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Linkage between temperature sensitivity of SOM decomposition and microbial communities depends on soil fractions
Global Change Biology ( IF 10.8 ) Pub Date : 2024-08-07 , DOI: 10.1111/gcb.17456 Shuqi Qin 1, 2 , Kai Fang 1, 3, 4 , Yutong Song 1, 2, 5 , Luyao Kang 1, 2, 5 , Siyu Wang 1, 2, 5 , Yuanhe Yang 1, 2, 5
Global Change Biology ( IF 10.8 ) Pub Date : 2024-08-07 , DOI: 10.1111/gcb.17456 Shuqi Qin 1, 2 , Kai Fang 1, 3, 4 , Yutong Song 1, 2, 5 , Luyao Kang 1, 2, 5 , Siyu Wang 1, 2, 5 , Yuanhe Yang 1, 2, 5
Affiliation
The magnitude of terrestrial carbon (C)‐climate feedback largely depends on the temperature sensitivity of soil organic matter (SOM) decomposition (Q 10 ). However, our understanding of determinants of Q 10 for SOM fractions such as particulate and mineral‐associated organic matter (POM and MAOM, respectively) is still inadequate. Particularly, it remains unclear whether microbial effects on Q 10 are fraction‐dependent, which induces large uncertainties in projecting soil C dynamics. Here, we conducted large‐scale topsoil sampling on the Tibetan Plateau, in combination with SOM fractionation and 300‐day laboratory incubation to assess SOM fraction‐dependent linkages between Q 10 and microbial properties. We found that compared with MAOM, POM had larger Q 10 and greater microbial diversity, and also structured distinct microbial communities as well as their co‐occurrence patterns. Furthermore, associations of Q 10 with microbial properties differed between the two SOM fractions. Bacterial community composition and relative abundance of bacterial keystone taxa affected Q 10 for POM and MAOM respectively, while bacterial alpha diversity showed opposite relationships with Q 10 for POM and MAOM. These findings highlight the necessity of incorporating SOM fraction‐dependent microbial properties and their linkages with Q 10 into Earth system models to accurately predict terrestrial C‐climate feedback.
中文翻译:
SOM 分解的温度敏感性与微生物群落之间的联系取决于土壤成分
陆地碳(C)-气候反馈的大小很大程度上取决于土壤有机质(SOM)分解的温度敏感性(问10 )。然而,我们对决定因素的理解问10对于颗粒物和矿物相关有机物(分别为 POM 和 MAOM)等 SOM 组分的分析仍然不足。特别是,目前尚不清楚微生物是否会影响问10是分数相关的,这在预测土壤碳动态时产生很大的不确定性。在这里,我们在青藏高原进行了大规模表土采样,结合 SOM 分馏和 300 天的实验室培养,以评估 SOM 分数依赖性之间的联系问10和微生物特性。我们发现,与MAOM相比,POM具有更大的问10和更大的微生物多样性,并且还构建了不同的微生物群落及其共现模式。此外,协会问10两种 SOM 组分之间的微生物特性不同。受影响的细菌群落组成和细菌关键类群的相对丰度问10分别为 POM 和 MAOM,而细菌 α 多样性与问10对于 POM 和 MAOM。这些发现强调了纳入 SOM 分数依赖性微生物特性及其与问10进入地球系统模型以准确预测陆地气候反馈。
更新日期:2024-08-07
中文翻译:
SOM 分解的温度敏感性与微生物群落之间的联系取决于土壤成分
陆地碳(C)-气候反馈的大小很大程度上取决于土壤有机质(SOM)分解的温度敏感性(问10 )。然而,我们对决定因素的理解问10对于颗粒物和矿物相关有机物(分别为 POM 和 MAOM)等 SOM 组分的分析仍然不足。特别是,目前尚不清楚微生物是否会影响问10是分数相关的,这在预测土壤碳动态时产生很大的不确定性。在这里,我们在青藏高原进行了大规模表土采样,结合 SOM 分馏和 300 天的实验室培养,以评估 SOM 分数依赖性之间的联系问10和微生物特性。我们发现,与MAOM相比,POM具有更大的问10和更大的微生物多样性,并且还构建了不同的微生物群落及其共现模式。此外,协会问10两种 SOM 组分之间的微生物特性不同。受影响的细菌群落组成和细菌关键类群的相对丰度问10分别为 POM 和 MAOM,而细菌 α 多样性与问10对于 POM 和 MAOM。这些发现强调了纳入 SOM 分数依赖性微生物特性及其与问10进入地球系统模型以准确预测陆地气候反馈。