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Independent corroboration of a previously proposed Palaeozoic link between eastern Australia and eastern North America

2003· article· en· W2018858688 on OpenAlexaboutno aff
Jerome E. Dobson

Bibliographic record

VenueJournal of Biogeography · 2003
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicEvolution and Paleontology Studies
Canadian institutionsnot available
Fundersnot available
KeywordsPaleozoicGeologyPaleontologyOrdovicianDevonianLaurentiaFold (higher-order function)PermianGondwanaOrogenyTectonics

Abstract

fetched live from OpenAlex

A new finding by Ebach & Humphries (2002) published in the Journal of Biogeography and reported in Science (Holden, 2002) amounts to independent corroboration of my earlier proposal (Dobson, 1992, 1996) that eastern Australia may have collided with eastern North America in the Paleozoic. They conclude, based on cladistic analysis of Lower Devonian trilobites, ‘New South Wales … has a closer association to the Appalachian province than it does to Victoria. The areas may be adjusted by aligning the palaeolongitude of Laurentia so it is closer to the eastern Australian coastline.’ In the mid-1990s, I tested the hypothesis that Australia and eastern North America met in rotational collision during the Palaeozoic with the corollary that the New England fold belt of Australia, rather than the Reguibat promontory of Africa, collided with the Alleghanian orogen in the central Appalachians (Dobson, 1996). Substantial corroborating evidence was presented in this journal: Identical Lancefieldian stage, zone 1 (Early Ordovician) graptolites of the Anisograptid family are found in identical environments in Newfoundland, Norway, and the Lachlan fold belt of Australia. Paleozoic granites are consistent with a tectonic model in which the Lachlan fold belt caused mechanical deformation of the Canadian Appalachians. The Lachlan and New England fold belts of Australia and the Alleghanian orogen of North America are tectonically consistent with this east coast hypothesis. Major deformations and magmatic episodes are coeval from Silurian to Permian. I concluded, ‘The tectonic, paleontologic, lithologic, and geometric evidence for this position is more abundant and precise than the stratigraphic evidence for a west coast location of Australia relative to North America.’ According to Holden (2002), ‘Ebach and Humphries…say that trilobites living in what is now the southern and central United States were more like ones from eastern Australia than those in Africa or South America. This suggests that accepted maps of the ancient landmasses of Gondwana (covering South America, Africa and Australia) and Laurentia (which included North America) are way off. ‘‘They moved right around the world 8000 kilometers west of where scientists originally placed them,’’ Ebach says.’ So far, so good, but there is a troubling contradiction in the interpretations offered by Ebach and Humphries. Their statement (p. 437) matches their cladistic diagram (Fig. 10, p. 438), but their map (Fig. 11b, p. 439) does not. The text and cladistic diagram fully support my east coast hypothesis, but their map inexplicably asserts a west coast hypothesis. Only they can explain the discrepancy.

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 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 score0.007
Threshold uncertainty score0.364

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 head0.027
GPT teacher head0.243
Teacher spread0.216 · 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 teacher head, 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

Citations1
Published2003
Admission routes1
Has abstractyes

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