(Q56874098)

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Boundary structures are formed by organic components of the Murchison carbonaceous chondrite

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title

Boundary structures are formed by organic components of the Murchison carbonaceous chondrite (English)

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main subject

carbonaceous chondrite

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David W. Deamer

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language of work or name

English

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publication date

October 1985

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published in

Nature

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volume

317

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page(s)

792-794

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issue

6040

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exact match

https://scigraph.springernature.com/pub.10.1038/317792a0

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A Nonenzymatic RNA Polymerase Model

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A theory for the origin of a self-replicating chemical system. I: Natural selection of the autogen from short, random oligomers

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Self-Organization of Molecular Systems and Evolution of the Genetic Apparatus

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Synthesis of phospholipids and membranes in prebiotic conditions

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Cyanamide mediated syntheses under plausible primitive earth conditions. V. The synthesis of phosphatidic acids

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Synthesis of phosphatidylcholine under possible primitive earth conditions

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Ufasomes are Stable Particles surrounded by Unsaturated Fatty Acid Membranes

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Liposomes from ionic, single-chain amphiphiles

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Carbon isotope composition of low molecular weight hydrocarbons and monocarboxylic acids from Murchison meteorite.

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Organic Compounds in Meteorites: They may have formed in the solar nebula, by catalytic reactions of carbon monoxide, hydrogen, and ammonia

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Quantification of monocarboxylic acids in the Murchison carbonaceous meteorite

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Evolution of self-assembly of probionts.

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Microvesicles in meteorites, a model of pre-biotic evolution

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Identifiers

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10.1038/317792A0

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1023139517

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(Q56874098)

Boundary structures are formed by organic components of the Murchison carbonaceous chondrite

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