Evidence map›Paper›PMID 31249387›Full record

ArticleScientific reports2019

Carbon cycle instability and orbital forcing during the Middle Eocene Climatic Optimum.

Martino Giorgioni, Luigi Jovane, Eric S Rego, Daniel Rodelli, Fabrizio Frontalini, Rodolfo Coccioni, Rita Catanzariti, Ercan Özcan

Abstract read
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Article in Scientific reports, 2019. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 7 papers.

0numbers the graph read from it
0cells of the map it votes in
7citing 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

7 citing papers in PubMed.

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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

8 authors.

Martino GiorgioniInstituto Oceanográfico, Universidade de São Paulo, São Paulo, 05508-120, Brazil. gmartino@unb.br.ORCID http://orcid.org/0000-0003-0565-3150
Luigi JovaneInstituto Oceanográfico, Universidade de São Paulo, São Paulo, 05508-120, Brazil.ORCID http://orcid.org/0000-0003-4348-4714
Eric S RegoInstituto Oceanográfico, Universidade de São Paulo, São Paulo, 05508-120, Brazil.
Daniel RodelliInstituto Oceanográfico, Universidade de São Paulo, São Paulo, 05508-120, Brazil.
Fabrizio FrontaliniDipartimento di Scienze Pure e Applicate (DiSPeA), Università degli Studi di Urbino "Carlo Bo", 61029, Urbino, Italy.ORCID http://orcid.org/0000-0002-0425-9306
Rodolfo CoccioniDipartimento di Scienze Pure e Applicate (DiSPeA), Università degli Studi di Urbino "Carlo Bo", 61029, Urbino, Italy.
Rita CatanzaritiIstituto di Geoscienze e Georisorse, Consiglio Nazionale delle Ricerche (CNR), 56124, Pisa, Italy.ORCID http://orcid.org/0000-0002-6408-0543
Ercan ÖzcanFaculty of Mines, Department of Geological Engineering, Istanbul Technical University (ITU), Maslak, 34469, Istanbul, Turkey.

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

The Middle Eocene Climatic Optimum (MECO) is a global warming event that occurred at about 40 Ma. In comparison to the most known global warming events of the Paleogene, the MECO has some peculiar features that make its interpretation controversial. The main peculiarities of the MECO are a duration of ~500 kyr and a carbon isotope signature that varies from site to site. Here we present new carbon and oxygen stable isotopes records (δ

Identifiers

PMID31249387
PMCPMC6597698

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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.