Carbon for nutrient exchange between Lycopodiella inundata and Mucoromycotina fine root endophytes is unresponsive to high atmospheric CO2

Non-vascular plants associating with arbuscular mycorrhizal (AMF) and Mucoromycotina ‘fine root endophyte’ (MFRE) fungi derive greater benefits from their fungal associates under higher atmospheric [CO2] (a[CO2]) than ambient; however, nothing is known about how changes in a[CO2] affect MFRE function in vascular plants. We measured movement of phosphorus (P), nitrogen (N) and carbon (C) between the lycophyte Lycopodiella inundata and Mucoromycotina fine root endophyte fungi using 33P-orthophosphate, 15 N-ammonium chloride and 14CO2 isotope tracers under ambient and elevated a[CO2] concentrations of 440 and 800 ppm, respectively. Transfers of 33P and 15 N from MFRE to plants were unaffected by changes in a[CO2]. There was a slight increase in C transfer from plants to MFRE under elevated a[CO2]. Our results demonstrate that the exchange of C-for-nutrients between a vascular plant and Mucoromycotina FRE is largely unaffected by changes in a[CO2]. Unravelling the role of MFRE in host plant nutrition and potential C-for-N trade changes between symbionts under different abiotic conditions is imperative to further our understanding of the past, present and future roles of plant-fungal symbioses in ecosystems. Supplementary Information The online version contains supplementary material available at 10.1007/s00572-021-01033-6.


Introduction
Changes in atmospheric CO 2 concentration (a[CO 2 ]) have been a prominent feature throughout Earth's environmental history (Leaky and Lau 2012). Geochemical models support fossil and stable isotope evidence indicating that the global environment underwent major changes throughout the Palaeozoic Era (541-250 Ma) (Berner et al. 2006;Bergman et al. 2004;Lenton et al. 2016), consisting of a stepwise increase of the Earth's atmospheric oxygen ([O 2 ]), and a simultaneous decline in a [CO 2 ]. Today, Earth faces environmental changes on a similar scale, but with a[CO 2 ] instead rising at an unprecedented rate (Meinshausen et al. 2011;Wilson et al. 2017).
Long before plants migrated onto land, Earth's terrestrial surfaces were colonised by a diverse array of microbes, including filamentous fungi (Blair 2009;Berbee et al. 2017). Around 500 Mya, plants made the transition from an aquatic to a terrestrial existence (Morris et al. 2018), facilitated by symbiotic fungi (Nicolson 1967;Pirozynski and Malloch 1975). These ancient fungal symbionts are thought to have played an important role in helping early land plants access scarce nutrients from the substrate onto which they had emerged, in much the same way as modern-day mycorrhizal fungi form nutritional mutualisms with plants (Pirozynski and Malloch 1975;Krings et al. 2012;Strullu-Derrien et al. 2014). It is highly likely that ancient mycorrhiza-like (or paramycorrhiza sensu Strullu-Derrien and Strullu 2007) fungi were closely related to, and subsequently evolved into, modern arbuscular mycorrhizal fungi (AMF) belonging to the fungal subphylum Glomeromycotina (also referred to as phylum Glomeromycota) (Redecker et al. 2000;Spatafora et al. 2017;Wijayawardene et al. 2018;Radhakrishnan et al. 2020).
Recently, it was discovered that extant non-vascular plants, including the earliest divergent clade of liverworts, associate with a greater diversity of fungi than was previously thought, notably forming endophytic associations with Endogonales, members of the Mucoromycotina (Bidartondo et al. 2011;Desirò et al. 2014;Strullu-Derrien et al. 2014;Rimington et al. 2015;Field et al. 2015a). Mucoromycotina is a partially saprotrophic fungal lineage (Bidartondo et al. 2011;Field et al. 2015bField et al. , 2016 sister to, or pre-dating, the Glomeromycotina AMF, both within Mucoromycota (Spatafora et al. 2017). This discovery, together with the emerging fossil evidence (Strullu-Derrien et al. 2014) and the demonstration that liverwort-Mucoromycotina fungal associations are nutritionally mutualistic (Field et al. 2015a; and often co-occur with AMF (Field et al. 2016), suggests that earlier land plants had greater symbiotic options available to them than was previously thought (Field et al. 2015b). Studies now show that symbioses with Mucoromycotina fungi are not limited to non-vascular plants but span almost the entire extant land plant kingdom (Rimington et al. 2015(Rimington et al. , 2020Orchard et al. 2017a;Hoysted et al. 2018Hoysted et al. , 2019, suggesting that this ancient association may also have key roles in modern terrestrial ecosystems. The latest research into the functional significance of plant-Mucoromycotina fine root endophyte (MFRE) associations indicates that MFRE play a complementary role to AMF by facilitating plant nitrogen (N) assimilation alongside AMF-facilitated plant phosphorus (P) acquisition through co-colonisation of the same plant host . Such functional complementarity is further supported by the observation that MFRE transfer significant amounts of 15 N but relatively little 33 P tracers to a host lycophyte, Lycopodiella inundata, in the first experimental demonstration of MFRE nutritional mutualism in a vascular plant . These results contrast with the majority of studies on MFRE and fine root endophytes (FRE) which have, to date, focussed on the role of the fungi in mediating plant phosphorus (P) acquisition (Orchard et al. 2017b, and literature within;Albornoz et al. 2020).
Today, plant-symbiotic fungi play critical roles in ecosystem structure and function. The bidirectional exchange of plant-fixed carbon (C) for fungal-acquired nutrients that is characteristic of most mycorrhizal symbioses (Field and Pressel 2018) holds huge significance for carbon and nutrient flows and storage across ecosystems (Leake et al. 2004;Rillig 2004;Averill et al. 2014). By forming mutualistic symbioses with the vast majority of plants, including economically important crops, mycorrhizal fungi have great potential for applications within a variety of sustainable management strategies in agriculture, conservation and restoration. Application of diverse mycorrhiza-forming fungi, including both AMF and MFRE, to promote sustainability in agricultural systems is particularly relevant in the context of global climate change and depletion of natural resources . The MFRE in particular may hold potential for agricultural applications to reduce use of chemical fertilisers within sustainable arable systems where routine over-use of N-based mineral fertilisers causes detrimental environmental and down-stream economic impacts (Thirkell et al. 2019), but realising this potential relies on improving our current understanding of MFRE diversity and function. Changes in abiotic factors such as a[CO 2 ] (Cotton 2018), which is predicted to continue rising in the future (Meinshausen et al. 2011), have been shown to affect the rate and quantity of carbon and nutrients exchanged between mycorrhizal partners (Field et al. 2012(Field et al. , 2015a(Field et al. , 2016Zheng et al. 2015;Thirkell et al. 2019). As such, insights into the impact of environmental factors relevant to future climate change on carbon for nutrient exchange between symbiotic fungi and plants must be a critical future research goal.
Experiments with liverworts associating with MFRE fungi, either in exclusive or in dual symbioses alongside AMF, suggest that these plants derive less benefit in terms of nutrient assimilation from their MFRE associates under a high a[CO 2 ] (1500 ppm) than under a lower a[CO 2 ] (440 ppm) (Field et al. 2015a(Field et al. , 2016, with the opposite being the case for liverworts associated only with AMF (Field et al. 2012). However, when vascular plants (Osmunda regalis and Plantago lanceolata) with AMF associations were exposed to high a[CO 2 ], there were no changes in mycorrhizal-acquired plant P assimilation (Field et al. 2012). Whether vascular plant-MFRE symbioses respond to changing a[CO 2 ] is unknown.
Here, using stable and radioisotope tracers, we investigate MFRE function in Lycopodiella inundata, a homosporous perennial lycophyte widely distributed in the northern hemisphere (Rasmussen and Lawesson 2002) that associates almost exclusively with MFRE fungal partners (Kowal et al. 2020), and how it responds to climate change-relevant shifts in a[CO 2 ]. Specifically, we test the hypotheses that (a) MFRE acquire greater amounts of plant-fixed C under high a[CO 2 ] of 800 ppm as a result of there being larger amounts of photosynthate available for transfer because of greater rates of C fixation by the plant via photosynthesis, and (b), increased C allocation from plant to fungus increases transfer and assimilation of 15 N and 33 P tracers from MFRE to plants to feed growing plant demand for nutrients to promote growth.

Plant material and growth conditions
Mature Lycopodiella inundata (L.) plants were collected from the wild in Thursley National Nature Reserve, Surrey, UK (SU 90,081 39,754), in June 2017. The L. inundata plants, which were weeded regularly to remove other plant species, were planted directly into pots (90mm diameter × 85-mm depth) containing a homogeneous mixture of acid-washed silica sand and 5% pot volume compost (No. 2; Petersfield) to aid retention properties of the substrate and to provide minimal nutrients. Soil surrounding plant roots (approximately one-fifth of the pot volume) was left intact to prevent damage to the roots and to act as a natural inoculum, including symbiotic fungi and associated microorganisms.
Based on the methods of Field et al. (2012), three windowed cylindrical plastic cores covered in 10-μm nylon mesh were inserted into the substrate within each experimental pot (see supplementary online material Fig. S1). Two of the cores were filled with the same substrate as the bulk soil within the pots, comprising a homogeneous mixture of acid-washed silica sand and compost (No. 2; Petersfield), together making up 95% of the core volume, native soil gathered from around the roots of wild plants to ensure cores contained the same microbial communities as in the bulk soil (4% core volume), and fine-ground tertiary basalt (1% core volume) to act as fungal bait (Field et al. 2015a). The third core was filled with glass wool to allow below-ground gas sampling throughout the 14 C-labelling period to monitor soil community respiration. Plants were watered every other day with distilled water with no other application of nutrient solutions. Microcosms shared a common drip tray within each cabinet only through the acclimation period, ensuring a common pool of rhizospheric microorganisms in each microcosm.
A total of 48 L. inundata microcosms were maintained in controlled environment chambers (model no. Micro Clima 1200; Snijders Labs) with a light cycle of 16-h daytime (20 °C and 70% humidity) and 8-h night-time (at 15 °C and 70% humidity). Daytime photosynthetically active radiation (PAR), supplied by LED lighting, was 225 μmol photons m −2 s −1 (similar to what L. inundata experience in the wild). Plants were grown at two contrasting CO 2 atmospheres: 440 ppm a[CO 2 ] (24 plants) to represent a modern-day atmosphere or 800 ppm a[CO 2 ] (24 plants) to simulate Palaeozoic atmospheric conditions on Earth at the time vascular plants are thought to have diverged (Berner 2006) as well as predicted a[CO 2 ] for 2100 (Meinshausen et al. 2011). Atmospheric [CO 2 ] was monitored using a Vaisala sensor system (Vaisala, Birmingham, UK), maintained through addition of gaseous CO 2 . All pots were rotated within cabinets, and plants were switched between cabinets with a[CO 2 ] adjusted accordingly every 2 weeks to control for possible cabinet and block effects. Plants were acclimated to chamber/growth regimes for 4 weeks to allow establishment of mycelial networks within pots. Before initiation of radioisotope labelling, mycelial networks were confirmed by destructively collecting soil from a rotated core for hyphal extraction and subsequent staining with trypan blue (Brundrett et al. 1996). Additionally, main roots were stained with acidified ink for the presence of fungi, based on the methods of Brundrett et al. (1996). All plants were processed for molecular identification of fungal symbionts within 1 week of collection from the wild and at the end of the experimental period using the protocol in Hoysted et al. (2019). Briefly, genomic DNA extraction and purification from L. inundata roots and subsequent amplification, cloning and sequencing were performed according to the methods of Rimington et al. (2015). The fungal 18S ribosomal rRNA gene was targeted using the fungal primer set NS1/ EF3 and a semi-nested approach with Mucoromycotinaand Glomeromycotina-specific primers described in Desirò et al. (2014).

Cytological analyses
Roots of experimental L. inundata plants were stained with trypan blue (Brundrett et al. 1996), which is common for identifying MFRE (Orchard et al. 2017b), and photographed under a Zeiss Axioscope (Zeiss, Oberkochen, Germany) equipped with a MRc digital camera. To quantify root colonisation by MFRE, five plants were randomly selected per treatment, and from these two intact, healthy roots (per plant) were excised and sectioned transversally in up to six segments (depending on root length) before being processed for scanning electron microscopy according to Duckett et al. (2006). Percentage root colonisation was then calculated by scoring each segment (from a total of 56 and 58 segments respectively for the elevated and ambient a[CO 2 ] treatments) as colonised or noncolonised under the scanning electron microscope (Fig. 1).
Quantification of C, 33 P and 15 N fluxes between lycophytes and fungi.
After the 4-week acclimation period, microcosms were moved to individual drip trays immediately before isotope labelling to avoid cross-contamination of the isotope tracers. A total of 100 μl of an aqueous mixture of 33 P-labelled orthophosphate (specific activity 111 TBq mmol −1 , 0.3 ng 33 P added; Hartmann analytics) and 15 N-ammonium chloride (1 mg ml −1 ; 0.1 mg 15 N added; Sigma-Aldrich) was introduced into one of the soil-filled mesh cores in each pot through the installed capillary tube. In half (n = 12) of the pots, cores containing isotope tracers were left static to preserve direct hyphal connections with the lycophytes. Fungal access to isotope tracers was limited in the remaining half (12) of the pots by rotating isotope tracer-containing cores through 90°, thereby severing the hyphal connections between the plants and core soil. These were rotated every second day thereafter, thus providing a control treatment that allows us to distinguish between fungal and microbial contributions to tracer uptake by plants, as well as passive diffusion of isotopes through the soil matrix. Assimilation of 33 P tracer into above-ground plant material was monitored using a hand-held Geiger counter held over the plant material daily.
At detection of peak activity in above-ground plant tissues (21 days after the addition of the 33 P and 15 N tracers), the tops of 33 P and 15 N-labelled cores were sealed with plastic caps and anhydrous lanolin, and the glass-wool cores were sealed with rubber septa (Suba-Seal, Sigma-Aldrich). Before lights were switched on at 8 a.m., each pot was sealed into a 3.5-l, gas-tight labelling chamber, and 2 ml 10% (w/v) lactic acid was added to 30 μl NaH 14 CO 3 (specific activity 1.621 GBq/mmol −1 ; Hartmann Analytics), releasing a 1.1-MBq pulse of 14 CO 2 gas into the headspace of the labelling chamber. Pots were maintained under growth chamber conditions, and 1 ml of headspace gas was sampled after 1 h and every 1.5 h thereafter. Below-ground respiration was monitored via gas sampling from within the glass-wool-filled core after 1 h and every 1.5 h thereafter for ~ 16 h.

Plant harvest and sample analyses
Upon detection of maximum below-ground flux of 14 C, ~ 16 h after the release of the 14 CO 2 pulse, each microcosm compartment (i.e. plant material and soil) was separated, freeze-dried, weighed and homogenised using a TissueLyser LT with steel ball bearings (Qiagen). The 33 P activity in plant (shoots and roots) and soil samples (cores and bulk) was quantified by digesting in concentrated H 2 SO 4 and liquid scintillation (Tricarb 3100TR liquid scintillation analyser, Isotech). The quantity of 33 P tracer that was transferred to a plant by its fungal partner was then calculated using previously published equations (Cameron et al. 2007).
To determine total symbiotic fungal-acquired 33 P transferred to L. inundata, the mean 33 P content of plants that did not have access to the tracer because cores into which the 33 P was introduced were rotated was subtracted from the total 33 P in each plant that did have access to the isotopes within the core via intact fungal hyphal connections (i.e. static cores). This calculation controls for diffusion of isotopes and microbial nutrient cycling in pots, ensuring only 33 P gained by the plant via intact fungal hyphal connections, are accounted and therefore serve as a conservative measure of the minimum fungal transfer of tracer to the plant.
Between 2 and 4 mg of freeze-dried, homogenised plant tissue (both shoots and roots, separately) was weighed into 6 × 4 mm 2 tin capsules (Sercon), and 15 N abundance was determined using a continuous flow IRMS (PDZ 2020 IRMS, Sercon). Air was used as the reference standard, and the IRMS detector was regularly calibrated to commercially available reference gases. The 15 N transferred from fungus to plant was then calculated using equations published previously in Field et al. (2016). In a similar manner as for the 33 P, the mean of the total 15 N in plants without access to the isotope because of broken hyphal connections between plant and core contents was subtracted from total 15 N in each plant with intact hyphal connections to the mesh-covered core to give fungal-acquired 15 N. Again, this provides a conservative measure of 15 N transfer from fungus to plant as it ensures only 15 N gained by the plant via intact fungal hyphal connections is accounted. The 14 C activity of plant (shoots and roots) and soil (cores and bulk) samples was quantified through sample oxidation (307 Packard Sample Oxidiser, Isotech) followed by liquid scintillation. Total C ( 12 C + 14 C) fixed by the plant and transferred to the fungal network was calculated as a function of the total volume and CO 2 content of the labelling chamber and the proportion of the supplied 14 CO 2 label fixed by plants. The difference in total C between the values obtained for static and rotated core contents in each pot is considered equivalent to the total C transferred from plant to symbiotic fungus within the soil core for that microcosm, noting that a small proportion will be lost through soil microbial respiration (Cameron et al. 2006). The total C budget for each experimental pot was calculated using equations from Cameron et al. (2006). Total percent allocation of plant-fixed C to extraradical symbiotic fungal hyphae was calculated by subtracting the activity (in becquerels, Bq) of rotated core samples from that detected in static core samples in each pot, dividing this by the sum of activity detected in all components (shoots, roots, static and rotated cores, and bulk soil) of each microcosm, then multiplying it by 100.

Statistics
Effects of a[CO 2 ] on the C, 33 P and 15 N fluxes between L. inundata and MFRE fungi were tested using analysis of variance (ANOVA) or Mann-Whitney U where indicated. Data were checked for homogeneity and normality using the Kolmogorov-Smirnov test. Where assumptions for ANOVA were not met, data were transformed using log 10 . If assumptions for ANOVA were still not met, a Mann-Whitney U test was performed. Significant differences comparing the proportion of root segments colonised and differences across the population of root segments were analysed using a Fisher's exact and an unpaired t-test, respectively. All statistics were carried out using the statistical software package SPSS Version 24 (IBM Analytics).

Molecular identification of fungal symbionts
Analysis of experimental Lycopodiella inundata plants grown under ambient and elevated a[CO 2 ] confirmed that they were colonised by Mucoromycotina fine root endophyte fungi within Endogonales. Glomeromycotina fungal sequences were not detected. Mucoromycotina OTUs that have previously been identified in wild-collected lycophytes from diverse locations (Rimington et al. 2015;Hoysted et al. 2019) were detected before and after the experiments (Gen-Bank/EMBL accession numbers: MK673773-MK673803).

Cytology of fungal colonisation in plants
Trypan blue staining and SEM of L. inundata roots grown under ambient and elevated a[CO 2 ] revealed the same fungal symbiont morphology consistent with that previously observed for L. inundata-Mucoromycotina FRE  and MFRE colonisation in other vascular plants (Orchard et al. 2017a) including fine branching, aseptate hyphae (< 2-μm diameter) with small intercalary and terminal swellings/vesicles (usually 5-10-but up to 15-μm diameter) but, differently from those in flowering plants, no arbuscules (Fig. 1). There was a significant difference across the population of root segments in the percentage of individual root fragments colonised grown under contrasting a[CO 2 ] (supplementary online material Fig. S2). Root segments from plants grown under 440 a[CO 2 ] had a significantly lower mean percent colonisation compared to root segments from plants grown under 800 ppm a[CO 2 ] (t = 2.182; df = 106.9, n = 58, 54).

C transfer from L. inundata to MFRE symbionts
The amount of carbon allocated from L. inundata to MFRE fungi under elevated a[CO 2 ] concentrations compared to that when plants were grown under a[CO 2 ] of 440 ppm was not statistically significant ( Fig. 2a; Mann-Whitney U = 194, P = 0.864, n = 24); nevertheless, the transfer was 2.8 times greater at 800 ppm than at 440 ppm. In terms of total C transferred from plants to MFRE (carbon in core, ng), similarly, L. inundata transferred ca. 2.7 times more C to MFRE fungal partners at elevated a[CO 2 ] concentrations of 800 ppm compared to those under a[CO 2 ] of 440 ppm ( Fig. 2b; Mann-Whitney U = 197.5, P = 0.942, n = 24).

Fungus-to-lycophyte 33 P and 15 N transfer
Mucoromycotina FRE transferred both 33 P and 15 N to L. inundata in both a[CO 2 ] treatments (Fig. 3). There were no significant differences in the amounts of either 33 P or 15   of 800 ppm (white bars). All bars in each panel represent the difference in isotopes between the static and rotated cores inserted into each microcosm. In all panels, error bars denote standard error of the mean. In panels (a, b), n = 24 for 800 ppm and for 440 ppm a[CO 2 ] inundata. (e) Total shoot P content (mg) equating to both plant and fungal-acquired P and (f) total shoot N content (mg) equating to both plant and fungal-acquired N in shoots of L. inundata. All experiments were conducted at an ambient a[CO 2 ] of 440 ppm (grey bars) and elevated a[CO 2 ] of 800 ppm (white bars). All bars in each panel (a-d) represent the difference in isotopes between the static and rotated cores inserted into each microcosm. In all panels, error bars denote standard error of the mean. In panels (a-d), n = 12, and panels (e-f), n = 24, for both 800 ppm and 440 ppm a[CO 2 ]

Discussion
Our results demonstrate for the first time that the exchange of C-for-nutrients between a vascular plant and MFRE symbionts is largely unaffected by changes in a[CO 2 ], with MFRE maintaining 33 P and 15 N assimilation and transfer to the plant host across a[CO 2 ] treatments (Fig. 3a, b) (Fig. 2a, b), but without a reciprocal increase in fungal-acquired 33 P or 15 N tracer assimilation. Although the difference in C transfer between plants under different a[CO 2 ] atmospheres was not statistically significant, our observation is in line with previous studies in which Mucoromycotina fungi (and both Mucoromycotina and AMF partners co-colonising the same host in 'dual' symbiosis) gained a greater proportion of recently fixed photosynthates from their non-vascular plant partners but did not deliver greater amounts of 33 P or 15 N tracers when grown under elevated a[CO 2 ] compared to current ambient conditions (Field et al. 2012(Field et al. , 2015a(Field et al. , 2016. This contrasts with patterns of carbon-for-nutrient exchange between other vascular plants and AMF where increased allocation of carbon to fungal symbionts is usually associated with increases in nutrient delivery from AMF to the host plant (Kiers et al. 2011;Wipf et al. 2019). Such variances may be partly explained by the different lifestyles of the partially saprotrophic Mucoromycotina vs. the strictly biotrophic Glomeromycotina (Field et al. 2015b(Field et al. , 2016Field and Pressel 2018). Therefore, conventional 'rules' governing AMF-plant symbioses may not necessarily apply to Mucoromycotina-plant symbioses. It is possible that when a[CO 2 ] is high, liverworts and relatively simple vascular plants such as L. inundata produce photosynthates that they are unable to utilise effectively for growth or reproduction as they possess no or limited vasculature and specialised storage organs to transport and store excess carbohydrates (Kenrick and Crane 1997). Consequently, surplus photosynthates may be either stored as insoluble starch granules, transferred directly to mycobionts (Field et al. 2016), or released into surrounding soil as exudates (Galloway et al. 2018). By moving excess photosynthates into mycobionts, the potential risk of pathogenicity from surrounding saprotrophic organisms such as bacteria and fungi may be reduced (Field et al. 2016).
Additionally, the biomass of mycorrhizal fungi may increase in response to elevated a[CO 2 ], but this increase does not necessarily result in greater nutrient transfer to the host plant (Alberton et al. 2005), instead inducing a negative feedback through enhanced competition for nutrients between the symbiotic partners (Fransson et al. 2007).
Studies on ectomycorrhizal fungi, another group of widespread plant-symbiotic fungi, some of which may act as facultative decomposers, showed that, despite an increase in the amount of extraradical hyphae under elevated a[CO 2 ], there was no corresponding enhanced transfer of N to the host, suggesting that the fungus had become a larger sink of nutrients (Fransson et al. 2005). While we did not measure fungal biomass in this study, our observation of greater colonisation in the roots of Lycopodiella plants grown under elevated a[CO 2 ] of 800 ppm compared to those grown under ambient concentrations but with no corresponding increase in fungus-to-plant N and P transfer may suggest a similar scenario.
We observed no difference in the amount of fungalacquired 33 P tracer transferred to L. inundata sporophytes between a[CO 2 ] treatments. This aligns with the responses of MFRE symbionts in non-vascular liverworts which also transferred the same amount (or more in the case of Treubia) of 33 P and more 15 N to plant hosts under ambient a[CO 2 ] compared to elevated a[CO 2 ] (Field et al. 2015a(Field et al. , 2016. The amount of 33 P transferred to L. inundata was up to 70 times less than has previously being recorded for Mucoromycotina in liverworts (Field et al. 2016) and for Glomeromycotinaassociated ferns and angiosperms (Field et al. 2012), despite the same amount of 33 P being made available, indicating that MFRE do not play a critical role in lycophyte P nutrition. MFRE transferred considerable amounts of 15 N to their host (see also Hoysted et al. 2019), under both a[CO 2 ] treatments. This observation together with previous findings that MFRE facilitate the transfer of both organic and inorganic 15 N to non-vascular plants (liverworts) suggest that MFRE may play a complementary role to AMF in plant nutrition, with a more prominent role in N assimilation than that of AMF Hoysted et al. 2019). While it has been shown that AMF can transfer N to their associated host (Ames et al. 1983;Hodge et al. 2001), significant doubts remain as to the ecological relevance of an AMF-N uptake pathway (see Read 1991;Smith and Smith 2011). In particular, the exact mechanism of N transfer and, more importantly, the amounts of N transferred via AMF compared to the N requirements of the plant remain equivocal . This murky view of AMF in N transfer, coupled with recent molecular re-identification of fine root endophytes as belonging within Mucoromycotina and not Glomeromycotina (Orchard et al. 2017a) and evidence pointing to a significant role of MFRE in 15 N transfer to both non-vascular (Field et al. 2015a(Field et al. , 2016 and vascular plants , suggests that effects on plant N nutrition previously ascribed to AMF instead might be attributable to co-occurring MFRE . Given that symbioses involving MFRE are much more widespread than initially thought, covering a wide variety of habitats (Bidartondo et al. 2011;Rimington et al. 2015Rimington et al. , 2020Orchard et al. 2017a, b, c;Hoysted et al. 2018Hoysted et al. , 2019, their role in plant N nutrition and responses to high a[CO 2 ] may have much broader ecological significance than previously assumed. It remains critical that we test how mycorrhizal plasticity (both AMF and MFRE) translates into function in order to understand how climate change may affect nutrient fluxes between symbionts in the past, present and, importantly, the future (Field and Pressel 2018).
In this study, we provide a first assessment of the effects of varying a[CO 2 ] on carbon-for-nutrient exchanges between MFRE and a vascular plant. Our results point to important differences in responses to changing a[CO 2 ] between MFRE and AMF and between MFRE symbioses in vascular vs. non-vascular plants; however, these results are so far restricted to one, early diverging, vascular species, generally growing in severely N-limited habitats. It is now critical that similar investigations are extended to a broader range of taxa, including flowering plants known to engage in symbiosis with both MFRE and AMF. In doing so, efforts towards the potential exploitation of these symbiotic fungi to help meet sustainability targets of the future may be better informed and the likelihood of success vastly improved.