Inorganic carbon acquisition in coastal Pacific phytoplankton communities

By P. Tortell, G. Rau, François M. M. Morel. 2000

203 citations recorded by the source corpus.

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In Oceanography

Citations in the corpus

Sources of inorganic carbon for phytoplankton in the eastern Subtropical and Equatorial Pacific Ocean (2002, methodology): “Among the diatom-dominated assemblages we have sampled for C uptake studies (Tortell et al. 1997, 2000; present study), we have observed significant differences in cellular C concentration factors, CA expression, and HCO uptake.23 Although much of this variability may reflect differences in species…”
Photoinhibition of photosynthesis is reduced by water flow in the reef-building coral Acropora digitifera (2005, background): “…insufficient to maintain photosynthesis under stress induced by high irradiance and high temperature (Weis et al. 1989), just as the photosynthetic-activity and carbon-uptake pathways are regulated by external carbon source (CO2 and HCO3–) concentrations for phytoplankton (Tortell et al. 2000).”
Climate change and control of the southeastern Bering Sea pelagic ecosystem (2002, background): “The interpretation of primary production rates from stable isotope ratios of carbon may be more complicated than previously recognized (Tortell et al., 2000; Gervais and Riebesell, 2001), and increases in water temperature or changes in the species composition of the phytoplankton may have…”
Acclimation to elevated carbon dioxide and ultraviolet radiation in the diatom Thalassiosira pseudonana: Effects on growth, photosynthesis, and spectral sensitivity of photoinhibition (2008, background): “However, the effect of elevated CO2 on growth and photosynthesis differs among studies, and more work is still needed to understand phytoplankton response to a rise in CO2 concentrations (Riebesell et al. 1993; Hein and Sand-Jensen 1997; Tortell et al. 2000).”
Effect of ocean acidification on microbial diversity and on microbe-driven biogeochemistry and ecosystem functioning (2010, background): “:P ratios at elevated 300 Liu et al.: Ocean acidification effects on microbes pCO2 (Burkhardt & Riebesell 1997, Burkhardt et al. 1999, Tortell et al. 2000).”
EFFECTS OF INCREASED TEMPERATURE AND CO2 ON PHOTOSYNTHESIS, GROWTH, AND ELEMENTAL RATIOS IN MARINE SYNECHOCOCCUS AND PROCHLOROCOCCUS (CYANOBACTERIA) 1 (2007, background): “Despite this, it is generally thought that phytoplankton will not show significant responses to rising atmospheric CO2, such as growth and photosynthetic rate increases (Goldman 1999, Raven and Falkowski 1999, Tortell et al. 2000, 2002).”
Responses of marine benthic microalgae to elevated CO2 (2011, unknown): “Our data contradict the results of some previous experiments on benthic and planktonic diatom species that suggest their responses to ocean pH changes will be negative (Torstensson et al. 2011) or small (Tortell et al. 1997, 2000; Burkhardt et al. 1999).”
Dynamics of silicon metabolism and silicon isotopic discrimination in a marine diatomas a function of pCO2 (2004, methodology): “Short-term (10 s) uptake rates were determined using a silicon oil centrifugation method (Badger et al. 1980; Tortell et al. 2000).”
Inorganic carbon uptake by Southern Ocean phytoplankton (2008, background): “…diffusive CO2 supply (Riebesell et al. 1993), but subsequent studies demonstrated the widespread occurrence of inorganic carbon-concentrating mechanisms (CCMs) in a variety of marine phytoplankton species and natural assemblages (Tortell et al. 2000; Giordano et al. 2005; Martin and Tortell 2006).”