Rising atmospheric carbon dioxide (CO2), primarily from human fossil fuel combustion,
reduces ocean pH and causes wholesale shifts in seawater carbonate chemistry. The …

The evolution of organisms capable of oxygenic photosynthesis paralleled a long-term
reduction in atmospheric CO2 and the increase in O2. Consequently, the competition …

There is increasing concern that accelerating environmental change attributed to human-
induced warming of the planet may substantially alter the patterns, distribution and intensity …

Climate change pressures will influence marine planktonic systems globally, and it is
conceivable that harmful algal blooms may increase in frequency and severity. These …

The interactions among dissolved organic matter (DOM), microplastics (MPs) and microbes
influence the fate of aqueous carbon and greenhouse gas emissions. However, the related …

Global photosynthesis consumes ten times more CO2 than net anthropogenic emissions,
and microalgae account for nearly half of this consumption. The high efficiency of algal …

Ocean ecosystems have responded and will continue to respond to climate changes of
different rates, magnitudes, and durations (virtually certain). Human societies depend on …

In this study, Scenedesmus obliquus SJTU-3 and Chlorella pyrenoidosa SJTU-2 were
cultivated with 0.03%, 5%, 10%, 20%, 30%, 50% CO2. The two microalgae could grow at …

The accumulation of inorganic carbon from seawater by eukaryotic marine phytoplankton is
limited by the diffusion of carbon dioxide (CO2) in water and the dehydration kinetics of …

Ocean acidification (OA), a consequence of anthropogenic carbon dioxide emissions, poses
a serious threat to marine organisms in tropical, open-ocean, coastal, deep-sea, and high …