Ocean acidification (OA) is one of the global issues caused by rising atmospheric CO 2. The
rising pCO 2 and resulting pH decrease has altered ocean carbonate chemistry. Microbes …

The ocean carbon cycle is tightly linked with the cycles of the major nutrient elements
nitrogen, phosphorus, and silicon. It is therefore likely that enrichment of the ocean with …

The ocean absorbs about 25% of anthropogenic CO 2 emissions, which alters its chemistry.
Among the changes of the carbonate system are an increase in the partial pressure of CO 2 …

Acidification of seawater caused by anthropogenic carbon dioxide (CO2) is anticipated to
influence the growth of dinitrogen (N2)–fixing phytoplankton, which contribute a large …

Ocean acidification (OA), caused by seawater CO2 uptake, has significant impacts on
marine calcifying organisms and phototrophs. However, the response of bacterial …

The predicted rise in anthropogenic CO 2 emissions will increase CO 2 concentrations and
decrease seawater pH in the upper ocean. Recent studies have revealed effects of pCO 2 …

Research into the effects of ocean acidification (OA) on marine organisms has greatly
increased during the past decade, as realization of the potential dramatic impacts has …

The uptake of anthropogenic CO2 by the ocean and the corresponding increase in surface
ocean CO2 concentrations have already caused a measurable decrease in seawater pH …

Marine bacteria are the main consumers of freshly produced organic matter. Many
enzymatic processes involved in the bacterial digestion of organic compounds were shown …

The effect of elevated seawater carbon dioxide (CO 2) on the activity of a natural
bacterioplankton community in an Arctic fjord system was investigated by a mesocosm …