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dc.contributor.authorLyons, Timothy W.
dc.contributor.authorFike, David A.
dc.contributor.authorZerkle, Aubrey Lea
dc.date.accessioned2016-12-01T00:32:59Z
dc.date.available2016-12-01T00:32:59Z
dc.date.issued2015-12-01
dc.identifier.citationLyons , T W , Fike , D A & Zerkle , A L 2015 , ' Emerging biogeochemical views of Earth's ancient microbial worlds ' Elements , vol. 11 , no. 6 , pp. 415-421 . https://doi.org/10.2113/gselements.11.6.415en
dc.identifier.issn1811-5209
dc.identifier.otherPURE: 231537014
dc.identifier.otherPURE UUID: c8a28493-3ba0-40fa-99a7-9f007dfa4a8c
dc.identifier.otherScopus: 84949206456
dc.identifier.otherORCID: /0000-0003-2324-1619/work/60427940
dc.identifier.urihttp://hdl.handle.net/10023/9904
dc.descriptionThis work was supported by the NASA Astrobiology Institute under Cooperative Agreement No. NNA15BB03A issued through the Science Mission Directorate (TWL), a Natural Environment Research Council Fellowship (NE/H016805/2) (AZ), and National Science Foundation grants (EAR-0951509, OCE-1061476, EAR-1124389, and OCE-1155346) and a Packard Fellowship (DAF).en
dc.description.abstractMicrobial processes dominate geochemical cycles at and near the Earth’s surface today. Their role was even greater in the past, with microbes being the dominant life form for the first 90% of Earth’s history. Most of their metabolic pathways originated billions of years ago as both causes and effects of environmental changes of the highest order, such as the first accumulation of oxygen in the oceans and atmosphere. Microbial processes leave behind diverse geochemical fingerprints that can remain intact for billions of years. These rock-bound signatures are now steering our understanding of how life coevolved with the environments on early Earth and are guiding our search for life elsewhere in the universe.
dc.language.isoeng
dc.relation.ispartofElementsen
dc.rights© 2015 by the Mineralogical Society of America. This work is made available online in accordance with the publisher’s policies. This is the author created, accepted version manuscript following peer review and may differ slightly from the final published version. The final published version of this work is available at https://dx.doi.org/10.2113/gselements.11.6.41en
dc.subjectEarly Earthen
dc.subjectMicrobiologyen
dc.subjectEnvironmental changeen
dc.subjectBiogeochemical cyclesen
dc.subjectBiosignaturesen
dc.subjectIsotopesen
dc.subjectAstrobiologyen
dc.subjectQH301 Biologyen
dc.subjectQR Microbiologyen
dc.subjectGE Environmental Sciencesen
dc.subjectT-NDASen
dc.subject.lccQH301en
dc.subject.lccQRen
dc.subject.lccGEen
dc.titleEmerging biogeochemical views of Earth's ancient microbial worldsen
dc.typeJournal articleen
dc.description.versionPostprinten
dc.contributor.institutionUniversity of St Andrews.Earth and Environmental Sciencesen
dc.contributor.institutionUniversity of St Andrews.St Andrews Isotope Geochemistryen
dc.identifier.doihttps://doi.org/10.2113/gselements.11.6.415
dc.description.statusPeer revieweden
dc.date.embargoedUntil2016-11-30


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