Interactive effects of increased pCO2, temperature and irradiance on the marine coccolithophore Emiliania huxleyi (Prymnesiophyceae)
By Yuanyuan Feng, Mark E. Warner, Yaohong Zhang, Jun Sun, Feixue Fu, J. Rose, D. Hutchins. 2008
305 citations recorded by the source corpus.
Subfields: Ecology, Oceanography
View Paper: https://www.semanticscholar.org/paper/593f5c12218cb5973673c6ee2455dd494baabe66
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In Ecology
- D. Hutchins
- Feixue Fu
- Philip W. Boyd
- N. Garcia
- M. Mulholland
- Mark E. Warner
- U. Riebesell
- Yuanyuan Feng
In Oceanography
Citations in the corpus
- Reviews and Syntheses: Responses of coccolithophores to ocean acidification: a meta-analysis (2015, background): “…decreasing with increased pCO2 (Bach et al., 2011; Barcelos e Ramos et al., 2010; De Bodt et al., 2010; Delille et al., 2005; Engel et al., 2005; Feng et al., 2008; Gao et al., 2009; Hoppe et al., 2011; Langer et al., 2009; Müller et al., 2010; Riebesell et al., 2000; Rokitta and Rost et al.,…”
- The C:N:P stoichiometry of organisms and ecosystems in a changing world: A review and perspectives (2012, background): “This stratification impedes the vertical mixing of the water column and reduces the availability of N and P in superficial waters (Beardall and Raven, 2004; Tortell et al., 2008; Feng et al., 2008).”
- Effects of changing pCO2 and phosphate availability on domoic acid production and physiology of the marine harmful bloom diatom Pseudo‐nitzschia multiseries (2011, methodology): “…between changing pCO2 and various permutations of nutrients, iron, light, and temperature on the physiologies of coccolithophorids such as Emiliania huxleyi (Feng et al. 2008) and the cyanobacteria Trichodesmium (Hutchins et al. 2007), Crocosphaera, and Synechococcus (Fu et al. 2007, 2008a).”
- Environmental control of open‐ocean phytoplankton groups: Now and in the future (2010, methodology): “C fixation by this group appears to be under-saturated at present-day pCO2 (Rost et al. 2003; Feng et al. 2008, 2009), so coccolithophores may be truly C-limited in today’s ocean.”
- Effects of CO2 and their modulation by light in the life‐cycle stages of the coccolithophore Emiliania huxleyi (2012, background): “huxleyi morphospecies complex (Riebesell et al. 2000; Langer et al. 2009; Feng et al. 2008) and has often been used to demonstrate the exceptionally high sensitivity of coccolithophores to OA.”
- Phytoplankton in a changing world: cell size and elemental stoichiometry (2010, background): “…to bubble cultures with air containing different concentrations of CO 2 ; this is arguably a better mimic of the real world situation, though some phytoplankton organisms are intolerant of bubbling (e.g. Fu et al., 2007, Riebesell et al., 2007, Feng et al., 2008, Iglesias-Rodriguez et al., 2008 ).”
- Interactions between changing pCO2, N2 fixation, and Fe limitation in the marine unicellular cyanobacterium Crocosphaera (2008, background): “…including diatoms (Burkhardt and Riebesell 1997; Tortell et al. 2002), cyanobacteria (Fu et al. 2007; Hutchins et al. 2007), coccolithophores (Feng et al. 2008), and harmful bloom flagellates (Fu et al. 2008), the effects of changing seawater pCO2 on unicellular N2-fixing cyanobacteria have…”
- Summary for Policymakers (2022, unknown): “Focusing more on the future, a third independent team of seven scientists (Feng et al., 2008) studied Emiliania huxleyi coccoliths that they isolated from the Sargasso Sea, and which they grew in semicontinuous culture media at low and high light intensities, low and high temperatures (20 and 24°C),”
- Mesocosm CO 2 perturbation studies: from organism to community level (2008, background): “Among these, studies on plankton organisms with CO 2 perturbation ranges relevant to non-deliberate ocean acidification have primarily focussed on coccolithophores (Riebesell et al., 2000; Zondervan et al., 2001, 2002; Sciandra et al., 2003; Leonardos and Geider, 2005; Langer et al., 2006; Feng et a”
- Environmental controls on coccolithophore calcification (2012, background): “Feng et al. (2008) grew Emiliania huxleyi strain CCMP 371 at 2 levels of PAR (50 and 400 µmol m−2 s−1) and 2 levels of CO2 (376 and 750 ppm).”