Abstract

Ocean acidification (OA) is one of the most significant threats to marine life, and is predicted to drive important changes in marine communities. Although OA impacts will be the sum of direct effects mediated by alterations of physiological rates and indirect effects mediated by shifts in species interactions and biogenic habitat provision, direct and indirect effects are rarely considered together for any given species. Here, we assess the potential direct and indirect effects of OA on a ubiquitous group of crustaceans: caprellid amphipods (Caprella laeviuscula and Caprella mutica). Direct physiological effects were assessed by measuring caprellid heart rate in response to acidification in the laboratory. Indirect effects were explored by quantifying caprellid habitat dependence on the hydroid Obelia dichotoma, which has been shown to be less abundant under experimental acidification. We found that OA resulted in elevated caprellid heart rates, suggestive of increased metabolic demand. We also found a strong, positive association between caprellid population size and the availability of OA-vulnerable O. dichotoma, suggesting that future losses of biogenic habitat may be an important indirect effect of OA on caprellids. For species such as caprellid amphipods, which have strong associations with biogenic habitat, a consideration of only direct or indirect effects could potentially misestimate the full impact of ocean acidification.

Highlights

  • Human activities are releasing substantial and increasing quantities of carbon dioxide into the atmosphere, and a sizeable fraction of these emissions are absorbed by the oceans (Sabine et al, 2004; Sabine & Tanhua, 2009)

  • Caprellids were most abundant on the hydroid O. dichotoma, while mussels (Mytilus trossulus) and tunicates (Botryllus schlosseri) hosted less than 5% of the individuals found in O. dichotoma

  • When we experimentally manipulated the amount of available O. dichotoma habitat, we found a positive relationship between O. dichotoma abundance and caprellid population size, supporting our hypothesis that caprellid population size is dependent on O. dichotoma abundance

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Summary

Introduction

Human activities are releasing substantial and increasing quantities of carbon dioxide into the atmosphere, and a sizeable fraction of these emissions are absorbed by the oceans (Sabine et al, 2004; Sabine & Tanhua, 2009). As anthropogenic CO2 dissolves in seawater, it alters carbonate chemistry and causes a decrease in pH (Feely et al, 2004; Quéré et al, 2009). This change in oceanic chemistry—termed ocean acidification (OA)—has resulted in a decrease of pH by 0.1 units since pre-industrial times, with further decreases of 0.3–0.5 units predicted within this century (Stocker et al, 2013).

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