Evidence map›Paper›PMID 39438650›Full record

ArticleScientific reports2024

Fossil biocalcite remains open to isotopic exchange with seawater for tens of millions of years.

Deyanira Cisneros-Lazaro, Arthur Adams, Jarosław Stolarski, Sylvain Bernard, Damien Daval, Alain Baronnet, Olivier Grauby, Lukas P Baumgartner, Torsten Vennemann, Jo Moore and 4 more

Abstract read
PubMed Full text at PMC Publisher
In one paragraph

Article in Scientific reports, 2024. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 1 paper.

0numbers the graph read from it
0cells of the map it votes in
1citing papers in PubMed
–field-weighted citation impact
1 · What the graph read from it

What it found

Each row is one number read from the abstract, on the scale the paper reported it, with its interval. Left of the dashed line favours the treatment, right favours the comparator. Under each row is the sentence it came from. New to these charts? A ten-minute tutorial.

The abstract states no effect estimate the extractor could read, or names no intervention and outcome on the map, so this paper lights no cell and moves no belief. It is still indexed, cited and linked below.

2 · The registry

The trial behind it

Trials whose registry record cites this paper, or whose number appears in the abstract. A trial that started after this paper was published is citing it as background, not reporting it.

Neither the registry nor the abstract names a trial number. If this is a trial report, that itself is worth knowing.

3 · Its place in the literature

Who cites it

1 citing paper in PubMed.

  1. Article
4 · The record

Corrections and comments

PubMed lists nothing against this paper. Absence here is not a guarantee, only a check that was made.

5 · Who and what money

Authors and funding

14 authors.

Deyanira Cisneros-LazaroLaboratory for Biological Geochemistry, School of Architecture, Civil and Environmental Engineering, Ecole Polytechnique Fédérale de Lausanne, 1015, Lausanne, Switzerland. deyanira.cisneroslazaro@epfl.ch.
Arthur AdamsLaboratory for Biological Geochemistry, School of Architecture, Civil and Environmental Engineering, Ecole Polytechnique Fédérale de Lausanne, 1015, Lausanne, Switzerland.
Jarosław StolarskiInstitute of Paleobiology, Polish Academy of Sciences, 00818, Warsaw, Poland.
Sylvain BernardInstitut de Minéralogie, de Physique des Matériaux et de Cosmochimie, Muséum National d'Histoire Naturelle, CNRS, Sorbonne Université, 75005, Paris, France.
Damien DavalInstitut des Sciences de la Terre, CNRS- Université Grenoble Alpes, 38058, Grenoble, France.
Alain BaronnetCentre Interdisciplinaire de Nanosciences de Marseille, CNRS - Aix-Marseille Université, 13288, Marseille, France.
Olivier GraubyCentre Interdisciplinaire de Nanosciences de Marseille, CNRS - Aix-Marseille Université, 13288, Marseille, France.
Lukas P BaumgartnerCenter for Advanced Surface Analysis, Institute of Earth Science, University of Lausanne, 1015, Lausanne, Switzerland.
Torsten VennemannInstitute of Earth Surface Dynamics, University of Lausanne, 1015, Lausanne, Switzerland.
Jo MooreCenter for Advanced Surface Analysis, Institute of Earth Science, University of Lausanne, 1015, Lausanne, Switzerland.
Claudia BaumgartnerCenter for Advanced Surface Analysis, Institute of Earth Science, University of Lausanne, 1015, Lausanne, Switzerland.
Cristina Martin OlmosLaboratory for Biological Geochemistry, School of Architecture, Civil and Environmental Engineering, Ecole Polytechnique Fédérale de Lausanne, 1015, Lausanne, Switzerland.
Stéphane EscrigLaboratory for Biological Geochemistry, School of Architecture, Civil and Environmental Engineering, Ecole Polytechnique Fédérale de Lausanne, 1015, Lausanne, Switzerland.
Anders MeibomLaboratory for Biological Geochemistry, School of Architecture, Civil and Environmental Engineering, Ecole Polytechnique Fédérale de Lausanne, 1015, Lausanne, Switzerland. anders.meibom@epfl.ch.

Funding

European Research Council 788752
6 · The paper itself

Abstract

Fossilized remains of marine calcifiers constitute the physical basis for reconstructions of both deep ocean and sea-surface temperatures going back millions of years, but paleoclimate records derived from their isotope and trace-element chemistry can be biased by diagenesis. Experiments simulating diagenesis in the presence of an

Identifiers

PMID39438650
PMCPMC11496820

What OpenQuestion holds

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LicenceCC BY
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Registered trials

None linked

Read under generation 80e0d062 · epoch 390. Bibliography from PubMed, PubMed Central and OpenAlex; grants from NIH RePORTER; trial links from ClinicalTrials.gov; estimates, votes and beliefs from the OpenQuestion graph.