Tree-ring cellulose δ18O variability in pine and oak and its potential to reconstruct precipitation and relative humidity in central Japan

Zhen Li, Takeshi Nakatsuka, Masaki Sano

Research output: Contribution to journalArticle

11 Citations (Scopus)

Abstract

Oxygen isotope ratios (δ18O) of tree-ring cellulose in pine (Pinus densiflora) and oak (Quercus serrate and Quercus variabilis) growing in central Japan from 1970 to 2011 share a common inter-annual variance among different cores in a tree, different trees in a species, and different species in a forest. The high mean correlation between the two radii (r = 0.738) of individual trees and the mean standard deviation of two measurements for the same year from the two radii of eight trees (σ = 0.361‰) reveals the reliability and representativeness of single cores. The significant correlation (r = 0.667, p < 0.01) between pine and oak cellulose δ18O suggests that δ18O in tree-ring cellulose is controlled by common external factors, and that it is possible to establish a unique δ18O chronology using different tree species. The δ18O values of tree-ring cellulose in pine and oak trees are negatively correlated with precipitation from June to August (correlation coefficients are -0.679 for pine and -0.583 for oak), which is attributable to the precipitation amount effect, mainly caused by the stagnant rain front (Baiu) in early summer and typhoons in late summer in this region. The δ18O values are negatively correlated with relative humidity from April to September for pine (r = -0.632, p < 0.01), and in June and July for oak (r = -0.437, p < 0.01); these correlations probably reflect different lengths of the growing season. Multiple regression analysis reveals that tree-ring δ18O values of pine and oak in this region are largely governed by summer precipitation. Relative humidity does not appear to greatly affect tree-ring δ18O of oak, in contrast to pine, which may be interpreted in terms of differences in leaf morphology and/or cellulose synthesis processes. Our results indicate that δ18O values of tree-ring cellulose can provide a potential crossdating tool, irrespective of the physiological differences between gymnosperms and angiosperms. In central Japan, tree-ring δ18O values of both pine and oak can act as reliable proxies of June-August precipitation, while pine trees tend to exhibit more potential for reconstruction of relative humidity.

Original languageEnglish
Pages (from-to)125-137
Number of pages13
JournalGeochemical Journal
Volume49
Issue number2
DOIs
Publication statusPublished - 2015
Externally publishedYes

Fingerprint

Precipitation (meteorology)
tree ring
cellulose
Cellulose
humidity
relative humidity
Japan
Atmospheric humidity
rings
Oxygen Isotopes
summer
leaf morphology
Regression analysis
oxygen isotope ratio
Rain
gymnosperm
oak
angiosperm
angiosperms
multiple regression

Keywords

  • Central Japan
  • Oak
  • Pine
  • Precipitation
  • Relative humidity
  • Tree-ring cellulose δO

ASJC Scopus subject areas

  • Geophysics
  • Geochemistry and Petrology

Cite this

Tree-ring cellulose δ18O variability in pine and oak and its potential to reconstruct precipitation and relative humidity in central Japan. / Li, Zhen; Nakatsuka, Takeshi; Sano, Masaki.

In: Geochemical Journal, Vol. 49, No. 2, 2015, p. 125-137.

Research output: Contribution to journalArticle

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abstract = "Oxygen isotope ratios (δ18O) of tree-ring cellulose in pine (Pinus densiflora) and oak (Quercus serrate and Quercus variabilis) growing in central Japan from 1970 to 2011 share a common inter-annual variance among different cores in a tree, different trees in a species, and different species in a forest. The high mean correlation between the two radii (r = 0.738) of individual trees and the mean standard deviation of two measurements for the same year from the two radii of eight trees (σ = 0.361‰) reveals the reliability and representativeness of single cores. The significant correlation (r = 0.667, p < 0.01) between pine and oak cellulose δ18O suggests that δ18O in tree-ring cellulose is controlled by common external factors, and that it is possible to establish a unique δ18O chronology using different tree species. The δ18O values of tree-ring cellulose in pine and oak trees are negatively correlated with precipitation from June to August (correlation coefficients are -0.679 for pine and -0.583 for oak), which is attributable to the precipitation amount effect, mainly caused by the stagnant rain front (Baiu) in early summer and typhoons in late summer in this region. The δ18O values are negatively correlated with relative humidity from April to September for pine (r = -0.632, p < 0.01), and in June and July for oak (r = -0.437, p < 0.01); these correlations probably reflect different lengths of the growing season. Multiple regression analysis reveals that tree-ring δ18O values of pine and oak in this region are largely governed by summer precipitation. Relative humidity does not appear to greatly affect tree-ring δ18O of oak, in contrast to pine, which may be interpreted in terms of differences in leaf morphology and/or cellulose synthesis processes. Our results indicate that δ18O values of tree-ring cellulose can provide a potential crossdating tool, irrespective of the physiological differences between gymnosperms and angiosperms. In central Japan, tree-ring δ18O values of both pine and oak can act as reliable proxies of June-August precipitation, while pine trees tend to exhibit more potential for reconstruction of relative humidity.",
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AB - Oxygen isotope ratios (δ18O) of tree-ring cellulose in pine (Pinus densiflora) and oak (Quercus serrate and Quercus variabilis) growing in central Japan from 1970 to 2011 share a common inter-annual variance among different cores in a tree, different trees in a species, and different species in a forest. The high mean correlation between the two radii (r = 0.738) of individual trees and the mean standard deviation of two measurements for the same year from the two radii of eight trees (σ = 0.361‰) reveals the reliability and representativeness of single cores. The significant correlation (r = 0.667, p < 0.01) between pine and oak cellulose δ18O suggests that δ18O in tree-ring cellulose is controlled by common external factors, and that it is possible to establish a unique δ18O chronology using different tree species. The δ18O values of tree-ring cellulose in pine and oak trees are negatively correlated with precipitation from June to August (correlation coefficients are -0.679 for pine and -0.583 for oak), which is attributable to the precipitation amount effect, mainly caused by the stagnant rain front (Baiu) in early summer and typhoons in late summer in this region. The δ18O values are negatively correlated with relative humidity from April to September for pine (r = -0.632, p < 0.01), and in June and July for oak (r = -0.437, p < 0.01); these correlations probably reflect different lengths of the growing season. Multiple regression analysis reveals that tree-ring δ18O values of pine and oak in this region are largely governed by summer precipitation. Relative humidity does not appear to greatly affect tree-ring δ18O of oak, in contrast to pine, which may be interpreted in terms of differences in leaf morphology and/or cellulose synthesis processes. Our results indicate that δ18O values of tree-ring cellulose can provide a potential crossdating tool, irrespective of the physiological differences between gymnosperms and angiosperms. In central Japan, tree-ring δ18O values of both pine and oak can act as reliable proxies of June-August precipitation, while pine trees tend to exhibit more potential for reconstruction of relative humidity.

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