Lichen biocrusts contribute to soil microbial biomass carbon in the northern temperate zone: A meta-analysis

IF 4 2区 农林科学 Q2 SOIL SCIENCE
Chang Tian, Chongfeng Bu, Shufang Wu, Kadambot H. M. Siddique
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Abstract

Biological soil crusts (biocrusts) have crucial ecological functions in dryland ecosystems, yet understanding the variations in soil microbial biomass within biocrusts across diverse ecosystems, climates and soil conditions remains limited. This knowledge gap constrains our understanding of how microbial communities within biocrusts regulate terrestrial carbon and nitrogen cycling. Hence, we conducted a meta-analysis using 255 paired observations from 42 study sites across the northern temperate ecosystem. The analysis revealed that biocrusts harbour significantly higher soil microbial biomass carbon and nitrogen (SMBC and SMBN, respectively) levels than bare (non-biocrust) soil across all habitat types. Notably, deeper soil layers (5–10 and >10 cm) accumulated less SMBC and SMBN than biocrust and biocrust–5-cm soil, revealing that biocrusts influence shallow soil environments. Ecosystem type, soil texture, depth and season emerged as key factors influencing the distribution of SMBC within biocrusts. Of particular interest, lichen biocrusts accumulated the most SMBC compared with other biocrust types. Furthermore, the difference in SMBC between biocrust and non-biocrust soils was more pronounced in oligotrophic habitats (e.g., desert, grassland, sand and sandy loam soils) than in eutrophic habitats (e.g., forest and loam soils). Random forest analysis confirmed that soil variables affected SMBC accumulation in biocrusts more than climatic factors. Soil organic carbon (SOC), as the primary source of SMBC, could be the most important determinant. Moreover, the disparity between non-biocrust SMBC and biocrust SMBC increased with increasing mean annual temperature (MAT) or decreasing altitude. These insights underscore the substantial contribution of lichen biocrusts to SMBC and emphasize the need to incorporate this knowledge into regional models for predicting the effects of climate change on soil carbon budgets within biocrust microbiomes in temperate ecosystems of the Northern Hemisphere.

地衣生物簇有助于增加北温带土壤微生物的生物量碳:荟萃分析
土壤生物结壳(生物结壳)在干旱地区的生态系统中具有重要的生态功能,但对不同生态系统、气候和土壤条件下生物结壳内土壤微生物生物量变化的了解仍然有限。这一知识空白限制了我们对生物簇内微生物群落如何调节陆地碳氮循环的理解。因此,我们利用北温带生态系统中 42 个研究地点的 255 个配对观测数据进行了荟萃分析。分析结果显示,在所有生境类型中,生物覆盖层的土壤微生物生物量碳和氮(SMBC 和 SMBN)水平明显高于裸露(非生物覆盖层)土壤。值得注意的是,较深的土层(5-10 厘米和 10 厘米)积累的 SMBC 和 SMBN 要少于生物覆盖层和生物覆盖层-5 厘米的土壤,这表明生物覆盖层会影响浅层土壤环境。生态系统类型、土壤质地、深度和季节是影响 SMBC 在生物覆盖层内分布的关键因素。尤其值得关注的是,与其他生物簇相比,地衣生物簇积累的 SMBC 最多。此外,与富营养化栖息地(如森林和壤土)相比,在低营养栖息地(如沙漠、草地、沙土和沙质壤土)中,生物簇与非生物簇之间的 SMBC 差异更为明显。随机森林分析证实,与气候因素相比,土壤变量对生物簇中 SMBC 积累的影响更大。土壤有机碳(SOC)作为 SMBC 的主要来源,可能是最重要的决定因素。此外,随着年平均气温(MAT)的升高或海拔的降低,非生物脆皮 SMBC 与生物脆皮 SMBC 之间的差异也会增大。这些见解强调了地衣生物群对SMBC的巨大贡献,并强调有必要将这一知识纳入区域模型,以预测气候变化对北半球温带生态系统生物群内土壤碳预算的影响。
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
European Journal of Soil Science
European Journal of Soil Science 农林科学-土壤科学
CiteScore
8.20
自引率
4.80%
发文量
117
审稿时长
5 months
期刊介绍: The EJSS is an international journal that publishes outstanding papers in soil science that advance the theoretical and mechanistic understanding of physical, chemical and biological processes and their interactions in soils acting from molecular to continental scales in natural and managed environments.
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