2001
DOI: 10.1016/s0012-821x(01)00399-5
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Oxygen isotope ratios of oak in east England: implications for reconstructing the isotopic composition of precipitation

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Cited by 108 publications
(75 citation statements)
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“…Significant correlations between time series of d 18 O from tree-ring cellulose and temperature, humidity, or precipitation d 18 O have previously been noted at an annual resolution by many researchers working in a range of environments (Luckman & Gray 1990;Lipp et al 1993;Buhay & Edwards 1995;Saurer, Aellen & Siegwolf 1997;Saurer, Borella & Leuenberger 1997;Anderson et al 1998Anderson et al , 2002Saurer, Cherubini & Siegwolf 2000;Robertson et al 2001). Although the many factors that can influence the d 18 O of the moisture prior to uptake by the roots of trees may be somewhat constant when viewed as annual means, changes can be highly variable over shorter time spans.…”
Section: Discussionmentioning
confidence: 88%
“…Significant correlations between time series of d 18 O from tree-ring cellulose and temperature, humidity, or precipitation d 18 O have previously been noted at an annual resolution by many researchers working in a range of environments (Luckman & Gray 1990;Lipp et al 1993;Buhay & Edwards 1995;Saurer, Aellen & Siegwolf 1997;Saurer, Borella & Leuenberger 1997;Anderson et al 1998Anderson et al , 2002Saurer, Cherubini & Siegwolf 2000;Robertson et al 2001). Although the many factors that can influence the d 18 O of the moisture prior to uptake by the roots of trees may be somewhat constant when viewed as annual means, changes can be highly variable over shorter time spans.…”
Section: Discussionmentioning
confidence: 88%
“…Hill et al (1995) also showed that oxygen atoms of carbohydrates in stem tissue are rapidly exchanged with stem water that directly derives from root, before being re-synthesized into cellulose at xylem. Recent field observations, however, have revealed that δ 18 O of tree-ring cellulose is actually affected by the relative humidity in the growing season to a certain degree, although it is mainly controlled by δ 18 O of precipitation (Saurer et al, 1997;Anderson et al, 1998;Robertson et al, 2001). recently compiled a mechanistic model for interpretation of isotope ratios in tree-ring cellulose, where the fraction of oxygen that undergoes exchange with stem water before cellulose synthesis was estimated as 0.42 by comparison of the modeled and observed δ 18 O of tree-ring cellulose.…”
Section: Introductionmentioning
confidence: 99%
“…Especially in a forest with a heavy snow cover, precipitation in winter may take more than several months to penetrate into the root depths (Robertson et al, 2001). It is also necessary to investigate within-site and between-species variations of δ 18 O signal in order to clarify whether a small-scale heterogeneity in soil texture and/or root distribution affect isotopic ratios of water assimilated by a tree (Meinzer et al, 2001).…”
Section: Introductionmentioning
confidence: 99%
“…δ 13 C air ) used to calculate foliar (2002 y) and tree-ring isotopic discrimination chronologies (from 1920 to 2002 y) were extrapolated by recent works of Francey et al (1999) and Robertson et al (2001). Based on these data, we have recomputed the long term time course of tree-rings Δ 13 C values.…”
Section: Isotopic Analysismentioning
confidence: 99%