CO2 control of Trichodesmium N2 fixation, photosynthesis, growth rates, and elemental ratios: Implications for past, present, and future ocean biogeochemistry

By D. Hutchins, Feixue Fu, Yaohong Zhang, Mark E. Warner, Yuanyuan Feng, Kevin J. Portune, P. Bernhardt, M. Mulholland. 2007

507 citations recorded by the source corpus.

Subfields: Ecology, Oceanography

View Paper: https://www.semanticscholar.org/paper/888464c8b35449ecaa03be1e45792a667935df61

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Citations in the corpus

A microbial source of phosphonates in oligotrophic marine systems (2009, background): “Phosphonates can therefore support marine primary production, as well as climate-driven increases in marine nitrogen fixatio”
Phytoplankton in a changing world: cell size and elemental stoichiometry (2010, background): “The slope and intercept are affected by the taxonomic composition of the data set and the growth conditions for each species (see text for discussion). changes in irradiance, temperature and carbon-dioxide (Finkel et al., 2006; Fu et al., 2007; Hutchins et al., 2007; Fu et al., 2008).”
Ocean acidification and marine microorganisms : responses and consequences (2015, background): “Short-term studies on Trichodesmium spp. reveal that OA or elevated pCO2 will substantially increase the N2 fixation (Hutchins et al., 2007; Levitan et al., 2007; Shetye et al., 2013).”
Responses of marine benthic microalgae to elevated CO2 (2011, unknown): “Experimental studies of bloom-forming cyanobacteria usually show a positive response to CO 2 enrichment (Barcelos e Ramos et al. 2007; Hutchins et al. 2007; Levitan et al. 2007; Fu et al. 2008a; Kranz et al. 2009).”
Co2 and phosphate availability control the toxicity of the harmful bloom dinoflagellate Karlodinium veneficum. (2010, methodology): “Experiments used identical semi-continuous culturing methods to measure phosphate and CO2 effects during acclimated steady-state growth (Hutchins et al. 2007, Fu et al. 2008).”
Consequences of increased temperature and CO2 for phytoplankton community structure in the Bering Sea (2007, methodology): “Photosynthesis vs. irradiance (P/E) curves were assessed using 14C-NaHCO3 uptake in 30 min incubations at the appropriate temperature (11 or 15°C, ±0.2°C) in a photosynthetron over an irradiance range of 0 to 850 µmol photons m–2 s–1 (Fu et al. 2007, Hutchins et al. 2007).”
Interactive effects of increased pCO2, temperature and irradiance on the marine coccolithophore Emiliania huxleyi (Prymnesiophyceae) (2008, methodology): “…caused by a decreased cellular P quota when pCO2 increased from 375 to 750 ppm. Recent work with the marine cyanobacteria Synechococcus (Fu et al., 2006, 2007) and Trichodesmium (Hutchins et al., 2007) has also demonstrated increases in cellular C/P ratios over a similar range of changing pCO2.”