Stable Isotopes in Plant Ecology

By Todd Dawson, S. Mambelli, A. Plamboeck, P. Templer, K. Tu. 2002

1,915 citations recorded by the source corpus.

Subfields: Atmospheric Science, Ecology, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/e2c955797cd3c2bcfcd53fcd63ba2e0a552c8822

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Citations in the corpus

Different soil moisture conditions change the outcome of the ectomycorrhizal symbiosis between Rhizopogon species and Pinus muricata (2007, methodology): “We also assessed the d 13 C of all Plant Soil (2007) 291:155–165 157 seedling leaves because d 13 C provides an integrated measure of plant carbon and water relations over the life of the leaf (Farquhar et al. 1989; Dawson et al. 2002).”
The problem of isotopic baseline: Reconstructing the diet and trophic position of fossil animals (2011, background): “, 1989), humidity (Dawson et al., 2002; Swap et al., 2004), mean annual rainfall (Swap et al.”
A niche for isotopic ecology (2007, background): “Stable isotopes can tell us much about the physiological pathways and status of resources (Dawson et al. 2002), but it is not always possible to determine the specific taxonomic identity of sources.”
Evaluation of methods to estimate production, biomass and turnover of ectomycorrhizal mycelium in forests soils : A review (2013, background): “One of the problems with isotope techniques is the risk of differences in labelling of different chemical components of the fungal biomass, some of them having a high turnover rate (respiratory substrates), while the heavy isotopewill have longer residence time in structural cell materials (Dawson e”
Interspecific variation in the elemental and stable isotope content of seagrasses in South Florida (2009, background): “:P) ratios and the stable isotopic content of plant material 9 (Farquhar et al. 1989, Dawson et al. 2002, Agren 2004).”
Can carbon-13 in large herbivores reflect the canopy effect in temperate and boreal ecosystems? Evidence from modern and ancient ungulates (2008, background): “In boreal and temperate ecosystems, where C4 plants are practically absent, C3 plants exhibit isotopic contrasts according to environmental conditions (see reviews in Tieszen, 1991; Heaton, 1999; Dawson et al., 2002).”
Partitioning the components of soil respiration: a research challenge (2006, methodology): “sources of respiration ( Dawson et al. 2002 ) as C respired by plants tends to be enriched in 13 C, but heterotrophically derived CO2 is depleted in 13 C,”
Evolution of habitat and environment of red deer (Cervus elaphus) during the Late-glacial and early Holocene in eastern France (French Jura and the western Alps) using multi-isotope analysis (δ13C, δ15N, δ18O, δ34S) of archaeological remains (2011, background): “Landscape closure is another important source of variation in plant d13C values since plants that develop under close canopies present depleted d13C values compared to the same plant form growing in more open conditions (review in Tieszen, 1991; Heaton, 1999; Dawson et al., 2002).”
Getting to the fat of the matter: models, methods and assumptions for dealing with lipids in stable isotope analyses (2007, background): “Stable isotopes have emerged as important tools for addressing questions of plant and animal physiology (Peterson and Fry 1987; Gannes et al. 1997; Dawson et al. 2002), paleoecology (Schwarcz and Schoeninger Communicated by Jay Rosenheim.”
Nitrogen Transfer Within and Between Plants Through Common Mycorrhizal Networks (CMNs) (2003, methodology): “…addition of labeled fertilizer would perturb the N balance of the soil and invalidate the N2 fixation measurement, use of the 15N natural abundance method to investigate the role of mycorrhizae in N transfer is increasing (Pate et al., 1993; Smith and Read, 1997; Evans, 2001; Dawson et al., 2002).”
Ectomycorrhizal lifestyle in fungi: global diversity, distribution, and evolution of phylogenetic lineages (2010, background): “Utilization of stable isotopes, particularly N and C has strongly enhanced understanding of energy flow from molecular to ecosystem levels (Dawson et al. 2002).”
Overlap and partitioning of the ecological and isotopic niches (2010, background): “These habitat-related differences likely stem from differences in evapo-transpiration and water-use efficiency of plants (Ehleringer et al. 1993, Lajtha and Marshall 1994, Dawson et al. 2002) in old-growth forest, young-growth stands, and dearcuts.”