TY - JOUR
T1 - Divergent accumulation of amino sugars and lignins mediated by soil functional carbon pools under tropical forest conversion
AU - Li, Tengteng
AU - Cheng, Hao
AU - Li, Yue
AU - Mou, Zhijian
AU - Zhu, Xiaomin
AU - Wu, Wenjia
AU - Zhang, Jing
AU - Kuang, Luhui
AU - Wang, Jun
AU - Hui, Dafeng
AU - Lambers, Hans
AU - Sardans, Jordi
AU - Peñuelas, Josep
AU - Ren, Hai
AU - Mohti, Azian Binti
AU - Liang, Naishen
AU - Liu, Zhanfeng
N1 - Funding Information:
This work was supported by the Key-Field Research and Development Program of Guangdong Province (No. 2022B1111230001 ), the National Natural Science Foundation of China ( 32201536 and 42177289 ), the Youth Innovation Promotion Association CAS ( 2019340 ), the Environment Research and Technology Development Fund of Environmental Restoration and Conservation Agency of Japan ( JPMEERF20172005 , JPMEERF20202006 ), the Spanish Government projects PID2019-110521GB-I00 and PID2020115770RB-I , Fundación Ramón Areces project CIVP20A6621 and Catalan government project ( SGR2021-1333 ), US National Science Foundation , USDA , and DOE projects.
Publisher Copyright:
© 2023
PY - 2023/7/10
Y1 - 2023/7/10
N2 - 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.
AB - 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.
KW - Amino sugars
KW - Lignin
KW - Mineral-associated organic carbon
KW - Particulate organic carbon
KW - Soil organic carbon
KW - Tropical forest conversions
UR - http://www.scopus.com/inward/record.url?scp=85152130933&partnerID=8YFLogxK
U2 - 10.1016/j.scitotenv.2023.163204
DO - 10.1016/j.scitotenv.2023.163204
M3 - Article
C2 - 37044342
AN - SCOPUS:85152130933
SN - 0048-9697
VL - 881
JO - Science of the Total Environment
JF - Science of the Total Environment
M1 - 163204
ER -