Physiological mechanisms influencing plant nitrogen isotope composition.
By R. Evans. Trends in Plant Science, 2001
845 citations recorded by the source corpus.
Subfields: Global and Planetary Change, Plant Science, Soil Science
View Paper: https://www.semanticscholar.org/paper/bc1687cf36587cfff77699cc09d8a5c7e0d55360
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Citations in the corpus
- The Nitrogen Paradox in Tropical Forest Ecosystems (2009, background): “However, this assumption likely oversimplifies the considerable complexity observed in 15N across different soil N pools and fractionating paths of the plant-soil N cycle (Boddey et al. 2000; Evans 2001; Högberg 1997; Houlton et al. 2006, 2007).”
- Specific leaf area explains differences in leaf traits between congeneric savanna and forest trees (2005, background): “N ( Evans 2001 ), the opposite relationship with pH would be expected.”
- Influence of seabird guano and camelid dung fertilization on the nitrogen isotopic composition of field-grown maize (Zea mays) (2012, background): “…or the course of their lives, plants will route and re-route nitrogen contained in their tissues depending on, for example, their growth stage (e.g. vegetative vs. reproductive) or environmental conditions (e.g. onset of winter) (Bausenwein et al., 2001a, 2001b; Evans, 2001; Kolb and Evans, 2002).”
- Dominance of legume trees alters nutrient relations in mixed species forest restoration plantings within seven years (2008, background): “However, this requires further research since the scope for interpreting plant N sources from d15N in leaves, litter and total soil alone is limited, due to 15N fractionation processes occurring by several mechanisms at several levels (Robinson 2001; Evans 2001; Schmidt et al. 2006).”
- Grass competition induces N2 fixation in some species of African Acacia (2007, methodology): “…we used the non-nodulating Acacia ataxacantha , grown under identical circumstances to the other legumes, as a reference plant in both the field and the pot experiments. δ 15 N values are determined by the integration of the entire soil- and plant-nitrogen cycle (Evans 2001; Robinson 2001).”
- Nitrogen isotopes in ectomycorrhizal sporocarps correspond to belowground exploration types (2010, background): “Nitrogen isotopes (expressed as δ(15)N values) are potentially useful because they are an integrated measure of processes affecting nitrogen dynamics (Högberg 1997; Evans 2001; Robinson 2001).”
- The carbon and nitrogen isotope composition of Australian grasses in relation to climate. (2009, background): “Although extensive fractionation may occur within plants (Evans 2001), foliar 515N tends to reflect soil 515N (Austin & Vitousek 1998; Handley et al 1999), and a number of authors have suggested that it is the 'openness' of the nitrogen cycle that primarily influences soil 815N (Austin & Vitousek 19”
- Plants on Plants – The Biology of Vascular Epiphytes (2016, background): “an approach based on theory which predicts that N-limited plants will reflect the natural (15)N abundance of their N sources, while P-limited plants fractionate against (15)N (Evans 2001).”
- Nitrogen Transfer Within and Between Plants Through Common Mycorrhizal Networks (CMNs) (2003, methodology): “Consequently, after translocation of relatively lower δ15N amino acids, plants would have a lower δ15N and the fungi a greater δ15N than the N source (Evans, 2001).”
- Functional leaf traits of vascular epiphytes: vertical trends within the forest, intra‐ and interspecific trait variability, and taxonomic signals (2016, background): “The d(15)N signatures of plants are mostly affected by their assimilatory pathway, but also by form (NO4 , NH 3 , N2) and d(15)N signature of the nitrogen source (Evans 2001).”
- Greater root phosphatase activity in nitrogen‐fixing rhizobial but not actinorhizal plants with declining phosphorus availability (2017, methodology): “son were collected for analyses to reduce seasonal variation of leaf d(15)N (Shearer & Kohl 1986; Evans 2001).”
- Growth of N2‐fixing African savanna Acacia species is constrained by below‐ground competition with grass (2010, methodology): “As the leaves of the trees were sampled from distinct areas, the soil d15N was used to calculate isotopic fractionation between soil and leaf as D15N = d15Nsoil ) d 15Nleaf, according to Evans (2001).”