Evolutionary and ecological perspectives on carbon acquisition in phytoplankton

By P. Tortell. 2000

230 citations recorded by the source corpus.

Subfields: Ecology, Oceanography, Renewable Energy, Sustainability and the Environment

View Paper: https://www.semanticscholar.org/paper/bb197f6f62cedecf59ec1fe1e42740f1f8fd958b

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Citations in the corpus

Response of photosynthesis to ocean acidification (2015, background): “Compared to other photoautotrophs, the form of rubisco found in diatoms has a relatively high specificity for CO2 vs. O2 (Badger et al., 1998; Tortell, 2000); nevertheless, the low equilibrium concentration and low diffusion coefficient for CO2 in water would limit photosynthesis without a CCM.…”
The effect of elevated CO2 on growth and competition in experimental phytoplankton communities (2011, background): “Species from a given major taxon (such as cyanobacteria or diatoms) have common physiological characteristics relating to CO2 uptake, including CCMs and the related CO2 compensation point, and differ consistently from species in other taxa (Birmingham & Colman, 1979; Tortell, 2000).”
Inorganic carbon acquisition in coastal Pacific phytoplankton communities (2000, background): “Significant taxonomic variability exists among phytoplankton in the kinetic properties of Rubisco and in the capacity of cells to accumulate internal inorganic C pools (Badger et al. 1998; Tortell 2000).”
Effects of increased atmospheric CO 2 on small and intermediate sized osmotrophs during a nutrient induced phytoplankton bloom (2007, background): “The experiment do, however, illustrate as10 previously suggested (Tortell, 2000), that the competitive balances between microbial taxa may be altered when atmospheric CO2 changes.”
Primary production during nutrient-induced blooms at elevated CO2 concentrations (2009, background): “While the affinity for CO2 differs among phytoplankton groups (Tortell, 2000), most species are able to regulate their carbon acquisition by CO2concentrating mechanisms (CCM) (Raven, 1991).”
How do marine diatoms fix 10 billion tonnes of inorganic carbon per year (2005, background): “However, data on marine diatoms cultured in air-equilibrium sea water often show intracellular inorganic carbon concentrations closer to the sea water values (Falkowski and Raven 1997; Badger and Spalding 2000; Tortell 2000).”
CO2 effects on taxonomic composition and nutrient utilization in an Equatorial Pacific phytoplankton assemblage (2002, background): “…can potentially limit the growth of large marine diatoms (Riebe- sell et al. 1993), while recent field studies have provided preliminary information on the CO2 sensitivity of oceanic primary production over various timescales (Chen & Durbin 1996, Hein & Sand-Jensen 1997, Tortell et al. 1997, 2000).”
Vulnerability of marine biodiversity to ocean acidification: A meta-analysis (2010, background): “A variety of phytoplankton taxa possess carbon concentrating mechanisms (Tortell, 2000), relaxing the dependence of calcification rates on water chemistry.”
The specialization continuum in pollination systems: diversity of concepts and implications for ecology, evolution and conservation (2017, background): “…it becomes important when one works with the biota of islands (e.g. Marten-Rodriguez et al. 2015) or extreme environments, such as the Arctic (e.g. Armbruster 2006), and becomes an explicit methodological issue in network studies (Bl€uthgen, Menzel & Bl€uthgen 2006; Pauw & Stanway 2015).”
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”
Rubisco specificity factor tends to be larger in plant species from drier habitats and in species with persistent leaves (2005, background): “…specificity factor has increased during evolution to compensate for the gradual atmospheric shift from high CO2 and low O2 to low CO2 and high O2 (Jordan & Ogren 1981; Tortell 2000) and, as a result, higher plants and diatoms display in general much higher values of t than cyanobacteria and algae.”
Carbon acquisition of bloom‐forming marine phytoplankton (2003, unknown): “As pointed out by Tortell (2000), the efficiency of the CCM of different taxonomic groups seems to be negatively correlated with the catalytic efficiency of their RubisCO.”
Differential effects of ocean acidification on growth and photosynthesis among phylotypes of Symbiodinium (Dinophyceae) (2011, background): “These groups appear to be physiologically distinct, especially with regard to their mode of inorganic carbon acquisition (Tortell 2000), perhaps explaining the wide variation in their sensitivity to OA.”
Carbon Acquisition Mechanisms of Algae: Carbon Dioxide Diffusion and Carbon Dioxide Concentrating Mechanisms (2003, background): “This topic has been considered by, inter alia, Raven (l997b,c), Badger et al. (1998) and Tortell (2000) ; see also Chen et al. (2000).”
Effect of CO2 concentration on the PIC/POC ratio in the coccolithophore Emiliania huxleyi grown under light-limiting conditions and different daylengths. (2002, background): “It has been reported that E. huxleyi has a low affinity for external CO2 (for review, see Raven and Johnston, 1991; Badger et al., 1998) and also has a low cellular carbon concentrating factor (Tortell, 2000).”