Document Type

Thesis

Degree Name

Master of Science (MSc)

Department

Biology

Program Name/Specialization

Integrative Biology

Faculty/School

Faculty of Science

First Advisor

Dr. Jennifer Baltzer

Advisor Role

Supervisor

Second Advisor

Dr. Cory Wallace

Abstract

Warming temperatures are exacerbating permafrost thaw disturbances in the Arctic. Permafrost thaw disturbances are facilitating tall, deciduous shrub expansion. However, potential productivity differences between shrubs that colonize disturbed areas and those in undisturbed tundra remain understudied. More productive shrubs optimize for fast growth over leaf longevity, meaning they may produce more abundant and higher quality litter which could accelerate decomposition rates and lead to faster nutrient cycling. Faster nutrient cycling could create a positive feedback loop between shrubs and soil, maintaining greater ecosystem productivity. I measured in situ soil characteristics and physiological and structural shrub functional traits for green alder (Alnus alnobetula) and dwarf birch (Betula glandulosa) growing in polygonal terrain (troughs and centers) and thaw slumps (within the thaw slump or an undisturbed control) in the low Arctic tundra of Northwest Territories, Canada. I also conducted a laboratory litter incubation experiment to assess the potential of accelerated nutrient-cycling in disturbances. I found that soil characteristics were altered in disturbances compared to controls. Thaw slumps displayed dramatic differences compared to undisturbed tundra, and polygonal terrain troughs had deeper active layer thickness than more-stable centers. Shrub traits did not differ between polygon centers and polygon troughs, however, in thaw slumps shrubs were significantly more productive than in undisturbed tundra. I found greater rates of litter decomposition in polygon troughs compared to centers, and greater decomposition of litter from thaw slumps compared to litter from undisturbed tundra regardless of the incubation substrate (disturbed vs. undisturbed). My results suggest that the effects of ice-wedge degradation in polygonal terrain troughs may be limited to increases in active layer thickness and litter decomposition, while large-scale thaw slump disturbances will increase soil nutrient availability and active layer thickness, stimulate productive shrub trait expression, and enhance decomposition rates of shrub litter. The increase in shrub productivity in thaw slumps marks a shift in ecosystem structure and function, while increases in decomposition may lead to faster nutrient cycling in polygonal terrain troughs. My findings suggest positive feedback between thaw slumps, shrub productivity, and decomposition which could reinforce or enhance the dominance of tall shrubs and contribute to tundra shrub expansion.

Convocation Year

2025

Convocation Season

Spring

Download

Available for download on Saturday, February 07, 2026

Share

COinS