Before the industrial revolution, the atmospheric CO 2 concentration was 180–330 ppm;
however, fossil-fuel combustion and forest destruction have led to increased atmospheric …

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 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 …

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

Since industrialization global CO2 emissions have increased, and as a consequence
oceanic pH is predicted to drop by 0.3–0.4 units before the end of the century–a process …

Abstract Using the Mediterranean coral Balanophyllia europaea naturally growing along a
pH gradient close to Panarea island (Italy) as a model, we explored the role of host …

Ocean acidification alters seawater carbonate chemistry, which can have detrimental
impacts for calcifying organisms such as bivalves. This study investigated the physiological …

We examined the synergistic effects of CO 2 injection on electro-chlorination in disinfection
of plankton and bacteria in simulated ballast water. Chlorination was performed at dosages …

Experimental results related to the effects of ocean acidification on planktonic marine
microbes are still rather inconsistent and occasionally contradictory. Moreover, laboratory or …

In contrast to clear stimulatory effects of rising temperature, recent studies of the effects of
CO2 on planktonic bacteria have reported conflicting results. To better understand the …