Abstract

Seawater changing chemistry has consequences on coastal ecosystems and their living resources. Future projections suggest the pH could drop ~0.2-0.3 pH units by the year 2100 under a business-as-usual (BAU) CO2 emission scenario. Marine calcifying organisms such as corals, calcifying algae, crustaceans, mussels, oysters and clams are most likely to be impacted by ocean acidification. The Isognomon alatus (flat tree oyster) is an important species that can be negatively affected by the lowering of seawater pH. Isognomon alatus is an important food source, a substrate for other benthic organisms (e.g., stone crab, Menippe mercenaria) and contribute to nutrients recycling in coastal ecosystems. The study was conducted to test the impacts acidified seawater CO2 on the growth of I. alatus under controlled laboratory conditions as well as field experiment. The Isognomon alatus lost weight and experienced negative growth rates of –0.56 ± 0.36 mg g-1day-1 under average pH values of 7.8 expected by the end of this century compared to a loss of –0.26 ± 0.23 mg g-1day-1 under ambient pH (value 8.1) conditions. In contrast, I. alatus incubated in a field experiment showed a gain in weight and positive growth of 3.30 ± 0.23 mg g-1day-1 despite exposure to pH levels (~7.4) during low tide significantly lower than those experienced in the laboratory. Overall, the results showed concern on the impacts of acidification flat tree oyster (Bivalvia:Isognomonidae). A decline of calcifying bivalves populations can impact coastal ecosystems function and indirectly affect the human beings that depend on them as a food source.    Key words: Ocean acidification, climate change, Isognomonidae, shell dissolution, bivalve's growth, estuarine.

Highlights

  • Anthropogenic carbon dioxide (CO2) emission and the effect of its accumulation in the atmosphere and uptake by the oceans have raised severe concerns for its consequences to Earth's climate and oceanic ecosystems (IPCC, 2007; Andersson et al, 2008; Cole, 2013; IPCC, 2013; Bates et al, 2014)

  • The average temperature progressively increased in the experimental tanks throughout the duration of the study, with occasional drops in temperature associated with cold fronts moving over Bermuda

  • From 11 to 18th March 2009, average salinity was slightly higher in acidification tanks than in control tanks due to reduced seawater flow rate and a higher evaporation rate because Tygon tubes that supplied seawater were partially blocked with organic particles

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Summary

Introduction

Anthropogenic carbon dioxide (CO2) emission and the effect of its accumulation in the atmosphere and uptake by the oceans have raised severe concerns for its consequences to Earth's climate and oceanic ecosystems (IPCC, 2007; Andersson et al, 2008; Cole, 2013; IPCC, 2013; Bates et al, 2014).

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