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首页> 外文期刊>Plant and Soil >Linking soil process and microbial ecology in freshwater wetland ecosystems.
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Linking soil process and microbial ecology in freshwater wetland ecosystems.

机译:将土壤过程与淡水湿地生态系统中的微生物生态学联系起来。

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摘要

Soil microorganisms mediate many processes such as nitrification, denitrification, and methanogenesis that regulate ecosystem functioning and also feed back to influence atmospheric chemistry. These processes are of particular interest in freshwater wetland ecosystems where nutrient cycling is highly responsive to fluctuating hydrology and nutrients and soil gas releases may be sensitive to climate warming. In this review we briefly summarize research from process and taxonomic approaches to the study of wetland biogeochemistry and microbial ecology, and highlight areas where further research is needed to increase our mechanistic understanding of wetland system functioning. Research in wetland biogeochemistry has most often been focused on processes (e.g., methanogenesis), and less often on microbial communities or on populations of specific microorganisms of interest. Research on process has focused on controls over, and rates of, denitrification, methanogenesis, and methanotrophy. There has been some work on sulfate and iron transformations and wetland enzyme activities. Work to date indicates an important process level role for hydrology and soil nutrient status. The impact of plant species composition on processes is potentially critical, but is as yet poorly understood. Research on microbial communities in wetland soils has primarily focused on bacteria responsible for methanogenesis, denitrification, and sulfate reduction. There has been less work on taxonomic groups such as those responsible for nitrogen fixation, or aerobic processes such as nitrification. Work on general community composition and on wetland mycorrhizal fungi is particularly sparse. The general goal of microbial research has been to understand how microbial groups respond to the environment. There has been relatively little work done on the interactions among environmental controls over process rates, environmental constraints on microbial activities and community composition, and changes in processes at the ecosystem level. Finding ways to link process-based and biochemical or gene-based assays is becoming increasingly important as we seek a mechanistic understanding of the response of wetland ecosystems to current and future anthropogenic perturbations. We discuss the potential of new approaches, and highlight areas for further research..
机译:土壤微生物介导许多过程,例如硝化,反硝化和产甲烷作用,这些过程调节生态系统的功能并反馈给大气化学。这些过程在淡水湿地生态系统中特别令人关注,在该生态系统中,养分循环对水文变化起着高度响应作用,养分和土壤气体释放可能对气候变暖敏感。在这篇综述中,我们简要总结了从过程和分类学方法到湿地生物地球化学和微生物生态学研究的研究,并重点介绍了需要进一步研究以增强我们对湿地系统功能的机械理解的领域。湿地生物地球化学的研究通常集中在过程(例如甲烷生成)上,而很少集中在微生物群落或感兴趣的特定微生物种群上。工艺研究集中于反硝化,甲烷生成和甲烷氧化作用的控制及其速率。在硫酸盐和铁的转化以及湿地酶活性方面已有一些工作。迄今为止的工作表明了水文和土壤养分状况的重要过程水平作用。植物物种组成对过程的影响可能至关重要,但至今知之甚少。湿地土壤中微生物群落的研究主要集中在负责甲烷生成,反硝化和硫酸盐还原的细菌。分类组的工作较少,例如负责固氮或需氧过程(例如硝化)的那些。有关一般社区组成和湿地菌根真菌的工作特别少。微生物研究的总体目标是了解微生物群如何对环境做出反应。关于过程速率的环境控制,微生物活动和群落组成的环境限制以及生态系统一级过程的变化之间的相互作用的研究相对较少。随着我们寻求对湿地生态系统对当前和未来人为干扰的响应的机械理解,寻找将基于过程的检测与基于生物化学或基于基因的检测联系起来的方法变得越来越重要。我们讨论了新方法的潜力,并强调了需要进一步研究的领域。

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