Sensitivity of three grassland communities to simulated extreme temperature and rainfall events

被引:81
|
作者
White, TA
Campbell, BD
Kemp, PD
Hunt, CL
机构
[1] AgResearch, Grassland Res Ctr, Palmerston North, New Zealand
[2] Massey Univ, Inst Nat Resources, Palmerston North, New Zealand
关键词
C3; C4; diversity; extreme climatic events; global climate change; stability;
D O I
10.1046/j.1365-2486.2000.00344.x
中图分类号
X176 [生物多样性保护];
学科分类号
090705 ;
摘要
Three grassland communities in New Zealand with differing climates and proportions of C3 and C4 species were subjected to one-off extreme heating (eight hours at 52.5 degrees C) and rainfall (the equivalent of 100 mm) events. A novel experimental technique using portable computer-controlled chambers simulated the extreme heating events. The productive, moist C3/C4 community was the most sensitive to the extreme events in terms of short-term community composition compared with a dry C3/C4 community or an exclusively C3 community. An extreme heating event caused the greatest change to plant community species abundance by favouring the expansion of C4 species relative to C3 species, shifting C4 species abundance from 43% up to 84% at the productive, moist site, This was observed both in the presence and absence of added water. In the absence of C4 species, heating reduced community productivity by over 60%. The short-term shifts in the abundance of C3 and C4 species in response to the single extreme climatic events did not have persistent effects on community structure or on soil nitrogen one year later. There was no consistent relationship between diversity and stability of biomass production of these plant communities, and species functional identity was the most effective explanation for the observed shifts in biomass production. The presence of C4 species resulted in an increased stability of productivity after extreme climatic events, but resulted in greater overall. shifts in community composition. The presence of C4 species may buffer grassland community productivity against an increased frequency of extreme heating events associated with future global climate change.
引用
收藏
页码:671 / 684
页数:14
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