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Lithologic control of priming effect in subtropical forest

文献类型： 外文期刊

作者： Tang, Tiangang 1 ; Zhang, Qi 3 ; Fu, Ruitong 4 ; Duan, Pengpeng 1 ; Zhang, Yuling 4 ; Yang, Xinyi 1 ; Wang, Kelin 1 ; Li, Dejun 1 ;

作者机构： 1.Chinese Acad Sci, Inst Subtrop Agr, Key Lab Agroecol Proc Subtrop Reg, Changsha, Peoples R China

2.Chinese Acad Sci, Inst Subtrop Agr, Huanjiang Observat & Res Stn Karst Ecosyst, Huanjiang, Peoples R China

3.Jilin Acad Agr Sci, Agrobiotechnol Res Inst, 1363 Caiyu Ave, Changchun 130033, Peoples R China

4.Shenyang Agr Univ, Coll Land & Environm, Key Lab Arable Land Conservat Northeast China, Natl Engn Lab Efficient Utilizat Soil & Fertilizer, Shenyang 110866, Peoples R China

5.Guangxi Ind Technol Res Inst Karst Rocky Desertifi, Nanning 530012, Peoples R China

关键词： Priming effect; Lithologic; Mineral protection; C accessibility; Microbial properties

期刊名称：CATENA （ 影响因子：6.2； 五年影响因子：6.4 ）

ISSN： 0341-8162

年卷期： 2024 年 238 卷

页码：

收录情况： SCI

摘要： Lithology is a pivotal factor in controlling soil organic carbon (C) stabilization. The decomposition of soil organic matter can be potentiated by plant C inputs, a phenomenon termed the 'priming effect' (PE), which is a crucial yet highly unpredictable factor in soil C dynamics. However, our understanding of lithology's influence on soil PE remains scant. Here, we quantified soil priming effects in forest soils with different lithology (limestone and clastic rock). Our findings reveal a positive PE intensity in limestone soils, averaging at 0.34 +/- 0.28 mg CO2-C/g SOC. Conversely, clastic rock soils exhibited a negative PE intensity, averaging at -0.38 +/- 0.48 mg CO2-C-1 g SOC. Glucose amendment primed 189.2 % more organic C from the limestone soil than from the clastic rock. Greater PE intensity is associated with higher soil pH, exchangeable calcium/magnesium and lower short-range order iron/aluminum minerals, simple SOC chemical structures, lower iron- and calcium-associated C, dissolved organic C and fungi:bacteria ratio. Additionally, the magnitude and direction of priming effect was negatively correlated with the ratio of fungal to bacterial growth on glucose, and microbial C use efficiency, but correlated positively with total oxidative enzyme activity. Our results provide evidence that priming effects intensity is inherently dependent on lithology, carrying significant implications for refining C cycling models amid changing environmental conditions.

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