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Journal ArticleDOI

A 31P nuclear magnetic resonance study of phosphate levels in roots of ectomycorrhizal and nonmycorrhizal plants of Castanea sativa Mill.

TL;DR: The level of orthophosphate in mycorrhizal roots was significantly lower than in nonmycorrhIZal ones, which indicates that this system relies upon the fungal polyphosphates as a major source of phosphate.
Abstract: 31P-Nuclear Magnetic Resonance (NMR) was used to assess phosphate distribution in ectomycorrhizal and nonmycorrhizal roots of Castanea sativa Mill. as well as in the mycorrhizal fungus Pisolithus tinctorius in order to gain insight into phosphate trafficking in these systems. The fungus P. tinctorius accumulated high levels of polyphosphates during the rapid phase of growth. Mycorrhizal and nonmycorrhizal roots accumulate orthophosphate. Only mycorrhizal roots presented polyphosphates. The content in polyphosphates increased along the 3 months of mycorrhiza formation. In mycorrhizal roots of plants cultured under axenic conditions, the orthophosphate pool decreased along the culture time. In nonmycorrhizal roots the decrease in the orthophosphate content was less pronounced. The level of orthophosphate in mycorrhizal roots was significantly lower than in nonmycorrhizal ones, which indicates that this system relies upon the fungal polyphosphates as a major source of phosphate.

Summary (2 min read)

Introduction

  • The increase in phosphate concentration in mycorrhizal plants was also correlated with increased photosynthetic rates, as the phosphate level of the chloroplast influences photosynthetic rates (Osmond 1981; Coombs 1985; Foyer and Spencer 1986; Jakobsen 1991) .
  • It was suggested that phosphate is translocated along hyphae as polyphosphate granules inside vacuoles (Cox et al. 1980 ).

Materials and methods

  • Castanea sativa micropropagated plants were obtained as previously described (Martins et al. 1996) .
  • The fungus Pisolithus tinctorius (Pers.) Coker and Couch isolate 289/Marx kindly supplied by Dr. Ingrid Kottke (Tübingen University) was maintained on a MMN solid medium (Marx 1969) .

Mycorrhizal synthesis

  • Fungus was inoculated 3 weeks before plant transfer.
  • In vitro mycorrhization of micropropagated plants was induced 4-5 weeks after plant rooting, by transfer of rooted plants to the petri dishes inoculated 3 weeks before with mycelium.
  • A portion of the petri dishes with roots was covered with aluminum foil to prevent oxidation of root phenols by light.
  • Control plants were transferred to petri dishes without fungus and maintained under the same conditions.

Sample preparation for NMR

  • Samples of excised root systems of mycorrhizal or control plants as well as samples of pure cultures of the fungus were prepared for NMR analysis.
  • Similar masses of material and similar packing were used in the different experiments.
  • Two glass capillaries were fitted into the NMR tube, one positioned a few millimeters from the bottom (inlet of medium) and the other just above the cotton wool filter that was used to restrict the volume of the biological material (outlet of medium).
  • The acquisition time of each spectrum was approximately 40 min.
  • In all the experiments, the probe head temperature was kept at 25°C.

Phosphate quantification

  • Extraction of total P from roots leaves and stems of mycorrhizal and nonmycorrhizal plants was performed according to Bowman (1988) .
  • Phosphate quantification was made 30, 40, 60 and 90 days after mycorrhizal induction in vitro by the molybdenum blue method according to John (1970) .

Results and discussion

  • 31 P-NMR spectra of the fungus samples, either in pure culture or extramatrical hyphae collected from petri dishes containing 1-month-old mycorrhizas, showed the presence of resonances due to the vacuolar orthophosphate pool and the polyphosphates pool (Fig. 1 ) as al-ready reported for P. tinctorius (Ashford et al. 1994 ) and for other fungi (Martin et al.
  • When present in a P-limiting medium, the stored polyphosphates are hydrolyzed, releasing Pi and maintaining Pi concentration within the fungal cell (Martin et al. 1985; MacFall et al. 1992) .
  • Chestnut mycorrhizas are able to accumulate phosphate, mostly in the form of polyphosphates, in contrast to nonmycorrhizal roots, which accumulate only orthophosphate (Fig. 2 ).
  • The differences in phosphate content between mycorrhizal and nonmycorrhizal plants decreased with time.

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Citations
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Book ChapterDOI
01 Jan 2008
TL;DR: In vitro mycorrhization under controlled conditions can provide important information about the physiology of symbiosis and the assessment of symbiotic establishment takes into account the formation of a mantle and a hartig net that were already developed at 30 days, when differences between fresh and dry weights of mycor rhizal and nonmycorrhizal plants can be quantified.
Abstract: In vitro mycorrhization can be made by several axenic and nonaxenic techniques but criticism exists about their artificiality and inability to reproduce under natural conditions. However, artificial mycorrhization under controlled conditions can provide important information about the physiology of symbiosis. Micropropagated Castanea sativa plants were inoculated with the mycorrhizal fungus Pisolithus tinctorius afterin vitro rooting. The mycorrhizal process was monitored at regular intervals in order to evaluate the mantle and hartig net formation, and the growth rates of mycorrhizal and nonmycorrhizal plants. Plant roots show fungal hyphae adhesion at the surface after 24 h of mycorrhizal induction. After 20 days a mantle can be observed and a hartig net is forming although the morphology of the epidermal cells remains unaltered. At 30 days of root-fungus contact the hartig net is well developed and the epidermal cells are already enlarged. After 50 days of mycorrhizal induction, growth was higher for mycorrhizal plants than for nonmycorrhizal ones. The length of the major roots was lower in mycorrhizal plants after 40 days. Fresh and dry weights were higher in mycorrhizal plants after 30 days. The growth rates of chestnut mycorrhizal plants are in agreement with the morphological development of the mycorrhizal structures observed at each mycorrhizal time. The assessment of symbiotic establishment takes into account the formation of a mantle and a hartig net that were already developed at 30 days, when differences between fresh and dry weights of mycorrhizal and nonmycorrhizal plants can be quantified. In vitro conditions, mycorrhization influences plant physiology after 20 days of root–fungus contact, namely in terms of growth rates. Fresh and dry weights, heights, stem diameter and growth rates increased while major root growth rate decreased in mycorrhizal plants.

20 citations


Cites background from "A 31P nuclear magnetic resonance st..."

  • ...…that the increased photosynthetic rates are related with the fungus necessity of carbon compounds and is named source-sink concept (Dosskey et al., 1990; 1991) although this seems to be just one of mechanism involved in photosynthetic increment in mycorrhizal plants (Martins et al., 1997; 1999)....

    [...]

  • ...…distinct forms: increased absorption of P and N in mycorrhizal plants influence the photosynthetic rates, as observed for forestry species when amended with P; the other resulting from enhanced flux of carbon compounds to the roots, promoted by mycorrhizal associations (Martins et al., 1997; 1999)....

    [...]

Book ChapterDOI
01 Jan 2012
TL;DR: Arbuscular mycorrhizal associations have now been recognized having a cosmopolitan and ubiquitous occurrence forming with the roots and underground portions of plants, and are being widely used as biological fertilizer at commercial level in many countries of the world.
Abstract: Arbuscular mycorrhizal (AM) associations have now been recognized having a cosmopolitan and ubiquitous occurrence forming with the roots and underground portions of plants. AM associations have been reported to enhance plant vigor by enabling them to absorb more nutrients. The thread like hyphae of the fungi work as conduits for pumping essential nutrients into the plant body, thereby imparting plant ample amount of resistance to combat with the soil born and other diseases. Due to these promising features of AM, they are being widely used as biological fertilizer at commercial level in many countries of the world and it has considerable practical significance in sustainable agricultural practices.

1 citations

References
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Book ChapterDOI
26 Oct 2015

3,503 citations

Book ChapterDOI
01 Jan 1996
TL;DR: In this article, Bremner et al. defined the nonexchangeable NHt as the NHt in soil that cannot be replaced by a neutral potassium salt solution (SSSA, 1987), in contrast to NHt which is extractable at room temperature with such a solution.
Abstract: Most soils contain inorganic nitrogen (N) in the form of ammonium (NHt) and nitrate (NO)"). Nitrite (NOz) also may be present, but the amount is usually too small to warrant its determination, except in cases where NHt or NHt-forming fertilizers are applied to neutral or alkaline soils. Several other forms of inorganic N have been proposed as intermediates during microbial transformations of N in soils, including hydroxylamine (NH20H), hyponitrous acid (H2N20 2), and nitramide (NH2N02), but these compounds are thermodynamically unstable and have not been detected in soil. Until the 1950s, inorganic N was believed to account for <2% of total soil N, on the assumption that NHt and NO)" are completely recovered by extracting soil with a neutral salt solution. The validity of this assumption was challenged by the finding that some soils contain NHt in a form that is not extracted by exchange with other cations (e.g., Rodrigues, 1954; Dhariwal & Stevenson, 1958; Stevenson & Dhariwal, 1959; Bremner & Harada, 1959; Bremner, 1959; Schachtschabel, 1960, 1961; Young, 1962), and by estimates that the proportion of soil N in this form can exceed 50% for some subsurface soils (Stevenson & Dhariwal, 1959; Young, 1962). In such cases, NHt is said to be fixed, and fixed NHt has subsequently been defined as the NHt in soil that cannot be replaced by a neutral potassium salt solution (SSSA, 1987), such as 1 or 2 M KCI or 0.5 M K2S04, in contrast to exchangeable NHt, which is extractable at room temperature with such a solution. Existing information indicates that fixed NHt occurs largely, if not entirely, between the layers of 2: I-type clay minerals, particularly vermiculite and illite (hydrous mica), and that fixation results from entrapment of NHt in ditrigonal voids in the exposed surfaces upon contraction of the clay lattice (Nommik & Vahtras, 1982). The term, nonexchangeable NHt, has been used by Bremner (1965) and Keeney and Nelson (1982) in previous editions of this publication as a more precise alternative to fixed NHt. The same term is used in the present treatment, with specific reference to NHt determined by the method described in "Determination of Nonexchangeable Ammonium," which involves digestion with an HF-HCI solution following treatment of the soil with alkaline KOBr to remove exchangeable NHt and labile organic-N compounds.

2,810 citations

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Q1. What are the contributions in this paper?

Martins et al. this paper found that mycorrhizal and nonmycizal roots accumulate orthophosphate, which indicates that this system relies upon the fungal polyphosphates as a major source of phosphate.