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1 The ~4 billion year co-evolution of Earth and its Biosphere Instructor: Carl B. Pilcher OLLI at SSU/Oakmont Life in the Universe: The Science of Astrobiology Week 3—January 28, 2016

The ~4 billion year co-evolution of Earth and its Biosphere · History of Oxygen Time before Present (billion yrs)! P O 2 (tm)! 1! 0.1! 0.01! 0.001! 0.0001! 0.00001! 4.5! 4! 3.5!

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Page 1: The ~4 billion year co-evolution of Earth and its Biosphere · History of Oxygen Time before Present (billion yrs)! P O 2 (tm)! 1! 0.1! 0.01! 0.001! 0.0001! 0.00001! 4.5! 4! 3.5!

1

The ~4 billion year co-evolution of Earth

and its Biosphere

Instructor: Carl B. Pilcher

OLLI at SSU/Oakmont

Life in the Universe: The Science of Astrobiology

Week 3—January 28, 2016

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SimonWilde,Cur/nUniv.,AustraliaandJohnValley,UniversityofWisconsin,Madison

TheJackHills,

WesternAustralia

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Evidence from >4 BY-old zircons

Cavosie et al. 2005

Imaging U-Pb age

Oxygen isotopes

[Li] & Li isotopes

REEs, Ti Mineral inclusions

Slide courtesy John Valley

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Cool Early Earth?

5

Earth4.3BY

•  4.4 BY Protocontinental Crust •  >4.3 BY End of Hadean •  >3.5 BY Life >4.3 BY?

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TheFaintYoungSunParadox

•  Modelsofstellarevolu/onandobserva/onsoflargenumbersofstarsindicatethatstarsgetbrighterastheyage.

•  Thesunhadonly~75%ofitscurrentluminosity(energyoutput)around4billionyearsago.

•  YettherewasapparentlyliquidwateronEarthatthat/me,implyingasurfacetemperatureroughlyequaltoorgreaterthanthesurfacetemperaturetoday.

•  Howcouldthishavebeenthecase?

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ManyPossibleExplana/onsfortheFaintYoungSunParadox

•  Moreatmosphericcarbondioxide(CO2;greenhousegas)•  Moreatmosphericmethane(CH4;greenhousegas)•  Moreatmosphericammonia(NH3;greenhousegas;butreadilydestroyedbyultravioletradia/on)

•  Organichazeshieldingatmospherefromradia/on,enablingNH3toincrease

•  Atmospherichydrogen(H2)andnitrogen(N2)togetheringreaterabundance(actlikeagreenhousegas)

•  Fewerclouds,allowingEarthtoabsorbmoresunlight(effectisn’tlargeenough)

•  Sunwasn’treallythatmuchfainter

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Twopossibleearlymetabolisms

H2+S0 H2Ssulfurrespira/onhydrogensulfurhydrogensulfide

4H2+CO2CH4+2H2Omethanogenesishydrogencarbondioxidemethanewater

Didlifehelpstabilizethecondi2onsforitsownexistencebycontribu2ng

methanetoEarth’searlyatmosphere?!

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Earth’sHistory

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10

History of Oxygen

Time before Present (billion yrs)!

P O2(a

tm)!

1!

0.1!

0.01!

0.001!

0.0001!

0.00001!4.5! 4! 3.5! 3! 2.5! 2! 1.5! 1! 0.5! 0!

Multi-cellular Life!

Prokaryotic Life!

First !Eukaryotic!

Life!

“Modern” O2!levels!

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Cyanobacteria

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Earth’sOceanComposi/onoverGeologicTime

AnbarandKnoll,Science297,1137(2002)

Fe2+

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Earth’sOceanComposi/onoverGeologicTime

AnbarandKnoll,Science297,1137(2002)

Fe2+

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Sulfur-bearingrocks

SulfateSO4

2-SulfidesH2S,HS-

Oxida/veweathering

Bacterialreduc/on

“Weathering”(erosionandchemicalaltera/on)ofsulfur-bearingrocksunderanoxygen-richatmosphere

Productsflowintooceans

Sulfate-reducingbacteria!

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Earth’sHistory

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“Drihing”con/nentsandPlateTectonics

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Pangaea(~200millionyearsago)

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Earth’sCrust

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Earth’sInteriorStructure

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PlateTectonics

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Earth’sPlateBoundaries

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TheCascades

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Carbonate-SilicateCycle

Organismsformingcarbonateshells,par/cularlypro/sts(single-celleukaryotes),playanessen/alroleincarbonaterockforma/on

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Carbonate-SilicateCycle

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M Vogt, Science 2015;350:1466-1468

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Earth’sOceanComposi/onoverGeologicTime

AnbarandKnoll,Science297,1137(2002)

Fe2+

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SnowballEarth

SnowballEarthsarethoughttohaveoccurred2.2-2.4BYago,justaherthebuild-upofoxygeninEarth’satmosphere,and580-750millionyearsago,justbeforetheCambrianExplosionwhenlarge,diverse,morecomplexanimalsappearabruptlyinthefossilrecord.

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MassEx/nc/ons

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Cretaceous-Ter/ary(K/T)Ex/nc/onEvent

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CausesofMassEx/nc/ons

•  Theother4majormassex/nc/ons,aswellassmallerex/nc/onevents,appearnottobeassociatedwithimpacts;thecausesappeartobegeological/biological.–  Theex/nc/onsweregradualorepisodic,occurringoverhundredsofthousandstomillionsofyears.

–  Therearefewifanyimpactscratersoftherightage.–  Therearecrediblegeological/biologicalexplana/ons.

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ThePermian-Triassic(P/T)Ex/nc/on•  The“motherofallex/nc/ons”

–  ≤96%ofalloceanspeciesand~70%ofalllandspeciesdiedoff•  TheSiberianfloodbasalterup/onscoincidedwiththeex/nc/ons.–  Anarearoughlythesizeofthe48con/guousstateswascoveredwithlavatoanaveragedepthofaboutamileoverapproximatelyamillionyears

– Muchoftheerup/onoccurredthroughtheworld’slargestcoalbasin,probablyconver/ngmuchofthecoaltocarbondioxideandmethane,bothimportantgreenhousegases.

–  Increasedatmospherictemperaturewouldleadtoincreasedrainfallandcon/nentalweathering,producingmoresulfaterunoffintotheoceans,returningtheoceanstemporarilytothesulfidiccondi/onsofthemid-Proterozoic.

D.H.Erwin,Ex2nc2on:HowLifeonEarthNearlyEnded250MillionYearsAgo,PrincetonUniv.Press,2006

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Conclusions•  Earthhasbeenhabitableforatleast3.5-4billionyearsandperhapslonger,almostsinceitsforma/on4.54billionyearsago.

•  AninterplayofgeologicalandbiologicalprocesseshasbeenresponsibleformaintainingEarth’shabitabilityoversuchalonginterval,despiteasubstan/alchangeinthebrightnessofthesun.

•  Thecourseofbiologicalevolu/onhasbeenaffectedbytheinterplayofgeologicalandbiologicalforces.–  Ifwecould“replaythetapeoflife”,itisveryunlikelythatwewouldreproducethesamehistoryoflifeonEarth.

S.J.Gould,WonderfulLife:TheBurgessShaleandtheNatureofHistory,Norton,1989

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Questions?

QUESTIONS?


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