Root trait controls on rhizosphere priming effects during early-stage litter decomposition in anoxic peat

IF 4.3 3区 环境科学与生态学 Q2 ENVIRONMENTAL SCIENCES
Biogeochemistry Pub Date : 2026-10-03 Epub Date: 2026-10-07 DOI:10.1007/s10533-026-01373-5
Namid Krüger, Maxim Dorodnikov, Simon Thomsen, Klaus-Holger Knorr, Peter Mueller
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Abstract

Litter represents the transitional stage between plant biomass and soil organic carbon, with its transformation influenced by overlying vegetation. Plant regulation of litter decomposition through priming effects in wetlands represents an important knowledge gap, as roots influence rhizosphere processes differently than in upland soils by releasing both exudates and oxygen into the otherwise water-saturated, oxygen-depleted soil matrix. To investigate the role of plants in rhizosphere priming in anoxic wetlands, two sedge species with contrasting belowground traits (rhizomatous vs. tussock-forming) were grown on uniformly carbon-13-labeled litter in waterlogged peat in a greenhouse microcosm experiment. Litter-derived respiration affected by sedge roots was quantified using a two-end-member mixing model. Rhizosphere enzyme activities were mapped using zymography, while oxygen and carbon dioxide (CO2) dynamics were visualized using planar optode imaging. Litterbag mass loss was determined gravimetrically. Cumulative litter-derived CO2 respiration was 87% higher under rhizomatous Eriophorum angustifolium and 106% higher under tussock-forming E. vaginatum than in the unplanted treatment, whereas litter mass loss was only 10 and 19% higher in the planted treatments, respectively. Initial positive priming effects of > + 200% declined to negative priming of < − 20% within 3 months in both planted treatments. In both species, β-glucosidase activity was elevated around mature roots, while acid phosphatase activity was elevated across the entire root system compared with background levels. Our study provides experimental evidence that sedges enhance early-stage litter decomposition in anoxic peat regardless of their belowground morphological traits, likely through root oxygen loss and stimulation of rhizosphere enzyme activity.

缺氧泥炭凋落物早期分解过程中根性状对根际启动效应的控制
凋落物是植物生物量与土壤有机碳之间的过渡阶段,其转化受上覆植被的影响。湿地植物通过启动效应调节凋落物分解,这是一个重要的知识缺口,因为根系通过向水分饱和、缺氧的土壤基质释放渗出物和氧气来影响根际过程,这与陆地土壤不同。为了研究缺氧湿地中植物在根际诱导中的作用,在温室微观环境试验中,将两种具有不同地下性状(根状生长和丛状生长)的莎草种在浸水泥炭中均匀碳-13标记的凋落物上。采用双端元混合模型量化了莎草根对凋落物源呼吸作用的影响。根际酶活性用酶谱法绘制,氧和二氧化碳(co2)动态用平面光电成像可视化。用重量法测定了垃圾袋的质量损失。与未种植处理相比,根生枇杷处理的累积凋落物来源CO 2呼吸量高87%,而植生枇杷处理的累积凋落物来源CO 2呼吸量高106%,而凋落物质量损失仅比未种植处理高10%和19%。两种处理的初始正启动效应在3个月内下降到负启动效应的<; - 20%。在这两个物种中,β-葡萄糖苷酶活性在成熟根周围升高,而酸性磷酸酶活性在整个根系中升高,与背景水平相比。我们的研究提供了实验证据,证明无论其地下形态特征如何,莎草都可能通过根氧损失和刺激根际酶活性来促进缺氧泥炭的早期凋落物分解。
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来源期刊
Biogeochemistry
Biogeochemistry 环境科学-地球科学综合
CiteScore
7.10
自引率
5.00%
发文量
112
审稿时长
3.2 months
期刊介绍: Biogeochemistry publishes original and synthetic papers dealing with biotic controls on the chemistry of the environment, or with the geochemical control of the structure and function of ecosystems. Cycles are considered, either of individual elements or of specific classes of natural or anthropogenic compounds in ecosystems. Particular emphasis is given to coupled interactions of element cycles. The journal spans from the molecular to global scales to elucidate the mechanisms driving patterns in biogeochemical cycles through space and time. Studies on both natural and artificial ecosystems are published when they contribute to a general understanding of biogeochemistry.
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