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Рядок 28:
|-
|rowspan="102" style="background:#ffffff"| n/a{{efn|References to the "Post-Cambrian Супереон" are not universally accepted, and therefore must be considered unofficial.}}
|rowspan="102" style="text-align:center; background:{{period color|phanerozoic}}"| [[Фанерозойський еон|Ф<br/>а<br/>н<br/>е<br/>р<br/>о<br/>з<br/>о<br/>й]]
|rowspan="24" style="background:{{period color|cenozoic}}"| [[Кайнозойська ера|Кайнозой]]{{efn|Historically, the [[Cenozoic]] has been divided up into the [[Quaternary]] and [[Tertiary]] sub-eras, as well as the [[Neogene]] and [[Paleogene]] periods. The 2009 version of the ICS time chart<ref name="cenozoic-division">{{cite web |url=http://www.stratigraphy.org/upload/ISChart2009.pdf |title=Archived copy |accessdate=2009-12-23 |deadurl=yes |archiveurl=https://web.archive.org/web/20091229003212/http://www.stratigraphy.org/upload/ISChart2009.pdf |archivedate=29 December 2009 |df=dmy-all }}</ref> recognizes a slightly extended Quaternary as well as the Paleogene and a truncated Neogene, the Tertiary having been demoted to informal status.}}
| rowspan="7" style="background-color: {{period color|quaternary}};" | [[Четвертинний період|Антропоген]], Q
Рядок 73:
| rowspan="6" style="background-color: {{period color|miocene}};" | [[Міоцен]], N<sub>1</sub>
| style="background-color: {{period color|messinian}};" | [[Мессінський ярус|Мессіній]], N<sub>1</sub>mes
| rowspan="2" | [[Messinian Event]] with hypersaline lakes in empty [[Mediterranean Basin]]. [[Greenhouse and Icehouse Earth|Moderate Icehouse climate]], punctuated by [[ice age]]s and re-establishment of [[East Antarctic Ice Sheet]]; Gradual separation of [[Chimpanzee–human last common ancestor|human and chimpanzee ancestors]]. [[Sahelanthropus tchadensis]] in Africa.
| style="background-color: {{period color|messinian}};" | [[Файл:Clavo dorado.svg|10px]] 7,246
|-
Рядок 96:
| rowspan="2" style="background-color: {{period color|oligocene}}; border-top: 2px solid grey;" | [[Олігоцен]], <s>P</s><sub>3</sub>
| style="background-color: {{period color|chattian}}; border-top: 2px solid grey;" | [[Хаттський ярус|Хатт]], <s>P</s><sub>3</sub>h
| rowspan="2" style="border-top: 2px solid grey;" |
| style="background-color: {{period color|chattian}}; border-top: 2px solid grey;" | 27,82
|-
| style="background-color: {{period color|rupelian}};" | [[Рюпельський ярус|Рюпель]], <s>P</s><sub>3</sub>r
| 27,82
| style="background-color: {{period color|rupelian}};" | 33,9
|-
| rowspan="4" style="background-color: {{period color|eocene}};" | [[Еоцен]], <s>Р</s><sub>2</sub>
| style="background-color: {{period color|priabonian}};" | [[Приабонський ярус|Приабон]], <s>Р</s><sub>2</sub>p
| rowspan="2" |
| 33,9
| style="background-color: {{period color|priabonian}};" | 37,8
|-
| style="background-color: {{period color|bartonian}};" | [[Бартонський ярус|Бартон]], <s>Р</s><sub>2</sub>b
| style="background-color: {{period color|bartonian}};" | 41.,2▼
| 37,8
▲| style="background-color: {{period color|bartonian}};" | 41.2
|-
| style="background-color: {{period color|lutetian}};" | [[Лютецький ярус|Лютец]], <s>Р</s><sub>2</sub>l
| rowspan="2" |
| 41,2
| style="background-color: {{period color|lutetian}};" | 47,8
|-
| style="background-color: {{period color|ypresian}};" | [[Іпрський ярус|Іпр]], <s>Р</s><sub>2</sub>i
| 47,8
| style="background-color: {{period color|ypresian}};" | 56,0
|-
| rowspan="3" style="background-color: {{period color|paleocene}};" | [[Палеоцен]], <s>Р</s><sub>1</sub>
| style="background-color: {{period color|thanetian}}" | [[Танетський ярус|Танет]], <s>Р</s><sub>1</sub>t
| rowspan="3" |
| 56,0
| style="background-color: {{period color|thanetian}}" |59,2
|-
| style="background-color: {{period color|selandian}};" | [[Зеландський ярус|Зеландій]], <s>Р</s><sub>1</sub>z
| 59,2
| style="background-color: {{period color|selandian}};" |61,6
|-
| style="background-color: {{period color|danian}};" | [[Данський ярус|Даній]], <s>Р</s><sub>1</sub>d
| 61,6
| style="background-color: {{period color|danian}};" |66,0
|-
Рядок 174 ⟶ 169:
| style="background-color:{{period color|berriasian}};" | [[Файл:Пустий ієрогліф.png|10px]] ~145,0
|-
| rowspan="11" style="background-color: {{period color|jurassic}}; border-top: 2px solid grey;" | [[Юрський період|Юра]], J
| rowspan="3" style="background-color: {{period color|late jurassic}}; border-top: 2px solid grey;" | [[Мальм]], J<sub>3</sub>
| style="background-color: {{period color|tithonian}}; border-top: 2px solid grey;" | [[Титонський ярус|Титон]], J<sub>3</sub>tt
| rowspan="11" style="border-top: 2px solid grey;" |
| style="background-color: {{period color|tithonian}}; border-top: 2px solid grey;" | 152,1
|-
| style="background-color: {{period color|kimmeridgian}};" | [[Кімериджський ярус|Кімеридж]], J<sub>3</sub>km
| 152,1
| style="background-color: {{period color|kimmeridgian}};" | 157,3
|-
| style="background-color: {{period color|oxfordian}};" | [[Оксфордський ярус|Оксфорд]], J<sub>3</sub>o
| 157,3
| style="background-color: {{period color|oxfordian}};" | 163,5
|-
| rowspan="4" style="background-color: {{period color|middle jurassic}};" | [[Доггер]], J<sub>2</sub>
| style="background-color: {{period color|callovian}};" | [[Келовейський ярус|Келовей]], J<sub>2</sub>k
| 163,5
| style="background-color: {{period color|callovian}};" | 166,1
|-
| style="background-color: {{period color|bathonian}};" | [[Батський ярус|Бат]], J<sub>2</sub>bt
| 166,1
| style="background-color: {{period color|bathonian}};" | 168,3
|-
| style="background-color: {{period color|bajocian}};" | [[Байоський ярус|Байос]], J<sub>2</sub>b
| 168,3
| style="background-color: {{period color|bajocian}};" | 170,3
|-
| style="background-color: {{period color|aalenian}};" | [[Ааленський ярус|Аален]], J<sub>2</sub>a
| 170,3
| style="background-color: {{period color|aalenian}};" | 174,1
|-
| rowspan="4" style="background-color: {{period color|early jurassic}};" | [[Лейас]], J<sub>1</sub>
| style="background-color: {{period color|toarcian}};" | [[Тоарський ярус|Тоар]], J<sub>1</sub>t
| 174,1
| style="background-color: {{period color|toarcian}};" | 182,7
|-
| style="background-color: {{period color|pliensbachian}};" | [[Плінсбахський ярус|Плінсбах]], J<sub>1</sub>p
| 182,7
| style="background-color: {{period color|pliensbachian}};" | 190,8
|-
| style="background-color: {{period color|sinemurian}};" | [[Синемюрський ярус|Синемюр]], J<sub>1</sub>s
| 190,8
| style="background-color: {{period color|sinemurian}};" | 199,3
|-
| style="background-color: {{period color|hettangian}};" | [[Геттанзький ярус|Геттанг]], J<sub>1</sub>h
| 199,3
| style="background-color: {{period color|hettangian}};" | 201,3
|-
Рядок 225 ⟶ 210:
| rowspan="3" style="background-color: {{period color|late triassic}}; border-top: 2px solid grey;" | [[Пізній тріас|Пізній]], T<sub>3</sub>
| style="background-color: {{period color|rhaetian}}; border-top: 2px solid grey;" | [[Ретський ярус|Рет]], T<sub>3</sub>r
| rowspan="7" style="border-top: 2px solid grey;" |
| style="background-color: {{period color|rhaetian}}; border-top: 2px solid grey;" | ~208,5
|-
| style="background-color: {{period color|norian}};" | [[Норійський ярус|Норій]], T<sub>3</sub>n
| ~208,5
| style="background-color: {{period color|norian}};" | ~227
|-
| style="background-color: {{period color|carnian}};" | [[Карнійський ярус|Карній]], T<sub>3</sub>c
| ~227
| style="background-color: {{period color|carnian}};" | ~237
|-
| rowspan="2" style="background-color: {{period color|middle triassic}};" | [[Середній тріас|Середній]], T<sub>2</sub>
| style="background-color: {{period color|ladinian}};" | [[Ладинський ярус|Ладиній]], T<sub>2</sub>l
| ~237
| style="background-color: {{period color|ladinian}};" | ~242
|-
| style="background-color: {{period color|anisian}};" | [[Анізійський ярус|Анізій]], T<sub>2</sub>a
| ~242
| style="background-color: {{period color|anisian}};" | 247,2
|-
| rowspan="2" style="background-color: {{period color|early triassic}};" | [[Ранній тріас|Ранній]], T<sub>1</sub>
| style="background-color: {{period color|olenekian}};" | [[Оленьокський ярус|Оленьок]], T<sub>1</sub>o
| 247,2
| style="background-color: {{period color|olenekian}};" | 251,2
|-
| style="background-color: {{period color|induan}};" | [[Індський ярус|Інд]], T<sub>1</sub>i
| 251,2
| style="background-color: {{period color|induan}};" | 251,902
|-
Рядок 258 ⟶ 237:
| rowspan="2" style="background-color: {{Period color|lopingian}}; border-top: 3px solid grey;" | [[Лопінгій]], P<sub>3</sub>
| style="background-color: {{Period color|changhsingian}}; border-top: 3px solid grey;" | [[Чангсінзький ярус|Чангсінг]], P<sub>3</sub>c
| rowspan="9" style="border-top: 3px solid grey;" |
| style="background-color: {{Period color|changhsingian}}; border-top: 3px solid grey;" | 254,14
|-
| style="background-color: {{Period color|wuchiapingian}}" | [[Вучапінзький ярус|Вучапінг]], P<sub>3</sub>v
|
| style="background-color: {{Period color|wuchiapingian}}" | 259,1
|-
| rowspan="3" style="background-color: {{Period color|guadalupian}}" | [[Гваделупій]], P<sub>2</sub>
| style="background-color: {{Period color|capitanian}}" | [[Кептенський ярус|Кептен]], P<sub>2</sub>c
| 259,1
| style="background-color: {{Period color|capitanian}}" | 265,1
|-
| style="background-color: {{Period color|wordian}}" | [[Вордійський ярус|Вордій]], P<sub>2</sub>w
| 265,1
| style="background-color: {{Period color|wordian}}" | 268,8
|-
| style="background-color: {{Period color|roadian}}" | [[Роудський ярус|Роуд]], P<sub>2</sub>r
| 268,8
| style="background-color: {{Period color|roadian}}" | 272,95
|-
| rowspan="4" style="background-color: {{Period color|cisuralian}}" | [[Цисуралій]], P<sub>1</sub>
| style="background-color: {{Period color|kungurian}}" | [[Кунгурський ярус|Кунгур]], P<sub>1</sub>k
| 272,95
| style="background-color: {{Period color|kungurian}}" | 283,5
|-
| style="background-color: {{Period color|artinskian}}" | [[Артинський ярус|Артин]], P<sub>1</sub>art
| 283,5
| style="background-color: {{Period color|artinskian}}" | 290,1
|-
| style="background-color: {{Period color|sakmarian}}" | [[Сакмарський ярус|Сакмарій]], P<sub>1</sub>s
| 290,1
| style="background-color: {{Period color|sakmarian}}" | 295,0
|-
| style="background-color: {{Period color|asselian}}" | [[Ассельський ярус|Ассель]], P<sub>1</sub>a
| 295,0
| style="background-color: {{Period color|asselian}}" | 298,9
|-
| rowspan="7" style="background-color: {{period color|Carboniferouscarboniferous}}"|; [[Carboniferous|Carbonborder-<brtop: />iferous]]{{efn|In2px Northsolid America,grey;" the Carboniferous is subdivided into [[Mississippian age|Mississippian]] and [[PennsylvanianКам'яновугільний (геологія)період|PennsylvanianКарбон]], Periods.}}C
| rowspan="4" style="background-color: {{period color|Pennsylvanianpennsylvanian}}; border-top: 2px solid grey;" | [[Pennsylvanian (геологія)|PennsylvanianПенсильваній]]
| style="background-color: {{period color|Gzheliangzhelian}}; border-top: 2px solid grey;" | [[GzhelianГжельський ярус|Гжель]], C<sub>3</sub>g
| rowspan="4" style="border-top: 2px solid grey;" |
|rowspan="4"| [[Pterygota|Winged insects]] radiate suddenly; some (esp. [[Protodonata]] and [[Palaeodictyoptera]]) are quite large. [[Amphibian]]s common and diverse. First [[reptile]]s and [[coal]] forests ([[Lepidodendron|scale tree]]s, ferns, [[Sigillaria|club tree]]s, [[Calamites|giant horsetail]]s, ''[[Cordaites]]'', etc.). Highest-ever [[Atmosphere of Earth|atmospheric]] [[oxygen]] levels. [[Goniatite]]s, brachiopods, bryozoa, bivalves, and corals plentiful in the seas and oceans. Testate [[foram]]s proliferate. [[Uralian orogeny]] in Europe and Asia. [[Variscan orogeny]] occurs towards middle and late Mississippian Periods.
| style="background-color: {{period color|Gzheliangzhelian}}"|; {{Periodborder-top: start|gzhelian}}2px ±&nbspsolid grey;0.1" |303,7
|-
| style="background-color: {{period color|Kasimoviankasimovian}};" | [[KasimovianКасимовський ярус|Касимов]], C<sub>3</sub>k
| style="background-color: {{period color|Kasimoviankasimovian}};"| {{Period start|kasimovian}} ±&nbsp;307,0.1
|-
| style="background-color: {{period color|Moscovianmoscovian}};" | [[MoscovianМосковський (Carboniferous)ярус|MoscovianМосковій]], C<sub>2</sub>m
| style="background-color: {{period color|Moscovianmoscovian}};"| {{Period start|moscovian}} ±&nbsp;0.315,2
|-
| style="background-color: {{period color|Bashkirianbashkirian}};" | [[BashkirianБашкирський ярус|Башкирій]], C<sub>2</sub>b
| style="background-color: {{period color|Bashkirian}}"| {{Period start|bashkirian}} ±&nbsp;0.4 [[Файл:Clavo" dorado.svg|10px]] 323,2
|-
| rowspan="3" style="background-color: {{period color|Mississippianmississippian}};" | [[Mississippian age|MississippianМіссісіпій]]
| style="background-color: {{period color|Serpukhovianserpukhovian}};" | [[SerpukhovianСерпуховський ярус|Серпуховій]], C<sub>1</sub>s
| rowspan="3" |
|rowspan="3"| Large [[Lycopodiophyta|primitive tree]]s, first [[Tetrapoda|land vertebrate]]s, and amphibious [[eurypterid|sea-scorpion]]s live amid [[coal]]-forming coastal [[brackish water|swamp]]s. Lobe-finned [[rhizodont]]s are dominant big fresh-water predators. In the oceans, early [[Chondrichthyes|shark]]s are common and quite diverse; [[echinoderm]]s (especially [[crinoid]]s and [[blastoid]]s) abundant. [[Coral]]s, [[bryozoa]], [[Goniatitida|goniatite]]s and brachiopods ([[Productida]], [[Spiriferida]], etc.) very common, but [[Trilobita|trilobite]]s and [[nautiloid]]s decline. [[Glaciation]] in East [[Gondwana]]. [[Mayor Island/Tuhua|Tuhua Orogeny]] in New Zealand tapers off.
| style="background-color: {{period color|Serpukhovianserpukhovian}};"| {{Period start|serpukhovian}} ±&nbsp;0.2330,9
|-
| style="background-color: {{period color|visean}};" | [[ViséanВізейський ярус|Візей]], C<sub>1</sub>v
| style="background-color: {{period color|visean}};"| {{Period start|visean}} ±&nbsp;0.4 [[Файл:Clavo dorado.svg|10px]] 346,7
|-
| style="background-color: {{period color|Tournaisiantournaisian}};" | [[TournaisianТурнейський ярус|Турней]], C<sub>1</sub>t
| style="background-color: {{period color|Tournaisiantournaisian}};"| {{Period start|tournaisian}} ±&nbsp;0.4 [[Файл:Clavo dorado.svg|10px]] 358,9
|-
| rowspan="7" style="background-color:{{period color|Devoniandevonian}}; border-top: 2px solid grey;" | [[DevonianДевонський період|Девон]], D
| rowspan="2" style="background-color:{{period color|Lateupper Devoniandevonian}}; border-top: 2px solid grey;" | [[LateПізній Devonianдевон|LateПізній]], D<sub>3</sub>
| style="background-color:{{period color|Famennianfamennian}}; border-top: 2px solid grey;" | [[FamennianФаменський ярус|Фаменій]], D<sub>3</sub>fm
| rowspan="7" style="border-top: 2px solid grey;" |
|rowspan="7"| First [[Lycopodiopsida|clubmoss]]es, [[Equisetophyta|horsetail]]s and [[fern]]s appear, as do the first [[seed]]-bearing plants ([[progymnosperm]]s), first trees (the progymnosperm ''[[Archaeopteris]]''), and first (wingless) [[insect]]s. [[Strophomenida|Strophomenid]] and [[Atrypida|atrypid]] [[brachiopod]]s, [[Rugosa|rugose]] and [[Tabulata|tabulate]] corals, and [[crinoid]]s are all abundant in the oceans. [[Goniatite]] [[Ammonite|ammonoids]] are plentiful, while squid-like [[Coleoidea|coleoids]] arise. Trilobites and armoured agnaths decline, while jawed fishes ([[Placodermi|placoderm]]s, [[Sarcopterygii|lobe-finned]] and [[Osteichthyes|ray-finned]] fish, and early [[Chondrichthyes|sharks]]) rule the seas. First [[amphibian]]s still aquatic. "Old Red Continent" of [[Euramerica]]. Beginning of [[Acadian Orogeny]] for [[Atlas Mountains|Anti-Atlas Mountains]] of North Africa, and [[Appalachian Mountains]] of North America, also the [[Antler Orogeny|Antler]], [[Variscan Orogeny|Variscan]], and [[Mayor Island/Tuhua|Tuhua Orogeny]] in New Zealand.
| style="background-color:{{period color|Famennianfamennian}}"|; {{Periodborder-top: start|famennian}}2px ±&nbspsolid grey;1.6" | [[Файл:Clavo doradoClavo_dorado.svg|10px]] 372,2 ± 1,6
|-
| style="background-color:{{period color|Frasnianfrasnian}};" | [[FrasnianФранський ярус|Франсій]], D<sub>3</sub>f
| style="background-color:{{period color|Frasnian}}"| {{Period start|frasnian}} ±&nbsp;1.6" [[Файл:Clavo dorado.svg|10px]]
|-
| rowspan="2" style="background-color:{{period color|Middlemiddle Devoniandevonian}};" | [[MiddleСередній Devonianдевон|MiddleСередній]], D<sub>2</sub>
| style="background-color:{{period color|Givetiangivetian}};" | [[GivetianЖиветський ярус|Живетій]], D<sub>2</sub>zv
| style="background-color:{{period color|Givetian}}"| {{Period start|givetian}} ±&nbsp;0.8" [[Файл:Clavo dorado.svg|10px]]
|-
| style="background-color:{{period color|Eifelianeifelian}};" | [[EifelianЕйфельський ярус|Ейфельський]], D<sub>2</sub>ef
| style="background-color:{{period color|Eifelian}}"| {{Period start|eifelian}} ±&nbsp;1.2" [[Файл:Clavo dorado.svg|10px]]
|-
| rowspan="3" style="background-color:{{period color|Earlylower Devoniandevonian}}" | [[EarlyРанній Devonianдевон|EarlyРанній]], D<sub>1</sub>
| style="background-color:{{period color|Emsianemsian}};" | [[EmsianЕмський ярус|Емсій]], D<sub>1</sub>e
| style="background-color:{{period color|Emsian}}"| {{Period start|emsian}} ±&nbsp;2.6" [[Файл:Clavo dorado.svg|10px]]
|-
| style="background-color:{{period color|Pragianpragian}};" | [[PragianПразький ярус|Празій]], D<sub>1</sub>p
| style="background-color:{{period color|Pragian}}"| {{Period start|pragian}} ±&nbsp;2.8" [[Файл:Clavo dorado.svg|10px]]
|-
| style="background-color:{{period color|Lochkovianlochkovian}};" | [[LochkovianЛохковський ярус|Лохковій]], D<sub>1</sub>l
| style="background-color:{{period color|Lochkovian}}"| {{Period start|lochkovian}} ±&nbsp;3.2" [[Файл:Clavo dorado.svg|10px]]
|-
| rowspan="8" style="background-color:{{period color|Siluriansilurian}}; border-top: 2px solid grey;" | [[SilurianСилурійський період|Силур]], S
| colspan="2" style="background-color:{{period color|Pridolipridoli}}; border-top: 2px solid grey;" | [[PridoliПржидольська epochепоха|PridoliПржидоль]], S<sub>3</sub>
| rowspan="8" style="border-top: 2px solid grey;" |
|rowspan="8"| First [[vascular plant]]s (the [[rhyniophytes]] and their relatives), first [[millipede]]s and [[Arthropleurida|arthropleurid]]s on land. First [[jawed fish]]es, as well as many [[ostracoderm|armoured]] [[agnatha|jawless fish]], populate the seas. [[Eurypterid|Sea-scorpions]] reach large size. [[Tabulate coral|Tabulate]] and [[Rugosa|rugose]] corals, [[brachiopod]]s (''Pentamerida'', [[Rhynchonellida]], etc.), and [[crinoid]]s all abundant. [[Trilobite]]s and [[mollusk]]s diverse; [[graptolite]]s not as varied. Beginning of [[Caledonian Orogeny]] for hills in England, Ireland, Wales, Scotland, and the [[Scandinavian Mountains]]. Also continued into Devonian period as the [[Acadian Orogeny]], above. [[Taconic Orogeny]] tapers off. [[Lachlan Orogeny]] on [[Australia (continent)|Australian continent]] tapers off.
| style="background-color:{{period color|Pridolipridoli}}"|; {{Periodborder-top: start|pridoli}}2px ±&nbsp;2.3solid [[Файл:Clavogrey;" dorado.svg|10px]] 423,0
|-
| rowspan="2" style="background-color:{{period color|Ludlowludlow}};" | [[LudlowЛудловська epochепоха|LudlowЛудлов]], S<sub>3</sub>
| style="background-color:{{period color|Ludfordianludfordian}};" | [[LudfordianЛудфордський ярус|Лудфордій]], S<sub>3</sub>l
| style="background-color:{{period color|Ludfordianludfordian}};"| {{Period start|ludfordian}} ±&nbsp;0.9 [[Файл:Clavo dorado.svg|10px]] 425,6
|-
| style="background-color:{{period color|Gorstiangorstian}};" | [[GorstianГорстський ярус|Горстій]], S<sub>3</sub>g
| style="background-color:{{period color|Gorstian}}"| {{Period start|gorstian}} ±&nbsp;0.5 [[Файл:Clavo" dorado.svg|10px]] 427,4
|-
| rowspan="2" style="background-color:{{period color|Wenlockwenlock}};" | [[WenlockВенлоцька epochепоха|WenlockВенлок]], S<sub>2</sub>
| style="background-color:{{period color|Homerianhomerian}};" | [[HomerianГомерійський ярус|Гомерій]], S<sub>2</sub>h
| style="background-color:{{period color|Homerian}}"| {{Period start|homerian}} ±&nbsp;0.7 [[Файл:Clavo" dorado.svg|10px]] 430,5
|-
| style="background-color:{{period color|Sheinwoodiansheinwoodian}};" | [[SheinwoodianШейнвудський ярус|Шейнвудій]], S<sub>2</sub>sh
| style="background-color:{{period color|Sheinwoodiansheinwoodian}};"| {{Period start|sheinwoodian}} ±&nbsp;0.8 [[Файл:Clavo dorado.svg|10px]] 433,4
|-
| rowspan="3" style="background-color:{{period color|Llandoveryllandovery}}" | [[LlandoveryЛландоверійська epochепоха|LlandoveryЛландоверій]], S<sub>1</sub>
| style="background-color:{{period color|Telychiantelychian}};" | [[TelychianТелицький ярус|Телицій]], S<sub>1</sub>t
| style="background-color:{{period color|Telychian}}"| {{Period start|telychian}} ±&nbsp;1.1 [[Файл:Clavo" dorado.svg|10px]] 438,5
|-
| style="background-color:{{period color|Aeronianaeronian}};" | [[AeronianАеронський ярус|Аероній]], S<sub>1</sub>a
| style="background-color:{{period color|Aeronian}}"| {{Period start|aeronian}} ±&nbsp;1.2" [[Файл:Clavo dorado.svg|10px]] 440,8
|-
| style="background-color:{{period color|Rhuddanianrhuddanian}};" | [[RhuddanianРудданський ярус|Рудданій]], S<sub>1</sub>r
| style="background-color:{{period color|Rhuddanian}}"| {{Period start|rhuddanian}} ±&nbsp;1.5 [[Файл:Clavo" dorado.svg|10px]] 443,8
|-
| rowspan="7" style="background-color:{{period color|Ordovicianordovician}}; border-top: 2px solid grey;" | [[OrdovicianОрдовицький період|Ордовик]], O
| rowspan="3" style="background-color:{{period color|Lateupper Ordovicianordovician}}; border-top: 2px solid grey;" | [[LateПізній Ordovicianордовик|LateВерхній/Пізній]], O<sub>3</sub>
| style="background-color:{{period color|Hirnantianhirnantian}}; border-top: 2px solid grey;" | [[HirnantianХірнантський ярус|Хірнант]], O<sub>3</sub>h
| rowspan="7" style="border-top: 2px solid grey;" |
|rowspan="7"| [[Invertebrate]]s diversify into many new types (e.g., long [[orthoconic|straight-shelled]] [[orthocerida|cephalopods]]). Early [[coral]]s, articulate [[brachiopod]]s (''Orthida'', ''Strophomenida'', etc.), [[Bivalvia|bivalves]], [[nautiloid]]s, [[trilobite]]s, [[ostracod]]s, [[bryozoa]], many types of [[echinoderms]] ([[crinoid]]s, [[Cystoidea|cystoids]], [[Asteroidea|starfish]], etc.), branched [[graptolite]]s, and other taxa all common. [[Conodont]]s (early [[plankton]]ic [[vertebrate]]s) appear. First [[Embryophyte|green plant]]s and [[fungus|fungi]] on land. Ice age at end of period.
| style="background-color:{{period color|Hirnantian}}"| {{Period start|hirnantian}}&nbsp;±&nbsp;1.4 [[Файлborder-top:Clavo dorado.svg2px solid grey;" |10px]] 445,2
|-
| style="background-color:{{period color|Katiankatian}};" | [[KatianКатійський ярус|Катій]], O<sub>3</sub>k
| style="background-color:{{period color|Katiankatian}};" | {{Period start|katian}}&nbsp;±&nbsp;453,0.7 [[Файл:Clavo dorado.svg|10px]]
|-
| style="background-color:{{period color|Sandbiansandbian}};" | [[SandbianСандбіанський ярус|Сандбіан]], O<sub>3</sub>s
| style="background-color:{{period color|Sandbiansandbian}};"| {{Period start|sandbian}}&nbsp;±&nbsp;0.9 [[Файл:Clavo dorado.svg|10px]] 458,4
|-
| rowspan="2" style="background-color:{{period color|Middlemiddle Ordovicianordovician}};" | [[MiddleСередній Ordovicianордовик|MiddleСередній]], O<sub>2</sub>
| style="background-color:{{period color|Darriwiliandarriwilian}};" | [[DarriwilianДарривільський ярус|Дарривілій]], O<sub>2</sub>drw
| style="background-color:{{period color|Darriwiliandarriwilian}};"| {{Period start|darriwilian}}&nbsp;±&nbsp;1.1 [[Файл:Clavo dorado467.svg|10px]] 3
|-
| style="background-color:{{period color|Dapingiandapingian}};" | [[DapingianДапінзький ярус|Дапінгій]], O<sub>2</sub>, O<sub>2</sub>dpg
| style="background-color:{{period color|Dapingian}}"| {{Period start|dapingian}}&nbsp;±&nbsp;1.4 [[Файл:Clavo" dorado.svg|10px]] 470,0
|-
| rowspan="2" style="background-color:{{period color|Earlyearly Ordovicianordovician}}" | [[EarlyРанній Ordovicianордовик|EarlyНижній/Ранній]], O<sub>1</sub>
| style="background-color:{{period color|Floianfloian}};" | [[FloianФлоський ярус|Флос]]<br, O<sub>1</sub>(formerly [[Arenig]])f
| style="background-color:{{period color|Floian}}"| {{Period start|floian}}&nbsp;±&nbsp;1.4 [[Файл:Clavo" dorado.svg|10px]] 477,7
|-
| style="background-color:{{period color|Tremadociantremadocian}};" | [[TremadocianТремадоцький ярус|Тремадок]], O<sub>1</sub>t
| style="background-color:{{period color|Tremadocian}}"| {{Period start|tremadocian}}&nbsp;±&nbsp;1.9 [[Файл:Clavo" dorado.svg|10px]] 485,4
|-
| rowspan="10" style="background-color:{{period color|Cambriancambrian}}; border-top: 2px solid grey;" | [[CambrianКембрійський період|Кембрій]], <s>C</s>
| rowspan="3" style="background-color:{{period color|Furongianfurongian}}; border-top: 2px solid grey;" | [[FurongianФуронгій]], <s>C</s><sub>4</sub>
| style="background-color:{{period color|Stagestage 10}}; border-top: 2px solid grey;" | ''[[CambrianКембрійський Stageярус 10|StageЯрус 10]]''
| rowspan="10" style="border-top: 2px solid grey;" |
|rowspan="10"| Major diversification of life in the [[Cambrian Explosion]]. Numerous fossils; most modern [[Animalia|animal]] [[Phylum|phyla]] appear. First [[chordate]]s appear, along with a number of extinct, problematic phyla. Reef-building [[Archaeocyatha]] abundant; then vanish. [[Trilobite]]s, [[priapulid]] worms, [[Porifera|sponges]], inarticulate [[brachiopod]]s (unhinged lampshells), and numerous other animals. [[Anomalocarid]]s are giant predators, while many Ediacaran fauna die out. [[Prokaryote]]s, [[protist]]s (e.g., [[foram]]s), [[fungus|fungi]] and [[algae]] continue to present day. [[Gondwana]] emerges. [[Petermann Orogeny]] on the [[Australia (continent)|Australian continent]] tapers off (550&ndash;535 [[Year#SI prefix multipliers|Ma]]). Ross Orogeny in Antarctica. [[Adelaide Geosyncline|Adelaide Geosyncline (Delamerian Orogeny)]], majority of orogenic activity from 514&ndash;500 [[Year#SI prefix multipliers|Ma]]. [[Lachlan Orogeny]] on [[Australia (continent)|Australian continent]], c. 540&ndash;440 [[Year#SI prefix multipliers|Ma]]. [[Atmosphere of Earth|Atmospheric]] CO<sub>2</sub> content roughly 15 times present-day ([[Holocene]]) levels (6000 ppmv compared to today's 400 ppmv)<ref name="Royer" />{{efn|name="atmospheric-carbon-dioxide"}}
| style="background-color:{{period color|Stagestage 10}}; border-top: 2px solid grey;" | ~489.,5
|-
| style="background-color:{{period color|Jiangshanianjiangshanian}};" | [[JiangshanianЦзяншанський ярус|Цзяншань]], <s>C</s><sub>4</sub>j
| style="background-color:{{period color|Jiangshanianjiangshanian}};" | ~494 [[Файл:Clavo dorado.svg|10px]]
|-
| style="background-color:{{period color|Paibianpaibian}};" | [[PaibianПаїбіанський ярус|Паїбіан]], <s>C</s><sub>4</sub>p
| style="background-color:{{period color|Paibianpaibian}};"| ~{{Period start|paibian}} [[Файл:Clavo dorado.svg|10px]] ~497
|-
| rowspan="3" style="background-color:{{period color|Seriesseries 3}};" | [[MiaolingianМяолінзька епоха|Мяолінг]], <s>C</s><sub>3</sub>
| style="background-color:{{period color|Guzhangianguzhangian}};" | [[GuzhangianГужанський ярус|Гужаній]], <s>C</s><sub>3</sub>g
| style="background-color:{{period color|Guzhangianguzhangian}};" | ~{{Period start|guzhangian}} [[Файл:Clavo dorado.svg|10px]] 500,5
|-
| style="background-color:{{period color|Drumiandrumian}};" | [[DrumianДрумійський ярус|Друмій]], <s>C</s><sub>3</sub>d
| style="background-color:{{period color|Drumiandrumian}};" | ~{{Period start|drumian}} [[Файл:Clavo dorado.svg|10px]] 504,5
|-
| style="background-color:{{period color|Stagestage 5}};" | [[WuliuanВулліанський ярус|Вулліан]], <s>C</s><sub>3</sub>w
| style="background-color:{{period color|Stagestage 5}};"| ~{{Period start|cambrian stage 5}}~509
|-
| rowspan="2" style="background-color:{{period color|Seriesseries 2}}" | ''[[CambrianКембрійська Seriesепоха 2|SeriesЕпоха 2]]'', <s>C</s><sub>2</sub>
| style="background-color:{{period color|Stagestage 4}};" | ''[[CambrianКембрійський Stageярус 4|StageЯрус 4]]''
| style="background-color:{{period color|Stagestage 4}};"| ~{{Period start|cambrian stage 4}}~514
|-
| style="background-color:{{period color|Stagestage 3}};" | ''[[CambrianКембрійський Stageярус 3|StageЯрус 3]]''
| style="background-color:{{period color|Stagestage 3}};" | ~{{Period start|cambrian stage 3}}521
|-
| rowspan="2" style="background-color:{{period color|Terreneuvianterreneuvian}}" | [[TerreneuvianТерреновіан]], <s>C</s><sub>1</sub>
| style="background-color:{{period color|Stagestage 2}};" | ''[[CambrianКембрійський Stageярус 2|StageЯрус 2]]''
| style="background-color:{{period color|Stagestage 2}};" | ~{{Period start|cambrian stage 2}}529
|-
| style="background-color:{{period color|Fortunianfortunian}};" | [[FortunianФортунійський ярус|Фортуній]], <s>C</s><sub>1</sub>f
| style="background-color:{{period color|Fortunian}}"| ~{{Period start|fortunian}}&nbsp;±&nbsp;1.0 [[Файл:Clavo" dorado.svg|10px]] 541,0
|-
|rowspan="18" style="text-align:center; background:{{period color|Precambrianprecambrian}}"| [[Precambrian]]{{efnДокембрій|name="aka-cryptozoic"|The [[PrecambrianД<br>о<br>к<br>е<br>м<br>б<br>р<br>і<br>й]] is also known as Cryptozoic.}}
|rowspan="10" style="text-align:center; background:{{period color|proterozoic}}"| [[Протерозой|П<br>р<br>о<br>т<br>е<br>р<br>о<br>з<br>о<br>й]]<br>Pr
|rowspan="10" style="background:{{period color|Proterozoic}}"| [[Proterozoic]]{{efn|name="Precambrian-Time"|The [[Proterozoic]], [[Archean]] and [[Hadean]] are often collectively referred to as the [[Precambrian|Precambrian Time]] or sometimes, also the Cryptozoic.}}
|rowspan="3" style="background:{{period color|Neoproterozoicneoproterozoic}}; border-top: 3px solid grey;"| [[NeoproterozoicНеопротерозой]]{{efn|name="Precambrian-Time"}}
|style="background:{{period color|Ediacaranediacaran}}; border-top: 3px solid grey;"| [[EdiacaranЕдіакарій]]
|colspan="3"| Good [[fossil]]s of the first [[Metazoa|multi-celled animalanimals]]s. [[Ediacaran biota]] flourish worldwide in seas. Simple [[trace fossil]]s of possible worm-like ''[[Trichophycus pedum|Trichophycus]]'', etc. First [[Porifera|spongesponges]]s and [[Trilobita|trilobitomorphtrilobitomorphs]]s. Enigmatic forms include many soft-jellied creatures shaped like bags, disks, or quilts (like ''[[Dickinsonia]]''). [[Taconic Orogeny]] in North America. [[Aravalli Range]] [[orogeny]] in [[Indian Subcontinent]]. Beginning of [[Petermann Orogeny]] on [[Australia (continent)|Australian continent]]. Beardmore Orogeny in Antarctica, 633&ndash;620 [[Year#SI prefix multipliers|Ma]].
|style="background:{{period color|Ediacaranediacaran}}"| ~{{Period start|ediacaran}} [[Файл:Clavo dorado.svg|10px]]
|-
|style="background:{{period color|Cryogeniancryogenian}}"| [[CryogenianКріогеній]]
|colspan="3"| Possible "«[[Snowball Earth]]"» period. [[Fossil]]s still rare. [[Rodinia]] landmass begins to break up. Late Ruker / Nimrod Orogeny in Antarctica tapers off.
|style="background:{{period color|Cryogenian}}"| ~{{Period start|cryogenian}}<!--- -635 to -720 (-850 < 2015) mya -&nbsp;— Cryogenian glaciation --->{{efn|name="absolute-age"|Defined by absolute age ([[Global Standard Stratigraphic Age]]).}}
|-
|style="background:{{period color|Toniantonian}}"| [[TonianТоній]]
|colspan="3"| [[Rodinia]] supercontinent persists. [[Sveconorwegian orogeny]] ends. [[Trace fossil]]s of simple [[multicellular|multi-celled]] [[Eukaryota|eukaryoteeukaryotes]]s. First radiation of [[dinoflagellate]]-like [[acritarch]]s. [[Grenville Orogeny]] tapers off in North America. [[Pan-African orogeny]] in Africa. Lake Ruker / Nimrod Orogeny in Antarctica, 1,000&nbsp;±&nbsp;150 [[Year#SI prefix multipliers|Ma]]. Edmundian Orogeny (c. 920 – 850920—850 [[Year#SI prefix multipliers|Ma]]), [[Gascoyne Complex]], Western Australia. [[Adelaide Geosyncline]] laid down on [[Australia (continent)|Australian continent]], beginning of [[Adelaide Geosyncline|Adelaide Geosyncline (Delamerian Orogeny)]] in Australia.
|style="background:{{period color|Toniantonian}}"| {{Period start|tonian}}{{efn|name="absolute-age"}}
|-
|rowspan="3" style="background:{{period color|Mesoproterozoicmesoproterozoic}}"| [[MesoproterozoicМезопротерозой]]{{efn|name="Precambrian-Time"}}
|style="background:{{period color|Stenianstenian}}"| [[StenianСтеній]]
|colspan="3"| Narrow highly [[Metamorphic rock|metamorphic]] belts due to [[orogeny]] as [[Rodinia]] forms. [[Sveconorwegian orogeny]] starts. Late Ruker / Nimrod Orogeny in Antarctica possibly begins. Musgrave Orogeny (c. 1,080 [[Year#SI prefix multipliers|Ma]]), [[Musgrave Block]], [[Central Australia]].
|style="background:{{period color|Stenian}}"| {{Period start|stenian}}{{efn|name="absolute-age"}}
|-
|style="background:{{period color|Ectasianectasian}}"| [[EctasianЕктазій]]
|colspan="3"| [[Platform cover]]s continue to expand. [[Green algae]] [[colony (biology)|colonies]] in the seas. [[Grenville Orogeny]] in North America.
|style="background:{{period color|Ectasianectasian}}"| {{Period start|ectasian}}{{efn|name="absolute-age"}}
|-
|style="background:{{period color|Calymmiancalymmian}}"| [[CalymmianКалімій]]
|colspan="3"| [[Platform cover]]s expand. Barramundi Orogeny, [[McArthur Basin]], [[Northern Australia]], and Isan Orogeny, [[circa|c.]]1,600 [[Year#SI prefix multipliers|Ma]], Mount Isa Block, Queensland
|style="background:{{period color|Calymmiancalymmian}}"| {{Period start|calymmian}}{{efn|name="absolute-age"}}
|-
|rowspan="4" style="background:{{period color|Paleoproterozoicpaleoproterozoic}}"| [[PaleoproterozoicПалеопротерозой]]{{efn| name="Precambrian-Time"}}
|style="background:{{period color|Statherianstatherian}}"| [[StatherianСтатерій (геологічний період)|Статерій]]
|colspan="3"| First [[Eukaryote|complex single-celled life]]: [[protist]]s with nuclei. [[Columbia (supercontinent)|Columbia]] is the primordial supercontinent. Kimban Orogeny in Australian continent ends. Yapungku Orogeny on [[Yilgarn craton]], in Western Australia. Mangaroon Orogeny, 1,680&ndash;1,620 [[Year#SI prefix multipliers|Ma]], on the [[Gascoyne Complex]] in Western Australia. Kararan Orogeny (1,650 [[Year#SI prefix multipliers|Ma]]), Gawler Craton, [[South Australia]].
|style="background:{{period color|Statherianstatherian}}"| {{Period start|statherian}}{{efn|name="absolute-age"}}
|-
|style="background:{{period color|Orosirianorosirian}}"| [[OrosirianОрозірій]]
|colspan="3"| The [[Atmosphere of Earth|atmosphere]] becomes [[oxygen]]ic. [[Vredefort crater|Vredefort]] and [[Sudbury Basin]] asteroid impacts. Much [[orogeny]]. [[Penokean orogeny|Penokean]] and [[Trans-Hudsonian Orogeny|Trans-Hudsonian Orogenies]] in North America. Early Ruker Orogeny in Antarctica, 2,000–1,700 [[Year#SI prefix multipliers|Ma]]. Glenburgh Orogeny, [[Gascoyne Complex|Glenburgh Terrane]], [[Australia (continent)|Australian continent]] [[circa|c.]] 2,005–1,920 [[Year#SI prefix multipliers|Ma]]. Kimban Orogeny, [[Gawler craton]] in Australian continent begins.
|style="background:{{period color|Orosirian}}"| {{Period start|orosirian}}{{efn|name="absolute-age"}}
|-
|style="background:{{period color|Rhyacianrhyacian}}"| [[Rhyacian]]
|colspan="3"| [[Bushveld Igneous Complex]] forms. [[Huronian]] glaciation.
|style="background:{{period color|Rhyacianrhyacian}}"| {{Period start|rhyacian}}{{efn|name="absolute-age"}}
|-
|style="background:{{period color|Sideriansiderian}}"| [[SiderianСідерій]]
|colspan="3"| [[Oxygen catastrophe]]: [[banded iron formation]]s forms. Sleaford Orogeny on [[Australia (continent)|Australian continent]], [[Gawler Craton]] 2,440&ndash;2,420 [[Year#SI prefix multipliers|Ma]].
|style="background:{{period color|Sideriansiderian}}"| {{Period start|siderian}}{{efn|name="absolute-age"}}
|-
|rowspan="4" style="background:{{period color|Archeanarchean}}"| [[ArcheanАрхей|А<br>р<br>х<br>е<br>й]]{{efn|name="Precambrian-Time"}}<br>Ar
|style="background:{{period color|Neoarcheanneoarchean}}"| [[NeoarcheanНеоархей]]{{efn|name="Precambrian-Time"}}
|colspan="4"| Stabilization of most modern [[craton]]s; possible [[Mantle (геологія)|mantle]] overturn event. Insell Orogeny, 2,650&nbsp;±&nbsp;150 [[Year#SI prefix multipliers|Ma]]. [[Abitibi greenstone belt]] in present-day [[Ontario]] and [[Quebec]] begins to form, stabilizes by 2,600 [[Year#SI prefix multipliers|Ma]].
|style="background:{{period color|Neoarcheanneoarchean}}"| {{Period start|neoarchean}}{{efn|name="absolute-age"}}
|-
|style="background:{{period color|Mesoarcheanmesoarchean}}"| [[MesoarcheanМезоархей]]{{efn|name="Precambrian-Time"}}
|colspan="4"| First [[stromatolite]]s (probably [[colony (biology)|colonial]] [[cyanobacteria]]). Oldest [[macrofossil]]s. Humboldt Orogeny in Antarctica. [[Blake River Megacaldera Complex]] begins to form in present-day [[Ontario]] and [[Quebec]], ends by roughly 2,696 [[Year#SI prefix multipliers|Ma]].
|style="background:{{period color|Mesoarchean}}"| {{Period start|mesoarchean}}{{efn|name="absolute-age"}}
|-
|style="background:{{period color|Paleoarcheanpaleoarchean}}"| [[PaleoarcheanПалеоархей]]{{efn|name="Precambrian-Time"}}
|colspan="4"| First known [[phototroph|oxygen-producing]] [[bacteria]]. Oldest definitive [[microfossils]]. Oldest [[craton]]s on Earth (such as the [[Canadian Shield]] and the [[Pilbara Craton]]) may have formed during this period.{{efn|name="Oldest-craton"|The age of the oldest measurable [[craton]], or [[continental crust]], is dated to 3,600–3,800 Ma.}} Rayner Orogeny in Antarctica.
|style="background:{{period color|Paleoarcheanpaleoarchean}}"| {{Period start|paleoarchean}}{{efn|name="absolute-age"}}
|-
|style="background:{{period color|Eoarcheaneoarchean}}"| [[EoarcheanЕоархей]]{{efn|name="Precambrian-Time"}}
|colspan="4"| [[Prokaryote|Simple single-celled life]] (probably [[bacteria]] and [[archaea]]). Oldest probable [[microfossil]]s. The first [[organism|life formforms]]s and [[self-replication|self-replicating]] [[RNA]] [[molecule]]s evolve around 4,000 [[Year#SI prefix multipliers|Ma]], after the [[Late Heavy Bombardment]] ends on Earth. [[Napier Mountains|Napier]] Orogeny in Antarctica, 4,000&nbsp;±&nbsp;200 [[Year#SI prefix multipliers|Ma]].
|style="background:{{period color|Eoarcheaneoarchean}}"| ~{{Period start|eoarchean}}
|-
|rowspan="4" style="background:{{period color|Hadeanhadean}}"| [[HadeanГадей]]{{efn|name="Precambrian-Time"}}{{efn|name="hadeon-not-formal"|Though commonly used, the [[Hadean]] is not a formal eon<ref name="OggEtAl2016">{{cite book | title=A Concise Geologic Time Scale: 2016 | publisher=Elsevier | first=J.G. | last=Ogg | first2=G. | last2=Ogg | first3=F.M. | last3=Gradstein | year=2016 | pages=20 | isbn=978-0-444-63771-0}}</ref> and no lower bound for the Archean and Eoarchean have been agreed upon. The Hadean has also sometimes been called the Priscoan or the Azoic. Sometimes, the Hadean can be found to be subdivided according to the [[lunar geologic timescale]]. These eras include the [[Cryptic era|Cryptic]] and [[Basin Groups]] (which are subdivisions of the [[Pre-Nectarian]] era), [[Nectarian]], and [[Early Imbrian]] units.}}
|style="background:{{period color|Hadeanhadean}}"| [[EarlyРанній Imbrianімбрій]]<br/> ([[NeohadeanНеогадей]]) (unofficial){{efn|name="Precambrian-Time"}}{{efn|name="Lunar-geologic-timescale-names"|These unit names were taken from the [[lunar geologic timescale]] and refer to geologic events that did not occur on Earth. Their use for Earth geology is unofficial. Note that their start times do not dovetail perfectly with the later, terrestrially defined boundaries.}}
|colspan="4"| Indirect [[photosynthetic]] evidence (e.g., [[kerogen]]) of primordial life. This era overlaps the beginning of the [[Late Heavy Bombardment]] of the [[Inner Solar System|Inner]] [[Solar System]], produced possibly by the planetary migration of [[Neptune]] into the [[Kuiper belt]] as a result of orbital resonances between [[Jupiter]] and [[Saturn]]. Oldest known rock (4,031 to 3,580 [[Year#SI prefix multipliers|Ma]]).<ref name="Oldest-rock">{{cite journal|doi=10.1007/s004100050465|title=Priscoan (4.00&ndash;4.03 Ga) orthogneisses from northwestern Canada|year=1999|last=Bowring|first=Samuel A.|journal=Contributions to Mineralogy and Petrology|volume=134|issue=1|pages=3|last2=Williams|first2=Ian S.|bibcode=1999CoMP..134....3B}} The oldest rock on Earth is the [[Acasta Gneiss]], and it dates to 4.03 Ga, located in the [[Northwest Territories]] of Canada.</ref>
|style="background:{{period color|Hadeanhadean}}"| 4130<ref name="goldblatt2010" />
|-
|style="background:{{period color|Hadeanhadean}}"| [[NectarianНектарній]]<br/> ([[MesohadeanМезогадей]]) (unofficial){{efn|name="Precambrian-Time"}}{{efn|name="Lunar-geologic-timescale-names"}}
|colspan="4"| Possible first appearance of [[plate tectonic]]s. This unit gets its name from the [[lunar geologic timescale]] when the [[Nectaris Basin]] and other greater [[lunar basin]]s form by big [[impact event]]s. Earliest evidence for life based on unusually high amounts of light isotopes of carbon, a common sign of life.
|style="background:{{period color|Hadeanhadean}}"| 4280<ref name="goldblatt2010" />
|-
|style="background:{{period color|Hadeanhadean}}"| [[BasinБасейнові Groupsгрупи]]<br/> ([[PaleohadeanПалеогадей]]) (unofficial){{efn|name="Precambrian-Time"}}{{efn| name="Lunar-geologic-timescale-names"}}
|colspan="4"| Закінчення фази раннього бомбардування планет. Найдавніший знайдений [[мінерал]]&nbsp;— [[циркон]] віком 4,406&nbsp;±&nbsp;0,008&nbsp;мрт<ref name="geology-wisc-edu"/>. [[Астероїд]]и і [[комета|комети]] приносять воду на Землю<ref name="geology-wisc-edu"/>.
|colspan="4"|End of the Early Bombardment Phase. Oldest known [[mineral]] ([[Zircon]], 4,404&nbsp;±&nbsp;8 [[Year#SI prefix multipliers|Ma]]). Asteroids and comets bring water to Earth.<ref name="geology-wisc-edu">{{cite web|url=http://www.geology.wisc.edu/%7Evalley/zircons/Wilde2001Nature.pdf|title=Geology.wisc.edu}}</ref>
|style="background:{{period color|Hadeanhadean}}"| 4533<ref name="goldblatt2010" />
|-
|style="background:{{period color|Hadeanhadean}}"| [[Cryptic era|CrypticКриптій]]<br/> ([[Cryptic era|EohadeanЕогадей]]) (unofficial){{efn|name="Precambrian-Time"}}{{efn|name="Lunar-geologic-timescale-names"}}
|colspan="4"| Формування [[Сонце|Сонця]] і [[Сонячна система|Сонячної системи]] (4,68-4,63&nbsp;мрт). Формування [[Земля|Землі]] (4,567&nbsp;— 4,570&nbsp;мрт), початок фази раннього бомбардування планет. Формування [[Місяць (супутник)|Місяця]] (4,533-4,527&nbsp;мрт), ймовірно через [[Модель ударного формування Місяця|величезне зіткнення]] з невідомим астрономічним тілом.
|colspan="4"| Formation of [[Moon]] (4,533 to 4,527 [[Year#SI prefix multipliers|Ma]]), probably from [[Giant impact hypothesis|giant impact]], since the end of this era. Formation of Earth (4,570 to 4,567.17 [[Year#SI prefix multipliers|Ma]]), Early Bombardment Phase begins. Formation of [[Sun]] (4,680 to 4,630 [[Year#SI prefix multipliers|Ma]]) <!--(Before the Hadean eon)-->.
|style="background:{{period color|Hadeanhadean}}"| {{Period start|hadean}}4570
|}
 
Отримано з https://uk.wikipedia.org/wiki/Геохронологічна_шкала