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Record W4251554341 · doi:10.1002/essoar.10500355.1

Using Postglacial Eolian Dune Depositional Ages from Northeast Alberta, Canada to Assess the Likelihood of Northwestward Routing of Lake Agassiz Overflow at the Onset of the Younger Dryas Cold Event

2019· preprint· en· W4251554341 on OpenAlexafffundabout
Kennedy Munyikwa

Bibliographic record

Venuenot available
Typepreprint
Languageen
FieldEarth and Planetary Sciences
TopicGeology and Paleoclimatology Research
Canadian institutionsAthabasca University
FundersAthabasca University
KeywordsYounger DryasGeologyOceanographyGlacial periodArcticGlacial lakeVarveHolocenePaleontologySediment

Abstract

fetched live from OpenAlex

The release of freshwater into the North Atlantic by glacial Lake Agassiz towards the end of the last glacial period is hypothesized to have triggered the Younger Dryas (Y.D.) cold event of 12.9 -11.7 ka ago. It is thought that the influx of freshwater into the Atlantic weakened meridional overturning circulation, impeding heat transport to the northern latitudes. A subject of debate at present is how the freshwater released from Lake Agassiz was routed to the ocean. One suggestion is that the retreat of the Laurentide Ice Sheet (LIS) from the Lake Superior Basin allowed water from Lake Agassiz, which was flowing south to the Gulf of Mexico, to be redirected eastward via the St Lawrence River to reach the Atlantic. Reported surface exposure ages indicate that the St Lawrence River route became available between 13.0 and 12.7 ka ago, timing that is coincident with the onset of the Y.D. event. An alternative route for the drainage from Lake Agassiz is that it flowed northwestwards to the Arctic Ocean via the Mackenzie River in northwest Canada. This suggestion has been affirmed by some modeling studies that found that meridional overturning in the North Atlantic would have been weakened more significantly if freshwater was introduced via the Arctic. A flow path, and deposits that have been identified on the Canadian Arctic Coastal Plain have yielded luminescence ages indicating that a major flood event occurred sometime between 13.0 and 11.7 ka ago. From that age range, however, it is not possible to ascertain if the flood triggered the Y.D. Thus, in this study, in order to determine a more precise timeline for the northwestward drainage of Lake Agassiz, we collected postglacial eolian dune sands from northeast Alberta, Canada, an area through which water from Lake Agassiz would have had to pass in order to reach the Arctic Ocean. The dune sands were sourced by wind from sediments left behind following the drainage of glacial Lake McConnell which had also been dammed in the region by the LIS. Preliminary luminescence ages obtained from the eolian sands suggest that northeast Alberta was free of both ice and glacial lakes by 13.5-12.5 ka ago. This indicates that flow from Lake Agassiz via the Mackenzie River cannot be excluded as a trigger for the Y.D. since the northwestward drainage path appears to have also been available at the start of the event.

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)0.001
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 score0.012
Threshold uncertainty score0.090

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0010.001
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0020.003
Science and technology studies0.0020.000
Scholarly communication0.0010.000
Open science0.0010.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0020.000

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 head0.025
GPT teacher head0.251
Teacher spread0.226 · 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
Published2019
Admission routes3
Has abstractyes

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