Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.3390/f14051032 |
Differences in the Responses of Tree-Ring Stable Carbon Isotopes of L. sibirica and P. schrenkiana to Climate in the Eastern Tianshan Mountains | |
Jia, Yi; Lv, Guanghui![]() | |
通讯作者 | Zhang, RB |
来源期刊 | FORESTS
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EISSN | 1999-4907 |
出版年 | 2023 |
卷号 | 14期号:5 |
英文摘要 | The eastern Tianshan Mountains are located in the arid interior of Asia, where tree growth is especially sensitive to climate. The ratio of stable carbon isotopes (d(13)C) in the tree rings can provide information on changes in atmospheric CO2 concentrations, water availability, and physiological processes within the tree. In particular, the use of tree-ring d(13)C values as a proxy for past atmospheric CO2 concentrations has gained widespread acceptance. In this study, detrended stable carbon isotope chronologies (C-13(corr)) of Larix sibirica Ledeb. and Picea schrenkiana Fisch. et Mey was established using tree-ring samples from high elevations in the eastern Tianshan Mountains of Xinjiang, China. The relationships between the tree-ring C-13(corr) and different climatic factors were explored using the correlation function and collinearity analysis. Our results demonstrate that the tree-ring d(13)C(corr) of L. sibirica is significantly and negatively correlated with precipitation and relative humidity during the growing season. The main climate factor affecting the stable carbon isotope fractionation of L. sibirica during the growing season is relative humidity during the growing season. The tree-ring d(13)C(corr) of P. schrenkiana is significantly and negatively correlated with the mean temperature, mean minimum temperature, precipitation, and vapor pressure deficit from the end of the previous growing season and throughout the current growing season, especially in summer. However, it is significantly and positively correlated with relative humidity, indicating that the relationship between the climate factors and the tree-ring stable carbon isotope fractionation of P. schrenkiana is more complex. Further analysis showed that summer temperature and summer precipitation jointly controlled the tree-ring stable carbon isotope fractionation of P. schrenkiana at a high elevation. This research has important implications for our understanding of past and future climate change, as well as for the development of effective strategies to mitigate and adapt to these changes. This study also contributed to the development of a more in-depth understanding of the effects of climate change on tree growth in extremely arid environments and provided evidence to support effective forest management in arid regions. |
英文关键词 | Larix sibirica Ledeb. and Picea schrenkiana Fisch. et Mey tree-ring stable carbon isotope climate response eastern Tianshan Mountains |
类型 | Article |
语种 | 英语 |
开放获取类型 | gold |
收录类别 | SCI-E |
WOS记录号 | WOS:000997615300001 |
WOS关键词 | NORTHERN SLOPES ; DELTA C-13 ; CELLULOSE ; VARIABILITY ; RECONSTRUCTION ; RATIOS ; TEMPERATURE ; SOUTHERN ; LIGNIN ; GROWTH |
WOS类目 | Forestry |
WOS研究方向 | Forestry |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/396420 |
推荐引用方式 GB/T 7714 | Jia, Yi,Lv, Guanghui,Guligena, Hailili,et al. Differences in the Responses of Tree-Ring Stable Carbon Isotopes of L. sibirica and P. schrenkiana to Climate in the Eastern Tianshan Mountains[J],2023,14(5). |
APA | Jia, Yi.,Lv, Guanghui.,Guligena, Hailili.,Qin, Li.,Peng, Zhengbing.,...&Zhang, Ruibo.(2023).Differences in the Responses of Tree-Ring Stable Carbon Isotopes of L. sibirica and P. schrenkiana to Climate in the Eastern Tianshan Mountains.FORESTS,14(5). |
MLA | Jia, Yi,et al."Differences in the Responses of Tree-Ring Stable Carbon Isotopes of L. sibirica and P. schrenkiana to Climate in the Eastern Tianshan Mountains".FORESTS 14.5(2023). |
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