Abstract

Ocean acidification is an emerging consequence of anthropogenic carbon dioxide emissions. The full extent of the biological impacts are currently not entirely defined. However, it is expected that invertebrate species that rely on the mineral calcium carbonate will be directly affected. Despite the limited understanding of the full extent of potential impacts and responses there is a need to identify potential pathways for human societies to be affected by ocean acidification. Research on these social implications is a small but developing field. This research contributes to this field by using an impact assessment framework, informed by a biophysical model of future species distributions, to investigate potential impacts facing Atlantic Canadian society from potential changes in shellfish fisheries driven by ocean acidification and climate change. New Brunswick and Nova Scotia are expected to see declines in resource accessibility but are relatively socially insulated from these changes. Conversely, Prince Edward Island, along with Newfoundland and Labrador are more socially vulnerable to potential losses in fisheries, but are expected to experience relatively minor net changes in access.

Highlights

  • Ocean acidification (OA) is a facet of climate change driven by increasing carbon dioxide (CO2) concentrations in the atmosphere and ocean [1,2]

  • In this analysis the Gulf and the Quebec management areas are treated as a single unit because both management areas are comparatively small and the biophysical model used to project distribution changes does not have sufficient resolution to reliably differentiate between these management areas

  • This study demonstrates that accounting for additional environmental factors can allow for different, and potentially more representative, narratives to emerge

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Summary

Introduction

Ocean acidification (OA) is a facet of climate change driven by increasing carbon dioxide (CO2) concentrations in the atmosphere and ocean [1,2]. Recognition of the potential for OA to act as a biological stressor in the marine environment has only been widely recognised in the past 15 to 20 years. Research addressing its biological implications has expanded rapidly [2,3,4], suggesting the potential for wide-ranging effects on marine organisms and ecosystems. Findings have been highly variable with some species showing positive physiological responses while many others respond negatively; responses have been seen to vary between populations of individual species [4,5]. Despite ranges of expected impacts, current understandings suggest that negative responses from marine species are likely to be more widespread than neutral or positive responses [3,4].

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