Evidence map›Paper›PMID 7708385›Full record

ArticleOrigins of life and evolution of the biosphere : the journal of the International Society for the Study of the Origin of Life1995

The effects of heavy meteorite bombardment on the early evolution--the emergence of the three domains of life.

M Gogarten-Boekels, E Hilario, J P Gogarten

Abstract read
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In one paragraph

Article in Origins of life and evolution of the biosphere : the journal of the International Society for the Study of the Origin of Life, 1995. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 17 papers.

0numbers the graph read from it
0cells of the map it votes in
17citing 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

17 citing papers in PubMed.

  1. Review
  2. Article
  3. Review
  4. Hidden Concepts in the History and Philosophy of Origins-of-Life Studies: a Workshop Report.Origins of life and evolution of the biosphere : the journal of the International Society for the Study of the Origin of Life · 2019
    Review
  5. Article
  6. Article
  7. Horizontal gene transfer from extinct and extant lineages: biological innovation and the coral of life.Philosophical transactions of the Royal Society of London. Series B, Biological sciences · 2009
    Review
  8. Article
  9. Article
  10. Article
  11. Initiation of clement surface conditions on the earliest Earth.Proceedings of the National Academy of Sciences of the United States of America · 2001
    Article
  12. Review
  13. The stability of the RNA bases: implications for the origin of life.Proceedings of the National Academy of Sciences of the United States of America · 1998
    Article
  14. Biochemical evolution. I. Polymerization On internal, organophilic silica surfaces of dealuminated zeolites and feldspars.Proceedings of the National Academy of Sciences of the United States of America · 1998
    Article
  15. The first living systems: a bioenergetic perspective.Microbiology and molecular biology reviews : MMBR · 1997
    Review
  16. The origin of life--did it occur at high temperatures?Journal of molecular evolution · 1995
    Article
  17. 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.

M Gogarten-BoekelsDept. Molecular and Cell Biology, University of Connecticut, Storrs 06269-3044.
E Hilario
J P Gogarten

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

A characteristic of many molecular phylogenies is that the three domains of life (Bacteria, Archaea, Eucarya) are clearly separated from each other. The analyses of ancient duplicated genes suggest that the last common ancestor of all presently known life forms already had been a sophisticated cellular prokaryote. These findings are in conflict with theories that have been proposed to explain the absence of deep branching lineages. In this paper we propose an alternative scenario, namely, a large meteorite impact that wiped out almost all life forms present on the early Earth. Following this nearly complete frustation of life on Earth, two surviving extreme thermophilic species gave rise to the now existing major groups of living organisms, the Bacteria and Archaea. [The latter also contributed the major portion to the nucleo-cytoplasmic component of the Eucarya]. An exact calibration of the molecular record with regard to time is not yet possible. The emergence of Eucarya in fossil and molecular records suggests that the proposed late impact should have occurred before 2100 million years before present (BP). If the 3500 million year old microfossils [Schopf, J. W. 1993: Science 260: 640-646] are interpreted as representatives of present day existing groups of bacteria (i.e., as cyanobacteria), then the impact is dated to around 3700 million years BP. The analysis of molecular sequences suggests that the separation between the Eucarya and the two prokaryotic domains is less deep then the separation between Bacteria and Archaea. The fundamental cell biological differences between Archaea and Eucarya were obtained over a comparatively short evolutionary distance (as measured in number of substitution events in biological macromolecules). Our interpretation of the molecular record suggests that life emerged early in Earth's history even before the time of the heavy bombardment was over. Early life forms already had colonized extreme habitats which allowed at least two prokaryotic species to survive a late nearly ocean boiling impact. The distribution of ecotypes on the rooted universal tree of life should not be interpreted as evidence that life originated in extremely hot environments.

Indexed as

Eukaryotic CellsPhylogenyProkaryotic CellsSolar SystemAmino Acid SequenceArchaeaBacteriaFossilsMolecular Sequence Data

Identifiers

PMID7708385

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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.