Interactions between changing pCO2, N2 fixation, and Fe limitation in the marine unicellular cyanobacterium Crocosphaera

By Feixue Fu, M. Mulholland, N. Garcia, A. Beck, P. Bernhardt, Mark E. Warner, S. Sañudo-Wilhelmy, D. Hutchins. 2008

168 citations recorded by the source corpus.

Subfields: Atmospheric Science, Ecology, Oceanography

View Paper: https://www.semanticscholar.org/paper/04c9229180257b53965ee896df0dd41dce39fc5b

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Atmospheric Science

1. Philip W. Boyd

In Ecology

1. D. Hutchins
2. Feixue Fu
3. Philip W. Boyd
4. N. Garcia
5. Jun Sun
6. David A. Caron
7. Yuanyuan Feng
8. E. Webb

In Oceanography

1. D. Hutchins
2. Feixue Fu
3. Philip W. Boyd
4. N. Garcia
5. Yuanyuan Feng
6. David A. Caron
7. Jun Sun
8. E. Webb

Citations in the corpus

• Differing responses of marine N2 fixers to warming and consequences for future diazotroph community structure (2014, methodology): “After the cultures reached steady state in each treatment, primary production was measured in duplicate using 24 h incubations of 30 ml subsamples with H14CO3 under the appropriate experimental growth conditions for each treatment (Fu et al. 2008).”
• Effect of ocean acidification on microbial diversity and on microbe-driven biogeochemistry and ecosystem functioning (2010, background): “…et al. (2008) Fu et al. (2007) Fu et al. (2007) Czerny et al. (2009) Barcelos e Ramos et al. (2007) Schulz et al. (2008)* Hutchins et al. (2007) Hutchins et al. (2007) Hutchins et al. (2007) Hutchins et al. (2007) Hutchins et al. (2007) Engel et al. (2002) Engel et al. (2002) Engel et al.…”
• 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).”
• Effects of changing pCO2 and phosphate availability on domoic acid production and physiology of the marine harmful bloom diatom Pseudo‐nitzschia multiseries (2011, background): “Our results raise the possibility that growth rates and toxicity of the diatom Pseudo-nitzschia multiseries could increase substantially in the future high-CO2 ocean, suggesting a potentially escalating negative effect of this harmful algal bloom species on the future marine environment.”
• Understanding the responses of ocean biota to a complex matrix of cumulative anthropogenic change (2012, background): “Climate-change mediated shifts in multiple environmental properties often exert non-linear and counterintuitive controls over many aspects of ocean biota (Fu et al. 2008, Rose et al. 2009a).”
• Effects of ocean acidification on macroalgal communities (2011, background): “Some cyanobacteria grow well with CO2 enrichment and their increased N2 fixation may alter ocean biogeochemistry (Fu et al., 2008; Kranz et al., 2009).”
• Response of photosynthesis to ocean acidification (2015, background): “Growth of the red tide forming raphidophyte Heterosigma akashiwo likewise increased under high CO2, although maximal photosynthetic rates remained unaltered (Fu et  al., 2008).”