Evidence map›Paper›PMID 39440294›Full record

ArticleJournal of the Royal Society of New Zealand2024

A new tiny fossil penguin from the Late Oligocene of New Zealand and the morphofunctional transition of the penguin wing.

Tatsuro Ando, Jeffrey H Robinson, Carolina Loch, Tamon Nakahara, Shoji Hayashi, Marcus D Richards, Robert Ewan Fordyce

Abstract read
In one paragraph

Article in Journal of the Royal Society of New Zealand, 2024. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 2 papers.

0numbers the graph read from it
0cells of the map it votes in
2citing 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

2 citing papers in PubMed.

  1. Article
  2. 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

7 authors.

Tatsuro AndoAshoro Museum of Paleontology, Ashoro, Japan.ORCID https://orcid.org/0000-0001-7553-5569
Jeffrey H RobinsonDepartment of Geology, University of Otago, Dunedin, New Zealand.
Carolina LochSir John Walsh Research Institute, Faculty of Dentistry, University of Otago, Dunedin, New Zealand.
Tamon NakaharaOkayama University of Science, Okayama, Japan.
Shoji HayashiOkayama University of Science, Okayama, Japan.
Marcus D RichardsDepartment of Geology, University of Otago, Dunedin, New Zealand.
Robert Ewan FordyceDepartment of Geology, University of Otago, Dunedin, New Zealand.

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

The Late Oligocene is a period of high penguin diversity, following major changes in the marine environment at the Eocene/Oligocene boundary and prior to the emergence of crown penguins in the Miocene. Historically, a large morphological gap existed between the most crownward

Indexed as

evolution of wingLatest OligoceneNew ZealandphylogenySmallest fossil penguin

Identifiers

PMID39440294
PMCPMC11459834

What OpenQuestion holds

Textmetadata
LicenceCC BY-NC-ND
Read underepoch 390

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.