Abstract

Abstract. Skeletonema costatum is a common bloom-forming diatom and encounters eutrophication and severe carbon dioxide (CO2) limitation during red tides. However, little is known regarding the role of phosphorus (P) in modulating inorganic carbon acquisition in S. costatum, particularly under CO2 limitation conditions. We cultured S. costatum under five phosphate levels (0.05, 0.25, 1, 4, 10 µmol L−1) and then treated it with two CO2 conditions (2.8 and 12.6 µmol L−1) for 2 h. The lower CO2 reduced net photosynthetic rate at lower phosphate levels (< 4 µmol L−1) but did not affect it at higher phosphate levels (4 and 10 µmol L−1). In contrast, the lower CO2 induced a higher dark respiration rate at lower phosphate levels (0.05 and 0.25 µmol L−1) and did not affect it at higher phosphate levels (> 1 µmol L−1). The lower CO2 did not change relative electron transport rate (rETR) at lower phosphate levels (0.05 and 0.25 µmol L−1) and increased it at higher phosphate levels (> 1 µmol L−1). Photosynthetic CO2 affinity (1/K0.5) increased with phosphate levels. The lower CO2 did not affect photosynthetic CO2 affinity at 0.05 µmol L−1 phosphate but enhanced it at the other phosphate levels. Activity of extracellular carbonic anhydrase was dramatically induced by the lower CO2 in phosphate-replete conditions (> 0.25 µmol L−1) and the same pattern also occurred for redox activity of the plasma membrane. Direct bicarbonate (HCO3-) use was induced when phosphate concentration was more than 1 µmol L−1. These findings indicate P enrichment could enhance inorganic carbon acquisition and thus maintain the photosynthesis rate in S. costatum grown under CO2-limiting conditions via increasing activity of extracellular carbonic anhydrase and facilitating direct HCO3- use. This study sheds light on how bloom-forming algae cope with carbon limitation during the development of red tides.

Highlights

  • Diatoms are unicellular photosynthetic microalgae that can be found worldwide in freshwater and oceans

  • Post hoc Least significant difference (LSD) comparison (P = 0.05) showed that 2.8 μmol of CO2 reduced net photosynthetic rate when the phosphate level was below 4 μmol L−1 but did not affect it at the higher phosphate levels

  • The present study investigated the role of P in regulating inorganic carbon acquisition and CO2 concentrating mechanisms in diatoms for the first time

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Summary

Introduction

Diatoms are unicellular photosynthetic microalgae that can be found worldwide in freshwater and oceans. Diatoms usually dominate the phytoplankton communities and form large-scale blooms in nutrient-rich zones and upwelling regions (Bruland et al, 2001; Anderson et al, 2008; Barton et al, 2016). Nutrient enrichment is considered to be a key factor that triggers algal blooms, albeit the occurrence of diatom blooms may be modulated by other environmental factors, such as temperature, light intensity, and salinity (Smetacek and Zingone, 2013; Jeong et al, 2015). When inorganic nitrogen and phosphorus are replete, diatoms can outcompete chrysophytes, raphidophytes, and dinoflagellates (Berg et al, 1997; Jeong et al, 2015; Barton et al, 2016) and dominate algal blooms due to their quicker nutrient uptake and growth rate

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