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Seawater carbonate chemistry and biogenic dimethylated sulfur compounds cycling
Ocean acidification (OA) affects marine primary productivity and community structure. Therefore, OA may influence the biogeochemical cycles of volatile biogenic dimethyl sulfide... -
Seawater carbonate chemistry and growth, production rates, and elemental quot...
The potential for adaptation of phytoplankton to future climate is often extrapolated based on single strain responses of a representative species, ignoring variability within... -
Seawater carbonate chemistry and physiology and toxicity of dinoflagellate Ka...
A batch culture experiment was conducted to study the interactive effects of ocean acidification (OA) and solar ultraviolet radiation (UVR, 280–400 nm) on the harmful... -
Seawater carbonate chemistry and calcification of an estuarine coccolithophore
Ocean acidification has the capacity to impact future coccolithophore growth, photosynthesis, and calcification, but experimental culture work with coccolithophores has produced... -
Seawater carbonate chemistry and growth, net photosynthesis rate, Chlorophyll...
Increasing CO2 levels in the surface water of oceans are expected to decrease oceanic pH and lead to seawater acidification. The responses of macroalgaea to this acidification... -
Seawater carbonate chemistry and growth and particulate organic nitrogen prod...
Phytoplankton in the upper oceans are exposed to changing light levels due to mixing, diurnal solar cycles and weather conditions. Consequently, effects of ocean acidification... -
Seawater carbonate chemistry and photosynthesis and photochemical efficiency ...
Ocean acidification (OA) is predicted to enhance photosynthesis in many marine taxa. However, photophysiology has multiple components that OA may affect differently, especially... -
Seawater carbonate chemistry and physiology and functional gene expression of...
Here, we examined two-way and multiple driver effects of ocean acidification and other key environmental drivers - nitrate, phosphate, irradiance, and temperature - on the... -
Seawater carbonate chemistry and particulate inorganic carbon, particulate or...
Coccolithophores are unicellular marine phytoplankton and important contributors to global carbon cycling. Most work on coccolithophore sensitivity to climate change has been on... -
Seawater carbonate chemistry and calcification rate, calcifying fluid pH, cal...
Natural variability in pH in the diffusive boundary layer (DBL), the discrete layer of seawater between bulk seawater and the outer surface of organisms, could be an important... -
Seawater carbonate chemistry and photo-physiological fitness, growth and carb...
Ecophysiological studies on Antarctic cryptophytes to assess whether climatic changes such as ocean acidification and enhanced stratification affect their growth in Antarctic... -
Seawater carbonate chemistry and biochemical composition of the coccolithopho...
Owing to the hierarchical organization of biology, from genomes over transcriptomes and proteomes down to metabolomes, there is continuous debate about the extent to which data... -
Seawater carbonate chemistry and coral calcification
Coral reefs are constructed by calcifiers that precipitate calcium carbonate to build their shells or skeletons through the process of calcification. Accurately assessing coral... -
Seawater carbonate chemistry and growth rate, photosynthetic carbon fixation ...
Marine phytoplankton such as bloom-forming, calcite-producing coccolithophores, are naturally exposed to solar ultraviolet radiation (UVR, 280–400 nm) in the ocean's upper mixed... -
Seawater carbonate chemistry and growth and chlorophyll, photochemical parame...
Elevated CO2 is leading to a decrease in pH in marine environments (ocean acidification [OA]), altering marine carbonate chemistry. OA can influence the metabolism of many... -
Seawater carbonate chemistry and particulate organic carbon accumulation of t...
Impacts of rising atmospheric CO2 concentrations and increased daily irradiances from enhanced surface water stratification on phytoplankton physiology in the coastal Southern... -
Seawater carbonate chemistry and tissue biomass composition, calcification of...
Ocean acidification (OA) is predicted to reduce reef coral calcification rates and threaten the long-term growth of coral reefs under climate change. Reduced coral growth at... -
Seawater carbonate chemistry and photosynthesis of seagrass Zostera japonica ...
Photosynthesis and respiration are vital biological processes that shape the diurnal variability of carbonate chemistry in nearshore waters, presumably ameliorating (daytime) or... -
Seawater carbonate chemistry and growth response in a diatom dominated phytop...
The ongoing increase in surface seawater CO2 level could potentially impact phytoplankton primary production in coastal waters; however, CO2 sensitivity studies on tropical... -
Seawater carbonate chemistry and photophysiology and hemolytic activity of th...
Due to global climate change, marine phytoplankton will likely experience low pH (ocean acidification), high temperatures and high irradiance in the future. Here, this work...