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Record W2988588055 · doi:10.1130/abs/2019am-334055

INVESTIGATING MAXIMUM TEMPERATURES USING RAMAN SPECTROSCOPY OF CARBONACEOUS MATERIAL IN CONODONTS: A COMPARISON WITH THE CONODONT COLOR ALTERATION INDEX

2019· article· en· W2988588055 on OpenAlexaboutno aff
Martyn L. Golding, R. Bruce McMillan

Bibliographic record

VenueAbstracts with programs - Geological Society of America · 2019
Typearticle
Languageen
FieldEngineering
TopicHydrocarbon exploration and reservoir analysis
Canadian institutionsnot available
Fundersnot available
KeywordsConodontRaman spectroscopyDiagenesisAnalytical Chemistry (journal)SpectroscopyMaturity (psychological)Materials scienceGeologyMineralogyChemistryOpticsPaleontologyEnvironmental chemistryPhysics

Abstract

fetched live from OpenAlex

The conodont Color Alteration Index (CAI) has been widely used to provide estimates of maximum temperature in studies of thermal maturity. Despite this, several drawbacks of CAI have been identified. Firstly, there is significant uncertainty in the identification of CAI; methods have been proposed to make the quantification of CAI more rigorous, but they are not routinely applied. Secondly, CAI is not just related to temperature but also to duration of heating; as this duration is commonly unknown, there is significant uncertainty in estimates of maximum temperature based on CAI. Finally, CAI has been shown to be affected not just by heat, but also by diagenesis; although no mechanism by which diagenesis would affect CAI has been clearly defined. Raman spectroscopy of carbonaceous material (RSCM) has been extensively used to calculate maximum temperatures experienced by organic matter in sedimentary rocks. As carbonaceous matter is heated, it becomes progressively more graphitized, leading to an increase in structural order that can be measured by Raman spectroscopy. A set of 49 conodont specimens with varying CAI from several localities in British Columbia, Canada, were analysed with Raman spectroscopy, and maximum temperatures for these specimens were calculated independently from CAI by using the Iterative Fitting of Raman Spectra (IFORS) technique. Maximum temperatures calculated with IFORS often show significant deviation from the temperatures estimated by CAI alone; CAI thus appears to be an inconsistent indicator of maximum temperature. The greatest variation between IFORS and CAI temperatures occurs in specimens with CAI of 2.5, 4.5, and 6.0. Analysis of minor and trace element compositions of these specimens shows that they also have relatively high concentrations of exogenous cations. Additional investigation of the biomineral component of conodonts using Raman spectroscopy shows that diagenetic alteration is pervasive. We propose that conodont color is affected by the diagenetic uptake of exogenous cations into conodonts, and, as a result, CAI does not solely reflect changes in temperature. In contrast, RSCM with IFORS is a relatively inexpensive and minimally-invasive technique for the independent calculation of maximum temperatures, which can replace or supplement CAI.

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)0.001
Version: metacan-v3-hybrid-931329e0061cValidation status: machine_predicted_unvalidated
Candidate categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Bench or experimental · Consensus signal: none
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.028
Threshold uncertainty score0.056

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.001
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0020.002
Science and technology studies0.0010.001
Scholarly communication0.0010.000
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 head0.015
GPT teacher head0.242
Teacher spread0.227 · 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 designBench or experimental
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
Published2019
Admission routes1
Has abstractyes

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