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硅影响草原植物的化学计量以及碳、氮和磷的积累。

Silicon Affects Plant Stoichiometry and Accumulation of C, N, and P in Grasslands.

作者信息

Hao Qian, Yang Shilei, Song Zhaoliang, Li Zichuan, Ding Fan, Yu Changxun, Hu Guozheng, Liu Hongyan

机构信息

Institute of Surface-Earth System Science, School of Earth System Science, Tianjin University, Tianjin, China.

Key Laboratory of Recycling and Eco-treatment of Waste Biomass of Zhejiang Province, Zhejiang University of Science and Technology, Hangzhou, China.

出版信息

Front Plant Sci. 2020 Aug 27;11:1304. doi: 10.3389/fpls.2020.01304. eCollection 2020.

Abstract

Silicon (Si) plays an important role in improving soil nutrient availability and plant carbon (C) accumulation and may therefore impact the biogeochemical cycles of C, nitrogen (N), and phosphorus (P) in terrestrial ecosystems profoundly. However, research on this process in grassland ecosystems is scarce, despite the fact that these ecosystems are one of the most significant accumulators of biogenic Si (BSi). In this study, we collected the aboveground parts of four widespread grasses and soil profile samples in northern China and assessed the correlations between Si concentrations and stoichiometry and accumulation of C, N, and P in grasses at the landscape scale. Our results showed that Si concentrations in plants were significantly negatively correlated ( < 0.01) with associated C concentrations. There was no significant correlation between Si and N concentrations. It is worth noting that since the Si concentration increased, the P concentration increased from less than 0.10% to more than 0.20% and therefore C:P and N:P ratios decreased concomitantly. Besides, the soil noncrystalline Si played more important role in C, N, and P accumulation than other environmental factors (e.g., MAT, MAP, and altitude). These findings indicate that Si may facilitate grasses in adjusting the utilization of nutrients (C, N, and P) and may particularly alleviate P deficiency in grasslands. We conclude that Si positively alters the concentrations and accumulation of C, N, and P likely resulting in the variation of ecological stoichiometry in both vegetation and litter decomposition in soils. This study further suggests that the physiological function of Si is an important but overlooked factor in influencing biogeochemical cycles of C and P in grassland ecosystems.

摘要

硅(Si)在提高土壤养分有效性和植物碳(C)积累方面发挥着重要作用,因此可能对陆地生态系统中碳、氮(N)和磷(P)的生物地球化学循环产生深远影响。然而,尽管草原生态系统是生物源硅(BSi)最重要的积累者之一,但关于该过程在草原生态系统中的研究却很少。在本研究中,我们采集了中国北方四种常见草类的地上部分和土壤剖面样本,并在景观尺度上评估了硅浓度与化学计量以及草类中碳、氮和磷积累之间的相关性。我们的结果表明,植物中的硅浓度与相关碳浓度呈显著负相关(<0.01)。硅与氮浓度之间没有显著相关性。值得注意的是,随着硅浓度的增加,磷浓度从低于0.10%增加到高于0.20%,因此碳磷比和氮磷比也随之降低。此外,土壤非晶质硅在碳、氮和磷积累方面比其他环境因素(如年均气温、年均降水量和海拔)发挥着更重要的作用。这些发现表明,硅可能有助于草类调节养分(碳、氮和磷)的利用,尤其可能缓解草原的磷缺乏。我们得出结论,硅正向改变碳、氮和磷的浓度和积累,可能导致植被和土壤凋落物分解中生态化学计量的变化。本研究进一步表明,硅的生理功能是影响草原生态系统中碳和磷生物地球化学循环的一个重要但被忽视的因素。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/9e05/7493684/1c101430882d/fpls-11-01304-g001.jpg

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