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热带洪泛区的树木覆盖的决定因素。

Determinants of tree cover in tropical floodplains.

机构信息

Department of Ecology and Evolutionary Biology, Yale University, Osborn Memorial Laboratories, 165 Prospect Street, New Haven, CT 06511, USA.

Yale Institute for Biospheric Studies, Yale University, New Haven, CT 06520, USA.

出版信息

Proc Biol Sci. 2019 Nov 6;286(1914):20191755. doi: 10.1098/rspb.2019.1755. Epub 2019 Oct 30.

Abstract

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.

摘要

森林、草原和稀树草原的区别在于树冠层的覆盖度。在热带洪泛区,尽管这些系统覆盖了热带陆地面积的 10%,但区分这些系统的因素却鲜为人知。季节性洪水可能给树木带来挑战(土壤缺氧)和好处(水分和养分沉积),其相对重要性可能取决于生态背景,例如,在更干旱的生态系统中,洪水是否能更有效地缓解水分胁迫。在这里,我们使用跨五大洲 13 个大型热带和亚热带洪泛区生态系统的遥感数据,表明气候水分平衡(即降水-潜在蒸散)与洪水、火灾和地形的相互作用强烈影响洪泛区的树木覆盖度。正如预测的那样,洪水增加了干旱洪泛区的树木覆盖度,但减少了湿润洪泛区的树木覆盖度。与高地一样,频繁的火灾减少了树木覆盖度,尤其是在湿润地区,但与高地不同的是,较低的海拔和更沙质的土壤减少了树木覆盖度。我们的研究结果表明,预测气候变化、土地利用和水文学对洪泛区生态系统的影响取决于对气候干扰相互作用的考虑。虽然全球范围内湿地的净转化仍在继续,但包括改变火灾频率和修建水坝在内的额外人为活动也将改变洪泛区的树木覆盖度,特别是在湿润气候条件下。

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