ECOLAB, Université de Toulouse, CNRS, Toulouse, France.
Géosciences Environnement Toulouse (GET), Université de Toulouse, CNRS, IRD, UPS, Toulouse, France.
Glob Chang Biol. 2018 Jun;24(6):2633-2648. doi: 10.1111/gcb.14059. Epub 2018 Feb 11.
Following 25 years of below average annual rainfall in the Sahel between 1970 and 1995, the return to more humid conditions has led to rapid postdrought recovery of the woody cover. However, the increase in the woody cover is not spatially homogeneous raising questions about the resilience of some woody vegetation types. Based on the analysis of field and remote sensing data collected on the tiger bush systems in the northern Sahel in Mali, this study noted the current and persistent degradation of these systems in the Sahel since the 1970s despite the recent improvement in rainfall since the mid-1990s and the general Sahel re-greening. Profound changes in the woody population pattern, tree density and cover, and floristic composition took place regardless of the site location along the south-north rainfall gradient. Associated with definite structural changes of the woody population, surface hydrology shifted from a sheet to concentrated run-off accelerating the collapse of the patterned woody population. Currently, there is no evidence in favour of reversing the current degradation process, at least at a decadal scale, although very sparse recolonization by pioneer woody vegetation has been observed in the driest sites along recently formed gullies. These observations support the hypothesis of an ecosystem shift, with long-term implications for the structure and functioning of the patterned vegetation, as well as the whole watershed landscape through increased run-off leading to stronger water flows in enlarged wadis, increased soil erosion upstream and sediment deposition downstream, enhanced water storage in ponds, and greater recharge of aquifers, which is an illustration of the "Sahelian paradox".
在 1970 年至 1995 年期间,萨赫勒地区经历了 25 年低于平均水平的年降雨量,随后气候转为更加湿润,导致木本植被迅速从干旱中恢复。然而,木本植被的增加并不是空间均匀的,这引发了人们对一些木本植被类型弹性的质疑。本研究基于在马里萨赫勒北部采集的实地和遥感数据的分析,指出自 20 世纪 70 年代以来,尽管自 20 世纪 90 年代中期以来降雨量有所改善,整个萨赫勒地区重新绿化,但这些系统仍在持续退化。无论在沿南北降雨梯度的哪个位置,木本种群模式、树木密度和覆盖度以及植物区系组成都发生了深刻的变化。与木本种群的明确结构变化相关的是,地表水文从片状径流转变为集中径流,加速了模式化木本种群的崩溃。目前,至少在十年的时间尺度上,没有证据表明当前的退化过程正在逆转,尽管在最近形成的沟壑中最干旱的地方已经观察到了先锋木本植被的稀疏再殖民化。这些观察结果支持了生态系统转变的假设,这对模式化植被的结构和功能以及整个流域景观都有长期影响,因为增加的径流量导致水流增强,在扩大的干谷中上游土壤侵蚀加剧,下游泥沙沉积增加,池塘储水增加,含水层补给增加,这说明了“萨赫勒悖论”。