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Record W2099641485 · doi:10.2110/palo.2005.p05-103r

LINGULIDE BRACHIOPODS AND THE TRACE FOSSIL <i>LINGULICHNUS</i> FROM THE TRIASSIC OF WESTERN CANADA: IMPLICATIONS FOR FAUNAL RECOVERY AFTER THE END-PERMIAN MASS EXTINCTION

2007· article· en· W2099641485 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.
aboutThe title or abstract carries a Canadian signal from the geographic lexicon.

Bibliographic record

VenuePalaios · 2007
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicPaleontology and Stratigraphy of Fossils
Canadian institutionsUniversity of AlbertaUniversity of CalgaryGeological Survey of Canada
Fundersnot available
KeywordsExtinction eventPermian–Triassic extinction eventPermianGeologyPaleontologyTrace fossilExtinction (optical mineralogy)TRACE (psycholinguistics)Structural basin

Abstract

fetched live from OpenAlex

Abstract The environmental distribution of lingulide brachiopods in western Canadian Triassic marine successions, their relationship with other infaunal organisms occupying the same ecospace, and their role in the aftermath of the Permian-Triassic extinction event is summarized. Western Canada is an ideal location to assess lingulide distribution patterns as upper Paleozoic and lower Mesozoic strata are extensively exposed, and lingulides (cf. Lingularia Biernat and Emig) and the trace fossil Lingulichnus Hakes are both common. A distribution comparison of in situ lingulides and Lingulichnus Hakes with concordantly emplaced lingulide shells and shell beds shows clearly that the latter is a poor indicator of true environmental distribution of these infaunal suspension feeders. Lingulides are rare in uppermost Paleozoic strata in the study area. Most occurrences consist of isolated valves or abraded material in erosional lags. Lingulides remain minor components of infaunal communities during the earliest Triassic (Griesbachian). Although lingulide valves and valve fragments are the dominant body fossil observed, trace fossil analysis indicates that lingulides were minor components of earliest Triassic infaunal communities. Lingulides increase in abundance and importance during the Dienerian and Smithian. Shallow and marginal marine trace-fossil assemblages of this age are dominated commonly by Lingulichnus. Lingulide fossils are less abundant but are found in many shallow and marginal marine lithofacies. Lingulides comprise only a minor component of late Smithian through Anisian infaunal communities. Canadian lingulide abundance reached an acme during the latest Middle Triassic (Ladinian). Fossil material is common in many environments, however, in situ lingulides and the trace fossil Lingulichnus occur primarily in tempestites in proximal offshore through lower shoreface settings and in intertidal flat settings. Although quantitatively more abundant in the Middle Triassic, lingulides were proportionally more abundant in Lower Triassic successions. Regardless of relative changes in abundance, the environmental distribution of lingulides did not differ between Early and Middle Triassic successions. Lingulides comprise only a minor component of Upper Triassic infaunal communities. Early Triassic lingulides did not occupy any environmental settings from which they were excluded prior to the Permian-Triassic extinction or after the postextinction recovery interval. Thus, lingulides were not postextinction disaster taxa but rather were ecological opportunists that dominated some Early Triassic shallow and marginal marine successions.

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 score0.854
Threshold uncertainty score0.920

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 studies0.0010.000
Scholarly communication0.0000.000
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 head0.012
GPT teacher head0.223
Teacher spread0.211 · 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