Genetic material (short DNA fragments) left behind by species in nonliving components of
the environment (eg soil, sediment, or water) is defined as environmental DNA (eDNA). This …

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 …

While the isolated responses of marine phytoplankton to climate warming and to ocean
acidification have been studied intensively, studies on the combined effect of both aspects of …

The Arctic Ocean has been experiencing rapid warming, which accelerates sea ice melt.
Further, the increasing area and duration of sea ice-free conditions enhance ocean uptake …

Diatoms account for up to 50% of marine primary production and are considered to be key
players in the biological carbon pump. Ocean acidification (OA) is expected to affect diatoms …

Dissolution of anthropogenic CO2 into the oceans results in ocean acidification (OA),
altering marine chemistry with consequences for primary, secondary, and tertiary food web …

Primary production in the Southern Ocean is dominated by diatom‐rich phytoplankton
assemblages, whose individual physiological characteristics and community composition …

Diatoms are so important in ocean food-webs that any human induced changes in their
abundance could have major effects on the ecology of our seas. The large chain-forming …

The impact of environmental change and anthropogenic stressors on coastal marine
systems will strongly depend on changes in the magnitude and composition of organic …

Ocean alkalinity enhancement (OAE) is currently discussed as a potential negative emission
technology to sequester atmospheric carbon dioxide in seawater. Yet, its potential risks or …