MétaCan
Menu
Back to cohort
Record W1992017740 · doi:10.1080/00288306.2003.9514998

Radiocarbon and luminescence dating of overbank deposits in outwash sediments of the Last Glacial Maximum in North Westland, New Zealand

2003· article· en· W1992017740 on OpenAlexaff
Anne Hormes, Frank Preusser, George H. Denton, Irka Hajdas, Dominik Weiß, Thomas F. Stocker, Christian Schlüchter

Bibliographic record

VenueNew Zealand Journal of Geology and Geophysics · 2003
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeology and Paleoclimatology Research
Canadian institutionsInstitute of Particle Physics
FundersSchweizerischer Nationalfonds zur Förderung der Wissenschaftlichen ForschungNational Science Foundation
KeywordsOutwash plainOverbankRadiocarbon datingGeologyGlacial periodThermoluminescence datingGeochemistryMarine isotope stageOptically stimulated luminescenceLoessMoraineLast Glacial MaximumGeomorphologyPaleontologyFluvialInterglacialQuartz

Abstract

fetched live from OpenAlex

Abstract In the Grey River valley, North Westland, New Zealand, extensive terraces of outwash sediments assigned to the Otira glaciation form outstanding geomorphologic features. Four layers of organic sediments subdivide stratified outwash gravels of the major terrace. The age of the fine‐grained sediments is constrained by 55 radiocarbon ( 14 C) ages and 8 optically stimulated luminescence (OSL) ages. The calibrated radiocarbon ages cover the age range between 21 350 and 23 890 cal yr BP. The ages for each different layer are consistent and are in stratigraphic order with mean ages of 22 350 cal yr BP (layer A), 22 470 cal yr BP (layer B), 22 930 cal yr BP (layer C), and 22 960 cal yr BP (layer D). OSL dating of the silty overbank deposits alternating with the organic beds imply a deposition at 21 700 ± 2600 yr. The use of different organic compounds for radiocarbon dating (separated organic residues, humic acids, terrestrial seeds) and the consistency with the luminescence dating support the reliability of the results. We use the informal name Raupo complex for the overbank deposits and consider it to reflect a moderate climate oscillation between two glacial advances during Oxygen Isotope Stage 2.

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 score0.424
Threshold uncertainty score0.842

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.001
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0020.002
Science and technology studies0.0010.001
Scholarly communication0.0010.000
Open science0.0000.000
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 head0.009
GPT teacher head0.215
Teacher spread0.206 · 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

Citations28
Published2003
Admission routes1
Has abstractyes

Explore more

Same venueNew Zealand Journal of Geology and GeophysicsSame topicGeology and Paleoclimatology ResearchFrench-language works237,207