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Soil-geomorphic heterogeneity governs patchy vegetation dynamics at an arid ecotone

机译:土壤-地貌异质性决定了干旱交错带的斑块植被动态

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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 m(2)) 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.
机译:众所周知,土壤特性会影响植被,但是土壤异质性在植被动态格局中的作用却鲜有记载。我们询问将草丛为主和稀疏植被区分开的过渡带的位置是否仅反映了退化的历史变化或与土壤固有特性的变化有关。然后,我们询问是否通过重复评估植被和裸露斑块的覆盖度和空间组织的变化航空摄影反映了与土壤变化或土壤变化的稳定模式无关的自组织动力学。我们发现当今的过渡带与从较弱的土壤向较发达的土壤转变有关。过渡带的某些部分在60年的时间内是稳定的,但是裸露和植被状态之间的转换以及永久性植被和裸露状态的变化主要发生在整个研究区域的小片(<40 m(2))斑块中。目前植被被植被覆盖或裸露的概率,以及植被在60年间持续存在和/或建立的概率与地表碳酸钙呈负相关,与地下粘土含量呈正相关。因此,只有一小部分景观易受植被变化的影响,而植被稀疏的地区可能具有较高的易感土壤斑块频率。斑块的动态变化和自组织过程可能受到微妙的(通常是无法识别的)土壤异质性的限制。

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