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Record W7066604052

THE ICHNOLOGICAL AND DEPOSITIONAL CONTEXT OF BIOERODED TRICERATOPS BONES FROM THE MAASTRICTHIAN FRENCHMAN FORMATION OF SOUTHERN SASKATCHEWAN, CANADA

2024· dissertation· en· W7066604052 on OpenAlexfundaboutno aff

Bibliographic record

VenueUniversity Library (University of Saskatchewan) · 2024
Typedissertation
Languageen
FieldEarth and Planetary Sciences
TopicGeological formations and processes
Canadian institutionsnot available
FundersDinosaur Research InstituteUniversity of AlbertaParks CanadaInternational Association of SedimentologistsUniversity of Regina
KeywordsBioerosionTrace fossilPaleoecologySedimentary depositional environmentContext (archaeology)TaphonomyIchnologyPaleobotanyIchnofacies
DOInot available

Abstract

fetched live from OpenAlex

Previous studies on osteic bioerosion trace fossils on dinosaur bones have contributed to our understanding of Mesozoic terrestrial paleoecology and depositional environments. In many cases, body fossils of the inferred tracemaker are either exceedingly rare or absent from the fossil record due to taphonomy. However, studies of bioerosion on dinosaur material conducted on Canadian specimens are uncommon, which is surprising given the volume of dinosaur material collected each year in the country. The ceratopsid Triceratops prorsus is the most common dinosaur fossil from the latest Maastrichtian Frenchman Formation in Saskatchewan, represented by thousands of specimens. Classifying osteic bioerosion trace fossils on Triceratops bones from the Frenchman Formation using established ichnotaxobases coupled with sedimentological data allows for insight into the hidden invertebrate diversity within the Frenchman Formation, as well as how plants used dinosaur bones as a nutrient source.\nStratigraphic sections of the Frenchman Formation were measured in four localities containing Triceratops specimens. All bioeroded specimens of Triceratops identified were preserved in organic-rich mudstone and siltstone deposits, representing floodplain paleosols. Soils are the ideal habitat for terrestrial invertebrate scavengers that serve as the decomposers of decaying animal matter during the early dry stages of decay. The large ichnodiversity of osteic bioerosion trace fossils preserved in Triceratops bones from the Frenchman Formation are the result of pupation chamber construction and necrophagous, and possibly osteophagous terrestrial invertebrates, likely beetles based on comparisons of extant carrion beetle behaviour. Rhizoetchings on bone can be attributed to ancient plant roots directly associated with the Triceratops bones. Established plant communities that utilize soils therefore have a significant ichnological footprint on post-mortem Triceratops bones following burial. Different degrees of preservation of Triceratops bones within floodplain and overbank deposits including poorly drained or water-logged paleosols indicate different taphonomic pathways. This thesis serves as a template for future taphonomic studies of vertebrate body fossils material, considering sedimentological and ichnological evidence on the bones.

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 score0.041
Threshold uncertainty score0.083

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.001
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0040.004
Science and technology studies0.0020.001
Scholarly communication0.0010.000
Open science0.0010.001
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0020.000

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 head0.005
GPT teacher head0.140
Teacher spread0.135 · 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
Published2024
Admission routes2
Has abstractyes

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