Microbial Effects on Elements Migration in Rock-Soil-Paeonia Szechuanica System

Feng Weina; Peng Peihao; Xie Chengsheng; Luo Wen

doi:10.13961/j.cnki.stbctb.2020.04.010

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Microbial Effects on Elements Migration in Rock-Soil-Paeonia Szechuanica System

- Microbial Effects on Elements Migration in Rock-Soil-Paeonia Szechuanica System
- Bulletin of Soiland Water Conservation Vol. 40, Issue 4, Pages: 67-74(2020)
- 作者机构：
  
  成都理工大学地球科学学院,四川,成都,610059
- 作者简介：
- 基金信息：
- DOI：10.13961/j.cnki.stbctb.2020.04.010
  CLC： S151.9
- Published：2020
- 稿件说明：
移动端阅览
Feng Weina, Peng Peihao, Xie Chengsheng, et al. Microbial Effects on Elements Migration in Rock-Soil-Paeonia Szechuanica System[J]. Bulletin of Soiland Water Conservation, 2020, 40(4): 67-74.
DOI：

Feng Weina, Peng Peihao, Xie Chengsheng, et al. Microbial Effects on Elements Migration in Rock-Soil-Paeonia Szechuanica System[J]. Bulletin of Soiland Water Conservation, 2020, 40(4): 67-74. DOI： 10.13961/j.cnki.stbctb.2020.04.010.

摘要

[目的] 研究四川牡丹岩土环境背景以及微生物在元素迁移过程中的作用，为了解营养元素的表生地球化学行为规律及微生物在元素迁移体系中的作用提供理论依据。[方法] 利用ICP-OES测定四川牡丹生境母岩、土壤以及种子的大量（P，S，K，Ca，Na，Mg，Al）、微量（Fe，Mn，Cu）营养元素含量，同时利用Illumina高通量测序技术测定根际土壤中细菌、真菌的组成和结构。[结果] ①四川牡丹生长土壤以弱碱富钙为主要特征，元素组成基本保留了母岩特征；②元素从母岩到土壤中的迁移富集系数排序为：Ca > Na > S > P > Mg > K > Al > Fe > Mn > Cu，植物吸收系数排序为：P > S > K > Cu > Mg > Ca > Na > Mn > Fe > Al；③碱土金属淋溶率和铝铁率对土壤细菌的多样性（Alpha）影响显著，但对真菌的影响不显著；④P，Mn的迁移主要受母岩控制，而Ca，Mg，Fe，S等元素的迁移富集受到了微生物的影响。[结论] 细菌和真菌在元素迁移体系中的作用相似，主要参与Fe，S，Mg，Ca的相关反应过程。

Abstract

[Objective] The environmental background of parent rock and soil of Paeonia szechuanica was studied in order to provide a theoretical reference for understanding the supergene geochemical behavior of nutrient elements and the role of microorganisms in elements migration. [Methods] The contents of nutrient elements (P

Cu) in the parent rocks

soil and the seeds of Paeonia szechuanica were measured by using ICP-OES. Meanwhile

the composition and structure of bacteria and fungi in the rhizosphere microorganisms were analyzed by using the Illumina platform. [Results] ① The soil of Paeonia szechuanica was characterized by alkalescence and rich calcium

and the element composition basically retained the characteristics of parent rock. ② The migration coefficients of elements migration from rocks into soil were listed as: Ca > Na > S > P > Mg > K > Al > Fe > Mn > Cu

and the absorption coefficients were listed as: P > S > K > Cu > Mg > Ca > Na > Mn > Fe > Al. ③ The leaching index of alkali metals and the ratio of Al to Fe shwowed a significant effect on soil bacterial diversity (Alpha)

but not on fungi. ④ The migrations of P and Mn were mianly controlled by the parent rock

while the migrations of Fe

and Ca were affected by microorganisms. [Conclusion] The bacteria and fungi play similar roles in the elements migration system and mainly involve in the reaction process of Fe

Ca and Mg.

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references

Richter D D, Billings S A.‘One physical system’:Tansley's ecosystem as Earth's critical zone[J]. New Phytologist, 2015,206(3):900-912.

朱永官,段桂兰,陈保冬,等.土壤-微生物-植物系统中矿物风化与元素循环[J].中国科学:地球科学,2014,1(6):1107-1116.

黄建辉,韩兴国.森林生态系统的生物地球化学循环:理论和方法[J].植物学报,1995,12(S2):195-223.

Carney K M, Hungate B A, Drake B G, et al. Altered soil microbial community at elevated CO

leads to loss of soil carbon[J]. Proceedings of the National Academy of Sciences, 2007,104(12):4990-4995.

沈菊培,贺纪正.微生物介导的碳氮循环过程对全球气候变化的响应[J].生态学报,2011,31(11):2957-2967.

Calvaruso C, Turpault M P, Frey-Klett P, et al. Increase of apatite dissolution rate by Scots pine roots associated or not with Burkholderia glathei PML1(12)Rp in open-system flow microcosms[J]. Geochimica et Cosmochimica Acta, 2013,106(S):287-306.

Zaharescu D G, Burghelea C I, Dontsova K, et al. Ecosystem composition controls the fate of rare earth elements during Incipient soil genesis[J]. Scientific Reports, 2017,7(1):2273-2286.

杨海花,东秀珠,黄力,等.典型生境重要地球元素循环的微生物驱动机制:第77期"双清论坛"综述[J].中国科学基金,2013,27(3):133-137.

Hahm W J, Riebe C S, Lukens C E, et al. Bedrock composition regulates mountain ecosystems and landscape evolution[J]. Proceedings of the National Academy of Sciences, 2014,111(9):3338-3343.

Ravi S, D'Odorico P, Breshears D, et al. Aeolian processes and the biosphere[J]. Reviews of Geophysics, 2011,49(3):114-123.

Ravi S, Breshears D D, Huxman T E, et al. Land degradation in drylands:Interactions among hydrologic-aeolian erosion and vegetation dynamics[J]. Geomorphology, 2010,116(3/4):236-245.

Wang X M, Lou J P, Cai D W, et al. Effects of earth surface processes on the heterogeneity of surface soil elements and the responses of vegetation elements in the Otindag Desert, China[J]. Catena, 2019,183:43208.

周晓慧,王娟,刘贤安,等.四川牡丹种实性状与环境因子的关系[J].东北林业大学学报,2018,46(9):41-45,58.

中华人民共和国生态环境保护部. HJ832-2017土壤和沉积物金属元素总量的消解微博消解法[S].北京:中国环境科学出版社,2017.

中华人民共和国国家环境保护部.HJ962-2018土壤pH测定:电位法[S].北京:中国环境科学出版社,2018.

冯玮娜,彭培好.四川牡丹根际微生物及种子内生菌组成[J].东北林业大学学报,2020,48(1):88-94.

Caporaso J G, Lauber C L, Walters W A, et al. Global patterns of 16S rRNA diversity at a depth of millions of sequences per sample[J]. Proceedings of the National Academy of Sciences of the United States of America, 2011,108(11S):4516-4522.

Toju H, Tanabe A S, Yamamoto S, et al. High-coverage ITS primers for the DNA-based identification of ascomycetes and basidiomycetes in environmental samples[J]. PLoS One, 2012,7(7):e40863.

王为,周尚哲,李炳元,等.崂山山顶风化坑化学风化过程的岩石化学与矿物学证据[J].第四纪研究,2012,32(1):158-166.

Tuomisto H. A diversity of beta diversities:straightening up a concept gone away(Part 1):Defining beta diversity as a function of alpha and gamma diversity[J]. Ecography, 2010,33(1):2-22.

迟清华,鄢明才.应用地球化学元素丰度数据手册[M].北京:地质出版社,2007.

魏复盛,郑春江,刘志虹.中国土壤元素背景值[M].北京:中国环境科学出版社,1990.

Bini C, Sartori G, Wahsha M, et al. Background levels of trace elements and soil geochemistry at regional level in NE Italy[J]. Journal of Geochemical Exploration, 2011,109(1/3):125-133.

杨帆,刘华忠,张华,等.东天山地区土壤中碱性障与元素分布的关系[J].物探与化探,2011,35(4):438-442.

王会儒,陈国鹏,王飞,等.干旱河谷植物生态适应与植被恢复[J].西北林学院学报,2015,30(5):60-67.

吴涌泉.基于微地形下的紫色砂岩和泥岩土壤剖面分异特性研究[D].重庆:西南大学,2010.

宋照亮,朱兆洲,杨成,等.西南乌江流域石灰岩风化过程中锰和磷的迁移富集[J].浙江林学院学报, 2008,25(6):705-710.

郝立波,陆继龙,马力.浅覆盖区土壤化学成分与基岩化学成分的关系及其意义:以大兴安岭北部地区为例[J].中国地质,2005,32(3):477-482.

Silvana T, Kamlesh J, Ivester A H, et al. Microbial community succession and bacterial diversity in soils during 77000 years of ecosystem development[J]. FEMS Microbiology Ecology, 2008,64(1):129-140.

贺纪正,李晶,郑袁明.土壤生态系统微生物多样性-稳定性关系的思考[J].生物多样性,2013,21(4):412-421.

Torres M A, Dong S, Nealson K H, et al. The kinetics of siderophore-mediated olivine dissolution[J]. Geobiology, 2019,17(4):401-416.

Balland-Bolou-Bi C, Poszwa A. Effect of calco-magnesian amendment on the mineral weathering abilities of bacterial communities in acidic and silicate-rich soils[J]. Soil Biology & Biochemistry, 2012,50:108-117.

胡敏,李芳柏.土壤微生物铁循环及其环境意义[J].土壤学报,2014,51(4):683-698.

Beimforde C, Feldberg K, Nylinder S, et al. Estimating the Phanerozoic history of the

Ascomycota lineages

:Combining fossil and molecular data[J]. Molecular Phylogenetics and Evolution, 2014,78:386-398.

牟文婷,张涛,孙建,等.新疆特殊生境岩石内生细菌末端限制性片段长度多态性技术分析[J].微生物学报,2012,52(3):381-388.

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