Widespread use of proton-pumping rhodopsin in Antarctic phytoplankton

Photosynthetic carbon (C) fixation by phytoplankton in the Southern Ocean (SO) plays a critical role in regulating air–sea exchange of carbon dioxide and thus global climate. In the SO, photosynthesis (PS) is often constrained by low iron, low temperatures, and low but highly variable light intensit...

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Bibliographic Details
Published in:Proceedings of the National Academy of Sciences
Main Authors: Andrew, Sarah M., Moreno, Carly M., Plumb, Kaylie, Hassanzadeh, Babak, Gómez-Consarnau, Laura, Smith, Stephanie N., Schofield, Oscar, Yoshizawa, Susumu, Fujiwara, Takayoshi, Sunda, William G., Hopkinson, Brian M., Septer, Alecia N., Marchetti, Adrian
Other Authors: National Science Foundation (US)
Format: Article in Journal/Newspaper
Language:English
Published: National Academy of Sciences (U.S.) 2023
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Online Access:http://hdl.handle.net/10261/354006
https://doi.org/10.1073/pnas.2307638120
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Summary:Photosynthetic carbon (C) fixation by phytoplankton in the Southern Ocean (SO) plays a critical role in regulating air–sea exchange of carbon dioxide and thus global climate. In the SO, photosynthesis (PS) is often constrained by low iron, low temperatures, and low but highly variable light intensities. Recently, proton-pumping rhodopsins (PPRs) were identified in marine phytoplankton, providing an alternate iron-free, light-driven source of cellular energy. These proteins pump protons across cellular membranes through light absorption by the chromophore retinal, and the resulting pH energy gradient can then be used for active membrane transport or for synthesis of adenosine triphosphate. Here, we show that PPR is pervasive in Antarctic phytoplankton, especially in iron-limited regions. In a model SO diatom, we found that it was localized to the vacuolar membrane, making the vacuole a putative alternative phototrophic organelle for light-driven production of cellular energy. Unlike photosynthetic C fixation, which decreases substantially at colder temperatures, the proton transport activity of PPR was unaffected by decreasing temperature. Cellular PPR levels in cultured SO diatoms increased with decreasing iron concentrations and energy production from PPR photochemistry could substantially augment that of PS, especially under high light intensities, where PS is often photoinhibited. PPR gene expression and high retinal concentrations in phytoplankton in SO waters support its widespread use in polar environments. PPRs are an important adaptation of SO phytoplankton to growth and survival in their cold, iron-limited, and variable light environment. This work was funded by the NSF Grants OPP1745036 (to A.N.S. and A.M.), OPP1744760 (to B.M.H.), and PLR1440435 (to O.S.). Peer reviewed