Functional shift in soil microbiome with decline in photosynthetic carbon input signifies rapid decrease of soil organic carbon during alpine grassland degradation

IF 5.1 1区 农林科学 Q1 SOIL SCIENCE
Minghua Song, Rui Pang, Yuqiang Tian, Yikang Li, Guiqiang Wang, Xingliang Xu
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Abstract

How photosynthetic carbon input regulates the microbial processes involved in carbon incorporation into soil organic carbon (SOC) and its stabilization during grassland degradation remains unclear. We utilized 13C to trace photosynthetic carbon incorporation into SOC and its pools, particulate (POC) and mineral-associated (MAOC) organic carbon, and carbon assimilation by soil microbes across five stages of alpine grassland degradation (S0, without grazing; S1, moderate grazing; S2–S4, light, moderate, and heavy degradation). As grassland approached S4, SOC in the top layer decreased by 53% compared with that in S3. A similar trend was observed in the middle and bottom soil layers, corresponding to a significant decrease in POC (decreased by 54, 40, and 35% in the top, middle and bottom layer, respectively) and carbon incorporation into POC (decreased by 83, 24, and 91% in the top, middle and bottom layer, respectively). A rapid decrease in MAOC was observed in S4, and carbon incorporation into MAOC decreased abruptly in the middle (10–20 cm) and bottom (20–30 cm) soil layers of S3. More than 57% of the incorporated carbon was concentrated in the top (0–10 cm) layers of S0-S4, whereas the middle and bottom layers of S3 and S4 exhibited nearly zero carbon incorporation. During degradation, fungal groups exhibited a downward trend in photosynthetic carbon assimilation, which was associated with their decreasing contribution to carbon incorporation into SOC. However, a relatively high proportion of bacteria participated in carbon assimilation at all soil depths at each stage, suggesting that more bacteria became active in decomposing the original SOC with decreasing carbon input. Our study successfully links aboveground and belowground processes which are crucial to comprehensively understand ecosystem responses to climate change and human activities.

随着光合碳输入的减少,土壤微生物组功能发生变化,表明高寒草地退化过程中土壤有机碳快速减少
在草地退化过程中,光合碳输入是如何调控土壤有机碳(SOC)转化及其稳定的微生物过程的,目前尚不清楚。我们利用13C追踪了高寒草地退化5个阶段(0,无放牧;S1,适度放牧;S2-S4,轻度、中度和重度降解)。当草地接近S4时,表层土壤有机碳比S3减少53%。中、底层土壤POC(顶层、中层和底层分别减少了54%、40%和35%)和POC碳含量(顶层、中层和底层分别减少了83%、24%和91%)均显著减少。S4土壤中MAOC含量快速下降,土壤中层(10 ~ 20 cm)和底层(20 ~ 30 cm) MAOC含碳量急剧下降。其中57%以上的碳集中在s0 ~ S4的顶层(0 ~ 10 cm),而S3和S4的中层和底层碳几乎为零。在降解过程中,真菌类群的光合碳同化呈下降趋势,这与它们对土壤有机碳的贡献减少有关。但各阶段各深度的细菌参与碳同化的比例均较高,说明随着碳输入的减少,细菌对原始有机碳的分解越来越活跃。我们的研究成功地将地上和地下过程联系起来,这对于全面了解生态系统对气候变化和人类活动的响应至关重要。
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
Biology and Fertility of Soils
Biology and Fertility of Soils 农林科学-土壤科学
CiteScore
11.80
自引率
10.80%
发文量
62
审稿时长
2.2 months
期刊介绍: Biology and Fertility of Soils publishes in English original papers, reviews and short communications on all fundamental and applied aspects of biology – microflora and microfauna - and fertility of soils. It offers a forum for research aimed at broadening the understanding of biological functions, processes and interactions in soils, particularly concerning the increasing demands of agriculture, deforestation and industrialization. The journal includes articles on techniques and methods that evaluate processes, biogeochemical interactions and ecological stresses, and sometimes presents special issues on relevant topics.
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