4.7 Article

Ocean acidification alleviates low-temperature effects on growth and photosynthesis of the red alga Neosiphonia harveyi (Rhodophyta)

Journal

JOURNAL OF EXPERIMENTAL BOTANY
Volume 64, Issue 18, Pages 5587-5597

Publisher

OXFORD UNIV PRESS
DOI: 10.1093/jxb/ert329

Keywords

Carbonic anhydrase; CCM; climate change; CO2; DIC; distribution; macroalgae; photosynthesis

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Funding

  1. German Federal Ministry for Science and Education (BMBF) [Forderkennzeichen 03F0608B]

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This study aimed to examine interactive effects between ocean acidification and temperature on the photosynthetic and growth performance of Neosiphonia harveyi. N. harveyi was cultivated at 10 and 17.5 C at present (similar to 380 atm), expected future (similar to 800 atm), and high (similar to 1500 atm) pCO(2). Chlorophyll a fluorescence, net photosynthesis, and growth were measured. The state of the carbon-concentrating mechanism (CCM) was examined by pH-drift experiments (with algae cultivated at 10 C only) using ethoxyzolamide, an inhibitor of external and internal carbonic anhydrases (exCA and intCA, respectively). Furthermore, the inhibitory effect of acetazolamide (an inhibitor of exCA) and Tris (an inhibitor of the acidification of the diffusive boundary layer) on net photosynthesis was measured at both temperatures. Temperature affected photosynthesis (in terms of photosynthetic efficiency, light saturation point, and net photosynthesis) and growth at present pCO(2), but these effects decreased with increasing pCO(2). The relevance of the CCM decreased at 10 C. A pCO(2) effect on the CCM could only be shown if intCA and exCA were inhibited. The experiments demonstrate for the first time interactions between ocean acidification and temperature on the performance of a non-calcifying macroalga and show that the effects of low temperature on photosynthesis can be alleviated by increasing pCO(2). The findings indicate that the carbon acquisition mediated by exCA and acidification of the diffusive boundary layer decrease at low temperatures but are not affected by the cultivation level of pCO(2), whereas the activity of intCA is affected by pCO(2). Ecologically, the findings suggest that ocean acidification might affect the biogeographical distribution of N. harveyi.

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