Seasonal dynamics of wood formation in Pinus halepensis from dry and semi-arid ecosystems in Spain

被引:153
作者
De Luis, Martin
Gricar, Jozica
Cufar, Katarina
Raventos, Jose
机构
[1] Univ Zaragoza, Dept Geografiay, Zaragoza 50009, Spain
[2] Slovenian Forestry Inst, SI-1000 Ljubljana, Slovenia
[3] Univ Ljubljana, Fac Biotech, Dept Wood Sci & Technol, SI-1000 Ljubljana, Slovenia
[4] Univ Alicante, Dept Ecol, Alicante 03080, Spain
关键词
aleppo pine; western Mediterranean; cambial activity; wood formation; tracheids; resin canals; false rings;
D O I
10.1163/22941932-90001651
中图分类号
S7 [林业];
学科分类号
0829 ; 0907 ;
摘要
The seasonal dynamics of cambial activity, wood formation, occurrence of false rings (FR), and tangential bands of resin canals (RC) were investigated in Pinus halepensis from three Mediterranean dry and semi-arid ecosystems in Spain. We collected intact tissues of phloem, cambium, and outer xylem at monthly intervals throughout 2004 from each time six trees at the three sites. Cell divisions in the cambium in all trees started before our first sampling in mid-March and ceased between November and December. Cambial activity was characterized by two maxima; one in spring and another in autumn. Trees still grew in summer but at a very low rate. The first solitary RC were formed in May or June and tangential bands of RC in June or July. In general, tangential bands of RC were observed in wider growth rings. The formation of tangential bands of RC seems to be induced by drought in the second half of the growing season. FR were formed as a result of cambial reactivation in autumn and were observed in growth rings that contained more than 50 cells in a radial row. It appears that summer drought and early autumn precipitation play an important role in false-ring formation.
引用
收藏
页码:389 / 404
页数:16
相关论文
共 39 条
[1]  
[Anonymous], 1978, MICROSCOPIC WOOD ANA
[2]   THE RELATIONSHIP BETWEEN CLIMATIC VARIABLES AND WOOD STRUCTURE IN PINUS-HALEPENSIS MILL .1. EFFECTS OF HUMIDITY AND TEMPERATURE [J].
ATTOLINI, MR ;
CALVANI, F ;
GALLI, M ;
NANNI, T ;
RUGGIERO, L ;
SCHAER, E ;
ZUANNI, F .
THEORETICAL AND APPLIED CLIMATOLOGY, 1990, 41 (03) :121-127
[3]  
Barbero Marcel, 1998, P153
[4]   Dendroclimatological potential of drought-sensitive tree stands in southern Tibet for the reconstruction of monsoonal activity [J].
Bräuning, A .
IAWA JOURNAL, 1999, 20 (03) :325-338
[5]   Identification, measurement and interpretation of tree rings in woody species from mediterranean climates [J].
Cherubini, P ;
Gartner, BL ;
Tognetti, R ;
Bräker, OU ;
Schoch, W ;
Innes, JL .
BIOLOGICAL REVIEWS, 2003, 78 (01) :119-148
[6]  
FAHN A, 1970, ISRAEL J BOT, V19, P429
[7]  
Fritts H., 1976, TREE RINGS CLIMATE
[8]  
Gartner Barbara L., 1995, P125, DOI 10.1016/B978-012276460-8/50008-4
[9]  
GINDEL I, 1967, MILL P 16 IUFRO C MU, V4, P188
[10]   Differentiation of terminal latewood tracheids in silver fir during autumn [J].
Gricar, J ;
Cufar, K ;
Oven, P ;
Schmitt, U .
ANNALS OF BOTANY, 2005, 95 (06) :959-965