Evidence map›Paper›PMID 35821210›Full record

ArticleNature communications2022

Early crustal processes revealed by the ejection site of the oldest martian meteorite.

A Lagain, S Bouley, B Zanda, K Miljković, A Rajšić, D Baratoux, V Payré, L S Doucet, N E Timms, R Hewins and 4 more

Open access · goldAbstract read
In one paragraph

Article in Nature communications, 2022. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 4 papers.

0numbers the graph read from it
0cells of the map it votes in
4citing papers in PubMed
4.8field-weighted citation impact, top 5% of its field
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

4 citing papers in PubMed, 33 citations in OpenAlex.

  1. Article
  2. Fundamental constraints and questions from the study of martian meteorites and the need for returned samples.Proceedings of the National Academy of Sciences of the United States of America · 2025
    Article
  3. Article
  4. 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 at 6 institutions in 4 countries.

A LagainSpace Science and Technology Centre, School of Earth and Planetary Science, Curtin University, Perth, WA, Australia. anthony.lagain@gmail.com.ORCID 0000-0002-5391-3001
S BouleyUniversité Paris-Saclay, CNRS, GEOPS, 91405, Orsay, France.
B ZandaIMCCE, Observatoire de Paris, 77 avenue Denfert-Rochereau, 75005, Paris, France.
K MiljkovićSpace Science and Technology Centre, School of Earth and Planetary Science, Curtin University, Perth, WA, Australia.ORCID 0000-0001-8644-8903
A RajšićSpace Science and Technology Centre, School of Earth and Planetary Science, Curtin University, Perth, WA, Australia.
D BaratouxGéosciences Environnement Toulouse, University of Toulouse, CNRS and IRD, Toulouse, 31400, France.
V PayréDepartment of Astronomy and Planetary Science, Northern Arizona University, Flagstaff, AZ, USA.
L S DoucetEarth Dynamics Research Group, TIGeR, School of Earth and Planetary Sciences, Curtin University, Perth, WA, Australia.ORCID 0000-0002-7542-0582
N E TimmsSpace Science and Technology Centre, School of Earth and Planetary Science, Curtin University, Perth, WA, Australia.
R HewinsInstitut de Minéralogie, de Physique des Matériaux et de Cosmochimie (IMPMC), Muséum national d'Histoire naturelle, Sorbonne Université et CNRS, 75005, Paris, France.ORCID 0000-0003-4220-3343
G K BenedixSpace Science and Technology Centre, School of Earth and Planetary Science, Curtin University, Perth, WA, Australia.ORCID 0000-0003-0990-8878
V MalarewicUniversité Paris-Saclay, CNRS, GEOPS, 91405, Orsay, France.
K ServisSpace Science and Technology Centre, School of Earth and Planetary Science, Curtin University, Perth, WA, Australia.ORCID 0000-0002-3596-100X
P A BlandSpace Science and Technology Centre, School of Earth and Planetary Science, Curtin University, Perth, WA, Australia.
Curtin University · AUCentre National de la Recherche Scientifique · FRCommonwealth Scientific and Industrial Research Organisation · AUNorthern Arizona University · USPlanetary Science Institute · USRutgers, The State University of New Jersey · US

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

The formation and differentiation of the crust of Mars in the first tens of millions of years after its accretion can only be deciphered from incredibly limited records. The martian breccia NWA 7034 and its paired stones is one of them. This meteorite contains the oldest martian igneous material ever dated: ~4.5 Ga old. However, its source and geological context have so far remained unknown. Here, we show that the meteorite was ejected 5-10 Ma ago from the north-east of the Terra Cimmeria-Sirenum province, in the southern hemisphere of Mars. More specifically, the breccia belongs to the ejecta deposits of the Khujirt crater formed 1.5 Ga ago, and it was ejected as a result of the formation of the Karratha crater 5-10 Ma ago. Our findings demonstrate that the Terra Cimmeria-Sirenum province is a relic of the differentiated primordial martian crust, formed shortly after the accretion of the planet, and that it constitutes a unique record of early crustal processes. This province is an ideal landing site for future missions aiming to unravel the first tens of millions of years of the history of Mars and, by extension, of all terrestrial planets, including the Earth.

Indexed as

MarsMeteoroidsEarth, PlanetExtraterrestrial EnvironmentGeology

Identifiers

PMID35821210
PMCPMC9276826
OpenAlexW4285093461

What OpenQuestion holds

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LicenceCC BY
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Registered trials

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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.