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Record W6990024313

A continental ichnological study across Romer’s Gap (Mississippian Period) in Southern New Brunswick: implications for the colonization of Lacustrine and Alluvial continental environments

2025· article· en· W6990024313 on OpenAlexaboutno aff

Bibliographic record

VenueSaint Mary's University Institutional Repository (Saint Mary's University) · 2025
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicPaleontology and Evolutionary Biology
Canadian institutionsnot available
Fundersnot available
KeywordsTetrapod (structure)Trace fossilAlluviumViséanTournaisianCarboniferousContinental marginAlluvial plainAggradation
DOInot available

Abstract

fetched live from OpenAlex

Vertebrate fossils from continental environments are rare in the Misssippian Period. This includes the interval spanning the Tournaisian and Visean stages historically known as ‘Romer’s Gap’, where the few known sites represent paleoenvironments close to open water rather than inland continental conditions. This thesis uses ichnofossils from the Mississippian-aged strata of southern New Brunswick, Canada as a proxy for biodiversity. Examination of the Horton, Sussex, and Mabou groups in the Martimes Basin has yielded diverse footprint ichnoassemblages representing the earliest-known Carboniferous tetrapods. Additionally, the latest Visean to Serpukhovian Mabou Group has yielded the oldest-known tetrapod burrows. The sedimentological record suggests the tetrapods responsible for trackways lived within forested wetlands on the margins of freshwater lakes and alluvial plains, thus representing the earliest colonization of continental paleoenvironments by tetrapods. Tetrapod burrowing represents the earliest known behavioral response of the group to climate change. Trace fossils demonstrate that diverse tetrapods were already adapted for continental ecosystems earlier in the Mississippian than previously recorded, representing the oldest known evidence for temnospondyls, anthracosaurs, and recumbirostran ‘microsaur’ lineages. Relic Devonian-grade polydactyl tetrapods similar to whatcheerids remained within the alluvial Kennebecasis Formation. The dryland, strongly seasonal alluvial settings of the Stilesville and Enrage formations preserve sparse tetrapod ichnofossils interpreted to have been made by anthracosaurs and recumbirostran microsaurs that were likely better-adapted to continental conditions. This study tests and mostly agrees with recently-established ichnobiochronological models for the Mississippian Period, with evidence of Valentian ichnobiochronological elements extending into the Mississippian Bluebeachian ichnobiochron, suggesting an overlap between them. The present research extends the known chronological distribution of several ichnogenera (Hylopus, Batrachichnus, Limnopus) earlier into the Tournaisian. This study also informally recognizes new tetrapod ichnofossil morphotypes that will be published as new ichnotaxa, including new trackways (‘Brachydactylopus’ and a new polydactyl trackway) and burrows (Reniformichnus ‘stringeri’ and Katarrhedrites ‘peekabooensis’).

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 score0.286
Threshold uncertainty score0.574

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0010.002
Science and technology studies0.0010.000
Scholarly communication0.0010.000
Open science0.0000.001
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 head0.013
GPT teacher head0.212
Teacher spread0.199 · 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
Published2025
Admission routes1
Has abstractyes

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