AUTHOR=Tames-Espinosa Mayte , Martínez Ico , Romero-Kutzner Vanesa , Coca Josep , Algueró-Muñiz María , Horn Henriette G. , Ludwig Andrea , Taucher Jan , Bach Lennart , Riebesell Ulf , Packard Theodore T. , Gómez May TITLE=Metabolic Responses of Subtropical Microplankton After a Simulated Deep-Water Upwelling Event Suggest a Possible Dominance of Mixotrophy Under Increasing CO2 Levels JOURNAL=Frontiers in Marine Science VOLUME=7 YEAR=2020 URL=https://www.frontiersin.org/journals/marine-science/articles/10.3389/fmars.2020.00307 DOI=10.3389/fmars.2020.00307 ISSN=2296-7745 ABSTRACT=

In the autumn of 2014, nine large mesocosms were deployed in the oligotrophic subtropical North-Atlantic coastal waters off Gran Canaria (Spain). Their deployment was designed to address the acidification effects of CO₂ levels from 400 to 1,400 μatm, on a plankton community experiencing upwelling of nutrient-rich deep water. Among other parameters, chlorophyll a (chl-a), potential respiration (Φ), and biomass in terms of particulate protein (B) were measured in the microplankton community (0.7–50.0 μm) during an oligotrophic phase (Phase I), a phytoplankton-bloom phase (Phase II), and a post-bloom phase (Phase III). Here, we explore the use of the Φ/chl-a ratio in monitoring shifts in the microplankton community composition and its metabolism. Φ/chl-a values below 2.5 μL O₂ h⁻¹ (μg chl-a)⁻¹ indicated a community dominated by photoautotrophs. When Φ/chl-a ranged higher, between 2.5 and 7.0 μL O₂ h⁻¹ (μg chl-a)⁻¹, it indicated a mixed community of phytoplankton, microzooplankton and heterotrophic prokaryotes. When Φ/chl-a rose above 7.0 μL O₂ h⁻¹ (μg chl-a)⁻¹, it indicated a community where microzooplankton proliferated (>10.0 μL O₂ h⁻¹ (μg chl-a)⁻¹), because heterotrophic dinoflagellates bloomed. The first derivative of B, as a function of time (dB/dt), indicates the rate of protein build-up when positive and the rate of protein loss, when negative. It revealed that the maximum increase in particulate protein (biomass) occurred between 1 and 2 days before the chl-a peak. A day after this peak, the trough revealed the maximum net biomass loss. This analysis did not detect significant changes in particulate protein, neither in Phase I nor in Phase III. Integral analysis of Φ, chl-a and B, over the duration of each phase, for each mesocosm, reflected a positive relationship between Φ and pCO₂ during Phase II [α = 230·10⁻⁵ μL O₂ h⁻¹ L⁻¹ (μatm CO₂)⁻¹ (phase-day)⁻¹, R² = 0.30] and between chl-a and pCO₂ during Phase III [α = 100·10⁻⁵ μg chl-a L⁻¹ (μ atmCO₂)⁻¹ (phase-day)⁻¹, R² = 0.84]. At the end of Phase II, a harmful algal species (HAS), Vicicitus globosus, bloomed in the high pCO₂ mesocosms. In these mesocosms, microzooplankton did not proliferate, and chl-a retention time in the water column increased. In these V. globosus-disrupted communities, the Φ/chl-a ratio [4.1 ± 1.5 μL O₂ h⁻¹ (μg chl-a)⁻¹] was more similar to the Φ/chl-a ratio in a mixed plankton community than to a photoautotroph-dominated one.