The combined effect of pH and dissolved inorganic carbon concentrations on the physiology of plastidic ciliate Mesodinium rubrum and its cryptophyte prey

Ocean acidification is caused by rising atmospheric partial pressure of CO 2 (pCO 2 ) and involves a lowering of pH combined with increased concentrations of CO 2 and dissolved in organic carbon in ocean waters. Many studies investigated the consequences of these combined changes on marine phytoplan...

Full description

Bibliographic Details
Main Authors: Eriksen, Christine Schultz Yde, Walli, Melanie Desmaret, Van de Waal, Dedmer B., Helmsing, Nico R., Dahl, Emma Ove, Sørensen, Helle, Hansen, Per Juel
Format: Article in Journal/Newspaper
Language:English
Published: 2023
Subjects:
DIC
pH
Online Access:https://pure.knaw.nl/portal/en/publications/bb351d76-1998-4651-a3d7-0b43fd64cd46
https://doi.org/10.1016/j.hal.2023.102509
https://hdl.handle.net/20.500.11755/bb351d76-1998-4651-a3d7-0b43fd64cd46
Description
Summary:Ocean acidification is caused by rising atmospheric partial pressure of CO 2 (pCO 2 ) and involves a lowering of pH combined with increased concentrations of CO 2 and dissolved in organic carbon in ocean waters. Many studies investigated the consequences of these combined changes on marine phytoplankton, yet only few attempted to separate the effects of decreased pH and increased pCO 2 . Moreover, studies typically target photoautotrophic phytoplankton, while little is known of plastidic protists that depend on the ingestion of plastids from their prey. Therefore, we studied the separate and interactive effects of pH and DIC levels on the plastidic ciliate Mesodinium rubrum, which is known to form red tides in coastal waters worldwide. Also, we tested the effects on their prey, which typically are cryptophytes belonging to the Teleaulax/Plagioslemis/Geminigera species complex. These cryptophytes not only serve as food for the ciliate, but also as a supplier of chloroplasts and prey nuclei. We exposed M. rubrum and the two cryptophyte species, T. acuta, T. amphioxeia to different pH (6.8 - 8) and DIC levels (∼ 6.5 - 26 mg C L -1 ) and assessed their growth and photosynthetic rates, and cellular chlorophyll a and elemental contents. Our findings did not show consistent significant effects across the ranges in pH and/or DIC, except for M. rubrum, for which growth was negatively affected only by the lowest pH of 6.8 combined with lower DIC concentrations. It thus seems that M. rubrum is largely resilient to changes in pH and DIC, and its blooms may not be strongly impacted by the changes in ocean carbonate chemistry projected for the end of the 21 st century.