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An increase in anthropogenic carbon dioxide is driving oceanic chemical shifts resulting in a long-term global decrease in ocean pH, colloquially termed ocean acidification (OA). Previous studies have demonstrated that OA can have negative physiological consequences for calcifying organisms, especially during early life-history stages. However, much of the previous research has focused on static exposure to future OA conditions, rather than variable exposure to elevatedpCO₂, which is more ecologically relevant for nearshore species. This study examines the effects of OA on embryonic and larval Pacific razor clams (Siliqua patula), a bivalve that produces a concretion during early shell development. Larvae were spawned and cultured over 28 days under threepCO₂treatments: a static highpCO₂of 867 μatm, a variable, dielpCO₂of 357 to 867 μatm, and an ambientpCO₂of 357 μatm. Our results indicate that the calcium carbonate polymorphism of the concretion phase ofS. patulawas amorphous calcium carbonate which transitioned to vaterite during the advanced D-veliger stage, with a final polymorphic shift to aragonite in adults, suggesting an increased vulnerability to dissolution under OA. However, exposure to elevatedpCO₂appeared to accelerate the transition of larvalS. patulafrom the concretion stage of shell development to complete calcification. There was no significant impact of OA exposure to elevated or variablepCO₂conditions onS. patulagrowth or HSP70 and calmodulin gene expression. This is the first experimental study examining the response of a concretion producing bivalve to future predicted OA conditions and has important implications for experimentation on larval mollusks and bivalve management.