Ocean acidification is considered detrimental to marine calcifiers, but mounting contradictory
evidence suggests a need to revisit this concept. This systematic review and meta‐analysis …

Elevations in atmospheric carbon dioxide (CO2) are anticipated to acidify oceans because
of fundamental changes in ocean chemistry created by CO2 absorption from the …

Over the next century, elevated quantities of atmospheric CO 2 are expected to penetrate
into the oceans, causing a reduction in pH (− 0.3/− 0.4 pH unit in the surface ocean) and in …

Global climate change has intensified the need to assess the capacity for natural
populations to adapt to abrupt shifts in the environment. Reductions in seawater pH …

For nearly a decade, the metazoan-focused research community has explored the impacts
of ocean acidification (OA) on marine animals, noting that changes in ocean chemistry can …

Ocean acidification is altering the oceanic carbonate saturation state and threatening the
survival of marine calcifying organisms. Production of their calcium carbonate exoskeletons …

Since the preindustrial era, the average surface ocean pH has declined by 0.1 pH units and
is predicted to decline by an additional 0.3 units by the year 2100. Although subtle, this …

Oceanic uptake of CO 2 from the atmosphere has significantly reduced surface seawater pH
and altered the carbonate chemistry within, leading to global Ocean Acidification (OA). The …

Heatwaves have become more frequent and intense in the last two decades, resulting in
detrimental effects on marine bivalves and ecosystems they sustain. Intertidal clams inhabit …

Ocean surface pH levels are predicted to fall by 0.3–0.4 pH units by the end of the century
and are likely to coincide with an increase in sea surface temperature of 2–4° C. The …