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Geološka kronologija – razlika između verzija

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{| class="wikitable" border="3" style="font-size:95%;"
|-
! [[Eon (geologygeologija)|Eon]]
! [[Era (geologygeologija)|Era]]
! colspan="2" | Period<sup>1</sup>
! SeriesNiz/<br>EpochEpoha
! Najvažniji događaji
! Major Events
! StartPočetak, MillionMiliona<br/>Years Agogodina<sup>2</sup>
|-
| rowspan="37" style="background:#B3E2D1" | [[PhanerozoicFanerozoik|PhaneFane-<br>rozoicrozoik]]
| rowspan="7" style="background:#FFFF00" | [[Cenozoic]]
| colspan="2" style="background:#FDCC8A" rowspan="4" | [[Neogene]]<sup>3</sup>
Red 97:
| style="background:#67B39F" | 251.0 ± 0.4 <sup>*</sup>
|-
| rowspan="22" style="background:#80B5D5" | [[PaleozoicPaleozoik]]
| rowspan="3" colspan="2" style="background:#67C6DE" | [[Permian]]
| style="background:#B3E3EE" | [[Lopingian]]
Red 157:
| style="background:#9858A8" | 443.7 ± 1.5 <sup>*</sup>
|-
| rowspan="3" colspan="2" style="background:#F981A6" | [[OrdovicianOrdovicij]]
| style="background:#FBB4BD" | [[LateKasni Ordovicianordovicij|UpperGornji/Latekasni]]
| rowspan="3" | [[InvertebrateBeskralješnaci]]s verysu diversevrlo andrazgranati includei manyuključuju newmnogo typesnovih tipova. EarlyRani coralskoralji, [[Brachiopodbrachiopodi]]s ([[Orthida]], [[Strophomenida]], etcitd), [[bivalvedvokrilne školjke]]s, [[nautiloidnautiloidi]]s, [[trilobitetrilobiti]]s, [[ostracodostrakodi]]s, [[bryozoa]], manymnogi types oftipovi [[echinodermsbodljokošci|bodljokošaca]] ([[Cystoidea|cystoids]], [[crinoidmorska zvijezda|morske zvijezde]]s, starfish, etcitd.), branchedrazgranati [[graptolitegraptoliti]]s, andi otherostali taxarazredi allsu commonučestali. [[ConodontKonodont]]si weresu primitivebili planktonicprimitivni vertebratesplanktonski thatkralješnjaci appearkoji atse thepojavljuju startna ofpočetku the Ordovicianordovicija. IceLedeno agedoba atna thekraju endperioda. of thePrve period.i vrlo Firstprimitivne very primitive landkopnene [[plantbiljka|biljke]]s.
| style="background:#FBB4BD" | 460.9 ± 1.6 <sup>*</sup>
|-
| style="background:#FA9AB1" | [[MiddleSrednji Ordovicianordovicij|MiddleSrednji]]
| style="background:#FA9AB1" | 471.8 ± 1.6
|-
| style="background:#E67DA4" | [[EarlyRani Ordovicianordovicij|LowerDonji/Earlyrani]]
| style="background:#E67DA4" | 488.3 ± 1.7 <sup>*</sup>
|-
| rowspan="3" colspan="2" style="background:#FB805F" | [[CambrianKambrij]]
| style="background:#FDCDB8" | [[FurongianFurongij]]
| rowspan="3" | MajorVelika diversificationdiversifikacija ofživota life in theu [[CambrianKambrijska eksplozija|Kambrijskoj Explosioneksploziji]]; moreviše thanod halfpolovice ofmodernih modern animalživotinja [[Phylum (biologybiologija)|phyla]] appearse pojavljuju, alongzajedno with as numbervelikim ofbrojem extinctizumrlih andi problematicproblematičnih formsformi. [[ArcheocyathaArheocijati]] abundantcvatu inu theranom early Cambriankambriju. [[TrilobiteTrilobiti]]s, [[PriapulidaPriapulidi]], [[Porifera|spongesspužve]], inarticulateneartikulirani [[brachiopodbrahiopod]]s, andi manyi othermnoge formsdruge allpoznate commonvrste. FirstPojava prvih [[chordatesvitkovci|svitkovaca]]s appear. [[Anomalocaris|anomalocaridsAnomalocaridi]] aresu topglavni predatorsgrabežljivci. EdicarianEdikarijanske animalsživotinje raresu rijetke, then diezatim outizumiru.
| style="background:#FDCDB8" | 501.0 ± 2.0 <sup>*</sup>
|-
| style="background:#E8AE97" | [[MiddleSrednji Cambriankambrij|Middlesrednji]]
| style="background:#E8AE97" | 513.0 ± 2.0
|-
| style="background:#E77C72" | [[EarlyRani Cambriankambrij|LowerDonji/Earlyrani]]
| style="background:#E77C72" | 542.0 ± 1.0 <sup>*</sup>
|-
| rowspan="10" style="background:#CCD891" | [[ProterozoicProterozoik|Proter-<br>ozoicozoik]]<br><sup>5</sup>
| rowspan="3" style="background:#CAA595" | [[NeoproterozoicNeoproterozoik|Neo-<br>proterozoicproterozoik]]
| colspan="2" style="background:#EAD8BC" | [[EdiacaranEdiakaran]]
| colspan="2" | FirstPrve [[metazoa|multi-celledvišestanične animalsživotinje]]. EdicarianEdicarianska fauna ([[vendobionta]]) flourishcvjeta worldwideširom svijta. SimpleJednostavni [[tracefosilizirani fossiltragovi]]s fromod worm-likecrvolikih animalsživotinja. FirstPrve [[Porifera|spongesspužve]].
| style="background:#EAD8BC" | 630 +5/-30 <sup>*</sup>
|-
| colspan="2" style="background:#DCABAA" | [[CryogenianKroogeniak]]
| colspan="2" | PossibleMogući period [[snowballSnježna Earthgrudva Zemlja|Snježne grudve Zemlje]] period, [[RodiniaRodinija]] begins tose breakpočinje uplomiti
| style="background:#DCABAA" | 850 <sup>6</sup>
|-
| colspan="2" style="background:#CBA46C" | [[TonianTonij]]
| colspan="2" | FirstPrvo širenje [[acritarchakritarh]] radiationa.
| style="background:#CBA46C" | 1000 <sup>6</sup>
|-
| rowspan="3" style="background:#DDC288" | [[MesoproterozoicMezoproterozoik|Meso-<br>proterozoicproterozoik]]
| colspan="2" style="background:#DDC288" | [[StenianStenij]]
| colspan="2" | NarrowProrijeđenje highlyvisoko [[metamorphicmetamorfska stijena|metamorfskih]] beltspojasa due tozbog [[orogenyorogenija|orogenije]] askada se stvara [[RodiniaRodinija]] formed.
| style="background:#DDC288" | 1200 <sup>6</sup>
|-
| colspan="2" style="background:#DDC288" | [[EctasianEkstazij]]
| colspan="2" | [[PlatformPlatformski coverpokrov]]si continuese tonastavljaju expandširiti
| style="background:#DDC288" | 1400 <sup>6</sup>
|-
| colspan="2" style="background:#DDC288" | [[CalymmianKalimmij]]
| colspan="2" | [[PlatformPlatformski coverpokrov]]si expandse šire
| style="background:#DDC288" | 1600 <sup>6</sup>
|-
| rowspan="4" style="background:#B3B25E" | [[PaleoproterozoicPaleoproterozoik|Paleo-<br>proterozoicproterozoik]]
| colspan="2" style="background:#B3B25E" | [[StatherianStaterij]]
| colspan="2" | FirstPrvi [[EukaryoteEukariote|complexsloženi single-celledvišestanični lifeživot]]. [[Columbia (supercontinentsuperkontinent)]].
| style="background:#B3B25E" | 1800 <sup>6</sup>
|-
| colspan="2" style="background:#B3B25E" | [[OrosirianOrosirij]]
| colspan="2" | U [[AtmosphereAtmosfera|atmosferu]] becameulazi [[oxygenkisik]]ic. [[Vredefort craterkrater|VredefortVredefortski]] and [[Sudbury BasinBazen|Sudburyjski]] asteroidasteroidni impactsudari. MuchMnogo [[orogenyorogenija|orogenije]].
| style="background:#B3B25E" | 2050 <sup>6</sup>
|-
| colspan="2" style="background:#B3B25E" | [[RhyacianRhyacij]]
| colspan="2" | [[Bushveld|BushveldBushveldska Formationformacija]] formedformirana. [[HuronianHuronij|Huronijska]] glaciationglacijacija.
| style="background:#B3B25E" | 2300 <sup>6</sup>
|-
| colspan="2" style="background:#B3B25E" | [[SiderianSiderij]]
| colspan="2" | [[naslage bandedvezanog iron formationželjeza]]s formedformirane
| style="background:#B3B25E" | 2500 <sup>6</sup>
|-
| rowspan="4" style="background:#99ADAC" | [[ArcheanArhej]]<br><sup>5</sup>
| style="background:#CBCDC8" | [[NeoarcheanNeoarhej]]
| colspan="4" | StabilizationStabilizacija ofvećine most modernmodernih [[cratonkraton]]sa, possiblemoguće izvrtanje [[MantlePokrivač (geologygeologija )|mantlepokrivača]] overturn event
| style="background:#CBCDC8" | 2800 <sup>6</sup>
|-
| style="background:#B2B5AF" | [[MesoarcheanMezoarhej]]
| colspan="4" | FirstPrvi [[stromatolitestromatoliti]]s
| style="background:#B2B5AF" | 3200 <sup>6</sup>
|-
| style="background:#999791" | [[PaleoarcheanPaleoarhej]]
| colspan="4" | FirstPrve knownpoznate [[phototroph|oxygen producingbakterije]] [[bacteriafototropi|proizvođači kisika]]
| style="background:#999791" | 3600 <sup>6</sup>
|-
| style="background:#809090" | [[EoarcheanEoarhej]]
| colspan="4" | [[ProkaryoteProkarioti|SimpleJednostavni single-celledjednostanični lifeživot]]
| style="background:#809090" | 3800
|-
| style="background:#809090" rowspan="4" | [[HadeanHad (period)|Had]]<br><sup>5,7</sup>
| style="background:#809090" | [[LowerDonji Imbrianimbrij]]
| colspan="4" | &nbsp;
| style="background:#809090" | c.3850
|-
| style="background:#809090" | [[NectarianNektarij]]
| colspan="4" | &nbsp;
| style="background:#809090" | c.3920
|-
| style="background:#809090" | [[BasinBazenske groupsgrupe]]
| colspan="4" | 4100 MYA - OldestNajstarija knownpoznata rockstijena
| style="background:#809090" | c.4150
|-
| style="background:#809090" | [[CrypticKriptička era|CrypticKriptik]]<sup>8</sup>
| colspan="4" | 4400 MYA - OldestNajstariji knownpoznati mineralminerali; 4570 MYA - Formation ofStvaranje [[EarthZemlja|Zemlje]]
| style="background:#809090" | c.4570
|}
Red 260:
<div style="font-size:90%;">
# Paleontologists often refer to [[faunal stage]]s rather than geologic periods. The stage nomenclature is quite complex. See [http://flatpebble.nceas.ucsb.edu/cgi-bin/bridge.pl?action=startScale Harland] for an excellent time ordered list of faunal stages.
# Datumi su neznatno nejasni uz uobičajene varijacije u nekoliko postotaka između različitih izvora. To je uglavnom zbog nesigurnosti [[Radiometrijsko datiranje|radiometrijskog datiranja]] i problema koji uzrokuje rijetkost pronalaženja nalaza pogodnih za radiometrijsko datiranje na mjestima gdje bi bili najkorisniji. Datumi i pogreške su u skladu s kronologijom [[Međunarodna komisija za stratigrafiju|Međunarodne komisije za stratigrafiju]] uz 2004. Datumi označeni zvjezdicom označavaju
# Dates are slightly uncertain with differences of a few percent between various sources being common. This is largely due to uncertainties in [[radiometric dating]] and the problem that deposits suitable for radiometric dating seldom occur exactly at the places in the geologic column where they would be most useful. The dates and errors quoted above are according to the [[International Commission on Stratigraphy]] 2004 time scale. Dates labeled with a * indicate boundaries where a [[Global Boundary Stratotype Section and Point]] has been internationally agreed upon.
[[GSSA|Globalne stratotipske granice i točke međe]] i o njima postoji međunarodni konsenzus.
# Historically, the [[Cenozoic]] has been divided up into the [[Quaternary]] and [[Tertiary]] sub-eras, as well as the [[Neogene]] and [[Paleogene]] periods. However, the International Commission on Stratigraphy has recently decided to stop endorsing the terms Quaternary and Tertiary as part of the formal nomenclature.
# In North America, the Carboniferous is subdivided into [[Mississippian]] and [[Pennsylvanian]] Periods.
# The [[ProterozoicProterozoik]], [[Archeanarhej]] andi [[HadeanHad (period)|had]] arese oftenponekad collectivelyzajedno referrednazivaju to askao [[PrecambrianPrakambrij|PrecambrianPredkambrijsko Timevrijeme]], and sometimesa alsonekad asjednostavno thekao [[CryptozoicKriptozoik]].
# DefinedDefinirano bykao absoluteapsolutno agedoba ([[GlobalGlobalno Standardstandardno Stratigraphicstratigrafsko Agedoba]]).
# ThoughIako commonlyse usedčesto koristi, the [[HadeanHad (period)|Had]] isnije not a formalformalni eon andi noo lowerdonjoj boundgranici forza theeoarhej Eoarcheanjoš hasnije beenpostignut agreed upondogovor. The Hadean has alsoHad sometimesse beentakođer calledponekad thenaziva [[Priscoan]].
# Ova četiri naziva su uzeta iz geologije Mjeseca. Njihova upotreba za geologiju Zemlje je neslužbena.
# These four era names were taken from Moon geology. Their use for Earth geology is unofficial.
# The start time for the [[Holocene]] epoch is here given as 11,430 years ago ± 130 years. For further discussion of the dating of this epoch, see [[Holocene]].
</div>
Izvor: https://sh.wikipedia.org/wiki/Geološka_kronologija