Climate change is likely to stimulate the development of harmful cyanobacterial blooms in
eutrophic waters, with negative consequences for water quality of many lakes, reservoirs …

The prokaryotic and eukaryotic microorganisms that drive the pelagic ocean's
biogeochemical cycles are currently facing an unprecedented set of comprehensive …

The availability of carbon from rising atmospheric carbon dioxide levels and of nitrogen from
various human-induced inputs to ecosystems is continuously increasing; however, these …

Over the coming century humanity may need to find reservoirs to store several trillions of
tons of carbon dioxide (CO2) emitted from fossil fuel combustion, which would otherwise …

Cyanobacteria are the most ancient phytoplankton on the planet and form harmful algal
blooms in freshwater, estuarine, and marine ecosystems. Recent research suggests that …

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

The oceans take up over 1 million tons of anthropogenic CO2 per hour, increasing dissolved
p CO2 and decreasing seawater pH in a process called ocean acidification (OA). At the …

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

Prediction of the impact of global climate change on marine HABs is fraught with difficulties.
However, we can learn important lessons from the fossil record of dinoflagellate cysts; long …

Nitrogen is a requisite and highly demanded element for living organisms on Earth.
However, increasing human activities have greatly altered the global nitrogen cycle …