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Record W2131530587 · doi:10.2110/jsr.2013.32

Genesis of Blackened Limestone Clasts At Late Cenozoic Subaerial Exposure Surfaces, Southern Australia

2013· article· en· W2131530587 on OpenAlexafffund
Carlyle R. Miller, Noel P. James, T. K. Kyser

Bibliographic record

VenueJournal of Sedimentary Research · 2013
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGeology and Paleoclimatology Research
Canadian institutionsQueen's University
FundersGeological Survey of Western AustraliaNatural Sciences and Engineering Research Council of Canada
KeywordsSubaerialGeologyClastic rockCenozoicGeochemistryPaleontologyMineralogySedimentary rockStructural basin

Abstract

fetched live from OpenAlex

Abstract: Black limestone clasts are present across the globe at modern and ancient subaerial exposure surfaces, and in intertidal and supratidal environments. These problematic clasts are particularly abundant at multiple subaerial exposure surfaces across southern Australia. The genesis of such exceptionally preserved clasts can be interpreted through universal fabrics across wide geographic regions and geologic ages. Regardless of location or age, all south Australian blackened clasts studied have a similar microstructure that is dominated by porous micritic laminae and chambered tubules. Such laminae are interpreted to represent calcified root cells and occur in two different varieties: 1) micrite-walled tubules with hollow centers that are thought to represent calcification in the rhizosphere or outer surfaces of the root, and 2) tubules consistent with calcification of both the medulla and cortex, which preserved medulla, cortex, and parenchymatic cells along with xylem vessels. Preserved root fabrics are present only in the blackest clasts and are consequently thought to be the main mechanism driving limestone blackening. The dark coloration in southern Australian clasts is derived from the impregnation of partially decayed terrestrial organic substances. These organic substances were trapped in the cellular structures of roots as they calcified and were subsequently prevented from further decay and oxidation. A threshold of approximately 7-weight % organic carbon is needed in the insoluble residue to produce the distinct black coloration in limestone. This process occurs at the base of slightly organic-rich humic soil profiles where they interact with underlying carbonate bedrock (B–C soil horizon). Roots both physically and chemically (through acid secretion) corrode the underlying limestone and provide the calcium bicarbonate needed in the root calcification process. Specific semiarid flora have the ability to calcify their cellular structures, which could explain why blackened clasts occur at only some unconformities. This result means that the formation of blackened clasts via root calcification and entrapment of organics relies upon specific conditions of semiarid plants and climate along with organic soils. Such conditions would be restricted to a specific climate regime and when combined with the new proposed blackening mechanism herein could help explain their limited distribution and occurrences worldwide.

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)0.003
metaresearch head score (Gemma)0.000
Version: codex-gemma-dda1882f352aValidation status: machine_predicted_unvalidated
Candidate categoriesInsufficient payload (model declined to judge)
Consensus categoriesInsufficient payload (model declined to judge)
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.020
Threshold uncertainty score0.998

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0030.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.000
Science and technology studies0.0000.001
Scholarly communication0.0000.000
Open science0.0010.000
Research integrity0.0000.001
Insufficient payload (model declined to judge)0.0220.002

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 head0.068
GPT teacher head0.312
Teacher spread0.244 · 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; both teacher heads agree on what is shown here.

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

Citations15
Published2013
Admission routes2
Has abstractyes

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