Bivalve shell formation in a naturally CO2-enriched habitat: Unraveling the resilience mechanisms from elemental signatures

Marine bivalves inhabiting naturally pCO(2)-enriched habitats can likely tolerate high levels of acidification. Consequently, elucidating the mechanisms behind such resilience can help to predict the fate of this economically and ecologically important group under near-future scenarios of CO2 -driven ocean acidification. Here, we assess the effects of four environmentally realistic pCO(2) levels (900, 1500, 2900 and 6600 mu atm) on the shell production rate of Mya arenaria juveniles originating from a periodically pCO(2) enriched habitat (Kiel Fjord, Western Baltic Sea). We find a significant decline in the rate of shell growth as pCO(2) increases, but also observe unchanged shell formation rates at moderate pCO(2) levels of 1500 and 2900 mu atm, the latter illustrating the capacity of the juveniles to partially mitigate the impact of high pCO(2). Using recently developed geochemical tracers we show that M. arenaria exposed to a natural pCO(2 )gradient from 900 to 2900 mu atm can likely concentrate HCO3- in the calcifying fluid through the exchange of HCO3-/Cl- and simultaneously maintain the pH homeostasis through active removal of protons, thereby being able to sustain the rate of shell formation to a certain extent. However, with increasing pCO(2) beyond natural maximum the bivalves may have limited capacity to compensate for changes in the calcifying fluid chemistry, showing significant shell growth reduction. Findings of the present study may pave the way for elucidating the underlying mechanisms by which marine bivalves acclimate and adapt to high seawater pCO(2). (C) 2018 Elsevier Ltd. All rights reserved.