How significant to plant N nutrition is the direct consumption of soil microbes by roots?

Summary –The high degree to which plant roots compete with soil microbes for organic forms of nitrogen (N) is becoming increasingly apparent. This has culminated in the finding that plants may consume soil microbes as a source of N, but the functional significance of this process remains unknown. –We used 15N- and 14C-labelled cultures of soil bacteria to measure rates of acquisition of microbes by sterile wheat roots and plants growing in soil. We compared these rates with acquisition of 15N delivered as nitrate, amino acid monomer (l-alanine) and short peptide (l-tetraalanine), and the rate of decomposition of [14C] microbes by indigenous soil microbiota. –Acquisition of microbe 15N by both sterile roots and roots growing in soil was one to two orders of magnitude slower than acquisition of all other forms of 15N. Decomposition of microbes was fast enough to account for all 15N recovered, but approximately equal recovery of microbe 14C suggests that microbes entered roots intact. –Uptake of soil microbes by wheat (Triticum aestivum) roots appears to take place in soil. If wheat is typical, the importance of this process to terrestrial N cycling is probably minor in comparison with fluxes of other forms of soil inorganic and organic N.


Introduction
Nitrogen (N) is a key factor in the control of primary productivity in terrestrial systems (Vitousek & Howarth, 1991;Liu & Greaver, 2010). Consequently, a mechanistic understanding of the processes controlling its availability to photosynthetic organisms is crucial not only to provide a wider understanding of the N cycle, but also to make predictions of carbon (C) residence in the terrestrial biosphere. However, the paradigm of plant-soil N cycling has shifted repeatedly over the last few decades and significant breakthroughs continue to be made.
Historically, it was thought that plants derived all of their N nutrition from the inorganic forms of N, NO À 3 and NH þ 4 . However, the principal form of N entering soils not receiving additions of inorganic fertilisers is protein derived from dead portions of plants, animals or microbes. Consequently, it was thought that protein must be cleaved by microbial extracellular proteases and taken up by microbes as amino acids before inorganic N could become available to plants. In many soils, soil microbes are C limited and often excrete much of the N acquired in amino acids as inorganic N (Schimel & Bennett, 2004;Roberts et al., 2009). By contrast, as photosynthetic organisms, plants generally have an abundant supply of C and are frequently limited by N. Thus, if plants acquire N only in inorganic forms, their competition with soil microbes for N-containing compounds is generally low. However, it is now widely accepted that plants are able to compete with soil microbes for more complex N-containing compounds, when proteins are cleaved only to amino acids (Borstlap, 1983;Chapin et al., 1993;Jones & Darrah, 1994;N€ asholm et al., 2009;Paungfoo-Lonhienne et al., 2012). Further, it has recently become apparent that plants and soil microbes are both able to acquire amino acids when proteins have been cleaved only to short peptides (Komarova et al., 2008;Hill et al., 2011aHill et al., , b,c, 2012Soper et al., 2011;Farrell et al., 2012). Due probably principally to methodological constraints and variation between ecosystems, the exact importance of organic N to plant N nutrition remains uncertain (Jones et al., 2005;N€ asholm et al., 2009;Hill et al., 2011a;Paungfoo-Lonhienne et al., 2012). Nevertheless, although the limiting element may differ between organisms, it is clear that fierce competition for soil organic N exists between plant roots and soil microbes.
In the quest for adequate N nutrition, some angiosperms have developed specialized structures to acquire nutrients via carnivory. Recent evidence has shown that entry of the prey-derived protein into the carnivorous plant can occur partially by endocytosis (Adlassnig et al., 2012). More surprisingly, it has also been shown that intact proteins may be acquired endocytotically by nonspecialist, nonmycorrhizal plant roots (Arabidopsis thaliana and Hakea actites; Paungfoo-Lonhienne et al., 2008).
Phagomixotrophic ingestion of intact microorganisms is widespread amongst algae and endocytosis of prokaryotes is the probable origin of photosynthesis in eukaryotes (Raven et al., 2009 recently direct uptake and digestion of microbes by angiosperms for nutritional purposes has been unrecognized (Rosenblueth & Martinez-Romero, 2006;Hardoim et al., 2008;Reinhold-Hurek & Hurek, 2011). However, it has recently been demonstrated that microbes are acquired by the roots of angiosperms and that their associated N can be used nutritionally by the plants (Paungfoo-Lonhienne et al., 2010). This discovery represents a potential step change in our understanding of competition for resources between soil microbes and plants, and how N is cycled in the terrestrial biosphere. What is not currently clear is what the quantitative significance of this process is when compared with other routes of plant N acquisition from soil. This investigation was predicated on the need to evaluate the significance of this new route of N acquisition to plants when growing alone in sterile media and in soil. As our model angiosperm we chose to use the widely investigated and agriculturally important crop plant, wheat (Triticum aestivum). Wheat has previously been shown to utilize N forms ranging in organism or protein decomposition state from short L-peptides to NO À 3 (N€ asholm et al., 2001;Hill et al., 2011c). We aimed to make a comparison of the rate of direct plant N acquisition from soil as intact bacteria with that as peptide, amino acid or inorganic N.

Soil
Agricultural Brown Earth soil (FAO classified as a Eutric Cambisol) was sampled (0-10 cm; n = 4) from Henfaes Agricultural Research Station, Abergwyngregyn, Bangor (53°14′N, 4°01′W). Upon return to the laboratory the soil was sieved to pass 5 mm, removing stones, earthworms and vegetation. Soil solution was collected via centrifugal drainage (Giesler & Lundstr€ om, 1993) and passed through a 1 kDa ultrafiltration membrane (Millipore). The collected soil solution was analysed for amino acids by the fluorometric method of Jones et al. (2002), before and after hydrolysis in 6 M HCl at 105°C for 16 h under N 2 . Fresh soil was extracted with 0.5 M K 2 SO 4 (1 : 5 w/v) and analysed for NO À 3 and NH þ 4 , according to Miranda et al. (2001) and Mulvaney (1996), respectively, and total extractable C and N using a Shimadzu TOC-V-TN analyser (Shimadzu Corp., Kyoto, Japan). Microbial biomass C and N were determined by measuring total K 2 SO 4 -extractable C and N before and after chloroform fumigation according to Voroney et al. (2008) (K EC = 0.35; K EN = 0.5). Soil moisture content was determined by oven drying at 105°C. The pH and electrical conductivity of the soil (1 : 5 w/v distilled water extract) were determined using standard electrodes. Soil total C and N were measured in a Carlo Erba NA 1500 Elemental Analyzer (Thermo Fisher Scientific, Milan, Italy).

Culture of soil microbes
15 N-labelled microbes Soil microbial cultures were obtained by adding c. 2 mg of soil to 50 ml of sterile (0.2 lm filtered) nutrient solution, in a sterile 250 ml Erlenmeyer flask, with a foam stopper. The nutrient solution contained cycloheximide (10 lg ml À1 ) to minimize growth of hyphal fungi, and the following macronutrients (in mM): KH 2 PO 4 , 8.0; MgSO 4 , 2.0; CaCl 2 , 0.2; KNO 3 , 1.0; glycine, 2.0. Glucose (50 mM) was added as a C source and micronutrients were included as Kao and Michayluk vitamin mixture (Sigma-Aldrich, Gillingham, UK) at a concentration of 1 : 100 (v/v). The soil and nutrient solution were incubated aerobically on a rotary shaker at 75 rpm at 20°C. After 3 d, 1 ml of the microbial suspension was added to 50 ml of new nutrient solution, as above, except without cycloheximide. After a further 3 d of incubation, 1 ml of the microbial suspension was sub-sampled and suspended in 50 ml of new media containing K 15 NO 3 , in replacement of the unlabelled KNO 3 , at the same concentration as above. This last step was repeated to ensure that microbial N was effectively all 15 N. After the final incubation, the microbial suspension was centrifuged at 4500 g for 10 min. The supernatant was discarded and the pellet was washed with 0.01 M CaCl 2 . The washing procedure was repeated twice, followed by re-suspension of the pellet in 20 ml of 0.01 M CaCl 2 . Total organic C and N of the microbial suspension were measured on the Shimadzu TOC-V-TN analyser. The suspension was subsequently diluted in 0.01 M CaCl 2 to make a final concentration of 1 mmol N l À1 (c. 6 mmol C l À1 ). The solution was used immediately following preparation. Haemocytometer counts found microbe numbers in the injected solution to be c. 8 9 10 6 cells ml À1 . 14 C-labelled microbes In order to sensitively measure plant incorporation of microbial C, a second culture of 14 C-labelled microbes was prepared. Due to constraints on stable isotope analysis, it was not possible to dual-label microbes with 15 N and 14 C. Initially the 14 C-labelled microbes were prepared in the same way as the 15 N-labelled microbes. However, after the second incubation 2 MBq of [U À14 C] glucose was added to the nutrient solution. To ensure high 14 C incorporation, the unlabelled glucose in the nutrient solution was reduced from 50 mM to 50 lM. After 2 d of incubation the washing procedure described above was carried out. The solution was diluted to 1 mmol N l À1 , and the 14 C activity in the microbial suspension was determined by liquid scintillation counting in a Wallac 1404 scintillation counter (Perkin-Elmer Life Sciences, Boston, MA, USA) after mixing with Scintisafe scintillation cocktail (Fisher Scientific, Loughborough, UK).

Uptake of N forms by plants growing in soil
Seeds of wheat (Triticum aestivum L. var. AC Barrie) were sown singly into rhizotubes (240 mm long; internal diameter 8 mm; Owen & Jones, 2001) containing 12 g of field-moist soil ( Table 1). The plants were grown at 15°C, 70% relative humidity and 16 h photoperiod (c. 500 lmol photons m À2 s À1 PAR) until the third leaf stage (root weight 0.03 AE 0.002 g DW; mean AE SEM; n = 23). Injections of 0.5 ml of the N-treatments were made into the rhizosphere halfway up the rhizotube, (i.e. at a depth of 12 cm) using sterile 1 ml polypropylene syringes with 18G needles. Rhizotubes allowed injection of solutes and . 14 C-labelled material was combusted in an OX400 Biological Oxidiser (Harvey Instruments Corp., Hillsdale, NJ, USA). Liberated 14 CO 2 was captured in Oxosol Scintillant (National Diagnostics, Atlanta, GA, USA) and 14 C activity measured by liquid scintillation counting. Three plants were retained as 15 N and 13 C background enrichment controls. Three rhizotubes were injected with 0.5 ml of blue ink to estimate how much root and soil came into contact with the injected solution. The resulting blue section was cut out of the rhizotube and roots were washed, dried (80°C) and weighed. A further four rhizotubes had the same section cut out to determine pre-injection pools of soil soluble N with which injected solutions mixed. Soil from these sections was extracted for 5 min in 6 ml of de-ionized water. Nitrate, amino acids and short peptides (< 1 kDa) in the extract were measured as for the starting soil or soil solution. Roots from rhizotubes used to determine soil N pools were washed, cleared in 10% w/v KOH, stained in 0.25% w/v aniline blue and inspected for mycorrhizal colonization by light microscopy after destaining and mounting in 80% w/v lactic acid.

Uptake of N forms by sterile plants
Seeds were surface sterilized in sodium hypochlorite (10-14% available chlorine) with one drop of Tween-20, for 10 min followed by 80% v/v ethanol for 1 min. Seeds were then washed thoroughly in sterile distilled water. Seeds were placed on agar plates to germinate, following which, they were transferred to 114 9 86 9 102 mm Phytatrays (Sigma-Aldrich). Phytatrays contained 10 g of sterile (autoclaved) perlite, with 60 ml of sterile 50% Long Ashton nutrient solution (containing Na-metasilicate). Plants were kept under the same conditions as the wheat grown in soil. Upon reaching the third leaf stage, the plants were removed from the perlite and rinsed thoroughly with distilled water and 0.01 M CaCl 2 as for plants grown in soil. The intact roots of three plants per treatment were submerged individually in sterile containers containing 4 ml of either 1 mM K 15 NO 3 , 1 mM [ 13 C 15 N] L-alanine, 250 lM [ 13 C 15 N] L-tetraalanine or 15 N labelled microbes (1 mmol N l À1 ). Solutions not containing cultured microbes were sterilized by filtration to 0.2 lm before use. After 1 h under the same conditions as when growing, plants were removed from solutions and washed, dried and weighed as above. Root and shoot were ground together before mass spectrometer analysis.
The diameter of fresh roots (n = 10) of three plants grown in sterile culture was measured using a micrometer. Root length was measured with a ruler. These roots were subsequently dried (80°C) and used to determine the approximate relationship between root length and dry weight.

Consumption of added microbes by the indigenous soil microbial community
In order to evaluate the rate at which microbes added to soil were predated and decomposed by pre-existing soil microbes, 14 C-labelled microbes were added to soil and their decomposition to 14 CO 2 measured according to Hill et al. (2008). Briefly, 2 g of soil was placed in each of three 10 ml glass tubes and 83 ll of the washed 14 C-labelled microbe suspension were added to the surface (matching the overall ratio of solution to soil in rhizotube injections). Air was drawn over the soil at a rate of c. 100 ml min À1 and 14 CO 2 was captured in two 3 ml vials of 0.1 M NaOH connected in series (described in detail in Hill et al., 2007). Vials of NaOH were changed 1, 5, 10, 20, 40 and 60 min after addition of the microbes to soil. There was no potential for significant loss of 14 CO 2 during changing of NaOH as pumping was suspended for this period. Captured 14 C was measured by liquid scintillation counting after mixing NaOH solution with Scintisafe scintillation cocktail. To account for 14 CO 2 lost in respiration from the microbial culture alone, the experiment was repeated with 1 ml of culture solution in sterile tubes without soil.

Statistical analysis
Data were analysed by One-way ANOVA with LSD post-hoc test (SPSS v14; SPSS, Chicago, IL, USA) after testing for normality and homogeneity of variance with Shapiro-Wilk and Levene's test, respectively. Data not normally distributed or without homogeneity of variance were log 10 -transformed before analysis. Following transformation all data were normally distributed and

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New Phytologist had homogeneity of variance. Statistical differences were accepted at P < 0.05. All presented probabilities are for post hoc comparisons.

Plants grown in sterile culture
Uptake of 15 N by sterile plant roots when in nonmicrobial forms was 18-, to c. 100-fold faster (tetraalanine, and alanine and nitrate, respectively; P < 0.001; Fig. 1) than when present in a microbial form. Uptake of 15 N-nitrate took place at the same rate as 15 N-alanine and 15 N uptake was approximately five-fold faster (P ≤ 0.003) in both these forms than as tetraalanine. Recovered 15 N accounted for 5.1 AE 0.6% of nitrate, 3.1 AE 0.2% of alanine, 0.84 AE 0.1% of tetraalanine and 0.046 AE 0.02% of microbe 15 N supplied in the 4 ml of solution. The ratio of the proportion of 13 C recovered to the proportion of 15 N recovered from organic forms of N was almost identical in plants supplied with alanine and those supplied with tetraalanine (0.63 AE 0.01 and 0.58 AE 0.04, respectively; mean AE SEM; n = 3; Fig. 2).
Roots within the microcosms were predominantly secondorder laterals and average root diameter was 0.3 AE 0.03 mm (mean AE SEM; n = 10). The specific root length was 63 AE 8 m g À1 DW.

Plants grown in soil
As in sterile culture, root uptake of 15 N added as nitrate, alanine or tetraalanine in plants grown in soil was much greater (P < 0.001; 208-, 32-and 46-fold, respectively; Fig. 1) than when added as the microbial suspension. Uptake of 15 N by roots of plants supplied with nitrate was six-and five-fold higher (P < 0.001) than in plants supplied with alanine or tetraalanine, respectively, which were not different from each other. After 1 h 15.8 AE 2% of the added nitrate 15 N, 4.5 AE 0.6% of the alanine 15 N and 3.9 AE 0.5% of the tetraalanine 15 N was recovered in plants, but only 0.079 AE 0.008% of the microbial 15 N. Postuptake partitioning of 15 N also differed (P < 0.02) between plants supplied with the different forms of N. The ratio of root 15 N to shoot 15 N was 1.2 AE 0.1 for plants supplied with microbial N, 2.4 AE 0.6 for those supplied with nitrate, 9.8 AE 1.5 for those supplied with tetraalanine and 18 AE 2.7 for plants supplied with alanine. Ratios for plants receiving nitrate and those receiving microbes were not statistically different.
Data for 13 C were much more variable than 15 N data in plants receiving dual-labelled compounds. This was especially true of shoots where 13 C recovery was only 26 AE 10 or 15 AE 7% (mean AE SEM; n = 3; alanine and tetraalanine, respectively) of that recovered in roots. Recovery of 13 C and 15 N from duallabelled compounds in plants grown in soil receiving N as both alanine and tetraalanine were not linearly correlated. The ratio of the proportion of 13 C recovered to the proportion of 15 N recovered was 0.6 in plants receiving alanine and 0.4 in those receiving tetraalanine, but we suggest that values for the ratio of 13 C to 15 N for plants grown in soil should be interpreted with caution. Recovered microbial 15 N and 14 C could not be correlated as they were separate samples. The mean value for recovery of 14 C was, however, similar to that for 15 N at 0.070 AE 0.02% of that injected.
From injections of ink into rhizotubes it was estimated that added solutes mixed with the soil of a 7 cm section of the rhizotube. These 7 cm sections contained 11.6 AE 0.8 mg root DW (approximately one-third of the total root in the rhizotube), 15.7 AE 9 nmol NO À 3 , 47.4 AE 8 nmol free amino acid N and 255 AE 34 nmol short (< 1 kDa) peptide N (mean AE SEM; n = 3 for root DW and n = 4 for solute concentrations). If it is assumed  that the root biomass in contact with labelled solutes was a constant 11.6 mg DW, pre-existing soil solutes mixed completely with labelled solutes, and L-alanine and L-tetraalanine are typical of all soil solution amino acids and short peptides, rates of uptake for alanine and tetraalanine remain statistically the same at 2.1 AE 0.3 and 2.5 AE 0.3 lmol N g À1 DW root h À1 , respectively. Uptake of nitrate is 7.0 AE 0.8 lmol N g À1 DW root h À1 , making it approximately three-fold greater (P < 0.001) than amino acid and peptide N uptake.
No evidence of mycorrhizal infection could be found on roots.
Over the hour of incubation, 3.1 AE 0.2% of the added microbial 14 C was mineralized to 14 CO 2 after accounting for that lost in respiration from the added microbes themselves (0.3 AE 0.06%).

Acquisition of dissolved forms of N
In sterile hydroponic culture, nitrate 15 N was taken up at the same rate as alanine 15 N and five times faster than tetraalanine 15 N. In contrast to the equal rate of nitrate and amino acid acquisition in sterile culture, competition from microbes caused a large reduction in acquisition of alanine 15 N relative to that of nitrate 15 N when the plants were grown in nonsterile soil. Previous investigations have suggested some form of preference of soil microbes for L-peptides over the amino acid monomer Hill et al., 2011bHill et al., , 2012. Consequently, it was surprising that while 15 N uptake of alanine was considerably reduced in soil, the rate of acquisition of 15 N as tetraalanine relative to nitrate by roots in soil was similar to that in sterile solution. Further, what evidence there is suggests that soil solution concentrations of amino acids bound in short peptides are generally higher than those of free amino acids Hill et al., 2011a,b,c; Table 1). This may indicate that acquisition of N as short L-peptides by wheat growing in agricultural soil exceeds that as L-amino acid monomers.
Realistic evaluation of the importance of different forms of soil N to plant nutrition presents formidable experimental problems, especially for organic forms. Even when attempting to determine relative fluxes, it is necessary to consider a range of potential caveats in the interpretation of data. We found no statistically significant correlation between recovered 13 C and 15 N for plants grown in soil. This may principally be a consequence of variation caused by the dilution of the 13 C taken up as intact alanine or tetraalanine in a c. 15 000-fold larger pool of plant carbon with a variable 13 C content. Some support for this view is provided by the much larger recovery of 13 C in roots than in shoots and the fact that rates of recovery of 13 C in plants grown in soil did not depart dramatically from those which would be expected from recovery of 15 N after losses in respiration (Hill et al., 2011c). Nevertheless, we cannot exclude the possibility that some or even all of the amino acid and/or peptide 15 N was acquired by plants following prior mineralization by soil microbes. Taking account of isotopic pool dilution in pre-existing pools of soil N also relies on various assumptions. Even if it is clear what proportion of pre-existing soil soluble N is mixed with, differing flux rates through soil pools for the different forms of N add uncertainty. For instance, the residence time of L-amino acids and short L-peptides in soil is probably only of the order of a few minutes . Thus, if acquired intact, the flux of N into plants as amino acid or peptide relative to that of forms of N which are less desirable to most soil microbes, such as nitrate, is probably underestimated with a chase period of an hour (Jones et al., 2005). If amino acid and peptide N are only acquired following mineralization, recovery of 15 N in plants would be likely to increase with the chase period. In this case, the actual flux of N derived from mineralization of organic forms would be underestimated due to dilution by pre-existing inorganic N and this dilution would probably increase with residence time. Many uncertainties relating to solute production sites and mobility in soil may also be of considerable importance in the design of experiments and interpretation of experimental data. Further, we know little about the composition of individual peptides in soil solution. For instance, 160 000 possible tetrapeptides may be formed from 20 common protein amino acids. To date, the availability to plants of very few peptides has been investigated. Consequently, after correction for pool dilution fluxes of, particularly peptide, N from soil to plant must be interpreted with some caution.

Acquisition of N as microbes
Nitrogen delivered to plant roots as a microbial culture was acquired both by plants with sterile roots and those growing in soil. In both cases the nitrate, amino acid monomer and tetrapeptide forms of N were taken up more than an order of magnitude faster than the microbial suspension. If all of the measured microbial 15 N acquired by plants was acquired as intact microbes, our results suggest that sterile roots of plants ingested c. 2 9 10 6 microbial cells g À1 root DW h À1 . This suggests that microbes were ingested at a rate of c. 32 000 cells m À1 root length h À1 or 35 cells mm À2 root surface area h À1 , although this does not take account of fine root structure such as root hairs, which may have a role in microbe acquisition (Paungfoo-Lonhienne et al., 2010;Mercado-Blanco & Prieto, 2012). To match the rate of N uptake as nitrate or alanine from sterile solution, plants would need to ingest c. 2 9 10 8 cells g À1 root DW h À1 and c. 4 9 10 7 to match N uptake as tetraalanine. When growing in soil, 15 N recovery suggests that plants ingested c. 390 000 cells g À1 root DW h À1 ; c. 6 cells mm À2 root surface area h À1 (assuming a constant 11.6 mg of root in a 7 cm section of rhizotube was accessed by injected microbes). If previous estimates of numbers of bacteria on wheat roots are typical and it is assumed that labelled microbes mixed homogeneously with existing rhizoplane microbes, this suggests that rates of uptake were c. 975 000 cells g À1 root DW h À1 : c. 15 cells mm À2 root surface area h À1 ; c. 4.5% of the standing rhizoplane bacterial biomass d À1 (Liljeroth, 1990). If it is assumed that injected cells mixed with all bacteria on the rhizoplane and in the rhizosphere, this value rises to c. 10 6 cells g À1 root DW h À1 or c. 16 cells mm À2 root surface area h À1 . Nevertheless, this flux of

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New Phytologist N into roots still represents only a maximum of c. 6% of the flux of other forms of N when they are similarly corrected for pool dilution. There are uncertainties in the dilution of amino acid, peptide and nitrate in pre-existing soil pools. However, very poor understanding of the process of direct microbe uptake by roots means that the size of the pool with which added microbes mixed is very difficult to establish. Consequently, our estimates of uptake of N as microbes are probably subject to the greatest uncertainty.
Three percent of the 14 C added to soil as microbes was mineralized to 14 CO 2 within an hour. This was around a fifth of the 14 C likely to be mineralized to 14 CO 2 if added to soil of this type as glucose (Hill et al., 2008). Nevertheless, respired 14 CO 2 was an almost 40-fold greater proportion of the microbial biomass 14 C than the proportion of the microbial 15 N which was recovered in plants (0.08%). Similarly, the 0.3% of the microbial 14 C respired by the living microbes alone was a six times greater proportion of microbial 14 C than the 0.05% of microbial 15 N recovered in sterile plants. This may indicate that in both soil and sterile solutions, the microbial 15 N recovered in plants was taken up as inorganic 15 N after microbial mineralization. However, although there is some uncertainty inherent in the measurement of 14 C and 15 N in separate plants, the close agreement between values for recovery of microbial 15 N and 14 C in plants growing in soil strongly suggests that 15 N was not acquired only in inorganic forms. We cannot completely exclude the possibility that both N and C were taken up as organic forms of N following prior lysis of microbes. In our opinion this seems unlikely to account for the entire flux of 14 C and 15 N, as that would necessitate the maintenance of the overall microbial 14 C to 15 N ratio in the organic forms of N taken up after any losses of C in respiration. Nevertheless, post-lysis, or even post-mineralization, plant uptake probably accounts for part of the flux of microbial N into roots.
Many living endophytes exist in plants, although our knowledge of how widespread the ability to survive within plants is amongst soil microbes is largely restricted to studies on a few species (Hardoim et al., 2008;Ryan et al., 2008;Reinhold-Hurek & Hurek, 2011). Our measurements of incorporation of microbial 15 N and 14 C cannot distinguish between microbes internalized and metabolized within root cells and those continuing to survive within the plant, that is within the apoplast or root wounds (Gantar, 2000;Hardoim et al., 2008;Paungfoo-Lonhienne et al., 2010). The close agreement between the 15 N and 14 C recovery from the microbial cells contrasts with the at least 40% of amino acid and peptide 13 C which was rapidly metabolized and lost in respiration. This may also indicate that microbes were not metabolized by the plant after uptake. Further, in some cases, endophytes move from root to shoot within the plant without apparent attack or digestion by the host with bacterial movement from the root epidermis to the stele occurring via the apoplast (Reinhold-Hurek et al., 2006;Rosenblueth & Martinez-Romero, 2006;Deering et al., 2011). Consequently, 15 N recovery in the shoot cannot be unequivocally attributed to degradation of microbes in the root, with subsequent transport of 15 N to the shoot (Paungfoo-Lonhienne et al., 2010). However, even if plant degradation of microbes took place more slowly than other forms of organic N and too slowly to be very obvious over the hour of experiment duration, eventual death and decomposition of some microbes within the plant does seem likely.
Assuming that bacteria can be internalized within root cells, it raises questions about the mechanism of cytophagocytosis and to what extent this is under direct control of the plant (Hardoim et al., 2008;Paungfoo-Lonhienne et al., 2010). Due to the small pore size of the cell wall (< 10 nm) relative to the size of bacterial cells (c. 1000 nm), internalization can only occur by loosening/digestion of the cell wall in mature root regions or possibly at weak points in actively growing cells (Reinhold-Hurek et al., 2006;Miralles et al., 2012). If the plant is actively undertaking this process to acquire N, strong selection for nonharmful bacteria is expected, bypassing myriad host-defence processes (Kogel et al., 2006;Rosenblueth & Martinez-Romero, 2006;H€ uckelhoven, 2007). Perhaps more probable is that many bacterial cells are taken up passively as has been demonstrated for a range of inert micro-and nanoparticulates (Solomon & Matthews, 2005;Miralles et al., 2012). However, whilst it is clear from many studies that live bacteria can rapidly enter and survive in the endorhizosphere, little evidence exists for the passive uptake of dead cells into the apoplast (Quadt-Hallmann et al., 1997;Hardoim et al., 2008).
Although considerable uncertainty surrounding mechanisms remains, our results suggest that acquisition of microbes from soil by wheat roots, with subsequent translocation of N, does take place. Thus, if this is actively undertaken, all three plant species investigated to date, Arabidopsis thaliana, Solanum lycopersicum and Triticum aestivum, appear to have this capacity (Paungfoo-Lonhienne et al., 2010). However, if wheat proves to be typical, low rates of uptake of N as intact microbial cells in comparison with uptake of common inorganic and organic forms of soil N suggest that the importance of this process to overall plant N nutrition is minor. Use of other forms of organic N is often considered to be most important in environments where N mineralization is slow (Chapin et al., 1993;Schimel & Bennett, 2004;N€ asholm et al., 2009;Hill et al., 2011a). Similarly, wider investigation may establish that uptake and digestion of soil microbes has high functional importance in some ecosystems; perhaps when free-living diazotrophs are abundant in an N-limited rhizosphere. In these respects, the use of microbes may be more significant in some angiosperms than it is in a highly-bred agricultural plant such as wheat. Of course, it may also be that microbes are primarily consumed as a source of some nutrient other than N, or that their consumption is only of transient importance.
Although each form of N differs in its mobility in soil, strong sorption of microbial cells to soil particles results in a slow rate of diffusion to the root surface (Foppen et al., 2005). Consequently, most microbes available to plants live and reproduce very close to roots and derive much of their nutrition from roots, for example, as exudates (Liljeroth, 1990;Brimecombe et al., 2001). This may mean that active consumption of these microbes primarily represents a mechanism by which plants recover lost nutrients, as has been proposed for some organic solutes (Jones et al., 2005).

Conclusion
Uncertainty still surrounds the extent to which plants can acquire different forms of organic N from soil. Previous studies undertaken in sterile hydroponic culture have clearly demonstrated the potential for plant roots to take up intact microbial cells, but the functional significance of this process in soil environments remains unknown. The results presented here for wheat plants grown in both hydroponics and in soil strongly suggest that the rate of uptake of N as intact microbial cells is very low in comparison with uptake of common inorganic and organic forms of soil N. Although wider investigation is needed and other functions cannot be excluded, this relatively low incorporation of microbial N suggests that digestion of soil microbes probably represents only a small component of overall plant N acquisition.