Wetland restoration after agricultural abandonment enhances soil organic carbon efficiently by stimulating plant- rather than microbial-derived carbon accumulation in Northeast China

被引:10
作者
Zheng, Huijie [1 ,2 ]
Liu, Deyan [1 ,3 ,5 ]
Yuan, Junji [1 ]
Li, Ye [1 ,2 ]
Li, Junjie [1 ,2 ]
Miao, Yuncai [1 ]
Chen, Zengming [1 ]
He, Tiehu [1 ]
Ding, Weixin [1 ,4 ,5 ]
机构
[1] Chinese Acad Sci, Inst Soil Sci, State Key Lab Soil & Sustainable Agr, Nanjing 210008, Peoples R China
[2] Univ Chinese Acad Sci, Beijing 100049, Peoples R China
[3] Nanjing Forestry Univ, Coinnovat Ctr Sustainable Forestry Southern China, Nanjing 210037, Peoples R China
[4] Univ Chinese Acad Sci, Nanjing 211135, Peoples R China
[5] Chinese Acad Sci, Inst Soil Sci, Nanjing 210008, Peoples R China
基金
中国国家自然科学基金;
关键词
Wetland restoration; Agricultural abandonment; Soil organic carbon; Stable carbon isotope; Amino sugars; Lignin phenols; ENZYME-ACTIVITY; LAND-USE; LIGNIN; DECOMPOSITION; OXIDATION; ISOTOPES; DYNAMICS; MATTER; SEQUESTRATION; DEGRADATION;
D O I
10.1016/j.catena.2024.108077
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Agricultural abandonment is a common measure for wetland restoration, which has been suggested as a policy goal with multiple environmental benefits, including improving regional microclimate and promoting soil organic carbon (SOC) accumulation. However, the processes of SOC accumulation during wetland restoration after agricultural abandonment are not clear. Here, we investigated variations in SOC pools and sources in the wetlands restored for one, three, and four years from the paddy field in Northeast China by measuring the delta 13 C values of SOC, amino sugars, and lignin phenols. Wetland restoration for three and four years increased the contents of SOC and new C by 22.6 - 37.2 and 27.9 - 43.0 g C kg - 1 , respectively, while did not affect old C content. This indicated that increased SOC was mainly due to new C accumulation during wetland restoration after agricultural abandonment. Wetland restoration for three and four years increased microbial -derived C content by 59.2 - 102 %, but did not change its proportion in SOC; in contrast, wetland restoration for three and four years increased plant -derived C content by 213 - 301 %, and its proportion in SOC by 106 - 122 %. Among lignin phenols in plant -derived C, wetland restoration for three and four years increased the contents of cinnamyl-, syringyl-, and vanillyl-monomers and the ratio of cinnamyl-/vanillyl-monomer, indicating that wetland restoration after agricultural abandonment was favorable to plant -derived C, especially easily decomposable component accumulation. Plant biomass and soil Fe 2+ /Fe 3+ ratio were identified as key factors influencing SOC content. The increasing plant inputs and retarding lignin degradation through suppressing peroxidase activity in lower oxidizing conditions promoted the accumulation of plant -derived C in SOC during wetland restoration after agricultural abandonment. Our result suggested that enhanced SOC during wetland restoration after agricultural abandonment was primarily due to efficient accumulation of plant -derived C rather than due to microbialderived C accumulation in Northeast China.
引用
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页数:11
相关论文
共 71 条
[1]  
Amelung W., 2001, Methods Using Amino Sugars as Markers for Microbial Residues in Soil, P233
[2]   Soil Organic Carbon and Nitrogen Variations with Vegetation Succession in Passively Restored Freshwater Wetlands [J].
An, Yu ;
Gao, Yang ;
Liu, Xiaohui ;
Tong, Shouzheng ;
Liu, Bo ;
Song, Tiejun ;
Qi, Qing .
WETLANDS, 2021, 41 (01)
[3]  
[Anonymous], 2000, Methods of soil agrochemical analysis
[4]   Lignin turnover kinetics in an agricultural soil is monomer specific [J].
Bahri, Haithem ;
Dignac, Marie-France ;
Rumpel, Cornelia ;
Rasse, Daniel P. ;
Chenu, Claire ;
Mariotti, Andre .
SOIL BIOLOGY & BIOCHEMISTRY, 2006, 38 (07) :1977-1988
[5]   Spatial variation of soil δ13C and its relation to carbon input and soil texture in a subtropical lowland woodland [J].
Bai, Edith ;
Boutton, Thomas W. ;
Liu, Feng ;
Ben Wu, X. ;
Hallmark, C. Thomas ;
Archer, Steven R. .
SOIL BIOLOGY & BIOCHEMISTRY, 2012, 44 (01) :102-112
[6]   Decomposition of grain-corn residues (Zea mays L.):: A litterbag study under three tillage systems [J].
Burgess, MS ;
Mehuys, GR ;
Madramootoo, CA .
CANADIAN JOURNAL OF SOIL SCIENCE, 2002, 82 (02) :127-138
[7]   Soil enzymes in a changing environment: Current knowledge and future directions [J].
Burns, Richard G. ;
DeForest, Jared L. ;
Marxsen, Juergen ;
Sinsabaugh, Robert L. ;
Stromberger, Mary E. ;
Wallenstein, Matthew D. ;
Weintraub, Michael N. ;
Zoppini, Annamaria .
SOIL BIOLOGY & BIOCHEMISTRY, 2013, 58 :216-234
[8]   Influence of water table levels on CO2 emissions in a Colorado subalpine fen:: an in situ microcosm study [J].
Chimner, RA ;
Cooper, DJ .
SOIL BIOLOGY & BIOCHEMISTRY, 2003, 35 (03) :345-351
[9]   The Microbial Efficiency-Matrix Stabilization (MEMS) framework integrates plant litter decomposition with soil organic matter stabilization: do labile plant inputs form stable soil organic matter? [J].
Cotrufo, M. Francesca ;
Wallenstein, Matthew D. ;
Boot, Claudia M. ;
Denef, Karolien ;
Paul, Eldor .
GLOBAL CHANGE BIOLOGY, 2013, 19 (04) :988-995
[10]   How much wetland has the world lost? Long-term and recent trends in global wetland area [J].
Davidson, Nick C. .
MARINE AND FRESHWATER RESEARCH, 2014, 65 (10) :934-941