The active functional microbes contribute differently to soil nitrification and denitrification potential under long-term fertilizer regimes in North-East China
Nitrogen (N) cycling microorganisms mediate soil nitrogen transformation processes, thereby affecting agricultural production and environment quality. However, it is not fully understood how active N-cycling microbial community in soil respond to long-term fertilization, as well as which microorgani...
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Published in | Frontiers in microbiology Vol. 13; p. 1021080 |
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Main Authors | , , , , , , , , |
Format | Journal Article |
Language | English |
Published |
Frontiers Media S.A
03.10.2022
|
Subjects | |
Online Access | Get full text |
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Summary: | Nitrogen (N) cycling microorganisms mediate soil nitrogen transformation processes, thereby affecting agricultural production and environment quality. However, it is not fully understood how active N-cycling microbial community in soil respond to long-term fertilization, as well as which microorganisms regulate soil nitrogen cycling in agricultural ecosystem. Here, we collected the soils from different depths and seasons at a 29-year fertilization experimental field (organic/chemical fertilizer), and investigated the transcriptions of N-cycling functional genes and their contribution to potential nitrification and denitrification. We found that long-term fertilization exerted significant impacts on the transcript abundances of nitrifiers (AOA
amo
A, AOB
amo
A and
hao
) and denitrifiers (
nar
G and
nos
Z), which was also notably influenced by season variation. The transcriptions of AOA
amo
A,
hao
, and
nar
G genes were lowest in autumn, and AOB
amo
A and
nos
Z transcript abundances were highest in autumn. Compared to no fertilization, soil potential nitrification rate (PNR) was reduced in fertilization treatments, while soil potential denitrification rate (PDR) was significantly enhanced in organic combined chemical fertilizer treatment. Both PNR and PDR were highest in 0–20 cm among the tested soil depths. Path model indicated active nitrifiers and denitrifiers had significant impact on soil PNR and PDR, respectively. The transcriptions of AOA
amo
A and
nxr
genes were significantly correlated with soil PNR (Pearson correlation,
r > 0.174
,
p < 0.05
). Significant correlation of
nap
A and
nos
Z transcriptions with soil PDR (Pearson correlation,
r > 0.234
,
p < 0.05
) was also revealed. Random forest analysis showed that SOC content and soil pH were the important factors explaining the total variance of active nitrifers and denitrifiers, respectively. Taken together, long-term fertilization regimes reduced soil PNR and enhanced PDR, which could be attributed to the different responses of active N-cycling microorganisms to soil environment variations. This work provides new insight into the nitrogen cycle, particularly microbial indicators in nitrification and denitrification of long-term fertilized agricultural ecosystems. |
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Bibliography: | ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 23 Reviewed by: Yong Li, Zhejiang University, China; Hong Pan, Shandong Agricultural University, China; Duntao Shu, Northwest A&F University, China This article was submitted to Microbiological Chemistry and Geomicrobiology, a section of the journal Frontiers in Microbiology Edited by: Yongxin Lin, Fujian Normal University, China These authors have contributed equally to this work and share first authorship |
ISSN: | 1664-302X 1664-302X |
DOI: | 10.3389/fmicb.2022.1021080 |