Dynamics of soil microbial C:N:P stoichiometry and its driving mechanisms following natural vegetation restoration after farmland abandonment
- 1. University of Chinese Academy of Sciences, Beijing 100049 (China)
- 2. State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation, Chinese Academy of Sciences and Ministry of Water Resources, Yangling, Shaanxi 712100 (China)
- 3. College of Forestry, Northwest A&F University, Yangling, Shaanxi 712100 (China)
- 4. Institute of Soil and Water Conservation, Northwest A&F University, Yangling, Shaanxi 712100 (China)
Description
Highlights: • Natural vegetation restoration increased microbial C:P and N:P ratios since farmland abandonment. • Natural succession aggravated microbial P limitation after farmland abandoned. • Microorganism remained elemental homeostatic regulation to resist P limitation. • Fungi played a strong role in shaping microbial elemental homeostasis and nutrient cycling. -- Abstract: Vegetation restoration after farmland abandonment has increased greatly and is commonly used to improve soil fertility and ecosystem service. Knowledge of soil community-level elemental homeostasis following natural vegetation restoration is specially limited for the abandoned farmlands. This study examined the changes in soil microbial biomass stoichiometry and homeostasis with a chronosequence of 3, 8, 13, 18, 23 and 30 years following natural vegetation restoration since farmland abandonment on the Loess Plateau, China. Vegetation communities, soil properties, microbial communities, and enzyme activities were analyzed to study the drivers on soil microbial C:N:P stoichiometry. The results showed that soil microbial biomass C: N ratios had little change following natural vegetation restoration since farmland abandonment, natural vegetation >23 years had significantly enhanced the microbial biomass C:P and N:P ratios by 26.1%–133.9% and 31.7%–67.4%, respectively. However, microbial biomass C:N, C:P and N:P ratios were constrained following natural vegetation restoration. Vegetation restoration for 30 years enhanced urease and alkaline phosphatase activities by 125.4% and 42.9%, respectively, which showed synchronous changes with N and P contents in microbial biomass. Soil fungi, urease and alkaline phosphatase were the drivers to the changes in microbial C:N:P stoichiometry. The results suggest that long-term vegetation restoration (>23 years) will aggravate microbial P limitation, however, soil microorganism maintained the homeostatic regulation of stoichiometric ratios to mitigate P limitation. Fungi played a strong role in shaping microbial community-level elemental homeostasis and nutrient cycling through releasing N-converting and P-converting enzymes into soil following natural vegetation restoration.
Additional details
Additional titles
- Augmented title (English)
- Ecological restoration;Fungi and bacteria;Homeostatic regulation;Soil enzyme;Soil microorganism;Stoichiometric ratios
Identifiers
- DOI
- 10.1016/j.scitotenv.2019.133613;
- PII
- S0048969719335387;
Publishing Information
- Journal Title
- Science of the Total Environment
- Journal Volume
- 693
- Journal Page Range
- vp.
- ISSN
- 0048-9697
- CODEN
- STENDL
INIS
- Country of Publication
- Netherlands
- Country of Input or Organization
- International Atomic Energy Agency (IAEA)
- INIS RN
- 55104053
- Subject category
- S54: ENVIRONMENTAL SCIENCES; S09: BIOMASS FUELS;
- Descriptors DEI
- ACID NEUTRALIZING CAPACITY; ALKALINE PHOSPHATASE; BACTERIA; BIOMASS; CHINA; COMMUNITIES; FUNGI; HOMEOSTASIS; MICROCOSMS; NITROGEN; NUTRIENTS; REGULATIONS; REMEDIAL ACTION; SOILS; STOICHIOMETRY; UREASE
- Descriptors DEC
- AMIDASES; ASIA; CHEMISTRY; ELEMENTS; ENERGY SOURCES; ENZYMES; ESTERASES; HYDROLASES; LAWS; MICROORGANISMS; NONMETALS; NON-PEPTIDE C-N HYDROLASES; ORGANIC COMPOUNDS; PHOSPHATASES; PLANTS; PROTEINS; RENEWABLE ENERGY SOURCES; WATER CHEMISTRY
Optional Information
- Copyright
- Copyright (c) 2019 Elsevier B.V. All rights reserved.