Facilitation among plants in alpine environments in the face of climate change

被引:121
作者
Anthelme, Fabien [1 ,2 ]
Cavieres, Lohengrin A. [3 ,4 ]
Dangles, Olivier [5 ,6 ]
机构
[1] IRD, UMR AMAP, Blvd Lironde,TA A 51-PS2, F-34398 Montpellier 5, France
[2] Univ Mayor San Andres, Inst Ecol, La Paz, Bolivia
[3] Univ Concepcion, Dept Bot, Fac Ciencias Nat & Oceanog, Concepcion, Chile
[4] Inst Ecol & Biodiversidad, Santiago, Chile
[5] Ctr Natl Rech Sci, Inst Rech Dev, Lab Evolut Genomes & Speciat, UR 072,UPR 9034, Gif Sur Yvette, France
[6] Univ Paris Sud 11, Orsay, France
关键词
competition; cushion plants; early snowmelt; facilitation; latitudinal gradient; nurse plant; stress-gradient hypothesis; global warming; STRESS-GRADIENT HYPOTHESIS; ATMOSPHERIC NITROGEN DEPOSITION; POSITIVE SPECIES INTERACTIONS; BIOTIC INTERACTIONS; PRIMARY SUCCESSION; CUSHION PLANT; RANGE SHIFTS; TROPICAL ANDES; GLOBAL CHANGE; LIFE-FORMS;
D O I
10.3389/fpls.2014.00387
中图分类号
Q94 [植物学];
学科分类号
071001 ;
摘要
While there is a large consensus that plantplant interactions are a crucial component of the response of plant communities to the effects of climate change, available data remain scarce, particularly in alpine systems. This represents an important obstacle to making consistent predictions about the future of plant communities. Here, we review current knowledge on the effects of climate change on facilitation among alpine plant communities and propose directions for future research. In established alpine communities, while warming seemingly generates a net facilitation release, earlier snowmelt may increase facilitation. Some nurse plants are able to buffer microenvironmental changes in the long term and may ensure the persistence of other alpine plants through local migration events. For communities migrating to higher elevations, facilitation should play an important role in their reorganization because of the harsher environmental conditions. In particular, the absence of efficient nurse plants might slow down upward migration, possibly generating chains of extinction. Facilitationclimate change relationships are expected to shift along latitudinal gradients because (1) the magnitude of warming is predicted to vary along these gradients, and (2) alpine environments are significantly different at low vs. high latitudes. Data on these expected patterns are preliminary and thus need to be tested with further studies on facilitation among plants in alpine environments that have thus far not been considered. From a methodological standpoint, future studies will benefit from the spatial representation of the microclimatic environment of plants to predict their response to climate change. Moreover, the acquisition of long-term data on the dynamics of plantplant interactions, either through permanent plots or chronosequences of glacial recession, may represent powerful approaches to clarify the relationship between plant interactions and climate change.
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页数:15
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