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Seawater carbonate chemistry and bioerosion of croal reef
Ocean acidification (OA), the gradual decline in ocean pH and [CO3 ] 2- caused by rising levels of atmospheric CO2, poses a significant threat to coral reef ecosystems,... -
Seawater carbonate chemistry and foraminiferal calcification
The response of the marine carbon cycle to changes in atmospheric CO2 concentrations will be determined, in part, by the relative response of calcifying and non-calcifying... -
Seawater carbonate chemistry and calcification and survival of the pteropod L...
The pteropod Limacina helicina frequently experiences seasonal exposure to corrosive conditions (Omega arag < 1) along the US West Coast and is recognized as one of the... -
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 population structure of Ervilia castanea (Mo...
Sites with naturally high CO2 conditions provide unique opportunities to forecast the vulnerability of coastal ecosystems to ocean acidification, by studying the biological... -
Seawater carbonate chemistry and net community calcification, production and ...
Previous studies have found that calcification in coral reefs is generally stronger during the day, whereas dissolution is prevalent at night. On the basis of these contrasting... -
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 growth rate, particulate organic (POC) and i...
Continuous accumulation of fossil CO2 in the atmosphere and increasingly dissolved CO2 in seawater leads to ocean acidification (OA), which is known to affect phytoplankton... -
Seawater carbonate chemistry and physiology and extrapallial fluid pH, calcif...
Increasing anthropogenic carbon dioxide is predicted to cause declines in ocean pH and calcium carbonate saturation state over the coming centuries, making it potentially harder... -
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 mortality, larval development, larval growth...
Ocean acidification and warming (OA-W) result mainly from the absorption of carbon dioxide and heat by the oceans, altering its physical and chemical properties and affecting... -
Seawater carbonate chemistry and calcification rate of 10 investigated specie...
The response of marine-calcifying organisms to ocean acidification (OA) is highly variable, although the mechanisms behind this variability are not well understood. Here, we use... -
Seawater carbonate chemistry and coral calcification rates
Estimates of heritability inform evolutionary potential and the likely outcome of many management actions, but such estimates remain scarce for marine organisms. Here, we report... -
Seawater carbonate chemistry and mussel respiration and calcification rates
Marine habitat‐forming species often play critical roles on rocky shores by ameliorating stressful conditions for associated organisms. Such ecosystem engineers provide... -
Seawater carbonate chemistry and resistance of corals and coralline algae to ...
Ocean acidification is a threat to the continued accretion of coral reefs, though some undergo daily fluctuations in pH exceeding declines predicted by 2100. We test whether... -
Seawater carbonate chemistry and calcification of Halimeda cuneata, photosynt...
The ultimate effect that ocean acidification (OA) and warming will have on the physiology of calcifying algae is still largely uncertain. Responses depend on the complex... -
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 calcification conditions and calcification r...
Ocean acidification is expected to negatively impact calcifying organisms, yet we lack understanding of their acclimation potential in the natural environment. Here we measured... -
Seawater carbonate chemistry and survival, calcification rate of 4 species of...
We conducted a 93-day experiment investigating the independent and combined effects of acidification (280−3300 µatm pCO2) and warming (28°C and 31°C) on calcification and linear...