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首页|期刊导航|生态学报|黄土高原水蚀风蚀交错区固氮微生物群落多样性在生物结皮中的演变规律

黄土高原水蚀风蚀交错区固氮微生物群落多样性在生物结皮中的演变规律

焦冰洁 徐琳 李香真 张丙昌

生态学报2023,Vol.43Issue(23):9662-9673,12.
生态学报2023,Vol.43Issue(23):9662-9673,12.DOI:10.20103/j.stxb.202210072842

黄土高原水蚀风蚀交错区固氮微生物群落多样性在生物结皮中的演变规律

Diazotrophic community diversity in the succession development of biological soil crusts in water-wind erosion crisscross region of the Loess Plateau

焦冰洁 1徐琳 2李香真 3张丙昌1

作者信息

  • 1. 山西师范大学地理科学学院,太原 030031||山西师范大学黄河中游生态环境研究中心,太原 030031
  • 2. 中国科学院成都生物研究所,成都 610041||四川农业大学生态林业研究所,成都 611100
  • 3. 中国科学院成都生物研究所,成都 610041
  • 折叠

摘要

Abstract

Biological soil crusting(BSCs)plays an important ecological function in water and soil retention,nutrient resupply in the Loess Plateau.Nitrogen fixing microorganisms are the key functional group for soil nitrogen fixation process and affect the soil N balance,however,the severe soil loss in the hydro erosive and erosive staggered zones of the Loess Plateau resulted in substantial loss of soil nutrients,especially N.BSCs develop widely in this region,and they play an important role in the process of nitrogen accumulation in soils in arid semi-arid regions.But the nitrogen fixation potential,diversity of nitrogen fixing microbial community and its key environmental control factors in different developmental stages of biological nodulation in this region are still unclear.Here,we used the Illumina hiseq platform to perform bioinformatics analysis of the amplified products of the nifH gene to reveal the distribution pattern of the nitrogen fixation potential and diversity of the microbial community,using the loess plateau water cavitation interlace as the research area,three biological crusting types and nude ground controls.The results showed that the BSCs succession significantly changed the nitrogenase activity(NAc),nifH gene abundance,and α-diversity of diazotrophs,while these parameters were significantly higher in moss crusts than those in bare soil,light and dark algal crusts,and lichen crusts.They also showed higher values in 0-2 cm biocrust layer than those in subsurface soil below BSCs.Diazotrophic community in bare soil was dominated by Rhodospirillales,Acidithiobacillales,and Rhizobiales of phylum Proteobacteria.Nostocales belonging to Cyanobacteria were the dominant diazotrophs in algal crusts,lichen crusts,and moss crusts.Trichormus and Nostoc were keystone species in Nostocales.However,compared with algal crusts and lichen crusts,the relative abundance of Nostocales significantly decreased and the relative abundance of Rhodospirillales,Acidithiobacillales,and Rhizobiales increased in moss crusts.Besides that,Cyanothece,Anabaena,Skermanella,Ruminclostridium were also dominant in algal crusts,lichen crusts,moss crusts.The relative abundance of Nostocales and Trichormus represented significant and positive correlations with nitrogenase activity and nifH gene abundance,while it was negatively correlated with Rhodospiraceae,Acidobacteria,Clostridiales and Rhizobiales;indicating that Trichormus might play key role in N inputs in BSCs on the Loess Plateau.The variations of physicochemical properties,including soil pH,organic matter,total nitrogen,water content caused by biological crust succession,altered the microhabitat,and exerted a comprehensive regulation on the diazotrophic community through environmental screening.Among soil physicochemical properties,pH and TN played critical role in regulating diazotrophic community.

关键词

黄土高原/水蚀风蚀交错区/生物结皮演替/固氮微生物

Key words

the Loess Plateau/water-wind erosion crisscross region/biological soil crusts succession/Diazotrophs

引用本文复制引用

焦冰洁,徐琳,李香真,张丙昌..黄土高原水蚀风蚀交错区固氮微生物群落多样性在生物结皮中的演变规律[J].生态学报,2023,43(23):9662-9673,12.

基金项目

国家自然科学基金项目(42271067,U2003214) (42271067,U2003214)

生态学报

OA北大核心CHSSCDCSCDCSTPCD

1000-0933

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