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Seawater carbonate chemistry and growth and photosynthetic oxygen rate and re...
Red tide and green tide are two common algal blooms that frequently occur in many areas in the global oceans. The algae causing red tide and green tide often interact with each... -
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 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 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 photosynthetic pigments and photophysiology ...
Ocean acidification, due to increased levels of anthropogenic carbon dioxide, is known to affect the physiology and growth of marine phytoplankton, especially in polar regions.... -
Seawater carbonate chemistry and growth rates, physiology, and geneexpression...
Heterosigma akashiwo is a raphidophyte known for forming ichthyotoxic blooms. In order to predict the potential impacts of rising CO2 on H. akashiwo it is necessary to... -
Seawater carbonate chemistry and photosynthesis and dark respiration of Thala...
Increasing atmospheric pCO2 leads to seawater acidification, which has attracted considerable attention due to its potential impact on the marine biological carbon pump and... -
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... -
Seawater carbonate chemistry and photosynthetic performance of Thalassiosira ...
The purpose of this study was to investigate the effects of ocean acidification and nutrient level on the growth and photosynthetic performance of the diatom Thalassiosira... -
Seawater carbonate chemistry and growth, nitrogen availability, photosynthesi...
In order to allow full comparability with other ocean acidification data sets, the R package seacarb (Gattuso et al, 2016) was used to compute a complete and consistent set of... -
H+-driven increase in CO2 uptake and decrease in HCO3- uptake explain coccoli...
Recent ocean acidification (OA) studies revealed that seawater [H+] rather than [CO2] or [ inline image] regulate short-term responses in carbon fluxes of Emiliania huxleyi.... -
Interactive effects of ocean acidification and nitrogen limitation on two blo...
Global climate change involves an increase in oceanic CO2 concentrations as well as thermal stratification of the water column, thereby reducing nutrient supply from deep to... -
Ocean acidification as one of multiple stressors: growth response of Thalassi...
Shifts in phytoplankton composition and productivity are anticipated in the future, because phytoplankton are frequently bottom-up controlled, and environmental conditions, like... -
Decreased photosynthesis and growth with reduced respiration in the model dia...
Studies on the long-term responses of marine phytoplankton to ongoing ocean acidification (OA) are appearing rapidly in the literature. However, only a few of these have... -
Environmental stability affects phenotypic evolution in a globally distribute...
Marine phytoplankton can evolve rapidly when confronted with aspects of climate change because of their large population sizes and fast generation times. Despite this, the... -
Combined effects of ocean acidification and light or nitrogen availabilities ...
Along with increasing oceanic CO2 concentrations, enhanced stratification constrains phytoplankton to shallower upper mixed layers with altered light regimes and nutrient... -
Effects of high CO2 levels on the ecophysiology of the diatom Thalassiosira w...
Iron availability in seawater, namely the concentration of dissolved inorganic iron ([Fe']), is affected by changes in pH. Such changes in the availability of iron should be... -
The impact of fluctuating light on the dinoflagellate Prorocentrum micans dep...
Increasing atmospheric pCO2 and its dissolution into oceans leads to ocean acidification and warming, which reduces the thickness of upper mixing layer (UML) and upward nutrient... -
Alleviation of solar ultraviolet radiation (UVR)-induced photoinhibition in d...
The study aimed to unravel the interaction between ocean acidification and solar ultraviolet radiation (UVR) in Chaetoceros curvisetus. Chaetoceros curvisetus cells were...