热带洪泛区树木覆盖的决定因素

J. H. Daskin, F. Aires, A. Staver
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引用次数: 7

摘要

树木覆盖将森林与稀树草原和草原区分开来。在热带洪泛区,尽管洪泛区覆盖了热带陆地的10%,但人们对区分这些系统的因素知之甚少。季节性洪水可能给树木带来挑战(土壤缺氧)和益处(水分和养分沉积),其相对重要性可能取决于生态环境,例如,洪水是否在更干旱的生态系统中更能缓解水压力。在这里,我们利用五大洲13个大型热带和亚热带洪泛区生态系统的遥感数据表明,气候水平衡(即降水潜在蒸散)与洪水、火灾和地形的相互作用强烈地增加了洪泛区的树木覆盖。正如预测的那样,洪水增加了干旱洪泛区的树木覆盖率,但减少了气候湿润的洪泛区的树木覆盖率。与高地一样,频繁的火灾减少了树木覆盖,特别是在潮湿地区,但与高地相反,低海拔和沙质土壤减少了树木覆盖。我们的研究结果表明,预测气候、土地利用和水文变化对洪泛平原生态系统的影响取决于考虑气候干扰的相互作用。在全球范围内进行湿地转换的同时,额外的人为活动,包括火灾频率的改变和大坝建设,也将改变洪泛区的树木覆盖,特别是在潮湿气候下。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Determinants of tree cover in tropical floodplains
Tree cover differentiates forests from savannas and grasslands. In tropical floodplains, factors differentiating these systems are poorly known, even though floodplains cover 10% of the tropical landmass. Seasonal inundation potentially presents trees with both challenges (soil anoxia) and benefits (moisture and nutrient deposition), the relative importance of which may depend on ecological context, e.g. if floods alleviate water stress more in more arid ecosystems. Here, we use remotely sensed data across 13 large tropical and sub-tropical floodplain ecosystems on five continents to show that climatic water balance (i.e. precipitation—potential evapotranspiration) strongly increases floodplain tree cover in interaction with flooding, fire and topography. As predicted, flooding increases tree cover in more arid floodplains, but decreases tree cover in climatically wetter ones. As in uplands, frequent fire reduced tree cover, particularly in wet regions, but—in contrast with uplands—lower elevation and sandier soils decreased tree cover. Our results suggest that predicting the impacts of changing climate, land use and hydrology on floodplain ecosystems depends on considering climate-disturbance interactions. While outright wetland conversion proceeds globally, additional anthropogenic activities, including alteration of fire frequencies and dam construction, will also shift floodplain tree cover, especially in wet climates.
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