https://doi.org/10.5194/bg-2022-165
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c Author(s) 2022. CC BY 4.0 License.
Phosphorus regulates fungal biomass production in a Norway spruce forest
Juan Pablo Almeidaa, Lorenzo Menichettib, Alf Ekbladc, Nicholas P. Rosenstockd, & HåkanWallandera
a
Lund University, Microbial Ecology, Dept of Biology, SE-223 62 Lund, Sweden
b
Sveriges Lantbruksuniversitet (SLU), Department of Ecology, Ulls Väg 17, Uppsala, Sweden
c
School of Science and Technology, Örebro University, SE- 701 82, Örebro, Sweden
d
Center for Environmental and Climate Research, Lund University, SE-22362 Lund, Sweden
Corresponding author: Juan Pablo Almeida, jpalmeidava@gmail.com
Abstract
1
2
Ectomycorrhizal fungi (EMF) are important components of the soil microbial
3
communities and EMF biomass can potentially increase carbon (C) stocks by
4
accumulating in the soils as necromass and producing recalcitrant structures. EMF
5
growth depends on the C allocated belowground by the host trees and the nutrient
6
limitation on tree growth is expected to influence this allocation. Therefore, studying
7
EMF production and understanding the factors that regulates it in natural soils is
8
important to understand C cycling in forests.
9
10
Ingrowth meshbags are commonly used to estimate EMF production, but these
11
measurements might not reflect the total EMF production since turnover rates of the
12
hyphae are not considered. Here we estimated fungal production and turnover in
13
response to P fertilization in a Norway spruce forest where nitrogen (N) deposition
14
has resulted in phosphorus (P) limitation of plant production by using a combination
15
of meshbags with different incubation periods and with Bayesian inferences. To test
16
how localized patches of N and P influence EMF production and turnover we
17
amended some bags with a nitrogen source (methylene urea) or P source (apatite).
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Additionally, the Bayesian model tested the effect of seasonality (time of meshbag
19
harvesting) on fungal production and turnover.
20
21
We found that turnover of EMF and was not affected by P fertilization or meshbag
22
amendment. P fertilization had a negative effect on EMF production in all the
23
meshbag amendments suggesting a reduced belowground C allocation to the
24
extramatrical mycelium under high P status. Apatite amendment significantly
25
increased EMF biomass production in comparison with the pure quartz bags in the
26
control plots but not in the P-fertilized plots. This indicates that P-rich patches
27
enhance EMF production in P limited forests, but not when P is not limiting. Urea
28
amendment had a general positive effect on EMF production, but this was
29
significantly reduced by P fertilization, suggesting that a decrease in EMF production
30
under high P status also will affect N foraging. Seasonality had a significant effect on
31
fungal production and the differences registered between the treatments were higher
32
during the warmer months and disappeared at the end of the growing season.
33
34
Many studies highlight the importance of N for regulating belowground C allocation
35
to EMF in northern coniferous forests, but here we show that the P status of the forest
36
can be equally important for belowground carbon allocation to EMF production in
37
areas with high N deposition.
38
39
40
Key words: Ectomycorrhizal fungi, fungal growth, fungal turnover, nitrogen
deposition, phosphorus limitation, apatite, methylene urea, Bayesian inference.
41
42
43
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1 Introduction:
45
In terrestrial ecosystems forest soils are important reservoirs for carbon (Falkowski et
46
al., 2000). Boreal forests contribute approximately 50% of the total forest carbon
47
stock from which around 85% is stored in the soil (Malhi et al., 1999). At least half of
48
the carbon stock in boreal soils originates from belowground carbon allocation
49
through roots (Clemmensen et al., 2013) and a large portion of boreal forest primary
50
production is allocated belowground by the trees (Gill & Finzi 2016). The carbon
51
dynamics in forest soils are highly dependent on the soil microbial communities that
52
either enhance C losses by degrading organic matter or increase C stocks by
53
immobilizing C (Clemmensen et al., 2013). Filamentous fungi forming mycorrhizal
54
associations for example, play an important role for C fluxes since some species have
55
the capability to degrade a great variety of organic compounds while others can
56
contribute to soil organic matter formation by releasing exudates that promote soil
57
aggregation (Rillig, 2005) or produce slowly decomposing and highly melanized
58
hydrophobic tissues (Almeida et al., 2022). The effect of EMF on soil microbial
59
communities might not be trivial since up to 20% of the net primary production is
60
allocated belowground to support the symbiosis (Hobbie, 2006). Therefore,
61
ectomycorrhizal mycelium is expected to be a significant part of the soil fungal
62
biomass and its production and turnover play an important role in forest carbon
63
cycling and organic matter formation (Ekblad et al., 2013). For that reason, the
64
development of methods that allows us to quantify EMF growth in forests natural
65
soils is of paramount importance (Fernandez, 2021)
66
67
Therefore, understanding the factors that regulate the growth rates of filamentous
68
fungi like EMF is important to understand carbon dynamics in soils. Growth rates of
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free-living fungi from natural soils has been studied in laboratory by measuring
70
labeled acetate incorporated in the fungal membrane component ergosterol (Sheng et
71
al., 2022; Rousk and Bååth, 2007) or labeled water incorporated into DNA (Schwartz
72
et al., 2016). Quantifying growth (production) of EMF natural communities on the
73
other hand is more complicated since EMF are dependent on plant roots (Smith and
74
Read, 2008) and such measurements must be performed when the fungi is living in
75
symbiosis. Many studies have attempted to quantify EMF production in situ in forests
76
soils by using ingrowth meshbags and fungal biomarkers like ergosterol or PLFAs
77
(Wallander et al., 2013). In those studies, EMF production has been estimated based
78
on the standing fungal biomass measured in meshbags after a specific time of
79
incubation in the soil (Ekblad et al., 2013; Wallander et al., 2013; Wallander et al.,
80
2001). However, the standing biomass does not necessary reflect growth since the
81
standing biomass is the result of the interaction between fungal growth and the
82
residence time of the fungal mycelium in the meshbag (Ekblad et al., 2016). In order
83
to overcome these shortcomings, some studies have estimated EMF production and
84
mycelium turnover by repeated harvests of mycelial meshbags, applying ergosterol as
85
a marker of mycelial biomass and mathematical models to estimate the production
86
and turnover of EMM biomass (Hagenbo et al., 2021; Hagenbo et al., 2017) or,
87
combined with analyses of chitin, to enable estimates of production and turnovers of
88
both bio- and necromass (Ekblad et al., 2016). In these studies, the standing biomass
89
and necromass were analyzed in bags incubated over periods varying in length,
90
combining several shorter periods, one after the other, with overlapping longer
91
periods. Common assumptions in these studies were that EMF growth occurs at a
92
constant rate and that biomass and necromass were lost at constant exponential rates
93
(Ekblad et al., 2016).
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95
By using this approach, Ekblad et al. (2016) tested the effect of nitrogen (N)
96
fertilization on EMF turnover and growth in a Pinus taeda forest. They reported that
97
fertilization significantly decreased both fungal standing biomass and growth but
98
turnover rates of biomass and necromass were not affected. It was suggested that the
99
decrease in fungal growth was regulated by changes in carbon allocation as a result of
100
an increase in soil fertility. These results are in line with evidence indicating that the
101
relative amount of carbon allocated to EMF is sensitive to plant nutrient status and
102
soil fertility (Gill & Finzi 2016). Thus, in boreal forests where N is the nutrient that
103
limits tree growth (Högberg et al., 2017), high amounts of carbon are invested below
104
ground to support ectomycorrhizal symbiosis to facilitate N uptake (Gill & Finzi
105
2016).
106
107
The role of N as limiting nutrient in high latitude forested ecosystems and its effect on
108
EMF is well known and has been described in several studies (Binkley & Högberg,
109
2016; Hedwall et al., 2013 ; Gill & Finzi, 2016) . However, it has been suggested that
110
anthropogenic N deposition can potentially change the forests nutrient requirements
111
and push the system toward phosphorus (P) limitation (Tarvainen et al., 2016; Du &
112
Fang, 2014; Akselsson et al., 2010; Vitousek et al., 2010). In fact, in a region with
113
high N deposition in southwest Sweden, Almeida et al. (2019) reported that P
114
fertilization had a stronger effect on tree growth than N fertilization, subverting the
115
expectation that N is the main nutrient regulating plant growth in northern forests. The
116
effect of the transition from N to P limitation on the below ground C allocation and
117
EMF growth has not been studied in natural soils, but P deficiency is expected to
118
increase EFM biomass to improve P foraging and uptake (Rosenstock et al., 2016;
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Ekblad et al. 1995; Wallander & Nylund 1992). In a field study, Rosenstock et al.,
120
(2016) reported an increase in root- and ECM standing biomass in a Norway spruce
121
(Picea alba) forest limited by P compared to forests with sufficient P. In the field
122
study performed by Almeida et al. (2019) however, no effect on EMF standing
123
biomass was found in meshbags incubated for 133 days. Yet, since only the standing
124
biomass was measured and the turnover rates and production were not estimated, we
125
cannot exclude the possibility that P fertilization had an effect on EMF production, an
126
effect that cannot be detected by studying the standing biomass alone.
127
128
In this study, we aimed to improve our understanding of EMF production and
129
turnover in natural soils and to test how EMF production is affected when P is
130
limiting tree growth. In the forest described by Almeida et al. (2019) we estimated
131
EMF production and turnover using the mathematical model of Ekblad et al. (2016)
132
with Bayesian inferences. Since EMF production is likely to follow root growth
133
which varies with season (Coutts & Nicoll, 1990 ; Walker et al., 1986), we performed
134
a more extensive incubation scheme and more frequent harvests of bags than in
135
Ekblad et al., (2016). This allowed us to test the model considering the treatments
136
effects (P fertilization and meshbags amendments) and also considering their
137
interactions with seasonality (time of the growing season). Because EMF growth is
138
subsidized by the host, in exchange for N and P, EMF production should be affected
139
by the nutrients found at the hyphal front. Indeed, EMF biomass in P-poor forests is
140
stimulated around localized patches of the P-rich mineral apatite (Rosenstock et al.,
141
2016; Berner et al., 2012; Hagerberg et al., 2003). Therefore, besides purely sand-
142
filled meshbags, we incubated meshbags amended with apatite or methylene urea
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(referred as urea throughout the manuscript) in order to simulate soil N and P nutrient
144
patches respectively.
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146
Our hypotheses were:
147
148
•
P fertilization will decrease the biomass production of EMF mycelia.
149
•
Apatite amendment will increase EMF biomass production in the control plots
150
151
152
but not in P fertilized plots.
•
Urea amendment will increase EMF biomass production in the P fertilized but
not in the control plots.
153
154
2 Materials and Methods:
155
156
2.1 Field site and fertilization treatments
157
This study was performed at Tönnersjöheden forestry research station (56° 41’ N, 13°
158
6’ E, 80 m a.s.l.) with a mean annual temperature of 6.4 °C and a mean annual
159
precipitation of 1064 mm (Högberg et al., 2013). Soils are podzols developed in a
160
glaciofluvial parent material with a pH (in H2O) of 4.05 and a C/N of 25.1 in the mor
161
layer (Hansson, 2011; Högberg et al., 2013). The forests consist of managed Norway
162
spruce (Picea abies) planted on former pastureland in 1979. The site is in southwest
163
Sweden with an N deposition of 14.5 kg N-1 ha-1 yr-1 (Rosenqvist et al., 2007), which
164
is high in comparison with most other forests in the country (Akselsson, 2010;
165
Högberg et al., 2013). The experiment consisted of 6 plots (30-40 m x 25 m); 3
166
control and 3 fertilized with 200 kg P ha-1 of superphosphate (100 kg ha-1 applied
167
twice in September 2011 and July 2012).
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2.2 Experimental design
169
To estimate EMF mycelial production, ingrowth meshbags (Wallander et al., 2001)
170
were incubated in the plots. The meshbags were cylindrical, 2 cm wide and 10 cm
171
long. They were made of 50 µm nylon mesh and filled with approximately 40 g of
172
quartz sand. Three different amendments in the meshbags were used: pure-quartz,
173
apatite-amended (quartz and 2% (w/w) crushed apatite mineral with a grain size of 50
174
to < 250 nm) and urea-amended (quartz and 0.5% (w/w) granulated methylene urea).
175
The mesh-bags were vertically installed into holes made with a soil corer (2 cm
176
diameter) with the upper end of the bag at level with the soil surface.
177
178
To calculate turnover rates and biomass production as done by Ekblad et al. (2016),
179
sequential meshbag incubations were performed. For a five-month period starting in
180
July 2015 and ending in November 2015, the meshbags were incubated for variable
181
periods of time (30, 60, 90, 120 or 150 days; Fig 1).
182
183
There were five different 30-day incubation periods. Four 60-day incubation periods
184
each overlapping with two 30-day incubation periods. Three 90-day incubation
185
periods each overlapping with three 30-day incubation periods. Two 120-day
186
incubation periods each overlapping with four 30-day incubation periods. One 150-
187
day incubation period overlapping with all 30-day incubation periods.
188
The bags incubated over 30 days were incubated sequentially and when one set of
189
bags was collected, a new set of bags was directly installed using the same holes as
190
the ones just emptied (Fig 1).
191
In each plot, a pure-quartz meshbag for each of the incubation periods described
192
above was placed along a 15 m long transect. The distance between each meshbag
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was approximately 1.5 m. The apatite-amended and urea-amended bags were placed
194
10 cm (perpendicular to the long transect) at each side of the quartz meshbags. Three
195
15 m long transects were done to have three sub-replicates (for each set of bags) that
196
were pooled before further analysis to give one sample from each incubation period
197
and amendment (quartz, apatite and urea) per plot.
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199
Each incubation period consisted of 54 meshbags (2 treatments C/P, 3 replicated
200
plots, three sub-replicates, three amendments (2 x 3 x 3 x 3 =54). In total, 810
201
meshbags were installed and collected according to their incubation period.
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203
July
August
September
October
November
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205
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208
209
210
211
212
213
214
215
216
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Figure 1: Overview of the incubation design. Different color bars represent the incubation time periods:
Yellow corresponds to 30 days, Light green to 60 days, Dark green to 90 days, Purple to 120 days and
Blue to 150 days of incubation. The arrows represent the points in time when the same holes from the
previous incubation were used to incubate the next set of meshbags.
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219
Upon harvest, the meshbags were kept in an icebox until arrival to the laboratory
220
where they were stored at -20oC.
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The fungal cell membrane compound ergosterol, a proxy for fungal biomass, was
222
extracted and measured from 5 g of the pooled samples as per Bahr et al. (2013)
223
using high-pressure liquid chromatography (auto sampler L2130 with UV detector
224
L2400 by Hitachi, Japan). The fungal biomass was then expressed as µg of ergosterol
225
per gram of sand in the meshbag.
226
227
2.3 Mathematical models
228
The turnover rates and fungal biomass production were estimated applying the
229
mathematical model used in Ekblad et al. (2016). In this paper however the
230
mathematical model was tested under two assumptions:
231
Fungal production was dependent on the treatments alone (Model 1), or fungal
232
production was depended on treatments and sampling season (Model 2), allowing to
233
test for the interactions between treatment and seasonal effects.
234
235
Model 1:
236
237
This model works under the assumption that EMF production occurs at a constant rate
238
and that biomass is lost at a constant exponential rate (see Hagenbo et al., 2017 &
239
Ekblad et al., 2016). Briefly, the sum of the biomass during two sequential short
240
incubation periods is expected to exceed the biomass in an overlapping longer
241
incubation period due to an on average older mycelium and hence larger turnover in
242
bags with a longer incubation period.
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244
The model in its differential form is defined as:
245
𝑑𝐵
=𝑃− 𝜇∙𝐵
𝑑𝑡
246
247
248
Equation 1
249
Where 𝑃 is the production of new mycelium (in mass units), 𝐵 is the mycelium
250
biomass (also in mass units) and 𝜇 represent the mortality, the fraction dying over a
251
specified time-period (adimensional). This equation is solved over time as:
252
253
Equation 2
𝐵(𝑡) =
254
𝑃!
∙ (1 − 𝑒 "! # )
𝜇!
255
In our case we assumed that both 𝑃! and 𝜇! are influenced by the fertilization
256
treatments, denoted here by 𝑘, and we therefore assigned a specific (unknown) P and
257
𝜇 to each treatment in the Bayesian model.
258
259
Model 2:
260
261
Equation 2 has been utilized in other publications (Hagenbo et al. 2021; Hagenbo et
262
al. 2017; Ekblad et al., 2016) and one of the main assumptions of this model is that
263
fungal production occurs at a constant rate. However, fungal production can vary
264
depending on the time of the year (Coutts & Nicoll, 1990 ; Walker et al., 1986) so we
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tested a modification of the model by introducing an additional degree of freedom
266
into the model represented by the term 𝛽!,% , dependent on sampling seasons ( 𝑗) and
267
their interactions with treatments (𝑘) so that the calibration can apply to each
268
treatment a correction for seasonality (independent from the other treatments). When
269
the term 𝛽!,% = 1 then the model is equivalent to what described in eq. 1 and 2. We
270
utilized this model to decompose 𝑃 in two components, defining a new term 𝑃′:
271
272
273
Equation 3
𝑃′!,% = 𝑃0! ∙ 𝛽!,%
274
275
𝑃′!,% corresponds to 𝑃! (if the distributions were perfectly symmetric the average for P
276
and P´ should converge to the same value) but the predicted biomass production now
277
is the results from the interactions between sampling season and treatments.
278
279
Eq. 3 is then substituted into Eq. 2 by substituting 𝑃 with 𝑃′. The resulting model is
280
equivalent to the one described by Eq. 2 for certain parameter combinations and
281
describes the same curve. The only difference is that now two components are used to
282
decompose the variance explained by the calibrated model in two separate terms: 𝑃0!
283
which expresses the production variable with treatments only (𝑘); and 𝛽!,% which
284
expresses the effects of seasonality and their interactions with treatments. 𝑃0! is now
285
equivalent to the production normalized by the seasonality effect
286
and 𝛽!,% vary independently (therefore describing each point as a combination of k
287
and j) we avoid to make any strong assumption on the effect of seasonality (since we
288
are not imposing a parametric function of time to describe it but we let it free to vary
&'!,#
(!,#
. By letting 𝑃0!
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for each time point) or on its interactions with treatments (which are still free to vary
290
depending on the treatment), while on the other end we maximize the information we
291
can extract from the data by representing the interactions between the terms in one
292
single model calibration. If we instead relied on fully independent calibrations within
293
each subset of seasons × treatments we would have had to divide the data in 𝑗 × 𝑘
294
subsets where we would calibrate each model parameter independently, limiting each
295
calibration to a smaller number of samples.
296
2.4 The calibration:
297
The model was calibrated within a formal Bayesian framework, developed with the
298
Stan toolbox (Stan Development Team, 2021). This approach is based on a numerical
299
implementation of Bayesian statistics, which allows for a continuous update of the
300
knowledge while new data are developed, based on stochastic principles (through a
301
modification of the Metropolis-Hastings sampler). While we refer to relative
302
publications for technical details, the main assets of the method are that: a) we can
303
integrate and utilize previous information in the calibration, defining it as prior
304
probability distributions of model parameters (from now on, “priors), b) such
305
information is combined with the statistical information contained in the data to
306
determine the posterior distributions of model parameters and consequently
307
predictions, and such distribution is non-parametric (so not assuming any specific
308
shape but determined only by the available information). The methodology is
309
therefore extremely useful to combine multiple sources of information and very
310
valuable when information is scarce, and at the same time quite robust given that it
311
estimates detailed posterior probability distributions (which can be examined closely).
312
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In our case the methodology allows us to draw information from publications. This
314
information is considered probabilistically. It does add information to our final results
315
(our posterior distributions), but such information is combined with the information
316
contained in our data. The chosen statistical approach updates the old information
317
with new data, and old and new information can be therefore compared.
318
319
We calibrated both a model with only Eq. 2 (so considering only treatment effects;
320
Model 1) and one considering Eq. 2 and Eq. 3 (considering treatments × seasonality
321
effects; Model 2).
322
Priors for 𝑃! and 𝜇! were derived from the literature, both expressed as normal
323
distributions with deviation prudentially estimated as 25% of the mean (please note
324
that this does not mean that the prior was limited within this range, due to the tails of
325
the normal distributions).
326
𝑃! was expressed as
𝑃! ∼ 𝑁(0.099, 0.099 ∙ 0.25)
327
328
329
While 𝜇! as
𝜇! ∼ 𝑁(0.009, 0.009 ∙ 0.25)
330
331
332
Both priors were based on the mean fungal biomass production and turnover for forest
333
of similar age as the forest in the current study estimated by Hagenbo et al. (2017)
334
after unit conversion. The Bayesian system was run considering one independent 𝑃!
335
and 𝜇! for each treatment.
336
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When we also considered Eq. 3, priors for 𝑃0! were defined as the priors for 𝑃! while
338
priors for 𝛽% were set as uniform between 0 and 5.
339
𝛽 ∼ 𝑈(0,5)
340
Please note that 𝛽% = 1 means no seasonality effect, 𝛽% = 5 means a five-fold increase
341
of production due to seasonality, while 𝛽% = 0 means a complete halt of production
342
due to seasonal effect.
343
344
2.5 Statistical analysis and probability distribution comparisons
345
The standing biomass, data was tested for homogeneity of variances and normal
346
distribution using Levene’s and Shapiro Wilk tests, respectively. Analysis of the
347
variances (ANOVA), Tukey’s Post-hoc test and Dunn analyses were performed on the
348
data to check for statistical differences between the fertilization treatments and
349
meshbag amendments. The Levene’s and Shapiro Wilk tests, as well as ANOVA and
350
Dunn analyses were done by using R (R Core Team, 2014).
351
352
The stochastic approach of the Bayesian method produces Markov chains Monte
353
Carlo (MCMC) that represents a probability distribution with as many discrete
354
parameter values as iterations in the chains (in our case 10 independent chains of
355
10000 iterations, so a total of 100000 iterations), with a histogram that approximates a
356
continuous distribution (probability distribution). Thus, the predicted fungal
357
production and turnover for each treatment (fertilization regime and meshbag
358
amendment) is represented by a probability distribution.
359
360
The means of the probability distributions were calculated and the highest density
361
intervals of the estimated parameters were interpreted as confidence intervals at 95%
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and 90% (Kruschke and Liddel, 2018). To test the significance of the treatments
363
(fertilization regime, meshbag amendment and season), the confidence intervals of the
364
probability distributions were compared.
365
3 Results:
366
367
3.1 Mycelial standing biomass
368
The standing biomass of mycelia in the meshbags was significantly affected by
369
incubation period (time of the year) (Kruskal-Wallis, p < 0.0001, X2 = 116.4).
370
Biomass in one-month incubation mesh bags from July, August and September was
371
significantly higher than the biomass collected in October and November for both
372
control plots and P fertilized plots (Dunn´s test, p < 0.001, X2 = 26.1) (Fig 2).
373
Biomass in two-months incubation mesh bags from July-August and August-
374
September was significantly higher than the biomass collected in September-October
375
and October-November for both control plots and P fertilized plots (Dunn´s test, p <
376
0.001, X2 = 27.7; Fig 2). Fertilization significantly affected the standing biomass in
377
the quartz, apatite and urea-amended meshbags (Kruskal-Wallis, p < 0.05, X2 = 6.5; p
378
< 0.0001, X2 = 18; p < 0.0001, X2 = 15.5; respectively). Phosphorus fertilization
379
reduced the standing biomass in all the incubation times (numbers of incubation days)
380
for apatite urea and amended meshbags (Fig 3). Apatite amendment significantly
381
increased the standing biomass in comparison with the pure-quartz bags in the control
382
plots after 60 and 150 days of incubation (Dunn´s test, p < 0.05, X2 = 18; p < 0.05, X2
383
= 11.2, respectively), and the effect of apatite was stronger after 150 days of
384
incubation where on average the biomass in the apatite bags was three-fold higher
385
than the biomass in the pure-quartz bags. Apatite amendment did not increase
386
biomass in the P-fertilized plots in any incubation time while urea amendment
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387
increased biomass in most of the incubation times and for both C and P fertilized plots
388
(Dunn´s test, p < 0.05) (Fig 3).
Control
Control
0.5
0.5
a
0.4
0.4
ab
0.3
0.2
0.1
0.1
0.0
0.5
0.0
0.5
a
ab
a
0.2
b
0.2
0.1
0.0
0.5
0.0
0.5
a
0.4
ab
b
ab
0.2
0.1
a
ab
ab
b
ab
a
ab
b
b
a
0.3
0.2
0.1
0.0
0.0
Phosphorus
Phosphorus
0.5
0.5
0.4
0.4
b
0.1
a
a
a
a
ab
0.2
b
b
0.1
ab
ab
b
b
quartz
a
0.3
0.3
0.2
a
0.1
0.0
0.5
0.0
0.5
a
0.4
b
0.3
0.2
urea
ab
urea
ab
0.3
0.1
a
a
a
a
a
0.1
r
ov
em
N
ob
ct
O
em
pt
be
er
r
be
t
us
2
FW
RE
HU
Se
Uí
EH
HP
SW
6H
Au
g
be
í1
ov
e
m
FW
R
2
HP
SW
6H
Wí
XV
AX
J
r
U
EH
U
EH
us
t
JX
O\
íA
ug
Ju
ly
0.0
0.0
390
391
392
393
394
395
a
0.4
0.4
0.2
389
0.2
0.0
0.5
0.0
0.5
0.4
0.3
0.1
quartz
Standing biomass (ergosterol ug per g)
b
apatite
ab
apatite
a
0.3
0.2
urea
b
urea
0.3
b
0.3
0.1
0.4
ab
quartz
0.3
ab
0.4
0.4
quartz
Standing biomass (ergosterol ug per g)
b
0.2
a
apatite
ab
apatite
0.3
Figure 2: Boxplot of the standing fungal biomass in the meshbags incubated in the soil for 2 and 1
months. The boxes represent the interquartile range of the data (The central represents the median).
Higher and lower whiskers represent minimum and maximum range of the data (1.5 times the length of
the interquartile range). Lowercase letters represents statistically significant (P<0.05) differences
between the incubation periods according to Dunn´s test.
396
397
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398
399
400 Figure 3: Standing fungal biomass in the three meshbags amendments (quartz-only, apatite and urea) and
401 in the control plots (red symbols) and P-fertilized plots (blue symbols) and control plots during different
402 incubation times (30, 60, 90, 120 and 150 days). The error bars represent the standard error of the mean.
403
404
3.2 Fungal production and turnover rates (Model 1)
405
The predicted fungal biomass production varied between the P-fertilized plots and the
406
control plots and between the meshbag amendments (Fig 4a). P fertilization
407
significantly decreased fungal production in all the meshbag amendments (urea and
408
apatite and quartz) (Table 1). In the P-fertilized plots the fungal production was
409
reduced to a third in the apatite and pure quartz bags in comparison with the prior
410
used to set the model (0.099 g m2 day-1). P fertilization caused a reduction on average
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411
of 43% in the quartz bags, 60% in the apatite bags and 39% in the urea bags in
412
comparison with the control plots.
413
414
The meshbags amended with urea had the highest predicted biomass production in
415
both control and P-fertilized plots (Fig 4). Relative to the quartz bags, the urea
416
amendment doubled the production in both fertilizer treatments. The apatite
417
amendment, in contrast, gave no significant change in production relative to the
418
quartz bags in the P-fertilized plots while a 35% increase was found relative to the
419
quartz bags in the Control plots (Table 1).
420
421
According to the mathematical modeling, the biomass turnover rates were not affected
422
by P fertilization or meshbag amendment (Fig 4 b).
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423
424
425
426
427
428
Figure 4: a) Probability distribution of the predicted fungal biomass production (Pk) (g m2 day-1) for the
different fertilizer treatments (Control and P fertilization) and meshbag amendments (quartz-only,
apatite and urea). b) Probability distribution of the turnover rates (day-1) for the different fertilizer
treatments (Control and P fertilization) and meshbag amendments (quartz-only, apatite or urea).
429
430
431
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432 Table 1. Mean of the fungal production in different treatments (Pk) estimated by Model 1. The Highest
433 Density Intervals (HDI, Kurshke and Liddel, 2018) represent the boundaries of each estimate at
434 different degrees of confidence.
Fertilization and
Mean fungal
HDI low
HDI high
HDI low
HDI high
amendment
production (g m2 day-1) (95%)
(95%)
(90%)
(90%)
control/apatite
0.094
0.072
0.117
0.075
0.113
control/urea
0.129
0.103
0.156
0.107
0.152
control/quartz
0.061
0.045
0.079
0.047
0.076
phosphorous/apatite
0.038
0.028
0.05
0.029
0.048
phosphorous/urea
0.079
0.059
0.1
0.062
0.096
phosphorous/quartz
0.035
0.026
0.045
0.027
0.043
435
436
437
3.3 Seasonal effect (Model 2)
438
The effect of seasonality as described by β had a positive effect on the predicted
439
fungal production and this effect was highest in July and decreased over time.
440
Moreover, the effect of β on fungal production differed depending on the fertilization
441
and on the meshbag amendment (Fig 5).
442
443
For example, in July the model suggests a seasonal effect increasing the predicted
444
fungal production by up to 5 times in the quartz meshbags from the P-fertilized plots
445
and up to 2.5 times in the urea meshbags in the control plots in comparison with the
446
apatite bags from the P-fertilized plots where season had no effect on fungal
447
production. The positive effect of sampling season on the fungal production, as
448
identified by the model, decreased in general with time and at the end of the growing
449
season (October and November) 𝛽 had the same effect on all the samples
450
independently from the treatment (fertilization and meshbag amendment).
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451
Even though the 𝛽 probability distributions of the different treatments were not
452
significantly different, the effect of the season on biomass production was important
453
and when we decompose fungal production by seasonality (P´k), the differences in
454
fungal production between P fertilized and control plots and between the meshbag
455
amendments are present only early in the season (July, August) and disappear in
456
September October and November (Fig 6).
457
458
459
Figure 5: Seasonality effect on biomass production expressed by the 𝛽 parameter for the different
months of the growing season.
22
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460
461
Figure 6: Probability distribution of P´k (g m2 day-1) for the different months of the growing season.
462
463
464
465
466
467
468
469
470
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471
4 Discussion:
472
473
4.1 Effect of P fertilization on fungal biomass production and turnover
474
In support of our first hypothesis, fungal biomass production declined in response to P
475
fertilization in all meshbag amendments (Fig 4a). These results contrast with those of
476
Almeida et al. (2018) who tested the effect of P fertilization on the fungal standing
477
biomass in the same plots as in the present study. This contrast is not depending on
478
variation in turnover rates between control and P fertilized plots since mortality was
479
not significantly affected by fertilization as shown in the current results. In the present
480
study, P had a negative effect on the fungal standing biomass in most of the
481
incubation periods (Fig 3). The fact that more incubation periods and a larger number
482
of bags were used makes the present study more reliable. Thus, the standing biomass
483
of one given incubation time might not truly reflect the effect of fertilization on fungal
484
growth. The use of the sequential incubation method and the mathematical model
485
allowed us to have a more robust estimate of the effect of P fertilization on the
486
extramatrical mycelium in this forest. P as a nutrient regulating fungal growth in
487
boreal forest was not reported before.
488
489
Fertilization experiments have been largely used to evaluate the effect of soil fertility
490
and nutrient status of the trees on carbon allocation and EMF production (Bahr et al.,
491
2015; Ekblad et al., 2013). However, studies on the effect of nutrient additions on
492
EMF in boreal forests have predominantly focused on N fertilization (Leppälammi-
493
Kujansu et al., 2013) probably because N is the most common limiting nutrient in
494
boreal forests (Högberg et al., 2017). Therefore, the effects of P additions alone on
495
boreal forests have not been widely tested. Due to the steep increase in anthropogenic
24
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496
C and N inputs relative to P inputs, plant nutrient stoichiometry can be altered and
497
lead to unbalanced nutrition and lead to P limitation (Jonard et al., 2015; Peñuelas et
498
al., 2013). Indeed, P fertilization enhanced tree growth in the forest where this study
499
was performed as reported by Almeida et al. (2019).
500
Belowground carbon allocation is expected to be reduced by P fertilization when the
501
system is P limited (Gower & Vitousek 1989; Keith et al. 1997) leading to a decrease
502
in EMM production (Treseder, 2004). We propose that the decreased fungal
503
production in the P-fertilized plots in our study is a result of a decrease in
504
belowground C allocation due to alleviated P limitation that reduced tree dependency
505
on EMF for P foraging and acquisition.
506
507
This reduction in fungal production was not trivial and P fertilization decreased the
508
predicted fungal production to a third in comparison with the fungal production of a
509
forest of similar age estimated by Hagenbo et al. (2017) (0.099 g m2 day-1). More
510
studies on the effect of P fertilization alone in northern forested ecosystems receiving
511
high levels of N deposition should be performed to test if P-limitation is widespread
512
in these ecosystems as reported in this single forest.
513
514
A decrease in EMF production caused by fertilization might reflect a change in the
515
fungal communities. When there is a decrease in belowground C allocation, some
516
EMF species that require less C for growth and produce lower biomass relative to
517
other members of the community might be selected. In the previous study in the same
518
research forest (Almeida et al., 2019), EMF fungal communities from soil and
519
meshbag samples significantly changed after P fertilization and P + N fertilization
520
respectively. In particular, the most abundant EMF species Tylospora asterophora
25
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521
increased when the plots were fertilized with P or P + N. Tylospora asterophora, a
522
short exploration type (Agerer & Raidl, 2004), is expected to produce less biomass
523
than species with long exploration mycelia. Therefore, it is possible than an increase
524
of this species relative abundance in the meshbags of the present study might be
525
related to the lower growth detected in the P fertilized plots. It is also expected that
526
turnover rates vary depending on the species traits of the EMF community (Ekblad et
527
al., 2016). For example, certain traits like rhizomorphs are expected to have longer
528
life span in comparison with smooth and short exploration type mycelium (Pritchard
529
et al., 2008; Ekblad et al., 2016). The significant increase of T. asterophora after P
530
fertilization could increase the overall mycelial turnover rate in these. However, there
531
was not a detectable effect on the turnover rates between control and P fertilized plots.
532
In a tree age chronosequence study in a boreal forest in central Sweden, Hagenbo et
533
al. (2018) reported no clear pattern in exploration types despite a significant shift in
534
fungal community composition and turnover with forest age. This suggests that
535
factors other than exploration types are also important to explain turnover rates.
536
Species-specific traits like mycelial life span, the degree of internal autolysis and the
537
amount of melanin in cell walls could potentially affect biomass turnover in EMF
538
communities (Hagenbo et al., 2018; Fernandez et al., 2013).
539
540
4.2 Effect of nutrient amendment on biomass production and turnover
541
Both nutrient amendments (urea and apatite) increased EMF production in
542
comparison with the quartz-only meshbags in the control plots. This is consistent with
543
mesocosm experiments that have shown that when organic (Wallander & Pallon,
544
2005; Leake et al., 2001; Bending & Read 1995 ) and mineral nutrient patches (Smits
545
et al., 2012 & Leake et al., 2008) are colonized by EMF, mycelial branching and
26
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546
proliferation increase to explore the nutrient patch. In support of our hypothesis,
547
apatite amendment increased EMF production in comparison with the pure quartz
548
bags but only in the control plots. Our results are consistent with the view that trees in
549
the control plots are P limited, and that they allocate more resources to the EMF when
550
exploring a P source like apatite. When P limitation is alleviated by fertilization
551
however, there is probably a decrease in C allocation to the root symbionts which
552
could cause the reduced EMF colonization in the apatite bags. This is supported by
553
other studies reporting that apatite amendment increases EMF standing biomass in
554
meshbags under P-poor conditions (Rosenstock et al., 2016; Berner et al., 2012; Hedh
555
et al., 2008; Hagerberg et al., 2003). In a fertilization study in nearby plots in the same
556
forest, Bahr et al., (2015) showed that apatite addition stimulated EMF standing
557
biomass in mesh bags, in control and in N-fertilized plots, but when N was added in
558
combination with P, on the other hand, no significant differences were found between
559
apatite amended and pure-quartz bags. All together these results provide evidence that
560
EMF growth is responsive to P nutrient patches, but this response is depended on the
561
P demand of the host.
562
563
From the two nutrient amendments, urea had the highest effect on fungal growth and
564
both in the control and P-fertilized plots. From a phytocentric point of view it could
565
be expected that EMF growing on a P rich source like apatite are rewarded with more
566
C from the P limited trees than EMF colonizing N bags. The stronger response of
567
EMF growth to the N nutrient patches than to P nutrient patches in the P-limited
568
control plots suggests that even though the forest is limited by P, N still has an
569
important effect on the growth of EMM.
570
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571
It is possible that P limitation results in a general increase in C allocation to the root
572
symbionts and the C invested by the tree is delivered indiscriminately among its
573
fungal symbionts, independently of the nutrient patch they are colonizing.
574
Probably this is not surprising since N is needed by fungus and plant alike and in
575
order to produce biomass to forage for P and enzymes to mineralize it, EMF requires
576
N. Thus, N uptake can improve the P nutrition of the mycorrhizal system and positive
577
feedback between plant and fungus might happen.
578
579
Despite the strong effect of N patches on fungal growth, P fertilization decreased
580
growth in all meshbags independent of the amendment. EMF communities in forests
581
are diverse and composed of species with different abilities to mineralize the different
582
nutrients present in the soils (Lilleskov et al., 2011). By amending the meshbags with
583
different nutrient types, fungal communities are selected depending on the nutrient
584
added (Almeida et al., 2019; Rosenstock et al., 2016). The consistent effect of P
585
fertilization on both nutrient patches and even in the barren quartz-only bags suggests
586
that P fertilization affects growth of different EMF communities alike and reduces
587
nutrient foraging for both N and P. This is consistent with the idea that alleviated P
588
limitation results in a general decrease of C delivered to the roots and the mycorrhizal
589
symbionts.
590
591
Previous studies on EMF growth have focused on fungal biomass collected from
592
meshbags filled with acid washed sand (see Hagenbo et al. 2021; Hagenbo et al. 2017;
593
Ekblad et al 2016). However, since the pure quartz mesh bags are devoid of nutrients
594
(except probably for dissolved organic material entering the bags during incubation),
595
they might underestimate EMF production in soils. Moreover, in soils most of N and
28
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596
P are heterogeneously distributed in nutrient patches (Hodge, 2006). For this reason,
597
amending the meshbags made possible to imitate the soil nutrient conditions that
598
influence EMF growth in forests and to understand how the nutrient regimes (both as
599
inorganic nutrient fertilization and as nutrient patches) affect EMF production. In fact,
600
the EMF growth in this study was influenced both by the nutrient at the hyphal front
601
(N and P amendment) and by the C provided by the roots (as shown by the effect of P
602
fertilization).
603
604
There were not differences in mycelium turnover between the different meshbag
605
amendments. This contrast with previous studies showing that the nature of a nutrient
606
patch could also affect hyphal turnover (Ekblad et al., 2013; Jansa et al., 2011).
607
Mineral substrates like feldspar have been shown to maintain fungal growth for up to
608
15 weeks (Rosling et al., 2004), while organic nutrient patches have been shown to
609
sustain fungal growth for around 5 weeks (Bending & Read 1995). Therefore, organic
610
substrates like urea are expected to be quickly depleted in soils. As a result, the EMF
611
hyphae is expected to autolyse and transfer the nutrients to other locations of the
612
exploring mycelium faster than during the slow weathering of mineral substrates like
613
apatite (Ekblad et al., 2013 ; Jansa et al., 2011). Therefore, it should be expected that
614
the apatite bags show lower turnover rates than the urea bags. In the present study
615
however, we could not detect differences between the two nutrient patches. The
616
material used to amend the urea meshbags in this study is methyleneurea which is a
617
slow N release molecule. Thus, methylene urea is hydrolyzed to ammonium at a
618
slower rate than the urea molecules (Högberg et al., 2020). Therefore, even if there is
619
evidence that some EMF species can directly consume urea (Morel et al., 2008;
29
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620
Yamanaka, 1999), these slow releasing nutrient sources might require a more
621
persistent mycelium than other organic sources.
622
623
Additionally, previous mesocosm experiments have shown that when EMF mycelium
624
grows on sand, longevity is enhanced in comparison with EMF growing on nutrient
625
patches (Wallander & Pallon 2005). Nutrient patches enhance growth and metabolic
626
activity of EMF, which may enhance turnover rates. For example, Bidartondo et al.
627
(2001) tested ectomycorrhizal growth response to apatite and ammonium in growth
628
chambers with EMF colonized Pinus muricata seedlings. It was found that apatite
629
and ammonium addition increased the respiration rates of EMF, which could be taken
630
as an indication of higher metabolic activity and probably higher mortality. Thus, it
631
can be expected that EMF growing on the quartz bags have lower turnover than the
632
mycelium colonizing the nutrient amendments, but this was not the case in this study.
633
These discrepancies relating EMF turnover rates between the current and previous
634
studies might be caused by shortcomings on the sequential incubation method used
635
for the model in this paper. This method relies on the premise that the sum of the
636
biomass from meshbags incubated for short continuous periods should exceed the
637
biomass from meshbags incubated from a long incubation time. However, in a
638
number of cases the mycelial biomass from a long incubation period was greater than
639
the sum of the consecutive shorter intervals. This could be caused by a delay or a lag
640
phase in fungal colonization inside the bags. It is possible that when a meshbag was
641
collected and the same hole was used to replace a new bag (Fig 2) there was a lag
642
phase before the hyphae could colonize the newly placed meshbag (Wallander et al.,
643
2013). Thus, those data points could have created noise in the data making the
644
turnover estimates less robust. In any case, if turnover in the EMF communities
30
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645
colonizing the nutrient amended bags is higher (as suggested by previous studies), and
646
was underestimated in the current study, then the high standing biomass measured in
647
the urea and apatite bags can only be explained by even higher EMF production than
648
the predicted in these results.
649
650
4.3 Seasonal effects on fungal growth
651
The general assumption of Model 1 is that fungal growth occurs at a constant rate.
652
However, this approximation has some limitations, since seasonality usually affects
653
the amount of C allocated to the roots (Coutts & Nicoll, 1990) and consequently EMF
654
root colonization (Walker et al., 1986). Indeed, the standing fungal biomass in the
655
mesh bags peaked in July and decreased over autumn (Fig 2). In this paper Model 2
656
allowed the predicted fungal growth to vary both with seasonality and with the
657
treatments (P fertilization and meshbag amendment). The introduction of these
658
different dependencies in the model allowed us to test for the interactions between
659
treatment and seasonal effects. It must be noted that the predicted fungal growth
660
resulting from Model 1 is not incorrect and truly reflects the fungal growth
661
differences between the treatments. However, by including seasonality in Model 2, we
662
could detect that those differences predicted earlier were highly dependent on the
663
season. Indeed, fungal growth not only increased early in the season, but the
664
magnitude of this increase depended on the treatments (Fig 5). Therefore, the
665
differences in biomass production between the fertilization regime and meshbag
666
amendments were significant only early in the season (Fig 6).
667
668
The fungal biomass seasonal peak reported in the current paper contrasts with
669
previous studies that have reported that the standing biomass in meshbags collected
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670
from a Pinus sylvestris (Hagenbo et al., 2021; Wallander et al., 2001), Pinus pinaster
671
(Hagenbo et al., 2021) and Picea albies (Wallander et al., 2001) forests was higher
672
during the autumn season. However, in a study performed in the same experimental
673
area as the present study, Wallander et al. (2013) found that the standing biomass in
674
September-October incubations was lower than the standing biomass in July-August
675
incubations. It has been reported that different EMF species have different seasonal
676
peaks (Castaño et al., 2017; Iotti et al., 2014; De la Varga et al., 2013) which could
677
explain the differences in fungal growth between previous studies and the current
678
experiment. Our results are also consistent with those from Coutts & Nicoll (1990)
679
who found that the mycelium extension of Laccaria proxima and Telephora terrestris
680
inoculated in Picea sitchensis peaked during July and decreased in autumn. The
681
mycelial extension was associated with soil temperature, which peaked early in the
682
growing season.
683
684
It could be also possible that non-mycorrhizal fungi had an important contribution to
685
the fungal growth detected in the current study. The meshbag system favors the
686
growth of EMF over non-mycorrhizal fungi as it has been shown in some studies
687
(Almeida et al., 2018; Rosenstock et al., 2016; Berner et al., 2012) which might
688
suggest that fungal growth in this study is influenced mostly by EMF. However, it has
689
been shown that the shorter the time period a meshbag remains underground the
690
higher the proportion of non-mycorrhizal fungi inside the bags (as measured by the
691
proportion of non-mycorrhizal DNA in Hagenbo et al., 2018). Non-mycorrhizal fungi
692
growth has been reported to respond positively to temperature (Pietikäinen et al.,
693
2005) which might imply that during the warmer months of July and August
694
filamentous non-mycorrhizal fungi growth was promoted and there was a higher
32
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695
colonization of this fungal guild inside the meshbags. Even so, the effects of the P
696
fertilization and meshbag amendment on fungal growth were higher early in the
697
season which might imply that the seasonal effect seen in the current study is
698
explained mostly by EMF as it was discussed previously.
699
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In conclusion, EMF production was strongly reduced when P was added to the
701
forests, suggesting a decline in belowground C allocated by the trees when the P
702
limitation was alleviated. This decline affected not only the foraging for P (apatite)
703
but also foraging for N (urea). The strong negative effect of P fertilization on EMF
704
production suggests a central role of P in regulating EMF biomass production in N
705
rich forests. Moreover, the effect of the reduced belowground C allocation and the
706
nutrient patches on EMF growth was significant only in the warmest months of the
707
growing season suggesting an important effect of seasonality on EMF growth
708
dynamics and nutrient uptake.
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