Borden Kira A, Mafa-Attoye Tolulope G, Dunfield Kari E, Thevathasan Naresh V, Gordon Andrew M, Isaac Marney E
Faculty of Land and Food Systems, The University of British Columbia, Vancouver, BC, Canada.
Centre for Sustainable Food Systems, The University of British Columbia, Vancouver, BC, Canada.
Front Plant Sci. 2021 Jul 8;12:681113. doi: 10.3389/fpls.2021.681113. eCollection 2021.
Predicting respiration from roots and soil microbes is important in agricultural landscapes where net flux of carbon from the soil to the atmosphere is of large concern. Yet, in riparian agroecosystems that buffer aquatic environments from agricultural fields, little is known on the differential contribution of CO sources nor the systematic patterns in root and microbial communities that relate to these emissions. We deployed a field-based root exclusion experiment to measure heterotrophic and autotrophic-rhizospheric respiration across riparian buffer types in an agricultural landscape in southern Ontario, Canada. We paired bi-weekly measurements of in-field CO flux with analysis of soil properties and fine root functional traits. We quantified soil microbial community structure using qPCR to estimate bacterial and fungal abundance and characterized microbial diversity using high-throughput sequencing. Mean daytime total soil respiration rates in the growing season were 186.1 ± 26.7, 188.7 ± 23.0, 278.6 ± 30.0, and 503.4 ± 31.3 mg CO-C m h in remnant coniferous and mixed forest, and rehabilitated forest and grass buffers, respectively. Contributions of autotrophic-rhizospheric respiration to total soil CO fluxes ranged widely between 14 and 63% across the buffers. Covariation in root traits aligned roots of higher specific root length and nitrogen content with higher specific root respiration rates, while microbial abundance in rhizosphere soil coorindated with roots that were thicker in diameter and higher in carbon to nitrogen ratio. Variation in autotrophic-rhizospheric respiration on a soil area basis was explained by soil temperature, fine root length density, and covariation in root traits. Heterotrophic respiration was strongly explained by soil moisture, temperature, and soil carbon, while multiple factor analysis revealed a positive correlation with soil microbial diversity. This is a first in-field study to quantify root and soil respiration in relation to trade-offs in root trait expression and to determine interactions between root traits and soil microbial community structure to predict soil respiration.
在土壤向大气的碳净通量备受关注的农业景观中,通过根系和土壤微生物预测呼吸作用十分重要。然而,在缓冲农田与水生环境的河岸农业生态系统中,人们对二氧化碳来源的差异贡献以及与这些排放相关的根系和微生物群落的系统模式知之甚少。我们在加拿大安大略省南部的一个农业景观中开展了一项基于田间的根系排除实验,以测量不同河岸缓冲类型中的异养和自养根际呼吸作用。我们每两周对田间二氧化碳通量进行一次测量,并分析土壤性质和细根功能性状。我们使用定量聚合酶链反应(qPCR)来估计细菌和真菌丰度,从而量化土壤微生物群落结构,并使用高通量测序来表征微生物多样性。在生长季节,残留针叶林和混交林、恢复林和草地缓冲带的平均日间土壤总呼吸速率分别为186.1±26.7、188.7±23.0、278.6±30.0和503.4±31.3毫克二氧化碳 - 碳每平方米每小时。自养根际呼吸对土壤总二氧化碳通量的贡献在各缓冲带中差异很大,范围在14%至63%之间。根系性状的协变表明,具有较高比根长和氮含量的根系具有较高的比根呼吸速率,而根际土壤中的微生物丰度与直径较粗、碳氮比更高的根系相关。基于土壤面积的自养根际呼吸变化可由土壤温度、细根长度密度和根系性状的协变来解释。异养呼吸则主要由土壤湿度、温度和土壤碳含量来解释,而多因素分析表明其与土壤微生物多样性呈正相关。这是第一项在田间量化根系和土壤呼吸与根系性状表达权衡关系,并确定根系性状与土壤微生物群落结构之间相互作用以预测土壤呼吸的研究。