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Record W6908329379 · doi:10.25949/19439840

Stratigraphy and conodont biozonation of the lower Devonian limestones, Waratah Bay, Victoria

2021· dissertation· en· W6908329379 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.

aboutThe title or abstract carries a Canadian signal from the geographic lexicon.
no affNo Canadian affiliation: this work is invisible to an affiliation-only frame.
No Canadian affiliation. An affiliation-only frame, the usual design, would never have seen this work. It is one of the works that make the case for inverting the frame.

Bibliographic record

VenueMacquarie University · 2021
Typedissertation
Languageen
FieldEarth and Planetary Sciences
TopicPaleontology and Stratigraphy of Fossils
Canadian institutionsnot available
Fundersnot available
KeywordsConodontDevonianStratigraphySection (typography)Sequence (biology)PulverizerPoint (geometry)

Abstract

fetched live from OpenAlex

The stratigraphical relationship of a number of limestone sequences belonging to two formations at Waratah Bay, Victoria, has been determined on lithographical and micro-faunal evidence. Two new members have been defined for the WARATAH LIMESTONE. The older, Lower Grinder Member, includes those sequences developed at Point Grinder (lower part). The Black Stack (new name), Robin Rocks and the uppermost part of the Bell Point section. The younger, Mushroom Rock Member, embraces Point Grinder (upper part), Kiln, Bird Rock, Gair Rock and Mushroom Rock sequences. The BELL POINT LIMESTONE, above the unconformity, has been re-defined, so that the uppermost part of the Bell Point section is now assigned to the Lower Grinder Member of the WARATAH FORMATION. The dark grey limestone sequences at the Bluff (Walkerville) and Point Grinder (uppermost part) are relegated to the BELL POINT FORMATION. Detailed description of the various carbonate sequences, together with field maps showing section traverses, are included under Appendix A; Section Profiles are in pocket. An early to middle Siegenian age is attributed to the Waratah Bay limestones on the presence of three diagnostic forms, Spathognothodus sulcatus (PHILIP), S. remscheidensis ZIEGLER and S. exiguous philipi KLAPPER. A conodont biozonation is proposed for part of the Lower Devonian with reference to KLAPPER's (1969) work on the conodont sequence at Royal Creek, Canada, in association with LENZ'S brachiopod stages. The Waratah Bay faunas permit the establishment of two zones and one sub-zone as follows: 1. Zone with Spagnognathodus victoriensis n.ps. and Ozarkodina grinderi n.sp., lying below the S. sulcatus zone; 2. Zone with S. sulcatus, associated with S. remscheidensis in the lower part (sub-zone). Of the 210 samples treated from Waratah Bay, 75 yielded conodonts, representing 13 genera and 40 species. Of these, 32 species are identifiable and 8 species are indeterminate. Six new species with short ranges within the Lower Devonian are described from Waratah Bay and figured on Plates 1 to 9. They are: Belodella australensis n.sp., Ligonodina waratahensis n.sp., Ozarkodina bischoffi n.sp., Ozarkodina grinderi n.sp., Spathognathodus victoriensis n.sp., and Trichonodella australis n.sp. A preliminary interpretation of the palaeo-environment, based on limited petrographic evidence together with conodont frequency, indicates that extremely variable conditions analogous to modern shore-line environments, were partly operative during deposition of the Waratah Bay limestones.

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 categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.126
Threshold uncertainty score0.896

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)0.0000.000

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 head0.007
GPT teacher head0.183
Teacher spread0.177 · 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