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在哥斯达黎加热带雨林的恢复过程中,固氮作用和森林生长的演替动态。

Successional dynamics of nitrogen fixation and forest growth in regenerating Costa Rican rainforests.

机构信息

Smithsonian Environmental Research Center, 647 Contees Wharf Road, Edgewater, Maryland, 21037, USA.

Department of Ecology and Evolutionary Biology, University of Connecticut, Storrs, Connecticut, 06269, USA.

出版信息

Ecology. 2019 Apr;100(4):e02637. doi: 10.1002/ecy.2637. Epub 2019 Mar 8.

Abstract

Regenerating tropical forests have an immense capacity to capture carbon and harbor biodiversity. The recuperation of the nitrogen cycle following disturbance can fuel biomass regeneration, but few studies have evaluated the successional dynamics of nitrogen and nitrogen inputs in tropical forests. We assessed symbiotic and asymbiotic nitrogen fixation, soil inorganic nitrogen concentrations, and tree growth in a well-studied series of five tropical forest plots ranging from 19 yr in age to old-growth forests. Wet-season soil inorganic nitrogen concentrations were high in all plots, peaking in the 29-yr-old plot. Inputs from symbiotic nitrogen fixation declined through succession, while asymbiotic nitrogen fixation peaked in the 37-yr-old plot. Consequently, the dominant nitrogen fixation input switched from symbiotic fixation in the younger plots to asymbiotic fixation in the older plots. Tree growth was highest in the youngest plots and declined through succession. Interestingly, symbiotic nitrogen fixation was negatively correlated with the basal area of nitrogen-fixing trees across our study plots, highlighting the danger in using nitrogen-fixing trees as a proxy for rates of symbiotic nitrogen fixation. Our results demonstrate that the nitrogen cycle has largely recuperated by 19 yr following disturbance, allowing for rapid biomass regeneration at our site. This work provides important insight into the sources and dynamics of nitrogen that support growth and carbon capture in regenerating Neotropical forests.

摘要

再生热带森林具有巨大的碳捕获能力和生物多样性庇护能力。干扰后氮循环的恢复可以促进生物量再生,但很少有研究评估过热带森林中氮和氮输入的演替动态。我们评估了 5 个热带森林样地中一系列从 19 年生到成熟林的样地中的共生和非共生固氮、土壤无机氮浓度和树木生长情况。所有样地在雨季的土壤无机氮浓度都很高,在 29 年生的样地中达到峰值。共生固氮的输入随着演替而减少,而非共生固氮在 37 年生的样地中达到峰值。因此,主要的固氮输入从年轻样地中的共生固氮转变为老年样地中的非共生固氮。树木生长在最年轻的样地中最高,并随着演替而下降。有趣的是,共生固氮与我们研究样地中固氮树木的基部面积呈负相关,这凸显了将固氮树木用作共生固氮率的替代指标的危险。我们的研究结果表明,干扰后 19 年内氮循环已经基本恢复,使得我们的地点能够快速进行生物量再生。这项工作为支持再生新热带森林生长和碳捕获的氮来源和动态提供了重要的见解。

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