Evidence map›Paper›PMID 36007008›Full record

ArticleScience advances2022

Ground penetrating radar observations of subsurface structures in the floor of Jezero crater, Mars.

Svein-Erik Hamran, David A Paige, Abigail Allwood, Hans E F Amundsen, Tor Berger, Sverre Brovoll, Lynn Carter, Titus M Casademont, Leif Damsgård, Henning Dypvik and 10 more

Abstract read
In one paragraph

Article in Science advances, 2022. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 8 papers.

0numbers the graph read from it
0cells of the map it votes in
8citing 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

8 citing papers in PubMed.

  1. Article
  2. Article
  3. Ancient ocean coastal deposits imaged on Mars.Proceedings of the National Academy of Sciences of the United States of America · 2025
    Article
  4. Article
  5. Article
  6. Article
  7. Article
  8. 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

20 authors.

Svein-Erik HamranUniversity of Oslo, Kjeller and Oslo, Norway.ORCID 0000-0002-1078-449X
David A PaigeUniversity of California, Los Angeles, Los Angeles, CA, USA.
Abigail AllwoodJet Propulsion Laboratory, California Institute of Technology, Pasadena, CA, USA.
Hans E F AmundsenVestfonna Geophysical, Trondheim, Norway.
Tor BergerUniversity of Oslo, Kjeller and Oslo, Norway.
Sverre BrovollUniversity of Oslo, Kjeller and Oslo, Norway.
Lynn CarterUniversity of Arizona, Tucson, AZ, USA.
Titus M CasademontUniversity of Oslo, Kjeller and Oslo, Norway.ORCID 0000-0002-5897-9659
Leif DamsgårdUniversity of Oslo, Kjeller and Oslo, Norway.ORCID 0000-0002-4601-8068
Henning DypvikUniversity of Oslo, Kjeller and Oslo, Norway.ORCID 0000-0003-0488-3763
Sigurd EideUniversity of Oslo, Kjeller and Oslo, Norway.ORCID 0000-0003-0061-1867
Alberto G FairénCentro de Astrobiología (CSIC-INTA), Madrid, Spain.ORCID 0000-0002-2938-6010
Rebecca GhentPlanetary Science Institute, Tucson, AZ, USA.ORCID 0000-0002-3173-6630
Jack KohlerNorwegian Polar Institute, Tromsø, Norway.ORCID 0000-0003-1963-054X
Michael T MellonCornell University, Ithaca, NY, USA.ORCID 0000-0001-7973-9585
Daniel C NunesJet Propulsion Laboratory, California Institute of Technology, Pasadena, CA, USA.ORCID 0000-0002-0937-7176
Dirk PlettemeierTechnische Universität Dresden, Dresden, Germany.ORCID 0000-0001-8229-3932
Patrick RussellUniversity of California, Los Angeles, Los Angeles, CA, USA.
Matt SieglerPlanetary Science Institute, Tucson, AZ, USA.ORCID 0000-0002-7940-3931
Mats Jørgen ØyanUniversity of Oslo, Kjeller and Oslo, Norway.

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

The Radar Imager for Mars Subsurface Experiment instrument has conducted the first rover-mounted ground-penetrating radar survey of the Martian subsurface. A continuous radar image acquired over the Perseverance rover's initial ~3-kilometer traverse reveals electromagnetic properties and bedrock stratigraphy of the Jezero crater floor to depths of ~15 meters below the surface. The radar image reveals the presence of ubiquitous strongly reflecting layered sequences that dip downward at angles of up to 15 degrees from horizontal in directions normal to the curvilinear boundary of and away from the exposed section of the Séitah formation. The observed slopes, thicknesses, and internal morphology of the inclined stratigraphic sections can be interpreted either as magmatic layering formed in a differentiated igneous body or as sedimentary layering commonly formed in aqueous environments on Earth. The discovery of buried structures on the Jezero crater floor is potentially compatible with a history of igneous activity and a history of multiple aqueous episodes.

Identifiers

PMID36007008
PMCPMC9410267

What OpenQuestion holds

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LicenceCC BY-NC
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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.