MétaCan
Menu
Back to cohort
Record W4400248620 · doi:10.1038/s41561-024-01479-1

Sustained increases in atmospheric oxygen and marine productivity in the Neoproterozoic and Palaeozoic eras

2024· article· en· W4400248620 on OpenAlexaff
Richard Stockey, Devon B. Cole, Úna C. Farrell, Heda Agić, Thomas H. Boag, Jochen J. Brocks, Donald E. Canfield, Meng Cheng, Peter W. Crockford, Huan Cui, Tais W. Dahl, Lucas Del Mouro, Keith Dewing, Stephen Q. Dornbos, Joseph F. Emmings, Robert R. Gaines, Timothy M. Gibson, Benjamin C. Gill, Geoffrey J. Gilleaudeau, Karin Goldberg, Romain Guilbaud, Galen P. Halverson, Emma U. Hammarlund, Kalev Hantsoo, Miles A. Henderson, Charles M. Henderson, Malcolm S.W. Hodgskiss, A.J.M. Jarrett, David T. Johnston, Pavel Kabanov, Julien Kimmig, Andrew H. Knoll, Marcus Kunzmann, Matthew A. LeRoy, Chao Li, David K. Loydell, Francis A. Macdonald, Joseph M. Magnall, N. Tanner Mills, Lawrence M. Och, Brennan O’Connell, Anaïs Pagès, Shanan E. Peters, Susannah M. Porter, Simon W. Poulton, Samantha R. Ritzer, Alan D. Rooney, Shane D. Schoepfer, Emily F. Smith, Justin V. Strauss, Gabriel Jubé Uhlein, Tristan White, Rachel Wood, Christina R. Woltz, I. A. Yurchenko, Noah J. Planavsky, Erik A. Sperling

Bibliographic record

VenueNature Geoscience · 2024
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicPaleontology and Stratigraphy of Fossils
Canadian institutionsUniversity of CalgaryMcGill UniversityGeological Survey of CanadaCarleton University
FundersUniversity of SouthamptonStanford Research Computing Center, Stanford UniversityAmerican Chemical Society Petroleum Research FundNational Science Foundation
KeywordsPaleozoicSedimentary rockGeologyContext (archaeology)Earth scienceAtmosphere (unit)ProductivityGeologic recordTrace fossilAtmospheric oxygenPaleontologyOxygen

Abstract

fetched live from OpenAlex

Abstract A geologically rapid Neoproterozoic oxygenation event is commonly linked to the appearance of marine animal groups in the fossil record. However, there is still debate about what evidence from the sedimentary geochemical record—if any—provides strong support for a persistent shift in surface oxygen immediately preceding the rise of animals. We present statistical learning analyses of a large dataset of geochemical data and associated geological context from the Neoproterozoic and Palaeozoic sedimentary record and then use Earth system modelling to link trends in redox-sensitive trace metal and organic carbon concentrations to the oxygenation of Earth’s oceans and atmosphere. We do not find evidence for the wholesale oxygenation of Earth’s oceans in the late Neoproterozoic era. We do, however, reconstruct a moderate long-term increase in atmospheric oxygen and marine productivity. These changes to the Earth system would have increased dissolved oxygen and food supply in shallow-water habitats during the broad interval of geologic time in which the major animal groups first radiated. This approach provides some of the most direct evidence for potential physiological drivers of the Cambrian radiation, while highlighting the importance of later Palaeozoic oxygenation in the evolution of the modern Earth system.

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)0.001
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 score0.133
Threshold uncertainty score0.974

Codex and Gemma teacher scores by category

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

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 head0.216
Teacher spread0.211 · 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 teacher head, not a consensus.

The models applied no category: nothing in the taxonomy fit this work.
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

Citations68
Published2024
Admission routes1
Has abstractyes

Explore more

Same venueNature GeoscienceSame topicPaleontology and Stratigraphy of FossilsFrench-language works237,207