Evidence map›Paper›PMID 11536619›Full record

ReviewOrigins of life and evolution of the biosphere : the journal of the International Society for the Study of the Origin of Life1989

Estimates of the maximum time required to originate life.

V R Oberbeck, G Fogleman, New Collective Author

Abstract readReview
PubMed Publisher
In one paragraph

Review in Origins of life and evolution of the biosphere : the journal of the International Society for the Study of the Origin of Life, 1989. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 9 papers.

0numbers the graph read from it
0cells of the map it votes in
9citing 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

9 citing papers in PubMed.

  1. The Astrobiology Primer v2.0.Astrobiology · 2016
    Review
  2. A review of conditions affecting the radiolysis due to 40K on nucleic acid bases and their derivatives adsorbed on clay minerals: implications in prebiotic chemistry.Origins of life and evolution of the biosphere : the journal of the International Society for the Study of the Origin of Life · 1996
    Review
  3. Origins of life: a comparison of theories and application to Mars.Origins of life and evolution of the biosphere : the journal of the International Society for the Study of the Origin of Life · 1996
    Review
  4. Chirality and life.Origins of life and evolution of the biosphere : the journal of the International Society for the Study of the Origin of Life · 1995
    Article
  5. Article
  6. Comets and the formation of biochemical compounds on the primitive Earth--a review.Origins of life and evolution of the biosphere : the journal of the International Society for the Study of the Origin of Life · 1992
    Review
  7. The origin and amplification of biomolecular chirality.Origins of life and evolution of the biosphere : the journal of the International Society for the Study of the Origin of Life · 1991
    Review
  8. Prebiotic chemistry in clouds.Journal of molecular evolution · 1991
    Article
  9. Impact constraints on the environment for chemical evolution and the continuity of life.Origins of life and evolution of the biosphere : the journal of the International Society for the Study of the Origin of Life · 1990
    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

3 authors.

V R OberbeckNASA Ames Research Center, Moffett Field, CA 94035, USA.
G Fogleman
New Collective Author

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

Fossils of the oldest microorganisms exist in 3.5 billion year old rocks and there is indirect evidence that life may have existed 3.8 billion years ago (3.8 Ga). Impacts able to destroy life or interrupt prebiotic chemistry may have occurred after 3.5 Ga. If large impactors vaporized the oceans, sterilized the planets, and interfered with the origination of life, life must have originated in the time interval between these impacts which increased with geologic time. Therefore, the maximum time required for the origination of life is the time that occurred between sterilizing impacts just before 3.8 Ga or 3.5 Ga, depending upon when life first appeared on Earth. If life first originated 3.5 Ga, and impacts with kinetic energies between 2 x 10(34) and 2 x 10(35) were able to vaporize the oceans, using the most probable impact flux, we find that the maximum time required to originate life would have been 67 to 133 million years (My). If life first originated 3.8 Ga, the maximum time to originate life was 2.5 to 11 My. Using a more conservative estimate for the flux of impacting objects before 3.8 Ga, we find a maximum time of 25 My for the same range of impactor kinetic energies. The impact model suggest that it is possible that life may have originated more than once.

Indexed as

Earth, PlanetEvolution, ChemicalOrigin of LifeFossilsMeteoroidsModels, TheoreticalTime FactorsNASA Center ARCNASA Discipline Exobiology

Identifiers

PMID11536619

What OpenQuestion holds

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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.