplasm. To achieve the CO(2) concentration necessary to saturate carbon fixation, the CO(2) is most likely concentrated within the pyrenoid, an organelle within the chloroplast where the CO(2)-fixating enzyme is located.
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                Author and article information

                Journal
                New Phytologist
                New Phytol
                Wiley-Blackwell
                0028646X
                March 2016
                March 2016
                : 209
                : 4
                : 1417-1427
                Article
                10.1111/nph.13728
                26529678
                6f7f5e22-47a7-43f9-8e1a-6a21a7b35274
                © 2016
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