2013
DOI: 10.1016/j.agrformet.2012.08.007
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Inter- and intra-annual stable carbon and oxygen isotope signals in response to drought in Mediterranean pines

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Cited by 141 publications
(116 citation statements)
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“…The positive correlation between the values of δ 13 C and productivity has also been reported in other studies (SARRIS et al, 2013) and may be due to a lower stomata conductance associated with the maintenance of the photosynthetic rate by the tolerant clone (DUCREY et al, 2008). This suggests that this clone has mechanisms that provide a greater transpiration efficiency and hence higher productivity than the drought-sensitive one when growing in environments under severe water deficit.…”
supporting
confidence: 58%
“…The positive correlation between the values of δ 13 C and productivity has also been reported in other studies (SARRIS et al, 2013) and may be due to a lower stomata conductance associated with the maintenance of the photosynthetic rate by the tolerant clone (DUCREY et al, 2008). This suggests that this clone has mechanisms that provide a greater transpiration efficiency and hence higher productivity than the drought-sensitive one when growing in environments under severe water deficit.…”
supporting
confidence: 58%
“…Barbour et al, 2002;Sarris et al, 2013), but there is a lack of focus in the literature on relating these changes to the discrete hydrological processes which control the availability of water at the rooting zone. Furthermore, to date, most studies have relied on differences between cellulosic isotope values from tree rings to infer water source variations, without deconvolving the actual signature of source water (Marshall and Monserud, 2006;Singer et al, 2013).…”
Section: Discussionmentioning
confidence: 99%
“…O values for Pinus radiata reflected the seasonal variations in water source use as did Sarris et al (2013) with Mediterranean Pinus halepensis which relied on deeper moisture sources, (depleted δ 18 O cell ), during drought conditions. To reliably interpret highly resolved δ 18 O cell values in relation to water sources requires a clear isotopic characterization of local and regional sources of water (e.g.…”
mentioning
confidence: 99%
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“…S1). This warming increases water evaporation and causes 18 O enrichment of water at the soil surface that is then archived in the tree-ring isotopic signature (Sarris et al, 2013). The second explanation relates to the increased soil water availability at the HT plot, where trees can use more accessible, shallower water sources that are relatively more 18 O enriched.…”
mentioning
confidence: 99%