Seasonal changes of δD and δ 18O in tree-ring cellulose of Quercus crispula suggest a change in post-photosynthetic processes during earlywood growth

被引:27
作者
Nabeshima, Eri [1 ]
Nakatsuka, Takeshi [2 ]
Kagawa, Akira [3 ]
Hiura, Tsutom [4 ]
Funada, Ryo [5 ]
机构
[1] Ehime Univ, Fac Agr, Matsuyama, Ehime 7908566, Japan
[2] Res Inst Humanity & Nat, Kita Ku, 457-4 Motoyama, Kamigamo, Kyoto 6038047, Japan
[3] Forestry & Forest Prod Res Inst, Wood Anat & Qual Lab, Tsukuba, Ibaraki 3058687, Japan
[4] Hokkaido Univ, Field Sci Ctr Northern Biosphere, Tomakomai Res Stn, Takaoka, Toyama 0530035, Japan
[5] Tokyo Univ Agr & Technol, Fac Agr, Saiwai Cho, Fuchu, Tokyo 1838509, Japan
关键词
annual ring; deciduous broad-leaved tree; hydrogen; isotope ratios; oxygen; relative humidity; ring-porous tree; starch; OXYGEN-ISOTOPE RATIOS; CAMBIAL REACTIVATION; FAGUS-SYLVATICA; PINUS-SYLVESTRIS; ORGANIC-MATTER; CARBON-DIOXIDE; WOOD FORMATION; GAS-EXCHANGE; HYDROGEN; VESSELS;
D O I
10.1093/treephys/tpy068
中图分类号
S7 [林业];
学科分类号
0829 ; 0907 ;
摘要
Leaf photosynthetic and post-photosynthetic processes modulate the isotope ratios of tree-ring cellulose. Post-photosynthetic processes, such as the remobilization of stored starch in early spring, are important to understanding the mechanisms of xylem formation in tree stems; however, untangling the isotope ratio signals of photosynthetic and post-photosynthetic processes imprinted on tree rings is difficult. Portions of carbon-bound hydrogen and oxygen atoms are exchanged with medium water during post-photosynthetic processes. We investigated the delta D and delta O-18 values of tree-ring cellulose using Quercus crispula Blume trees in two different habitats to evaluate seasonal changes in the exchange rate (f-value) of hydrogen or oxygen with medium water, and examined the associations of the post-photosynthetic processes. Theoretically, if the f-value is constant, delta D and delta O-18 would be positively correlated due to meteorological factors, while variation in the f-value will create a discrepancy and weak correlation between delta D and delta O-18 due to the exchange of carbon-bound hydrogen and oxygen with medium water. The values of delta D decreased drastically from earlywood to latewood, while those of delta O-18 increased to a peak and then decreased toward the latewood. The estimated seasonal f-value was high at the beginning of earlywood and decreased toward the latewood. The post-photosynthetic processes associated with changes in the f-value were the remobilization of stored starch and triose cycling during cellulose synthesis because of the shortage of photo-assimilates in early spring. Although we did not evaluate relevant physiological parameters, the seasonal pattern of delta D and delta O-18 in tree-ring cellulose of Q. crispula was clear, suggesting that the dual isotope (delta D and delta O-18) approach can be used to reveal the resource allocation mechanisms underlying seasonal xylem formation.
引用
收藏
页码:1829 / 1840
页数:12
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