Latitudinal variation in radial growth phenology of Cryptomeria japonica D. Don trees in Japan

被引:7
作者
Nishizono, Tomohiro [1 ]
Zushi, Kotaro [2 ]
Hiroshima, Takuya [3 ]
Toyama, Keisuke [4 ]
Kitahara, Fumiaki [5 ]
Terada, Fumiko [6 ]
Takagi, Masahiro [7 ]
Saito, Satoshi [8 ]
机构
[1] Forestry & Forest Prod Res Inst, Dept Forest Management, 1 Matsunosato, Tsukuba, Ibaraki 3058687, Japan
[2] Toyama Forestry & Forest Prod Res Ctr, 3 Yoshimine, Tateyama, Toyama 9301362, Japan
[3] Univ Tokyo Forests, Ecohydrol Res Inst, 11-44 Goizuka, Seto, Aichi 4890031, Japan
[4] Univ Tokyo Chiba Forest, 770 Amatsu, Kamogawa, Chiba 2995503, Japan
[5] Forestry & Forest Prod Res Inst, Shikoku Res Ctr, 2-915 Asakura Nishimachi, Kochi 7808077, Japan
[6] Hokkaido Res Org, Forestry Res Inst, Donan Stn, 372-2 Kikyo, Hakodate, Hokkaido 0410801, Japan
[7] Univ Miyazaki, Fac Agr, 11300 Tano Cho, Miyazaki 8891702, Japan
[8] Forestry & Forest Prod Res Inst, Dept Plant Ecol, Tsukuba, Ibaraki 3058687, Japan
来源
FORESTRY | 2018年 / 91卷 / 02期
基金
日本学术振兴会;
关键词
WOOD FORMATION; XYLEM PHENOLOGY; SCOTS PINE; CONIFERS; DENDROMETER; FOREST; TEMPERATURES; XYLOGENESIS; DYNAMICS; PATTERNS;
D O I
10.1093/forestry/cpx055
中图分类号
S7 [林业];
学科分类号
0829 ; 0907 ;
摘要
We investigated the latitudinal variation in radial growth phenology (onset, cessation, and duration of radial growth) of Cryptomeria japonica D. Don trees in Japan. The radial growth was observed using dendrometers in 16 stands at multiple latitudes throughout Japan. The onset of radial growth showed a clear latitudinal gradient: at high-latitude sites, C. japonica growth started later than at low-latitude sites. However, cessation of radial growth was independent of latitude. Consequently, the duration of radial growth (defined based on the onset and cessation dates) showed a weak but significant latitudinal gradient: at high-latitude sites, C. japonica trees grew for a shorter period than trees at low-latitude sites. The onset and duration of growth were respectively strongly and weakly affected by temperature, although growth cessation was not explained by temperature or precipitation. The latitudinal gradient for duration of radial growth weakly but significantly supports the hypothesis that regional variation in growth phenology is a key factor responsible for the regional variation in long-term growth. Furthermore, we found that growth duration was more variable at low latitudes than at high latitudes.
引用
收藏
页码:206 / 216
页数:11
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