Climatic forcing of xylem formation in Qilian juniper on the northeastern Tibetan Plateau

被引:27
|
作者
He, Minhui [1 ]
Yang, Bao [1 ]
Wang, Zhangyong [1 ]
Braeuning, Achim [2 ]
Pourtahmasi, Kambiz [3 ]
Oladi, Reza [3 ]
机构
[1] Chinese Acad Sci, Cold & Arid Reg Environm & Engn Res Inst, Key Lab Desert & Desertificat, 320 Donggang West Rd, Lanzhou 730000, Peoples R China
[2] Univ Erlangen Nurnberg, Inst Geog, Wetterkreuz 15, D-91058 Erlangen, Germany
[3] Univ Tehran, Fac Nat Resources, Dept Wood Sci & Technol, POB 31585-4314, Karaj, Iran
来源
TREES-STRUCTURE AND FUNCTION | 2016年 / 30卷 / 03期
基金
美国国家科学基金会;
关键词
Micro-coring method; Dendrometer measurements; Climate factors; Sabina przewalskii Kom; Northeastern Tibetan Plateau; STEM GROWTH-PATTERNS; BALSAMEA L. MILL; WOOD FORMATION; CAMBIAL ACTIVITY; BLACK SPRUCE; ANNUAL PRECIPITATION; RADIUS VARIATIONS; RAIN EXCLUSION; TREE-GROWTH; XYLOGENESIS;
D O I
10.1007/s00468-015-1333-x
中图分类号
S7 [林业];
学科分类号
0829 ; 0907 ;
摘要
Cambial activity of similar to 100-year-old Qilian juniper trees initiated before the middle of May at an elevation of 3200 m a.s.l.; June and July were the main stem radial increment period. Around the middle of August, all xylem cell differentiation periods are completed. Precipitation or relative humidity is the main limiting factor for tree radial growth on the northeastern Tibetan Plateau. Previous studies have found that annual tree-ring width series of Qilian juniper (Sabina przewalskii Kom.) in the northeastern Tibetan Plateau (TP) are mostly moisture controlled, irrespective of site elevation. Knowing precisely the cambial growth dynamics during a vegetation period can lead to a better understanding of the climatic factors driving regional tree growth patterns. We observed wood formation with micro-cores taken at weekly intervals from late April to early October 2013, and monitored daily stem radial changes with high-resolution electronic point dendrometers in 30-min intervals. Dormant cambium contained 5-6 cell layers in the cambium zone. Cambial activity initiated before the middle of May in all the monitored trees. About three quarters of the total cell production or radial growth formed during June and July. Lignification of secondary walls of new xylem cells continued from end of May to middle of August. After the middle of August, the cambium entered into the inactive period. Dendrometer measurements confirmed that June and July were the main stem radial increment period. Nonparametric Kendall's Tau correlations indicate that daily relative humidity and precipitation significantly influence stem growth in May. No obvious relationships were detected in June. In July, significant negative influences of maximum temperature and positive effects of relative humidity prevailed. Overall, growing season precipitation or associated relative humidity is the limiting factor for tree stem radial increments on the intra-annual scale. Our results present a thorough understanding of Qilian juniper xylogenesis and its climate forcing within the whole growing season on the northeastern TP.
引用
收藏
页码:923 / 933
页数:11
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