Bestelmeyer Brandon T, Ward Judy P, Havstad Kris M
USDA-ARS, Jornada Experimental Range and Jornada Basin LTER, MSC 3JER, Box 30003, New Mexico State University, Las Cruces, New Mexico 88003, USA.
Ecology. 2006 Apr;87(4):963-73. doi: 10.1890/0012-9658(2006)87[963:shgpvd]2.0.co;2.
Soil properties are well known to affect vegetation, but the role of soil heterogeneity in the patterning of vegetation dynamics is poorly documented. We asked whether the location of an ecotone separating grass-dominated and sparsely vegetated areas reflected only historical variation in degradation or was related to variation in inherent soil properties. We then asked whether changes in the cover and spatial organization of vegetated and bare patches assessed using repeat aerial photography reflected self-organizing dynamics unrelated to soil variation or the stable patterning of soil variation. We found that the present-day ecotone was related to a shift from more weakly to more strongly developed soils. Parts of the ecotone were stable over a 60-year period, but shifts between bare and vegetated states, as well as persistently vegetated and bare states, occurred largely in small (<40 m2) patches throughout the study area. The probability that patches were presently vegetated or bare, as well as the probability that vegetation persisted and/or established over the 60-year period, was negatively related to surface calcium carbonate and positively related to subsurface clay content. Thus, only a fraction of the landscape was susceptible to vegetation change, and the sparsely vegetated area probably featured a higher frequency of susceptible soil patches. Patch dynamics and self-organizing processes can be constrained by subtle (and often unrecognized) soil heterogeneity.
土壤性质对植被的影响广为人知,但土壤异质性在植被动态格局形成中的作用却鲜有文献记载。我们探究了分隔草地为主和植被稀疏区域的生态交错带的位置,是仅反映了历史退化差异,还是与土壤固有性质的差异有关。接着,我们又探究了利用重复航空摄影评估的植被覆盖区和裸地斑块的覆盖度及空间组织变化,是反映了与土壤变化无关的自组织动态,还是土壤变化的稳定格局。我们发现,现今的生态交错带与土壤从发育较弱向发育较强的转变有关。生态交错带的部分区域在60年期间保持稳定,但在整个研究区域内,裸地和植被状态之间的转变,以及持续的植被和裸地状态,大多发生在小面积(<40平方米)的斑块中。斑块当前为植被覆盖或裸地的概率,以及植被在60年期间持续存在和/或形成的概率,与地表碳酸钙呈负相关,与地下黏土含量呈正相关。因此,只有一部分景观易发生植被变化,植被稀疏区域可能具有更高频率的易受影响土壤斑块。斑块动态和自组织过程可能受到细微(且常未被认识到)的土壤异质性的限制。