Abstract

Early evidence suggests that DNA methylation can mediate phenotypic responses of marine calcifying species to ocean acidification (OA). Few studies, however, have explicitly studied DNA methylation in calcifying tissues through time. Here, we examined the phenotypic and molecular responses in the extrapallial fluid and mantle (fluid and tissue at the calcification site) in the Eastern oyster (Crassostrea virginica) exposed to experimental OA over 80 days. Oysters were reared under three experimental pCO2 treatments (‘control’, 580 μatm; ‘moderate OA’, 1000 uatm; ‘high OA’, 2800 μatm) and sampled at 6 time points (24 hours - 80 days). We found that high OA initially induced changes in the pH of the extrapallial fluid (pHEPF) relative to the external seawater, but the magnitude of this difference was highest at 9 days and diminished over time. Calcification rates were significantly lower in the high OA treatment compared to the other treatments. To explore how oysters regulate their extrapallial fluid, gene expression and DNA methylation were examined in the mantle-edge tissue of oysters from day 9 and 80 in the control and high OA treatments. Mantle tissue mounted a significant global molecular response (both in the transcriptome and methylome) to OA that shifted through time. Although we did not find individual genes that were significantly differentially expressed to OA, the pHEPF was correlated with the eigengene expression of several co-expressed gene clusters. A small number of OA-induced differentially methylated loci were discovered, which corresponded with a weak association between OA-induced changes in genome-wide gene body DNA methylation and gene expression. Gene body methylation, however, was not significantly correlated with the eigengene expression of pHEPF correlated gene clusters. These results suggest that in C. virginica, OA induces a subtle response in a large number of genes, but also indicates that plasticity at the molecular level may be limited. Our study highlights the need to re-assess the plasticity of tissue-specific molecular responses in marine calcifiers, as well as the role of DNA methylation and gene expression in mediating physiological and biomineralization responses to OA.

Highlights

  • Ocean acidification (OA), a decrease in seawater pH due to the uptake of anthropogenic CO2, is expected to have substantial effects on marine species and ecosystems in the near future (Orr et al, 2005; Guinotte and Fabry, 2008; Doney et al, 2009)

  • We tested the hypothesis that C. virginica pH of the extrapallial fluid (pHEPF) was associated with ocean acidification (OA) using a linear model that included both fixed effects, their interaction, and the random effect of tank nested within block

  • One-tailed t-tests showed that pH of oysters in all treatments was significantly lower than 0 at almost all time points of the experiment (Figure 1B, “Env”), indicating a strong tendency for oysters to maintain a more acidic EPF fluid relative to their environment

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Summary

Introduction

Ocean acidification (OA), a decrease in seawater pH due to the uptake of anthropogenic CO2, is expected to have substantial effects on marine species and ecosystems in the near future (Orr et al, 2005; Guinotte and Fabry, 2008; Doney et al, 2009). OA is driving a shift in the carbonate system equilibrium, resulting in decreased availability of carbonate ions and lower calcium carbonate saturation state (Feely et al, 2004; Orr et al, 2005). This may be problematic for marine calcifying species, which build their shells and skeletons from calcium and carbonate ions. Prolonged exposure to OA tends to have negative effects on calcification, metabolism, and growth, as observed in corals (e.g., Anthony et al, 2008), pteropods (e.g., Bednaršek et al, 2012), gastropods (e.g., Melatunan et al, 2013), and bivalves (e.g., Talmage and Gobler, 2010).

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