Evidence map›Paper›PMID 33446849›Full record

ArticleScientific reports2021

ExoFiT trial at the Atacama Desert (Chile): Raman detection of biomarkers by representative prototypes of the ExoMars/Raman Laser Spectrometer.

Marco Veneranda, Guillermo Lopez-Reyes, Jesus Saiz, Jose Antonio Manrique-Martinez, Aurelio Sanz-Arranz, Jesús Medina, Andoni Moral, Laura Seoane, Sergio Ibarmia, Fernando Rull

Erratum issuedAbstract read
In one paragraph

Article in Scientific reports, 2021. The graph could read no effect estimate from its abstract, so it casts no vote on the map. An erratum has been issued. Cited by 3 papers.

0numbers the graph read from it
0cells of the map it votes in
3citing 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

3 citing papers in PubMed.

  1. Review
  2. Article
  3. Review
4 · The record

Corrections and comments

5 · Who and what money

Authors and funding

10 authors.

Marco VenerandaDepartment of Condensed Matter Physics, Crystallography and Mineralogy, Univ. of Valladolid, Spain, Ave. Francisco Vallés, 8, 47151, Boecillo, Spain. marco.veneranda.87@gmail.com.
Guillermo Lopez-ReyesDepartment of Condensed Matter Physics, Crystallography and Mineralogy, Univ. of Valladolid, Spain, Ave. Francisco Vallés, 8, 47151, Boecillo, Spain.
Jesus SaizDepartment of Condensed Matter Physics, Crystallography and Mineralogy, Univ. of Valladolid, Spain, Ave. Francisco Vallés, 8, 47151, Boecillo, Spain.
Jose Antonio Manrique-MartinezDepartment of Condensed Matter Physics, Crystallography and Mineralogy, Univ. of Valladolid, Spain, Ave. Francisco Vallés, 8, 47151, Boecillo, Spain.
Aurelio Sanz-ArranzDepartment of Condensed Matter Physics, Crystallography and Mineralogy, Univ. of Valladolid, Spain, Ave. Francisco Vallés, 8, 47151, Boecillo, Spain.
Jesús MedinaDepartment of Condensed Matter Physics, Crystallography and Mineralogy, Univ. of Valladolid, Spain, Ave. Francisco Vallés, 8, 47151, Boecillo, Spain.
Andoni MoralNational Institute for Aerospace Technology (INTA), Torrejón de Ardoz, Spain.
Laura SeoaneNational Institute for Aerospace Technology (INTA), Torrejón de Ardoz, Spain.
Sergio IbarmiaNational Institute for Aerospace Technology (INTA), Torrejón de Ardoz, Spain.
Fernando RullDepartment of Condensed Matter Physics, Crystallography and Mineralogy, Univ. of Valladolid, Spain, Ave. Francisco Vallés, 8, 47151, Boecillo, Spain.

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

In this work, the analytical research performed by the Raman Laser Spectrometer (RLS) team during the ExoFiT trial is presented. During this test, an emulator of the Rosalind Franklin rover was remotely operated at the Atacama Desert in a Mars-like sequence of scientific operations that ended with the collection and the analysis of two drilled cores. The in-situ Raman characterization of the samples was performed through a portable technology demonstrator of RLS (RAD1 system). The results were later complemented in the laboratory using a bench top RLS operation simulator and a X-Ray diffractometer (XRD). By simulating the operational and analytical constraints of the ExoMars mission, the two RLS representative instruments effectively disclosed the mineralogical composition of the drilled cores (k-feldspar, plagioclase, quartz, muscovite and rutile as main components), reaching the detection of minor phases (e.g., additional phyllosilicate and calcite) whose concentration was below the detection limit of XRD. Furthermore, Raman systems detected many organic functional groups (-C≡N, -NH

Identifiers

PMID33446849
PMCPMC7809400

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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.