Dynamics of labile soil organic carbon during the development of mangrove and salt marsh ecosystems

Labile fractions of soil carbon pools are sensitive to environmental changes, which would influence the stabilization of soil carbon. However, it is unclear whether the dynamics of labile organic carbon (LOC) and soil organic carbon (SOC) are coupled and how they influence each other in coastal wetl...

Descripción completa

Guardado en:
Detalles Bibliográficos
Autores principales: Lina Cui, Huimin Sun, Xuhua Du, Wenting Feng, Yugang Wang, Jinchi Zhang, Jiang Jiang
Formato: article
Lenguaje:EN
Publicado: Elsevier 2021
Materias:
Acceso en línea:https://doaj.org/article/d3b88a24c020486ea4c7f2acc11964ca
Etiquetas: Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!
id oai:doaj.org-article:d3b88a24c020486ea4c7f2acc11964ca
record_format dspace
spelling oai:doaj.org-article:d3b88a24c020486ea4c7f2acc11964ca2021-12-01T04:54:53ZDynamics of labile soil organic carbon during the development of mangrove and salt marsh ecosystems1470-160X10.1016/j.ecolind.2021.107875https://doaj.org/article/d3b88a24c020486ea4c7f2acc11964ca2021-10-01T00:00:00Zhttp://www.sciencedirect.com/science/article/pii/S1470160X21005409https://doaj.org/toc/1470-160XLabile fractions of soil carbon pools are sensitive to environmental changes, which would influence the stabilization of soil carbon. However, it is unclear whether the dynamics of labile organic carbon (LOC) and soil organic carbon (SOC) are coupled and how they influence each other in coastal wetland. The present work investigated the trends of soil carbon fractions among mangrove and Spartina alterniflora communities with different stand ages (1, 5, 10, and 15 years), at Quanzhou Bay Estuary Wetland Nature Reserve, China. We found that SOC in a mangrove ecosystem increased over time, while there was no significant trend in S. alterniflora dominated ecosystems. The highest LOC of mangrove appeared in 5-year-old communities, and then decreased with stand age. In S. alterniflora communities, content of labile fractions increased with the stand age. These trends indicated different soil carbon dynamics when comparing mangrove and S. alterniflora ecosystems. The development of mangroves promoted accumulation of recalcitrant carbon, while S. alterniflora ecosystems contributed to an increase of labile carbon. This phenomenon is probably caused by the characteristics of vegetation and the hydrological conditions. Mangroves contribute more refractory organic carbon to the soil carbon pool, while accumulation of LOC in S. alterniflora communities may inhibit the stabilization of SOC. Our study on the relationship of LOC and SOC implies that complex interactions occur among soil carbon pools and environmental conditions in coastal wetlands, suggesting soil carbon models should take into account decoupled dynamics of LOC and SOC.Lina CuiHuimin SunXuhua DuWenting FengYugang WangJinchi ZhangJiang JiangElsevierarticleMangroveSalt marshStand ageSoil organic carbonLabile organic carbonEcologyQH540-549.5ENEcological Indicators, Vol 129, Iss , Pp 107875- (2021)
institution DOAJ
collection DOAJ
language EN
topic Mangrove
Salt marsh
Stand age
Soil organic carbon
Labile organic carbon
Ecology
QH540-549.5
spellingShingle Mangrove
Salt marsh
Stand age
Soil organic carbon
Labile organic carbon
Ecology
QH540-549.5
Lina Cui
Huimin Sun
Xuhua Du
Wenting Feng
Yugang Wang
Jinchi Zhang
Jiang Jiang
Dynamics of labile soil organic carbon during the development of mangrove and salt marsh ecosystems
description Labile fractions of soil carbon pools are sensitive to environmental changes, which would influence the stabilization of soil carbon. However, it is unclear whether the dynamics of labile organic carbon (LOC) and soil organic carbon (SOC) are coupled and how they influence each other in coastal wetland. The present work investigated the trends of soil carbon fractions among mangrove and Spartina alterniflora communities with different stand ages (1, 5, 10, and 15 years), at Quanzhou Bay Estuary Wetland Nature Reserve, China. We found that SOC in a mangrove ecosystem increased over time, while there was no significant trend in S. alterniflora dominated ecosystems. The highest LOC of mangrove appeared in 5-year-old communities, and then decreased with stand age. In S. alterniflora communities, content of labile fractions increased with the stand age. These trends indicated different soil carbon dynamics when comparing mangrove and S. alterniflora ecosystems. The development of mangroves promoted accumulation of recalcitrant carbon, while S. alterniflora ecosystems contributed to an increase of labile carbon. This phenomenon is probably caused by the characteristics of vegetation and the hydrological conditions. Mangroves contribute more refractory organic carbon to the soil carbon pool, while accumulation of LOC in S. alterniflora communities may inhibit the stabilization of SOC. Our study on the relationship of LOC and SOC implies that complex interactions occur among soil carbon pools and environmental conditions in coastal wetlands, suggesting soil carbon models should take into account decoupled dynamics of LOC and SOC.
format article
author Lina Cui
Huimin Sun
Xuhua Du
Wenting Feng
Yugang Wang
Jinchi Zhang
Jiang Jiang
author_facet Lina Cui
Huimin Sun
Xuhua Du
Wenting Feng
Yugang Wang
Jinchi Zhang
Jiang Jiang
author_sort Lina Cui
title Dynamics of labile soil organic carbon during the development of mangrove and salt marsh ecosystems
title_short Dynamics of labile soil organic carbon during the development of mangrove and salt marsh ecosystems
title_full Dynamics of labile soil organic carbon during the development of mangrove and salt marsh ecosystems
title_fullStr Dynamics of labile soil organic carbon during the development of mangrove and salt marsh ecosystems
title_full_unstemmed Dynamics of labile soil organic carbon during the development of mangrove and salt marsh ecosystems
title_sort dynamics of labile soil organic carbon during the development of mangrove and salt marsh ecosystems
publisher Elsevier
publishDate 2021
url https://doaj.org/article/d3b88a24c020486ea4c7f2acc11964ca
work_keys_str_mv AT linacui dynamicsoflabilesoilorganiccarbonduringthedevelopmentofmangroveandsaltmarshecosystems
AT huiminsun dynamicsoflabilesoilorganiccarbonduringthedevelopmentofmangroveandsaltmarshecosystems
AT xuhuadu dynamicsoflabilesoilorganiccarbonduringthedevelopmentofmangroveandsaltmarshecosystems
AT wentingfeng dynamicsoflabilesoilorganiccarbonduringthedevelopmentofmangroveandsaltmarshecosystems
AT yugangwang dynamicsoflabilesoilorganiccarbonduringthedevelopmentofmangroveandsaltmarshecosystems
AT jinchizhang dynamicsoflabilesoilorganiccarbonduringthedevelopmentofmangroveandsaltmarshecosystems
AT jiangjiang dynamicsoflabilesoilorganiccarbonduringthedevelopmentofmangroveandsaltmarshecosystems
_version_ 1718405692583313408