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Seawater carbonate chemistry and calcification of the crustose coralline alga...
Anthropogenic CO2 emissions have exacerbated two environmental stressors, global climate warming and ocean acidification (OA), that have serious implications for marine... -
Ocean acidification slows nitrogen fixation and growth in the dominant diazot...
Dissolution of anthropogenic CO(2) increases the partial pressure of CO(2) (pCO(2)) and decreases the pH of seawater. The rate of Fe uptake by the dominant N(2)-fixing... -
Seawater carbonate chemistry and protein content, respiration, symbiodinium d...
Efforts to evaluate the response of coral larvae to global climate change (GCC) and ocean acidification (OA) typically employ short experiments of fixed length, yet it is... -
Interactive effects of ocean acidification and nitrogen limitation on the dia...
Climate change is expected to bring about alterations in the marine physical and chemical environment that will induce changes in the concentration of dissolved CO2 and in... -
Growth, respiration and photophysiology of coral massive Porites spp. in the ...
I tested the hypothesis that high pCO2 (76.6 Pa and 87.2 Pa vs. 42.9 Pa) has no effect on the metabolism of juvenile massive Porites spp. after 11 days at 28 °C and 545 µmol... -
Calcification rate of massive Porites spp. and Porites rus in the experiment ...
This study tested the hypothesis that the response of corals to temperature and pCO2 is consistent between taxa. Juvenile massive Porites spp. and branches of P. rus from the... -
Seawater carbonate chemistry and plankton community structure during a winter...
Plankton communities play a key role in the marine food web and are expected to be highly sensitive to ongoing environmental change. Oceanic uptake of anthropogenic carbon...