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.
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.
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Who cites it
17 citing papers in PubMed.
- The Last Universal Common Ancestor of Ribosome-Encoding Organisms: Portrait of LUCA.Journal of molecular evolution · 2024Review
- Macrobiont: Cradle for the Origin of Life and Creation of a Biosphere.Life (Basel, Switzerland) · 2020Article
- Multidomain ribosomal protein trees and the planctobacterial origin of neomura (eukaryotes, archaebacteria).Protoplasma · 2020Review
- 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 · 2019Review
- Single-molecule paleoenzymology probes the chemistry of resurrected enzymes.Nature structural & molecular biology · 2011Article
- On the origin of life in the zinc world. 2. Validation of the hypothesis on the photosynthesizing zinc sulfide edifices as cradles of life on Earth.Biology direct · 2009Article
- 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 · 2009Review
- Article
- Signature of a primitive genetic code in ancient protein lineages.Journal of molecular evolution · 2007Article
- Protein disulfide oxidoreductases and the evolution of thermophily: was the last common ancestor a heat-loving microbe?Journal of molecular evolution · 2007Article
- Initiation of clement surface conditions on the earliest Earth.Proceedings of the National Academy of Sciences of the United States of America · 2001Article
- Protein phylogenies and signature sequences: A reappraisal of evolutionary relationships among archaebacteria, eubacteria, and eukaryotes.Microbiology and molecular biology reviews : MMBR · 1998Review
- 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 · 1998Article
- 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 · 1998Article
- The first living systems: a bioenergetic perspective.Microbiology and molecular biology reviews : MMBR · 1997Review
- The origin of life--did it occur at high temperatures?Journal of molecular evolution · 1995Article
- How long did it take for life to begin and evolve to cyanobacteria?Journal of molecular evolution · 1994Article
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3 authors.
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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.
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