Soil depth affects bacterial, but not fungal community structure and
assembly in Robinia pseudoacacia planta
Abstract
Afforestation is an effective approach to rehabilitating degraded
ecosystems, but its implementation often causes standing forest soil
microbial communities to fluctuate. It is unknown how changes deep and
forest ages (chronosequence) affect soil microbial diversity and
assembly, hindering our ability to understand the sustainability of
rehabilitated ecosystems. To address this issue, we focused on acquiring
biophysical data from a chronosequence of Robinia pseudoacacia
plantations of 10 to 50 years old in the exploration of soil microbial
(bacterial and fungal) community dynamics associated with variations in
species diversity and assembly. Results showed that soil depth effects
bacterial, but not fungal diversity, the bacterial diversity was
significantly higher in the topsoil than subsoil, while fungal diversity
did not differ between the two soil layers. The composition of both
bacterial and fungal communities (at the phylum level) was significantly
influenced by soil layer and forest age. The assembly processes of soil
bacterial and fungal communities were predominantly driven by
deterministic processes (homogeneous selection). However, with the
increase of forest age, the βNTI values for bacterial communities
significantly decreased in both soil layer, but the βNTI values of
fungal communities significantly increased in the topsoil. Soil carbon
composition (i.e., particulate organic carbon, easily oxidizable organic
carbon) were the main factors regulating the variation of soil bacterial
and fungal assembly processes among different forest ages. Network
analysis showed that the network structure of bacteria in the subsoil
were more complex than in the topsoil, whereas no significant structural
differences were observed in the fungal networks between the two soil
layers. Additionally, study highlights that soil organic carbon (SOC),
particulate organic carbon (POC), easily oxidizable organic carbon
(EOC), and total nitrogen (TN) are key factors influencing microbial
community composition, co-occurrence network, and assembly processes in
different soil layers. Our study demonstrated the importance of soil
carbon composition in the assembly of forest soil microbial community.
These findings offer valuable insights for future research on deep soil
microbial diversity and forest ecosystem succession, particularly in
ecologically fragile regions.