Common mycorrhizal networks of European Beech trees drive belowground allocation and distribution of plant-derived C in soil

Author(s):  
Bruna Imai ◽  
Stefan Gorka ◽  
Julia Wiesenbauer ◽  
Werner Mayerhofer ◽  
Christina Kaiser

<p>Mycorrhizal fungi are an important partner of almost all land plants, who trade soil nutrients, such as Phosphorus or Nitrogen, for photosynthetic Carbon (C). Moreover, mycorrhizal fungi connect multiple plants with their mycelium in so called Common Mycorrhizal Networks (CMNs). CMNs formed by ectomycorrhizal (EM) fungi are an inherent part of boreal and temperate forests, often termed the ‘wood-wide web’. However, the role of these networks for plant belowground C allocation and distribution is not well known.</p><p>Here, we examined how plant photosynthates are distributed within EM mycelium networks connecting pairs of young beech trees, addressing the following questions: (1) Is the total belowground C allocation of plant photosynthates influenced by the size of the mycorrhizal network and its access to resources? (2) Is the belowground C distribution within a CMN altered if trees have unequal access to C from photosynthesis? (3) Do CMNs amplify or alleviate competition for nutrients between connected trees?</p><p>We planted young beech trees in pots in a special two-plant box set-up which allows to control the establishment of mycorrhizal networks between them. For this, two plant pots, penetrable by fungal hyphae but not by roots, were placed inside of plastic boxes and the interstitial space was filled with quartz sand. In addition, a hyphal-exclusive N source consisting of <sup>15</sup>N labeled peat (‘peat bag’), was buried within each plant pot. Two treatments were applied in a fully factorial design: 1) Allowing/preventing the establishment of a CMN between the pots (some pots were turned around at a regular interval to prevent the establishment of CMNs) and 2) inequality of access to photoassimilated C (in part of the boxes one of the two plants was shaded). In a <sup>13</sup>C-CO<sub>2</sub> labeling approach, we traced <sup>13</sup>C assimilated by one plant of each tree pair into belowground pools of both plants by isotope ratio mass spectrometry (EA-IRMS) and <sup>13</sup>C phospholipid fatty acid (PLFAs) analysis (GC-IRMS). At the same time, we investigated plant uptake of <sup>15</sup>N via mycorrhiza by EA-IRMS.</p><p>Our results demonstrate that plants relied mostly on their fungal partners to acquire nutrients (63% of plant N was derived from mycorrhiza-exclusive peat bags), and also directed the majority of the C allocated belowground to their mycorrhizal partners. The presence of a larger mycorrhizal network connecting to another plant and an additional N source almost doubled photosynthetic CO<sub>2</sub> assimilation and belowground C allocation by plants. Fungi translocated carbon via hyphal linkages preferentially into mycorrhiza-exclusive nutrient patches, even when they were located within the realm of a neighboring plant and this necessitates to cross a nutrient-poor zone of sand. Shading did not affect the belowground distribution of C.</p><p>We conclude that belowground ectomycorrhizal networks represent a significant sink strength for plant photosynthates and may thus be a major driver of C sequestration in beech forest soils. The belowground distribution of C via fungal networks is mainly related to the distribution of nutrient-rich patches in the soil and less to differences in the photosynthetic capacity of the host plants.</p>

2014 ◽  
Vol 94 (6) ◽  
pp. 1025-1032 ◽  
Author(s):  
F. L. Walley ◽  
A. W. Gillespie ◽  
Adekunbi B. Adetona ◽  
J. J. Germida ◽  
R. E. Farrell

Walley, F. L., Gillespie, A. W., Adetona, A. B., Germida, J. J. and Farrell, R. E. 2014. Manipulation of rhizosphere organisms to enhance glomalin production and C-sequestration: Pitfalls and promises. Can. J. Plant Sci. 94: 1025–1032. Arbuscular mycorrhizal fungi (AMF) reportedly produce glomalin, a glycoprotein that has the potential to increase soil carbon (C) and nitrogen (N) storage. We hypothesized that interactions between rhizosphere microorganisms, such as plant growth-promoting rhizobacteria (PGPR), and AMF, would influence glomalin production. Our objectives were to determine the effects of AMF/PGPR interactions on plant growth and glomalin production in the rhizosphere of pea (Pisum sativum L.) with the goal of enhancing C and N storage in the rhizosphere. One component of the study focussed on the molecular characterization of glomalin and glomalin-related soil protein (GRSP) using complementary synchrotron-based N and C X-ray absorption near-edge structure (XANES) spectroscopy, pyrolysis field ionization mass spectrometry (Py-FIMS), and proteomics techniques to characterize specific organic C and N fractions associated with glomalin production. Our research ultimately led us to conclude that the proteinaceous material extracted, and characterized in the literature, as GRSP is not exclusively of AMF origin. Our research supports the established concept that GRSP is important to soil quality, and C and N storage, irrespective of origin. However, efforts to manipulate this important soil C pool will remain compromised until we more clearly elucidate the chemical nature and origin of this resource.


2004 ◽  
Vol 82 (8) ◽  
pp. 1140-1165 ◽  
Author(s):  
Suzanne W Simard ◽  
Daniel M Durall

It is well known from laboratory studies that a single mycorrhizal fungal isolate can colonize different plant species, form interplant linkages, and provide a conduit for interplant transfer of isotopic carbon, nitrogen, phosphorus, or water. There is increasing laboratory and field evidence that the magnitude and direction of transfer is influenced by physiological source–sink gradients between plants. There is also evidence that mycorrhizal fungi play a role in regulating transfer through their own source–sink patterns, frequency of links, and mycorrhizal dependency. Although it is plausible that connections are extensive in nature, field studies have been hampered by our inability to observe them in situ and by belowground complexity. In future, isotopic tracers, morphological observations, microsatellite techniques, and fluorescent dyes will be useful in the study of networks in nature. Mycorrhizal networks have the potential to influence patterns of seedling establishment, interplant competition, plant diversity, and plant community dynamics, but studies in this area are just beginning. Future plant community studies would benefit from concurrent experimental use of fungal network controls, isotopic labeling, direct observation of interplant linkages, and long-term observation in the field. In this paper, we review recent literature on mycorrhizal networks and interplant carbon transfer, suggest future research directions, and highlight promising scientific approaches.Key words: common mycorrhizal network, carbon transfer, source–sink, establishment, competition, diversity.


2012 ◽  
Vol 9 (8) ◽  
pp. 3357-3380 ◽  
Author(s):  
S. Luyssaert ◽  
G. Abril ◽  
R. Andres ◽  
D. Bastviken ◽  
V. Bellassen ◽  
...  

Abstract. Globally, terrestrial ecosystems have absorbed about 30% of anthropogenic greenhouse gas emissions over the period 2000–2007 and inter-hemispheric gradients indicate that a significant fraction of terrestrial carbon sequestration must be north of the Equator. We present a compilation of the CO2, CO, CH4 and N2O balances of Europe following a dual constraint approach in which (1) a land-based balance derived mainly from ecosystem carbon inventories and (2) a land-based balance derived from flux measurements are compared to (3) the atmospheric data-based balance derived from inversions constrained by measurements of atmospheric GHG (greenhouse gas) concentrations. Good agreement between the GHG balances based on fluxes (1294 ± 545 Tg C in CO2-eq yr−1), inventories (1299 ± 200 Tg C in CO2-eq yr−1) and inversions (1210 ± 405 Tg C in CO2-eq yr−1) increases our confidence that the processes underlying the European GHG budget are well understood and reasonably sampled. However, the uncertainty remains large and largely lacks formal estimates. Given that European net land to atmosphere exchanges are determined by a few dominant fluxes, the uncertainty of these key components needs to be formally estimated before efforts could be made to reduce the overall uncertainty. The net land-to-atmosphere flux is a net source for CO2, CO, CH4 and N2O, because the anthropogenic emissions by far exceed the biogenic sink strength. The dual-constraint approach confirmed that the European biogenic sink removes as much as 205 ± 72 Tg C yr−1 from fossil fuel burning from the atmosphere. However, This C is being sequestered in both terrestrial and inland aquatic ecosystems. If the C-cost for ecosystem management is taken into account, the net uptake of ecosystems is estimated to decrease by 45% but still indicates substantial C-sequestration. However, when the balance is extended from CO2 towards the main GHGs, C-uptake by terrestrial and aquatic ecosystems is offset by emissions of non-CO2 GHGs. As such, the European ecosystems are unlikely to contribute to mitigating the effects of climate change.


2020 ◽  
Vol 10 (1) ◽  
Author(s):  
Veronika Řezáčová ◽  
Milan Řezáč ◽  
Hana Gryndlerová ◽  
Gail W. T. Wilson ◽  
Tereza Michalová

AbstractIn a globalized world, plant invasions are common challenges for native ecosystems. Although a considerable number of invasive plants form arbuscular mycorrhizae, interactions between arbuscular mycorrhizal (AM) fungi and invasive and native plants are not well understood. In this study, we conducted a greenhouse experiment examining how AM fungi affect interactions of co-occurring plant species in the family Asteracea, invasive Echinops sphaerocephalus and native forb of central Europe Inula conyzae. The effects of initial soil disturbance, including the effect of intact or disturbed arbuscular mycorrhizal networks (CMNs), were examined. AM fungi supported the success of invasive E. sphaerocephalus in competition with native I. conyzae, regardless of the initial disturbance of CMNs. The presence of invasive E. sphaerocephalus decreased mycorrhizal colonization in I. conyzae, with a concomitant loss in mycorrhizal benefits. Our results confirm AM fungi represent one important mechanism of plant invasion for E. sphaerocephalus in semi-natural European grasslands.


2005 ◽  
Vol 83 (6) ◽  
pp. 638-646 ◽  
Author(s):  
J M Kranabetter

The possible benefit of common mycorrhizal network linkages to seedling growth was tested in a low light partial-cut forest understory. Naturally regenerated western hemlock (Tsuga heterophylla Raf.) and hybrid spruce (Picea glauca × Picea sitchensis [Moench] Voss) seedlings were transplanted directly into soil or within bags of different pore sizes to restrict the amounts of root and ectomycorrhizal contact. The 5-year study included "full contact" (no bag), "moderate contact" (250-µm openings), and "low contact" (4-µm openings) treatments. Height increment was lowest for full contact seedlings over most of the experiment, and highest for low contact seedlings by years 4 and 5. Full contact seedlings also had slightly lower foliar N content than moderate and low contact seedlings. There were no significant interactions in growth detected between tree species and treatments, despite the higher potential for common mycorrhizal network linkages between a western hemlock understory and canopy. Fifty-eight ectomycorrhizal fungal morphotypes were identified on the seedlings, including many with smooth mantles or with only sparse emanating hyphae, which likely reduced the potential for common mycorrhizal network linkages. These results would support the more traditional concepts of competition for scarce resources by isolated seedlings as the primary interaction for the understory of these mature forests.Key words: common mycorrhizal networks, facilitation, shade tolerance, competition.


2006 ◽  
Vol 72 (6) ◽  
pp. 3901-3907 ◽  
Author(s):  
P. J. Maxfield ◽  
E. R. C. Hornibrook ◽  
R. P. Evershed

ABSTRACT A time series phospholipid fatty acid (PLFA) 13C-labeling study was undertaken to determine methanotrophic taxon, calculate methanotrophic biomass, and assess carbon recycling in an upland brown earth soil from Bronydd Mawr (Wales, United Kingdom). Laboratory incubations of soils were performed at ambient CH4 concentrations using synthetic air containing 2 parts per million of volume of 13CH4. Flowthrough chambers maintained a stable CH4 concentration throughout the 11-week incubation. Soils were analyzed at weekly intervals by gas chromatography (GC), GC-mass spectrometry, and GC-combustion-isotope ratio mass spectrometry to identify and quantify individual PLFAs and trace the incorporation of 13C label into the microbial biomass. Incorporation of the 13C label was seen throughout the experiment, with the rate of incorporation decreasing after 9 weeks. The δ13C values of individual PLFAs showed that 13C label was incorporated into different components to various extents and at various rates, reflecting the diversity of PLFA sources. Quantitative assessments of 13C-labeled PLFAs showed that the methanotrophic population was of constant structure throughout the experiment. The dominant 13C-labeled PLFA was 18:1ω7c, with 16:1ω5 present at lower abundance, suggesting the presence of novel type II methanotrophs. The biomass of methane-oxidizing bacteria at optimum labeling was estimated to be about 7.2 � 106 cells g−1 of soil (dry weight). While recycling of 13C label from the methanotrophic biomass must occur, it is a slower process than initial 13CH4 incorporation, with only about 5 to 10% of 13C-labeled PLFAs reflecting this process. Thus, 13C-labeled PLFA distributions determined at any time point during 13CH4 incubation can be used for chemotaxonomic assessments, although extended incubations are required to achieve optimum 13C labeling for methanotrophic biomass determinations.


Oecologia ◽  
2007 ◽  
Vol 154 (3) ◽  
pp. 455-466 ◽  
Author(s):  
Amanda L. Schoonmaker ◽  
François P. Teste ◽  
Suzanne W. Simard ◽  
Robert D. Guy

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