The conundrum of marine N2 fixation
By C. Mahaffey. 2005
257 citations recorded by the source corpus.
Subfields: Ecology, Oceanography
View Paper: https://www.semanticscholar.org/paper/95b02739e9feb4167cccdc9c923b740c94013d42
How researchers see this paper
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In Ecology
- D. Hutchins
- Feixue Fu
- Mark E. Warner
- Yuanyuan Feng
- M. Mulholland
- Yaohong Zhang
- P. Bernhardt
- J. Young
In Oceanography
- D. Hutchins
- Feixue Fu
- Mark E. Warner
- M. Mulholland
- Yuanyuan Feng
- Yaohong Zhang
- P. Bernhardt
- M. Varela
Citations in the corpus
- Latitudinal distribution of Trichodesmium spp. and N 2 fixation in the Atlantic Ocean (2010, background): “Biological N2 fixation represents a major process of new nitrogen supply to the euphotic zone in tropical and subtropical regions of the open ocean (Karl et al., 2002; Mahaffey et al., 2005).”
- Eutrophication of lakes cannot be controlled by reducing nitrogen input: Results of a 37-year whole-ecosystem experiment (2008, background): “Also, unlike the Baltic, many estuaries have rather rapid flushing that would result in the continuous dilution of any N fixed by cyanobacteria (36), potentially keeping an estuary in a chronic N-deficient state despite high rates of N fixation.”
- CO2 control of Trichodesmium N2 fixation, photosynthesis, growth rates, and elemental ratios: Implications for past, present, and future ocean biogeochemistry (2007, background): “new production in some oligotrophic tropical and subtropical oceans (Capone et al. 2005; Mahaffey et al. 2005).”
- Iron availability limits the ocean nitrogen inventory stabilizing feedbacks between marine denitrification and nitrogen fixation (2007, background): “chemical tracer approaches [Michaels et al., 1996; Gruber and Sarmiento, 1997; Mahaffey et al., 2005] (see Hansell et al.”
- Stable isotopic evidence for trophic groupings and bio-regionalization of predators and their prey in oceanic waters off eastern Australia (2009, background): “value. In addition, nitrogen fixation can also be an important process in nutrient poor waters, which will also cause a trend to more depleted d 15 N values ( Mahaffey et al. 2005 ).”