Abstract

Sites with naturally high CO2 conditions provide unique opportunities to forecast the vulnerability of coastal ecosystems to ocean acidification, by studying the biological responses and potential adaptations to this increased environmental variability. In this study, we investigated the bivalve Ervilia castanea in coastal sandy sediments at reference sites and at volcanic CO2 seeps off the Azores, where the pH of bottom waters ranged from average oceanic levels of 8.2, along gradients, down to 6.81, in carbonated seawater at the seeps. The bivalve population structure changed markedly at the seeps. Large individuals became less abundant as seawater CO2 levels rose and were completely absent from the most acidified sites. In contrast, small bivalves were most abundant at the CO2 seeps. We propose that larvae can settle and initially live in high abundances under elevated CO2 levels, but that high rates of post-settlement dispersal and/or mortality occur. Ervilia castanea were susceptible to elevated CO2 levels and these effects were consistently associated with lower food supplies. This raises concerns about the effects of ocean acidification on the brood stock of this species and other bivalve molluscs with similar life history traits.

Highlights

  • Increasing atmospheric CO2 concentrations have caused the pH of the surface ocean to fall by 0.1 units since the pre-industrial age (Bindoff et al, 2019; Dupont and Pörtner, 2013; Feely et al, 2009; Keeling et al, 2017) and further decreases, between 0.1 (RCP2.6) or 0.3 (RCP8.5) pH units, are expected by 2100 (Bindoff et al, 2019)

  • One of the advantages of conducting ocean acidification research using natural CO2 gradients is that the responses observed are not restricted to the direct effect of carbonate chemistry, and include the indirect consequences of trophic interactions and changes in habitat complexity (Fabricius et al, 2015; Hale et al, 2011; Range et al, 2012)

  • Transplant experiments including measurements of mineralization and dissolution of the shell, physiological, metabolic and genetic endpoints could enlighten and complement the responses observed in this study

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Summary

Introduction

Increasing atmospheric CO2 concentrations have caused the pH of the surface ocean to fall by 0.1 units since the pre-industrial age (Bindoff et al, 2019; Dupont and Pörtner, 2013; Feely et al, 2009; Keeling et al, 2017) and further decreases, between 0.1 (RCP2.6) or 0.3 (RCP8.5) pH units, are expected by 2100 (Bindoff et al, 2019). Care is needed to assess potential anomalies in temperature, alkalinity, metals and H2S which are frequently found at these volcanic sites and can influence biological responses, but are not associated with ocean acidification (Vizzini et al, 2013; Mishra et al, 2020) This type of in situ approach has shown that ocean acidification can lead to ecosystem simplification and reorganization of marine communities (Fabricius et al, 2015; Kroeker et al, 2013a, 2011; Agostini et al, 2018). Communities tend to change from being dominated by calcareous organisms to non-calcareous ones (Baggini et al, 2014; Christen et al, 2013; Hall-Spencer et al, 2008), granting the latter a perceived advantage in a future acidified ocean (Kroeker et al, 2013b; Vihtakari et al, 2013)

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