- Author
- Cristina Gasperini
- Promoter
- Pieter De Frenne (UGent)
- Organization
- Abstract
- Forest ecosystems buffer climate extremes and mitigate climate change effects below the canopy by creating a different microclimate which might serve as local refugia for many species under climate warming scenarios. Forest buffering capacity varies greatly depending on forest structure or macroclimatic temperature, and is severely threatened by increasing forest fragmentation and land use change that create more forest edges, whose buffering capacity is lower compare to forest interiors. Worldwide, a significant extent of the total forest area is located next to a forest edge and therefore subjected to strong edge effects. Edge effects are regarded as one of the main drivers of habitat fragmentation impacts on biodiversity. However, our understanding of how the forest respond to this alteration is based almost exclusively on herb layer community studies, although this is not sufficient to understand forest understorey community responses. Particularly, edge effects on the soil seed bank of temperate forests in the context of climate change are scarcely studied. This is a shortcoming as the soil seed bank is a key component of the biodiversity of plant communities and plays a crucial role in forest conservation, population dynamics and forest functioning. The main goal of this research was to assess forest edge effects on soil seed bank composition and diversity along macroclimatic and microclimatic gradients and in relation to climate change. To reach this objective we studied the soil seed bank of ancient European temperate deciduous forests with two field experimental studies (realised soil seed bank) and a greenhouse experiment (potential soil seed bank). Besides quantifying the amount and diversity of seeds stored belowground, we also focused on the germination responses and seedling establishment as the environmental conditions required in these early stages as well as the impacts of environmental changes on them can differ greatly from that of the adults. A deeper knowledge of seed germination and seedlings' development and adaptations to 1 forest microclimate is pivotal as the establishment is a critical phase in the plant life cycle. In the field studies, we focused on two distinct climatic regions and forest types (thermophilous forests of Italy and mesophilous forests of Belgium). We sampled the soil seed bank and then, through the installation of experimental plots in the forest, we translocated the soil from the forest edge to the interior (and vice versa) and from high to low elevation forests (to simulate climate warming). In the greenhouse experiment, we covered a 2300 km latitudinal gradient crossing nine European regions. We compared the persistent soil seed bank collecting soil samples in 90 plots from northern to southern Europe, from low elevation to high elevation forest, from dense to open forests and from the forest edge to the forest interior. Edge effects altered the soil seed bank diversity and composition by increasing the proportion of open habitat and generalist species. However, no significant influence on the proportion of typical forest species was observed. These findings highlight, on the one side, the importance of protecting large forest areas to reduce the inflow of external seeds in the soil seed bank and avoid potential compositional shifts and, on the other side, the ecological value of forest edge microhabitat, which is not unsuitable for the persistence of forest herbs seeds and seedlings. The present amount of typical forest herbs stored as persistent seeds in forests suggests that the contribution of soil seed banks towards the survival of forest species in communities undergoing environmental changes could be substantial. At least in the short term, seed banks are expected to buffer environmental variations induced by the edge effect through the maintenance of belowground species richness and thus through effects on the aboveground community composition. Additionally, simulated climate warming changed both the taxonomic and the functional composition of the realised soil seed bank, with negative consequences on the germination of forest herbs and the increase of warm-adapted species in the realised communities. Climate warming is thus expected to induce compositional 2 and functional shifts in temperate forest understorey communities through constraints in the germination of soil seed bank species. These changes might result in altered forest biodiversity and functioning. With future rising temperatures, dense forest cover and management practices that do not cause the opening of the canopy on a large scale should be adopted. In this way, temperature extremes would be better buffered and the conservation of shade-tolerant forest species of the understorey more likely be assured. Indeed, we found that forest structure affected the germination responses from the seed bank. Specifically, denser canopies promoted forest species regeneration whereas open canopies promoted those of light demanding and generalist species. This PhD research gives a novel perspective on the impact of forest fragmentation, edge effects and climate change on temperate forest ecosystems and provides guidelines on how to preserve biodiversity through the soil seed bank. We suggest that the expected combined negative effects of climate change and edge effects might be partially mitigated in the future by preventing further forest fragmentation, by management of the existing forest edges and by the use of forest management methods that prevent the creation of large clearings. Finally, we provide a complete list of species and relative abundance of the realised and potential soil seed banks along forest edges and interiors of temperate European forests, from Norway to Italy. We believe that this can be an important tool for forest managers oriented to conservation goals. Further, we expect that this knowledge may be a valuable starting point for future studies and a basis for resurveys to monitor the effects of changing climatic conditions on forest ecosystems.
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Citation
Please use this url to cite or link to this publication: http://hdl.handle.net/1854/LU-01HBR5QBZ1YCK0QCNJX8EG7G72
- MLA
- Gasperini, Cristina. The Effects of Macroclimate and Microclimate on Soil Seed Banks in Temperate Forests. Florence University ; Ghent University. Faculty of Bioscience Engineering, 2023.
- APA
- Gasperini, C. (2023). The effects of macroclimate and microclimate on soil seed banks in temperate forests. Florence University ; Ghent University. Faculty of Bioscience Engineering, Florence, Italy ; Ghent, Belgium.
- Chicago author-date
- Gasperini, Cristina. 2023. “The Effects of Macroclimate and Microclimate on Soil Seed Banks in Temperate Forests.” Florence, Italy ; Ghent, Belgium: Florence University ; Ghent University. Faculty of Bioscience Engineering.
- Chicago author-date (all authors)
- Gasperini, Cristina. 2023. “The Effects of Macroclimate and Microclimate on Soil Seed Banks in Temperate Forests.” Florence, Italy ; Ghent, Belgium: Florence University ; Ghent University. Faculty of Bioscience Engineering.
- Vancouver
- 1.Gasperini C. The effects of macroclimate and microclimate on soil seed banks in temperate forests. [Florence, Italy ; Ghent, Belgium]: Florence University ; Ghent University. Faculty of Bioscience Engineering; 2023.
- IEEE
- [1]C. Gasperini, “The effects of macroclimate and microclimate on soil seed banks in temperate forests,” Florence University ; Ghent University. Faculty of Bioscience Engineering, Florence, Italy ; Ghent, Belgium, 2023.
@phdthesis{01HBR5QBZ1YCK0QCNJX8EG7G72,
abstract = {{Forest ecosystems buffer climate extremes and mitigate climate change effects
below the canopy by creating a different microclimate which might serve as local
refugia for many species under climate warming scenarios. Forest buffering
capacity varies greatly depending on forest structure or macroclimatic temperature,
and is severely threatened by increasing forest fragmentation and land use change
that create more forest edges, whose buffering capacity is lower compare to forest
interiors. Worldwide, a significant extent of the total forest area is located next to a
forest edge and therefore subjected to strong edge effects. Edge effects are regarded
as one of the main drivers of habitat fragmentation impacts on biodiversity.
However, our understanding of how the forest respond to this alteration is based
almost exclusively on herb layer community studies, although this is not sufficient
to understand forest understorey community responses. Particularly, edge effects
on the soil seed bank of temperate forests in the context of climate change are
scarcely studied. This is a shortcoming as the soil seed bank is a key component of
the biodiversity of plant communities and plays a crucial role in forest
conservation, population dynamics and forest functioning.
The main goal of this research was to assess forest edge effects on soil seed bank
composition and diversity along macroclimatic and microclimatic gradients and in
relation to climate change. To reach this objective we studied the soil seed bank of
ancient European temperate deciduous forests with two field experimental studies
(realised soil seed bank) and a greenhouse experiment (potential soil seed bank).
Besides quantifying the amount and diversity of seeds stored belowground, we also
focused on the germination responses and seedling establishment as the
environmental conditions required in these early stages as well as the impacts of
environmental changes on them can differ greatly from that of the adults. A deeper
knowledge of seed germination and seedlings' development and adaptations to
1
forest microclimate is pivotal as the establishment is a critical phase in the plant life
cycle. In the field studies, we focused on two distinct climatic regions and forest
types (thermophilous forests of Italy and mesophilous forests of Belgium). We
sampled the soil seed bank and then, through the installation of experimental plots
in the forest, we translocated the soil from the forest edge to the interior (and vice
versa) and from high to low elevation forests (to simulate climate warming). In the
greenhouse experiment, we covered a 2300 km latitudinal gradient crossing nine
European regions. We compared the persistent soil seed bank collecting soil
samples in 90 plots from northern to southern Europe, from low elevation to high
elevation forest, from dense to open forests and from the forest edge to the forest
interior.
Edge effects altered the soil seed bank diversity and composition by increasing the
proportion of open habitat and generalist species. However, no significant influence
on the proportion of typical forest species was observed. These findings highlight,
on the one side, the importance of protecting large forest areas to reduce the inflow
of external seeds in the soil seed bank and avoid potential compositional shifts and,
on the other side, the ecological value of forest edge microhabitat, which is not
unsuitable for the persistence of forest herbs seeds and seedlings. The present
amount of typical forest herbs stored as persistent seeds in forests suggests that the
contribution of soil seed banks towards the survival of forest species in
communities undergoing environmental changes could be substantial. At least in
the short term, seed banks are expected to buffer environmental variations induced
by the edge effect through the maintenance of belowground species richness and
thus through effects on the aboveground community composition. Additionally,
simulated climate warming changed both the taxonomic and the functional
composition of the realised soil seed bank, with negative consequences on the
germination of forest herbs and the increase of warm-adapted species in the
realised communities. Climate warming is thus expected to induce compositional
2
and functional shifts in temperate forest understorey communities through
constraints in the germination of soil seed bank species. These changes might result
in altered forest biodiversity and functioning. With future rising temperatures,
dense forest cover and management practices that do not cause the opening of the
canopy on a large scale should be adopted. In this way, temperature extremes
would be better buffered and the conservation of shade-tolerant forest species of
the understorey more likely be assured. Indeed, we found that forest structure
affected the germination responses from the seed bank. Specifically, denser
canopies promoted forest species regeneration whereas open canopies promoted
those of light demanding and generalist species.
This PhD research gives a novel perspective on the impact of forest fragmentation,
edge effects and climate change on temperate forest ecosystems and provides
guidelines on how to preserve biodiversity through the soil seed bank. We suggest
that the expected combined negative effects of climate change and edge effects
might be partially mitigated in the future by preventing further forest
fragmentation, by management of the existing forest edges and by the use of forest
management methods that prevent the creation of large clearings. Finally, we
provide a complete list of species and relative abundance of the realised and
potential soil seed banks along forest edges and interiors of temperate European
forests, from Norway to Italy. We believe that this can be an important tool for
forest managers oriented to conservation goals. Further, we expect that this
knowledge may be a valuable starting point for future studies and a basis for
resurveys to monitor the effects of changing climatic conditions on forest
ecosystems.}},
author = {{Gasperini, Cristina}},
isbn = {{9789463576185}},
language = {{eng}},
pages = {{XIV, 326}},
publisher = {{Florence University ; Ghent University. Faculty of Bioscience Engineering}},
school = {{Ghent University}},
title = {{The effects of macroclimate and microclimate on soil seed banks in temperate forests}},
year = {{2023}},
}