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Intraspecific transfer of carbon between plants linked by a common mycorrhizal network

Authors:

Abstract

To quantify the involvement of arbuscular mycorrhiza (AM) fungi in the intraspecific transport of carbon (C) between plants we fumigated established Festuca ovina turf for one week with air containing depleted 13C. This labelled current assimilate in a section of mycorrhizal or non-mycorrhizal turf. Changes in the 13/12C ratio of adjacent, unfumigated plants, therefore, allowed the movement of C between labelled and unlabelled plants to be estimated. In mycorrhizal turves, 41% of the C exported to the roots from the leaves was transported to neighbouring plants. The most likely explanation of this is was the transport of C via a common hyphal network connecting the roots of different plants. No inter-plant transport of C was detected in non-mycorrhizal turves. There was no evidence that the C left fungal structures and entered the roots of receiver plants. Mycorrhizal colonisation increased carbon transport from leaves to root from 10% of fixed carbon when non-mycorrhizal to 36% in mycorrhizal turves. These results suggest that AM fungi impose a significantly greater C drain on host plants than was previously thought.
Plant and Soil 192: 153–159, 1997. 153
c
1997 Kluwer Academic Publishers. Printed in the Netherlands.
Intraspecific transfer of carbon between plants linked by a common
mycorrhizal network
J.D. Graves
1
, N.K. Watkins
1
, A.H. Fitter
1
, D. Robinson
2
and C. Scrimgeour
2
1
Biology Department, The University of York, PO Box 373, York YO1 5YW, UK and
2
Scottish Crop Research
Institute, Invergowrie, Dundee DD2 5DA, UK
Received 10 December 1996. Accepted in revised form 7 May 1997
Keywords: arbuscular mycorrhiza,carbonallocation, carbon cost, carbon transport, commonmycorrhizalnetwork,
13
C
Abstract
To quantify the involvement of arbuscular mycorrhiza (AM) fungi in the intraspecific transport of carbon (C)
between plants we fumigated established Festuca ovina turf for one week with air containing depleted
13
C. This
labelled current assimilate in a section of mycorrhizal or non-mycorrhizal turf. Changes in the
13 12
C ratio of
adjacent, unfumigated plants, therefore, allowed the movement of C between labelled and unlabelled plants to be
estimated.Inmycorrhizalturves,41%oftheCexportedtotherootsfromtheleaveswastransportedtoneighbouring
plants. The most likely explanation of this is was the transport of C via a common hyphal network connecting
the roots of different plants. No inter-plant transport of C was detected in non-mycorrhizal turves. There was no
evidencethat the Cleft fungalstructuresandenteredtheroots of receiver plants. Mycorrhizalcolonisationincreased
carbontransportfrom leavesto rootfrom10% of fixed carbon when non-mycorrhizalto 36% in mycorrhizalturves.
These results suggest that AM fungi impose a significantly greater C drain on host plants than was previously
thought.
Introduction
The hyphae of arbuscular mycorrhizal (AM) fungi
have been observed to link the roots of plants of the
samespecies (Hirrel and Gerdemann, 1979)and plants
of different species (Heap and Newman, 1980). AM
colonisation is believed frequently to arise from grow-
ing roots contacting the hyphae emanating from the
roots of other plants in the community. Therefore, it is
likely that most plants capable of infection are inter-
connected by a common mycorrhizal network (CMN)
(Newman, 1988) unless there is a greater degree of
specificity in the interaction than is generally believed.
Studiesusing
14
Chavedemonstratedcarbon move-
ment between plants linked by mycorrhizal hyphae
(Francis and Read, 1984; Hirrel and Gerdemann,
1979). However, such studies have been unable to:
(i) measure transport in both directions and thereby
demonstrate whether there is any net transport in one
FAX No:+441904432860.E-mail:JDG3@York.ac.uk
direction, since no simultaneous measurement of
12
C
flow is possible, and (ii) in the case of pulse labelled
experimentstoquantifytheC transfer,becausethespe-
cific activity of the source is unknown. Furthermore,
the factors determining movement of C are uncertain.
Francis and Read (1984) found that shading of the
receiver plant increased C movement towards it, sug-
gestingthatsource-sinkrelationshipscontrolledmove-
ment. In contrast, Waters and Borowicz (1994) found
that there was no increase in
14
C transfer when one
neighbour was clipped above ground to alter its sink
strength for C.
Some of the problems inherent in using
14
C
have been overcome by using ratios of stable iso-
topes (
13 12
C) to trace C transfer. Watkins et al.
(1996)utilised the natural difference in
13
C abundance
between the C
3
species Plantago lanceolata (mean
13
C-28‰) and the C
4
Cynodon dactylon (mean
13
C
-13.5‰) to estimate C transfer between them. They
demonstrated C transfer from the C
3
to the C
4
plant
JS: PIPS No. 141614 BIO2KAP
plso6702.tex; 1/10/1997; 19:37; v.7; p.1
154
was in the range 0 to 41% (i.e. up to 41% of the C
in the ‘receiver plant originated from the ‘donor to
whichit wasconnected).However,C transferwas usu-
ally less than 10%. Clearly a major limitation of this
technique is that it can only be used on C
3
-C
4
pairs
of plants. We describe here a
13
C technique which
can quantify C movement between plants with the
same photosynthetic pathway. It relies on a fumiga-
tion procedure whereby half the plants are exposed to
air from which all the CO
2
has been removed and then
replaced with CO
2
from a bottled gas source. The bot-
tled CO
2
is much more depleted in
13
C(
13
C -30‰)
than atmospheric CO
2
is ( -8‰) and can therefore be
used to isotopicallylabel plants exposed to it. We used
this technique to quantify AM mediated C movement
between Festuca ovina plants growing in a turf to esti-
mate how much C was transferred between plants of
the same species when their roots were colonised or
not by AM.
Material and methods
Turf preparation
Nine turves of Festuca ovina (25 cm 40 cm 14 cm
depth)werecutfromlarge(2.5m 2.5m 40cmdepth)
turveswhich had been grownon a 50%sand/50%John
Innes compost mixture in a glasshouse for over a year.
One of the large turves was non-mycorrhizal whilst
the other had been inoculated with 550 g of a mixture
of four species of the genus Glomus obtained from
Agricultural Genetics Company (MicroBio Division,
Rothamsted Experimental Station, Harpenden, UK).
Turves were watered as required and when there were
signs of nutrient deficiency they were watered with
a Rorison’s nutrient solution. Mycorrhizal and non-
mycorrhizalturves were of a similar appearance. Each
small turf was placed into a plastic box (25.5 cm 42
cm 15 cm and left for approximately 8 weeks before
use. A partition was placed across the middle of each
box and in orderto ensure that there was no subsurface
leakage of air between fumigation compartments this
partition penetrated 2 cm below the soil surface. The
turf was watered daily and to encourage plant growth,
two days prior to the fumigation period the turf was
watered with a Rorisons solution modified to contain
no phosphorous.
Fumigation procedure
Each turf was fumigatedseparately for a period of one
week. In total five mycorrhizal turves were treated and
four non-mycorrhizal turves (one less than intended
owing to the breakdown of the growth chamber). For
each fumigation run a turf was placed within a Sanyo
Fitotron growth chamberat 16 C day/12 Cnighttem-
perature, with a photosynthetic photon flux density of
250 mol m
2
s
1
at plant height during the 16 hour
photoperiod. Two perspex boxes (25 cm 20 cm 20
cm height, volume 101) were placed over the turf, one
on either side of the central partition, and airtight seals
made at their bases (see Figure 1a). Air was drawn
througheach of the boxes by fans at a rate of 2.5 1 s
1
.
One side of the turf received air from the outside of
the building (containing CO
2
with
13
C = -8‰where
13
C=[(
13 12
C
sample
/
13 12
C
standard
)-1 1000). The oth-
er side of the turf received air from which all the
CO
2
had been removed by passing through a soda
lime column and replaced with CO
2
from a cylinder
(with
13
C<30‰; Figure 1). CO
2
concentration in the
airstream was adjusted to that in the ambient air using
an ADC WA524 (Analytical Development Company,
Hoddesdon, UK) CO
2
controller.
Plant sampling and analysis
Samples were taken from each corner of each com-
partment (see Figure 1b). Thus in each compartment,
two samples were taken from a point 2 cm from the
divide and two samples 18 cm away from the divide.
Several individual plants were removed in each sam-
ple and divided into roots and shoots. Only roots still
connected to the shoots were included in the root frac-
tion.
13
C was determined in oven dried samples as
described by Watkins et al. (1996). Analytical preci-
sion was 0.2‰. For each turfthepresenceor absence
of mycorrhizal colonisation was checked in root sub-
samples using the staining procedure of Merryweath-
er and Fitter (1991). All root samples from the myc-
orrhizal turves were heavily colonised by AM fun-
gi whilst all root samples from the non-mycorrhizal
turves were uncolonised.
Calculation of carbon transfer
In order to calculated whether C had been transferred
from plants rooted in the labelled side of the turf to
plants in the unlabelled side, comparisons were made
between plants close to the divide and those distant
plso6702.tex; 1/10/1997; 19:37; v.7; p.2
155
Figure 1. a.Plan of the system used to fumigate one side of a Festuca ovina turf with
13
C depleted CO
2
whilst the other side is flushed with
ambient air. b. Location and coding of tissue samples taken from the Festuca ovina turf after one weeks fumigation (top view). c. Root and
shoot
13
C values (mean and standard error) after one week of labelling.
plso6702.tex; 1/10/1997; 19:37; v.7; p.3
156
from the divide. With reference to Figure 1b we can
usethe followingsymbolsto designatethe
13
C values
of the four root samples:
Ab
r
= Ambient air, plant close to the border, root
sample
Ad
r
= Ambient air, plant distant from the border,
root sample
Fb
r
= fumigated with bottled CO
2
, plant close to
the border, root sample
Fd
r
= Fumigated with bottled CO
2
, plant distant
from the border, root sample
Shoot samples are designated by a subscript s
insteadofsubscriptr.Cin, ororiginatingfrom,labelled
plants was more depleted in
13
C(i.e.hadamore
negative
13
C) than C, in or originating from, plants
exposed to ambient CO
2
.
Ad and Fd values were considered to represent
‘background’
13
C abundances in the shoots and roots.
This assumed that plants close to the partition had con-
siderablymoremycorrhizalconnectionswith eachoth-
er than with those distant from the partition. So, Ad
plants were less likely to have received C from plants
grown in labelled CO
2
than Ab plant. Thus, Ab
r
-Ad
r
canbe used as an indexofhowmuchCmovedfromFb
to Ab plants during the week long fumigation. Had no
C moved this index would be zero. Had net movement
occurredfrom the plants receiving
13
C depleted C, this
indexwouldbenegative(Ab
r
<Ad
r
).Forthemovement
of C in the reverse direction, the corresponding index
isFb
r
-Fd
r
. Again,thiswouldbezero fornoC transfer,
but positive if C had been transferred.
The proportion of Carbon transferred can be esti-
mated in the mycorrhizal turves.
If index of
13
C
depleted C crossing the divide
and index of the background amount
of
13
C-depleted C received by the fumigated roots
then proportion of total
13
C-depleted C that is transferred
Table 1. Comparison of the index of carbon movement between myc-
orrhizal and non-mycorrhizal turves. Ab
r
-Ad
r
= a measure of the
13
C
depleted carbon that has moved from the fumigated side of the chamber
whilst Fb
r
-Fd
r
is a measure of the amount of
13
C enriched carbon that has
moved in the opposite direction (see text for details). values calculated
by one way analysis of variance, F
1 7
. The standard error of the mean is
shown in brackets
Mycorrhizal turves Non-mycorrhizal turves =
Ab -Ad -0.388 (0.152) 0.093 (0.107) 0.045
Fb -Fd 0.012 (0.234) 0.0425 (0.082) 0.92
The total amount of
13
C-depleted C absorbed (L
t
) can
be represented as:
Thus, the proportion of that
13
C-depleted C that is
transferred from shoots to roots (L
r s
) is given by:
This assumes that above and below ground biomass
are equal.
Results
Ab
r
-Ad
r
was negative in mycorrhizal turves, indicat-
ing net movement of C from labelled plants (Figure
1c, Table 1). This index was not significantly different
from zero in the non-mycorrhizal turves and was less
thanthe precisionofthe
13
Canalysis(see above).The
difference in Ab
r
-Ad
r
between mycorrhizal and non-
mycorrhizal turves was significant ( =0.045).Howev-
er, the index Fb
r
-Fd
r
was not significantly different
fromzeroineitherthe mycorrhizalor non-mycorrhizal
turves and, again, was less than analytical precision.
The proportion of C transferred in mycorrhizal
turves was 0.41 ( 0.04 SE). No detectable amount
of C was transferred in non-mycorrhizal turves since
no significant movements of C were detected (Figure
1c, Table 1).
Sinceeachturfwas fumigatedseparately,therewas
variationintheamountof Cabsorbedby theturvesas a
consequence of differentphotosyntheticrates between
individual exposures.
Therefore, the amount of
13
C-depleted C received
by the fumigated side of the turves will vary between
runs. However, there was a significant correlation
plso6702.tex; 1/10/1997; 19:37; v.7; p.4
157
Figure 2. The relationship between the indices of the amount of
13
C
depleted carbon reaching theroots offumigated plants (Fd
r
-Ad
r
)and
the amount of
13
C depleted carbon crossing the central divide into
the roots of plants treated with ambient air (Ab
r
-Ad
r
) in mycorrhizal
turves. Regression equation y=0.551x + 0.173, r
2
=0.92, F
1 3
=33.7,
=0.01. Each point represents one turf.
( =0.01) between the amount of
13
C depleted C that
was transferred (Ab
r
Ad
r
) and the total amount of
13
C
depleted C that was absorbed (Fd
r
-Ad
r
) (Figure 2).
Itispossiblethat gas leakageoffumigatedaircould
occurfromonehalfofthechambertotheother.If sothe
Ab plants would be closer to any contamination which
could alter their
13
C signal and such an alteration
would be apparent in shoot tissue. However, Ab
s
-Ad
s
was not significantly different from zero (Student’s t
test =0.27).
The proportion of that
13
C-depleted C that is trans-
ferred from shoots to roots(L
r s
) was 0.36 ( 0.07 SE)
in mycorrhizal turves compared with 0.10 ( 0.04 SE)
forthe non-mycorrhizalturves; the differencebetween
them was significant (Anova, F
1 7
=9.78, =0.017).
Discussion
Robustness of the technique
We have demonstrated that stable carbon measure-
ments coupled with fumigation using
13
C depleted
CO
2
can be usedto quantifyC transfer between plants.
This technique has several advantages over the use of
14
C especially where long term fumigation is need-
ed to measure processes near equilibrium. Using
13
C
labelling,net C transport over long periods of time can
be measured. At the same time, C transfer from shoots
to roots can be estimated. Experiments which use con-
tinuouslabelling with
14
Care capable of quantifyingC
flux from the labelled plant to the unlabelled plant but
are incapableof simultaneouslymeasuring the amount
of C moving in the opposite direction. Therefore the
net C transfer cannot be quantified. This severely con-
strainsthe designof experimentsto investigatethe fac-
tors that control C movement. This constraint which
can be relieved adopting the use of stable C isotope
labelling. A disadvantage of using
13
C labelling is that
the plants must be fumigated for a relatively long peri-
od of time. Judging from our results one week is near
the minimum period required to ensure a sufficient
change in the
13
C/
12
C ratio. In contrast
14
C labelling
can be used to investigate C movement over much
shorter time scales.
Potentially this technique can be used to measure
bi-directionalmovementofC,althoughweonlydetect-
ed transfer away from the fumigated plants. However,
the sensitivity of this technique is less for the plants
on the fumigated side of the divide as there is an addi-
tional source of error affecting their
13
C value. The
13
C value of the roots of these plants can be affect-
ed both by variation in the amount of
13
C-depleted C
absorbedphotosyntheticallyby thesampledplants and
by the amount of transport from neighbouring unfu-
migated plants. In contrast the
13
C value of plants on
the unfumigated side is only affected by the amount
of
13
C-depleted C transferred from the fumigated side
of the divide. We do not therefore believe that these
results demonstrate unequivocally one-way transfer.
A potentially serious problem with this technique
is the possible leakage of gas from one chamber to the
other. Thoseplantsnearestthesourceof contamination
would fix more of this gas thereby leading to a differ-
ence in the
13
C value of the Ab
s
and Ad
s
samples.
Two pieces of evidence indicate that such contami-
nation did not occur. First the amount transferred is
positively correlated with the amount of
13
C depleted
C entering the roots of the fumigated plants. Secondly,
if there were gaseous contamination then the shoots of
the unfumigatedplants would be more heavily labelled
than their roots and there would be a significant dif-
ference between the Ab
s
and Ad
s
samples. No such
difference was observed.
Role of C demand in plant-mycorrhizal associations
Being mycorrhizal increased carbon transfer to the
roots from 10% of the carbon fixed to 36%. This is
larger than other estimates of increased root allocation
in mycorrhizalplants; an increase of 10% in Vicia faba
(Pang and Paul, 1980), 14% in Allium porrum (Snell-
plso6702.tex; 1/10/1997; 19:37; v.7; p.5
158
groveetal.,1982)and Glycine max (Harrisetal.,1985)
and 37% in Citrus volkameriana (Peng et al., 1993).
Then are three possible reasons for the higher figure
in our study: i) that AM colonisation was better estab-
lished in this > 1 year old, perennial turf compared
with annual crop species a few weeks old; ii) a com-
mon mycorrhizal network interlinking many plants is
greater sink for C than the mycelium associated with
a single plant; and iii) that the root fraction of mycor-
rhizal plants was lower than that of non-mycorrhizal
plants, which is commonly observed (Hayman and
Mosse, 1972; Smith, 1982).
There was a significant difference in the index of
transport (Ab
r
-Ad
r
) between the mycorrhizal and non-
mycorrhizal turves. However, there was also greater
transport of
13
C-depleted C to the roots in the myc-
orrhizal plants. Therefore, if transport via the CMN
occurred, two factors might have determined the size
of that transfer: alteration in the source-sink relation-
ships within the donor plant; and the amount of C
exported from that plant into the CMN.
Our results rule out an alternative explanation for
the significant difference in Ab
r
-Ad
r
. This is that some
other process, such as transfer and re-assimilation of
root exudates (Jones and Darrah, 1995) was responsi-
blefor the observedCtransfer,detectableinthemycor-
rhizal turves because of the greater amount of labelled
C in the roots of those plants. However, if that were
true, C would enter the rootcells via an uptake process
and C metabolic pathways. Some of that C would then
be transferred to the shoots. In our experiments, no
transfer of ‘donor C to ‘receiver’ shoots was detected
(i.e. Ab
s
-Ad
s
0). This is consistent with otherresults
(e.g. Francis and Read, 1984; Watkins et al., 1996). It
strongly suggests that C transferred from one plant to
anothervia aCMN remains in fungalstructures within
roots.
Approximately 41% of the
13
C depleted C export-
ed from leaves to roots of fumigated F. o vi na was
transported to nearby unfumigated plants. This is con-
siderably greater than the average transfer detected by
Watkins et al. (1996) between neighbouring plants of
different species. Plantago lanceolata and Cynodon
dactylon (< 10%). The Watkins et al. study differed
from the present one in two important ways: AM
colonisation in the Festuca turves was well estab-
lished whereas between P. lanceolata and C. dacty-
lon colonisation was only a few weeks old; and intra-
specific CMN links may be more abundant than inter-
specific links. Although the latter explanation is possi-
ble,Chiarelloetal.(1982)showedinafieldexperiment
that movement of materials between mycorrhizally-
linked plants in a field experiment was apparently
unconstrained by taxonomic relatedness. The more
likely explanation is therefore, that colonisation was
more intense in this mature turf.
Conclusions
Our results confirm the demonstration by Watkins et
al. (1996) that transfer of C between the root systems
of neighbouring plants connected by a CMN can be
considerable. They emphasise that the carbon cost of
mycorrhizal symbiosis to the plant can be large, and
possibly much greater in established vegetation than
has been proposed from experiments on single plants.
There has been much debate on the physiological and
ecologicalsignificanceofC transportbyaCMN(New-
man, 1988), but this new evidence strongly suggests
that C stays within fungal structures in the roots of
‘receiverplants and that speculations about the ability
of adult plants to ‘foster juveniles, for example, are
probably unfounded. The large quantities of C mov-
ing from root system to root system within the fungal
mycelium suggest that transfer is a reflection of the
growth pattern of the fungus, rather than the operation
of symbiotic processes.
Acknowledgements
This work was funded by the Natural Environment
Research Council under the Terrestrial Initiative in
GlobalEnvironmentalResearch (TIGER)programme.
We are grateful to Dr RDP Cargeeg of the Agricultural
Genetics Company for the supply of the mycorrhizal
inoculum.
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Section editor: J H Graham
plso6702.tex; 1/10/1997; 19:37; v.7; p.7
... These results suggest that the host plant maintained a supply of C to its AMF symbionts to ensure its own ability to obtain soil mineral nutrition from the AMF's mycelia (Fitter et al., 1998;Lekberg et al., 2010). On the other hand, C transfer via an AM network does not allow resource sharing among linked plants (Robinson and Fitter, 1999). The mycocentric view is that fungal structures within roots are parts of extended mycelia through which fungi move C according to their own C demands, not those of their autotrophic hosts (Fitter et al., 1998). ...
... They concluded that an asymmetric C exchange between coexisting plant species could contribute to forest resilience. However, the mechanism of C transfer and role of mycorrhizal hyphae in the direct transfer of C are not well established (Robinson and Fitter, 1999;Smith and Read, 2008). Therefore, more needs to be done to lay out the arguments for why and how CAMN transfer of C could contribute to the accumulation of C in ecosystems. ...
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Arbuscular mycorrhizal fungi (AMF) are ubiquitous in soil and form nutritional symbioses with ~80% of vascular plant species, which significantly impact global carbon (C) and nitrogen (N) biogeochemical cycles. Roots of plant individuals are interconnected by AMF hyphae to form common AM networks (CAMNs), which provide pathways for the transfer of C and N from one plant to another, promoting plant coexistence and biodiversity. Despite that stable isotope methodologies (¹³C, ¹⁴C and ¹⁵N tracer techniques) have demonstrated CAMNs are an important pathway for the translocation of both C and N, the functioning of CAMNs in ecosystem C and N dynamics remains equivocal. This review systematically synthesizes both laboratory and field evidence in interplant C and N transfer through CAMNs generated through stable isotope methodologies and highlights perspectives on the system functionality of CAMNs with implications for plant coexistence, species diversity and community stability. One-way transfers from donor to recipient plants of 0.02-41% C and 0.04-80% N of recipient C and N have been observed, with the reverse fluxes generally less than 15% of donor C and N. Interplant C and N transfers have practical implications for plant performance, coexistence and biodiversity in both resource-limited and resource-unlimited habitats. Resource competition among coexisting individuals of the same or different species is undoubtedly modified by such C and N transfers. Studying interplant variability in these transfers with ¹³C and ¹⁵N tracer application and natural abundance measurements could address the eco physiological significance of such CAMNs in sustainable agricultural and natural ecosystems.
... Some of the main arguments against these experiments, call for the use of appropriate controls using mesh barriers [21] excluding root-root contact and passive C diffusion through soil. Several studies [22,23] have shown that C fixed by one plant transferred to the root system, and presumably the hyphae, of the second plant. However, for C to have any eco-physiological importance for the recipient plant, it needs to move out of the roots of the recipient plant. ...
... For DNA-SIP, we used a published protocol [22,44] with the following modifications: 4 ± 1.6 μg DNA samples were loaded onto gradient buffer (GB) to a total volume of 1.15 ml. The GB + DNA solution was mixed with 5 mL of cesium chloride (CsCl, Thermo Scientific, Waltham, USA). ...
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Inter-kingdom belowground carbon (C) transfer is a significant, yet hidden, biological phenomenon, due to the complexity and highly dynamic nature of soil ecology. Among key biotic agents influencing C allocation belowground are ectomycorrhizal fungi (EMF). EMF symbiosis can extend beyond the single tree-fungus partnership to form common mycorrhizal networks (CMNs). Despite the high prevalence of CMNs in forests, little is known about the identity of the EMF transferring the C and how these in turn affect the dynamics of C transfer. Here, Pinus halepensis and Quercus calliprinos saplings growing in forest soil were labeled using a ¹³CO2 labeling system. Repeated samplings were applied during 36 days to trace how ¹³C was distributed along the tree-fungus-tree pathway. To identify the fungal species active in the transfer, mycorrhizal fine root tips were used for DNA-stable isotope probing (SIP) with ¹³CO2 followed by sequencing of labeled DNA. Assimilated ¹³CO2 reached tree roots within four days and was then transferred to various EMF species. C was transferred across all four tree species combinations. While Tomentella ellisii was the primary fungal mediator between pines and oaks, Terfezia pini, Pustularia spp., and Tuber oligospermum controlled C transfer among pines. We demonstrate at a high temporal, quantitative, and taxonomic resolution, that C from EMF host trees moved into EMF and that C was transferred further to neighboring trees of similar and distinct phylogenies.
... Over the last three decades, it has been described, in agro-ecosystems, that nutrients can be transferred between neighbouring plants (Bethlenfalvay et al., 1991;Fitter et al., 1998;Jalonen et al., 2009;Thilakarathna et al., 2016). With the use of isotopes, interplant transfer of various macro-and micro-elements essential for plants, such as nitrogen, phosphorus, and carbon has been reported to follow concentration gradients through shared mycorrhizal fungi, root exudates or through root decomposition (Fitter et al., 1998;Graves et al., 1997;Jones et al., 2009;Kravchenko et al., 2021;Ren et al., 2013;Robinson & Fitter, 1999). Interplant nutrient transfer has been mainly studied in agroecosystems ...
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Phenological segregation among species in a community is assumed to promote coexistence, as using resources at different times reduces competition. However, other unexplored nonalternative mechanisms can also result in a similar outcome. This study first tests whether plants can redistribute nitrogen (N) among them based on their nutritional temporal demand (i.e. phenology). Field ¹⁵N labelling experiments showed that ¹⁵N is transferred between neighbour plants, mainly from low N‐demand (late flowering species, not reproducing yet) to high N‐demand plants (early flowering species, currently flowering‐fruiting). This can reduce species' dependence on pulses of water availability, and avoid soil N loss through leaching, having relevant implications in the structuring of plant communities and ecosystem functioning. Considering that species phenological segregation is a pervasive pattern in plant communities, this can be a so far unnoticed, but widely spread, ecological process that can predict N fluxes among species in natural communities, and therefore impact our current understanding of community ecology and ecosystem functioning.
... The amounts reported by Giesemann et al. (2021) are substantial, with proportional C gain up to 73% for the angiosperm Gentiana lutea L. and up to 93% for the fern Athyrium filix-femina (L.) Roth. These data contrast with earlier studies (with AM plants that form the Arum-type mycorrhiza) where the amount of C found in the receiver mycorrhizal plants was quite small and mainly located in the roots, suggesting that the larger part or almost all of this C was actually in the AM fungal biomass and hence under fungal control and used for storage (Fitter et al. 1998;Graves et al. 1997;Pfeffer et al. 2004). The authors of those earlier studies therefore concluded that the C transfer does not have an impact on plant fitness, while it is an important element in fungal C budget and hence fungal fitness. ...
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Background Arbuscular mycorrhizal (AM) symbiosis has been referred to as the mother of all plant root symbioses as it predated the evolution of plant roots. The AM research is a multidisciplinary field at the intersection of soil science, mycology, and botany. However, in recent decades the nature and properties of soils, in which the AM symbiosis develops and functions, have received less attention than desired. Scope In this review we discuss a number of recent developments in AM research. We particularly cover the role of AM symbiosis in acquisition of phosphorus, nitrogen, heavy metals and metalloids, as well as water by plants from soil; mycorrhizal effects on plant nutritional stoichiometry and on the carbon cycle; the hyphosphere microbiome; so-called facultative mycorrhizal plants; explanations for lack of mycorrhizal benefit; common mycorrhizal networks; and arbuscular and ectomycorrhizal ecosystems. Conclusion We reflect on what has previously been described as mycorrhizal ‘dogmas’. We conclude that these are in fact generalisations on the AM symbiosis that are well supported by multiple studies, while admitting that there potentially is a geographical bias in mycorrhizal research that developed in temperate and boreal regions, and that research in other ecosystems might uncover a greater diversity of viable mycorrhizal and non-mycorrhizal strategies than currently acknowledged. We also note an increasing tendency to overinterpret data, which may lead to stagnation of some research fields due to lack of experiments designed to test the mechanistic basis of processes rather than cumulating descriptive studies and correlative evidences.
... The common mycorrhizal networks (CMNs) link all the host plants in the ecosystems. In CMNs, host plants transfer carbon molecules to fungi (Graves et al. 1997;Wang et al. 2016), where fungi transport the nutrients and water to the host plants in return (Awaydul et al. 2019;Egerton-Warburton et al. 2007;He et al. 2019b;Müller et al. 2020;Muneer et al. 2020;Singh et al. 2019;Walder et al. 2015). Interaction in the CMNs is critical for vegetation establishment (Bent et al. 2011;Kytöviita et al. 2003) and may have essential roles in maintaining monodominance in tropical rain forests (McGuire 2007). ...
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Mycorrhizal symbiosis has been evolved to be ubiquitous in natural and agricultural ecosystems. Mycorrhiza formation helps host plants acquire more nutrients and water, thereby improving host plant resistance to abiotic and biotic stresses. Molecular crosstalk begins between symbiotic partners before the establishment of mycorrhizal symbiosis. Signaling molecules and small secreted proteins are then released from the two symbionts. Signaling molecules released from the fungi include Myc factors, indole 3-acetic acid, and hypaphorine, etc. Meanwhile, they secrete some carbohydrate active enzymes (e.g., proteases and lipases), and proteins with conserved LysM and CFEM motifs. These secreted signaling molecules and proteins function outside the host cell wall and improve the establishment efficiency of mycorrhizal symbiosis. Here we focus on the functions of these signaling molecules and secreted proteins released from mycorrhizal fungi at the early stage of mycorrhiza formation. Since global advances are much slower than those involved in pathogenic fungi, we hope the research in this field promotes deservedly.
... The total 14 C transfer was expected to be greater in the intra-than inter-specific treatments; this prediction was based on several previous studies which suggested that C transfer is preferential when receiver plants are full-siblings of the donor tree . A theory known as the kin selection theory is widely supported by previous studies (Graves et al., 1997;Verbruggen et al., 2012;Platt and Bever, 2009;Dudley et al., 2013;Murphy and Dudley, 2009;Asay, 2013). The mother tree hypothesis goes further suggesting that recognition can go as far as trees sensing their root exudates of their offspring (Nara, 2006). ...
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Soil microorganisms and their symbiotic relationships with plants are fundamental to nutrient cycling in temperate forest ecosystems. This highly diverse microbiome contains up to a quarter of Earth’s biodiversity, but our understanding of how this affects the function of forests is not well understood. This thesis investigated the role of plant symbionts on the allocation of C to belowground microbial symbionts and to ground vegetation via microbial symbionts. Radio-isotope pulse labelling was used to determine the belowground C dynamics of these highly complex systems by allowing us to quantify pools and fluxes within the plant-microbe-soil continuum. In Chapter 3, the role of arbuscular and ecto-mycorrhizal fungi in belowground allocation of C in three temperate tree species was investigated by destructive harvesting of trees 336 days after a pulse label had been applied. The results suggested that Alnus glutinosa and Betula pendula allocated C belowground to microbes, whereas Castanea sativa transferred the C to the soil where it was sequestered. In Chapter 4, inter- and intra-specific C transfer was studied using trees connected via a common mycorrhizal network (CMN), the results suggested that more C was transferred between inter- than intra-specific species combinations. In Chapter 5, C transferred via three “donor” tree species to the root nodules of A. glutinosa “receiver” tree connected with a CMN was investigated using the methodology pioneered in Chapter 3. The plant: fungal amalgam preferentially allocated C from the donor trees to the root nodules of the receiver A. glutinosa tree. We postulated that this was due to the considerable energetic demands of nitrogen-fixation by Frankia alni in the root nodule creating a strong C sink. In Chapter 6, the transfer of C from 13-year-old coppiced A. glutinosa and C. sativa trees to ground vegetation via CMN was investigated. 14C activity in the ground vegetation under the A. glutinosa trees was expected to be greatest, as A. glutinosa share arbuscular mycorrhizal partnerships with the ground vegetation. No difference in 14C activity was found in the hyphae, soil solution or ground vegetation under A. glutinosa. We postulated that this could be due to root grafting, mycorrhizal types exchanging nutrients, or reabsorption of tree rhizodeposits. Overall this study suggests that the plant: microbe symbiosis that is ubiquitous across the temperate biome is both important for nutrient cycling and C storage, but also that the sharing of resources via CMNs could be altering plant competition dynamics that have previously been based on the assumption that plants are not physically connected and actively sharing resources. Further work to determine how plants or mycorrhizae control belowground resource sharing could lead to a paradigm shift in our understanding of competition and facilitation in plant community dynamics.
... Moreover, extensively branched extraradical mycelia can interconnect neighboring plants to form common mycorrhizal networks (CMNs) [4][5][6]. These CMNs can affect the distribution of mineral nutrients like carbon [7,8], N [9], and phosphorus [10] among the connected plants. This could ultimately influence the plant's establishment [11,12], survival [13,14], growth [15] and physiology [16,17]. ...
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Common mycorrhizal networks (CMNs) allow the transfer of nutrients between plants, influencing the growth of the neighboring plants and soil properties. Cleistogene squarrosa (C. squarrosa) is one of the most common grass species in the steppe ecosystem of Inner Mongolia, where nitrogen (N) is often a key limiting nutrient for plant growth, but little is known about whether CMNs exist between neighboring individuals of C. squarrosa or play any roles in the N acquisition of the C. squarrosa population. In this study, two C. squarrosa individuals, one as a donor plant and the other as a recipient plant, were planted in separate compartments in a partitioned root-box. Adjacent compartments were separated by 37 µ m nylon mesh, in which mycorrhizal hyphae can go through but not roots. The donor plant was inoculated with arbuscular mycorrhizal (AM) fungi, and their hyphae potentially passed through nylon mesh to colonize the roots of the recipient plant, resulting in the establishment of CMNs. The formation of CMNs was verified by microscopic examination and 15 N tracer techniques. Moreover, different levels of N fertilization (N0 = 0, N1 = 7.06, N2 = 14.15, N3 = 21.19 mg/kg) were applied to evaluate the CMNs' functioning under different soil nutrient conditions. Our results showed that when C. squarrosa-C. squarrosa was the association, the extraradical mycelium transferred the 15 N in the range of 45-55% at different N levels. Moreover, AM fungal colonization of the recipient plant by the extraradical hyphae from the donor plant significantly increased the plant biomass and the chlorophyll content in the recipient plant. The extraradical hyphae released the highest content of glomalin-related soil protein into the rhizosphere upon N2 treatment, and a significant positive correlation was found between hyphal length and glomalin-related soil proteins (GRSPs). GRSPs and soil organic carbon (SOC) were significantly correlated with mean weight diameter (MWD) and helped in the aggregation of soil particles, resulting in improved soil structure. In short, the formation of CMNs in this root-box experiment supposes the existence of CMNs in the typical steppe plants, and CMNs-mediated N transfer and root colonization increased the plant growth and soil properties of the recipient plant.
Chapter
Arbuscular mycorrhizal (AM) fungi are of paramount importance that develop a good mutual relationship with higher plants. The impact of different environmental gases on AM symbiosis has not been studied extensively. The available data suggest that elevated CO2 increases the biomass and productivity of plants. However, the effect of CO2 on mycorrhizal symbiosis is still a matter of debate. The impact of CO2 on the development of mycorrhiza and spore production is a very interesting aspect to be unravelled. Assessment of the effect of SO2 and O3 is also not much congenial to the growth and development of mycorrhizal fungi. These gases cause enormous negative impacts on the plant’s biomass and productivity, as well as mycorrhizal network. In general, the effects of these gases are influential to biomass production and mycorrhizal spore formation and thus need further attention from the researchers.
Preprint
Mycorrhizal fungi can interlink and connect plants in a common mycorrhizal network (CMN). Studying CMNs is challenging due to pathways of material transfer but also plant and mycorrhizal effects that have to be tested and controlled in order to be able to evaluate the presence and magnitude of a specific CMN effect. These controls let to a clear but strict definition of CMN which requires experiments to fulfill specific criteria: at least two plants are connected by the CMN, all plants are mycorrhized, the roots of the connected plants are separated, there is a CMN treatment tested, and the hyphal continuity is tested. Here, we evaluate the evidence base of the CMN research specifically for arbuscular mycorrhiza via a systematic mapping approach. We found that not all studies were testing true CMNs but rather common fungal networks (CFN), including filamentous fungi other than the targeted mycorrhizal fungi. The number of articles conducting experiments on CMNs drops strongly with increasingly stringent fulfillment of the CMN definition. Additionally, there is a focus on lab studies and specific fungal strains; however, researchers have used diverse plant species setups. Also plant, fungal and resource transfer responses are preferentially measured, while microbial community metrics and ecosystem functions and processes are neglected.We see a need to strengthen the CMN evidence base and thus we call for a renewed research effort on CMN, focusing on a whole range of levels of mechanistic resolution (from CFN to CMN with and without hyphal continuity). Additionally, neglected experimental situations (e.g. field studies in general) and microbial community or ecosystem-level responses should be included in future research.
Article
We examined how simulated herbivory, fungicide, and genet affect the magnitude and direction of net carbon transfer between paired mycorrhizal Lotus corniculatus. One plant in each pair was labeled with C-14, and C-14 levels in the unlabeled plant were quantified. Without fungicide, the roots of unlabeled plants received significantly more C-14 when the labeled partner was clipped than when the unlabeled plant was clipped, indicating that net carbon flow was away from clipped plants and toward unclipped plants. Because the specific activity of donor roots was unaffected by simulated herbivory, fungicide, and genet, significant differences in net carbon flow were not simply due to differences in C-14 uptake by labeled plants. Clipping did not affect carbon transfer between plants in trays treated with the fungicide benomyl, which probably reduced but did not eliminate VAM colonization. The three genets did not differ. The median C-14 levels of unlabeled root samples were only 1.2% the C-14 levels of labeled plants' roots and thus constituted a very small portion of their carbon budget. C-14 levels in stems of unlabeled plants were never above background, suggesting that the fungal symbiont retained most of the transferred carbon. Although clipping can affect net carbon flow, we failed to detect significant differences in the amount of C-14 leaking from the roots of clipped vs unclipped plants. This study suggests that grazed mycorrhizal plants are unlikely to gain significant amounts of carbohydrates from neighbors and may actually experience a net loss.
Article
S ummary Carbon (C) transfer between onion plants was enhanced by vesicular‐arbuscular mycorrhizas formed by the fungus, Glomus etunicatus. By applying pentachloronitrobenzene (PCNB) to hyphae, C translocation to the root was reduced but not eliminated indicating that two transfer processes may be involved; namely, cytoplasmic translocation within hyphae and mass flow along hyphal walls. Most of the transferred C remained in the roots; little or no C was translocated to the shoots. Therefore, it is uncertain whether C was released to the recipient plant or retained in fungal tissue.
Article
Changes in the natural abundance of 13C were used to quantify carbon transfer between C3 and C4 plants in a common mycorrhizal network. Experiments using two mesh sizes to either prevent (0.45 μm) or allow (20 μm) mycorrhizal connections between Plantago lanceolata (C3) and Cynodon dactylon (C4) plants were run. Root and shoot samples were taken for δ13C determinations.It could not be assumed that all the pairs of plants were linked; therefore non-parametric statistical tests were used. In order to measure transfer between pairs of plants the shoot δ13C value was used as a reference and the deviation of the root δ13 C value from this as a measure of carbon transfer. As the C. dactylon root δ13 C value became more negative with the 20 μm mesh present, the root-shoot difference increased. In P. lanceolata both the root and shoot δ13C values became less negative but the root-shoot difference did increase gradually. When the root-shoot difference in C. dactylon was plotted against root δ13C value the relationship was ≈unity, suggesting that transferred carbon remained in the roots and fungal material did not move into the shoots. In P. lanceolata the results showed that the slope of the relationship between root-shoot difference and root δ13C value was ≈0.5. This suggests any transferred carbon moved into both the root and shoot material.The root-shoot difference can be used to estimate % carbon transfer. For individual C. dactylon plants the results varied from 0 to 41% with most values falling at 10% or below. It was not possible to calculate % transfer amounts for P. lanceolata. This range of variation could have important implications for plant interactions in communities.
Article
A two-compartment growth chamber in which the aboveground plant materials were exposed to ¹⁴CO2 and the belowground portion was exposed to ¹⁵N2 under normal atmospheric pressure was designed for carbon and nitrogen transfer studies. Vicia faba infected with vesicular-arbuscular fungus Glomus mossae and non-mycorrhizal plants fixed similar quantities of N2 at an age of 6½ wk. Approximately 0.10 mg N was fixed∙g⁻¹ dry plant materials∙day⁻¹ and 40 mg C∙g⁻¹ dry matter day⁻¹ were synthesized by mycorrhizal and non-mycorrhizal fababeans during 48 h exposure to ¹⁴CO2 at 6½ wk with no apparent difference in yield of dry matter. The non-mycorrhizal plants transferred 37% of the fixed ¹⁴C beneath ground. The mycorrhizal ones transferred 47% of the fixed ¹⁴C beneath ground. Most of the difference could be accounted for in the belowground respiration. The ¹⁴CO2 produced by root-microbial systems of the mycorrhizal fababeans was twice as great as that of the nonmycorrhizal; both contained active rhizobium.
Article
Carbon uptake and allocation in plants that were largely dependent on microbial symbionts for N and P was compared to that in plants given inorganic fertilizer. Soybeans (Glycine max L. Merr.) were grown in sterilized soil and were either left uninoculated, or were inoculated with Rhizobium japonicum (Kirschner), or both R. japonicum and Glomus fasciculatum (Thaxter sensu Gerd.). Uninoculated plants were given N and/or P fertilizer at rates required to produce plants similar in size to inoculated plants. Carbon flows to plant parts, root nodules and vesicular-arbuscular mycorrhizas were measured in six- and nine-week-old plants by determining the distributions of 14C after pulse labelling with 14CO2. Root nodules in non-mycorrhizal plants utilized 9% of total photosynthate; this was increased to 12% in nodulated, mycorrhizal plants. Mycorrhizas used 17% of the total photosynthate of six-week-old plants; this fell to 8% after nine weeks. Rates of 14CO2 fixation in leaves of nodulated or nodulated plus mycorrhizal plants were up to 52% higher than in plants without microbial symbionts. Part of the increase was due to higher specific leaf area in plants colonized by symbionts, but other factors such as source-sink relationships, starch mobilization and leaf P concentrations were also involved in the host-plant adaptations to the C demand of the microbial endophytes.
Article
Leek plants (Allium porrum) were grown on partially sterilized soil either inoculated (M) or not (NM) with the vesicular-arbuscular mycorrhizal fungus, Glomus mosseae. They were pulse-fed with 14CO2 in an apparatus which allowed CO2 subsequently respired either by the shoots or by the roots plus soil to be separately monitored. There were three experiments. In two, plants were harvested 48 h after labelling and in the third after 214 h. At harvest, the distribution of 14C between shoot, root, soil organic matter and root washings was measured. Similar growth curves for M and NM plants were obtained by supplying extra phosphorus to the latter, so that C distributions for both treatments could be compared directly. In all three experiments, about 7 % more of the total fixed C was translocated from shoot to root in M plants compared to NM plants. In the third experiment, this extra translocate could be accounted for by increased root respiration plus increased loss of C to the soil but, despite this drain, M and NM plants had equal rates of C assimilation per unit of leaf area. However, shoots of M plants had a lower content of dry matter and hence higher assimilation rates expressed on a dry matter basis. Increased hydration is suggested as a mechanism whereby leaf area and hence C assimilation increases in mycorrhizal plants and which offsets the effects of the drain imposed by the mycorrhizas.
Article
Onion plants were grown in a range of soils labeled with 32P. It was found that although the mycorrhizal plants had taken up more phosphorus and grown larger, the proportion of 32P to total P (specific activity) taken up by mycorrhizal and non-mycorrhizal plants after 10 weeks was not significantly different. It is concluded that the mycorrhizal roots used the same source of labile phosphate but explored a greater volume of soil beyond the zone of phosphate depletion near the root surface. There was no indication that mycorrhizal roots had access to sources of phosphate different from those accessible to non-mycorrhizal roots. The specific activity of NaHCO3-extractable phosphorus differed considerably between the eight soils but the specific activity of absorbed phosphorus in the plants always corresponded closely to that of the soil in which they had grown.
Article
Publisher Summary The chapter discusses mycorrhiza, a symbiotic, non-pathogenic association between a plant root and a fungus. This paper first summarizes evidence that mycorrhizal links between plants that occur. It then reviews evidence on various possible functions of these links, and finally considers if there is any evidence that the links influence the species composition and structure of plant communities, and ecosystem processes such as nutrient cycling. Evidence on almost every aspect of mycorrhizal links and their possible roles is inadequate; any conclusions must therefore be preliminary and tentative. There is evidence that seedlings can become infected by forming mycorrhizal links with established plants, and growth of seedlings of some species is faster under these conditions. Transfer of I4C from one plant to another via mycorrhizal links can occur, but it is not clear that net transfer of organic compounds is ever great enough to increase significantly growth or survival of the receiver plant. There is no clear evidence that mycorrhizal links prevent these relationships from occurring or introduce fundamentally new interactions between plants. The evidence so far available suggests that mycorrhizal links can alter the relationships between plants, but that they do so by modifying competition and nutrient cycling rather than replacing them.
Article
S ummary During early growth of mycorrhizal and non‐mycorrhizal plants of Trifolium subterraneum fertilized with soluble (Na 2 HPO 4 ) phosphate, inflow of phosphate (moles P absorbed per unit length root per unit time) into mycorrhizal roots from soil exceeded that into non‐mycorrhizal roots over a range of levels of phosphate. High rates of uptake (up to 45 × 10 ⁻¹⁵ mol phosphate cm ⁻¹ s ⁻¹ ) were associated with reductions in root: shoot dry wt ratios. The length of mycorrhizal root per plant was little affected by fertilization with phosphate. However, rapid growth of roots at high levels of Na 2 HPO 4 resulted in reductions in percentage root length infected by mycorrhizas. Results are discussed with respect to rates of uptake by whole plants and to differences in distribution of phosphate between roots and shoots in mycorrhizal and non‐mycorrhizal plants.
Article
Using a buried slide technique, hyphal connections are shown to exist between different roots on one plant, Lolium perenne L., and also between two roots of different species L. perenne and Plantago lanceolata L. These two species are commonly found together in permanent pasture.