Arid
DOI10.1093/treephys/tpx160
Cambial phenology in Juniperus przewalskii along different altitudinal gradients in a cold and arid region
Zhang, Junzhou1,2; Gou, Xiaohua1; Pederson, Neil2; Zhang, Fen1; Niu, Haoge1; Zhao, Shoudong2,3; Wang, Fang1
通讯作者Gou, Xiaohua
来源期刊TREE PHYSIOLOGY
ISSN0829-318X
EISSN1758-4469
出版年2018
卷号38期号:6页码:840-852
英文摘要

Knowing more precisely the cambial phenology and wood formation dynamics of trees can lead to a better understanding on how trees react to short-term changes in environmental conditions. Such an understanding could also shed light on the physiological foundation of climate-growth interactions at a regional scale. Although it has been documented that temperature is an important factor determining the cambial phenology in cold and humid climates, there is less agreement on the driver(s) that trigger the onset and end of wood formation in cold and arid climates. Here, the phenological traits of cambial activity and xylem formation were analyzed biweekly along an altitudinal transect ranging from 3580 to 3980 m above sea level, a transect that covers the distribution of Qilian juniper (Juniperus przewalskii Kom.) along a slope of the Tibetan Plateau. Cambial phenology and the duration and rate of wood formation were assessed from anatomical observations during the growing season of the developing xylem obtained from microcores collected from the stem of 10 trees total in 2012 (five at two altitudes each) and 25 trees (five at five altitudes each) in 2013. We found that the onset of wood formation was significantly correlated with altitude in 2013, with onset beginning 8.2 days earlier with every 100 m decrease in elevation. The change in onset with elevation corresponds to a change of 14.1 days degrees C-1 when adjusted for the monitored altitudinal lapse rate of -0.58 degrees C per 100 m. The duration of wood formation lasted from mid-May to mid-August, with the length of the 2013 growing season decreasing from 97 to 65 days from low to high elevation. Although the end of growing season appeared minimally related to altitude during both growing seasons, differences in end of wood production and wood formation between the two growing seasons were significant. It appears that summer drought conditions constricted the end of growing season across all elevations along our transect in 2013. Sensitivity analysis found xylem growth was positively correlated with rate and duration of wood production, with the former explaining most variability in growth. Our findings provide new data on the timing and duration of wood formation and help quantify the potential impacts of global warming on tree growth and productivity in cold and arid regions.


英文关键词altitudes drought global warming northeastern Tibetan Plateau Qilian juniper xylogenesis
类型Article
语种英语
国家Peoples R China ; USA
收录类别SCI-E
WOS记录号WOS:000435576100006
WOS关键词SACHALINENSIS SCHMIDT MASTERS ; EASTERN QILIAN MOUNTAINS ; LOCALLY HEATED STEMS ; TIBETAN PLATEAU ; PINUS-SYLVESTRIS ; WOOD FORMATION ; NORTHWESTERN CHINA ; SCOTS PINE ; ASSIMILATION PRODUCTS ; CELL-DIFFERENTIATION
WOS类目Forestry
WOS研究方向Forestry
来源机构兰州大学 ; 北京师范大学
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/213498
作者单位1.Lanzhou Univ, Coll Earth & Environm Sci, Minist Educ, Key Lab Western Chinas Environm Syst, Lanzhou 730000, Gansu, Peoples R China;
2.Harvard Univ, Harvard Forest, 324 North Main St, Petersham, MA 01366 USA;
3.Beijing Normal Univ, Fac Geog Sci, State Key Lab Earth Surface Proc & Resource Ecol, Beijing 100875, Peoples R China
推荐引用方式
GB/T 7714
Zhang, Junzhou,Gou, Xiaohua,Pederson, Neil,et al. Cambial phenology in Juniperus przewalskii along different altitudinal gradients in a cold and arid region[J]. 兰州大学, 北京师范大学,2018,38(6):840-852.
APA Zhang, Junzhou.,Gou, Xiaohua.,Pederson, Neil.,Zhang, Fen.,Niu, Haoge.,...&Wang, Fang.(2018).Cambial phenology in Juniperus przewalskii along different altitudinal gradients in a cold and arid region.TREE PHYSIOLOGY,38(6),840-852.
MLA Zhang, Junzhou,et al."Cambial phenology in Juniperus przewalskii along different altitudinal gradients in a cold and arid region".TREE PHYSIOLOGY 38.6(2018):840-852.
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