TY - JOUR
T1 - Recent strengthening of correlations between tree-ring δ13C and δ18O in mesic western China
T2 - Implications to climatic reconstruction and physiological responses
AU - Liu, Xiaohong
AU - An, Wenling
AU - Leavitt, Steven W.
AU - Wang, Wenzhi
AU - Xu, Guobao
AU - Zeng, Xiaomin
AU - Qin, Dahe
N1 - Funding Information:
This research was supported by the National Natural Science Foundation of China ( 41121001 , 41171167 ), by the self-determination project of the State Key Laboratory of Cryospheric Sciences ( SKLCS-ZZ-2013-01-03 ) and the Knowledge Innovation Project of the Chinese Academy of Sciences ( KZCX2-YW-QN308 ). We gratefully acknowledge the journal's three anonymous reviewers for their constructive comments on earlier versions of this manuscript.
PY - 2014/2
Y1 - 2014/2
N2 - 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.
AB - 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.
KW - Relative humidity
KW - Stomatal control
KW - Tree rings
KW - δC-δO relationship
UR - https://www.scopus.com/pages/publications/84891285511
UR - https://www.scopus.com/pages/publications/84891285511#tab=citedBy
U2 - 10.1016/j.gloplacha.2013.12.005
DO - 10.1016/j.gloplacha.2013.12.005
M3 - Article
AN - SCOPUS:84891285511
SN - 0921-8181
VL - 113
SP - 23
EP - 33
JO - Global and Planetary Change
JF - Global and Planetary Change
ER -