Graminoids Increase Greenhouse Gas Emissions From Thawed Permafrost at the End of the Growing Season

IF 12.5 1区 环境科学与生态学 Q1 BIODIVERSITY CONSERVATION
Marie Mollenkopf, Katja Lenge, Sören Drabesch, Sylvain Monteux, Sigrid van Grinsven, Prachi Joshi, Ellen Dorrepaal, Birgit Wild, Andreas Kappler, E. Marie Muehe
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引用次数: 0

Abstract

Amplified Arctic warming can induce strong ecosystem changes with adverse climate feedbacks through greenhouse gas (GHG) release. Shifting plant species and traits with permafrost thaw may contribute to the permafrost carbon feedback. How vegetation dynamics in thawing permafrost systems affect GHG release and how this varies with season, plant species, and soil conditions is poorly understood. Here, we assessed GHG emissions, redox potentials, and geochemical signatures as well as the carbon input in the form of root exudation along a vegetation density gradient and a permafrost thaw gradient over a growing season in Stordalen mire, Sweden. Ecosystem respiration and CH4 emissions increased along the thaw gradient from bog to fen, possibly due to high graminoid root carbon release rates into an anoxic soil, fuelling fast organic matter oxidation and lowering redox potentials to enhance methanogenesis. CH4 emissions increased seven-fold with increasing graminoid cover compared to non-vascular plant controls in the thawed soil. Plants may mediate CH4 transport, which was responsible for 80% of the graminoid-induced increase in CH4 emissions in the bog environment. In the fen environment, graminoid root carbon release stimulated CH4 formation, which dominated by contributing 70% of the graminoid-induced increase. Overall, photosynthesis-related CO2 fixation was substantial in the early and peak growing season, but when expressed as CO2 equivalents, CH4 release offset this uptake, resulting in net positive radiative forcings from graminoid-vegetated thawed soils throughout the growing season. Graminoids increased the net CO2-equivalent flux up to 8.9-fold compared to non-vascular plant locations with the strongest forcing toward late season in graminoid-vegetated fens. Our study showcases how fine-scaled, plant-mediated processes differently contribute to GHG emissions across a thawed bog and fen soil and how the time of growing season can overprint these effects to determine whether the system is a net GHG source or sink.

Abstract Image

禾本科植物在生长季节结束时增加了融化的永久冻土的温室气体排放。
放大的北极变暖可以引起强烈的生态系统变化,并通过温室气体(GHG)释放产生不利的气候反馈。随着冻土融化,植物种类和性状的变化可能有助于冻土碳反馈。冻土融化系统中的植被动态如何影响温室气体释放,以及这种影响如何随季节、植物种类和土壤条件而变化,人们知之甚少。在这里,我们评估了瑞典斯托达伦沼泽一个生长季节的温室气体排放、氧化还原电位和地球化学特征,以及沿植被密度梯度和永久冻土融化梯度以根分泌物形式输入的碳。生态系统呼吸和CH4排放沿从沼泽到沼泽的融化梯度增加,可能是由于禾本科根碳向缺氧土壤的高释放速率,促进了有机物的快速氧化,降低了氧化还原电位,从而促进了甲烷的生成。与非维管植物对照相比,解冻土壤中禾草覆盖增加,CH4排放量增加7倍。植物可能介导CH4运输,这是沼泽环境中80%由禾草素引起的CH4排放增加的原因。在沼泽环境中,禾本科植物的根碳释放促进了CH4的形成,占禾本科植物诱导增加的70%。总的来说,光合作用相关的CO2固定在生长季节的早期和高峰是大量的,但当以CO2当量表示时,CH4释放抵消了这种吸收,导致整个生长季节来自禾草类植被融化土壤的净正辐射强迫。禾本科植物使净co2当量通量比非维管束植物增加了8.9倍,禾本科植物对后期的强迫作用最强。我们的研究展示了精细尺度的、植物介导的过程如何对融化的沼泽和沼泽土壤中的温室气体排放做出不同的贡献,以及生长季节的时间如何叠加这些影响,以确定该系统是温室气体的净源还是汇。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Global Change Biology
Global Change Biology 环境科学-环境科学
CiteScore
21.50
自引率
5.20%
发文量
497
审稿时长
3.3 months
期刊介绍: Global Change Biology is an environmental change journal committed to shaping the future and addressing the world's most pressing challenges, including sustainability, climate change, environmental protection, food and water safety, and global health. Dedicated to fostering a profound understanding of the impacts of global change on biological systems and offering innovative solutions, the journal publishes a diverse range of content, including primary research articles, technical advances, research reviews, reports, opinions, perspectives, commentaries, and letters. Starting with the 2024 volume, Global Change Biology will transition to an online-only format, enhancing accessibility and contributing to the evolution of scholarly communication.
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