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凋落物输入降低了两种亚热带森林土壤中土壤有机质分解对增温的响应。

Litter input decreased the response of soil organic matter decomposition to warming in two subtropical forest soils.

机构信息

Key Laboratory of Forest Ecology and Management, Institute of Applied Ecology, Chinese Academy of Sciences, Shenyang 110164, P. R. China.

Huitong Experimental Station of Forest Ecology, Chinese Academy of Sciences, Huitong 418307, P.R. China.

出版信息

Sci Rep. 2016 Sep 20;6:33814. doi: 10.1038/srep33814.

Abstract

Interaction effect of temperature and litter input on SOM decomposition is poor understood, restricting accurate prediction of the dynamics and stocks of soil organic carbon under global warming. To address this knowledge gap, we conducted an incubation experiment by adding (13)C labeled leaf-litter into a coniferous forest (CF) soil and a broadleaved forest (BF) soil. In this experiment, response of the temperature sensitivity (Q10) of SOM decomposition to the increase in litter input was investigated. The temperature dependences of priming effect (PE) and soil microbial community were analyzed. The Q10 for CF soil significantly decreased from 2.41 in no-litter treatment to 2.05 in litter-added treatment and for BF soil from 2.14 to 1.82, suggesting that litter addition decreases the Q10. PE in the CF soil was 24.9% at 20 °C and 6.2% at 30 °C, and in the BF soil the PE was 8.8% at 20 °C and -7.0% at 30 °C, suggesting that PE decreases with increasing temperature. Relative PE was positively related to the concentrations of Gram-negative bacterial and fungal PLFAs. This study moves a step forward in understanding warming effect on forest carbon cycling by highlighting interaction effect of litter input and warming on soil carbon cycling.

摘要

温度和凋落物输入对土壤有机质分解的相互作用影响理解较差,限制了对全球变暖下土壤有机碳动态和储量的准确预测。为了解决这一知识空白,我们通过向针叶林(CF)土壤和阔叶林(BF)土壤中添加(13)C 标记的叶凋落物来进行培养实验。在这个实验中,我们研究了土壤有机质分解的温度敏感性(Q10)对凋落物输入增加的响应。分析了激发效应(PE)和土壤微生物群落对温度的依赖性。CF 土壤的 Q10 从无凋落物处理的 2.41 显著降低到添加凋落物处理的 2.05,BF 土壤的 Q10 从 2.14 降低到 1.82,表明凋落物添加降低了 Q10。CF 土壤在 20°C 时的激发效应为 24.9%,在 30°C 时为 6.2%,BF 土壤在 20°C 时为 8.8%,在 30°C 时为-7.0%,表明激发效应随温度升高而降低。相对激发效应与革兰氏阴性菌和真菌 PLFA 的浓度呈正相关。本研究通过强调凋落物输入和升温对土壤碳循环的相互作用影响,在理解升温对森林碳循环的影响方面前进了一步。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8ec7/5028766/130aef442723/srep33814-f1.jpg

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