Effects of forest types on soil carbon content in aggregate faction under climate transition zone

Variations in soil aggregates and soil organic carbon (SOC) in response to land-use change are important to understanding the carbon cycle in forest ecosystems. However, few studies investigated the effect of forest type on aggregate stability, SOC content, and particulate organic carbon (POC) conte...

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Main Authors: Xiongde Dong, Kunpeng Zhao, Jian Wang, Haoran Gui, Yutong Xiao, Zhijie Chen, Yuan Miao, Shijie Han
Format: Article
Language:English
Published: Frontiers Media S.A. 2023-01-01
Series:Frontiers in Environmental Science
Subjects:
Online Access:https://www.frontiersin.org/articles/10.3389/fenvs.2022.1052175/full
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author Xiongde Dong
Xiongde Dong
Kunpeng Zhao
Kunpeng Zhao
Jian Wang
Jian Wang
Haoran Gui
Haoran Gui
Yutong Xiao
Yutong Xiao
Zhijie Chen
Zhijie Chen
Yuan Miao
Yuan Miao
Shijie Han
Shijie Han
author_facet Xiongde Dong
Xiongde Dong
Kunpeng Zhao
Kunpeng Zhao
Jian Wang
Jian Wang
Haoran Gui
Haoran Gui
Yutong Xiao
Yutong Xiao
Zhijie Chen
Zhijie Chen
Yuan Miao
Yuan Miao
Shijie Han
Shijie Han
author_sort Xiongde Dong
collection DOAJ
description Variations in soil aggregates and soil organic carbon (SOC) in response to land-use change are important to understanding the carbon cycle in forest ecosystems. However, few studies investigated the effect of forest type on aggregate stability, SOC content, and particulate organic carbon (POC) content. Therefore, we collected soil and fine root samples in two natural forests (Pinus massoniana and Quercus variabilis) and a planted forest (Cunninghamia lanceolata) in a warm temperate–subtropical climate transition zone to analyze the effect of forest type on aggregate stability, SOC content, and POC content. The results showed that the mean weight diameter (MWD) of the soil aggregates was significantly higher in Quercus variabilis and Pinus massoniana forests (62% and 21%, respectively) than in the Cunninghamia lanceolata forest due to higher mycelial length density, mycelial infection rate, and glomalin content. Similarly, the SOC and POC contents were significantly higher in Quercus variabilis and Pinus massoniana forests than in the Cunninghamia lanceolata forest (p < 0.05). The dominant size fraction of aggregate was highly correlated with the carbon fraction content. The SOC and POC contents and fungal traits (mycelial length density, mycelial infection rate, and glomalin content) were significantly positively correlated with the MWD. These results indicated that natural forests had higher aggregate stability than planted forests due to higher SOC content and more favorable fungal traits in the warm temperate–subtropical climate transition zone.
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spelling doaj.art-2dc479c996c54931ab8dbc734383187f2023-01-10T14:15:05ZengFrontiers Media S.A.Frontiers in Environmental Science2296-665X2023-01-011010.3389/fenvs.2022.10521751052175Effects of forest types on soil carbon content in aggregate faction under climate transition zoneXiongde Dong0Xiongde Dong1Kunpeng Zhao2Kunpeng Zhao3Jian Wang4Jian Wang5Haoran Gui6Haoran Gui7Yutong Xiao8Yutong Xiao9Zhijie Chen10Zhijie Chen11Yuan Miao12Yuan Miao13Shijie Han14Shijie Han15International Joint Research Laboratory for Global Change Ecology, School of Life Sciences, Henan University, Kaifeng, Henan, ChinaYellow River Floodplain Ecosystems Research Station, Henan University, Xingyang, ChinaInternational Joint Research Laboratory for Global Change Ecology, School of Life Sciences, Henan University, Kaifeng, Henan, ChinaYellow River Floodplain Ecosystems Research Station, Henan University, Xingyang, ChinaInternational Joint Research Laboratory for Global Change Ecology, School of Life Sciences, Henan University, Kaifeng, Henan, ChinaYellow River Floodplain Ecosystems Research Station, Henan University, Xingyang, ChinaInternational Joint Research Laboratory for Global Change Ecology, School of Life Sciences, Henan University, Kaifeng, Henan, ChinaYellow River Floodplain Ecosystems Research Station, Henan University, Xingyang, ChinaInternational Joint Research Laboratory for Global Change Ecology, School of Life Sciences, Henan University, Kaifeng, Henan, ChinaYellow River Floodplain Ecosystems Research Station, Henan University, Xingyang, ChinaInternational Joint Research Laboratory for Global Change Ecology, School of Life Sciences, Henan University, Kaifeng, Henan, ChinaState Key Laboratory of Subtropical Mountain Ecology (Funded by Ministry of Science and Technology and Fujian Province), Fujian Normal University, Fuzhou, Fujian, ChinaInternational Joint Research Laboratory for Global Change Ecology, School of Life Sciences, Henan University, Kaifeng, Henan, ChinaYellow River Floodplain Ecosystems Research Station, Henan University, Xingyang, ChinaInternational Joint Research Laboratory for Global Change Ecology, School of Life Sciences, Henan University, Kaifeng, Henan, ChinaYellow River Floodplain Ecosystems Research Station, Henan University, Xingyang, ChinaVariations in soil aggregates and soil organic carbon (SOC) in response to land-use change are important to understanding the carbon cycle in forest ecosystems. However, few studies investigated the effect of forest type on aggregate stability, SOC content, and particulate organic carbon (POC) content. Therefore, we collected soil and fine root samples in two natural forests (Pinus massoniana and Quercus variabilis) and a planted forest (Cunninghamia lanceolata) in a warm temperate–subtropical climate transition zone to analyze the effect of forest type on aggregate stability, SOC content, and POC content. The results showed that the mean weight diameter (MWD) of the soil aggregates was significantly higher in Quercus variabilis and Pinus massoniana forests (62% and 21%, respectively) than in the Cunninghamia lanceolata forest due to higher mycelial length density, mycelial infection rate, and glomalin content. Similarly, the SOC and POC contents were significantly higher in Quercus variabilis and Pinus massoniana forests than in the Cunninghamia lanceolata forest (p < 0.05). The dominant size fraction of aggregate was highly correlated with the carbon fraction content. The SOC and POC contents and fungal traits (mycelial length density, mycelial infection rate, and glomalin content) were significantly positively correlated with the MWD. These results indicated that natural forests had higher aggregate stability than planted forests due to higher SOC content and more favorable fungal traits in the warm temperate–subtropical climate transition zone.https://www.frontiersin.org/articles/10.3389/fenvs.2022.1052175/fullsoil aggregate stabilityorganic carbondifferent forest typesparticle organic carbonfungal traits
spellingShingle Xiongde Dong
Xiongde Dong
Kunpeng Zhao
Kunpeng Zhao
Jian Wang
Jian Wang
Haoran Gui
Haoran Gui
Yutong Xiao
Yutong Xiao
Zhijie Chen
Zhijie Chen
Yuan Miao
Yuan Miao
Shijie Han
Shijie Han
Effects of forest types on soil carbon content in aggregate faction under climate transition zone
Frontiers in Environmental Science
soil aggregate stability
organic carbon
different forest types
particle organic carbon
fungal traits
title Effects of forest types on soil carbon content in aggregate faction under climate transition zone
title_full Effects of forest types on soil carbon content in aggregate faction under climate transition zone
title_fullStr Effects of forest types on soil carbon content in aggregate faction under climate transition zone
title_full_unstemmed Effects of forest types on soil carbon content in aggregate faction under climate transition zone
title_short Effects of forest types on soil carbon content in aggregate faction under climate transition zone
title_sort effects of forest types on soil carbon content in aggregate faction under climate transition zone
topic soil aggregate stability
organic carbon
different forest types
particle organic carbon
fungal traits
url https://www.frontiersin.org/articles/10.3389/fenvs.2022.1052175/full
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