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Record W7041965183

Paleolimnological Assessment of Algal Production During the Holocene Thermal Maximum from the Sediment Record of a Boreal Lake in Northeastern Ontario

2017· dissertation· en· W7041965183 on OpenAlexaboutno aff

Bibliographic record

VenueQSpace (Queen's University Library) · 2017
Typedissertation
Languageen
FieldEarth and Planetary Sciences
TopicGeology and Paleoclimatology Research
Canadian institutionsnot available
Fundersnot available
KeywordsHoloceneDiatomBorealPollenSedimentClimate changePaleolimnologyAlgaeTaiga
DOInot available

Abstract

fetched live from OpenAlex

The Holocene Thermal Maximum (HTM) was a period of enhanced warmth during the early-to- mid Holocene period largely caused by enhanced solar insolation. In northwestern Ontario, the HTM was characterized by a lower abundance of Picea pollen and an increase in Cupressaceae and Ambrosia pollen. Pollen-based inferences suggest HTM temperatures were elevated by approximately 2-3°C, and lake levels were regionally lower than today, suggesting warmer and more arid conditions than today. This warming resulted in increased algal production and associated cyanobacteria blooms in lakes in northwestern Ontario. In northeastern Ontario, climate projections suggest the HTM was 2-3°C warmer. However, to date, there has been little research on the impact of the HTM on boreal lakes in northeastern Ontario, creating a gap in our understanding of the effects of climate change on aquatic ecosystems. A pollen study conducted previously suggests the HTM was warm and wet in northeastern Ontario, and his pollen framework is used to infer past changes in climate for this study. In this thesis a paleolimnological approach is used to assess how algal assemblages changed over the Holocene from a sediment core from Charland Lake, a boreal lake in northeastern Ontario near Timmins, and if the proxy data supports a conclusion of higher levels of algal production during the warmer HTM. A carbon-dated sediment core taken from the deep-water flat central basin of Charland Lake was examined for sedimentary pigments, diatom assemblages, and percent organic matter. Statistical analysis revealed diatom and pigment assemblages and concentrations varied throughout the Holocene, broadly coinciding with changes in the regional climate as inferred from past research. Lake-water production was low after deglaciation and through the HTM, potentially attributable with an unstable landscape and associated contributions of fine clastic material to the lake. Lake-water production was highest during the post-HTM period (~4460-2590 cal yr BP), but before the onset of modern conditions. The results also suggest that the last ~4500 years had higher levels of lake-water production, than during the HTM, likely related to interactions that depend on location and landscape characteristics. In comparison to northwestern Ontario, changes in the proxies of production were not very large.

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)0.000
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 score0.055
Threshold uncertainty score0.111

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0010.002
Science and technology studies0.0020.000
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 head0.011
GPT teacher head0.208
Teacher spread0.197 · 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
Published2017
Admission routes1
Has abstractyes

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