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Record W355437865

History of Cordilleran Ice Sheet activity recorded in core MD02-2496: Vancouver Island, British Columbia.

2007· article· en· W355437865 on OpenAlexaboutno aff
T. Cosma

Bibliographic record

VenueDeep Blue (University of Michigan) · 2007
Typearticle
Languageen
FieldEnvironmental Science
TopicLandslides and related hazards
Canadian institutionsnot available
Fundersnot available
KeywordsGeologyOceanographyIce sheetCore (optical fiber)ArchaeologyPhysical geographyGeographyEngineeringTelecommunications
DOInot available

Abstract

fetched live from OpenAlex

MD02-2496, a marine core from the continental slope off Vancouver Island, contains detailed late Quaternary Cordilleran Ice Sheet records. Multi-proxy data establish depositional patterns related to glacial phases while stable isotopes allow correlation between Cordilleran Ice Sheet activity and global climatic change. Magnetic susceptibility, color reflectance, and mass accumulation rates (MAR) of lithogenic sediment document the initiation of glaciomarine sedimentation (Fraser Glaciation) at ∼30 Ka. Reduced magnetic susceptibility validates a brief ice retreat ∼23 Ka (19.2 14 C kyrs BP, Port Moody). MARS, grainsize, and cyclic sedimentation suggest the ice margin became proximal to the shelf edge at ∼19 Ka. Spectral analysis of the interval 19 to 17 Ka suggests either lunar or solar forcing of ice sheet instability. Catastrophic ice sheet retreat is indicated by the gradual onset and abrupt cessation of ice rafted detritus deposition (IRD, >250mum grains g -1 ), between ∼17 Ka and ∼16.2 Ka. Another IRD pulse identifies a second ice sheet retreat at ∼14.6 Ka. Glacial advance (the Sumas Events), between ∼12.8 and 11.5 Ka, is indicated by increased abundance of medium-coarse silts, sands, with high magnetic susceptibility and poor sorting. Based on the sediment characteristics of this sequence of events, an older ice sheet advance with associated catastrophic retreat has been identified. Submillennial climate variability is revealed by the planktonic delta 18 O record. Between stadial and interstadial conditions, sea surface temperatures (SSTs) ranged between 1.5 to 3°C. Interstadial SSTs (7 to 9°C) off southern British Columbia were ∼2.5°C cooler than those off Southern California, while stadial SSTs (∼5 to 6.5°C) were similar between the regions. Increased western North American margin SST gradients during interstadials may have strengthened the North Pacific High and related northerly winds associated with upwelling. Environmental conditions during interstadials were similar to warm Pacific Decadal and negative North Pacific America Oscillations. The MD02-2496 planktonic delta 18 O record decoupled from other Pacific SST records between 28.5 and ∼15 Ka. This anomalous negative regional delta 18 Owater indicates either freshening of local surface waters, or a precipitation shift from predominantly rain to snow. Evidence for freezing air temperatures could explain the absence of ice sheet response to submillennial climate change.

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 score0.030
Threshold uncertainty score0.061

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0020.004
Science and technology studies0.0010.000
Scholarly communication0.0010.000
Open science0.0010.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0050.001

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 head0.006
GPT teacher head0.164
Teacher spread0.158 · 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
Published2007
Admission routes1
Has abstractyes

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