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Taphonomic Control on Microstructure in Early Neoproterozoic Reefal Stromatolites and Thrombolites

2000· article· en· W2178097138 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 · 2000
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicPaleontology and Stratigraphy of Fossils
Canadian institutionsQueen's University
Fundersnot available
KeywordsGeologyCitationPaleontologyTaphonomyReefQueen (butterfly)ArchaeologyLibrary scienceGeographyOceanographyComputer scienceEcology

Abstract

fetched live from OpenAlex

Other| April 01, 2000 Taphonomic Control on Microstructure in Early Neoproterozoic Reefal Stromatolites and Thrombolites ELIZABETH C. TURNER; ELIZABETH C. TURNER 1Department of Geological Sciences, Queen's University, Kingston, Ontario, K7L 3N6, Canada Search for other works by this author on: GSW Google Scholar NOËL P. JAMES; NOËL P. JAMES 1Department of Geological Sciences, Queen's University, Kingston, Ontario, K7L 3N6, Canada Search for other works by this author on: GSW Google Scholar GUY M. NARBONNE GUY M. NARBONNE 1Department of Geological Sciences, Queen's University, Kingston, Ontario, K7L 3N6, Canada Search for other works by this author on: GSW Google Scholar PALAIOS (2000) 15 (2): 87–111. https://doi.org/10.1669/0883-1351(2000)015<0087:TCOMIE>2.0.CO;2 Article history accepted: 08 Dec 1999 first online: 03 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Twitter LinkedIn Tools Icon Tools Get Permissions Search Site Citation ELIZABETH C. TURNER, NOËL P. JAMES, GUY M. NARBONNE; Taphonomic Control on Microstructure in Early Neoproterozoic Reefal Stromatolites and Thrombolites. PALAIOS 2000;; 15 (2): 87–111. doi: https://doi.org/10.1669/0883-1351(2000)015<0087:TCOMIE>2.0.CO;2 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyPALAIOS Search Advanced Search Abstract Early Neoproterozoic reefs of the Little Dal Group, Northwest Territories, are built by stromatolites and thrombolites containing calcified filamentous cyanobacteria and interstitial cement. Micritic and microcrystalline carbonate grew in or on extracellular cyanobacterial sheaths, preserving filaments when mineralization was early relative to sheath degradation, or grumeaux when mineralization was later. Filamentous microstructure is volumetrically predominant in the reefs; less common are micritic and grumelous microstructures already known from late Proterozoic stromatolites and Phanerozoic thrombolites. Textural intergradation of filamentous-calcimicrobial microstructure with these non-filamentous microstructures reflects microstructural variation developed through differential preservation at the scale of individual filaments and laminae. Textural gradients from filaments to grumeaux, and from calcimicrobial to stromatolitic and thrombolitic microstructure types, imply that a wide variety of microbialite microstructure types can be derived from a single progenitor community. This suggests that taphonomic variables may be as important in the development of microbialite microstructure as the biology of the microbial mat community. It also challenges recent suggestions that the Neoproterozoic increase in thromboids was related to the rise of multicellular organisms. These conclusions have broad implications for the interpretation of fossil microbialites, many of which might have been more closely related in origin than hitherto suspected. You do not have access to this content, please speak to your institutional administrator if you feel you should have access.

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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 score0.062
Threshold uncertainty score0.719

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)0.0010.000

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 head0.005
GPT teacher head0.186
Teacher spread0.181 · 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