Spatial distribution of soil organic carbon across diverse vegetation types in a tidal wetland

被引:1
作者
Jia, Wenli [1 ,2 ,3 ]
Chu, Xiaojing [2 ,3 ]
Wang, Xiaojie [2 ,3 ]
Li, Peiguang [2 ,3 ]
Lu, Aobu [4 ]
Zhao, Mingliang [2 ,3 ]
Lu, Feng [5 ]
Huang, Wanxin [2 ,3 ,6 ]
Yu, Dongxue [7 ]
Song, Weimin [2 ,3 ]
Zhang, Xiaoshuai [2 ,3 ]
Liu, Haifang [5 ]
Han, Guangxuan [2 ,3 ]
机构
[1] Liaocheng Univ, Sch Geog & Environm, Liaocheng 252000, Peoples R China
[2] Chinese Acad Sci, Yantai Inst Coastal Zone Res YIC, CAS Key Lab Coastal Environm Proc & Ecol Remediat, Shandong Key Lab Coastal Environm Proc,YICCAS, Yantai 264003, Shandong, Peoples R China
[3] Chinese Acad Sci, Res Stn Coastal Marsh Ecosyst, Yellow River Delta Field Observat, Dongying 257000, Shandong, Peoples R China
[4] Univ British Columbia, Fac Forestry, Vancouver, BC V6T 1Z4, Canada
[5] Adm Bur Yellow River Delta Natl Nat Reserve, Dongying 257091, Peoples R China
[6] Ludong Univ, Sch Life Sci, Yantai 264025, Peoples R China
[7] Hohai Univ, Coll Hydrol & Water Resources, Nanjing 210098, Peoples R China
关键词
Tidal wetland; Vegetation type; Soil water content; Soil organic carbon; YELLOW-RIVER ESTUARY; COASTAL WETLANDS; LAND-USE; VERTICAL-DISTRIBUTION; PHRAGMITES-AUSTRALIS; SALINITY; STORAGE; SALT; DECOMPOSITION; SALINIZATION;
D O I
10.1016/j.marpolbul.2024.117203
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Tidal wetlands are significant contributors to global "blue carbon" resources. The water and salt gradients in tidal wetlands shape vegetation distribution and store significant amounts of soil organic carbon (SOC). We selected four distinct regions within the intertidal zone comprising three distinct vegetation types: low-tide saltmarsh Suaeda salsa (LS), high-tide saltmarsh Suaeda salsa (HS), mid-high-tide Phragmites australis (P), and high-tide Tamarix chinensis (T). Through field sampling and indoor analysis, we found significant differences in SOC levels across various vegetation types along the land-sea gradient. Among these, LS exhibited the highest SOC levels, while P had the lowest. Additionally, there were vertical variations of SOC within a 1-m range among different vegetation types. Mantel analysis and SEM demonstrated that SWC influences SOC content by manipulating vegetation types, thereby regulating total soil carbon. Overall, our findings provide valuable insights for further investigating the effects of vegetation succession on soil carbon pool evolution.
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页数:8
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