1Phosphate starvation response (PSR) in non-mycorrhizal plants comprises transcriptional reprogramming 2 resulting in severe physiological changes to the roots and shoots and repression of plant immunity. Thus, 3 plant-colonizing microorganisms -the plant microbiota -are exposed to direct influence by the soil's 4 phosphorous (P) content itself, as well as to the indirect effects of soil P on the microbial niches shaped 5 by the plant. The individual contribution of these factors to plant microbiota assembly remains unknown. 6To disentangle these direct and indirect effects, we planted PSR-deficient Arabidopsis mutants in a long-7 term managed soil P gradient, and compared the composition of their shoot and root microbiota to wild 8 type plants across different P concentrations. PSR-deficiency had a larger effect on the composition of 9 both bacterial and fungal plant-associated microbiota composition than P concentrations in both roots 10 and shoots. The fungal microbiota was more sensitive to P concentrations per se than bacteria, and less 11 depended on the soil community composition. 12Using a 185-member bacterial synthetic community (SynCom) across a wide P concentration gradient in 13 an agar matrix, we demonstrated a shift in the effect of bacteria on the plant from a neutral or positive 14 interaction to a negative one, as measured by rosette size. This phenotypic shift is accompanied by 15 changes in microbiota composition: the genus Burkholderia is specifically enriched in plant tissue under P 16 starvation. Through a community drop-out experiment, we demonstrate that in the absence of 17Burkholderia from the SynCom, plant shoots accumulate higher phosphate levels than shoots colonized 18 with the full SynCom, only under P starvation, but not under P-replete conditions. Therefore, P-stressed 19 plants allow colonization by latent opportunistic competitors found within their microbiome, thus 20 exacerbating the plant's P starvation. 213The microbial community composition in soil, while governed by its own set of ecological processes [19], 30 has an immense influence on the composition of the plant microbiota [20][21][22]. Correlations with soil 31 microbial diversity, and by derivation, with plant microbiota composition and diversity, were observed for 32 soil abiotic factors such as pH [19,[23][24][25], drought [25][26][27][28][29][30] and nutrient concentrations [19,25,[31][32][33][34][35]. Soil 33 nutrient concentrations, in particular orthophosphate (Pi) -the only form of phosphorous (P) that is 34 available to plants -produce comparatively modest to unmeasurable changes in microbial community 35 composition [35,36]. Nevertheless, available soil Pi concentrations influences where a plant-microbe 36 interaction lies along the mutualism-pathogenicity continuum [17]. 37 Non-mycorrhizal plants respond to phosphate limitation by employing a range of phosphate starvation 38 response (PSR) mechanisms. These manifest as severe physiological and morphological changes to the 39 root and shoot, such as lateral ...