2021
DOI: 10.1016/j.earscirev.2021.103839
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Disentangling the abiotic versus biotic controls on C3 plant leaf carbon isotopes: Inferences from a global review

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Cited by 13 publications
(5 citation statements)
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“…4), although the Kohn (2010) relation was most similar in terms of slope and had a higher R 2 than the Diefendorf et al (2010) correlation. For the individual Godavari C 3 plants, we noted considerable variation in δ 13 C values for any certain amount of precipitation, in line with earlier studies that found high inter-and intraspecies variation in C 3 plant δ 13 C values in response to MAP (Ma et al, 2012;Liu et al, 2013Liu et al, , 2014Basu et al, 2021;Luo et al, 2021). Moreover, the individual Godavari C 3 plants were not evenly distributed over the entire precipitation range, making it more difficult to establish a correlation.…”
Section: Resultssupporting
confidence: 86%
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“…4), although the Kohn (2010) relation was most similar in terms of slope and had a higher R 2 than the Diefendorf et al (2010) correlation. For the individual Godavari C 3 plants, we noted considerable variation in δ 13 C values for any certain amount of precipitation, in line with earlier studies that found high inter-and intraspecies variation in C 3 plant δ 13 C values in response to MAP (Ma et al, 2012;Liu et al, 2013Liu et al, , 2014Basu et al, 2021;Luo et al, 2021). Moreover, the individual Godavari C 3 plants were not evenly distributed over the entire precipitation range, making it more difficult to establish a correlation.…”
Section: Resultssupporting
confidence: 86%
“…The mean annual precipitation (MAP) in the Godavari basin was used to evaluate the control of drought stress on plant δ 13 C values, as prior studies found evidence for a relationship between MAP and δ 13 C values of C 3 plants around the world (Stewart et al, 1995;Diefendorf et al, 2010;Kohn, 2010). Nonetheless, field surveys and data compilations of C 3 vegetation in drought-stressed regions reported high interand intraspecies variation in C 3 plant δ 13 C values in response to MAP (Ma et al, 2012;Liu et al, 2013Liu et al, , 2014Basu et al, 2021;Luo et al, 2021). The range of ∼ 500 to 1500 mm yr −1 MAP in the Godavari basin was markedly lower than in tropical forests, where MAP is typically > 2000 mm yr −1 and where the majority of global C 3 biomass occurs (Kohn, 2010).…”
Section: Precipitation and Regression Analysismentioning
confidence: 99%
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“…Given that iWUE is regulated by a rapid response of A and gs to environmental variables (Prentice et al, 2014;Basu et al, 2021), time-integrated iWUE can reflect adaptability of plants to their environment, especially in areas with large environmental fluctuations (Maxwell et al, 2018;Guerrieri et al, 2019). Leaf carbon isotope discrimination during photosynthesis ( 13 C) is linearly related to the ratio of the partial pressures of intercellular (Ci) to ambient (Ca) CO 2 (Ci/Ca), and is influenced by both A and gs over a period when the leaf is produced (Farquhar et al, 1989;Maxwell et al, 2018;Prieto et al, 2018).…”
Section: Introductionmentioning
confidence: 99%
“…Given that iWUE is regulated by a rapid response of A and gs to environmental variables (Prentice et al, 2014;Basu et al, 2021), time-integrated iWUE can reflect adaptability of plants to their environment, especially in areas with large environmental fluctuations (Maxwell et al, 2018;Guerrieri et al, 2019). Leaf carbon isotope discrimination during photosynthesis ( 13 C) is linearly related to the ratio of the partial pressures of intercellular (Ci) to ambient (Ca) CO 2 (Ci/Ca), and is influenced by both A and gs over a period when the leaf is produced (Farquhar et al, 1989;Maxwell et al, 2018;Prieto et al, 2018).…”
Section: Introductionmentioning
confidence: 99%