Oceanic uptake of anthropogenic carbon dioxide (CO2) causes pronounced shifts in marine
carbonate chemistry and a decrease in seawater pH. Increasing evidence indicates that …

In situ mesocosm experiments on the effect of ocean acidification (OA) are an important tool
for investigating potential OA-induced changes in natural plankton communities. In this study …

Anthropogenic carbon dioxide (CO 2) emissions are reducing the pH in the world's oceans.
The plankton community is a key component driving biogeochemical fluxes, and the effect of …

The Baltic Sea is a unique environment as the largest body of brackish water in the world.
Acidification of the surface oceans due to absorption of anthropogenic CO 2 emissions is an …

Community approaches to investigating ocean acidification (OA) effects suggest a high
tolerance of micro-and mesozooplankton to carbonate chemistry changes expected to occur …

Threatened by climate change and ocean warming, coral reef ecosystems have been
shifting in geographic ranges toward a higher latitude area. The water-associated microbial …

Oligotrophic waters (OW), generally favour longer food chain facilitated by the microbial
loop. In such ecosystems, physical mixing (eg upwelling, and winter convection) inject …

Taucher et al. Plankton Responses to Upwelling and CO2 of each mesocosm's volume with
deep water and successfully simulated a deep water upwelling event that induced a …