Temperature sensitivity of anaerobic CO2 production in soils of Phragmites australis marshes with distinct hydrological characteristics in the Yellow River estuary
Temperature sensitivity (Q10) is important to reveal carbon decomposition responding to climate change. It’s remains limited to understand how Q10 of anaerobic soil organic matter (SOM) decomposition is regulated by soil property in various wetlands with distinct hydrological characteristics. In the...
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Elsevier
2021-05-01
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Online Access: | http://www.sciencedirect.com/science/article/pii/S1470160X21000741 |
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author | Yue Liu Jisong Yang Kai Ning Andong Wang Qiuxian Wang Xuehong Wang Shuwen Wang Zhenbo Lv Yajie Zhao Junbao Yu |
author_facet | Yue Liu Jisong Yang Kai Ning Andong Wang Qiuxian Wang Xuehong Wang Shuwen Wang Zhenbo Lv Yajie Zhao Junbao Yu |
author_sort | Yue Liu |
collection | DOAJ |
description | Temperature sensitivity (Q10) is important to reveal carbon decomposition responding to climate change. It’s remains limited to understand how Q10 of anaerobic soil organic matter (SOM) decomposition is regulated by soil property in various wetlands with distinct hydrological characteristics. In the present study, samples of soil at the depths of 0–10 cm, 10–20 cm and 20–30 cm were collected in three typical Phragmites australis marshes, including a freshwater marsh (FPa), a no-tidal salt marsh (NTPa) and a tidal salt marsh (TPa), in the Yellow River estuary. The soil samples were incubated at 10 °C, 20 °C and 30 °C, respectively, to determine the rates of anaerobic CO2 production, Q10 values, and their relations to soil properties. Over 70-d incubation, temperature rise significantly increased the mean rates by 70%–136% (from 10 °C to 20 °C) and 64%–142% (from 20 °C to 30 °C) among the marshes, with the mean Q10 values ranging from 1.61 to 2.66. The rates of CO2 production and Q10 values were significantly affected by wetland type and soil depth. Among marshes, the Q10 of the FPa and NTPa soils was higher than that of the TPa soil (for 0–10 cm and 10–20 cm but for 20–30 cm); along soil depths, the Q10 of the top soil was higher than that of the subsoil (for FPa and NTPa but for TPa). Q10 was affected by total organic carbon (TOC), salinity and pH, and the effects were different with marshes. TOC was a main factor regulating Q10 for the freshwater and the no-tidal salt marshes, while salinity and pH were main factors for the tidal salt marsh. The findings highlight an interactive mechanism of soil property and tidal underlying the response of SOM decomposition to temperature change in estuarine wetlands. |
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language | English |
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spelling | doaj.art-c98229808887400fb08aa206c8380fa22022-12-21T20:35:03ZengElsevierEcological Indicators1470-160X2021-05-01124107409Temperature sensitivity of anaerobic CO2 production in soils of Phragmites australis marshes with distinct hydrological characteristics in the Yellow River estuaryYue Liu0Jisong Yang1Kai Ning2Andong Wang3Qiuxian Wang4Xuehong Wang5Shuwen Wang6Zhenbo Lv7Yajie Zhao8Junbao Yu9Key Laboratory of Ecological Restoration and Conservation of Coastal Wetlands in Universities of Shandong, The Institute for Advanced Study of Coastal Ecology, Ludong University, Yantai, ChinaKey Laboratory of Ecological Restoration and Conservation of Coastal Wetlands in Universities of Shandong, The Institute for Advanced Study of Coastal Ecology, Ludong University, Yantai, China; Dongying Academy of Agricultural Sciences, Dongying, China; Corresponding authors at: No.186th Hongqi Middle Road, Zhifu District, Yantai 264025, China (Y. Liu).Dongying Academy of Agricultural Sciences, Dongying, ChinaShandong Yellow River Delta National Nature Reserve Administration Committee, Dongying, ChinaKey Laboratory of Ecological Restoration and Conservation of Coastal Wetlands in Universities of Shandong, The Institute for Advanced Study of Coastal Ecology, Ludong University, Yantai, ChinaKey Laboratory of Ecological Restoration and Conservation of Coastal Wetlands in Universities of Shandong, The Institute for Advanced Study of Coastal Ecology, Ludong University, Yantai, ChinaKey Laboratory of Ecological Restoration and Conservation of Coastal Wetlands in Universities of Shandong, The Institute for Advanced Study of Coastal Ecology, Ludong University, Yantai, ChinaKey Laboratory of Ecological Restoration and Conservation of Coastal Wetlands in Universities of Shandong, The Institute for Advanced Study of Coastal Ecology, Ludong University, Yantai, ChinaShandong Yellow River Delta National Nature Reserve Administration Committee, Dongying, ChinaKey Laboratory of Ecological Restoration and Conservation of Coastal Wetlands in Universities of Shandong, The Institute for Advanced Study of Coastal Ecology, Ludong University, Yantai, China; Corresponding authors at: No.186th Hongqi Middle Road, Zhifu District, Yantai 264025, China (Y. Liu).Temperature sensitivity (Q10) is important to reveal carbon decomposition responding to climate change. It’s remains limited to understand how Q10 of anaerobic soil organic matter (SOM) decomposition is regulated by soil property in various wetlands with distinct hydrological characteristics. In the present study, samples of soil at the depths of 0–10 cm, 10–20 cm and 20–30 cm were collected in three typical Phragmites australis marshes, including a freshwater marsh (FPa), a no-tidal salt marsh (NTPa) and a tidal salt marsh (TPa), in the Yellow River estuary. The soil samples were incubated at 10 °C, 20 °C and 30 °C, respectively, to determine the rates of anaerobic CO2 production, Q10 values, and their relations to soil properties. Over 70-d incubation, temperature rise significantly increased the mean rates by 70%–136% (from 10 °C to 20 °C) and 64%–142% (from 20 °C to 30 °C) among the marshes, with the mean Q10 values ranging from 1.61 to 2.66. The rates of CO2 production and Q10 values were significantly affected by wetland type and soil depth. Among marshes, the Q10 of the FPa and NTPa soils was higher than that of the TPa soil (for 0–10 cm and 10–20 cm but for 20–30 cm); along soil depths, the Q10 of the top soil was higher than that of the subsoil (for FPa and NTPa but for TPa). Q10 was affected by total organic carbon (TOC), salinity and pH, and the effects were different with marshes. TOC was a main factor regulating Q10 for the freshwater and the no-tidal salt marshes, while salinity and pH were main factors for the tidal salt marsh. The findings highlight an interactive mechanism of soil property and tidal underlying the response of SOM decomposition to temperature change in estuarine wetlands.http://www.sciencedirect.com/science/article/pii/S1470160X21000741Temperature sensitivityAnaerobic SOM decompositionPhragmites australis marshSoil propertyEstuarine wetland |
spellingShingle | Yue Liu Jisong Yang Kai Ning Andong Wang Qiuxian Wang Xuehong Wang Shuwen Wang Zhenbo Lv Yajie Zhao Junbao Yu Temperature sensitivity of anaerobic CO2 production in soils of Phragmites australis marshes with distinct hydrological characteristics in the Yellow River estuary Ecological Indicators Temperature sensitivity Anaerobic SOM decomposition Phragmites australis marsh Soil property Estuarine wetland |
title | Temperature sensitivity of anaerobic CO2 production in soils of Phragmites australis marshes with distinct hydrological characteristics in the Yellow River estuary |
title_full | Temperature sensitivity of anaerobic CO2 production in soils of Phragmites australis marshes with distinct hydrological characteristics in the Yellow River estuary |
title_fullStr | Temperature sensitivity of anaerobic CO2 production in soils of Phragmites australis marshes with distinct hydrological characteristics in the Yellow River estuary |
title_full_unstemmed | Temperature sensitivity of anaerobic CO2 production in soils of Phragmites australis marshes with distinct hydrological characteristics in the Yellow River estuary |
title_short | Temperature sensitivity of anaerobic CO2 production in soils of Phragmites australis marshes with distinct hydrological characteristics in the Yellow River estuary |
title_sort | temperature sensitivity of anaerobic co2 production in soils of phragmites australis marshes with distinct hydrological characteristics in the yellow river estuary |
topic | Temperature sensitivity Anaerobic SOM decomposition Phragmites australis marsh Soil property Estuarine wetland |
url | http://www.sciencedirect.com/science/article/pii/S1470160X21000741 |
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