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土壤质地调节非洲热带稀树草原树木对降雨强度的响应。

Soil texture mediates tree responses to rainfall intensity in African savannas.

机构信息

Department of Ecology and Evolutionary Biology, Yale University, 165 Prospect St, New Haven, CT, 06511, USA.

出版信息

New Phytol. 2018 Sep;219(4):1363-1372. doi: 10.1111/nph.15254. Epub 2018 Jun 4.

Abstract

Rainfall variability is a major determinant of soil moisture, but its influence on vegetation structure has been challenging to generalize. This presents a major source of uncertainty in predicting vegetation responses to potentially widespread shifts in rainfall frequency and intensity. In savannas, where trees and grasses coexist, conflicting lines of evidence have suggested, variously, that tree cover can either increase or decrease in response to less frequent, more intense rainfall. Here, we use remote sensing products and continent-wide soil maps for sub-Saharan Africa to analyze how soil texture and fire mediate the response of savanna tree cover to rainfall climatology. Tree cover increased with mean wet-season rainfall and decreased with fire frequency, consistent with previous analyses. However, responses to rainfall intensity varied: tree cover dramatically decreased with rainfall intensity on clayey soils, at high rainfall, and with rainfall spread over longer wet seasons; conversely, on sandy soils, at low rainfall, and with shorter wet seasons, tree cover instead increased with rainfall intensity. Tree cover responses to rainfall climatology depend on soil texture, accounting for substantial variation in tree cover across African savannas. Differences in underlying soils may lead to divergent responses of savannas to global change.

摘要

降雨变率是土壤湿度的主要决定因素,但它对植被结构的影响很难概括。这是预测植被对降雨频率和强度潜在广泛变化的响应时的一个主要不确定性来源。在稀树草原中,树木和草共存,各种相互矛盾的证据表明,树木覆盖度可能会随着降雨量减少和强度增加而增加或减少。在这里,我们使用撒哈拉以南非洲的遥感产品和全大陆土壤图来分析土壤质地和火灾如何调节稀树草原树木覆盖度对降雨气候的响应。树木覆盖度随湿季平均降雨量增加而增加,随火灾频率降低而增加,这与之前的分析一致。然而,对降雨强度的响应却有所不同:在粘土地上,在高降雨量和降雨持续时间较长的湿季,树木覆盖度随降雨强度显著降低;相反,在沙质土壤上,在降雨量较低和湿季较短的情况下,树木覆盖度反而随降雨强度增加而增加。树木覆盖度对降雨气候的响应取决于土壤质地,这解释了非洲稀树草原上树木覆盖度的巨大变化。基础土壤的差异可能导致稀树草原对全球变化的反应不同。

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