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dc.contributor.authorBuddıng, Edwin
dc.contributor.authorAkı, Cüneyt
dc.contributor.authorDemircan, Osman
dc.contributor.authorGündüz, Bülent
dc.contributor.authorGündüz, Güngör
dc.contributor.authorÖzel, Mehmet Emin
dc.date.accessioned02.07.201910:49:13
dc.date.accessioned2019-07-02T19:36:26Z
dc.date.available02.07.201910:49:13
dc.date.available2019-07-02T19:36:26Z
dc.date.issued2012
dc.identifier.issn1300-0101
dc.identifier.urihttps://hdl.handle.net/20.500.12507/72
dc.description.abstractWe adopt that the large residual chemical potential energy (CPE) among reagents of the biosphere constitutes the key physical problem posed by life. We associate the formation of this CPE with the nearresonant behaviour of a two-stage ‘A-B’ molecular process that behaves as a self-sustaining parametric oscillator. Under suitable conditions, such an oscillator generates CPE when forced by a periodic (daily) insolation. The net growth factor required to explain the current mean excess of biospheric CPE is $\sim5x10^{-12}d^{-1}$. This aligns with the mean exponential coefficient of secular oxygen generation in the terrestrial atmosphere. It is also consistent with a feasible scale of oxygen production in certain prebiotic natural photosynthesis scenarios, that can be candidates for the initial A subprocess on the Earth. We schematize initial evolutionary development of the A-B process, including the important role of the intermediate AB compound that provides negative feedback. Supportive C-type molecules also develop as a by-product. The diurnally related distribution of $H_2O_2$ on Mars may illustrate a comparable proto-biospheric scheme, and there may be analogous processes on Jupiter. The exponential growth in the lengths of terrestrial nucleotide chain molecules also supports its validity, as does the corresponding growth in measures of cellular complexity. We compare the scenario’s implications with biological evidence on the possible co-evolution of blue-light photoreception and circadian timing in Archean photoautotrophs. We consider how a surviving level of cellular organization of circadian rhythmicity, from ancient through to modern times, may be interpreted along these lines, comparing our model with a previously published, comparable, biochemical one.en_US
dc.description.abstractWe adopt that the large residual chemical potential energy (CPE) among reagents of the biosphere constitutes the key physical problem posed by life. We associate the formation of this CPE with the nearresonant behaviour of a two-stage ‘A-B’ molecular process that behaves as a self-sustaining parametric oscillator. Under suitable conditions, such an oscillator generates CPE when forced by a periodic (daily) insolation. The net growth factor required to explain the current mean excess of biospheric CPE is $\sim5x10^{-12}d^{-1}$. This aligns with the mean exponential coefficient of secular oxygen generation in the terrestrial atmosphere. It is also consistent with a feasible scale of oxygen production in certain prebiotic natural photosynthesis scenarios, that can be candidates for the initial A subprocess on the Earth. We schematize initial evolutionary development of the A-B process, including the important role of the intermediate AB compound that provides negative feedback. Supportive C-type molecules also develop as a by-product. The diurnally related distribution of $H_2O_2$ on Mars may illustrate a comparable proto-biospheric scheme, and there may be analogous processes on Jupiter. The exponential growth in the lengths of terrestrial nucleotide chain molecules also supports its validity, as does the corresponding growth in measures of cellular complexity. We compare the scenario’s implications with biological evidence on the possible co-evolution of blue-light photoreception and circadian timing in Archean photoautotrophs. We consider how a surviving level of cellular organization of circadian rhythmicity, from ancient through to modern times, may be interpreted along these lines, comparing our model with a previously published, comparable, biochemical one.en_US
dc.language.isoengen_US
dc.rightsinfo:eu-repo/semantics/openAccessen_US
dc.subjectFiziken_US
dc.subjectUygulamalıen_US
dc.titleNear-resonant diurnal reactions: a physical model applicable to origin of life processesen_US
dc.typearticleen_US
dc.relation.journalTurkish Journal of Physicsen_US
dc.contributor.departmentFen Edebiyat Fakültesien_US
dc.identifier.volume36en_US
dc.identifier.issue3en_US
dc.identifier.startpage473en_US
dc.identifier.endpage493en_US
dc.relation.publicationcategoryMakale - Ulusal Hakemli Dergi - Kurum Öğretim Elemanıen_US


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