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Grant: Discovery Grants Program - Individual

Université du Québec à Rimouski

$58,400.00

Tree-ring research in the eastern Canadian taiga

FY 2023-24

Summary
The boreal forest is by far the most important biome of Canada. Boreal vegetation is important for our industry and our way of living. However, the boreal forest is expected to warm rapidly and experience more fires, thus threatening the services it provides. This research aims to use tree-rings to understand the dynamics of the Eastern Canadian taiga under the dominant influence of fire disturbance and climate change and to reconstruct past climate change from ancient subfossil trees. The first objective is to reconstruct the empirical fire interval frequency distribution to quantify how much the North American boreal forest can absorb the fire activity and protect itself by limiting the prevalence of deleterious short fire intervals. Because more severe fire weather conditions are anticipated with climate change, the second objective is to evaluate how this self-protection may collapse due to more severe fires in the future. The third objective is to use X-ray-based latewood density measurements from subfossil trees sampled in lake sediments to develop a temperature reconstruction covering the complete Common Era in the North American boreal forest. This will provide context to evaluate the importance of the current warming trend and will be a long-awaited addition to improve large-scale (e.g. Northern hemisphere) climate reconstructions by international teams. The fourth objective is to quantify the negative impact of volcanism on black spruce productivity across the Eastern Canadian boreal forest during the last millenium. Although tree rings have been used to reconstruct the climatic impact of volcanoes, the impact of volcanoes on tree productivity is unknown, notably for black spruce, the most important tree species in the North American boreal forest and one of the most successful plant species on Earth in terms of standing biomass. The last objective is to share our complete millennial tree-ring database, including all metadata. Overall, this research will contribute important findings and data to anticipate and manage upcoming climate changes and associated forest trajectories.
Program
Discovery Grants Program - Individual
Location
Quebec, Canada
Recipient Type
Academia
Type
Grant
Source
NSERC's Awards Data

As published

Application id
RGPIN-2021-02692
Name nom
Arseneault, Dominique
Department département
Biologie, chimie et géographie - Biologie, chimie et géographie
Organization id
58
Institution établissement
Université du Québec à Rimouski
Province en
Québec
Province fr
Québec
Country en
CANADA
Country fr
CANADA
Fiscal year exercice financier
2023
Competition year année de concours
2021
Award amount
58400
Program id
RGPIN
Program name en
Discovery Grants Program - Individual
Program name fr
Programme de subventions à la découverte - individuelles
Group en
DISCOVERY RESEARCH
Group fr
RECHERCHE AXÉE SUR LA DÉCOUVERTE
Committee code
1506
Committee name en
Geosciences
Committee name fr
Géosciences
Area of application code
400
Area of application group en
Environment
Area of application group fr
Environnement
Area of application en
Environment
Area of application fr
Environnement
Research subject code
4700
Research subject group en
Evolution and ecology
Research subject group fr
Evolution and ecology
Research subject en
Évolution et écologie
Research subject fr
Évolution et écologie
Application title
Tree-ring research in the eastern Canadian taiga
Keyword
Boreal forest; Emergent properties; Lake subfossil trees; Landscape resilience; Landscape resistance; Large-scale patterns and processes; Millennial dendroclimatology; Multiple climate proxies; Wildfire activity
Application summary
The boreal forest is by far the most important biome of Canada. Boreal vegetation is important for our industry and our way of living. However, the boreal forest is expected to warm rapidly and experience more fires, thus threatening the services it provides. This research aims to use tree-rings to understand the dynamics of the Eastern Canadian taiga under the dominant influence of fire disturbance and climate change and to reconstruct past climate change from ancient subfossil trees. The first objective is to reconstruct the empirical fire interval frequency distribution to quantify how much the North American boreal forest can absorb the fire activity and protect itself by limiting the prevalence of deleterious short fire intervals. Because more severe fire weather conditions are anticipated with climate change, the second objective is to evaluate how this self-protection may collapse due to more severe fires in the future. The third objective is to use X-ray-based latewood density measurements from subfossil trees sampled in lake sediments to develop a temperature reconstruction covering the complete Common Era in the North American boreal forest. This will provide context to evaluate the importance of the current warming trend and will be a long-awaited addition to improve large-scale (e.g. Northern hemisphere) climate reconstructions by international teams. The fourth objective is to quantify the negative impact of volcanism on black spruce productivity across the Eastern Canadian boreal forest during the last millenium. Although tree rings have been used to reconstruct the climatic impact of volcanoes, the impact of volcanoes on tree productivity is unknown, notably for black spruce, the most important tree species in the North American boreal forest and one of the most successful plant species on Earth in terms of standing biomass. The last objective is to share our complete millennial tree-ring database, including all metadata. Overall, this research will contribute important findings and data to anticipate and manage upcoming climate changes and associated forest trajectories.