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Record W2153573979 · doi:10.1002/ppp.572

A chronology of Late‐Pleistocene permafrost events in southern New Jersey, Eastern USA

2007· article· en· W2153573979 on OpenAlex

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.

Bibliographic record

VenuePermafrost and Periglacial Processes · 2007
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeology and Paleoclimatology Research
Canadian institutionsUniversity of Ottawa
FundersUniversity of OttawaNational Park ServiceNational Center for Atmospheric ResearchNew Jersey Forest Service
KeywordsPermafrostThermokarstGeologyChronologyPleistoceneFrost weatheringGeomorphologyFrost (temperature)HolocenePaleontologyPhysical geographyOceanographySoil waterSoil science

Abstract

fetched live from OpenAlex

Abstract Frost fissures, filled with wind‐abraded sand and mineral soil, and numerous small‐scale non‐diastrophic deformations, occur in the near‐surface sediments of the Pine Barrens of southern New Jersey. The fissures are the result of thermal‐contraction cracking and indicate the previous existence of either permafrost or seasonally‐frozen ground. The deformations reflect thermokarst activity that occurred when permafrost degraded, icy layers melted and density‐controlled mass displacements occurred in water‐saturated sediments. Slopes and surficial materials of the area reflect these cold‐climate conditions. Optically‐stimulated luminescence permits construction of a tentative Late‐Pleistocene permafrost chronology. This indicates Illinoian, Early‐Wisconsinan and Late‐Wisconsinan episodes of permafrost and/or deep seasonal frost and a Middle‐Wisconsinan thermokarst event. Copyright © 2007 John Wiley & Sons, Ltd.

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)0.000
metaresearch head score (Gemma)0.000
Version: codex-gemma-dda1882f352aValidation status: machine_predicted_unvalidated
Candidate categoriesInsufficient payload (model declined to judge)
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.167
Threshold uncertainty score0.998

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.000
Science and technology studies0.0000.000
Scholarly communication0.0000.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0030.000

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 head0.021
GPT teacher head0.262
Teacher spread0.241 · 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