Shifting environmental conditions resulting from anthropogenic climate change have
recently garnered much attention in the aquaculture industry; however, ocean acidification …

The oceans are taking up over one million tons of fossil CO 2 per hour, resulting in
increased p CO 2 and declining pH, leading to ocean acidification (OA). At the same time …

Ocean acidification (OA) is generally assumed to negatively impact calcification rates of
marine organisms. At a local scale however, biological activity of macrophytes may generate …

The incidence and severity of extraordinary macroalgae blooms (green tides) are
increasing. Here, climate change (ocean warming and acidification) impacts on life history …

Under ocean acidification (OA), the 200% increase in CO 2 (aq) and the reduction of pH by
0.3–0.4 units are predicted to affect the carbon physiology and growth of macroalgae. Here …

Ocean acidification (OA) is the reduction in seawater pH due to the absorption of human-
released CO2 by the world's oceans. The average surface oceanic pH is predicted to …

The effects of global stressors on a species may be mediated by the stressors' impact on
coexisting taxa. For instance, herbivore–algae interactions may change due to alterations in …

Increased plant biomass is observed in terrestrial systems due to rising levels of
atmospheric CO2, but responses of marine macroalgae to CO2 enrichment are unclear. The …

Estuarine macroalgae are important primary producers in aquatic ecosystems, and often
foundation species providing structurally complex habitat. Climate change alters many …

In many temperate regions, brown macroalgae fulfil essential ecosystem services such as
the provision of structure, the fixation of nutrients and carbon, and the production of biomass …