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Response of radial growth to warming and CO2 enrichment in southern Northeast China: a case of Pinus tabulaeformis
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  • 作者:Zhenju Chen ; Xianliang Zhang ; Xingyuan He ; Nicole K. Davi ; Lulu Li…
  • 刊名:Climatic Change
  • 出版年:2015
  • 出版时间:June 2015
  • 年:2015
  • 卷:130
  • 期:4
  • 页码:559-571
  • 全文大小:1,527 KB
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  • 作者单位:Zhenju Chen (1) (2)
    Xianliang Zhang (1)
    Xingyuan He (2)
    Nicole K. Davi (3) (4)
    Lulu Li (1)
    Xueping Bai (1)

    1. Tree-Ring Laboratory, Forestry College/Research Station of Liaohe-River Plain Forest Ecosystem CFERN, Shenyang Agriculture University, Shenyang, 110866, China
    2. Qingyuan Forest CERN, Chinese Academy of Sciences, Shenyang, 110164, China
    3. Tree-Ring Laboratory, Lamont-Doherty Earth Observatory, Columbia University, New York, NY, 10964, USA
    4. Department of Environmental Science, William Paterson University, Wayne, NJ, 07040, USA
  • 刊物类别:Earth and Environmental Science
  • 刊物主题:Earth sciences
    Meteorology and Climatology
  • 出版者:Springer Netherlands
  • ISSN:1573-1480
文摘
The southern part of northeast China has experienced a marked warming and drying climate. We provide dendrochronological evidence for atmospheric CO<sub>2sub> fertilization and the impacts of warming on Chinese pine (Pinus tabulaeformis) growth. The results of this study show that increased temperature has a negative effect on pine growth during a major part of the growing season and a weakly positive effects on growth during the remaining portion of the year. The monthly temperatures explain ca. 20?% of the total variance in the annual radial growth of Chinese pine from 1901 to 2009. An increase of approximately 3-?°C is the maximum that Chinese pine can tolerate in this region with an annual rainfall of 500-00?mm. Our results suggest a that there is a proportional response to warming only up to a maximum of 1 °C warming, and indicate the complexitiesof succession in forest ecosystems in terms of adaptation and evolution in local pine populations under a rapid warming condition. In addition, increasing atmospheric CO<sub>2sub> concentrations have a positive effect on tree growth. This effect can be detected with conventional dendrochronological methods.

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