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Record W2767674308 · doi:10.1002/jqs.2997

Development, evolution and drainage of glacial Lake Naskaupi during the deglaciation of north‐central Quebec and Labrador

2017· article· en· W2767674308 on OpenAlex
Hugo Dubé‐Loubert, Martin Roy

Why this work is in the frame

A frame that forgets how it found something cannot be audited. These are the routes that admitted this work.

affAt least one author lists a Canadian institution in the pinned OpenAlex snapshot.
fundA Canadian funder is recorded on the work.
aboutThe title or abstract carries a Canadian signal from the geographic lexicon.

Bibliographic record

VenueJournal of Quaternary Science · 2017
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeology and Paleoclimatology Research
Canadian institutionsUniversité du Québec à Montréal
FundersNatural Sciences and Engineering Research Council of Canada
KeywordsDeglaciationGeologyGlacial lakeMeltwaterShelf iceGlacial periodLandformPhysical geographyIce sheetStage (stratigraphy)Drainage basinHydrology (agriculture)GeomorphologyOceanographyCryosphereIce streamSea icePaleontologyGeography

Abstract

fetched live from OpenAlex

ABSTRACT Deglaciation of north‐central Quebec and Labrador led to the development of large ice‐dammed lakes in river valleys surrounding Ungava Bay. These lakes are poorly understood due to uncertainties in the regional pattern of ice retreat. Lake Naskaupi occupied the George River valley where systematic mapping of glacial landforms and extensive elevation measurements of shorelines reveal a complex history characterized by multiple lake levels. Our reconstruction documents three well‐defined lake levels marking extensive lake stages. Additional lake levels are poorly developed and relate to short‐lived, transient lake stages. During its main stage (N2′), Lake Naskaupi consisted of two separate basins that evolved independently for some time. This configuration resulted from the persistence of cold‐based ice conditions during the deglaciation that caused the retreating ice margin to remain in the middle section of the river valley. The presence of this ice dam is supported by large‐scale outburst flood deposits that record the abrupt drainage of the southern Naskaupi basin. The magnitude of the elevation changes between the remaining lower lake levels suggests the occurrence of at least one other major drawdown before the final lake drainage. Reconstruction of the N2′ lake stage provides a minimum meltwater volume estimate for the lake.

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.

Full frame distilled prediction

Teacher imitation

Not calibrated prevalence, not ground truth. Human validation pending. Learned from the 10,348 direct Codex labels and 10,348 direct Gemma labels. Candidate is the union of thresholded teacher heads; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels or direct frontier model labels.

metaresearch head score (Codex)0.001
metaresearch head score (Gemma)0.000
Version: codex-gemma-dda1882f352aValidation 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 score0.084
Threshold uncertainty score0.932

Codex and Gemma teacher scores by category

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

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 head0.015
GPT teacher head0.244
Teacher spread0.229 · 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