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dbo:wikiPageRedirects dbr:Ordovician .
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dbo:wikiPageWikiLink dbr:Ordovician .
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dbr:Meguma_terrane dbo:wikiPageWikiLink dbr:Ordovician .
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dbp:age dbr:Ordovician .
dbr:Brace_Mountain dbo:wikiPageWikiLink dbr:Ordovician ;
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dbr:Clingmans_Dome dbo:wikiPageWikiLink dbr:Ordovician .
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dbp:age dbr:Ordovician .
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dbp:age dbr:Ordovician .
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dbr:Galena_Group dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Garrard_Siltstone dbo:wikiPageWikiLink dbr:Ordovician ;
dbp:age dbr:Ordovician .
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@prefix wikipedia-en: .
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dbr:Cotter_Formation dbo:wikiPageWikiLink dbr:Ordovician ;
dbp:age dbr:Ordovician .
dbr:Temple_Butte_Formation dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Jefferson_City_Formation dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Sunblood_Formation dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Vinini_Formation dbo:wikiPageWikiLink dbr:Ordovician ;
dbp:age dbr:Ordovician .
dbr:Charlottetown_Boulder_Park dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Chepultepec_Formation dbo:wikiPageWikiLink dbr:Ordovician .
dbr:John_Boyd_Thacher_State_Park dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Kimmswick_Limestone dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Lahaska_Creek dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Lake_Engure_Nature_Park dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Lawn_Hill_crater dbo:wikiPageWikiLink dbr:Ordovician ;
dbp:age dbr:Ordovician .
dbr:Cockeysville_Marble dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Highland_Rim dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Manitou_Limestone dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Maquoketa_Formation dbo:wikiPageWikiLink dbr:Ordovician .
dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Knob_Noster_State_Park dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Kotelny_Island dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Natural_Tunnel_State_Park dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Red_River_Formation dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Champlain_Thrust dbo:wikiPageWikiLink dbr:Ordovician .
dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Worthington_Mountains dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Oklahoma_City_Oil_Field dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Everton_Dolomite dbo:wikiPageWikiLink dbr:Ordovician ;
dbp:age dbr:Ordovician .
dbr:Everton_Formation dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Paleontology_in_Wisconsin dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Trifolium_friscanum dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Zonguldak_basin dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Richards_Spur dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Paleontology_in_Michigan dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Bennett_Island dbo:wikiPageWikiLink dbr:Ordovician .
dbr:De_Long_Islands dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Geology_of_Hainan_Island dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Germany_Valley dbo:wikiPageWikiLink dbr:Ordovician .
dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Paleontology_in_Tennessee dbo:wikiPageWikiLink dbr:Ordovician .
dbo:wikiPageWikiLink dbr:Ordovician .
dbo:wikiPageWikiLink dbr:Ordovician .
dbo:wikiPageWikiLink dbr:Ordovician .
dbo:wikiPageWikiLink dbr:Ordovician .
dbo:wikiPageWikiLink dbr:Ordovician .
dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Cincinnati_Arch dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Pencader_Tunnel dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Frencrinuroides dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Ignacio_Formation dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Cape_Rawson_Formation dbo:wikiPageWikiLink dbr:Ordovician .
dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Blue_Mountain_Formation dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Brent_crater dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Elwin_Inlet dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Monkhead dbo:wikiPageWikiLink dbr:Ordovician ;
dbp:age dbr:Ordovician .
dbr:Mount_Paul dbo:wikiPageWikiLink dbr:Ordovician ;
dbp:age dbr:Ordovician .
dbr:Mount_Pleasant_Caldera dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Orthocone dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Annieopsquotch_Mountains dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Bathurst_Mining_Camp dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Maligne_Mountain dbo:wikiPageWikiLink dbr:Ordovician ;
dbp:age dbr:Ordovician .
dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Denella dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Gabriceraurus dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Hapsiceraurus dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Happy_Valley_Forest dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Spinodus dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Nealeodus dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Ontario_Highway_36 dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Orcanopterus dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Ceratiocaris dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Raymondaspis dbo:wikiPageWikiLink dbr:Ordovician .
dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Ireland dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Marble dbo:wikiPageWikiLink dbr:Ordovician .
dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Ooid dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Mollusca dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Gastropoda dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Shropshire dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Botany dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Anglesey dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Calcite dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Wyangala dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Lachlan_Fold_Belt dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Trace_fossil dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Paibi dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Endocerida dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Eurypterid dbo:wikiPageWikiLink dbr:Ordovician .
dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Geography_of_Illinois dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Geology_of_Illinois dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Yorkshire_Dales dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Variscan_orogeny dbo:wikiPageWikiLink dbr:Ordovician .
dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Johan_Wilhelm_Dalman dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Geology_of_the_Iberian_Peninsula dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Scafells dbo:wikiPageWikiLink dbr:Ordovician .
dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Lodge_Hill_Cemetery dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Panasqueira dbo:wikiPageWikiLink dbr:Ordovician .
dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Orbicular_granite dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Sierra_de_la_Culebra dbo:wikiPageWikiLink dbr:Ordovician ;
dbp:age dbr:Ordovician .
dbr:Slate_industry_in_Spain dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Petermann_Orogeny dbo:wikiPageWikiLink dbr:Ordovician .
dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Western_Block_of_the_North_China_Craton dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Thiviers-Payzac_Unit dbo:wikiPageWikiLink dbr:Ordovician .
dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Plectronoceratoidea dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Plectronocerida dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Neocephalopoda dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Tarphycerida dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Discosorida dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Ascocerida dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Oncocerida dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Bajkaloceras dbo:wikiPageWikiLink dbr:Ordovician .
dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Geology_of_Ceredigion dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Cambrian_Mountains dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Tuareg_Shield dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Asaphus dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Geology_of_Lithuania dbo:wikiPageWikiLink dbr:Ordovician .
dbo:wikiPageWikiLink dbr:Ordovician .
dbr:Kittatinny_Mountain dbo:wikiPageWikiLink dbr:Ordovician .
dbo:wikiPageWikiLink dbr:Ordovician .
@prefix rdf: .
@prefix yago: .
dbr:Ordovician rdf:type yago:PhysicalEntity100001930 ,
yago:WikicatFossils ,
yago:Dodo110022908 ,
yago:Oldster110376523 ,
yago:YagoLegalActorGeo ,
yago:YagoLegalActor ,
yago:Adult109605289 .
@prefix owl: .
dbr:Ordovician rdf:type owl:Thing ,
dbo:Country ,
yago:Organism100004475 ,
yago:LivingThing100004258 ,
yago:CausalAgent100007347 ,
yago:Whole100003553 ,
yago:Object100002684 ,
yago:Person100007846 .
@prefix geo: .
dbr:Ordovician rdf:type geo:SpatialThing .
@prefix rdfs: .
dbr:Ordovician rdfs:label "Ordovicium"@sv ,
"Ordoviciano"@it ,
"Ordovik"@cs ,
"\u30AA\u30EB\u30C9\u30D3\u30B9\u7D00"@ja ,
"\u041E\u0440\u0434\u043E\u0432\u0438\u043A\u0441\u043A\u0438\u0439 \u043F\u0435\u0440\u0438\u043E\u0434"@ru ,
"Ordov\u00EDcico"@es ,
"Ordovicien"@fr ,
"\u5965\u9676\u7EAA"@zh ,
"\u039F\u03C1\u03B4\u03BF\u03B2\u03AF\u03BA\u03B9\u03B1 \u03C0\u03B5\u03C1\u03AF\u03BF\u03B4\u03BF\u03C2"@el ,
"Ordowik"@pl ,
"Ordovisium"@in ,
"Ordoviziar"@eu ,
"Ordovicio"@eo ,
"Ordovicium"@nl ,
"\u041E\u0440\u0434\u043E\u0432\u0438\u0446\u044C\u043A\u0438\u0439 \u043F\u0435\u0440\u0456\u043E\u0434"@uk ,
"\u0627\u0644\u0639\u0635\u0631 \u0627\u0644\u0623\u0648\u0631\u062F\u0648\u0641\u064A\u0634\u064A"@ar ,
"Ordovizium"@de ,
"Ordoviciano"@pt ,
"Ordovici\u00E0"@ca ,
"Ordovician"@en ,
"\uC624\uB974\uB3C4\uBE44\uC2A4\uAE30"@ko ;
rdfs:comment "Ordovicium \u00E4r en geologisk period i den paleozoiska eran. Den b\u00F6rjade vid kambriums slut 485 miljoner \u00E5r f\u00F6re nutid och slutade n\u00E4r silur tog vid 444 miljoner \u00E5r f\u00F6re nutid. Den senare delen av ordovicium k\u00E4nnetecknas av en stor nedisning p\u00E5 Gondwana, den s\u00E5 kallade Hirnantiska istiden. Detta ledde till att havsniv\u00E5n sj\u00F6nk och livsutrymmet f\u00F6r alla marina organismer minskade. Man tror att denna istid var en av anledningarna till det stora massutd\u00F6ende som finns registrerat i det fossila arkivet."@sv ,
"\uC624\uB974\uB3C4\uBE44\uC2A4\uAE30(Ordovician)\uB294 \uACE0\uC0DD\uB300\uC758 6\uAC1C \uAE30 \uC911\uC5D0\uC11C \uB450 \uBC88\uC9F8 \uAE30\uC774\uB2E4. \uCE84\uBE0C\uB9AC\uC544\uAE30 \uB2E4\uC74C\uC5D0 \uC624\uBA70, \uC2E4\uB8E8\uB9AC\uC544\uAE30\uBCF4\uB2E4 \uC804\uC774\uB2E4. \uC624\uB974\uB3C4\uBE44\uC2A4\uAE30\uB77C\uB294 \uC774\uB984\uC740 \uC6E8\uC77C\uC2A4\uC9C0\uBC29\uC758 \uC624\uB974\uB3C4\uBE44\uC2A4 \uBD80\uC871\uC73C\uB85C\uBD80\uD130 \uC720\uB798\uD558\uC600\uC73C\uBA70 1879\uB144 \uAC00 \uC815\uC758\uD558\uC600\uB2E4. \uC774 \uC804\uC5D0\uB294 \uACFC \uC774 \uBD81\uC6E8\uC77C\uC2A4\uC758 \uC554\uC11D\uCE35\uC744 \uCE84\uBE0C\uB9AC\uC544\uAE30\uB85C \uB123\uC744 \uAC83\uC778\uC9C0 \uC2E4\uB8E8\uB9AC\uC544\uAE30\uB85C \uB123\uC744\uAC83\uC778\uC9C0\uC5D0 \uAD00\uD55C \uB17C\uC7C1\uC774 \uC788\uC5C8\uB2E4. \uB7A9\uC6CC\uC2A4\uB294 \uBB38\uC81C\uAC00 \uB418\uB294 \uC554\uC11D\uCE35\uC758 \uD654\uC11D \uC0DD\uBB3C\uAD70\uC774 \uCE84\uBE0C\uB9AC\uC544\uAE30\uC640\uB3C4 \uC2E4\uB8E8\uB9AC\uC544\uAE30\uC640\uB3C4 \uB2E4\uB978\uAC83\uC744 \uD655\uC778\uD558\uACE0, \uC774 \uCE35\uC774 \uC0C8\uB86D\uAC8C \uB3C5\uB9BD\uB418\uC5B4\uC57C \uD568\uC744 \uC54C\uAC8C \uB418\uC5C8\uB2E4. \uC624\uB974\uB3C4\uBE44\uC2A4\uAE30\uAC00 \uC778\uC815\uB418\uB294 \uAC83\uC740 \uC601\uAD6D\uC5D0\uC11C\uB294 \uC624\uB79C \uC2DC\uAC04\uC774 \uD544\uC694\uD588\uC9C0\uB9CC, \uB2E4\uB978 \uACF3\uC5D0\uC11C\uB294 \uACE7 \uBC1B\uC544\uB4E4\uC5EC\uC84C\uB2E4. \uADF8\uB9AC\uACE0 1906\uB144\uC5D0 \uACE0\uC0DD\uB300\uC758 \uD55C \uAE30\uB85C \uACF5\uC778\uB418\uC5C8\uB2E4."@ko ,
"\u0627\u0644\u0623\u0648\u0631\u062F\u0641\u064A\u0634\u064A \u0623\u0648 \u0627\u0644\u0623\u0631\u062F\u0648\u0641\u064A\u0633\u064A \u0623\u0648 \u0627\u0644\u0623\u0648\u0631\u062F\u0648\u0641\u064A\u0643\u064A (\u0628\u0627\u0644\u0644\u0627\u062A\u064A\u0646\u064A\u0629: Ordovician)\u060C \u0648\u0647\u0648 \u062B\u0627\u0646\u064A \u0627\u0644\u0639\u0635\u0648\u0631 \u0627\u0644\u0633\u062A\u0629 \u0645\u0646 \u062D\u0642\u0628\u0629 \u0627\u0644\u062D\u064A\u0627\u0629 \u0627\u0644\u0642\u062F\u064A\u0645\u0629 \u0648\u062F\u0647\u0631 \u0627\u0644\u0628\u0634\u0627\u0626\u0631\u060C \u0627\u0645\u062A\u062F \u0645\u0646 485.4 \u00B1 1.9 \u0625\u0644\u0649 443.8 \u00B1 1.5 \u0645\u0644\u064A\u0648\u0646 \u0633\u0646\u0629 \u0645\u0636\u062A\u060C \u0644\u0645\u062F\u0629 41.6 \u0645\u0644\u064A\u0648\u0646 \u0633\u0646\u0629 \u062A\u0642\u0631\u064A\u0628\u0627. \u064A\u0633\u0628\u0642\u0647 \u0627\u0644\u0643\u0627\u0645\u0628\u0631\u064A\u060C \u0648\u064A\u0644\u064A\u0647 \u0627\u0644\u0633\u064A\u0644\u0648\u0631\u064A."@ar ,
"Na escala de tempo geol\u00F3gico, o Ordoviciano ou Ordov\u00EDcico \u00E9 o per\u00EDodo da era Paleozoica do \u00E9on Fanerozoico que est\u00E1 compreendido h\u00E1 entre 488 a 443 milh\u00F5es de anos aproximadamente. O per\u00EDodo Ordoviciano sucede o per\u00EDodo Cambriano e precede o per\u00EDodo Siluriano, ambos de sua era. Divide-se nas \u00E9pocas Ordoviciana Inferior, Ordoviciana M\u00E9dia e Ordoviciana Superior, da mais antiga para a mais recente."@pt ,
"Het Ordovicium is een periode uit de geologische tijdschaal (of een systeem in de stratigrafie), die ongeveer van 485 tot 443 miljoen jaar geleden duurde. Het Ordovicium is onderdeel van het Paleozo\u00EFcum, het volgt op het Cambrium en wordt opgevolgd door het Siluur."@nl ,
"\u5965\u9676\u7EAA\uFF08\u82F1\u8A9E\uFF1AOrdovician\uFF0C\u767C\u97F3\uFF1A /\u0254\u02D0rd\u0259\u02C8v\u026A\u0283\u0259n/\uFF0C\u7B26\u53F7O\uFF09\u662F\u5730\u8D28\u65F6\u4EE3\u4E2D\u663E\u751F\u5B99\u53E4\u751F\u4EE3\u7684\u7B2C\u4E8C\u4E2A\u7EAA\uFF0C\u7EA6\u5F00\u59CB\u4E8E4.85\u4EBF\u5E74\u524D\uFF0C\u7ED3\u675F\u4E8E4.43\u4EBF\u5E74\u524D\u3002"@zh ,
"\u30AA\u30EB\u30C9\u30D3\u30B9\u7D00\uFF08\u30AA\u30EB\u30C9\u30D3\u30B9\u304D\u3001Ordovician period\uFF09\u3068\u306F\u3001\u5730\u8CEA\u6642\u4EE3\u3001\u53E4\u751F\u4EE3\u524D\u671F\u306B\u304A\u3051\u308B\u533A\u5206\u3067\u3001\u7D044\u51048830\u4E07\u5E74\u524D\u304B\u3089\u7D044\u51044370\u4E07\u5E74\u524D\u307E\u3067\u3092\u6307\u3059\u3002\u30AA\u30EB\u30C9\u30D3\u30B9\u306E\u540D\u524D\u306F\u3001\u6A21\u5F0F\u5730\u3067\u3042\u308B\u30A6\u30A7\u30FC\u30EB\u30BA\u5730\u65B9\u306B\u4F4F\u3093\u3067\u3044\u305F\u53E4\u4EE3\u30B1\u30EB\u30C8\u7CFB\u90E8\u65CF\u300C\u300D(Ordovices) \u304B\u3089\u3064\u3044\u305F\u3002\u5965\u9676\u7D00\uFF08\u304A\u3046\u3068\u3046\u304D\uFF09\u3068\u3082\u3044\u3046\u3002 \u30AA\u30EB\u30C9\u30D3\u30B9\u7D00\u306F\u3001\u751F\u7269\u306E\u591A\u69D8\u5316\u304C\u30AB\u30F3\u30D6\u30EA\u30A2\u7D00\u4E26\u306B\u9032\u3093\u3060\u6642\u4EE3\u3067\u3042\u308B\u3002\u30AA\u30A6\u30E0\u30AC\u30A4\u306B\u4EE3\u8868\u3055\u308C\u308B\u8EDF\u4F53\u52D5\u7269\u3084\u4E09\u8449\u866B\u306E\u3088\u3046\u306A\u7BC0\u8DB3\u52D5\u7269\u3001\u7B46\u77F3\u306E\u3088\u3046\u306A\u534A\u7D22\u52D5\u7269\u304C\u6804\u3048\u305F\u3002\u307E\u305F\u3001\u30AA\u30EB\u30C9\u30D3\u30B9\u7D00\u5F8C\u671F\u306B\u306F\u984E\u3092\u6301\u3064\u9B5A\u985E\u304C\u767B\u5834\u3057\u305F\u3002 \u30AA\u30EB\u30C9\u30D3\u30B9\u7D00\u672B\u306B\u306F\u5927\u91CF\u7D76\u6EC5\u304C\u8D77\u3053\u3063\u305F\u3002"@ja ,
"Ordovicio estas la 2-a epoko de la paleozoika erao, kiam aperis la senmakzelaj fi\u015Doj (prafi\u015Doj), cefalopodoj (na\u016Dtiloj). \u011Ci da\u016Dris de 488 \u011Dis 444 milionoj da jaroj. \u011Cin sekvis silurio."@eo ,
"\u041E\u0440\u0434\u043E\u0301\u0432\u0438\u043A\u0441\u043A\u0438\u0439 \u043F\u0435\u0440\u0438\u0301\u043E\u0434 (\u043E\u0440\u0434\u043E\u0301\u0432\u0438\u043A) \u2014 \u0432\u0442\u043E\u0440\u043E\u0439 \u043F\u0435\u0440\u0438\u043E\u0434 \u043F\u0430\u043B\u0435\u043E\u0437\u043E\u0439\u0441\u043A\u043E\u0439 \u044D\u0440\u044B. \u041D\u0430\u0441\u0442\u0443\u043F\u0438\u043B \u0437\u0430 \u043A\u0435\u043C\u0431\u0440\u0438\u0439\u0441\u043A\u0438\u043C \u043F\u0435\u0440\u0438\u043E\u0434\u043E\u043C \u0438 \u0441\u043C\u0435\u043D\u0438\u043B\u0441\u044F \u0441\u0438\u043B\u0443\u0440\u0438\u0439\u0441\u043A\u0438\u043C. \u041F\u0440\u043E\u0434\u043E\u043B\u0436\u0430\u043B\u0441\u044F \u043E\u0442 485,4 \u00B1 1,9 \u0434\u043E 443,8 \u00B1 1,5 \u043C\u043B\u043D \u043B\u0435\u0442 \u043D\u0430\u0437\u0430\u0434 (\u043E\u043A\u043E\u043B\u043E 42 \u043C\u043B\u043D \u043B\u0435\u0442). \u041A\u043E\u043C\u043F\u043B\u0435\u043A\u0441 \u043E\u0442\u043B\u043E\u0436\u0435\u043D\u0438\u0439 (\u0433\u043E\u0440\u043D\u044B\u0445 \u043F\u043E\u0440\u043E\u0434), \u0441\u043E\u043E\u0442\u0432\u0435\u0442\u0441\u0442\u0432\u0443\u044E\u0449\u0438\u0445 \u044D\u0442\u043E\u043C\u0443 \u043F\u0435\u0440\u0438\u043E\u0434\u0443, \u043D\u0430\u0437\u044B\u0432\u0430\u0435\u0442\u0441\u044F \u043E\u0440\u0434\u043E\u0432\u0438\u043A\u0441\u043A\u043E\u0439 \u0441\u0438\u0441\u0442\u0435\u043C\u043E\u0439."@ru ,
"\u041E\u0440\u0434\u043E\u0432\u0438\u0446\u044C\u043A\u0438\u0439 \u043F\u0435\u0440\u0456\u043E\u0434, \u043E\u0440\u0434\u043E\u0432\u0438\u043A (\u0440\u043E\u0441. \u043E\u0440\u0434\u043E\u0432\u0438\u043A\u0441\u043A\u0438\u0439 \u043F\u0435\u0440\u0438\u043E\u0434, \u043E\u0440\u0434\u043E\u0432\u0438\u043A, \u0430\u043D\u0433\u043B. Ordovician period, \u043D\u0456\u043C. Ordoviz(ium) n) \u2014 \u0434\u0440\u0443\u0433\u0438\u0439 \u0433\u0435\u043E\u043B\u043E\u0433\u0456\u0447\u043D\u0438\u0439 \u043F\u0435\u0440\u0456\u043E\u0434 \u043F\u0430\u043B\u0435\u043E\u0437\u043E\u0439\u0441\u044C\u043A\u043E\u0457 \u0435\u0440\u0438. \u041D\u0430\u0437\u0432\u0430 \u043F\u043E\u0445\u043E\u0434\u0438\u0442\u044C \u0432\u0456\u0434 \u043D\u0430\u0437\u0432\u0438 \u0441\u0442\u0430\u0440\u043E\u0434\u0430\u0432\u043D\u044C\u043E\u0433\u043E \u043F\u043B\u0435\u043C\u0435\u043D\u0456 \u043E\u0440\u0434\u043E\u0432\u0438\u043A\u0456\u0432, \u0449\u043E \u043C\u0435\u0448\u043A\u0430\u043B\u043E \u0432 \u0423\u0435\u043B\u044C\u0441\u0456."@uk ,
"Das Ordovizium ist das zweite chronostratigraphische System (bzw. Periode in der Geochronologie) des Pal\u00E4ozoikums in der Erdgeschichte. Das Ordovizium begann vor etwa 485,4 Millionen Jahren und endete vor rund 443,4 Millionen Jahren. Es wird vom Kambrium unterlagert, die Schichten des Kambriums sind also die \u00E4ltesten des Pal\u00E4ozoikums. Auf das Ordovizium folgt das Silur."@de ,
"L'Ordovici\u00E0 \u00E9s el per\u00EDode geol\u00F2gic que comen\u00E7\u00E0 fa 485,4 \u00B1 1,9 milions d'anys i s'acab\u00E0 fa 443,8 \u00B1 1,5 milions d'anys. Es tracta del segon per\u00EDode de l'era del Paleozoic. El seu nom fa refer\u00E8ncia als ordovics, l'\u00FAltima tribu gal\u00B7lesa que se sotmet\u00E9 als romans, i al fet que les roques utilitzades per descriure el per\u00EDode es troben a l'antic territori dels ordovics al nord de Gal\u00B7les."@ca ,
"Ordoviziarra Paleozoikoko bigarren garaia da, Kanbriarraren ondoren eta Siluriarraren aurretik. Berez bi garai hauen artean zeuden harri batzuen inguruko eztabaidarekin bukatzeko izendatu zuen Charles Lapworthek 1879an. Ofizialki 1906an onartu zuen Geologiako Nazioarteko Kongresuak. Orain dela 488.3 milioi urte hasi zen eta orain dela 443.7 milioi urte bukatu. Biak handiekin bat egiten duten garaiak dira. Ordoviziar garaia zatitzeko honako atalak bereizten dira: \n* Behe Ordoviziarra: ( eta ) \n* Ordoviziar ertaina: (Caradoc, , Llandeilo) \n* Goi Ordoviziarra: (Ashgill)"@eu ,
"Ordovik je geologick\u00FD \u00FAtvar star\u0161\u00EDch prvohor (paleozoikum) a je tedy tak\u00E9 sou\u010D\u00E1st\u00ED e\u00F3nu fanerozoika. N\u00E1zev podle starov\u011Bk\u00E9ho kmene Ordovik\u016F (ve Walesu ob\u00FDvali \u00FAzem\u00ED severn\u011B od Silur\u016F) zavedl Charles Lapworth roku 1879 pro ulo\u017Eeniny tzv. druh\u00E9 fauny, kter\u00FDm v \u010Cech\u00E1ch odpov\u00EDdala Barrandova etapa D. N\u00E1zev s\u00E1m byl v\u0161ak kodifikov\u00E1n a\u017E na 21. geologick\u00E9m kongresu v Kodani roku 1960."@cs ,
"L'Ordoviciano \u00E8 il secondo dei sei (sette in Nord America) periodi geologici in cui \u00E8 suddivisa l'era geologica paleozoica e copre il periodo di tempo tra 485,4\u00B11,9 e 443,8\u00B11,5 milioni di anni fa. Segue il periodo Cambriano ed \u00E8 seguito dal periodo Siluriano."@it ,
"Ordowik (ang. Ordovician) \n* w sensie geochronologicznym \u2013 drugi okres ery paleozoicznej. Trwa\u0142 oko\u0142o 42 miliony lat (od 485,4\u202F\u00B1\u202F1,9 do 443,4\u202F\u00B1\u202F1,5 milion\u00F3w lat temu). Ordowik dzieli si\u0119 na trzy epoki: ordowik wczesny, ordowik \u015Brodkowy i ordowik p\u00F3\u017Any. \n* w sensie chronostratygraficznym \u2013 drugi system eratemu paleozoicznego, wy\u017Cszy od kambru, ni\u017Cszy od syluru. Dzieli si\u0119 na trzy oddzia\u0142y: ordowik dolny, ordowik \u015Brodkowy i ordowik g\u00F3rny. Mi\u0119dzynarodowy stratotyp granicy kambr/ordowik znajduje si\u0119 na Green Point (zachodnie wybrze\u017Ce Nowej Fundlandii, Kanada). Dolna granica ordowiku oparta jest o pierwsze pojawienie si\u0119 konodonta Iapetognathus fluctivagus."@pl ,
"\u0397 \u039F\u03C1\u03B4\u03BF\u03B2\u03AF\u03BA\u03B9\u03B1 \u03C0\u03B5\u03C1\u03AF\u03BF\u03B4\u03BF\u03C2 \u03B5\u03AF\u03BD\u03B1\u03B9 \u03BC\u03AF\u03B1 \u03B3\u03B5\u03C9\u03BB\u03BF\u03B3\u03B9\u03BA\u03AE \u03C0\u03B5\u03C1\u03AF\u03BF\u03B4\u03BF\u03C2 \u03C4\u03B7\u03C2 \u03A0\u03B1\u03BB\u03B1\u03B9\u03BF\u03B6\u03C9\u03B9\u03BA\u03AE\u03C2 \u03BA\u03B1\u03B9 \u03B5\u03BA\u03C4\u03B5\u03AF\u03BD\u03B5\u03C4\u03B1\u03B9 \u03C3\u03B5 \u03C7\u03C1\u03BF\u03BD\u03B9\u03BA\u03CC \u03B4\u03B9\u03AC\u03C3\u03C4\u03B7\u03BC\u03B1 488,3 \u00B1 1,7 \u03AD\u03C9\u03C2 443,7 \u00B1 1,5 \u03B5\u03BA\u03B1\u03C4\u03BF\u03BC\u03BC\u03CD\u03C1\u03B9\u03B1 \u03AD\u03C4\u03B7 \u03C0.\u03C0. (ICS, 2004). \u0391\u03BA\u03BF\u03BB\u03BF\u03C5\u03B8\u03B5\u03AF \u03C4\u03B7\u03BD \u039A\u03AC\u03BC\u03B2\u03C1\u03B9\u03B1 \u03C0\u03B5\u03C1\u03AF\u03BF\u03B4\u03BF \u03BA\u03B1\u03B9 \u03B1\u03BA\u03BF\u03BB\u03BF\u03C5\u03B8\u03B5\u03AF\u03C4\u03B1\u03B9 \u03B1\u03C0\u03CC \u03C4\u03B7 \u03A3\u03B9\u03BB\u03BF\u03CD\u03C1\u03B9\u03B1 \u03C0\u03B5\u03C1\u03AF\u03BF\u03B4\u03BF. \u0388\u03BB\u03B1\u03B2\u03B5 \u03C4\u03BF \u03CC\u03BD\u03BF\u03BC\u03AC \u03C4\u03B7\u03C2 \u03B1\u03C0\u03CC \u03C4\u03B7\u03BD \u03BF\u03C5\u03B1\u03BB\u03B9\u03BA\u03AE \u03C6\u03C5\u03BB\u03AE \u03C4\u03C9\u03BD \u039F\u03C1\u03B4\u03BF\u03B2\u03AF\u03BA\u03C9\u03BD. \u03A0\u03B1\u03C1\u03AC \u03C4\u03BF \u03B3\u03B5\u03B3\u03BF\u03BD\u03CC\u03C2 \u03CC\u03C4\u03B9 \u03B7 \u03B1\u03BD\u03B1\u03B3\u03BD\u03CE\u03C1\u03B9\u03C3\u03AE \u03C4\u03B7\u03C2 \u03C9\u03C2 \u03B4\u03B9\u03B1\u03BA\u03C1\u03B9\u03C4\u03AE \u03B3\u03B5\u03C9\u03BB\u03BF\u03B3\u03B9\u03BA\u03AE \u03C0\u03B5\u03C1\u03AF\u03BF\u03B4\u03BF\u03C2 \u03AC\u03C1\u03B3\u03B7\u03C3\u03B5 \u03C3\u03C4\u03BF \u0397\u03BD\u03C9\u03BC\u03AD\u03BD\u03BF \u0392\u03B1\u03C3\u03AF\u03BB\u03B5\u03B9\u03BF, \u03AD\u03B3\u03B9\u03BD\u03B5 \u03B3\u03C1\u03AE\u03B3\u03BF\u03C1\u03B1 \u03B1\u03C0\u03BF\u03B4\u03B5\u03BA\u03C4\u03AE \u03C3\u03B5 \u03AC\u03BB\u03BB\u03B5\u03C2 \u03C7\u03CE\u03C1\u03B5\u03C2 \u03BA\u03B1\u03B9 \u03C5\u03B9\u03BF\u03B8\u03B5\u03C4\u03AE\u03B8\u03B7\u03BA\u03B5 \u03B5\u03C0\u03AF\u03C3\u03B7\u03BC\u03B1 \u03C4\u03BF 1906, \u03C9\u03C2 \u03C0\u03B5\u03C1\u03AF\u03BF\u03B4\u03BF\u03C2 \u03C4\u03B7\u03C2 \u03C0\u03B1\u03BB\u03B1\u03B9\u03BF\u03B6\u03C9\u03B9\u03BA\u03AE\u03C2 \u03B5\u03C0\u03BF\u03C7\u03AE\u03C2 \u03B1\u03C0\u03CC \u03C4\u03BF ."@el ,
"Ordovisium adalah suatu periode pada era Paleozoikum yang berlangsung antara 488,3 \u00B1 1,7 hingga 443,7 \u00B1 1,5 juta tahun lalu. Periode ini melanjutkan periode Kambrium dan diikuti oleh periode Silur. Periode yang mendapat namanya dari salah satu suku di Wales, Ordovices, ini didefinisikan oleh pada tahun 1879 untuk menyelesaikan persengketaan antara pengikut Adam Sedgwick dan yang masing-masing mengelompokkan yang sama di Wales utara masuk dalam periode Kambrium dan Silur. Lapworth mengamati bahwa fosil fauna pada strata yang dipersengketakan ini berbeda dengan fauna pada periode Kambrium maupun Silur sehingga seharusnya memiliki periode tersendiri."@in ,
"The Ordovician (/\u0254\u02D0rd\u0259\u02C8v\u026A\u0283i.\u0259n, -do\u028A-, -\u02C8v\u026A\u0283\u0259n/ or-d\u0259-VISH-ee-\u0259n, -\u2060doh-, -\u2060VISH-\u0259n) is a geologic period and system, the second of six periods of the Paleozoic Era. The Ordovician spans 41.6 million years from the end of the Cambrian Period 485.4 million years ago (Mya) to the start of the Silurian Period 443.8 Mya."@en ,
"El Ordov\u00EDcico es la fragmentaci\u00F3n de la escala temporal geol\u00F3gica que pertenece a la Era Paleozoica; esta se divide en seis periodos de los que el Ordov\u00EDcico ocupa el segundo lugar posterior al C\u00E1mbrico y precediendo al Sil\u00FArico. Comenz\u00F3 hace unos 485 millones de a\u00F1os y termin\u00F3 hace unos 444 millones de a\u00F1os;\u200B\u200B en obras cl\u00E1sicas, se consideraba que el ordov\u00EDcico abarcaba de los 505 millones de a\u00F1os hasta hace 440 millones de a\u00F1os. Debe su nombre a la tribu celta de los Ordovicos, que vivieron en el centro y norte de Gales, lugar donde el ge\u00F3logo ingl\u00E9s Charles Lapworth identific\u00F3 este sistema en 1879."@es ,
"L\u2019Ordovicien est le second des six syst\u00E8mes g\u00E9ologiques constituant le Pal\u00E9ozo\u00EFque. Il s\u2019\u00E9tend de - 485,4 \u00B1 1,9 \u00E0 - 443,4 \u00B1 1,5 millions d'ann\u00E9es (Ma). Il est pr\u00E9c\u00E9d\u00E9 par le Cambrien et suivi par le Silurien. Les couches g\u00E9ologiques de l\u2019Ordovicien renferment aujourd\u2019hui de vastes r\u00E9servoirs de p\u00E9trole et de gaz naturel dans certaines r\u00E9gions du monde. Il correspond \u00E0 une \u00E9poque o\u00F9 l'oc\u00E9an global et l'atmosph\u00E8re terrestre se sont refroidis, conjointement \u00E0 une explosion de la biodiversit\u00E9 sur la plan\u00E8te."@fr .
@prefix skos: .
@prefix ns12: .
dbr:Ordovician skos:exactMatch ns12:i116698 .
@prefix xsd: .
dbr:Ordovician geo:lat "49.682899"^^xsd:float ;
geo:long "-57.965302"^^xsd:float ;
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@prefix dct: .
@prefix dbc: .
dbr:Ordovician dct:subject dbc:Geological_periods ,
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dbc:Ordovician ;
dbo:abstract "\u041E\u0440\u0434\u043E\u0432\u0438\u0446\u044C\u043A\u0438\u0439 \u043F\u0435\u0440\u0456\u043E\u0434, \u043E\u0440\u0434\u043E\u0432\u0438\u043A (\u0440\u043E\u0441. \u043E\u0440\u0434\u043E\u0432\u0438\u043A\u0441\u043A\u0438\u0439 \u043F\u0435\u0440\u0438\u043E\u0434, \u043E\u0440\u0434\u043E\u0432\u0438\u043A, \u0430\u043D\u0433\u043B. Ordovician period, \u043D\u0456\u043C. Ordoviz(ium) n) \u2014 \u0434\u0440\u0443\u0433\u0438\u0439 \u0433\u0435\u043E\u043B\u043E\u0433\u0456\u0447\u043D\u0438\u0439 \u043F\u0435\u0440\u0456\u043E\u0434 \u043F\u0430\u043B\u0435\u043E\u0437\u043E\u0439\u0441\u044C\u043A\u043E\u0457 \u0435\u0440\u0438. \u041D\u0430\u0437\u0432\u0430 \u043F\u043E\u0445\u043E\u0434\u0438\u0442\u044C \u0432\u0456\u0434 \u043D\u0430\u0437\u0432\u0438 \u0441\u0442\u0430\u0440\u043E\u0434\u0430\u0432\u043D\u044C\u043E\u0433\u043E \u043F\u043B\u0435\u043C\u0435\u043D\u0456 \u043E\u0440\u0434\u043E\u0432\u0438\u043A\u0456\u0432, \u0449\u043E \u043C\u0435\u0448\u043A\u0430\u043B\u043E \u0432 \u0423\u0435\u043B\u044C\u0441\u0456."@uk ,
"Ordovik je geologick\u00FD \u00FAtvar star\u0161\u00EDch prvohor (paleozoikum) a je tedy tak\u00E9 sou\u010D\u00E1st\u00ED e\u00F3nu fanerozoika. N\u00E1zev podle starov\u011Bk\u00E9ho kmene Ordovik\u016F (ve Walesu ob\u00FDvali \u00FAzem\u00ED severn\u011B od Silur\u016F) zavedl Charles Lapworth roku 1879 pro ulo\u017Eeniny tzv. druh\u00E9 fauny, kter\u00FDm v \u010Cech\u00E1ch odpov\u00EDdala Barrandova etapa D. N\u00E1zev s\u00E1m byl v\u0161ak kodifikov\u00E1n a\u017E na 21. geologick\u00E9m kongresu v Kodani roku 1960."@cs ,
"\u0627\u0644\u0623\u0648\u0631\u062F\u0641\u064A\u0634\u064A \u0623\u0648 \u0627\u0644\u0623\u0631\u062F\u0648\u0641\u064A\u0633\u064A \u0623\u0648 \u0627\u0644\u0623\u0648\u0631\u062F\u0648\u0641\u064A\u0643\u064A (\u0628\u0627\u0644\u0644\u0627\u062A\u064A\u0646\u064A\u0629: Ordovician)\u060C \u0648\u0647\u0648 \u062B\u0627\u0646\u064A \u0627\u0644\u0639\u0635\u0648\u0631 \u0627\u0644\u0633\u062A\u0629 \u0645\u0646 \u062D\u0642\u0628\u0629 \u0627\u0644\u062D\u064A\u0627\u0629 \u0627\u0644\u0642\u062F\u064A\u0645\u0629 \u0648\u062F\u0647\u0631 \u0627\u0644\u0628\u0634\u0627\u0626\u0631\u060C \u0627\u0645\u062A\u062F \u0645\u0646 485.4 \u00B1 1.9 \u0625\u0644\u0649 443.8 \u00B1 1.5 \u0645\u0644\u064A\u0648\u0646 \u0633\u0646\u0629 \u0645\u0636\u062A\u060C \u0644\u0645\u062F\u0629 41.6 \u0645\u0644\u064A\u0648\u0646 \u0633\u0646\u0629 \u062A\u0642\u0631\u064A\u0628\u0627. \u064A\u0633\u0628\u0642\u0647 \u0627\u0644\u0643\u0627\u0645\u0628\u0631\u064A\u060C \u0648\u064A\u0644\u064A\u0647 \u0627\u0644\u0633\u064A\u0644\u0648\u0631\u064A. \u062A\u0645\u062A \u062A\u0633\u0645\u064A\u0629 \u0627\u0644\u0623\u0648\u0631\u062F\u0648\u0641\u064A\u0634\u064A \u0646\u0633\u0628\u0629 \u0625\u0644\u0649 (\u0623\u0648\u0631\u062F\u0648\u0641\u0627\u064A\u0633\u064A\u0633) \u0627\u0644\u062A\u064A \u064A\u0639\u064A\u0634 \u0641\u064A\u0647\u0627 \u0642\u0628\u064A\u0644\u0629 \u0643\u0644\u062A \u0648\u0642\u062F \u0623\u0637\u0644\u0642 \u0647\u0630\u0627 \u0627\u0644\u0623\u0633\u0645 \u0627\u0644\u062C\u064A\u0648\u0644\u0648\u062C\u064A \u0627\u0644\u0625\u0646\u062C\u0644\u064A\u0632\u064A \u062A\u0634\u0627\u0631\u0644\u0632 \u0644\u0627\u0628\u0648\u0648\u0631\u062B \u0639\u0627\u0645 1879 \u0648\u0630\u0644\u0643 \u0644\u062D\u0644 \u062E\u0644\u0627\u0641 \u0628\u064A\u0646 \u0622\u062F\u0645 \u0633\u064A\u062F\u062C\u0648\u064A\u0643 \u0627\u0644\u0644\u0630\u0627\u0646 \u062D\u062F\u062F\u0627 \u0646\u0641\u0633 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\u0648\u0627\u0646\u0647 \u064A\u0646\u0628\u063A\u064A \u0644\u0647\u0627 \u0623\u0646 \u062A\u0648\u0636\u0639 \u0641\u064A \u0646\u0638\u0627\u0645 \u062E\u0627\u0635\u0629 \u0628\u0647\u0627. \u062A\u0645 \u0642\u0628\u0648\u0644 \u0627\u0644\u0623\u0648\u0631\u062F\u0648\u0641\u064A\u0634\u064A \u062F\u0648\u0644\u064A\u0627 \u0639\u0627\u0645 1960 (\u0628\u0639\u062F \u0648\u0641\u0627\u0629 \u0644\u0627\u0628\u0648\u0648\u0631\u062B \u0628\u0627\u0631\u0628\u0639\u064A\u0646 \u0639\u0627\u0645\u0627)\u060C \u0639\u0646\u062F\u0645\u0627 \u062A\u0645 \u0627\u0639\u062A\u0645\u0627\u062F\u0647 \u0639\u0644\u0649 \u0623\u0646\u0647 \u0639\u0635\u0631 \u0631\u0633\u0645\u064A \u062A\u0627\u0628\u0639 \u0644\u062D\u0642\u0628\u0629 \u0627\u0644\u062D\u064A\u0627\u0629 \u0627\u0644\u0642\u062F\u064A\u0645\u0629 \u0645\u0646 \u0642\u0628\u0644 \u0627\u0644\u0627\u062A\u062D\u0627\u062F \u0627\u0644\u062F\u0648\u0644\u064A \u0644\u0644\u0639\u0644\u0648\u0645 \u0627\u0644\u062C\u064A\u0648\u0644\u0648\u062C\u064A\u0629. \u0627\u0633\u062A\u0645\u0631 \u0627\u0632\u062F\u0647\u0627\u0631 \u0627\u0644\u062D\u064A\u0627\u0629 \u062E\u0644\u0627\u0644 \u0627\u0644\u0623\u0648\u0631\u062F\u0648\u0641\u064A\u0634\u064A \u0643\u0645\u0627 \u062D\u062F\u062B \u0641\u064A \u0627\u0644\u0633\u0627\u0628\u0642 \u0641\u064A \u0639\u0635\u0631 \u0627\u0644\u0643\u0627\u0645\u0628\u0631\u064A\u060C \u0631\u063A\u0645 \u062D\u062F\u0648\u062B \u0627\u0644\u0627\u0646\u0642\u0631\u0627\u0636 \u0627\u0644\u062C\u0645\u0627\u0639\u064A \u0627\u0644\u0643\u0628\u064A\u0631 \u0641\u064A \u0646\u0647\u0627\u064A\u0629 \u0627\u0644\u0639\u0635\u0631. \u0648\u0633\u064A\u0637\u0631\u062A \u0627\u0644\u0644\u0627\u0641\u0642\u0627\u0631\u064A\u0627\u062A (\u0627\u0644\u0631\u062E\u0648\u064A\u0627\u062A \u0648\u0645\u0641\u0635\u0644\u064A\u0627\u062A \u0627\u0644\u0623\u0631\u062C\u0644) \u0639\u0644\u0649 \u0627\u0644\u0645\u062D\u064A\u0637\u0627\u062A. \u0648\u0623\u062F\u0649 \u062D\u062F\u062B \u0627\u0644\u0623\u0648\u0631\u062F\u0648\u0641\u064A\u0634\u064A \u0627\u0644\u0639\u0638\u064A\u0645 \u0644\u0644\u062A\u0646\u0648\u0639 \u0627\u0644\u062D\u064A\u0648\u064A \u0625\u0644\u0649 \u0632\u064A\u0627\u062F\u0629 \u062A\u0646\u0648\u0639 \u0627\u0644\u062D\u064A\u0627\u0629\u060C \u0648\u0627\u0633\u062A\u0645\u0631\u062A \u0627\u0644\u0623\u0633\u0645\u0627\u0643 \u0627\u0644\u062A\u064A \u062A\u0639\u062A\u0628\u0631 \u0623\u0648\u0644 \u0641\u0642\u0627\u0631\u064A\u0627\u062A \u062D\u0642\u064A\u0642\u064A\u0629 \u0641\u064A \u0627\u0644\u0639\u0627\u0644\u0645 \u0641\u064A \u0627\u0644\u062A\u0637\u0648\u0631\u060C \u0648\u0642\u062F \u0638\u0647\u0631\u062A \u0630\u0648\u0627\u062A \u0627\u0644\u0641\u0643 \u0644\u0644\u0645\u0631\u0629 \u0627\u0644\u0623\u0648\u0644\u0649 \u0641\u064A \u0622\u062E\u0631 \u0647\u0630\u0627 \u0627\u0644\u0639\u0635\u0631. \u0648\u0627\u0633\u062A\u0645\u0631\u062A \u0627\u0644\u062D\u064A\u0627\u0629 \u0641\u064A \u0627\u0644\u062A\u0646\u0648\u0639 \u0639\u0644\u0649 \u0627\u0644\u064A\u0627\u0628\u0633\u0629. \u0648\u062A\u0639\u0631\u0636\u062A \u0627\u0644\u0623\u0631\u0636 \u062E\u0644\u0627\u0644 \u0627\u0644\u0623\u0648\u0631\u062F\u0648\u0641\u064A\u0634\u064A \u0644\u0636\u0631\u0628\u0627\u062A \u0646\u064A\u0632\u0643\u064A\u0629 \u0633\u0646\u0648\u064A\u0629 \u062A\u0639\u0627\u062F \u062D\u0648\u0627\u0644\u064A 100 \u0636\u0639\u0641 \u0639\u062F\u062F \u0627\u0644\u0646\u064A\u0627\u0632\u0643 \u0627\u0644\u062A\u064A \u0636\u0631\u0628\u062A \u0627\u0644\u0623\u0631\u0636 \u0645\u0642\u0627\u0631\u0646\u0629 \u0628\u0627\u0644\u0632\u0645\u0646 \u0627\u0644\u062D\u0627\u0644\u064A."@ar ,
"\u0397 \u039F\u03C1\u03B4\u03BF\u03B2\u03AF\u03BA\u03B9\u03B1 \u03C0\u03B5\u03C1\u03AF\u03BF\u03B4\u03BF\u03C2 \u03B5\u03AF\u03BD\u03B1\u03B9 \u03BC\u03AF\u03B1 \u03B3\u03B5\u03C9\u03BB\u03BF\u03B3\u03B9\u03BA\u03AE \u03C0\u03B5\u03C1\u03AF\u03BF\u03B4\u03BF\u03C2 \u03C4\u03B7\u03C2 \u03A0\u03B1\u03BB\u03B1\u03B9\u03BF\u03B6\u03C9\u03B9\u03BA\u03AE\u03C2 \u03BA\u03B1\u03B9 \u03B5\u03BA\u03C4\u03B5\u03AF\u03BD\u03B5\u03C4\u03B1\u03B9 \u03C3\u03B5 \u03C7\u03C1\u03BF\u03BD\u03B9\u03BA\u03CC \u03B4\u03B9\u03AC\u03C3\u03C4\u03B7\u03BC\u03B1 488,3 \u00B1 1,7 \u03AD\u03C9\u03C2 443,7 \u00B1 1,5 \u03B5\u03BA\u03B1\u03C4\u03BF\u03BC\u03BC\u03CD\u03C1\u03B9\u03B1 \u03AD\u03C4\u03B7 \u03C0.\u03C0. (ICS, 2004). \u0391\u03BA\u03BF\u03BB\u03BF\u03C5\u03B8\u03B5\u03AF \u03C4\u03B7\u03BD \u039A\u03AC\u03BC\u03B2\u03C1\u03B9\u03B1 \u03C0\u03B5\u03C1\u03AF\u03BF\u03B4\u03BF \u03BA\u03B1\u03B9 \u03B1\u03BA\u03BF\u03BB\u03BF\u03C5\u03B8\u03B5\u03AF\u03C4\u03B1\u03B9 \u03B1\u03C0\u03CC \u03C4\u03B7 \u03A3\u03B9\u03BB\u03BF\u03CD\u03C1\u03B9\u03B1 \u03C0\u03B5\u03C1\u03AF\u03BF\u03B4\u03BF. \u0388\u03BB\u03B1\u03B2\u03B5 \u03C4\u03BF \u03CC\u03BD\u03BF\u03BC\u03AC \u03C4\u03B7\u03C2 \u03B1\u03C0\u03CC \u03C4\u03B7\u03BD \u03BF\u03C5\u03B1\u03BB\u03B9\u03BA\u03AE \u03C6\u03C5\u03BB\u03AE \u03C4\u03C9\u03BD \u039F\u03C1\u03B4\u03BF\u03B2\u03AF\u03BA\u03C9\u03BD. \u03A0\u03B1\u03C1\u03AC \u03C4\u03BF \u03B3\u03B5\u03B3\u03BF\u03BD\u03CC\u03C2 \u03CC\u03C4\u03B9 \u03B7 \u03B1\u03BD\u03B1\u03B3\u03BD\u03CE\u03C1\u03B9\u03C3\u03AE \u03C4\u03B7\u03C2 \u03C9\u03C2 \u03B4\u03B9\u03B1\u03BA\u03C1\u03B9\u03C4\u03AE \u03B3\u03B5\u03C9\u03BB\u03BF\u03B3\u03B9\u03BA\u03AE \u03C0\u03B5\u03C1\u03AF\u03BF\u03B4\u03BF\u03C2 \u03AC\u03C1\u03B3\u03B7\u03C3\u03B5 \u03C3\u03C4\u03BF \u0397\u03BD\u03C9\u03BC\u03AD\u03BD\u03BF \u0392\u03B1\u03C3\u03AF\u03BB\u03B5\u03B9\u03BF, \u03AD\u03B3\u03B9\u03BD\u03B5 \u03B3\u03C1\u03AE\u03B3\u03BF\u03C1\u03B1 \u03B1\u03C0\u03BF\u03B4\u03B5\u03BA\u03C4\u03AE \u03C3\u03B5 \u03AC\u03BB\u03BB\u03B5\u03C2 \u03C7\u03CE\u03C1\u03B5\u03C2 \u03BA\u03B1\u03B9 \u03C5\u03B9\u03BF\u03B8\u03B5\u03C4\u03AE\u03B8\u03B7\u03BA\u03B5 \u03B5\u03C0\u03AF\u03C3\u03B7\u03BC\u03B1 \u03C4\u03BF 1906, \u03C9\u03C2 \u03C0\u03B5\u03C1\u03AF\u03BF\u03B4\u03BF\u03C2 \u03C4\u03B7\u03C2 \u03C0\u03B1\u03BB\u03B1\u03B9\u03BF\u03B6\u03C9\u03B9\u03BA\u03AE\u03C2 \u03B5\u03C0\u03BF\u03C7\u03AE\u03C2 \u03B1\u03C0\u03CC \u03C4\u03BF ."@el ,
"Na escala de tempo geol\u00F3gico, o Ordoviciano ou Ordov\u00EDcico \u00E9 o per\u00EDodo da era Paleozoica do \u00E9on Fanerozoico que est\u00E1 compreendido h\u00E1 entre 488 a 443 milh\u00F5es de anos aproximadamente. O per\u00EDodo Ordoviciano sucede o per\u00EDodo Cambriano e precede o per\u00EDodo Siluriano, ambos de sua era. Divide-se nas \u00E9pocas Ordoviciana Inferior, Ordoviciana M\u00E9dia e Ordoviciana Superior, da mais antiga para a mais recente. Os limites do Ordoviciano s\u00E3o marcados pela ocorr\u00EAncia de planct\u00F4nicos. As rochas s\u00E3o geralmente os argilitos escuros, org\u00E2nico que carregam os restos dos grapt\u00F3litos e podem ter sulfeto de ferro. Naquele per\u00EDodo os terremotos eram frequentes."@pt ,
"\u5965\u9676\u7EAA\uFF08\u82F1\u8A9E\uFF1AOrdovician\uFF0C\u767C\u97F3\uFF1A /\u0254\u02D0rd\u0259\u02C8v\u026A\u0283\u0259n/\uFF0C\u7B26\u53F7O\uFF09\u662F\u5730\u8D28\u65F6\u4EE3\u4E2D\u663E\u751F\u5B99\u53E4\u751F\u4EE3\u7684\u7B2C\u4E8C\u4E2A\u7EAA\uFF0C\u7EA6\u5F00\u59CB\u4E8E4.85\u4EBF\u5E74\u524D\uFF0C\u7ED3\u675F\u4E8E4.43\u4EBF\u5E74\u524D\u3002"@zh ,
"The Ordovician (/\u0254\u02D0rd\u0259\u02C8v\u026A\u0283i.\u0259n, -do\u028A-, -\u02C8v\u026A\u0283\u0259n/ or-d\u0259-VISH-ee-\u0259n, -\u2060doh-, -\u2060VISH-\u0259n) is a geologic period and system, the second of six periods of the Paleozoic Era. The Ordovician spans 41.6 million years from the end of the Cambrian Period 485.4 million years ago (Mya) to the start of the Silurian Period 443.8 Mya. The Ordovician, named after the Welsh tribe of the Ordovices, was defined by Charles Lapworth in 1879 to resolve a dispute between followers of Adam Sedgwick and Roderick Murchison, who were placing the same rock beds in North Wales in the Cambrian and Silurian systems, respectively. Lapworth recognized that the fossil fauna in the disputed strata were different from those of either the Cambrian or the Silurian systems, and placed them in a system of their own. The Ordovician received international approval in 1960 (forty years after Lapworth's death), when it was adopted as an official period of the Paleozoic Era by the International Geological Congress. Life continued to flourish during the Ordovician as it did in the earlier Cambrian Period, although the end of the period was marked by the Ordovician\u2013Silurian extinction events. Invertebrates, namely molluscs and arthropods, dominated the oceans, with members of the latter group probably starting their establishment on land during this time, becoming fully established by the Devonian. The first land plants are known from this period. The Great Ordovician Biodiversification Event considerably increased the diversity of life. Fish, the world's first true vertebrates, continued to evolve, and those with jaws may have first appeared late in the period. About 100 times as many meteorites struck the Earth per year during the Ordovician compared with today."@en ,
"Ordoviziarra Paleozoikoko bigarren garaia da, Kanbriarraren ondoren eta Siluriarraren aurretik. Berez bi garai hauen artean zeuden harri batzuen inguruko eztabaidarekin bukatzeko izendatu zuen Charles Lapworthek 1879an. Ofizialki 1906an onartu zuen Geologiako Nazioarteko Kongresuak. Orain dela 488.3 milioi urte hasi zen eta orain dela 443.7 milioi urte bukatu. Biak handiekin bat egiten duten garaiak dira. Ordoviziar garaia zatitzeko honako atalak bereizten dira: \n* Behe Ordoviziarra: ( eta ) \n* Ordoviziar ertaina: (Caradoc, , Llandeilo) \n* Goi Ordoviziarra: (Ashgill)"@eu ,
"Das Ordovizium ist das zweite chronostratigraphische System (bzw. Periode in der Geochronologie) des Pal\u00E4ozoikums in der Erdgeschichte. Das Ordovizium begann vor etwa 485,4 Millionen Jahren und endete vor rund 443,4 Millionen Jahren. Es wird vom Kambrium unterlagert, die Schichten des Kambriums sind also die \u00E4ltesten des Pal\u00E4ozoikums. Auf das Ordovizium folgt das Silur."@de ,
"Ordowik (ang. Ordovician) \n* w sensie geochronologicznym \u2013 drugi okres ery paleozoicznej. Trwa\u0142 oko\u0142o 42 miliony lat (od 485,4\u202F\u00B1\u202F1,9 do 443,4\u202F\u00B1\u202F1,5 milion\u00F3w lat temu). Ordowik dzieli si\u0119 na trzy epoki: ordowik wczesny, ordowik \u015Brodkowy i ordowik p\u00F3\u017Any. \n* w sensie chronostratygraficznym \u2013 drugi system eratemu paleozoicznego, wy\u017Cszy od kambru, ni\u017Cszy od syluru. Dzieli si\u0119 na trzy oddzia\u0142y: ordowik dolny, ordowik \u015Brodkowy i ordowik g\u00F3rny. Mi\u0119dzynarodowy stratotyp granicy kambr/ordowik znajduje si\u0119 na Green Point (zachodnie wybrze\u017Ce Nowej Fundlandii, Kanada). Dolna granica ordowiku oparta jest o pierwsze pojawienie si\u0119 konodonta Iapetognathus fluctivagus. System ordowicki wydzieli\u0142 w 1879 roku, ko\u0144cz\u0105c sp\u00F3r mi\u0119dzy Adamem Sedgwickiem a Roderickiem Murchisonem o warstwy graniczne kambru i syluru. Nazwa pochodzi od celtyckiego plemienia Ordowik\u00F3w zamieszkuj\u0105cego p\u00F3\u0142nocn\u0105 Wali\u0119."@pl ,
"L'Ordovici\u00E0 \u00E9s el per\u00EDode geol\u00F2gic que comen\u00E7\u00E0 fa 485,4 \u00B1 1,9 milions d'anys i s'acab\u00E0 fa 443,8 \u00B1 1,5 milions d'anys. Es tracta del segon per\u00EDode de l'era del Paleozoic. El seu nom fa refer\u00E8ncia als ordovics, l'\u00FAltima tribu gal\u00B7lesa que se sotmet\u00E9 als romans, i al fet que les roques utilitzades per descriure el per\u00EDode es troben a l'antic territori dels ordovics al nord de Gal\u00B7les. Segueix el per\u00EDode Cambri\u00E0 i precedeix el Siluri\u00E0. L'Ordovici\u00E0 fou definit per en Charles Lapworth el 1879, per resoldre una disputa entre els seguidors d'Adam Sedgwick i Roderick Murchison, que situaven els mateixos estrats del nord de Gal\u00B7les en els per\u00EDodes Cambri\u00E0 i Siluri\u00E0 respectivament. En Lapworth, reconeixent que la fauna f\u00F2ssil present en els estrats en disputa eren diferents tant dels del Cambri\u00E0 com els del Siluri\u00E0, es va adonar que havien de ser situats en un per\u00EDode propi. Mentre que el reconeixement del per\u00EDode Ordovici\u00E0 fou lent al Regne Unit, altres zones del m\u00F3n el van acceptar r\u00E0pidament. Va ser homologat internacionalment el 1906, quan fou adoptat com un per\u00EDode oficial del Paleozoic pel Congr\u00E9s Geol\u00F2gic Internacional."@ca ,
"\u30AA\u30EB\u30C9\u30D3\u30B9\u7D00\uFF08\u30AA\u30EB\u30C9\u30D3\u30B9\u304D\u3001Ordovician period\uFF09\u3068\u306F\u3001\u5730\u8CEA\u6642\u4EE3\u3001\u53E4\u751F\u4EE3\u524D\u671F\u306B\u304A\u3051\u308B\u533A\u5206\u3067\u3001\u7D044\u51048830\u4E07\u5E74\u524D\u304B\u3089\u7D044\u51044370\u4E07\u5E74\u524D\u307E\u3067\u3092\u6307\u3059\u3002\u30AA\u30EB\u30C9\u30D3\u30B9\u306E\u540D\u524D\u306F\u3001\u6A21\u5F0F\u5730\u3067\u3042\u308B\u30A6\u30A7\u30FC\u30EB\u30BA\u5730\u65B9\u306B\u4F4F\u3093\u3067\u3044\u305F\u53E4\u4EE3\u30B1\u30EB\u30C8\u7CFB\u90E8\u65CF\u300C\u300D(Ordovices) \u304B\u3089\u3064\u3044\u305F\u3002\u5965\u9676\u7D00\uFF08\u304A\u3046\u3068\u3046\u304D\uFF09\u3068\u3082\u3044\u3046\u3002 \u30AA\u30EB\u30C9\u30D3\u30B9\u7D00\u306F\u3001\u751F\u7269\u306E\u591A\u69D8\u5316\u304C\u30AB\u30F3\u30D6\u30EA\u30A2\u7D00\u4E26\u306B\u9032\u3093\u3060\u6642\u4EE3\u3067\u3042\u308B\u3002\u30AA\u30A6\u30E0\u30AC\u30A4\u306B\u4EE3\u8868\u3055\u308C\u308B\u8EDF\u4F53\u52D5\u7269\u3084\u4E09\u8449\u866B\u306E\u3088\u3046\u306A\u7BC0\u8DB3\u52D5\u7269\u3001\u7B46\u77F3\u306E\u3088\u3046\u306A\u534A\u7D22\u52D5\u7269\u304C\u6804\u3048\u305F\u3002\u307E\u305F\u3001\u30AA\u30EB\u30C9\u30D3\u30B9\u7D00\u5F8C\u671F\u306B\u306F\u984E\u3092\u6301\u3064\u9B5A\u985E\u304C\u767B\u5834\u3057\u305F\u3002 \u30AA\u30EB\u30C9\u30D3\u30B9\u7D00\u672B\u306B\u306F\u5927\u91CF\u7D76\u6EC5\u304C\u8D77\u3053\u3063\u305F\u3002"@ja ,
"\uC624\uB974\uB3C4\uBE44\uC2A4\uAE30(Ordovician)\uB294 \uACE0\uC0DD\uB300\uC758 6\uAC1C \uAE30 \uC911\uC5D0\uC11C \uB450 \uBC88\uC9F8 \uAE30\uC774\uB2E4. \uCE84\uBE0C\uB9AC\uC544\uAE30 \uB2E4\uC74C\uC5D0 \uC624\uBA70, \uC2E4\uB8E8\uB9AC\uC544\uAE30\uBCF4\uB2E4 \uC804\uC774\uB2E4. \uC624\uB974\uB3C4\uBE44\uC2A4\uAE30\uB77C\uB294 \uC774\uB984\uC740 \uC6E8\uC77C\uC2A4\uC9C0\uBC29\uC758 \uC624\uB974\uB3C4\uBE44\uC2A4 \uBD80\uC871\uC73C\uB85C\uBD80\uD130 \uC720\uB798\uD558\uC600\uC73C\uBA70 1879\uB144 \uAC00 \uC815\uC758\uD558\uC600\uB2E4. \uC774 \uC804\uC5D0\uB294 \uACFC \uC774 \uBD81\uC6E8\uC77C\uC2A4\uC758 \uC554\uC11D\uCE35\uC744 \uCE84\uBE0C\uB9AC\uC544\uAE30\uB85C \uB123\uC744 \uAC83\uC778\uC9C0 \uC2E4\uB8E8\uB9AC\uC544\uAE30\uB85C \uB123\uC744\uAC83\uC778\uC9C0\uC5D0 \uAD00\uD55C \uB17C\uC7C1\uC774 \uC788\uC5C8\uB2E4. \uB7A9\uC6CC\uC2A4\uB294 \uBB38\uC81C\uAC00 \uB418\uB294 \uC554\uC11D\uCE35\uC758 \uD654\uC11D \uC0DD\uBB3C\uAD70\uC774 \uCE84\uBE0C\uB9AC\uC544\uAE30\uC640\uB3C4 \uC2E4\uB8E8\uB9AC\uC544\uAE30\uC640\uB3C4 \uB2E4\uB978\uAC83\uC744 \uD655\uC778\uD558\uACE0, \uC774 \uCE35\uC774 \uC0C8\uB86D\uAC8C \uB3C5\uB9BD\uB418\uC5B4\uC57C \uD568\uC744 \uC54C\uAC8C \uB418\uC5C8\uB2E4. \uC624\uB974\uB3C4\uBE44\uC2A4\uAE30\uAC00 \uC778\uC815\uB418\uB294 \uAC83\uC740 \uC601\uAD6D\uC5D0\uC11C\uB294 \uC624\uB79C \uC2DC\uAC04\uC774 \uD544\uC694\uD588\uC9C0\uB9CC, \uB2E4\uB978 \uACF3\uC5D0\uC11C\uB294 \uACE7 \uBC1B\uC544\uB4E4\uC5EC\uC84C\uB2E4. \uADF8\uB9AC\uACE0 1906\uB144\uC5D0 \uACE0\uC0DD\uB300\uC758 \uD55C \uAE30\uB85C \uACF5\uC778\uB418\uC5C8\uB2E4."@ko ,
"Ordovicio estas la 2-a epoko de la paleozoika erao, kiam aperis la senmakzelaj fi\u015Doj (prafi\u015Doj), cefalopodoj (na\u016Dtiloj). \u011Ci da\u016Dris de 488 \u011Dis 444 milionoj da jaroj. \u011Cin sekvis silurio."@eo ,
"El Ordov\u00EDcico es la fragmentaci\u00F3n de la escala temporal geol\u00F3gica que pertenece a la Era Paleozoica; esta se divide en seis periodos de los que el Ordov\u00EDcico ocupa el segundo lugar posterior al C\u00E1mbrico y precediendo al Sil\u00FArico. Comenz\u00F3 hace unos 485 millones de a\u00F1os y termin\u00F3 hace unos 444 millones de a\u00F1os;\u200B\u200B en obras cl\u00E1sicas, se consideraba que el ordov\u00EDcico abarcaba de los 505 millones de a\u00F1os hasta hace 440 millones de a\u00F1os. Debe su nombre a la tribu celta de los Ordovicos, que vivieron en el centro y norte de Gales, lugar donde el ge\u00F3logo ingl\u00E9s Charles Lapworth identific\u00F3 este sistema en 1879. En este per\u00EDodo, un d\u00EDa ten\u00EDa 21 horas y no hab\u00EDa animales en tierra firme por la escasez de ox\u00EDgeno en la atm\u00F3sfera. Abundan los f\u00F3siles, entre los que destacan los trilobites y en algunas regiones se formaron los yacimientos de petr\u00F3leo y gas."@es ,
"Het Ordovicium is een periode uit de geologische tijdschaal (of een systeem in de stratigrafie), die ongeveer van 485 tot 443 miljoen jaar geleden duurde. Het Ordovicium is onderdeel van het Paleozo\u00EFcum, het volgt op het Cambrium en wordt opgevolgd door het Siluur. Het Ordovicium was een periode met een relatief warm klimaat en een hoog zeeniveau, met als korte uitzondering een ijstijd in het Laat-Ordovicium. Het leven speelde zich nog voornamelijk af in het water, hoewel er aanwijzingen zijn dat primitieve planten en insecten al in vochtige omgevingen op het land voorkwamen. Succesvolle groepen zeedieren waren de inktvissen en graptolieten. In het Ordovicium verschenen ook de eerste kaakloze vissen."@nl ,
"L\u2019Ordovicien est le second des six syst\u00E8mes g\u00E9ologiques constituant le Pal\u00E9ozo\u00EFque. Il s\u2019\u00E9tend de - 485,4 \u00B1 1,9 \u00E0 - 443,4 \u00B1 1,5 millions d'ann\u00E9es (Ma). Il est pr\u00E9c\u00E9d\u00E9 par le Cambrien et suivi par le Silurien. L\u2019Ordovicien a \u00E9t\u00E9 d\u00E9fini par Charles Lapworth en 1879 pour r\u00E9soudre un probl\u00E8me de paternit\u00E9 de certaines couches g\u00E9ologiques. Adam Sedgwick et Roderick Murchison ont plac\u00E9 ces couches respectivement dans le Cambrien et le Silurien. Lapworth reconna\u00EEt que les fossiles pr\u00E9sents dans les strates disput\u00E9es sont distincts de ceux du Cambrien ou du Silurien et les attribue \u00E0 un nouveau syst\u00E8me, nomm\u00E9 Ordovicien en r\u00E9f\u00E9rence aux Ordovices, un peuple brittonique de l\u2019actuel Pays de Galles. Les couches g\u00E9ologiques de l\u2019Ordovicien renferment aujourd\u2019hui de vastes r\u00E9servoirs de p\u00E9trole et de gaz naturel dans certaines r\u00E9gions du monde. Il correspond \u00E0 une \u00E9poque o\u00F9 l'oc\u00E9an global et l'atmosph\u00E8re terrestre se sont refroidis, conjointement \u00E0 une explosion de la biodiversit\u00E9 sur la plan\u00E8te."@fr ,
"L'Ordoviciano \u00E8 il secondo dei sei (sette in Nord America) periodi geologici in cui \u00E8 suddivisa l'era geologica paleozoica e copre il periodo di tempo tra 485,4\u00B11,9 e 443,8\u00B11,5 milioni di anni fa. Segue il periodo Cambriano ed \u00E8 seguito dal periodo Siluriano. L'Ordoviciano, il cui nome deriva da una trib\u00F9 gallese (gli Ordovici), fu definito da Charles Lapworth nel 1879 per risolvere una disputa tra i seguaci di Adam Sedgwick e di Roderick Murchison che avevano attribuito le stesse rocce del nord del Galles rispettivamente al Cambriano ed al Siluriano. Lapworth risolse la contesa proponendo un nuovo periodo, perch\u00E9 aveva riconosciuto che la fauna fossile negli strati oggetto della disputa era diversa sia da quella del Cambriano che da quella del Siluriano. Nel Regno Unito l'adozione del nuovo periodo fu lenta, mentre nelle altre parti del mondo l'Ordoviciano fu accettato velocemente. Esso ricevette il riconoscimento internazionale nel 1906, quando fu adottato ufficialmente come periodo del Paleozoico dal Congresso Internazionale di Geologia. I sedimenti dell'Ordoviciano contengono abbondanti fossili, in particolare: trilobiti, brachiopodi, cefalopodi, crinoidi, graptoliti, coralli. In talune regioni i sedimenti ordoviciani contengono giacimenti di idrocarburi."@it ,
"\u041E\u0440\u0434\u043E\u0301\u0432\u0438\u043A\u0441\u043A\u0438\u0439 \u043F\u0435\u0440\u0438\u0301\u043E\u0434 (\u043E\u0440\u0434\u043E\u0301\u0432\u0438\u043A) \u2014 \u0432\u0442\u043E\u0440\u043E\u0439 \u043F\u0435\u0440\u0438\u043E\u0434 \u043F\u0430\u043B\u0435\u043E\u0437\u043E\u0439\u0441\u043A\u043E\u0439 \u044D\u0440\u044B. \u041D\u0430\u0441\u0442\u0443\u043F\u0438\u043B \u0437\u0430 \u043A\u0435\u043C\u0431\u0440\u0438\u0439\u0441\u043A\u0438\u043C \u043F\u0435\u0440\u0438\u043E\u0434\u043E\u043C \u0438 \u0441\u043C\u0435\u043D\u0438\u043B\u0441\u044F \u0441\u0438\u043B\u0443\u0440\u0438\u0439\u0441\u043A\u0438\u043C. \u041F\u0440\u043E\u0434\u043E\u043B\u0436\u0430\u043B\u0441\u044F \u043E\u0442 485,4 \u00B1 1,9 \u0434\u043E 443,8 \u00B1 1,5 \u043C\u043B\u043D \u043B\u0435\u0442 \u043D\u0430\u0437\u0430\u0434 (\u043E\u043A\u043E\u043B\u043E 42 \u043C\u043B\u043D \u043B\u0435\u0442). \u041A\u043E\u043C\u043F\u043B\u0435\u043A\u0441 \u043E\u0442\u043B\u043E\u0436\u0435\u043D\u0438\u0439 (\u0433\u043E\u0440\u043D\u044B\u0445 \u043F\u043E\u0440\u043E\u0434), \u0441\u043E\u043E\u0442\u0432\u0435\u0442\u0441\u0442\u0432\u0443\u044E\u0449\u0438\u0445 \u044D\u0442\u043E\u043C\u0443 \u043F\u0435\u0440\u0438\u043E\u0434\u0443, \u043D\u0430\u0437\u044B\u0432\u0430\u0435\u0442\u0441\u044F \u043E\u0440\u0434\u043E\u0432\u0438\u043A\u0441\u043A\u043E\u0439 \u0441\u0438\u0441\u0442\u0435\u043C\u043E\u0439. \u0416\u0438\u0437\u043D\u044C \u0432 \u043E\u0440\u0434\u043E\u0432\u0438\u043A\u0435 \u043F\u0440\u043E\u0434\u043E\u043B\u0436\u0430\u043B\u0430 \u0431\u0443\u0440\u043D\u043E \u0440\u0430\u0437\u0432\u0438\u0432\u0430\u0442\u044C\u0441\u044F. \u0421\u043E\u043F\u043E\u0441\u0442\u0430\u0432\u0438\u043C\u0430\u044F \u0441 \u043A\u0435\u043C\u0431\u0440\u0438\u0439\u0441\u043A\u0438\u043C \u0432\u0437\u0440\u044B\u0432\u043E\u043C \u043F\u0440\u043E\u0438\u0441\u0445\u043E\u0434\u0438\u043B\u0430 \u0432 \u0442\u0435\u0447\u0435\u043D\u0438\u0435 \u0432\u0441\u0435\u0433\u043E \u043F\u0435\u0440\u0438\u043E\u0434\u0430. \u041C\u043E\u043B\u043B\u044E\u0441\u043A\u0438 \u0438 \u0447\u043B\u0435\u043D\u0438\u0441\u0442\u043E\u043D\u043E\u0433\u0438\u0435 \u043F\u0440\u043E\u0434\u043E\u043B\u0436\u0430\u043B\u0438 \u043E\u0441\u0442\u0430\u0432\u0430\u0442\u044C\u0441\u044F \u0434\u043E\u043C\u0438\u043D\u0438\u0440\u0443\u044E\u0449\u0438\u043C\u0438 \u043C\u043E\u0440\u0441\u043A\u0438\u043C\u0438 \u0436\u0438\u0432\u043E\u0442\u043D\u044B\u043C\u0438. \u041F\u043E\u044F\u0432\u043B\u044F\u044E\u0442\u0441\u044F \u043F\u0435\u0440\u0432\u044B\u0435 \u0447\u0435\u043B\u044E\u0441\u0442\u043D\u043E\u0440\u043E\u0442\u044B\u0435 \u0440\u044B\u0431\u044B. \u0421\u0443\u0448\u0430 \u043F\u043E \u0431\u043E\u043B\u044C\u0448\u0435\u0439 \u0447\u0430\u0441\u0442\u0438 \u043F\u0440\u043E\u0434\u043E\u043B\u0436\u0430\u043B\u0430 \u043E\u0441\u0442\u0430\u0432\u0430\u0442\u044C\u0441\u044F \u043F\u0443\u0441\u0442\u044B\u043D\u043D\u043E\u0439, \u043E\u0434\u043D\u0430\u043A\u043E \u0432 \u043F\u0440\u0438\u0431\u0440\u0435\u0436\u043D\u044B\u0445 \u0437\u043E\u043D\u0430\u0445 \u0441\u0442\u0430\u043B\u0438 \u043F\u043E\u044F\u0432\u043B\u044F\u0442\u044C\u0441\u044F \u043F\u0435\u0440\u0432\u044B\u0435 \u043D\u0430\u0437\u0435\u043C\u043D\u044B\u0435 \u0440\u0430\u0441\u0442\u0435\u043D\u0438\u044F. \u0412 \u043E\u0440\u0434\u043E\u0432\u0438\u043A\u0435 \u043D\u0430 \u0417\u0435\u043C\u043B\u044E \u0433\u043E\u0440\u0430\u0437\u0434\u043E \u0447\u0430\u0449\u0435 \u043F\u0430\u0434\u0430\u043B\u0438 \u043C\u0435\u0442\u0435\u043E\u0440\u0438\u0442\u044B, \u0447\u0435\u043C \u0432 \u043D\u0430\u0441\u0442\u043E\u044F\u0449\u0435\u0435 \u0432\u0440\u0435\u043C\u044F."@ru ,
"Ordovicium \u00E4r en geologisk period i den paleozoiska eran. Den b\u00F6rjade vid kambriums slut 485 miljoner \u00E5r f\u00F6re nutid och slutade n\u00E4r silur tog vid 444 miljoner \u00E5r f\u00F6re nutid. Den senare delen av ordovicium k\u00E4nnetecknas av en stor nedisning p\u00E5 Gondwana, den s\u00E5 kallade Hirnantiska istiden. Detta ledde till att havsniv\u00E5n sj\u00F6nk och livsutrymmet f\u00F6r alla marina organismer minskade. Man tror att denna istid var en av anledningarna till det stora massutd\u00F6ende som finns registrerat i det fossila arkivet. Tv\u00E5 av sju \u00E5ldrar (etager) inom ordovicium \u00E4r uppkallade efter geologiska fyndplatser i Sverige (Flo och Sandby)."@sv ,
"Ordovisium adalah suatu periode pada era Paleozoikum yang berlangsung antara 488,3 \u00B1 1,7 hingga 443,7 \u00B1 1,5 juta tahun lalu. Periode ini melanjutkan periode Kambrium dan diikuti oleh periode Silur. Periode yang mendapat namanya dari salah satu suku di Wales, Ordovices, ini didefinisikan oleh pada tahun 1879 untuk menyelesaikan persengketaan antara pengikut Adam Sedgwick dan yang masing-masing mengelompokkan yang sama di Wales utara masuk dalam periode Kambrium dan Silur. Lapworth mengamati bahwa fosil fauna pada strata yang dipersengketakan ini berbeda dengan fauna pada periode Kambrium maupun Silur sehingga seharusnya memiliki periode tersendiri. Periode ini terbagi menjadi 3 kala, yaitu Ordovisium awal, Ordovisium tengah, dan Ordovisium akhir."@in ;
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dbr:Llandeilo_stage ,
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dbp:timeStart "485.4"^^xsd:double ;
dbp:upperGsspAcceptDate 1984 ;
dbp:celestialBody "earth"@en ;
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dbp:upperBoundaryDef "FAD of the Graptolite Akidograptus ascensus"@en ;
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dbp:timeEndUncertainty "1.5"^^xsd:double .
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