Shift from flooding to drying enhances the respiration of soil aggregates by changing microbial community composition and keystone taxa

Changes in the water regime are among the crucial factors controlling soil carbon dynamics. However, at the aggregate scale, the microbial mechanisms that regulate soil respiration under flooding and drying conditions are obscure. In this research, we investigated how the shift from flooding to dryi...

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Main Authors: Kai Zhu, Weitao Jia, Yu Mei, Shengjun Wu, Ping Huang
Format: Article
Language:English
Published: Frontiers Media S.A. 2023-05-01
Series:Frontiers in Microbiology
Subjects:
Online Access:https://www.frontiersin.org/articles/10.3389/fmicb.2023.1167353/full
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author Kai Zhu
Weitao Jia
Yu Mei
Shengjun Wu
Ping Huang
author_facet Kai Zhu
Weitao Jia
Yu Mei
Shengjun Wu
Ping Huang
author_sort Kai Zhu
collection DOAJ
description Changes in the water regime are among the crucial factors controlling soil carbon dynamics. However, at the aggregate scale, the microbial mechanisms that regulate soil respiration under flooding and drying conditions are obscure. In this research, we investigated how the shift from flooding to drying changes the microbial respiration of soil aggregates by affecting microbial community composition and their co-occurrence patterns. Soils collected from a riparian zone of the Three Gorges Reservoir, China, were subjected to a wet-and-dry incubation experiment. Our data illustrated that the shift from flooding to drying substantially enhanced soil respiration for all sizes of aggregate fractions. Moreover, soil respiration declined with aggregate size in both flooding and drying treatments. The keystone taxa in bacterial networks were found to be Acidobacteriales, Gemmatimonadales, Anaerolineales, and Cytophagales during the flooding treatment, and Rhizobiales, Gemmatimonadales, Sphingomonadales, and Solirubrobacterales during the drying treatment. For fungal networks, Hypocreales and Agaricalesin were the keystone taxa in the flooding and drying treatments, respectively. Furthermore, the shift from flooding to drying enhanced the microbial respiration of soil aggregates by changing keystone taxa. Notably, fungal community composition and network properties dominated the changes in the microbial respiration of soil aggregates during the shift from flooding to drying. Thus, our study highlighted that the shift from flooding to drying changes keystone taxa, hence increasing aggregate-scale soil respiration.
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spelling doaj.art-a0d64be686164378ab938c3593b2dc572023-05-12T09:03:14ZengFrontiers Media S.A.Frontiers in Microbiology1664-302X2023-05-011410.3389/fmicb.2023.11673531167353Shift from flooding to drying enhances the respiration of soil aggregates by changing microbial community composition and keystone taxaKai ZhuWeitao JiaYu MeiShengjun WuPing HuangChanges in the water regime are among the crucial factors controlling soil carbon dynamics. However, at the aggregate scale, the microbial mechanisms that regulate soil respiration under flooding and drying conditions are obscure. In this research, we investigated how the shift from flooding to drying changes the microbial respiration of soil aggregates by affecting microbial community composition and their co-occurrence patterns. Soils collected from a riparian zone of the Three Gorges Reservoir, China, were subjected to a wet-and-dry incubation experiment. Our data illustrated that the shift from flooding to drying substantially enhanced soil respiration for all sizes of aggregate fractions. Moreover, soil respiration declined with aggregate size in both flooding and drying treatments. The keystone taxa in bacterial networks were found to be Acidobacteriales, Gemmatimonadales, Anaerolineales, and Cytophagales during the flooding treatment, and Rhizobiales, Gemmatimonadales, Sphingomonadales, and Solirubrobacterales during the drying treatment. For fungal networks, Hypocreales and Agaricalesin were the keystone taxa in the flooding and drying treatments, respectively. Furthermore, the shift from flooding to drying enhanced the microbial respiration of soil aggregates by changing keystone taxa. Notably, fungal community composition and network properties dominated the changes in the microbial respiration of soil aggregates during the shift from flooding to drying. Thus, our study highlighted that the shift from flooding to drying changes keystone taxa, hence increasing aggregate-scale soil respiration.https://www.frontiersin.org/articles/10.3389/fmicb.2023.1167353/fullsoil respirationsoil aggregateswater regime changesmicrobial communityco-occurrence networkkeystone taxa
spellingShingle Kai Zhu
Weitao Jia
Yu Mei
Shengjun Wu
Ping Huang
Shift from flooding to drying enhances the respiration of soil aggregates by changing microbial community composition and keystone taxa
Frontiers in Microbiology
soil respiration
soil aggregates
water regime changes
microbial community
co-occurrence network
keystone taxa
title Shift from flooding to drying enhances the respiration of soil aggregates by changing microbial community composition and keystone taxa
title_full Shift from flooding to drying enhances the respiration of soil aggregates by changing microbial community composition and keystone taxa
title_fullStr Shift from flooding to drying enhances the respiration of soil aggregates by changing microbial community composition and keystone taxa
title_full_unstemmed Shift from flooding to drying enhances the respiration of soil aggregates by changing microbial community composition and keystone taxa
title_short Shift from flooding to drying enhances the respiration of soil aggregates by changing microbial community composition and keystone taxa
title_sort shift from flooding to drying enhances the respiration of soil aggregates by changing microbial community composition and keystone taxa
topic soil respiration
soil aggregates
water regime changes
microbial community
co-occurrence network
keystone taxa
url https://www.frontiersin.org/articles/10.3389/fmicb.2023.1167353/full
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