Abstract

Abstract. Anthropogenic carbon dioxide (CO2) emissions are causing severe changes in the global inorganic carbon balance of the oceans. Associated ocean acidification is expected to pose a major threat to marine ecosystems worldwide, and it is also expected to be amplified in the Baltic Sea where the system is already exposed to relatively large natural seasonal and diel pH fluctuations. We studied the responses of larvae of the benthic key species Macoma balthica to a range of future CO2 scenarios using six ∼ 55 m3 mesocosms encompassing the entire pelagic community. The mesocosms were deployed in the northern Baltic Sea in June 2012. We focused on the survival, growth and subsequent settlement process of Macoma balthica when exposed to different levels of future CO2. The size and time to settlement of M. balthica increased along the CO2 gradient, suggesting a developmental delay. With ongoing climate change, both the frequency and extent of regularly occurring high CO2 conditions are likely to increase, and a permanent pH decrease will likely occur. The strong impact of increasing CO2 levels on early-stage bivalves is alarming as these stages are crucial for sustaining viable populations, and a failure in their recruitment would ultimately lead to negative effects on the population.

Highlights

  • Anthropogenic CO2 emissions are causing severe changes in the oceans (Feely et al, 2004)

  • In this study we investigated the effects of different future CO2 scenarios on the larval survival, growth and settling of a Baltic Sea benthic key species M. balthica in a largescale mesocosm setting

  • We found that M. balthica settled later along the increasing f CO2 gradient of the mesocosms

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Summary

Introduction

Anthropogenic CO2 emissions are causing severe changes in the oceans (Feely et al, 2004). The majority of studies investigating the biological effects of future CO2 levels have focused on their impacts on calcifying species and on pelagic primary producers. Pelagic calcifiers such as bivalve early-life stages are generally considered susceptible to increasing CO2 levels (Kurihara, 2008; Dupont and Thorndyke, 2009), with a range of observed (mostly negative) impacts on development, survival and growth of larval stages as consequences of the CO2 increase (Gazeau et al, 2013). The settling and survival of post-larvae are impacted by the changes in the water chem-

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