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Organic matter composition and stability in estuarine wetlands depending on soil salinity

Wu, Lele (författare)
Tianjin Univ, China
Song, Zhaoliang (författare)
Tianjin Univ, China;Haihe Lab Sustainable Chem Transformat, China
Wu, Yuntao (författare)
Lishui Univ, China
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Xia, Shaopan (författare)
Nanjing Agr Univ, China
Kuzyakov, Yakov (författare)
Univ Goettingen, Germany;RUDN Univ, Russia;Univ Exeter, UK
Hartley, Iain P. (författare)
Kazan Fed Univ, Russia
Fang, Yunying (författare)
Griffith Univ, Australia
Yu, Changxun, 1983- (författare)
Linnéuniversitetet,Institutionen för biologi och miljö (BOM)
Wang, Yidong (författare)
Tianjin Normal Univ, China
Chen, Ji (författare)
Chinese Acad Sci, China;Aarhus Univ, Denmark
Guo, Laodong (författare)
Univ Wisconsin Milwaukee, USA
Li, Zimin (författare)
Chinese Acad Sci, China
Zhao, Xiangwei (författare)
Tianjin Univ, China
Yang, Xiaomin (författare)
Guizhou Univ, China
Zhang, Zhenqing (författare)
Tianjin Normal Univ, China
Liu, Shuyan (författare)
Natl Nat Reserve Management Ctr Liujiang Basin Geo, China
Wang, Weiqi (författare)
Fujian Normal Univ, China
Ran, Xiangbin (författare)
Minist Nat Resources, China
Liu, Cong-Qiang (författare)
Tianjin Univ, China;Haihe Lab Sustainable Chem Transformat, China
Wang, Hailong (författare)
Foshan Univ, China;Guangdong Acad Sci, China
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 (creator_code:org_t)
Elsevier, 2024
2024
Engelska.
Ingår i: Science of the Total Environment. - : Elsevier. - 0048-9697 .- 1879-1026. ; 945
  • Tidskriftsartikel (refereegranskat)
Abstract Ämnesord
Stäng  
  • Coastal wetlands are key players in mitigating global climate change by sequestering soil organic matter. Soil organic matter consists of less stable particulate organic matter (POM) and more stable mineral -associated organic matter (MAOM). The distribution and drivers of MAOM and POM in coastal wetlands have received little attention, despite the processes and mechanisms differ from that in the upland soils. We explored the distribution of POM and MAOM, their contributions to SOM, and the controlling factors along a salinity gradient in an estuarine wetland. In the estuarine wetland, POM C and N were influenced by soil depth and vegetation type, whereas MAOM C and N were influenced only by vegetation type. In the estuarine wetland, SOM was predominantly in the form of MAOM ( > 70 %) and increased with salinity (70 % -76 %), leading to long-term C sequestration. Both POM and MAOM increased with SOM, and the increase rate of POM was higher than that of MAOM. Aboveground plant biomass decreased with increasing salinity, resulted in a decrease in POM C (46 % - 81 %) and N (52 % -82 %) pools. As the mineral amount and activity, and microbial biomass decreased, the MAOM C (2.5 % -64 %) and N pool (8.6 % -59 %) decreased with salinity. When evaluating POM, the most influential factors were microbial biomass carbon (MBC) and dissolved organic carbon (DOC). Key parameters, including MBC, DOC, soil salinity, soil water content, aboveground plant biomass, mineral content and activity, and bulk density, were identified as influencing factors for both MAOM abundance. Soil water content not only directly controlled MAOM, but together with salinity also indirectly regulated POM and MAOM by controlling microbial biomass and aboveground plant biomass. Our findings have important implications for improving the accumulation and increased stability of soil organic matter in coastal wetlands, considering the global sea level rise and increased frequency of inundation.

Ämnesord

NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Miljövetenskap (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Environmental Sciences (hsv//eng)

Nyckelord

Particulate organic matter
Mineral-associated organic matter
Tidal wetlands
Sea-level rise
Blue carbon
Vegetation habitats
Salinity gradient
Miljövetenskap
Environmental Science

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