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Afforested and abandoned land ecosystems exhibit distinct soil microbial biomass stoichiometric homeostasis over chronosequence

Bibliographic Data

ID21648150
AuthorsXing Wang (0000-0002-3230-3482, College of Agronomy Northwest A&F University Yangling People's Republic of China), Zhenjiao Zhang (College of Agronomy Northwest A&F University Yangling People's Republic of China), Qi Zhang (0009-0000-5229-2496, College of Agronomy Northwest A&F University Yangling People's Republic of China), Chengjie Ren (0000-0003-4959-3129, College of Agronomy Northwest A&F University Yangling People's Republic of China), Gaihe Yang (0000-0003-4226-9019, College of Agronomy Northwest A&F University Yangling People's Republic of China), Zekun Zhong (Institute of Soil and Water Conservation Northwest A&F University Yangling People's Republic of China, corresponding author), Xinhui Han (0000-0002-7124-4278, College of Agronomy Northwest A&F University Yangling People's Republic of China, corresponding author)
Year2023
Volume34
Issue17
Pages5389-5400
Publication date2023-11-01
Open AccessYes
TypeARTICLE
VenueLand Degradation and Development (JOURNAL)
Journal identifiersISSN: 1085-3278 • E-ISSN: 1099-145X
PublisherWiley (PUBLISHER • GB)
DOI10.1002/ldr.4852
OpenAlexW4385706735
LanguageEN
References cited56

Revegetation influences microbial biomass stoichiometry by altering the substrate conditions, yet the differences in microbial stoichiometry homeostasis and the underlying drivers under different revegetation approaches remain unexplored. Here, we selected sites across three age classes of Robinia pseudoacacia plantation (RP) and abandoned land (AL), and quantified the microbial stoichiometric characteristics during farmland‐initiated restoration. Plant community composition, leaf and soil nutrients, and microbial community composition and diversity were also measured. We found that revegetation of former farmland under both restoration types resulted in non‐isometric changes in soil carbon (C), nitrogen (N), and phosphorus (P) contents, that is, decoupling of soil C and N from P. However, AL and RP succession exhibited homeostatic and plastic microbial biomass stoichiometry, respectively, in response to altered substrate stoichiometry. These differences were associated with adjustments in the above‐ and belowground biomes. Specifically, the synergistic increase of Compositae and Actinobacteria in the late AL succession allowed the ecosystem to reduce P demand and maintain microbial stoichiometric homeostasis. In contrast, higher leaf C and N input during RP succession may have resulted excessive microbial storage of elements, which in turn leads to stoichiometric convergence between microbial biomass and soil resources. In addition, RP succession caused changes in microbial community structure, mainly the continuous increase of Proteobacteria (copiotrophs, r‐strategists), which also potentially increased the requirement for resources to maintain homeostasis and ensure the rapid growth. These findings demonstrate that AL has a comparatively greater efficacy in maintaining microbial stoichiometric homeostasis during long‐term revegetation. Our study also highlights the importance of appropriately managing existing RP plantations to alleviate the pressure of P deficiency and sustainably maintain this fragile ecosystem

Biology · Chronosequence · Ecological stoichiometry · Ecological succession · Ecosystem · Microbial population biology · Revegetation · Environmental Science · Microbial Community Ecology and Physiology · Soil Carbon and Nitrogen Dynamics · Soil erosion and sediment transport · Ecology

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