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DOI: 10.1016/j.gloplacha.2013.12.005
Title:
Recent strengthening of correlations between tree-ring δ13C and δ18O in mesic western China: Implications to climatic reconstruction and physiological responses
Author: Liu X.; An W.; Leavitt S.W.; Wang W.; Xu G.; Zeng X.; Qin D.
ISSN: 0921-8465
Publishing Year: 2014
Volume: 113
pages begin: 23
pages end: 33
Language: 英语
Keyword: δ13C-δ18O relationship ; Relative humidity ; Stomatal control ; Tree rings
Scopus Keyword: Analysis of temporal changes ; Climatic reconstruction ; Physiological response ; Spatial correlations ; Stomatal control ; Temporal fluctuation ; Temporal relationships ; Tree rings ; Atmospheric humidity ; Carbon ; Global warming ; Isotopes ; Moisture ; O rings ; Photosynthesis ; Forestry ; carbon isotope ; cellulose ; climate effect ; coniferous tree ; oxygen isotope ; photosynthesis ; physiological response ; reconstruction ; relative humidity ; stomata ; temporal variation ; tree ring ; Carbon ; Forestry ; Humidity ; Isotopes ; Moisture ; Photosynthesis ; Rings ; Trees ; China
English Abstract: We examined the temporal relationships between stable isotopes of carbon (δ13C) and oxygen (δ18O) from annual tree-ring cellulose of Abies georgei on the moist Batang-Litang plateau, western China. Climatic response analysis reveals that tree-ring δ13C contains a strong moisture signal, and that δ13C was especially influenced by relative humidity and precipitation in May through August during the period 1960-2005. In addition, tree-ring δ13C and temperature in May to August are positively correlated because of the high-elevation tree growth sites. Drought is also recorded in tree-ring δ13C, reflecting the integrated influences of temperature and moisture on stomatal regulation and photosynthesis. Generally, correlations between δ13C and δ18O remained positive, but not significant, in most of the investigated period, and this correlation switched to highly significant from 1969 onwards. Changes in the δ13C-δ18O relationship reflect changes in water stress on carbon isotopic discrimination, suggesting an increase in stomatal control of photosynthesis in recent decades, which is consistent with the overall drying trend in the region. Spatial correlation maps confirm that during the past century the response of tree-ring δ13C to temperature and precipitation differs before and after 1969. Using previously reported δ18O results and new δ13C results on the same samples, we determined that the climatic signal recorded in tree-ring δ18O is more stable than that of δ13C. Analysis of temporal changes in the δ13C-δ18O correlations indicates that dominant processes and the controlling factors on tree-ring δ13C potentially shift over the long term under temporal fluctuations of dry-wet spells, especially under recent global warming, and stomatal control of photosynthesis may adjust to region-wide changes in climate in this region where water stress on forest was formerly minor. © 2013.
Related Link: https://www.scopus.com/inward/record.uri?eid=2-s2.0-84891285511&doi=10.1016%2fj.gloplacha.2013.12.005&partnerID=40&md5=5760030ac1ebec27f93a90cd46647bdd
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被引频次[WOS]:9   [查看WOS记录]     [查看WOS中相关记录]
Document Type: 期刊论文
Identifier: http://119.78.100.158/handle/2HF3EXSE/11371
Appears in Collections:全球变化的国际研究计划

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Affiliation: State Key Laboratory of Cryospheric Sciences, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China

Recommended Citation:
Liu X.,An W.,Leavitt S.W.,et al. Recent strengthening of correlations between tree-ring δ13C and δ18O in mesic western China: Implications to climatic reconstruction and physiological responses[J],2014-01-01,113.
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