Interplay of soil characteristics and arbuscular mycorrhizal fungi diversity in alpine wetland restoration and carbon stabilization

Alpine wetlands are critical ecosystems for global carbon (C) cycling and climate change mitigation. Ecological restoration projects for alpine grazing wetlands are urgently needed, especially due to their critical role as carbon (C) sinks. However, the fate of the C pool in alpine wetlands after re...

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Main Authors: Hao Tang, Qian Li, Qian Bao, Biao Tang, Kun Li, Yang Ding, Xiaojuan Luo, Qiushu Zeng, Size Liu, Xiangyang Shu, Weijia Liu, Lei Du
Format: Article
Language:English
Published: Frontiers Media S.A. 2024-04-01
Series:Frontiers in Microbiology
Subjects:
Online Access:https://www.frontiersin.org/articles/10.3389/fmicb.2024.1376418/full
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author Hao Tang
Hao Tang
Qian Li
Qian Bao
Qian Bao
Biao Tang
Kun Li
Yang Ding
Yang Ding
Yang Ding
Xiaojuan Luo
Qiushu Zeng
Size Liu
Xiangyang Shu
Xiangyang Shu
Weijia Liu
Lei Du
Lei Du
author_facet Hao Tang
Hao Tang
Qian Li
Qian Bao
Qian Bao
Biao Tang
Kun Li
Yang Ding
Yang Ding
Yang Ding
Xiaojuan Luo
Qiushu Zeng
Size Liu
Xiangyang Shu
Xiangyang Shu
Weijia Liu
Lei Du
Lei Du
author_sort Hao Tang
collection DOAJ
description Alpine wetlands are critical ecosystems for global carbon (C) cycling and climate change mitigation. Ecological restoration projects for alpine grazing wetlands are urgently needed, especially due to their critical role as carbon (C) sinks. However, the fate of the C pool in alpine wetlands after restoration from grazing remains unclear. In this study, soil samples from both grazed and restored wetlands in Zoige (near Hongyuan County, Sichuan Province, China) were collected to analyze soil organic carbon (SOC) fractions, arbuscular mycorrhizal fungi (AMF), soil properties, and plant biomass. Moreover, the Tea Bag Index (TBI) was applied to assess the initial decomposition rate (k) and stabilization factor (S), providing a novel perspective on SOC dynamics. The results of this research revealed that the mineral-associated organic carbon (MAOC) was 1.40 times higher in restored sites compared to grazed sites, although no significant difference in particulate organic carbon (POC) was detected between the two site types. Furthermore, the increased MAOC after restoration exhibited a significant positive correlation with various parameters including S, C and N content, aboveground biomass, WSOC, AMF diversity, and NH4+. This indicates that restoration significantly increases plant primary production, litter turnover, soil characteristics, and AMF diversity, thereby enhancing the C stabilization capacity of alpine wetland soils.
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spelling doaj.art-b3ee070def404cbbbf1f0aac35eac9792024-04-10T05:19:39ZengFrontiers Media S.A.Frontiers in Microbiology1664-302X2024-04-011510.3389/fmicb.2024.13764181376418Interplay of soil characteristics and arbuscular mycorrhizal fungi diversity in alpine wetland restoration and carbon stabilizationHao Tang0Hao Tang1Qian Li2Qian Bao3Qian Bao4Biao Tang5Kun Li6Yang Ding7Yang Ding8Yang Ding9Xiaojuan Luo10Qiushu Zeng11Size Liu12Xiangyang Shu13Xiangyang Shu14Weijia Liu15Lei Du16Lei Du17Key Laboratory of Land Resources Evaluation and Monitoring in Southwest (Sichuan Normal University), Ministry of Education, Chengdu, ChinaThe Faculty of Geography Resource Sciences, Sichuan Normal University, Chengdu, ChinaCollege of Resources, Sichuan Agricultural University, Chengdu, ChinaKey Laboratory of Land Resources Evaluation and Monitoring in Southwest (Sichuan Normal University), Ministry of Education, Chengdu, ChinaThe Faculty of Geography Resource Sciences, Sichuan Normal University, Chengdu, ChinaSichuan Provincial Cultivated Land Quality and Fertilizer Workstation, Chengdu, ChinaSichuan Academy of Forestry, Chengdu, ChinaKey Laboratory of Land Resources Evaluation and Monitoring in Southwest (Sichuan Normal University), Ministry of Education, Chengdu, ChinaThe Faculty of Geography Resource Sciences, Sichuan Normal University, Chengdu, ChinaState Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan, ChinaThe Faculty of Geography Resource Sciences, Sichuan Normal University, Chengdu, ChinaThe Faculty of Geography Resource Sciences, Sichuan Normal University, Chengdu, ChinaResearch Center for Carbon Sequestration and Ecological Restoration, Tianfu Yongxing Laboratory, Chengdu, ChinaKey Laboratory of Land Resources Evaluation and Monitoring in Southwest (Sichuan Normal University), Ministry of Education, Chengdu, ChinaThe Faculty of Geography Resource Sciences, Sichuan Normal University, Chengdu, ChinaChengdu Academy of Agriculture and Forestry Sciences, Chengdu, ChinaKey Laboratory of Land Resources Evaluation and Monitoring in Southwest (Sichuan Normal University), Ministry of Education, Chengdu, ChinaThe Faculty of Geography Resource Sciences, Sichuan Normal University, Chengdu, ChinaAlpine wetlands are critical ecosystems for global carbon (C) cycling and climate change mitigation. Ecological restoration projects for alpine grazing wetlands are urgently needed, especially due to their critical role as carbon (C) sinks. However, the fate of the C pool in alpine wetlands after restoration from grazing remains unclear. In this study, soil samples from both grazed and restored wetlands in Zoige (near Hongyuan County, Sichuan Province, China) were collected to analyze soil organic carbon (SOC) fractions, arbuscular mycorrhizal fungi (AMF), soil properties, and plant biomass. Moreover, the Tea Bag Index (TBI) was applied to assess the initial decomposition rate (k) and stabilization factor (S), providing a novel perspective on SOC dynamics. The results of this research revealed that the mineral-associated organic carbon (MAOC) was 1.40 times higher in restored sites compared to grazed sites, although no significant difference in particulate organic carbon (POC) was detected between the two site types. Furthermore, the increased MAOC after restoration exhibited a significant positive correlation with various parameters including S, C and N content, aboveground biomass, WSOC, AMF diversity, and NH4+. This indicates that restoration significantly increases plant primary production, litter turnover, soil characteristics, and AMF diversity, thereby enhancing the C stabilization capacity of alpine wetland soils.https://www.frontiersin.org/articles/10.3389/fmicb.2024.1376418/fullecological restorationcarbon stabilizationarbuscular mycorrhizal fungitea bag indexclimate change mitigation
spellingShingle Hao Tang
Hao Tang
Qian Li
Qian Bao
Qian Bao
Biao Tang
Kun Li
Yang Ding
Yang Ding
Yang Ding
Xiaojuan Luo
Qiushu Zeng
Size Liu
Xiangyang Shu
Xiangyang Shu
Weijia Liu
Lei Du
Lei Du
Interplay of soil characteristics and arbuscular mycorrhizal fungi diversity in alpine wetland restoration and carbon stabilization
Frontiers in Microbiology
ecological restoration
carbon stabilization
arbuscular mycorrhizal fungi
tea bag index
climate change mitigation
title Interplay of soil characteristics and arbuscular mycorrhizal fungi diversity in alpine wetland restoration and carbon stabilization
title_full Interplay of soil characteristics and arbuscular mycorrhizal fungi diversity in alpine wetland restoration and carbon stabilization
title_fullStr Interplay of soil characteristics and arbuscular mycorrhizal fungi diversity in alpine wetland restoration and carbon stabilization
title_full_unstemmed Interplay of soil characteristics and arbuscular mycorrhizal fungi diversity in alpine wetland restoration and carbon stabilization
title_short Interplay of soil characteristics and arbuscular mycorrhizal fungi diversity in alpine wetland restoration and carbon stabilization
title_sort interplay of soil characteristics and arbuscular mycorrhizal fungi diversity in alpine wetland restoration and carbon stabilization
topic ecological restoration
carbon stabilization
arbuscular mycorrhizal fungi
tea bag index
climate change mitigation
url https://www.frontiersin.org/articles/10.3389/fmicb.2024.1376418/full
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