Evidence map›Paper›PMID 40556941›Full record

ArticleACS earth & space chemistry2025

Noble Gases in Archean Barites: Precise Determination of the Isotopic Fractionation of Atmospheric Xenon 3.48 Ga Ago.

Guillaume Avice, Helge Mißbach-Karmrodt, Félix Vayrac, Joachim Reitner

Abstract read
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Article in ACS earth & space chemistry, 2025. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 2 papers.

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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

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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

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3 · Its place in the literature

Who cites it

2 citing papers in PubMed.

  1. Article
  2. Fluid inclusions: tiny windows into global paleo-environments.Communications earth & environment · 2025
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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

4 authors.

Guillaume AviceUniversité Paris Cité, Institut de Physique du Globe de Paris, CNRS, F-75005 Paris, France.ORCID https://orcid.org/0000-0003-0962-0049
Helge Mißbach-KarmrodtGeobiology Working Group, University of Cologne, DE 50923 Cologne, Nordrhein-Westfalen, Germany.ORCID https://orcid.org/0000-0003-4053-1204
Félix VayracUniversité Paris Cité, Institut de Physique du Globe de Paris, CNRS, F-75005 Paris, France.
Joachim ReitnerGeobiology, University of Göttingen, DE 37073 Göttingen, Niedersachsen, Germany.

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

Following the evolution of the composition of the atmosphere informs on the entire geological evolution of our planet. The discovery that Archean atmospheric xenon was isotopically fractionated compared to modern atmospheric xenon paved the way for using this noble gas as a tracer of hydrogen escape on the primitive Earth. The curve of the evolution of the isotopic composition of atmospheric xenon remains, however, poorly defined. Recent studies proposed that the evolution was discontinuous with brief episodes of escape and fractionation of xenon separated by up to several 100 Ma long pauses. Similarly, some major unknowns remain regarding the progressive depletion of xenon in the atmosphere due to the proposed escape mechanism. In this study, we report the noble gas elemental ratios and isotopic compositions of noble gases released from a ca. 3.48 Ga old barite sample from the Dresser Formation (North Pole, Australia) by stepwise crushing in high vacuum. All samples released xenon enriched in light isotopes relative to heavy isotopes compared to modern atmospheric xenon but with various degrees of isotopic fractionation. Krypton is enriched in heavy isotopes relative to light isotopes in some crushed samples. After correction for Kr and Xe loss, results show that 3.48 Ga ago atmospheric xenon was fractionated by -19.1 ± 1.8‰ per atomic mass unit (u

Indexed as

Archeanatmospherefluid inclusionsgeochemistryhabitabilitynoble gases

Identifiers

PMID40556941
PMCPMC12183778

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