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Record W7028068558

Drivers of Holocene Carbon Uptake and Release in Peatlands of the Hudson Bay Lowlands, Canada

2021· dissertation· en· W7028068558 on OpenAlexaboutno aff

Bibliographic record

VenueTSpace (University of Toronto) · 2021
Typedissertation
Languageen
FieldEnvironmental Science
TopicPeatlands and Wetlands Ecology
Canadian institutionsnot available
Fundersnot available
KeywordsPeatHoloceneTestate amoebaeBogCarbon sinkClimate changeCarbon cycleWetlandWater tableVegetation (pathology)
DOInot available

Abstract

fetched live from OpenAlex

Northern peatlands are a key component of the terrestrial carbon cycle, acting as both a source and sink of carbon. Therefore, to predict impacts from anthropogenic climate change and create effective land management policies, constraining how environmental factors impact peatland carbon fluxes is critical, especially in peatland-rich regions such as the Hudson Bay Lowlands (HBL), Canada. This thesis aims to understand how local-scale factors impacted Holocene carbon uptake and release in the HBL using paleoecological and geochemical analyses of radiocarbon-dated peat cores. Paleoecological analyses of a site on the southern HBL margin demonstrate that landscape position controls local hydrology and can subsequently limit Holocene carbon accumulation rates (CARs). This record also demonstrates a summer bias in temperature and validates pH reconstructions from lipid biomarker proxies. Paired treed fen and bog sites from the western HBL margin show markedly high carbon masses owing to deep peat accumulation with old initiation ages. Mean testate amoeba trait values reflect hydrology and food web structure and are also influenced by vegetation shifts and peatland type. Further, mixotrophic taxa are not related to higher millennial-scale CARs, suggesting a minor role for their primary production in long-term carbon storage. The above records were synthesized with other hydrological records derived from testate amoebae across the HBL to reconstruct paleo-methane fluxes via a linear regression model developed from modern relationships between methane fluxes and water table depths. Land availability controlled by glacial isostatic adjustment was an important control on Holocene emissions when fluxes were scaled to regional emissions. The combined hydrological reconstructions also suggest that peatlands were drier under warmer Middle Holocene conditions. A charcoal record collected from the western HBL margin supports drier conditions, as warmer Middle Holocene conditions were related to higher fire frequency. Although higher fire frequency did not have a significant impact on millennial-scale CARs, carbon loss from combustion was potentially doubled, which has implications for atmospheric carbon budgets. Overall, this thesis advances our understanding of the complex interplay between climate and local processes in long-term carbon dynamics that is of fundamental importance for conservation priorities and constraining future carbon emissions.

Fetched live from OpenAlex and de-inverted. Abstracts are not stored in this database: the inverted indexes are 8.6 GB of the frame’s 9.3 GB of text, and the host has 13 GB free.

How this classification was reachedexpand

Full frame machine prediction

Teacher imitation

Not calibrated prevalence, not ground truth. Human validation pending. The Gemma side is a direct model label for every work in the frame, read from the title-only record. The Codex side is a classifier learned from the 10,348 direct Codex labels and calibrated to design-weighted sample rates; fields without enough sample support carry no Codex call. Candidate is the union of the two sides; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels.

metaresearch head score (Codex)0.000
metaresearch head score (Gemma)0.001
Version: metacan-v3-hybrid-931329e0061cValidation status: machine_predicted_unvalidated
Candidate categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.017
Threshold uncertainty score0.122

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.001
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0010.002
Science and technology studies0.0010.001
Scholarly communication0.0010.000
Open science0.0000.001
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0010.000

Machine scores (provisional)

The two teacher heads of the student model, read on this work. A score orders the frame for review; it never asserts a category, and the validation status ships verbatim with every row.

Baseline scores from an immature model (maturity gate not passed, 7 training rounds). Scores rank; they never assert a category.

Opus teacher head0.004
GPT teacher head0.185
Teacher spread0.181 · how far apart the two teachers sit on this one work
Validation statusscore_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from it

Classification

machine, unvalidated

Machine predicted; a candidate call from one source (direct Gemma or distilled Codex), not a consensus.

The models applied no category: nothing in the taxonomy fit this work.
Study designObservational
Domainnot available
GenreEmpirical

How this classification was reached, model by model and score by score, is at the end of the page under "How this classification was reached".

Quick stats

Citations0
Published2021
Admission routes1
Has abstractyes

Explore more

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