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湿地甲烷排放的隐藏根源。

The hidden roots of wetland methane emissions.

作者信息

Määttä Tiia, Malhotra Avni

机构信息

Department of Geography, University of Zürich, Zürich, Switzerland.

Biological Sciences Division, Pacific Northwest National Laboratory, Richland, Washington, USA.

出版信息

Glob Chang Biol. 2024 Feb;30(2):e17127. doi: 10.1111/gcb.17127.

DOI:10.1111/gcb.17127
PMID:38337165
Abstract

Wetlands are the largest natural source of methane (CH ) globally. Climate and land use change are expected to alter CH emissions but current and future wetland CH budgets remain uncertain. One important predictor of wetland CH flux, plants, play an important role in providing substrates for CH -producing microbes, increasing CH consumption by oxygenating the rhizosphere, and transporting CH from soils to the atmosphere. Yet, there remain various mechanistic knowledge gaps regarding the extent to which plant root systems and their traits influence wetland CH emissions. Here, we present a novel conceptual framework of the relationships between a range of root traits and CH processes in wetlands. Based on a literature review, we propose four main CH -relevant categories of root function: gas transport, carbon substrate provision, physicochemical influences and root system architecture. Within these categories, we discuss how individual root traits influence CH production, consumption, and transport (PCT). Our findings reveal knowledge gaps concerning trait functions in physicochemical influences, and the role of mycorrhizae and temporal root dynamics in PCT. We also identify priority research needs such as integrating trait measurements from different root function categories, measuring root-CH linkages along environmental gradients, and following standardized root ecology protocols and vocabularies. Thus, our conceptual framework identifies relevant belowground plant traits that will help improve wetland CH predictions and reduce uncertainties in current and future wetland CH budgets.

摘要

湿地是全球最大的甲烷(CH₄)天然来源。气候和土地利用变化预计会改变CH₄排放,但当前及未来的湿地CH₄收支仍不确定。湿地CH₄通量的一个重要预测因子——植物,在为产CH₄微生物提供底物、通过根际充氧增加CH₄消耗以及将CH₄从土壤输送到大气方面发挥着重要作用。然而,关于植物根系及其性状在多大程度上影响湿地CH₄排放,仍存在各种机制方面的知识空白。在此,我们提出了一个关于湿地一系列根系性状与CH₄过程之间关系的全新概念框架。基于文献综述,我们提出了与CH₄相关的根系功能的四个主要类别:气体运输、碳底物供应、物理化学影响和根系结构。在这些类别中,我们讨论了个体根系性状如何影响CH₄的产生、消耗和运输(PCT)。我们的研究结果揭示了在物理化学影响方面性状功能、菌根在PCT中的作用以及根系动态变化方面的知识空白。我们还确定了优先研究需求,例如整合来自不同根系功能类别的性状测量、沿环境梯度测量根系与CH₄的联系,以及遵循标准化的根系生态学协议和术语。因此,我们的概念框架确定了相关的地下植物性状,这将有助于改进湿地CH₄预测,并减少当前及未来湿地CH₄收支的不确定性。

相似文献

1
The hidden roots of wetland methane emissions.湿地甲烷排放的隐藏根源。
Glob Chang Biol. 2024 Feb;30(2):e17127. doi: 10.1111/gcb.17127.
2
Soil properties and sediment accretion modulate methane fluxes from restored wetlands.土壤特性和沉积物累积调节了湿地修复后的甲烷通量。
Glob Chang Biol. 2018 Sep;24(9):4107-4121. doi: 10.1111/gcb.14124. Epub 2018 Apr 10.
3
Plant-mediated CH exchange in wetlands: A review of mechanisms and measurement methods with implications for modelling.湿地植物介导的 CH 交换:机制与测量方法综述及其对模型化的影响。
Sci Total Environ. 2024 Mar 1;914:169662. doi: 10.1016/j.scitotenv.2023.169662. Epub 2023 Dec 28.
4
Climatic zone effects of non-native plant invasion on CH and NO emissions from natural wetland ecosystems.外来植物入侵对天然湿地生态系统CH和NO排放的气候带效应。
Sci Total Environ. 2024 Jan 1;906:167855. doi: 10.1016/j.scitotenv.2023.167855. Epub 2023 Oct 14.
5
The positive net radiative greenhouse gas forcing of increasing methane emissions from a thawing boreal forest-wetland landscape.不断增加的甲烷排放对北极森林湿地景观导致的正净辐射温室气体强迫。
Glob Chang Biol. 2017 Jun;23(6):2413-2427. doi: 10.1111/gcb.13520. Epub 2016 Oct 26.
6
Non-native plant invasion can accelerate global climate change by increasing wetland methane and terrestrial nitrous oxide emissions.外来植物入侵会通过增加湿地甲烷和陆地氧化亚氮排放加速全球气候变化。
Glob Chang Biol. 2022 Sep;28(18):5453-5468. doi: 10.1111/gcb.16290. Epub 2022 Jun 19.
7
The role of oxygen in stimulating methane production in wetlands.氧气在刺激湿地甲烷产生中的作用。
Glob Chang Biol. 2021 Nov;27(22):5831-5847. doi: 10.1111/gcb.15831. Epub 2021 Aug 18.
8
Methane emissions partially offset carbon sink function in global wetlands: An analysis based on global data.甲烷排放部分抵消了全球湿地的碳汇功能:基于全球数据的分析
Ying Yong Sheng Tai Xue Bao. 2023 Nov;34(11):2958-2968. doi: 10.13287/j.1001-9332.202311.006.
9
Identifying dominant environmental predictors of freshwater wetland methane fluxes across diurnal to seasonal time scales.确定淡水湿地甲烷通量在昼夜到季节时间尺度上的主要环境预测因子。
Glob Chang Biol. 2021 Aug;27(15):3582-3604. doi: 10.1111/gcb.15661. Epub 2021 May 29.
10
Climate-driven increase of natural wetland methane emissions offset by human-induced wetland reduction in China over the past three decades.过去三十年来,中国因气候变化导致的自然湿地甲烷排放量增加,而人为减少湿地导致的排放量减少。
Sci Rep. 2016 Nov 28;6:38020. doi: 10.1038/srep38020.

引用本文的文献

1
Greenhouse Gas Mitigation Potential of Temperate Fen Paludicultures.温带沼泽地水产养殖的温室气体减排潜力
Glob Chang Biol. 2025 Aug;31(8):e70385. doi: 10.1111/gcb.70385.
2
Variations in Ecosystem-Scale Methane Fluxes Across a Boreal Mire Complex Assessed by a Network of Flux Towers.通过通量塔网络评估北方泥炭沼复合体生态系统尺度甲烷通量的变化
Glob Chang Biol. 2025 May;31(5):e70223. doi: 10.1111/gcb.70223.
3
Rising Water Levels and Vegetation Shifts Drive Substantial Reductions in Methane Emissions and Carbon Dioxide Uptake in a Great Lakes Coastal Freshwater Wetland.
水位上升和植被变化导致五大湖沿岸淡水湿地的甲烷排放量大幅减少和二氧化碳吸收量下降。
Glob Chang Biol. 2025 Feb;31(2):e70053. doi: 10.1111/gcb.70053.
4
Fate of methane in canals draining tropical peatlands.热带泥炭地排水渠中甲烷的命运。
Nat Commun. 2024 Nov 11;15(1):9766. doi: 10.1038/s41467-024-54063-x.
5
Belowground plant allocation regulates rice methane emissions from degraded peat soils.地下植物分配调节退化泥炭地水稻甲烷排放。
Sci Rep. 2024 Jun 25;14(1):14593. doi: 10.1038/s41598-024-64616-1.