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Dryad

Data from: Brood chamber carbonate chemistry is dynamically shaped by warming, acidification, and maternal ventilation in the brooding oyster Ostrea edulis

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Jul 29, 2026 version files 38.64 MB

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Abstract

Brooding organisms can modify the chemical environment experienced by developing offspring, potentially altering their exposure to climate change. In marine systems, however, the carbonate chemistry of brood chambers, and the mechanisms governing it, remain poorly resolved. Here, we combine high- resolution measurements of brood chamber pH, CO2, and valve gape in the European flat oyster (Ostrea edulis) to quantify how warming, ocean acidification, and maternal ventilation interact to shape the internal environment experienced by brooded larvae. Brood chamber pH was consistently lower than that of the surrounding seawater and responded to external conditions in a state- dependent manner governed by maternal ventilation and respiration. When oysters were actively ventilating, brood chamber chemistry tracked ambient seawater with a persistent offset, whereas valve closure led to rapid CO2 accumulation and pronounced declines in pH. These dynamics generated highly variable and behaviorally mediated exposure regimes, in which metabolic processes distorted ambient chemical signals over short timescales. Paired pH and CO2 measurements provided preliminary constraints on aragonite saturation state (Ωₐᵣ), revealing that undersaturated conditions (Ωₐᵣ < 1) can occur within brood chambers even when overlying seawater remains favorable. Together, these results demonstrate that brood chambers function as dynamic microenvironments in which larval exposure to ocean acidification is governed not only by external conditions, but also by maternal behavior. Because warming enhances metabolic CO2 production and intensifies acidification within the chamber, future climate change is likely to amplify both the magnitude and variability of larval exposure. These findings help explain the apparent resilience of brooding species to ocean acidification, while also highlighting potential limits as environmental conditions move beyond historical bounds.