Divergent accumulation of amino sugars and lignins mediated by soil functional carbon pools under tropical forest conversion

Tropical primary forests are being destroyed at an alarming rate and converted for other land uses which is expected to greatly influence soil carbon (C) cycling. However, our understanding of how tropical forest conversions affect the accumulation of compounds in soil functional C pools remains unc...

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Veröffentlicht in:The Science of the total environment 2023-07, Vol.881 (C), p.163204-163204, Article 163204
Hauptverfasser: Li, Tengteng, Cheng, Hao, Li, Yue, Mou, Zhijian, Zhu, Xiaomin, Wu, Wenjia, Zhang, Jing, Kuang, Luhui, Wang, Jun, Hui, Dafeng, Lambers, Hans, Sardans, Jordi, Peñuelas, Josep, Ren, Hai, Mohti, Azian Binti, Liang, Naishen, Liu, Zhanfeng
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container_issue C
container_start_page 163204
container_title The Science of the total environment
container_volume 881
creator Li, Tengteng
Cheng, Hao
Li, Yue
Mou, Zhijian
Zhu, Xiaomin
Wu, Wenjia
Zhang, Jing
Kuang, Luhui
Wang, Jun
Hui, Dafeng
Lambers, Hans
Sardans, Jordi
Peñuelas, Josep
Ren, Hai
Mohti, Azian Binti
Liang, Naishen
Liu, Zhanfeng
description Tropical primary forests are being destroyed at an alarming rate and converted for other land uses which is expected to greatly influence soil carbon (C) cycling. However, our understanding of how tropical forest conversions affect the accumulation of compounds in soil functional C pools remains unclear. Here, we collected soils from primary forests (PF), secondary forests (SF), oil-palm (OP), and rubber plantations (RP), and assessed the accumulation of plant- and microbial-derived compounds within soil organic carbon (SOC), particulate (POC) and mineral-associated (MAOC) organic C. PF conversion to RP greatly decreased SOC, POC, and MAOC concentrations, whereas conversion to SF increased POC concentrations and decreased MAOC concentrations, and conversion to OP only increased POC concentrations. PF conversion to RP decreased lignin concentrations and increased amino sugar concentrations in SOC pools which increased the stability of SOC, whereas conversion to SF only increased the lignin concentrations in POC, and conversion to OP just increased lignin concentrations in POC and decreased it in MAOC. We observed divergent dynamics of amino sugars (decrease) and lignin (increase) in SOC with increasing SOC. Only lignin concentrations increased in POC with increasing POC and amino sugars concentrations decreased in MAOC with increasing MAOC. Conversion to RP significantly decreased soil enzyme activities and microbial biomasses. Lignin accumulation was associated with microbial properties, whereas amino sugar accumulation was mainly associated with soil nutrients and stoichiometries. These results suggest that the divergent accumulation of plant- and microbial-derived C in SOC was delivered by the distribution and original composition of functional C pools under forest conversions. Forest conversions changed the formation and stabilization processes of SOC in the long run which was associated with converted plantations and management. The important roles of soil nutrients and stoichiometry also provide a natural-based solution to enhance SOC sequestration via nutrient management in tropical forests. [Display omitted] •Primary forests converted to rubber plantations reduced SOC, POC, and MAOC storage.•Increased lignin and decreased amino sugars with increasing SOC concentrations•Primary forest conversion changed distributions of POC and MAOC and their origins.•Amino sugars accumulation was more affected by soil nutrients and stoichiometry.•Lignin accumulation
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However, our understanding of how tropical forest conversions affect the accumulation of compounds in soil functional C pools remains unclear. Here, we collected soils from primary forests (PF), secondary forests (SF), oil-palm (OP), and rubber plantations (RP), and assessed the accumulation of plant- and microbial-derived compounds within soil organic carbon (SOC), particulate (POC) and mineral-associated (MAOC) organic C. PF conversion to RP greatly decreased SOC, POC, and MAOC concentrations, whereas conversion to SF increased POC concentrations and decreased MAOC concentrations, and conversion to OP only increased POC concentrations. PF conversion to RP decreased lignin concentrations and increased amino sugar concentrations in SOC pools which increased the stability of SOC, whereas conversion to SF only increased the lignin concentrations in POC, and conversion to OP just increased lignin concentrations in POC and decreased it in MAOC. We observed divergent dynamics of amino sugars (decrease) and lignin (increase) in SOC with increasing SOC. Only lignin concentrations increased in POC with increasing POC and amino sugars concentrations decreased in MAOC with increasing MAOC. Conversion to RP significantly decreased soil enzyme activities and microbial biomasses. Lignin accumulation was associated with microbial properties, whereas amino sugar accumulation was mainly associated with soil nutrients and stoichiometries. These results suggest that the divergent accumulation of plant- and microbial-derived C in SOC was delivered by the distribution and original composition of functional C pools under forest conversions. Forest conversions changed the formation and stabilization processes of SOC in the long run which was associated with converted plantations and management. The important roles of soil nutrients and stoichiometry also provide a natural-based solution to enhance SOC sequestration via nutrient management in tropical forests. [Display omitted] •Primary forests converted to rubber plantations reduced SOC, POC, and MAOC storage.•Increased lignin and decreased amino sugars with increasing SOC concentrations•Primary forest conversion changed distributions of POC and MAOC and their origins.•Amino sugars accumulation was more affected by soil nutrients and stoichiometry.•Lignin accumulation was more affected by microbial properties.</description><identifier>ISSN: 0048-9697</identifier><identifier>EISSN: 1879-1026</identifier><identifier>DOI: 10.1016/j.scitotenv.2023.163204</identifier><identifier>PMID: 37044342</identifier><language>eng</language><publisher>Netherlands: Elsevier B.V</publisher><subject>Amino sugars ; Biomass ; Carbon ; Environmental Sciences &amp; Ecology ; Forests ; Lignin ; Mineral-associated organic carbon ; Particulate organic carbon ; Rubber ; Soil ; Soil organic carbon ; Tropical forest conversions</subject><ispartof>The Science of the total environment, 2023-07, Vol.881 (C), p.163204-163204, Article 163204</ispartof><rights>2023</rights><rights>Copyright © 2023. 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The important roles of soil nutrients and stoichiometry also provide a natural-based solution to enhance SOC sequestration via nutrient management in tropical forests. 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However, our understanding of how tropical forest conversions affect the accumulation of compounds in soil functional C pools remains unclear. Here, we collected soils from primary forests (PF), secondary forests (SF), oil-palm (OP), and rubber plantations (RP), and assessed the accumulation of plant- and microbial-derived compounds within soil organic carbon (SOC), particulate (POC) and mineral-associated (MAOC) organic C. PF conversion to RP greatly decreased SOC, POC, and MAOC concentrations, whereas conversion to SF increased POC concentrations and decreased MAOC concentrations, and conversion to OP only increased POC concentrations. PF conversion to RP decreased lignin concentrations and increased amino sugar concentrations in SOC pools which increased the stability of SOC, whereas conversion to SF only increased the lignin concentrations in POC, and conversion to OP just increased lignin concentrations in POC and decreased it in MAOC. We observed divergent dynamics of amino sugars (decrease) and lignin (increase) in SOC with increasing SOC. Only lignin concentrations increased in POC with increasing POC and amino sugars concentrations decreased in MAOC with increasing MAOC. Conversion to RP significantly decreased soil enzyme activities and microbial biomasses. Lignin accumulation was associated with microbial properties, whereas amino sugar accumulation was mainly associated with soil nutrients and stoichiometries. These results suggest that the divergent accumulation of plant- and microbial-derived C in SOC was delivered by the distribution and original composition of functional C pools under forest conversions. Forest conversions changed the formation and stabilization processes of SOC in the long run which was associated with converted plantations and management. The important roles of soil nutrients and stoichiometry also provide a natural-based solution to enhance SOC sequestration via nutrient management in tropical forests. [Display omitted] •Primary forests converted to rubber plantations reduced SOC, POC, and MAOC storage.•Increased lignin and decreased amino sugars with increasing SOC concentrations•Primary forest conversion changed distributions of POC and MAOC and their origins.•Amino sugars accumulation was more affected by soil nutrients and stoichiometry.•Lignin accumulation was more affected by microbial properties.</abstract><cop>Netherlands</cop><pub>Elsevier B.V</pub><pmid>37044342</pmid><doi>10.1016/j.scitotenv.2023.163204</doi><tpages>1</tpages><oa>free_for_read</oa></addata></record>
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subjects Amino sugars
Biomass
Carbon
Environmental Sciences & Ecology
Forests
Lignin
Mineral-associated organic carbon
Particulate organic carbon
Rubber
Soil
Soil organic carbon
Tropical forest conversions
title Divergent accumulation of amino sugars and lignins mediated by soil functional carbon pools under tropical forest conversion
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