Abstract

Ocean acidification, the ongoing decline of surface ocean pH and [COn}{}{}_{3}^{2-}] due to absorption of surplus atmospheric CO2, has far-reaching consequences for marine biota, especially calcifiers. Among these are teleost fishes, which internally calcify otoliths, critical elements of the inner ear and vestibular system. There is evidence in the literature that ocean acidification increases otolith size and alters shape, perhaps impacting otic mechanics and thus sensory perception. Here, larval Clark’s anemonefish, Amphiprion clarkii (Bennett, 1830), were reared in various seawater pCO2/pH treatments analogous to future ocean scenarios. At the onset of metamorphosis, all otoliths were removed from each individual fish and analyzed for treatment effects on morphometrics including area, perimeter, and circularity; scanning electron microscopy was used to screen for evidence of treatment effects on lateral development, surface roughness, and vaterite replacement. The results corroborate those of other experiments with other taxa that observed otolith growth with elevated pCO2, and provide evidence that lateral development and surface roughness increased as well. Both sagittae exhibited increasing area, perimeter, lateral development, and roughness; left lapilli exhibited increasing area and perimeter while right lapilli exhibited increasing lateral development and roughness; and left asterisci exhibited increasing perimeter, roughness, and ellipticity with increasing pCO2. Right lapilli and left asterisci were only impacted by the most extreme pCO2 treatment, suggesting they are resilient to any conditions short of aragonite undersaturation, while all other impacted otoliths responded to lower concentrations. Finally, fish settlement competency at 10 dph was dramatically reduced, and fish standard length marginally reduced with increasing pCO2. Increasing abnormality and asymmetry of otoliths may impact inner ear function by altering otolith-maculae interactions.

Highlights

  • Since the advent of the industrial revolution, humankind has inadvertently relocated a significant volume of carbon to the troposphere, where it resides as a greenhouse gas, warming the earth via radiative forcing (IPCC, 2013)

  • Scoring for the crystal habit and mineralogy metrics never deviated from the norm for any otolith type in any treatment

  • Whereas left sagittae responses were best represented as a linear model, right sagittae responses were best represented as a curvilinear model, with responses leveling out between the 1,600 μatm pCO2/pH 7.60 and 3,000 μatm pCO2/pH 7.30 treatments

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Summary

Introduction

Since the advent of the industrial revolution, humankind has inadvertently relocated a significant volume of carbon to the troposphere, where it resides as a greenhouse gas, warming the earth via radiative forcing (IPCC, 2013). Global warming is not the sole consequence of surplus atmospheric CO2: the surface ocean has absorbed approximately 30% of anthropogenic CO2 emissions (Mikaloff Fletcher et al, 2006; Le Quéré et al, 2010), contributing to ocean acidification (Caldeira & Wickett, 2003). While this absorption is an important sink, abating the greenhouse effect (IPCC, 2013), it has consequences for marine ecosystems. From population abundances to community shifts, ocean acidification has the potential to alter the ecological landscape of the ocean (Gaylord et al, 2015)

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