Carbon acquisition of bloom‐forming marine phytoplankton
By B. Rost, U. Riebesell, S. Burkhardt, D. Sültemeyer. 2003
491 citations recorded by the source corpus.
Subfields: Oceanography
View Paper: https://www.semanticscholar.org/paper/df5da3f1a00ecbce083e251d63acda632ddc7a27
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In Oceanography
Citations in the corpus
- Reviews and Syntheses: Responses of coccolithophores to ocean acidification: a meta-analysis (2015, background): “…Gephyrocapsa oceanica – confirm the hypothesis that some coccolithophores might benefit from higher CO 2 concentrations, since their rate of carbon fixation is below CO 2 saturation at preindustrial CO 2 levels (Riebesell et al., 2000; Riebesell, 2004; Rost et al., 2003; Nimer and Merrett, 1996).”
- Physiological responses of the calcifying rhodophyte, Corallina officinalis (L.), to future CO2 levels (2012, methodology): “In parallel, we expected the carbonic anhydrase activity to be downregulated when more CO2 was available, which has been found in previous algal studies under elevated CO2 levels (Nelson et al. 1969; García-Sánchez et al. 1994; Rost et al. 2003).”
- Coccolithophores and the biological pump: responses to environmental changes (2004, methodology): “Owing to the operation of CCMs, most marine phytoplankton have high affinities for inorganic carbon and reach photosynthetic carbon saturation under ambient CO2 levels (Raven and Johnston 1991).”
- The effect of pCO2 on carbon acquisition and intracellular assimilation in four marine diatoms (2009, background): “Ecological implications and conclusions It has been proposed that the dominance of species during bloom situations may depend on their ability to operate an efficient and regulated CCM (Rost et al., 2003; Trimborn et al., 2008).”
- The effect of elevated CO2 on growth and competition in experimental phytoplankton communities (2011, background): “Much more extensive experiments to evaluate phytoplankton growth and competition under varying levels and combinations of global change factors (Rost et al., 2008) and experiments long enough to allow for evolutionary adaptation and its interaction with ecological responses (Collins & Bell, 2004;…”
- Primary production during nutrient-induced blooms at elevated CO2 concentrations (2009, background): “The affinity for CO 2 differs among phytoplankton species (Rost et al. 2003), and some phytoplankton species are able to change their CO 2 supply by CO 2 -concentrating mechanisms (CCM) (Raven, 1991).”
- Interactive effects of increased pCO2, temperature and irradiance on the marine coccolithophore Emiliania huxleyi (Prymnesiophyceae) (2008, background): “Compared with diatoms and Phaeocystis, E. huxleyi cells have low affinities for inorganic carbon, and their photosynthesis is carbon-limited at present-day oceanic CO2 levels (Rost et al., 2003; Riebesell, 2004).”
- Environmental controls on coccolithophore calcification (2012, methodology): “Data from the membrane inlet mass spectrometer method suggest uptake of both CO2 and HCO3− to supply photosynthesis in coccolithophores (Rost et al. 2003, 2007, Tchernov et al. 2003, Schulz et al. 2007), while isotope disequili - brium experiments suggest a predominant role for CO2 entry (Sikes et…”
- Harmful algal blooms and climate change: Learning from the past and present to forecast the future (2015, background): “CO2 enrichment is expected to relieve the energy requirements of carbon concentrating mechanisms (CCM) and particularly benefit those species having Form II Rubisco (ribulose-1,5-bis-phosphate carboxylase-oxygenase), which has a low affinity for CO2 (Beardall et al., 2009; Giordano et al., 2005; Rav”
- Increased carbon dioxide availability alters phytoplankton stoichiometry and affects carbon cycling and growth of a marine planktonic herbivore (2012, background): “Higher availability of carbon and the subsequent changes in seawater nutrient composition, caused by the relatively lower availability of mineral nutrients compared to C, may also cause shifts in competitive interactions between algae (e.g. Kuffner et al. 2007; Rost et al. 2003; Swanson and Fox 2007”
- Response of coccolithophorid Emiliania huxleyi to elevated partial pressure of CO2 under nitrogen limitation (2003, background): “…for a protein associated with an active transport of CO2 and HCO3– across the plasmalemma, external and internal carbonate anhydrase (CA) activities, generally associated with the CCM, have been detected in various strains of E. huxleyi (Nimer et al. 1994b, Elzenga et al. 2000, Rost et al. 2003).”
- Effects of CO2 and their modulation by light in the life‐cycle stages of the coccolithophore Emiliania huxleyi (2012, background): “Decreased Ci affinities in response to elevated PCO2 have been reported for diploid E. huxleyi (strain PLYB92/11; Rost et al. 2003), a number of diatoms (Trimborn et al. 2008), and also cyanobacteria (Sültemeyer et al. 1998).”
- Ocean Acidification and Its Potential Effects on Marine Ecosystems (2008, background): “…rates when grown under high pCO2 conditions equivalent to ca. 760 micro atmosphere (µatm) (Tortell et al. 1997; Hein & Sand-Jensen 1997; Burkhardt et al. 2001; Tortell and Morel 2002; Rost et al. 2003; Beardall & Raven 2004; Schippers et al. 2004; Giordano et al. 2005; Martin & Tortell 2006).”