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. 2021 Jan 13;11:597745. doi: 10.3389/fmicb.2020.597745

FIGURE 8.

FIGURE 8

Hypothetic model, summarizing the potential interplay between fertilization management, soil factors, root exudation and rhizosphere microbial communities in lettuce-Olpidium interactions. Pathogen-conducive scenarios are indicated by red labels, while green labels represent pathogen-suppressive scenarios. A high drainage potential of the loamy sand soils (HUB-LTE) counteracts the motility of Olpidium zoospores, which is stimulated by low moisture draining in the silty loam soils (DOK-LTE), thereby promoting Olpidium pathogen pressure. In the pathogen suppressive scenario, long-term mineral fertilization reduces the soil AMF inoculum (arbuscular mycorrhizal fungi). Consequently, lower AMF colonization is associated with lower sugar consumption by the fungal partner and with higher sugar exudation. The higher availability of easily accessible carbohydrates attracts rhizosphere colonization by Gammaproteobacteria (i.e., Pseudomonadaceae) and Mortierella with documented plant growth-promoting and pathogen-suppressive properties. This is further promoted by higher root exudation of dicarboxylates (i.e., succinate) with known functions as chemoattractants and substrates for siderophore production in many Pseudomonas species with plant growth-promoting properties. Moreover, Pseudomonas inoculation can stimulate root exudation of benzoate with antifungal properties in lettuce. By contrast, in the pathogen-conducive scenario, high relative abundance of AMF in the rhizosphere associated with high fungal sugar consumption drastically reduces the rhizosphere sugar concentrations of lettuce plants grown in DOK-LTE soils with long-term organic fertilization (BIODYN2), counteracting root colonization by potentially beneficial Pseudomonadaceae and Mortierella species, thereby favoring Olpidium infection. A low C/N ratio in the rhizosphere soil solution, promoted by high background concentrations of amino acids probably related with more intense organic N mineralization under long-term organic fertilization further reduces the relative abundance of Pseudomonadaceae in the rhizosphere (for details, see section “Discussion”). Photos by courtesy of Markus Weinmann, Namis Eltlbany, and Khalid Hameed.