Nitrogen isotope fractionation in 12 species of marine phytoplankton during growth on nitrate
By J. Needoba, N. Waser, P. Harrison, S. Calvert. 2003
206 citations recorded by the source corpus.
Subfields: Ecology, Oceanography
View Paper: https://www.semanticscholar.org/paper/9d736ab21d4e3da0b018995f0a4ad4d8d6b86b23
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In Ecology
In Oceanography
Citations in the corpus
- INFLUENCE OF LOW LIGHT AND A LIGHT: DARK CYCLE ON NO3– UPTAKE, INTRACELLULAR NO3–, AND NITROGEN ISOTOPE FRACTIONATION BY MARINE PHYTOPLANKTON 1 (2004, methodology): “C), whereas aMass balance was calculated by (final PN/initial NO3 ) 100. bFrom Needoba et al. (2003). the E. huxleyi population divided mostly at night (Fig.”
- THE MECHANISM OF ISOTOPE FRACTIONATION DURING ALGAL NITRATE ASSIMILATION AS ILLUMINATED BY THE 15N/14N OF INTRACELLULAR NITRATE 1 (2004, methodology): “%) in similar culture conditions (Waser et al. 1998, Needoba et al. 2003) is the result of higher relative efflux by the smaller cell.”
- Stable C and N isotopic composition of cold-water corals from the Newfoundland and Labrador continental slope: Examination of trophic, depth and spatial effects (2008, background): “For d(15)N, we expected lower values at the northern sites, where NO3 is less limiting, because phytoplankton discriminate against (15)N (Needoba et al., 2003).”