VOL THR EE / ISSUE T WO O R I G I N, E V O L U T I O N, E X T I N C T I O N THE EPIC STORY OF LIFE ON EARTH £9.99 0 2 9 772054 638003 THE COLLECTION Life story VOL 3 / ISSUE 2 HOWdidlifebegin?Thisisoneoftheeternal Whatdrovethisprocess?Whatwerethefirst LIFE ON EARTH: questions.Allcultureshaveacreationstory, complexcreaturesonEarth,andwhatdrove ORIGINS, EVOLUTION, butmodernsciencehasthebestoneofall– thesuccessiveexplosionsofevolutionary EXTINCTION anear-completeaccountofhowourplanet creativity? wentfromabarrenlumpofrocktoone Chapter3takesatourofthemost coveredinarichdiversityofplants,animals fascinatingfossilseverdiscovered,including andmicrobes. feathereddinosaursandmyriadotherlong- NEWSCIENTIST THECOLLECTION Foralmostabillionyearsafteritformed, deadcreatures.Whatcanwelearnaboutthe 110HighHolborn, Earthwasalifelessplacewithhellish behaviourofanimalsfromtheirfossilised LondonWC1V6EU +44(0)2076111202 conditions.Butaround3.8billionyearsago, remains,andwherecanwefind“missing [email protected] afterthesurfacehadcooledandoceans links”thattellsusaboutkeytransitionssuch Editor-in-chiefGrahamLawton formed,somethingamazinghappened.Out ashowbirdstookflight? EditorAlisonGeorge ofEarth’sprimordialchemicalsaroseanentity InChapter4wetakealookatGaiatheory, ArteditorCraigMackie PicturesNewScientist capableofreplicatingitself.Lifewasborn.The tacklingthecontroversialquestionofwhether picturedesk rest,astheysay,isprehistory. ourplanetactslikeagiantorganism,capable SubeditorJuliaBrown GraphicsDaveJohnston Theforcesofevolutionworkedonthis ofregulatingitsownenvironment. ProductioneditorMickO’Hare simplelifeformanditsdescendantstocreate Chapter5isallabouttheunifyingtheory ProjectmanagerHenryGomm PublisherJohnMacFarlane allmannerofusefuladaptationsincludinga oflife.Althoughthebeautifulandsimple systemtocaptureenergyfromthesun ideaofevolutionbynaturalselectionwas ©2016ReedBusiness InformationLtd,England (photosynthesis),biologicalcomputers firstput forward in 1858, many myths and NewScientistTheCollectionis (brains)andevenabiologicalwheel. misconceptions about it still persist. We tackle publishedfourtimesperyearby ReedBusinessInformationLtd Wewillprobablyneverknowexactlyhow them head on. ISSN2054-6386 thisfirstlifearoseorwhatitwaslike,butthere Where there’s life, there’s death. This is the PrintedinEnglandbyPrecision aremanyothermysterieswecanhopeto appropriate subject of our final chapter: ColourPrinting,Telford, solve.ThisissueofNewScientist:The extinction. The fossil record reveals that most Shropshire,anddistributedby MarketforceUKLtd Collectiontacklesthesequestions.Ittellsthe species that existed have gone. Why? What +44(0)2031483333 epicstoryoftheonlylivingplanetweknowof were the biggest mass extinctions? And what Displayadvertising +44(0)2076111291 intheuniverse,fromlife’soriginstothe would our planet look like if all life suddenly [email protected] watershedmomentsinitshistory. died? Chapter1isaboutthedawnoflife.Charles Prepare to go on a journey of a lifetime. Cover image Darwinimaginedthatlifearosein“some Aixsponza warmlittlepond”,buttherearemanyother Alison George, Editor possiblecradlesoflife.Whereandwhendidit happen?Whatingredientswereneeded,and was the event inevitable? Chapter 2 explores the key steps in the early development of life. For the first 1.5 million years of its existence, life consisted of simple microbes, but then things got more interesting. Cells developed internal “organs” and multicellular life eventually followed. Life on Earth: Origins, Evolution, Extinction | NewScientist: The Collection | 1 CONTENTS THE COLLECTION 2 CONTRIBUTORS VOL3/ISSUE2 ColinBarras isawriterinAnnArbor,Michigan LIFEONEARTH: StephenBattersby isaconsultantforNewScientist ORIGINS, MichaelJ.Benton isattheUniversityofBristol,UK MichaelChorost EVOLUTION, isawriterbasedinWashingtonDC StuartClark isaconsultantforNewScientist EXTINCTION JamesO’Donoghue The history isawriterinNorwich,UK JeffHecht isaconsultantforNewScientist of life BobHolmes isaconsultantforNewScientist DanJones isawriterinBrighton,UK NickLane isatUniversityCollegeLondon MichaelMarshall isdeputyeditoratBBCEarth MichaellePage isareporteratNewScientist PatShipman isatPennsylvaniaStateUniversity TobyTyrell isattheUniversityofSouthampton,UK Tim Vernimmen is a writer based near Antwerp,Belguim Peter Ward is at the University of WashingtoninSeattle 1 28 Riseofthewatereaters Howlifegotitsoxygen 32 Genesisrevisited Didoxygenreallykick-startcomplexlife? 36 Life’slongfuse Solvingthemysteriesofthefirst complex life 42 Theotherbigbang The origin HowlifeonEarthtookoff 46 Second coming of life The truly momentous event in animal evolution 6 Meetyourmaker Hominginontheancestorofalllife 10 Dawnoftheliving Thesearchforthefirstreplicator 14 Inevitable,fluke,orboth? Iflifeisinevitable,wherearethealiens? 20 Underacoldsun Howdidlifestartonthisinhospitableplanet? 24 Home and dry The articles here were first published No primal soup: creating life without water in New Scientist between April 2007 and February 2015. They have been updated and revised. 2 | NewScientist: The Collection | Life on Earth: Origins, Evolution, Extinction 3 5 6 Fossils Evolution Extinction 50 Signsofearlylife 76 Theultimateguidetoabeautifultheory 114Deathonamassivescale Fossils-anexpertguide Bustingthemythsandmisconceptions Aguidetomassextinctions 54 Findthegaps 86 Inthefastlane 120Noah’snightmare Closinginonthemissinglinks Lifeischangingbeforeourveryeyes Wehavetochoosewhichspeciestosave 60 Turnedtostone 92 TheXfactor 124Earth after life Thesevenmostrevealingfossilseverfound Asinglegenetoshuffleupnewspecies What if everything died out tomorrow? 4 96 Winningcombinations Evolvability:cashinginonthegeneticlottery 101Adaptfirst,mutatelater Isevolutionoutoforder? 105Theascentoflife Doeslifehaveadirection? 108Unnaturalselection Humansarethegreatestforceinevolution Gaia 66 Callintheclouds Howlivingthingsshapetheweather 70 Gaia’seviltwin Lifeisitsownworstenemy 74 Gaia: the verdict Just how motherly is the Earth? 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C H A P T E R O N E THE ORIGIN OF LIFE NZA O AIXSP MEET YOUR MAKER Whatdidthelastcommon IN1859,whenCharlesDarwinpublished Sincethenwehavediscoveredamultitude OnTheOriginofSpecies,hededicatedan ofintermediatelinks:fishthatcouldcrawl, ancestorofalllifelooklike? entirechaptertotheproblemofmissing lizardswithmammal-likejaws,whaleswith MichaelLePagedelves “intermediatelinks”–transitionalformsthat legs,giraffeswithshortnecksandmany bridgedtheevolutionarygapsbetweenclosely others(see“Findthegaps”,page54).But intotheprimordialsoup relatedspecies.Ifhistheorywascorrect,the there’soneweareunlikelyevertofind:the fossilrecordshouldbefullofthem.Where linkbetweentheearliestproto-lifeandlifeas werethey? weknowit,alsoknownasthelastuniversal Atthetimeitwasarealproblem,asfew commonancestor,orLUCA. suchfossilshadbeenfound.Thencame LUCAlivedaround4billion years ago – thespectaculardiscovery,in1861,of a tiny, fragile life form that is the direct Archaeopteryx,withthewingsandfeathers ancestor of every single living thing, from ofabirdandtheteethandtailofadinosaur. aardvarks to zebras. It wasn’t the very first 6|NewScientist:TheCollection|LifeonEarth:Origins,Evolution,Extinction These tell us much about what LUCA was like. We know it used DNA to store recipes for proteins, for instance. We even know what many of those recipes were, because many vital proteins found in all cells today must have come from LUCA. And from the nature of these proteins, it is clear that LUCA used an energy-rich molecule called ATP to fuel cellular processes, just as our cells do. How did LUCA make its ATP? Anyone designing life from scratch would probably make ATP using chemical reactions inside thecell.Butthat’snothowitisdone.Instead, energyfromfoodorsunlightisusedtopower aprotein“pump”thatshuntshydrogenions– protons– out of the cell. This creates a difference in proton concentration, or a gradient, across the cell membrane. Protons then flow back into the cell through another protein embedded in the membrane, which uses the energy to produce ATP. Think of a sink To understand it in energy terms, think of a double kitchen sink. The small sink represents the inside of the cell and the large one the outside world. Start by filling the large sink with water, leaving the small one empty. The difference in water levels is a potential source of energy: drill a hole in the divider and water will flow into the small sink. The flow could be used to turn a tiny turbine – which is essentiallywhattheATP-makingproteinis, aturbineturnedbyprotonsandotherpositive ions(seediagram,page8). This process is so convoluted that when biochemist Peter Mitchell proposed it in 1961 it was dismissed as nonsense. But it has turned out to be common to all life, so most biologists thinkitmustbehowLUCAmadeATP. Exploitingaprotongradientrequiresa membranethatisimpermeabletoprotons– they should only be able to flow in through the turbine. So it’s assumed that LUCA had an impermeable membrane. But there is no life: thousands, if not millions, of years of newworkonaleadinghypothesisforthe evidence that this is the case. In fact, the evolutionary experimentation preceded it. originoflifemighthavesolvedmanyofthe nature of LUCA’s membrane is an enigma. But understanding LUCA would give us our mysteries.Itpaintsadetailedpictureofwhere To understand why, we have to backtrack best view yet of the origin of life. ourearliestancestorlived,howitlivedand to the 1970s, when it was thought that life We already know a surprising amount. whatitwaslike.Preparetomeetyourmaker. could be divided into two great “empires”. Although any traces LUCA left in rocks were Darwinhimselfwasamongthefirst In one were animals, plants and fungi, and in probably obliterated aeons ago, something far scientiststospeculateonhowlifeoriginated: the other the much simpler bacteria. Then more revealing survives inside today’s living heenvisageda“warmlittlepond,withallsorts microbiologist Carl Woese discovered that cells: a biological operating system that is ofammoniaandphosphoricsalts,lights,heat, the bacterial empire actually contained two common to all life and must have been shared electricity,etcpresent”.Wewillprobablynever radically different types of life. A third by LUCA too. knowexactlyhowLUCAcametobe,butwecan “domain”, now known as archaea, had been Many features of LUCA, though, have makeeducatedguessesbylookingatsomeof hiding in plain sight. remained enigmatic, even paradoxical. But thefeaturesoftoday’slivingsystems. Archaea often look like bacteria, and are > LifeonEarth:Origins,Evolution,Extinction|NewScientist:TheCollection|7 “ The building blocks of life would have formed spontaneously within the vents” similar in many ways – as you would expect explain why life uses proton gradients to given that both evolved from LUCA, probably generate ATP. Now, says Lane, it can also quite soon after it existed. There are also some explain another of life’s key features: the fundamental differences between them. membranes of archaea and bacteria. One is their membranes. Distinct from the better known black Both bacteria and archaea have membranes smokers, alkaline hydrothermal vents are made of water-repellent fatty molecules. places where warm alkaline fluids, at Simple fatty molecules tend to flip around, temperatures of between 40 °C and 90 °C, making the membrane leaky, so both bacteria well up through cracks in the sea floor. As and archaea tacked on a water-loving the fluid hits the cold seawater, minerals phosphate group to stabilise the molecules precipitate out of solution, gradually forming and make their membranes impermeable. rocky chimneys up to 60 metres tall, full of They took very different routes, though. narrow channels and pores. Bacterial membranes are made of fatty acids bound to the phosphate group while archaeal Building blocks of life membranes are made of isoprenes bonded to phosphate in a different way. This suggests Alkaline vents were present in primordial seas that their membranes evolved independently. too. Within these ancient vents, Lane, Russell WA This leads to something of a paradox: if and Martin think, the building blocks of life NO LUCA already had an impermeable membrane would have formed spontaneously. The walls for exploiting proton gradients, why would its would have been rich in iron and sulphide, for interface between the proton-poor alkaline descendants have independently evolved two example, which can catalyse complex organic vent fluid and the proton-rich seawater. This different kinds of impermeable membrane? reactions. What’s more, temperature gradients is the ultimate origin of the proton gradients Nick Lane of University College London, a within the pores should have created high that power life today. biochemist and award-winning science writer, concentrations of organic compounds and The stage was now set for the evolution, via has come up with a startling answer that favoured the formation of large molecules, a series of gradual steps, of the turbine protein challenges many widely held ideas. Far from including lipids – fat molecules – and RNA. that straddles the membrane and produces being impermeable, LUCA’s membrane was So it would have been a perfect setting for ATP. This was a crucial step in early evolution, leaky. In fact, he argues, it had to be leaky. the RNA world widely thought to have been though the cells could only survive at the Lane starts from the assumption that life the first step towards life. This may have been interface between vent fluids and seawater, originated on the sea floor at places called where self-replicating sets of RNA and other where there was a gradient to exploit. Only alkaline hydrothermal vents. This was molecules first emerged and began to evolve later did they evolve the ability to generate proposed in 1989 by Michael Russell of NASA. into cell-like organisms with simple their own gradient using proton pumps. Its proponents, including Lane and William membranes. These proto-life forms needed It is a neat hypothesis but as critics have Martin of the University of Dusseldorf in energy – and it was provided, Martin and Lane pointed out, there is a big catch. Early cells that Germany,havearguedthatitalonecan argue,bythenaturalprotongradientatthe hadtheATPturbineproteinbutnotproton Life powers up The earliest life on Earth could well have evolved at an undersea hydrothermal vent around 4 billion years ago. PROTON How did this cell get its energy, and how did it evolve to colonise the rest of the planet? SODIUMION The cell lives on the boundary between acid, proton- Later cells evolve a "revolving door" protein that Eventually cells develop a dedicated proton pump rich seawater, and alkaline vent luid. It develops a efortlessly pumps sodium ions out while letting and a leak-proof membrane. These cells can generate protein that, like a turbine, extracts energy from the protons in. The sodium later re-enters through the their own proton gradient across the membrane to proton gradient (diference in concentration) turbine protein, generating even more energy obtain energy, and can leave the vent behind ACID SEAWATER TTUURRBBIINNEE REEVOOLVINNNGG DDOORR PRROOOTON PUMP PPPRROOTT GGRAADIE LEAKY LEAK-PROOF MEMBRANE MEMBRANE ALKALINE VENT FLUID 8 | NewScientist: The Collection | Life on Earth: Origins, Evolution, Extinction