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The Great Oxygenation Event as a consequence of ecological dynamics modulated by planetary change.

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Τίτλος: The Great Oxygenation Event as a consequence of ecological dynamics modulated by planetary change.
Συγγραφείς: Olejarz J; Department of Organismic and Evolutionary Biology, Harvard University, Cambridge, MA, USA. jasonolejarz@gmail.com., Iwasa Y; Department of Bioscience, School of Science and Technology, Kwansei Gakuin University, Sanda-shi, Hyogo, Japan., Knoll AH; Department of Organismic and Evolutionary Biology, Harvard University, Cambridge, MA, USA., Nowak MA; Department of Organismic and Evolutionary Biology, Harvard University, Cambridge, MA, USA.; Department of Mathematics, Harvard University, Cambridge, MA, USA.
Πηγή: Nature communications [Nat Commun] 2021 Jun 28; Vol. 12 (1), pp. 3985. Date of Electronic Publication: 2021 Jun 28.
Τύπος έκδοσης: Journal Article; Research Support, Non-U.S. Gov't
Γλώσσα: English
Στοιχεία περιοδικού: Publisher: Nature Pub. Group Country of Publication: England NLM ID: 101528555 Publication Model: Electronic Cited Medium: Internet ISSN: 2041-1723 (Electronic) Linking ISSN: 20411723 NLM ISO Abbreviation: Nat Commun Subsets: MEDLINE
Imprint Name(s): Original Publication: [London] : Nature Pub. Group
Ιατρικοί όροι (MeSH): Earth, Planet* , Evolution, Planetary*, Cyanobacteria/*metabolism, Atmosphere ; Oxidation-Reduction
Περίληψη: The Great Oxygenation Event (GOE), ca. 2.4 billion years ago, transformed life and environments on Earth. Its causes, however, are debated. We mathematically analyze the GOE in terms of ecological dynamics coupled with a changing Earth. Anoxygenic photosynthetic bacteria initially dominate over cyanobacteria, but their success depends on the availability of suitable electron donors that are vulnerable to oxidation. The GOE is triggered when the difference between the influxes of relevant reductants and phosphate falls below a critical value that is an increasing function of the reproductive rate of cyanobacteria. The transition can be either gradual and reversible or sudden and irreversible, depending on sources and sinks of oxygen. Increasing sources and decreasing sinks of oxygen can also trigger the GOE, but this possibility depends strongly on migration of cyanobacteria from privileged sites. Our model links ecological dynamics to planetary change, with geophysical evolution determining the relevant time scales.
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Proc Natl Acad Sci U S A. 2009 Oct 6;106(40):16925-9. (PMID: 19805080)
Proc Natl Acad Sci U S A. 2015 May 26;112(21):6562-7. (PMID: 25964326)
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Science. 2001 Aug 3;293(5531):839-43. (PMID: 11486082)
Environ Microbiol. 2017 Mar;19(3):1251-1265. (PMID: 28035767)
Nature. 2014 Feb 20;506(7488):307-15. (PMID: 24553238)
Sci Adv. 2017 Nov 22;3(11):eaao4795. (PMID: 29202032)
Sci Adv. 2017 May 17;3(5):e1603076. (PMID: 28560344)
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Am J Sci. 1998 Oct;298(8):621-72. (PMID: 11542256)
Proc Natl Acad Sci U S A. 2012 Nov 6;109(45):18300-5. (PMID: 23090989)
Proc Natl Acad Sci U S A. 2013 Oct 15;110(42):16736-41. (PMID: 24082125)
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Nat Commun. 2019 Jul 9;10(1):3026. (PMID: 31289261)
Nature. 2006 Oct 12;443(7112):683-6. (PMID: 17036001)
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Entry Date(s): Date Created: 20210629 Date Completed: 20210722 Latest Revision: 20210722
Update Code: 20260130
PubMed Central ID: PMC8238953
DOI: 10.1038/s41467-021-23286-7
PMID: 34183660
Βάση Δεδομένων: MEDLINE
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  – Url: https://dx.doi.org/doi:10.1038/s41467-021-23286-7
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  Data: The Great Oxygenation Event as a consequence of ecological dynamics modulated by planetary change.
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  Data: <searchLink fieldCode="AU" term="%22Olejarz+J%22">Olejarz J</searchLink>; Department of Organismic and Evolutionary Biology, Harvard University, Cambridge, MA, USA. jasonolejarz@gmail.com.<br /><searchLink fieldCode="AU" term="%22Iwasa+Y%22">Iwasa Y</searchLink>; Department of Bioscience, School of Science and Technology, Kwansei Gakuin University, Sanda-shi, Hyogo, Japan.<br /><searchLink fieldCode="AU" term="%22Knoll+AH%22">Knoll AH</searchLink>; Department of Organismic and Evolutionary Biology, Harvard University, Cambridge, MA, USA.<br /><searchLink fieldCode="AU" term="%22Nowak+MA%22">Nowak MA</searchLink>; Department of Organismic and Evolutionary Biology, Harvard University, Cambridge, MA, USA.; Department of Mathematics, Harvard University, Cambridge, MA, USA.
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  Data: <searchLink fieldCode="JN" term="%22101528555%22">Nature communications</searchLink> [Nat Commun] 2021 Jun 28; Vol. 12 (1), pp. 3985. <i>Date of Electronic Publication: </i>2021 Jun 28.
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  Data: <searchLink fieldCode="MM" term="%22Earth%2C+Planet%22">Earth, Planet*</searchLink> <br /><searchLink fieldCode="MM" term="%22Evolution%2C+Planetary%22">Evolution, Planetary*</searchLink><br /><searchLink fieldCode="MM" term="%22Cyanobacteria%22">Cyanobacteria</searchLink>/<searchLink fieldCode="MM" term="%22Cyanobacteria+metabolism%22">*metabolism</searchLink><br /><searchLink fieldCode="MH" term="%22Atmosphere%22">Atmosphere</searchLink> ; <searchLink fieldCode="MH" term="%22Oxidation-Reduction%22">Oxidation-Reduction</searchLink>
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  Label: Abstract
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  Data: The Great Oxygenation Event (GOE), ca. 2.4 billion years ago, transformed life and environments on Earth. Its causes, however, are debated. We mathematically analyze the GOE in terms of ecological dynamics coupled with a changing Earth. Anoxygenic photosynthetic bacteria initially dominate over cyanobacteria, but their success depends on the availability of suitable electron donors that are vulnerable to oxidation. The GOE is triggered when the difference between the influxes of relevant reductants and phosphate falls below a critical value that is an increasing function of the reproductive rate of cyanobacteria. The transition can be either gradual and reversible or sudden and irreversible, depending on sources and sinks of oxygen. Increasing sources and decreasing sinks of oxygen can also trigger the GOE, but this possibility depends strongly on migration of cyanobacteria from privileged sites. Our model links ecological dynamics to planetary change, with geophysical evolution determining the relevant time scales.
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  Label: References
  Group: RefInfo
  Data: Photosynth Res. 2006 May;88(2):109-17. (PMID: <searchLink fieldCode="PM" term="%2216453059%22">16453059)</searchLink><br />Nature. 2011 Oct 12;478(7368):229-32. (PMID: <searchLink fieldCode="PM" term="%2221993759%22">21993759)</searchLink><br />Proc Natl Acad Sci U S A. 2020 Jun 30;117(26):14756-14763. (PMID: <searchLink fieldCode="PM" term="%2232546521%22">32546521)</searchLink><br />ISME J. 2018 Feb;12(2):568-584. (PMID: <searchLink fieldCode="PM" term="%2229328062%22">29328062)</searchLink><br />Proc Natl Acad Sci U S A. 2020 Jun 16;117(24):13314-13320. (PMID: <searchLink fieldCode="PM" term="%2232482849%22">32482849)</searchLink><br />Nature. 2009 Apr 9;458(7239):750-3. (PMID: <searchLink fieldCode="PM" term="%2219360085%22">19360085)</searchLink><br />Philos Trans R Soc Lond B Biol Sci. 2008 Aug 27;363(1504):2651-64. (PMID: <searchLink fieldCode="PM" term="%2218468980%22">18468980)</searchLink><br />Science. 1992 Jan 3;255(5040):74-7. (PMID: <searchLink fieldCode="PM" term="%2211536492%22">11536492)</searchLink><br />Sci Adv. 2020 Feb 26;6(9):eaax1420. (PMID: <searchLink fieldCode="PM" term="%2232133393%22">32133393)</searchLink><br />Nature. 2002 May 9;417(6885):159-62. (PMID: <searchLink fieldCode="PM" term="%2212000956%22">12000956)</searchLink><br />Science. 2007 Sep 28;317(5846):1903-6. (PMID: <searchLink fieldCode="PM" term="%2217901330%22">17901330)</searchLink><br />Astrobiology. 2002 Spring;2(1):27-41. (PMID: <searchLink fieldCode="PM" term="%2212449853%22">12449853)</searchLink><br />Orig Life Evol Biosph. 2016 Mar;46(1):51-65. (PMID: <searchLink fieldCode="PM" term="%2226286084%22">26286084)</searchLink><br />Physiology (Bethesda). 2016 Jan;31(1):60-72. (PMID: <searchLink fieldCode="PM" term="%2226674552%22">26674552)</searchLink><br />Proc Natl Acad Sci U S A. 2009 Oct 6;106(40):16925-9. (PMID: <searchLink fieldCode="PM" term="%2219805080%22">19805080)</searchLink><br />Proc Natl Acad Sci U S A. 2015 May 26;112(21):6562-7. (PMID: <searchLink fieldCode="PM" term="%2225964326%22">25964326)</searchLink><br />Proc Natl Acad Sci U S A. 1977 May;74(5):2152-6. (PMID: <searchLink fieldCode="PM" term="%2216592398%22">16592398)</searchLink><br />Science. 2001 Aug 3;293(5531):839-43. (PMID: <searchLink fieldCode="PM" term="%2211486082%22">11486082)</searchLink><br />Environ Microbiol. 2017 Mar;19(3):1251-1265. (PMID: <searchLink fieldCode="PM" term="%2228035767%22">28035767)</searchLink><br />Nature. 2014 Feb 20;506(7488):307-15. (PMID: <searchLink fieldCode="PM" term="%2224553238%22">24553238)</searchLink><br />Sci Adv. 2017 Nov 22;3(11):eaao4795. (PMID: <searchLink fieldCode="PM" term="%2229202032%22">29202032)</searchLink><br />Sci Adv. 2017 May 17;3(5):e1603076. (PMID: <searchLink fieldCode="PM" term="%2228560344%22">28560344)</searchLink><br />Nature. 2017 Jan 19;541(7637):386-389. (PMID: <searchLink fieldCode="PM" term="%2228002400%22">28002400)</searchLink><br />Microbes Environ. 2019 Sep 25;34(3):278-292. (PMID: <searchLink fieldCode="PM" term="%2231413226%22">31413226)</searchLink><br />Am J Sci. 1998 Oct;298(8):621-72. (PMID: <searchLink fieldCode="PM" term="%2211542256%22">11542256)</searchLink><br />Proc Natl Acad Sci U S A. 2012 Nov 6;109(45):18300-5. (PMID: <searchLink fieldCode="PM" term="%2223090989%22">23090989)</searchLink><br />Proc Natl Acad Sci U S A. 2013 Oct 15;110(42):16736-41. (PMID: <searchLink fieldCode="PM" term="%2224082125%22">24082125)</searchLink><br />Environ Microbiol. 2016 Feb;18(2):325-40. (PMID: <searchLink fieldCode="PM" term="%2226549614%22">26549614)</searchLink><br />Nat Commun. 2019 Jul 9;10(1):3026. (PMID: <searchLink fieldCode="PM" term="%2231289261%22">31289261)</searchLink><br />Nature. 2006 Oct 12;443(7112):683-6. (PMID: <searchLink fieldCode="PM" term="%2217036001%22">17036001)</searchLink><br />Proc Natl Acad Sci U S A. 2017 Sep 12;114(37):E7737-E7745. (PMID: <searchLink fieldCode="PM" term="%2228808007%22">28808007)</searchLink><br />Geobiology. 2017 May;15(3):366-384. (PMID: <searchLink fieldCode="PM" term="%2228378894%22">28378894)</searchLink><br />Science. 2000 Aug 4;289(5480):756-9. (PMID: <searchLink fieldCode="PM" term="%2210926533%22">10926533)</searchLink><br />Science. 2018 Apr 20;360(6386):320-323. (PMID: <searchLink fieldCode="PM" term="%2229567810%22">29567810)</searchLink>
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