School of Geosciences, University of Edinburgh, Crew Building, Kings Buildings, Edinburgh, EH9 3FF, United Kingdom.
Smithsonian Tropical Research Institute, 0843-03092, Balboa, Ancon, Panama.
Ecology. 2018 Nov;99(11):2455-2466. doi: 10.1002/ecy.2482. Epub 2018 Oct 26.
More than 200 years ago, Alexander von Humboldt reported that tropical plant species richness decreased with increasing elevation and decreasing temperature. Surprisingly, coordinated patterns in plant, bacterial, and fungal diversity on tropical mountains have not yet been observed, despite the central role of soil microorganisms in terrestrial biogeochemistry and ecology. We studied an Andean transect traversing 3.5 km in elevation to test whether the species diversity and composition of tropical forest plants, soil bacteria, and fungi follow similar biogeographical patterns with shared environmental drivers. We found coordinated changes with elevation in all three groups: species richness declined as elevation increased, and the compositional dissimilarity among communities increased with increased separation in elevation, although changes in plant diversity were larger than in bacteria and fungi. Temperature was the dominant driver of these diversity gradients, with weak influences of edaphic properties, including soil pH. The gradients in microbial diversity were strongly correlated with the activities of enzymes involved in organic matter cycling, and were accompanied by a transition in microbial traits towards slower-growing, oligotrophic taxa at higher elevations. We provide the first evidence of coordinated temperature-driven patterns in the diversity and distribution of three major biotic groups in tropical ecosystems: soil bacteria, fungi, and plants. These findings suggest that interrelated and fundamental patterns of plant and microbial communities with shared environmental drivers occur across landscape scales. These patterns are revealed where soil pH is relatively constant, and have implications for tropical forest communities under future climate change.
200 多年前,亚历山大·冯·洪堡(Alexander von Humboldt)曾报道,随着海拔的升高和温度的降低,热带植物物种丰富度会降低。令人惊讶的是,尽管土壤微生物在陆地生物地球化学和生态学中起着核心作用,但在热带山脉上,植物、细菌和真菌多样性的协调模式尚未被观察到。我们研究了一条沿安第斯山脉的横断带,海拔跨度为 3.5 公里,以测试热带森林植物、土壤细菌和真菌的物种多样性和组成是否遵循类似的生物地理模式,并具有共同的环境驱动因素。我们发现所有三组的物种多样性都随着海拔的升高而协调变化:随着海拔的升高,物种丰富度下降,群落之间的组成差异随着海拔的升高而增加,尽管植物多样性的变化大于细菌和真菌。温度是这些多样性梯度的主要驱动因素,土壤特性(包括土壤 pH)的影响较弱。微生物多样性的梯度与参与有机质循环的酶的活性密切相关,并且伴随着微生物特征在较高海拔向生长缓慢、贫营养的分类群的转变。我们提供了第一个证据,证明了热带生态系统中三个主要生物群(土壤细菌、真菌和植物)的多样性和分布存在协调的温度驱动模式。这些发现表明,与环境驱动因素相关的植物和微生物群落的相互关联和基本模式在景观尺度上发生。这些模式在土壤 pH 相对稳定的情况下显现出来,并对未来气候变化下的热带森林群落产生影响。