大气二氧化碳浓度升高对稻田甲烷排放及相关微生物过程影响的研究进展。

Q3 Environmental Science
Mao-Hui Tian, Li-Dong Shen, Wei-Ci Su
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引用次数: 0

摘要

稻田被认为是甲烷(CH4)的重要排放源,在全球气候变化中起着举足轻重的作用。大气中二氧化碳(CO2)浓度(e[CO2])的升高对稻田的碳循环产生了深远的影响。了解 e[CO2] 对 CH4 排放的影响以及潜在的微生物过程,对于加强稻田固碳和减少排放至关重要。我们回顾了 e[CO2] 对水稻田中 CH4 排放的影响,重点研究了与碳循环相关的微生物的活性、丰度、群落结构和多样性。我们还描述了在 e[CO2] 条件下各种微生物过程在减缓 CH4 排放中的作用,以及主要的环境决定因素。总之,e[CO2]实验平台的类型、熏蒸持续时间、浓度梯度和二氧化碳富集方法都会影响水稻田的甲烷排放。e[CO2]最初会刺激甲烷排放,但随着时间的推移可能会减少,这表明甲烷排放微生物群落对 e[CO2] 的适应性很强。这种反应表现出一种趋势,即开始时会减弱,随后对 CH4 排放的积极影响会加强。二氧化碳浓度突然增加的实验可能会高估甲烷的排放量。e[CO2]对微生物过程的影响主要表现为甲烷菌、好氧和厌氧甲烷营养体的活性和丰度增强。它极大地改变了养甲烷生物群落的组成和多样性,而对甲烷菌和厌氧养甲烷生物群落的影响则微乎其微。最后,我们概述了未来的研究方向:1)综合研究 e[CO2] 对水稻田中 CH4 排放、甲烷生成以及好氧和厌氧养甲烷菌的影响,可以阐明气候变化对 CH4 排放的影响机制;2)长期研究对于更准确、更真实地了解 e[CO2] 对 CH4 排放及相关微生物过程的影响机制至关重要;3)有必要开展多尺度(时间和空间)、多因子(二氧化碳浓度、温度、大气氮沉降和水管理措施)和多方法(观测、数据和模型集成)的研究,以有效减少评估未来气候变化情景下稻田中 CH4 排放及相关微生物过程对 e[CO2] 的响应的不确定性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Research progress on the effects of elevated atmospheric CO2 concentration on CH4 emission and related microbial processes in paddy fields.

Paddy fields are recognized as significant sources of methane (CH4) emissions, playing a pivotal role in global climate change. Elevated atmospheric carbon dioxide (CO2) concentrations (e[CO2]) exert a profound influence on the carbon cycling of paddy fields. Understanding the effects of e[CO2] on CH4 emissions, as well as the underlying microbial processes, is crucial for enhancing carbon sequestration and reducing emissions in paddy fields. We reviewed the impacts of e[CO2] on CH4 emission in paddy fields, focusing on the activity, abundance, community structure, and diversity of carbon-cycling-related microbes. We also delineated the roles of various microbial processes in mitigating CH4 emissions under e[CO2], as well as the primary environmental determinants. Overall, the type of e[CO2] experimental platforms, duration of fumigation, concentration gradients, and the methods of CO2 enrichment all influence CH4 emissions from paddy fields. e[CO2] initially stimulates CH4 emissions, which may decrease over time, indicating an adaptability of the methane-emitting microbial community to e[CO2]. This response exhibits a trend of initial attenuation followed by an intensification of the positive effects on CH4 emissions. Experiments with abrupt increase of CO2 concentration might overestimate CH4 emissions. The impact of e[CO2] on microbial processes is predominantly characterized by enhanced activities and abundance of methanogens, aerobic and anaerobic methanotrophs. It significantly alters the community composition and diversity of methanotrophs, with minimal effects on methanogens and anaerobic methanotrophic communities. Finally, we outlined future research directions: 1) Integrated investigations into the effects of e[CO2] on CH4 emissions, methanogenesis, and both aerobic and anaerobic methanotrophs in paddy fields could elucidate the mechanisms underlying the impacts of climate change on CH4 emissions; 2) Long-term studies are essential to understand the mechanisms of e[CO2] on CH4 emissions and associated microbial processes more accurately and realistically; 3) Multi-scale (temporal and spatial), multi-factorial (CO2 concentration, temperature, atmospheric nitrogen deposition, and water management practices), and multi-methodological (observational, data, and model integration) research is necessary to effectively reduce the uncertainties in assessing the response of CH4 emissions in paddy fields and related microbial processes to e[CO2] under future climate change scenarios.

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应用生态学报
应用生态学报 Environmental Science-Ecology
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