Intraseasonal climate and habitat-specific variability controls the flowering phenology of high alpine plant species

被引:79
作者
Huelber, Karl [1 ,2 ]
Winkler, Manuela [3 ]
Grabherr, Georg [2 ]
机构
[1] Vienna Inst Nat Conservat & Anal, A-1090 Vienna, Austria
[2] Univ Vienna, Dept Conservat Biol Vegetat Ecol & Landscape Ecol, Fac Ctr Biodivers, Fac Life Sci, A-1091 Vienna, Austria
[3] Univ Nat Resources & Appl Life Sci, Inst Bot, Dept Integrat Biol, A-1180 Vienna, Austria
关键词
Central European Alps; climate warming; temperature sum; snow cover duration; REPRODUCTIVE PHENOLOGY; SWISS ALPS; TEMPORAL VARIABILITY; SEED DEVELOPMENT; LIFE-HISTORY; LONG-TERM; RESPONSES; TRENDS; VEGETATION; DURATION;
D O I
10.1111/j.1365-2435.2009.01645.x
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
P> High alpine plants endure a cold climate with short growing seasons entailing severe consequences of an improper timing of development. Hence, their flowering phenology is expected to be rigorously controlled by climatic factors. We studied ten alpine plant species from habitats with early and late melting snow cover for 2 years and compared the synchronizing effect of temperature sums (TS), time of snowmelt (SM) and photoperiod (PH) on their flowering phenology. Intraseasonal and habitat-specific variation in the impact of these factors was analysed by comparing predictions of time-to-event models using linear mixed-effects models. Temperature was the overwhelming trigger of flowering phenology for all species. Its synchronizing effect was strongest at or shortly after flowering indicating the particular importance of phenological control of pollination. To some extent, this pattern masks the common trend of decreasing phenological responses to climatic changes from the beginning to the end of the growing season for lowland species. No carry-over effects were detected. As expected, the impact of photoperiod was weaker for snowbed species than for species inhabiting sites with early melting snow cover, while for temperature the reverse pattern was observed. Our findings provide strong evidence that alpine plants will respond quickly and directly to increasing temperature without considerable compensation due to photoperiodic control of phenology.
引用
收藏
页码:245 / 252
页数:8
相关论文
共 65 条
[1]  
ADLER W, 1994, EXKURSIONSFLORA VONO
[2]  
[Anonymous], 1999, Applied Survival Analysis: Time-to-Event
[3]  
Arft AM, 1999, ECOL MONOGR, V69, P491, DOI 10.1890/0012-9615(1999)069[0491:ROTPTE]2.0.CO
[4]  
2
[5]   Variations of snow depth and duration in the Swiss Alps over the last 50 years: Links to changes in large-scale climatic forcings [J].
Beniston, M .
CLIMATIC CHANGE, 1997, 36 (3-4) :281-300
[6]   Snow pack in the Swiss Alps under changing climatic conditions: an empirical approach for climate impacts studies [J].
Beniston, M ;
Keller, F ;
Goyette, S .
THEORETICAL AND APPLIED CLIMATOLOGY, 2003, 74 (1-2) :19-31
[7]   Shifting plant phenology in response to global change [J].
Cleland, Elsa E. ;
Chuine, Isabelle ;
Menzel, Annette ;
Mooney, Harold A. ;
Schwartz, Mark D. .
TRENDS IN ECOLOGY & EVOLUTION, 2007, 22 (07) :357-365
[8]   Phytophenological trends in Switzerland [J].
Defila, C ;
Clot, B .
INTERNATIONAL JOURNAL OF BIOMETEOROLOGY, 2001, 45 (04) :203-207
[9]  
Dunne JA, 2003, ECOL MONOGR, V73, P69, DOI 10.1890/0012-9615(2003)073[0069:SMFPRT]2.0.CO
[10]  
2