Evidence for the Coupling of Plant Functional Diversity and Soil Biogeochemistry Under Climatic Stress in Pacific Northwest Grasslands

IF 3.7 3区 环境科学与生态学 Q2 ENVIRONMENTAL SCIENCES
Barbara Bomfim, Hilary R. Dawson, Paul B. Reed, Katherine L. Shek, Brendan J. M. Bohannan, Scott D. Bridgham, Lucas C. R. Silva
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Abstract

Increasing warming and drought severity are projected for the Pacific Northwest (PNW) and are expected to negatively impact species composition and ecosystem function. In this study, we test the hypothesis that the impact of climatic stress (i.e., experimental warming and drought) on PNW grasslands are mediated by interactions between plant functional diversity and soil biogeochemical processes, including symbiotic nitrogen (N) fixation in legumes and free-living asymbiotic nitrogen fixation (ANF) by soil microorganisms. To test this hypothesis, we measured the response of plants and soils to three years of warming (+2.5°C) and drought (−40% precipitation) in field experiments replicated at three different sites across a ∼520-km latitudinal gradient. We observed interactive effects of warming and drought on functional diversity and soil biogeochemical properties, including both positive and negative changes in ANF. Although direct measurements of symbiotic nitrogen fixation (SNF) rates were not conducted, the observed variations in ANF, in conjunction with changes in legume cover, suggest a compensatory mechanism that may offset reductions in SNF. Generally, high ANF rates coincided with low legume cover, suggesting a connection between shifts in species composition and N cycling. Our ANF estimates were performed using isotopically labeled dinitrogen (15N2) in tandem with soil carbon (C), phosphorus (P) and iron (Fe), pH, and moisture content. Along the latitudinal drought severity gradient, ANF rates were correlated with changes in species composition and soil N, P, moisture, and pH levels. These results highlight the importance of soil-plant-atmosphere interactions in understanding the impacts of climatic stress on ecosystem composition and function.

气候胁迫下西北太平洋草原植物功能多样性与土壤生物地球化学耦合的证据
预计太平洋西北地区(PNW)的变暖和干旱程度将加剧,并将对物种组成和生态系统功能产生负面影响。在本研究中,我们验证了气候胁迫(即实验升温和干旱)对PNW草原的影响是由植物功能多样性和土壤生物地球化学过程(包括豆科植物的共生固氮(N)和土壤微生物的自由生活非共生固氮(ANF))之间的相互作用介导的。为了验证这一假设,我们测量了植物和土壤对三年变暖(+2.5°C)和干旱(- 40%降水)的响应,在三个不同的地点重复了在约520公里的纬度梯度。研究发现,增温和干旱对土壤功能多样性和生物地球化学性质的交互影响,包括土壤土壤养分的正、负变化。虽然没有进行共生固氮速率的直接测量,但观察到的共生固氮速率的变化,以及豆科植物覆盖的变化,表明存在一种补偿机制,可以抵消共生固氮速率的减少。一般来说,高ANF率与低豆科植物覆盖相一致,表明物种组成的变化与N循环之间存在联系。我们使用同位素标记的二氮(15N2)与土壤碳(C)、磷(P)和铁(Fe)、pH和水分含量进行了ANF估算。沿干旱严重程度的纬度梯度,ANF率与物种组成和土壤N、P、水分和pH水平的变化相关。这些结果强调了土壤-植物-大气相互作用对理解气候胁迫对生态系统组成和功能的影响的重要性。
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来源期刊
Journal of Geophysical Research: Biogeosciences
Journal of Geophysical Research: Biogeosciences Earth and Planetary Sciences-Paleontology
CiteScore
6.60
自引率
5.40%
发文量
242
期刊介绍: JGR-Biogeosciences focuses on biogeosciences of the Earth system in the past, present, and future and the extension of this research to planetary studies. The emerging field of biogeosciences spans the intellectual interface between biology and the geosciences and attempts to understand the functions of the Earth system across multiple spatial and temporal scales. Studies in biogeosciences may use multiple lines of evidence drawn from diverse fields to gain a holistic understanding of terrestrial, freshwater, and marine ecosystems and extreme environments. Specific topics within the scope of the section include process-based theoretical, experimental, and field studies of biogeochemistry, biogeophysics, atmosphere-, land-, and ocean-ecosystem interactions, biomineralization, life in extreme environments, astrobiology, microbial processes, geomicrobiology, and evolutionary geobiology
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