Succession of bacterial community composition in coastal agricultural soils along a 1000-year reclamation chronosequence in Hangzhou Bay, China

Soil bacterial successional trajectories under frequently disturbed circumstances (such as agricultural practice) are less known due to the complexity and uncertainty of disturbance. Here, a reclaimed coastal soil chronosequence spanning over a millennium was studied to understand the variation in s...

Descripción completa

Guardado en:
Detalles Bibliográficos
Autores principales: Feng Wang, Wentao Peng, Bo Zhang, Ying Cao, Juan Zhao, Hui Cao
Formato: article
Lenguaje:EN
Publicado: Elsevier 2021
Materias:
Acceso en línea:https://doaj.org/article/03a6ed3fb1ab4ddd8a241b1eb52da39f
Etiquetas: Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!
id oai:doaj.org-article:03a6ed3fb1ab4ddd8a241b1eb52da39f
record_format dspace
spelling oai:doaj.org-article:03a6ed3fb1ab4ddd8a241b1eb52da39f2021-12-01T04:31:18ZSuccession of bacterial community composition in coastal agricultural soils along a 1000-year reclamation chronosequence in Hangzhou Bay, China1470-160X10.1016/j.ecolind.2020.106972https://doaj.org/article/03a6ed3fb1ab4ddd8a241b1eb52da39f2021-02-01T00:00:00Zhttp://www.sciencedirect.com/science/article/pii/S1470160X20309110https://doaj.org/toc/1470-160XSoil bacterial successional trajectories under frequently disturbed circumstances (such as agricultural practice) are less known due to the complexity and uncertainty of disturbance. Here, a reclaimed coastal soil chronosequence spanning over a millennium was studied to understand the variation in soil microorganisms. We used 16S rRNA gene-based quantitative PCR to determine bacterial number and Illumina Sequencing to analyse bacterial community composition and diversity. Despite 10-fold higher 16S rRNA gene copy number, coastal sediments showed the lowest bacterial phylogenetic diversity, demonstrating that bacteria acclimatised in the destination environment with low nutrient and high salinity. Among the reclaimed soil, regular variation in microbial distribution (abundance and diversity) and the “disturbance climax” theory can explain the dynamics of bacterial succession. Consistent with soil physicochemical variables, bacterial community varied in an orderly way and changed more drastically at initial stage (early 60 years) but only slightly fluctuated thereafter. The soil variables soil organic matter (SOM), total nitrogen (TN), and electrical conductivity (EC) were confirmed to be the main factors affecting bacterial succession, among which SOM played a dominant role in initial and long-term reclamation stage (500 ~ 1000 years), while TN was more important in mid-term reclamation (5 ~ 280 years).Feng WangWentao PengBo ZhangYing CaoJuan ZhaoHui CaoElsevierarticleBacterial community successionCoastal wetland reclamationChronosequencesAgricultural soilHangzhou BayEcologyQH540-549.5ENEcological Indicators, Vol 121, Iss , Pp 106972- (2021)
institution DOAJ
collection DOAJ
language EN
topic Bacterial community succession
Coastal wetland reclamation
Chronosequences
Agricultural soil
Hangzhou Bay
Ecology
QH540-549.5
spellingShingle Bacterial community succession
Coastal wetland reclamation
Chronosequences
Agricultural soil
Hangzhou Bay
Ecology
QH540-549.5
Feng Wang
Wentao Peng
Bo Zhang
Ying Cao
Juan Zhao
Hui Cao
Succession of bacterial community composition in coastal agricultural soils along a 1000-year reclamation chronosequence in Hangzhou Bay, China
description Soil bacterial successional trajectories under frequently disturbed circumstances (such as agricultural practice) are less known due to the complexity and uncertainty of disturbance. Here, a reclaimed coastal soil chronosequence spanning over a millennium was studied to understand the variation in soil microorganisms. We used 16S rRNA gene-based quantitative PCR to determine bacterial number and Illumina Sequencing to analyse bacterial community composition and diversity. Despite 10-fold higher 16S rRNA gene copy number, coastal sediments showed the lowest bacterial phylogenetic diversity, demonstrating that bacteria acclimatised in the destination environment with low nutrient and high salinity. Among the reclaimed soil, regular variation in microbial distribution (abundance and diversity) and the “disturbance climax” theory can explain the dynamics of bacterial succession. Consistent with soil physicochemical variables, bacterial community varied in an orderly way and changed more drastically at initial stage (early 60 years) but only slightly fluctuated thereafter. The soil variables soil organic matter (SOM), total nitrogen (TN), and electrical conductivity (EC) were confirmed to be the main factors affecting bacterial succession, among which SOM played a dominant role in initial and long-term reclamation stage (500 ~ 1000 years), while TN was more important in mid-term reclamation (5 ~ 280 years).
format article
author Feng Wang
Wentao Peng
Bo Zhang
Ying Cao
Juan Zhao
Hui Cao
author_facet Feng Wang
Wentao Peng
Bo Zhang
Ying Cao
Juan Zhao
Hui Cao
author_sort Feng Wang
title Succession of bacterial community composition in coastal agricultural soils along a 1000-year reclamation chronosequence in Hangzhou Bay, China
title_short Succession of bacterial community composition in coastal agricultural soils along a 1000-year reclamation chronosequence in Hangzhou Bay, China
title_full Succession of bacterial community composition in coastal agricultural soils along a 1000-year reclamation chronosequence in Hangzhou Bay, China
title_fullStr Succession of bacterial community composition in coastal agricultural soils along a 1000-year reclamation chronosequence in Hangzhou Bay, China
title_full_unstemmed Succession of bacterial community composition in coastal agricultural soils along a 1000-year reclamation chronosequence in Hangzhou Bay, China
title_sort succession of bacterial community composition in coastal agricultural soils along a 1000-year reclamation chronosequence in hangzhou bay, china
publisher Elsevier
publishDate 2021
url https://doaj.org/article/03a6ed3fb1ab4ddd8a241b1eb52da39f
work_keys_str_mv AT fengwang successionofbacterialcommunitycompositionincoastalagriculturalsoilsalonga1000yearreclamationchronosequenceinhangzhoubaychina
AT wentaopeng successionofbacterialcommunitycompositionincoastalagriculturalsoilsalonga1000yearreclamationchronosequenceinhangzhoubaychina
AT bozhang successionofbacterialcommunitycompositionincoastalagriculturalsoilsalonga1000yearreclamationchronosequenceinhangzhoubaychina
AT yingcao successionofbacterialcommunitycompositionincoastalagriculturalsoilsalonga1000yearreclamationchronosequenceinhangzhoubaychina
AT juanzhao successionofbacterialcommunitycompositionincoastalagriculturalsoilsalonga1000yearreclamationchronosequenceinhangzhoubaychina
AT huicao successionofbacterialcommunitycompositionincoastalagriculturalsoilsalonga1000yearreclamationchronosequenceinhangzhoubaychina
_version_ 1718405822759829504