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DOI | 10.1093/aob/mcp158 |
Dendrochronological potential of the alpine shrub Rhododendron nivale on the south-eastern Tibetan Plateau | |
Liang, Eryuan; Eckstein, Dieter | |
通讯作者 | Liang, EY (通讯作者) |
发表日期 | 2009 |
ISSN | 0305-7364 |
EISSN | 1095-8290 |
起始页码 | 665 |
结束页码 | 670 |
卷号 | 104期号:4 |
英文摘要 | Shrubs and dwarf shrubs are wider spread on the Tibetan Plateau than trees and hence offer a unique opportunity to expand the present dendrochronological network into extreme environments beyond the survival limit of trees. Alpine shrublands on the Tibetan Plateau are characterized by rhododendron species. The dendrochronological potential of one alpine rhododendron species and its growth response to the extreme environment on the south-east Tibetan Plateau were investigated. Twenty stem discs of the alpine snowy rhododendron (Rhododendron nivale) were collected close to the tongue of the Zuoqiupu Glacier in south-east Tibet, China. The skeleton plot technique was used for inter-comparison between samples to detect the growth pattern of each stem section. The ring-width chronology was developed by fitting a negative exponential function or a straight line of any slope. Bootstrapping correlations were calculated between the standard chronology and monthly climate data. The wood of snowy rhododendron is diffuse-porous with evenly distributed small-diameter vessels. It has well-defined growth rings. Most stem sections can be visually and statistically cross-dated. The resulting 75-year-long standard ring-width chronology is highly correlated with a timberline fir chronology about 200 km apart, providing a high degree of confidence in the cross-dating. The climate/growth association of alpine snowy rhododendron and of this timberline fir is similar, reflecting an impact of monthly mean minimum temperatures in November of the previous year and in July during the year of ring formation. The alpine snowy rhododendron offers new research directions to investigate the environmental history of the Tibetan Plateau in those regions where up to now there was no chance of applying dendrochronology. |
关键词 | TEMPERATURE RECONSTRUCTIONTREERINGSGLACIERCLIMATEJUNIPERRIVERAREA |
英文关键词 | South-east Tibetan Plateau; Rhododendron nivale; alpine shrub; growth ring; cross-dating; dendroclimatological potential; climate; growth association |
语种 | 英语 |
WOS研究方向 | Plant Sciences |
WOS类目 | Plant Sciences |
WOS记录号 | WOS:000269195900006 |
来源期刊 | ANNALS OF BOTANY
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来源机构 | 中国科学院青藏高原研究所 |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/257656 |
推荐引用方式 GB/T 7714 | Liang, Eryuan,Eckstein, Dieter. Dendrochronological potential of the alpine shrub Rhododendron nivale on the south-eastern Tibetan Plateau[J]. 中国科学院青藏高原研究所,2009,104(4). |
APA | Liang, Eryuan,&Eckstein, Dieter.(2009).Dendrochronological potential of the alpine shrub Rhododendron nivale on the south-eastern Tibetan Plateau.ANNALS OF BOTANY,104(4). |
MLA | Liang, Eryuan,et al."Dendrochronological potential of the alpine shrub Rhododendron nivale on the south-eastern Tibetan Plateau".ANNALS OF BOTANY 104.4(2009). |
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