Soil Labile Organic Carbon and Nitrate Nitrogen are the Main Factors Driving Carbon-Fixing Pathways During Vegetation Restoration in the Loess Plateau, China

47 Pages Posted: 1 Apr 2024

See all articles by Yujie Liang

Yujie Liang

affiliation not provided to SSRN

Rong Fu

affiliation not provided to SSRN

Ahejiang Sailike

affiliation not provided to SSRN

Yangyang Liu

Northwest Agricultural and Forestry University

Zhouchang Yu

affiliation not provided to SSRN

Rong Wang

affiliation not provided to SSRN

Ning Peng

affiliation not provided to SSRN

Shicai Li

affiliation not provided to SSRN

Wei Zhang

affiliation not provided to SSRN

Yangyang Liu

affiliation not provided to SSRN

Abstract

Microbial fixation of CO2 is a crucial pathway in the regulation of soil carbon cycling, however, the microbial carbon fixation pathways and their driving factors among different vegetation types remain unclear. Therefore, soil physicochemical properties, soil organic carbon (SOC), carbon-fixing microorganisms, and carbon sequestration genes in a farmland (FL) and four typical vegetation types (Robinia pseudoacacia (RP), Caragana korshinskii (CK), Prunus sibirica (PS), and grassland (GL) in the Wuliwan watershed were identified using macro-genome sequencing and other analytical methods. The results showed that SOC content increased in the following order: RP>CK>PS~GL>FL (P <0.05). The proportion of recalcitrant organic carbon (ROC) increased, whereas that of labile organic carbon (LOC) decreased. Among the six carbon fixation pathways identified, the DC/4-HB cycle had the highest relative abundance of 25.10%-25.52%. Changes in the type of vegetation restoration caused a significant difference (P<0.05) in the relative abundance of carbon-fixing microorganisms, with Actinobacteria and Proteobacteria being the most prevalent. From a carbon perspective, LOC has a closer relationship with carbon-fixing microorganisms and carbon-fixing pathways than does ROC. Furthermore, there was a significant positive correlation (P<0.05) between the composition and function of these microorganisms and soil nutrients like soil total nitrogen (STN), soil ammonium nitrogen (SAN), and soil nitrate nitrogen (SNN), and a negative correlation with soil bulk density (SBD) and pH. Using a random forest model, we predicted that the rTCA cycle would significantly influence SOC. In conclusion, this study explored the link between soil organic carbon and microbial composition and metabolic processes in different vegetation restoration types, which provides a new reference for soil carbon uptake mechanisms.

Keywords: Loess Plateau, planted forest, Vegetation restoration, microbial carbon sequestration pathways

Suggested Citation

Liang, Yujie and Fu, Rong and Sailike, Ahejiang and Liu, Yangyang and Yu, Zhouchang and Wang, Rong and Peng, Ning and Li, Shicai and Zhang, Wei and Liu, Yangyang, Soil Labile Organic Carbon and Nitrate Nitrogen are the Main Factors Driving Carbon-Fixing Pathways During Vegetation Restoration in the Loess Plateau, China. Available at SSRN: https://ssrn.com/abstract=4780178 or http://dx.doi.org/10.2139/ssrn.4780178

Yujie Liang

affiliation not provided to SSRN ( email )

Rong Fu

affiliation not provided to SSRN ( email )

Ahejiang Sailike

affiliation not provided to SSRN ( email )

Yangyang Liu

Northwest Agricultural and Forestry University ( email )

China

Zhouchang Yu

affiliation not provided to SSRN ( email )

Rong Wang

affiliation not provided to SSRN ( email )

Ning Peng

affiliation not provided to SSRN ( email )

Shicai Li

affiliation not provided to SSRN ( email )

Wei Zhang (Contact Author)

affiliation not provided to SSRN ( email )

Yangyang Liu

affiliation not provided to SSRN ( email )

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