Stable oxygen isotope composition of plant tissue: a review.

By Margaret M. Barbour. Functional Plant Biology, 2007

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Climate-related variability in carbon and oxygen stable isotopes among populations of Aleppo pine grown in common-garden tests (2008, background): “of source and atmospheric water, (2) evaporative enrichment of leaf water due to transpiration, and (3) biochemical fractionation during the synthesis of organic matter (Farquhar et al. 1998; Barbour 2007).”
Intra-annual density fluctuations in tree rings: how, when, where, and why? (2016, background): “Data on δ18O in combination with δ13C help to determine whether changes in δ13C are due to modifications in photosynthetic levels or in stomatal conductance (Scheidegger et al. 2000; Barbour 2007).”
Molecular Paleohydrology: Interpreting the Hydrogen-Isotopic Composition of Lipid Biomarkers from Photosynthesizing Organisms (2012, background): “Summary and discussions of leaf-water models can be found in the recent literature (Barbour 2007, Farquhar et al. 2007, Ferrio et al. 2009, Kahmen et al. 2008).”
Breeding for Yield Potential and Stress Adaptation in Cereals (2008, background): “In this context oxygen isotope composition (δ18O) in plant tissues might be an alternative since it reflects (among other effects) evaporative enrichment of leaf water caused by transpiration (Barbour, 2007; Farquhar et al., 2007).”