This is a list of primary-sourced content which has been removed from the Abiogenesis article. Generally, this means that the significance of these statements are unclear due to a lack of mention in reliable secondary or tertiary sources. The statements are being placed here in case their significance is established in the future.
Early conditions
editThe earliest life on Earth
edit- Lazcano and Miller (1994) suggest that the rapidity of the evolution of life is dictated by the rate of recirculating water through mid-ocean submarine vents. Since complete recirculation takes 10 million years, any organic compounds produced by then would be altered or destroyed by temperatures exceeding 300 °C (572 °F). They estimate that the development of a 100 kilobase genome of a DNA/protein primitive heterotroph into a 7000 gene filamentous cyanobacterium would have required only 7 Ma.[1]
Current models
edit- In vitro evolution of pre-biological polymer catalysts has been demonstrated in 2000 by Hiroaki Suga and supports, he suggests, the RNA world model of abiogenesis.[2]
- M. Sumper and R. Luce of Eigen's laboratory accidentally discovered that a mixture containing no RNA at all but only RNA bases and Q-Beta Replicase can, under the right conditions, spontaneously generate self-replicating RNA which evolves into a form similar to Spiegelman's Monster.[3]
Origin of organic molecules
editChemical synthesis
edit- Research by Christof Biebricher showed the formation of RNA molecules 400 bases long under freezing conditions using an RNA template, a single-strand chain of RNA that guides the formation of a new strand of RNA. As that new RNA strand grows, it adheres to the template.[4]
- Martin and Russell showed that physical compartmentation by cell membranes from the environment and self-organization of self-contained redox reactions are the most conserved attributes of living things, and they argue therefore that inorganic matter with such attributes would be life's most likely last common ancestor.[5]
Homochirality
edit- Noyes showed that beta decay caused the breakdown of D-leucine, in a racemic mixture, and that the presence of 14C, present in larger amounts in organic chemicals in the early Earth environment, could have been the cause.[6]
RNA world
editRNA synthesis and replication
editOrigin of metabolism
editIron-sulfur world
edit- Harold J. Morowitz concludes that given sufficient concentrations of ingredients, the Krebs cycle will "spin" of its own, as the concentration of each intermediate rises, it tends to convert into the next intermediate spontaneously. It thus appears to be in origin, not a creation of the genes, but the product of thermodynamics and chemistry alone.[8]
Deep sea vent hypothesis
edit- In 2013 Ignatov and Mosin made an analysis of a jellyfish. This analysis also showed that life may have predominantly originated in hot mineral water.[9]
- In 2011 Marie-Laure Pons explored the oldest rocks on the planet containing serpentine. French scientists demonstrated that water was rich in carbonates.[10]
Thermosynthesis
edit- It is assumed RNA sequences were selected among the randomly synthesized RNAs by the relative speed and efficiency increase of "first protein" synthesis, for instance by the creation of RNA that functioned as messenger RNA,[11] transfer RNA[12] and ribosomal RNA, or, even more generally, all the components of the RNA world were also generated and selected. This accounts for the origin of the genetic machinery.
References
edit- ^ Lazcano, A.; Miller, S. L. (1994). "How long did it take for life to begin and evolve to cyanobacteria?". Journal of Molecular Evolution. 39 (6): 546–54. doi:10.1007/BF00160399. PMID 11536653.
- ^ Suga, Hiroaki et al. (2000), "Ribozyme-catalyzed tRNA aminoacylation" (Nature Structural Biology 7, 28 - 33)
- ^ Sumper, M; Luce, R. (1975). "Evidence for de novo production of self-replicating and environmentally adapted RNA structures by bacteriophage Qbeta replicase". Proceedings of the National Academy of Sciences. 72 (1): 162–166. Bibcode:1975PNAS...72..162S. doi:10.1073/pnas.72.1.162. PMC 432262. PMID 1054493.
- ^ Trinks, Hauke; Schröder, Wolfgang; Biebricher, Christof (October 2005). "Ice And The Origin Of Life". Origins of Life and Evolution of Biospheres. 35 (5): 429–45. Bibcode:2005OLEB...35..429T. doi:10.1007/s11084-005-5009-1. PMID 16231207. Retrieved 2008-02-11.
- ^ Martin, William; Russell, Michael J. (2003). "On the origins of cells: a hypothesis for the evolutionary transitions from abiotic geochemistry to chemoautotrophic prokaryotes, and from prokaryotes to nucleated cells". Philosophical Transactions of the Royal Society B. 358 (1429): 59–83, discussion 83–5. doi:10.1098/rstb.2002.1183. PMC 1693102. PMID 12594918.
- ^ Noyes, HP; Bonner, WA; Tomlin, JA (April 1977). "On the origin of biological chirality via natural beta-decay". Orig. Life. 8 (1): 21–3. Bibcode:1977OrLi....8...21N. doi:10.1007/BF00930935. PMID 896189.
- ^ Levy, Matthew; Miller, Stanley L. (1998). "The stability of the RNA bases: Implications for the origin of life". PNAS. 95 (14): 7933–8. Bibcode:1998PNAS...95.7933L. doi:10.1073/pnas.95.14.7933. PMC 20907. PMID 9653118.
- ^ Smith E & Morowitz, H. (2004) "Universality in Intermediary Metabolism" (Proceedings of the Nat. Academy of Sciences 101:13168-73)
- ^ Ignatov, I., Mosin, O. V. (2013) Modeling of Possible Processes for Origin of Life and Living Matter in Hot Mineral and Seawater with Deuterium, Journal of Environment and Earth Science, 3(14): 103-118.
- ^ Pons, M.L., Quitte, G., Fujii, T., et al. (2011) Early archean serpentine mud volcanoes at Isua, Greenland, as a niche for early life, PNAS, 108(43):17639–17643.
- ^ Muller, A.W.J. (2005). "Thermosynthesis as energy source for the RNA world: a model for the bioenergetics of the origin of life". Biosystems. 82 (1): 93–102. doi:10.1016/j.biosystems.2005.06.003. PMID 16024164.
- ^ Sun, F.J.; Caetano-Anolles, G. (2008). "The origin and evolution of tRNA inferred from phylogenetic analysis of structure". Journal of Molecular Evolution. 66 (1): 21–35. doi:10.1007/s00239-007-9050-8. PMID 18058157.