Abstract
High levels of nitrogen (N) deposition might result in a transition from N to phosphorus (P) limitation in high latitude forests. This
could have fundamental consequences for forest production, nutrient acquisition and nutrient leaching.
I studied a Norway spruce forest in a region of high N deposition in southwest Sweden and added N, P or N+P to force the
system to N or P limitation. I studied tree growth and foliar nutrient concentration. Also, using ingrowth meshbags, I followed
ectomycorrhizal (EMF) production, foraging for N and P patches (urea and apatite) and community composition.
I found that tree production was limited by P. Furthermore, P fertilization reduced EMF production indicating that EMF biomass
production was stimulated by P-limiting conditions. Apatite had a positive effect on EMF production when the system was Plimited.
P fertilization reduced foraging for nutrients by EMF, also for N rich urea. P had a stronger effect on the composition of
EMF communities than N, suggesting that P nutrition had a larger impact on belowground carbon (C) allocation than N in this
ecosystem. Furthermore, certain EMF species responded positively to apatite under P limiting conditions, which might have
increased mobilization of P from this source.
To enhance my understanding of P mobilization from different P compounds by EMF, I studied one species, Paxillus involutus,
under more controlled conditions in the laboratory. P. involutus is adapted to high N deposition levels and has a documented
capability to take up P from poorly soluble sources. I found that P. involutus was able to take up P from apatite, P bound to
goethite and from phytic acid. Moreover, I found that iron-reducing activity was produced when these sources were provided
but not when the fungus was provided with soluble P (phosphate). One possible interpretation to this result was that iron (Fe)
reduction is a way for the fungus to prevent that newly liberated phosphate ions are captured by Fe3+ and became unavailable
for uptake.
In conclusion, the high production of EMF found in P-limited forest decline when P is added, probably due to reduced
belowground C allocation when less foraging for P is needed. EMF communities are strongly regulated by P in these forests
and species better adapted for P foraging are probably selected for under these conditions.
could have fundamental consequences for forest production, nutrient acquisition and nutrient leaching.
I studied a Norway spruce forest in a region of high N deposition in southwest Sweden and added N, P or N+P to force the
system to N or P limitation. I studied tree growth and foliar nutrient concentration. Also, using ingrowth meshbags, I followed
ectomycorrhizal (EMF) production, foraging for N and P patches (urea and apatite) and community composition.
I found that tree production was limited by P. Furthermore, P fertilization reduced EMF production indicating that EMF biomass
production was stimulated by P-limiting conditions. Apatite had a positive effect on EMF production when the system was Plimited.
P fertilization reduced foraging for nutrients by EMF, also for N rich urea. P had a stronger effect on the composition of
EMF communities than N, suggesting that P nutrition had a larger impact on belowground carbon (C) allocation than N in this
ecosystem. Furthermore, certain EMF species responded positively to apatite under P limiting conditions, which might have
increased mobilization of P from this source.
To enhance my understanding of P mobilization from different P compounds by EMF, I studied one species, Paxillus involutus,
under more controlled conditions in the laboratory. P. involutus is adapted to high N deposition levels and has a documented
capability to take up P from poorly soluble sources. I found that P. involutus was able to take up P from apatite, P bound to
goethite and from phytic acid. Moreover, I found that iron-reducing activity was produced when these sources were provided
but not when the fungus was provided with soluble P (phosphate). One possible interpretation to this result was that iron (Fe)
reduction is a way for the fungus to prevent that newly liberated phosphate ions are captured by Fe3+ and became unavailable
for uptake.
In conclusion, the high production of EMF found in P-limited forest decline when P is added, probably due to reduced
belowground C allocation when less foraging for P is needed. EMF communities are strongly regulated by P in these forests
and species better adapted for P foraging are probably selected for under these conditions.
Original language | English |
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Qualification | Doctor |
Awarding Institution |
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Supervisors/Advisors |
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Award date | 2019 Feb 8 |
Place of Publication | Lund |
Publisher | |
ISBN (Print) | 978-91-7753-952-0 |
ISBN (electronic) | 978-91-7753-953-7 |
Publication status | Published - 2019 Jan |
Bibliographical note
Defence detailsDate: 2019-02-08
Time: 10:00
Place: Blå hallen, Ekologihuset, Sölvegatan 37, Lund
External reviewer(s)
Name: Andrea Polle
Title: Professor
Affiliation: University of Göttingen, Tyskland
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Subject classification (UKÄ)
- Natural Sciences
- Biological Sciences
Keywords
- Phosphorus and nitrogen limitation, nitrogen deposition, ectomycorrhizal fungi, community composition,apatite, Paxillus involutus