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dc.contributor.authorKee, Terence
dc.contributor.authorBryant, David
dc.contributor.authorHerschy, Barry
dc.contributor.authorMarriott, Katie
dc.contributor.authorCosgrove, Nichola
dc.contributor.authorPasek, Matthew
dc.contributor.authorAtlas, Zachary
dc.contributor.authorCousins, Claire Rachel
dc.date.accessioned2016-05-09T10:30:05Z
dc.date.available2016-05-09T10:30:05Z
dc.date.issued2013-07-19
dc.identifier.citationKee , T , Bryant , D , Herschy , B , Marriott , K , Cosgrove , N , Pasek , M , Atlas , Z & Cousins , C R 2013 , ' Phosphate activation via reduced oxidation state phosphorus (P). Mild routes to condensed-P energy currency molecules ' , Life , vol. 3 , no. 3 . https://doi.org/10.3390/life3030386en
dc.identifier.issn2075-1729
dc.identifier.otherPURE: 206022451
dc.identifier.otherPURE UUID: 05387173-730e-412c-a0ea-11c7f08723d7
dc.identifier.otherScopus: 84894315186
dc.identifier.otherORCID: /0000-0002-3954-8079/work/60196594
dc.identifier.urihttp://hdl.handle.net/10023/8757
dc.descriptionThe authors thank the EPSRC (grant EP/F042558/1), the Leverhulme Trust (grant F07112AA), the STFC and the UK Space Agency (Aurora Fellowship to TPK).en
dc.description.abstractThe emergence of mechanisms for phosphorylating organic and inorganic molecules is a key step en route to the earliest living systems. At the heart of all contemporary biochemical systems reside reactive phosphorus (P) molecules (such as adenosine triphosphate, ATP) as energy currency molecules to drive endergonic metabolic processes and it has been proposed that a predecessor of such molecules could have been pyrophosphate [P2O74−; PPi(V)]. Arguably the most geologically plausible route to PPi(V) is dehydration of orthophosphate, Pi(V), normally a highly endergonic process in the absence of mechanisms for activating Pi(V). One possible solution to this problem recognizes the presence of reactive-P containing mineral phases, such as schreibersite [(Fe,Ni)3P] within meteorites whose abundance on the early Earth would likely have been significant during a putative Hadean-Archean heavy bombardment. Here, we propose that the reduced oxidation state P-oxyacid, H-phosphite [HPO32−; Pi(III)] could have activated Pi(V) towards condensation via the intermediacy of the condensed oxyacid pyrophosphite [H2P2O52−; PPi(III)]. We provide geologically plausible provenance for PPi(III) along with evidence of its ability to activate Pi(V) towards PPi(V) formation under mild conditions (80 °C) in water.
dc.language.isoeng
dc.relation.ispartofLifeen
dc.rights© 2013 by the authors; licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution license (http://creativecommons.org/licenses/by/3.0/).en
dc.subjectPhosphorusen
dc.subjectPrebiotic chemistryen
dc.subjectOrigin of lifeen
dc.subjectMeteoritesen
dc.subjectQH301 Biologyen
dc.subjectGE Environmental Sciencesen
dc.subject.lccQH301en
dc.subject.lccGEen
dc.titlePhosphate activation via reduced oxidation state phosphorus (P). Mild routes to condensed-P energy currency moleculesen
dc.typeJournal articleen
dc.description.versionPublisher PDFen
dc.contributor.institutionUniversity of St Andrews.Earth and Environmental Sciencesen
dc.identifier.doihttps://doi.org/10.3390/life3030386
dc.description.statusPeer revieweden


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