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Aims: Contrasting nutrient-acquisition strategies would explain why species differ in their distribution in relation to soil phosphorus (P) availability, promoting diversity. However, what drives the differential distribution of plant species with the same P-acquisition strategy remains poorly understood. Methods: We selected two Haemodoraceae species, Anigozanthos flavidus and Macropidia fuliginosa, to investigate physiological responses in non-mycorrhizal monocots adapted to different edaphic habitats that vary in P availability. Plants were grown in nutrient solution in large tanks at a range of P concentrations (0, 0.1, 1, 10 µM P). After seven months, we measured growth, photosynthetic rate, net P-uptake capacity, and leaf [P]. Results: Fresh weights of A. flavidus plants were highest at 1 µM P and lowest at 0 µM P. Fresh weights of M. fuliginosa plants were lowest at 10 µM P compared with those at other P levels. Rates of P uptake by A. flavidus showed a steady decline with increasing P level during growth from 0 to 1 µM P, and then a sharp decline from 1 to 10 µM P. Rates of P uptake in M. fuliginosa did not differ among growth P levels, except between 0 and 1 µM P. Both species showed a drastic increase in the concentration of both total P and inorganic P at 10 µM P. Conclusions: The results support our hypothesis that A. flavidus is efficient in down-regulating its P-uptake capacity, while M. fuliginosa is not. Thus, partly explaining the narrower and wider distribution of these species. [ABSTRACT FROM AUTHOR]

Aims: Non-mycorrhizal species such as Banksia (Proteaceae) that depend on root exudates to acquire phosphorus (P) are prominent in south-western Australia, a biodiversity hotspot on severely P-impoverished soils. We investigated the consequences of an exudate-releasing P-mobilising strategy related to control of iron (Fe) acquisition in two Banksia species, B. attenuata R.Br. and B. laricina C. Gardner, that differ greatly in their geographical distribution and rarity. Methods: We undertook solution culture experiments to measure root-mediated Fe reduction (FeR) in non-cluster and cluster roots at four stages of cluster-root development, and whole root systems for plants grown at 2 to 300 μM Fe (as Fe-EDTA). As a positive control, we used Pisum sativum (cv. Dunn) to validate the FeR assay. Results: Unlike typical Strategy I species, both Banksia species showed no significant variation in FeR, for either cluster or non-cluster roots, when grown at a wide range of Fe supply. For roots of different developmental stages, we measured a range for B. attenuata cluster roots of 0.13 ± 0.03 to 1.29 ± 0.14 μmol Fe3+ reduced g−1 FW h−1 and 0.56 ± 0.11 to 1.10 ± 0.24 μmol Fe3+ reduced g−1 FW h−1 in non-cluster roots. Similarly, for B. laricina cluster-roots, FeR ranged from 0.22 ± 0.07 to 1.21 ± 0.37 μmol Fe3+ reduced g−1 FW h−1, and in non-cluster roots from 0.56 ± 0.11 to 0.71 ± 0.08 μmol Fe3+ reduced g−1 FW h−1. We also observed only minor differences for whole-root system FeR, and even though B. attenuata showed signs of leaf Fe deficiency in the 2 μM Fe treatment, its FeR was the lowest of both species across all treatments at 0.079 ± 0.009 μmol Fe3+ reduced g−1 FW h−1, compared with the fastest rate of 0.20 ± 0.014 μmol Fe3+ reduced g−1 FW h−1 for B. laricina in the 28 μM Fe treatment. Taking plants through a pulse from low to high Fe, then back to low Fe supply did not elucidate any significant response in FeR. Conclusions: Although Fe acquisition is tightly controlled in the investigated Banksia species, such control is not based on regulation of FeR, which challenges the model that is commonly accepted for Strategy I species. [ABSTRACT FROM AUTHOR]