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Ecology of Nitrogen Fixing Nitrifying and Denitrifying Microorganisms in Tropical Forest Soils

机译:热带森林土壤中固氮反硝化和反硝化微生物的生态学

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摘要

Soil microorganisms play important roles in nitrogen cycling within forest ecosystems. Current research has revealed that a wider variety of microorganisms, with unexpected diversity in their functions and phylogenies, are involved in the nitrogen cycle than previously thought, including nitrogen-fixing bacteria, ammonia-oxidizing bacteria and archaea, heterotrophic nitrifying microorganisms, and anammox bacteria, as well as denitrifying bacteria, archaea, and fungi. However, the vast majority of this research has been focused in temperate regions, and relatively little is known regarding the ecology of nitrogen-cycling microorganisms within tropical and subtropical ecosystems. Tropical forests are characterized by relatively high precipitation, low annual temperature fluctuation, high heterogeneity in plant diversity, large amounts of plant litter, and unique soil chemistry. For these reasons, regulation of the nitrogen cycle in tropical forests may be very different from that of temperate ecosystems. This is of great importance because of growing concerns regarding the effect of land use change and chronic-elevated nitrogen deposition on nitrogen-cycling processes in tropical forests. In the context of global change, it is crucial to understand how environmental factors and land use changes in tropical ecosystems influence the composition, abundance and activity of key players in the nitrogen cycle. In this review, we synthesize the limited currently available information regarding the microbial communities involved in nitrogen fixation, nitrification and denitrification, to provide deeper insight into the mechanisms regulating nitrogen cycling in tropical forest ecosystems. We also highlight the large gaps in our understanding of microbially mediated nitrogen processes in tropical forest soils and identify important areas for future research.
机译:土壤微生物在森林生态系统内的氮循环中起重要作用。当前的研究表明,与以前认为的相比,氮循环涉及的微生物数量更多,其功能和系统发育具有意想不到的多样性,其中包括固氮细菌,氨氧化细菌和古细菌,异养硝化微生物和厌氧氨氧化细菌。 ,以及反硝化细菌,古细菌和真菌。然而,这项研究的绝大部分集中在温带地区,对于热带和亚热带生态系统中的氮循环微生物的生态学知之甚少。热带森林的特点是相对较高的降水量,较低的年温度波动,植物多样性的高度异质性,大量的植物凋落物以及独特的土壤化学性质。由于这些原因,热带森林中氮循环的调节可能与温带生态系统的调节有很大不同。这一点非常重要,因为人们日益关注土地利用变化和长期升高的氮沉降对热带森林中氮循环过程的影响。在全球变化的背景下,至关重要的是要了解热带生态系统中的环境因素和土地利用变化如何影响氮循环中关键参与者的组成,丰度和活动。在这篇综述中,我们综合了有关固氮,硝化和反硝化所涉及的微生物群落的有限的当前可用信息,以提供对调节热带森林生态系统中氮循环的机制的更深入的了解。我们还强调了我们对热带森林土壤中微生物介导的氮过程的认识方面的巨大差距,并确定了未来研究的重要领域。

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