Abstract

Ocean acidification is considered as a crucial stressor for marine communities. In this study, we tested the effects of the IPCC RPC6.0 end-of-century acidification scenario on a natural plankton community in the Gullmar Fjord, Sweden, during a long-term mesocosm experiment from a spring bloom to a mid-summer situation. The focus of this study was on microzooplankton and its interactions with phytoplankton and mesozooplankton. The microzooplankton community was dominated by ciliates, especially small Strombidium sp., with the exception of the last days when heterotrophic dinoflagellates increased in abundance. We did not observe any effects of high CO2 on the community composition and diversity of microzooplankton. While ciliate abundance, biomass and growth rate were not affected by elevated CO2, we observed a positive effect of elevated CO2 on dinoflagellate abundances. Additionally, growth rates of dinoflagellates were significantly higher in the high CO2 treatments. Given the higher Chlorophyll a content measured under high CO2, our results point at mainly indirect effects of CO2 on microzooplankton caused by changes in phytoplankton standing stocks, in this case most likely an increase in small-sized phytoplankton of <8 μm. Overall, the results from the present study covering the most important part of the growing season indicate that coastal microzooplankton communities are rather robust towards realistic acidification scenarios.

Highlights

  • Atmospheric CO2 concentrations have increased considerably from 280 μatm at pre-industrial times to currently about 400 μatm [1] and are predicted to reach up to 1000 μatm by the end of this century (IPCC scenario RPC6.0) [2]

  • We investigated the impacts of high CO2 levels on natural plankton communities during a long-term mesocosm study in the Gullmar Fjord, Skagerrak

  • We found a positive effect of high CO2 on the growth rates of total dinoflagellates (p-value = 0.043) and athecate dinoflagellates

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Summary

Introduction

Atmospheric CO2 concentrations have increased considerably from 280 μatm at pre-industrial times to currently about 400 μatm [1] and are predicted to reach up to 1000 μatm by the end of this century (IPCC scenario RPC6.0) [2]. The oceans act as a major CO2 sink and have absorbed about 30% of the anthropogenic CO2 since the beginning of the industrial revolution [3]. This obviously has affected the ocean’s carbonate system, leading to increased CO2 and PLOS ONE | DOI:10.1371/journal.pone.0165800. Low CO2 Sensitivity of Microzooplankton in the Skagerrak role in study design, data collection and analysis, decision to publish, or preparation of the manuscript

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