Biodiv Sci ›› 2022, Vol. 30 ›› Issue (10): 22435. DOI: 10.17520/biods.2022435
Special Issue: 土壤生物与土壤健康
• Reviews • Previous Articles Next Articles
Shenglei Fu1,*(), Manqiang Liu2, Weixin Zhang1, Yuanhu Shao1
Received:
2022-07-30
Accepted:
2022-10-11
Online:
2022-10-20
Published:
2022-10-22
Contact:
Shenglei Fu
Shenglei Fu, Manqiang Liu, Weixin Zhang, Yuanhu Shao. A review of recent advances in the study of geographical distribution and ecological functions of soil fauna diversity[J]. Biodiv Sci, 2022, 30(10): 22435.
Fig. 1 The distribution of species richness of representative soil fauna along latitudes in northern hemisphere. Species richness in panels a-f refers to the mean value of species richness within a specific latitude range for a given group of soil fauna; data for collembola within 10°-20° N was shown, instead of that within 20°-30° N since the data was not available; data for termite within 40°-50° N, instead of that within 50°-60° N, was shown since almost no termite was reported in further northern regions with higher latitude. Data sources: earthworm (Phillips et al, 2019), termite (Deca?ns, 2010), oribatid mite (Maraun et al, 2007; Deca?ns, 2010), collembola (Potapov et al, 2022a) and nematode (Boag & Yeates, 1998).
Fig. 2 The changes in sampling sites of soil fauna community in China. The legend of “sampling sites during 2010-2020” refers to the new sampling sites during 2010-2020 based on literature analysis from CNKI; while the “sampling sites before 2010” refers to the sampling sites during 1980-2008 in studies represented by Yin et al, and the main data sources are from monographs edited by Yin, 1992, 2000; Zhao & Xie, 1996; Yin, 2001; Zhang, 2006; Liao & Li, 2009.
Fig. 3 Conceptual diagram of pathways for the effects of soil fauna on soil multifunctionality. Soil fauna have different effects on soils, litters and plant roots, among which, macrofauna (e.g. earthworm), mesofauna (e.g. springtail) and microfauna (e.g. nematode) potentially show the strong impact on soils, litters and plant roots, respectively. These changes can directly affect soil properties, as well as indirectly affect soil microbial properties such as microbial biomass, diversity and activity via modifying soil abiotic properties, e.g., pH, soil organic matter (SOM), nutrient and aggregate. Finally, these changes could also positively or negatively affect soil multifunctionality, such as the improvement of soil structure, the transformation of soil organic matter and the maintaining of plant health. The arrow width is proportional to the strength of the relationship. Solid and dashed arrows indicate direct and indirect effects, respectively.
Fig. 4 A schematic diagram showing energetic structure of soil micro-food webs and their relation to ecosystem multifunctionality. The C refers to the flux of energy through a given taxa of consumption, i.e., CH, CF, CB indicates flux of energy through herbivores, fungivores and bacterivores, respectively. The flux of energy through microbivores (CF and CB) has been shown to be related to litter decomposition and nutrient cycling, while the flux of energy through herbivores is typically related to plant productivity, and the flux of energy through predators is related to top-down controls on ecosystem drivers. The flow uniformity of energy in the soil micro-food web indicates the energy distribution of different channels, which determines the functional stability of food webs. Resources exert strong effects on the energetic structure of food webs by shifting the diversity and composition of soil micro-food webs. These shifts in soil biodiversity and composition could optimize the energetic structure of soil micro-food webs to support ecosystem services.
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