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Seasonal transfer of oxygen isotopes from precipitation and soil to the tree ring: source water versus needle water enrichment
Author(s) -
Treydte Kerstin,
Boda Sonja,
Graf Pannatier Elisabeth,
Fonti Patrick,
Frank David,
Ullrich Bastian,
Saurer Matthias,
Siegwolf Rolf,
Battipaglia Giovanna,
Werner Willy,
Gessler Arthur
Publication year - 2014
Publication title -
new phytologist
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 3.742
H-Index - 244
eISSN - 1469-8137
pISSN - 0028-646X
DOI - 10.1111/nph.12741
Subject(s) - xylem , precipitation , dendrochronology , phloem , growing season , soil water , environmental science , isotopes of oxygen , water transport , atmospheric sciences , agronomy , botany , biology , chemistry , soil science , water flow , geology , paleontology , physics , nuclear chemistry , meteorology
Summary For accurate interpretation of oxygen isotopes in tree rings (δ 18 O), it is necessary to disentangle the mechanisms underlying the variations in the tree's internal water cycle and to understand the transfer of source versus leaf water δ 18 O to phloem sugars and stem wood. We studied the seasonal transfer of oxygen isotopes from precipitation and soil water through the xylem, needles and phloem to the tree rings of Larix decidua at two alpine sites in the Lötschental (Switzerland). Weekly resolved δ 18 O records of precipitation, soil water, xylem and needle water, phloem organic matter and tree rings were developed. Week‐to‐week variations in needle‐water 18 O enrichment were strongly controlled by weather conditions during the growing season. These short‐term variations were, however, not significantly fingerprinted in tree‐ring δ 18 O. Instead, seasonal trends in tree‐ring δ 18 O predominantly mirrored trends in the source water, including recent precipitation and soil water pools. Modelling results support these findings: seasonal tree‐ring δ 18 O variations are captured best when the week‐to‐week variations of the leaf water signal are suppressed. Our results suggest that climate signals in tree‐ring δ 18 O variations should be strongest at temperate sites with humid conditions and precipitation maxima during the growing season.