Evidence map›Paper›PMID 42467770›Full record

ArticleScience advances2026

The origin of Cretaceous-Palaeogene impactor revealed by nickel isotopes.

Georgy V Makhatadze, Frédéric Moynier, Leslie-Anne Brun, Steven Goderis, Philippe Claeys, Christian Koeberl

Abstract read
In one paragraph

Article in Science advances, 2026. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Not yet cited in PubMed.

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

0 citing papers in PubMed.

No citing paper in PubMed yet.

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

6 authors.

Georgy V MakhatadzeUniversité Paris Cité, Institut de Physique du Globe de Paris, CNRS; 75005 Paris, France.ORCID 0000-0002-9182-3015
Frédéric MoynierUniversité Paris Cité, Institut de Physique du Globe de Paris, CNRS; 75005 Paris, France.ORCID 0000-0003-4321-5581
Leslie-Anne BrunUniversité Paris Cité, Institut de Physique du Globe de Paris, CNRS; 75005 Paris, France.ORCID 0009-0001-1434-2963
Steven GoderisArchaeology, Environmental Changes & Geo-Chemistry, Vrije Universiteit Brussel; 1050 Brussels, Belgium.ORCID 0000-0002-6666-7153
Philippe ClaeysArchaeology, Environmental Changes & Geo-Chemistry, Vrije Universiteit Brussel; 1050 Brussels, Belgium.ORCID 0000-0002-4585-7687
Christian KoeberlDepartment of Lithospheric Research, University of Vienna; 1090 Vienna, Austria.ORCID 0000-0001-5155-7405

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

Sixty-six million years ago, non-avian dinosaurs and other taxa went extinct during one of the largest mass extinctions in the history of life on Earth. The extinction was likely caused by an asteroid of unknown origin, responsible for the Chicxulub impact structure. Existing evidence identifies the impactor as an asteroid, similar to carbonaceous chondrites. However, carbonaceous chondrites are a diverse class of meteorites, leaving the exact nature of the impactor unclear. By measuring Ni isotopes in marine clays containing the impact ejecta, we constrain the impactor to one group of carbonaceous chondrites-CO chondrites-and some ungrouped chondrites. This study highlights the use of Ni isotopes in fingerprinting extraterrestrial materials on Earth. Given that CO chondrites are "dry" compared to the other carbonaceous chondrites and would have delivered much less volatiles, which are thought to be essential in causing the extinction, this work allows further studies of the mechanism behind the extinction.

Identifiers

PMID42467770
PMCPMC13378546

What Socratic holds

Textmetadata
LicenceCC BY-NC
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 Socratic graph.