Radial growth of two dominant montane conifer tree species in response to climate change in North-Central China.
North-Central China is a region in which the air temperature has clearly increased for several decades. Picea meyeri and Larix principis-rupprechtii are the most dominant co-occurring tree species within the cold coniferous forest belt ranging vertically from 1800 m to 2800 m a.s.l. in this region. Based on a tree-ring analysis of 292 increment cores sampled from 146 trees at different elevations, this study aimed to examine if the radial growth of the two species in response to climate is similar, whether the responses are consistent along altitudinal gradients and which species might be favored in the future driven by the changing climate. The results indicated the following: (1) The two species grew in different rhythms at low and high elevation respectively; (2) Both species displayed inconsistent relationships between radial growth and climate data along altitudinal gradients. The correlation between radial growth and the monthly mean temperature in the spring or summer changed from negative at low elevation into positive at high elevation, whereas those between the radial growth and the total monthly precipitation displayed a change from positive into negative along the elevation gradient. These indicate the different influences of the horizontal climate and vertical mountainous climate on the radial growth of the two species; (3) The species-dependent different response to climate in radial growth appeared mainly in autumn of the previous year. The radial growth of L. principis-rupprechtii displayed negative responses both to temperature and to precipitation in the previous September, October or November, which was not observed in the radial growth of P. meyeri. (4) The radial growth of both species will tend to be increased at high elevation and limited at low elevation, and L. principis-rupprechtii might be more favored in the future, if the temperature keeps rising.
State Key Laboratory of Earth Surface Processes and Resource Ecology, Beijing Normal University, Beijing, China; Key Laboratory of Traditional Chinese Medicine Protection and Utilization, Beijing Normal University, Beijing, China; College of Resources Science and Technology, Beijing Normal University, Beijing, China.
Yuan
Y
Jiang
State Key Laboratory of Earth Surface Processes and Resource Ecology, Beijing Normal University, Beijing, China; College of Resources Science and Technology, Beijing Normal University, Beijing, China; Beijing Municipal Research Institute of Environmental Protection, Beijing, China.
Wentao
W
Zhang
State Key Laboratory of Earth Surface Processes and Resource Ecology, Beijing Normal University, Beijing, China; College of Resources Science and Technology, Beijing Normal University, Beijing, China.
Mingchang
M
Wang
State Key Laboratory of Earth Surface Processes and Resource Ecology, Beijing Normal University, Beijing, China; College of Resources Science and Technology, Beijing Normal University, Beijing, China.
Muyi
M
Kang
State Key Laboratory of Earth Surface Processes and Resource Ecology, Beijing Normal University, Beijing, China.
Manyu
M
Dong
D000531:Altitude; D002681:China; D002980:Climate; D057231:Climate Change; D017753:Ecosystem; D005843:Geography; D012621:Seasons; D013045:Species Specificity; D013696:Temperature; D064028:Tracheophyta / Q000254:growth & development*; D014197:Trees / Q000254:growth & development*