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Record W2614576513 · doi:10.1130/g21945.1

Model of seawater composition for the Phanerozoic

2005· article· en· W2614576513 on OpenAlexaffabout
Robert V. Demicco, Tim K. Lowenstein, Lawrence A. Hardie, Ronald J. Spencer

Bibliographic record

VenueGeology · 2005
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGroundwater and Isotope Geochemistry
Canadian institutionsUniversity of Calgary
Fundersnot available
KeywordsCitationIconLibrary scienceDownloadComposition (language)PhanerozoicHistoryGeologyArchaeologyComputer scienceWorld Wide WebPaleontologyArtLiterature

Abstract

fetched live from OpenAlex

Research Article| November 01, 2005 Model of seawater composition for the Phanerozoic Robert V. Demicco; Robert V. Demicco 1 Department of Geological Sciences and Environmental Studies, Binghamton University, Binghamton, New York 13902-6000, USA Search for other works by this author on: GSW Google Scholar Tim K. Lowenstein; Tim K. Lowenstein 1 Department of Geological Sciences and Environmental Studies, Binghamton University, Binghamton, New York 13902-6000, USA Search for other works by this author on: GSW Google Scholar Lawrence A. Hardie; Lawrence A. Hardie 2Earth and Planetary Sciences Department, Johns Hopkins University, Baltimore, Maryland 21218, USA Search for other works by this author on: GSW Google Scholar Ronald J. Spencer Ronald J. Spencer 3Department of Geology and Geophysics, University of Calgary, Calgary, Alberta T2N 1N4, Canada Search for other works by this author on: GSW Google Scholar Geology (2005) 33 (11): 877–880. https://doi.org/10.1130/G21945.1 Article history received: 08 Jun 2005 rev-recd: 29 Jun 2005 accepted: 06 Jul 2005 first online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Robert V. Demicco, Tim K. Lowenstein, Lawrence A. Hardie, Ronald J. Spencer; Model of seawater composition for the Phanerozoic. Geology 2005;; 33 (11): 877–880. doi: https://doi.org/10.1130/G21945.1 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 We present an inverse model of Phanerozoic seawater composition calibrated against updated paleoseawater compositions from fluid inclusions in marine halites. The model considers step-wise alteration of seawater composition via: (1) variable input of river water, (2) variable rates of alteration of seawater through reactions at mid-ocean ridges, and (3) variable rates of alteration of seawater through reactions on ridge flanks and across the ocean floor in general. The model achieves agreement with paleoseawater fluid inclusion data for Na+, Ca2+, SO42−, and K+, particularly when variable runoff is considered. Variable rates of basalt- seawater interactions at both ridges and ridge flanks are required to understand the evolution of seawater, particularly the observed, near-constant concentration of K+ through time. You do not have access to this content, please speak to your institutional administrator if you feel you should have access.

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: Simulation or modeling · Consensus signal: Simulation or modeling
GenreCandidate signal: Empirical · Consensus signal: none
Teacher disagreement score0.038
Threshold uncertainty score0.075

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.001
Meta-epidemiology (narrow)0.0010.000
Meta-epidemiology (broad)0.0010.001
Bibliometrics0.0010.001
Science and technology studies0.0010.001
Scholarly communication0.0010.001
Open science0.0010.001
Research integrity0.0020.001
Insufficient payload (model declined to judge)0.0090.003

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 head0.022
GPT teacher head0.214
Teacher spread0.192 · 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 designSimulation or modeling
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

Citations149
Published2005
Admission routes2
Has abstractyes

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