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Effects of black shale weathering on the mobility of rhenium and platinum group elements

2000· article· en· W2092464961 on OpenAlex
Bernhard Peucker‐Ehrenbrink, Robyn Hannigan

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

VenueGeology · 2000
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicPaleontology and Stratigraphy of Fossils
Canadian institutionsnot available
FundersWoods Hole Oceanographic InstitutionNational Science Foundation
KeywordsRadiogenic nuclideGeologyCitationGeochemistryOil shaleRheniumEarth scienceLibrary sciencePaleontologyComputer scienceChemistry

Abstract

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Research Article| May 01, 2000 Effects of black shale weathering on the mobility of rhenium and platinum group elements Bernhard Peucker-Ehrenbrink; Bernhard Peucker-Ehrenbrink 1Woods Hole Oceanographic Institution, MS 25, Woods Hole, Massachusetts 02543-1541, USA Search for other works by this author on: GSW Google Scholar Robyn E. Hannigan Robyn E. Hannigan 1Woods Hole Oceanographic Institution, MS 25, Woods Hole, Massachusetts 02543-1541, USA Search for other works by this author on: GSW Google Scholar Geology (2000) 28 (5): 475–478. https://doi.org/10.1130/0091-7613(2000)28<475:EOBSWO>2.0.CO;2 Article history received: 22 Oct 1999 rev-recd: 14 Feb 2000 accepted: 23 Feb 2000 first online: 02 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Bernhard Peucker-Ehrenbrink, Robyn E. Hannigan; Effects of black shale weathering on the mobility of rhenium and platinum group elements. Geology 2000;; 28 (5): 475–478. doi: https://doi.org/10.1130/0091-7613(2000)28<475:EOBSWO>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 SocietyGeology Search Advanced Search Abstract Radiogenic Os from the continents dominates the late Cenozoic marine Os budget. A variety of proposed radiogenic sources includes organic-rich sediments, Precambrian shields, and Re-rich sulfides. Identifying the dominant sources of radiogenic Os to the oceans has a strong impact on past climate models because weathering of silicates acts as a net sink of CO2, whereas weathering of organic matter acts as a source. Here we investigate the effects of black shale weathering on the integrity of the Re-Os isotope system and release of Re and platinum group elements. Time-correlative pairs of fresh (drill core) and weathered (outcrop) black shales of Late Ordovician age (Utica Shale magnafacies, Québec) were analyzed for Re, Os, Ir, Pt, and Pd, as well as total S, N, and C (as Ccarb and Corg). The results indicate that 25%–64% of the initial Re budget, 45%–90% of the Os budget, 14%–65% of the Ir budget, 60%–77% of the Pt budget, 69%–86% of the Pd budget, and 44%–96% of the Corg budget are lost during weathering. We use positive correlations of Os, Pt, and Pd with Corg and N to calculate the respective platinum group element concentrations in the unweathered organic matter end member as ∼3 ng/g Os, ∼9 ng/g Pt, and 11–24 ng/g Pd. Although black shales make up <1% of the continental crust, mass-balance calculations indicate that such facies contribute significantly to the labile Os inventory of the continental crust. 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 categoriesInsufficient payload (model declined to judge)
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.060
Threshold uncertainty score1.000

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 head0.008
GPT teacher head0.196
Teacher spread0.189 · 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