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Nutrient solubilization and uptake facilitation refer to the collective processes, primarily driven by various soil microorganisms (including bacteria such as *Bacillus*, *Pseudomonas*, *Rhizobium*, and fungi such as *Aspergillus*) that convert nutrients from insoluble forms (such as mineral phosphates or organic nitrogen) into soluble ions (like phosphate, ammonium, nitrate) available for plant absorption[3][5][4]. These mechanisms are critical for plant health and agricultural productivity and include secretion of organic acids, production of extracellular enzymes (e.g. phosphatases for phosphate, proteases for nitrogen), and establishment of symbiotic relationships (such as mycorrhizae, or Rhizobium-legume nodulation)[3][5][4]. Microbes may regulate pH in the rhizosphere, produce chelating or redox-active metabolites, or express membrane-bound transporters that facilitate the movement of solubilized nutrients into microbial or plant cells[2][5]. There is no single receptor or protein responsible for "nutrient solubilization and uptake facilitation"—it is a multi-component process involving different gene products and microbial metabolic pathways[3][5][4]. *Note:* The phrase as given is too broad and not referring to a defined therapeutic or molecular target; it describes a microbial ecological function rather than an individual molecule, receptor, transporter, or enzyme. For specific molecular targets, one should focus on individual proteins (e.g., phosphate transporter, nitrogenase, phosphatase) involved in these processes[3][5][4].
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