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It is the longest of the Phanerozoic eras, lasting from 538.8 to 251.902 million years ago, and is subdivided into six geologic periods (from oldest to youngest):" /> <meta property="og:site_name" content="DBpedia" />  </head> <body about="http://dbpedia.org/resource/Paleozoic">  <nav class="navbar navbar-expand-md navbar-light bg-light fixed-top align-items-center"> <div class="container-xl"> <a class="navbar-brand" href="http://wiki.dbpedia.org/about" title="About DBpedia" style="color: #2c5078"> <img class="img-fluid" src="/statics/images/dbpedia_logo_land_120.png" alt="About DBpedia" /> </a> <button class="navbar-toggler" type="button" data-bs-toggle="collapse" data-bs-target="#dbp-navbar" aria-controls="dbp-navbar" aria-expanded="false" aria-label="Toggle navigation"> </button> <div class="collapse navbar-collapse" id="dbp-navbar"> <ul class="navbar-nav me-auto mb-2 mb-lg-0"> <li class="nav-item dropdown"> <a class="nav-link dropdown-toggle" href="#" id="navbarDropdownBrowse" 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class="text-muted"> An Entity of Type: <a href="http://www.w3.org/2003/01/geo/wgs84_pos#SpatialThing">SpatialThing</a>, from Named Graph: <a href="http://dbpedia.org">http://dbpedia.org</a>, within Data Space: <a href="http://dbpedia.org">dbpedia.org</a> </div> </div> </div> <div class="row pt-2"> <div class="col-xs-9 col-sm-10"> The Paleozoic (or Palaeozoic) Era is the earliest of three geologic eras of the Phanerozoic Eon.The name Paleozoic ( /ˌpæli.əˈzoʊ.ɪk, -i.oʊ-, ˌpeɪ-/ pal-ee-ə-ZOH-ik, -⁠ee-oh-, pay-;) was coined by the British geologist Adam Sedgwick in 1838by combining the Greek words palaiós (παλαιός, "old") and zōḗ (ζωή), "life", meaning "ancient life"). It is the longest of the Phanerozoic eras, lasting from 538.8 to 251.902 million years ago, and is subdivided into six geologic periods (from oldest to youngest): </div> <div class="col-xs-3 col-sm-2"> <a href="#" class="thumbnail"> <img src="http://commons.wikimedia.org/wiki/Special:FilePath/Trilobite_Heinrich_Harder.jpg?width=300" alt="thumbnail" class="img-fluid" /> </a> </div> </div> </div> </section>   <section> <div class="container-xl"> <div class="row"> <div class="table-responsive"> <table class="table table-hover table-sm table-light"> <thead> <tr> <th class="col-xs-3 ">Property</th> <th class="col-xs-9 px-3">Value</th> </tr> </thead> <tbody> <tr class="odd"><td class="col-2"><a class="uri" href="http://dbpedia.org/ontology/abstract">dbo:abstract</a> </td><td class="col-10 text-break"><ul> <li style="display:none;">حقبة الحياة القديمة أو الحياة المبكرة أو الحَفِيريّ (باللاتينية: Paleozoic)، بالاغريقية: (palaios = παλαιός = قديم + zoe = ζωή = حياة)، وهي أول وأطول حقبة من الحقب الجيولوجية الثلاثة لدهر البشائر، امتدت من 541 ± 1.0 إلى 251.902 ± 0.024 مليون سنة مضت، لمدة 289.098 مليون سنة تقريبا. كانت الفترة الزمنية لحقبة الحياة القديمة مثيرة من ناحية التغيرات الجيولوجية، والمناخية، والتطورية. فقد شهد العصر الكامبري تنوع حيوي يعتبر الأسرع والأوسع انتشارا في تاريخ الأرض، وقد عرف باسم الانفجار الكامبري، الذي ظهرت فيه معظم الشعب الحديثة. وقد تطورت خلال حقبة الحياة القديمة كل من: مفصليات الأرجل، والرخويات، والسمك، والبرمائيات، ومندمجات الأقواس وثنائيات الأقواس. بدأت الحياة في المحيطات وانتقلت في النهاية إلى اليابسة، وفي أواخر حقبة الحياة القديمة، سيطرت على اليابسة أشكال مختلفة من الكائنات الحية. غطت القارات غابات كبيرة من النباتات البدائية، وقد شكل الكثير منها طبقات الفحم في أوروبا وشرق أمريكا الشمالية. وبنهاية الحقبة، سادت الزواحف المندمجة والثنائية الأقواس الكبيرة والمتطورة، وظهرت أولى النباتات الحديثة (المخروطيات). انتهت حقبة الحياة القديمة بأكبر انقراض جماعي في تاريخ الأرض، حدث انقراض البرمي-الثلاثي. وكانت آثار هذه الكارثة المدمرة بأن أنهكت الحياة على الأرض مدة 30 مليون سنة حتى تعافت في حقبة الحياة الوسطى. وكان انتعاش الحياة في البحر أسرع بكثير. (ar)</li> <li style="display:none;">Paleozoikum (z řec. paleos, starý a zóé, život), česky prvohory, je nejstarší ze tří geologických ér fanerozoika, nejmladšího eonu (věku) Země. Podle současného datování tato éra zahrnuje období před 541 až 252 miliony let a trvala zhruba 289 milionů let. Dělí se na celkem šest period (od nejstarší): kambrium, ordovik, silur, devon, karbon a perm. Paleozoikum začíná kambrickou explozí, mohutným rozvojem vícebuněčných organismů, a končí vymíráním na konci permu, největším hromadným vymíráním druhů v historii Země, po kterém nastupuje éra mezozoika (druhohor), nazývaná také "érou plazů". (cs)</li> <li style="display:none;">El Paleozoic és l'era geològica que començà fa 541 ± 1,0 milions d'anys i s'acabà fa 251,902 ± 0,024 milions d'anys. Es tracta de la primera època de l'eó Fanerozoic, que encara dura. El seu nom deriva de les paraules gregues antigues παλαιός (paleós), que significa 'antic', i ζωή (zoé), que significa 'vida', i en el seu conjunt vol dir 'vida antiga'. La divisió del temps en diferents eres, la divisió més gran del temps geològic, ve ja de Giovanni Arduino, del segle xviii, tot i que el seu nom original per l'era ara coneguda com el Paleozoic era «Primitiu». El Paleozoic inclou sis períodes geològics; del més antic al més recent --el Cambrià, l'Ordovicià, el Silurià, el Devonià, el Carbonífer i el Permià. S'estén des de fa uns 542 milions d'anys fins fa uns 251 milions d'anys. Segueix el Precambrià i precedeix el Mesozoic. El Paleozoic va des del temps de la primera aparició en abundància de fòssils de closca dura fins al temps en què els continents començaven a ser dominats per rèptils grans i relativament sofisticats, així com per vegetals relativament moderns. El límit inferior se'n situava clàssicament en la primera aparició de criatures conegudes com a trilobits i arqueociats. El límit superior està situat en una extinció massiva 300 milions d'anys més tard, conegut com l'extinció permiana. La pràctica moderna situa el límit més antic en la primera aparició d'un fòssil característic anomenat . Geològicament, el Paleozoic comença poc després de la fragmentació d'un supercontinent anomenat Rodínia, i al final d'una època glacial global (vegeu Glaciació varangiana). Durant el Paleozoic primitiu, la massa terrestre de la Terra es va trencar en un gran nombre de continents relativament petits. Cap al final de l'era, els continents s'agruparen de nou en un supercontinent anomenat Pangea, que incloïa la major part de l'àrea terrestre de la Terra. Al principi de l'era, la vida només consistia en bacteris, algues, esponges i una varietat de formes lleugerament enigmàtiques conegudes com a «organismes ediacarians». Un gran nombre d'estructures corpòries aparegueren quasi simultàniament al començament de l'era, un fenomen conegut com a «explosió cambriana». Hi ha algunes proves que organismes senzills ja podrien haver envaït la terra al començament del Paleozoic, però els vegetals i animals substancials no van arribar a la Terra fins al Silurià i no van començar a prosperar fins al Devonià. Tot i que es coneixen vertebrats primitius des de principis del Paleozoic, les formes animals dominants foren els invertebrats fins a mitjans del Paleozoic. Les poblacions de peixos van explotar durant el Devonià. Durant el Paleozoic tardà, grans boscos de vegetals primitius van prosperar en la Terra, formant les grans capes de carbó d'Europa i l'est de Nord-amèrica. Cap al final de l'era, els primers rèptils grans i sofisticats i les primeres coníferes ja havien evolucionat. (ca)</li> <li style="display:none;">Ο Παλαιοζωικός αιώνας είναι ο πρώτος από τους τρεις του Φανεροζωικού μεγααιώνα. Καλύπτει την περιόδο από περίπου 542 εώς 251 εκατομμύρια χρόνια προ παρόντος (π.π.) (ICS, 2004) και ακολουθείται από το Μεσοζωικό αιώνα. Περιλαμβάνει έξι περιόδους. Από την νεότερη ως τη αρχαιότερη είναι οι εξής: * Η Πέρμια (299–251 π.π.). * Η Λιθανθρακοφόρος (359,2–299 π.π.) * Η Δεβόνια (416–359,2 π.π.) * Η Σιλούρια (443,7–416 π.π.) * Η Ορδοβίκια (488,3–443,7 π.π.) * Η Κάμβρια (542–488,3 π.π.) (el)</li> <li style="display:none;">Paleozoiko estas la unua erao post la antaŭkambrio, dum kiu formiĝis la kambria, ordovicia, siluria, devonia, karbonia kaj permia formacioj. Ĉi tiu erao komenciĝis antaŭ 550 milionoj da jaroj kaj daŭris ĝis 355 milionoj da jaroj. 1 En milionoj da jaroj. (eo)</li> <li style="display:none;">Das Paläozoikum, auch Erdaltertum oder Erdaltzeit, ist die älteste der drei Ären, in die das Äon Phanerozoikum in der geologischen Zeitskala untergliedert wird. Es umfasst den Zeitraum von ca. 541 Millionen Jahre bis ca. 251,9 Millionen Jahre vor heute. Auf das Paläozoikum folgte das Mesozoikum (Erdmittelalter). (de)</li> <li style="display:none;">Paleozoikoa Lurraren Historiako garai geologiko bat da. Bere iraupena 291 milioi urtekoa izan zen. Hasiera orain dela 542 milioi urte kokatzen da eta bukaera orain dela 251 milioi urte.Paleontologikoki hasiera Kanbriarreko leherketarekin bat jartzen dugu eta bukaera lehenengo extintzio masiboarekin. Bere barnean honako periodoak daude: * Kanbriarra. Orain dela 570 milioi urte. * Ordoviziarra. Orain dela 510 milioi urte * Siluriarra. Orain dela 439 milioi urte. * Devoniarra. Orain dela 408 milioi urte. * Karboniferoa. Orain dela 360 milioi urte. * Permiarra. Orain dela 280 milioi urte. (eu)</li> <li style="display:none;">El Paleozoico o era paleozoica es una división de la escala temporal geológica que pertenece al eón Fanerozoico, con la categoría de era (como tiempo) y eratema (como conjunto de rocas). El Paleozoico sucede al supereón Precámbrico y precede al Mesozoico. De más de 290 millones de años (M.a.) de duración, se inició hace 541 millones de años y acabó hace unos 252 millones de años. Su nombre procede del griego «palaio/παλαιο» («viejo») y «zoe/ζωη» («vida»), que significa «vida antigua». Anteriormente era conocido por los términos, hoy obsoletos, de Primario o era primaria. Geológicamente, el Paleozoico se inicia poco después de la desintegración del supercontinente Pannotia y acaba con la formación del supercontinente Pangea. Durante la mayor parte de la era, la superficie de la Tierra se divide en un número relativamente pequeño de continentes. El Paleozoico abarca desde la proliferación de animales con concha y exoesqueleto hasta que el mundo empezó a ser dominado por los grandes reptiles y por plantas relativamente modernas, como las coníferas. (es)</li> <li style="display:none;">Le Paléozoïque est une ère géologique qui s'étend de −541 à −252,2 Ma (millions d'années). Anciennement appelée Ère Primaire ou Ère des Poissons, elle est la première ère du Phanérozoïque. Son début correspond classiquement à l'apparition de nombreux animaux à coquilles dures, bien que l'on sache maintenant qu'il en existe depuis l'Édiacarien, dernier système du Néoprotérozoïque (l'ère précédant le Paléozoïque). Il s'achève par l'extinction Permien-Trias au cours de laquelle près de 95% de la faune marine et de 70% des vertébrés terrestres auraient disparu. (fr)</li> <li style="display:none;">570-230 milliún bliain ó shin. Thosaigh orgánaigh ilcheallacha is éisc ag teacht chun cinn. Roinntear an ré seo ina tréimhsí mar seo: an tréimhse Chaimbriach (570-500 milliún bliain ó shin) inar thosaigh ainmhithe mara gan chnámh droma; an tréimhse Ordaivíseach (500-435 milliún bliain ó shin) inar thosaigh na chéad éisc, fungais is feamainn; an tréimhse Shiliúrach (435-400 milliún bliain ó shin) inar tharla na chéad phlandaí ar thalamh thirim; an tréimhse Dheavónach (400-345 milliún bliain ó shin) inar mhéadaigh na héisc is ar thosaigh na feithidí is na hainmhithe tire; an tréimhse Charbónmhar (345-280 milliún bliain ó shin) inar thosaigh na reiptílí is na débheathaigh; an tréimhse Pheirmeach (280-230 milliun bliain ó shin) inar díothaíodh an-chuid de na hainmhithe gan chnámh droma is ar thosaigh na foraoisí cónaiféaracha. (ga)</li> <li>The Paleozoic (or Palaeozoic) Era is the earliest of three geologic eras of the Phanerozoic Eon.The name Paleozoic ( /ˌpæli.əˈzoʊ.ɪk, -i.oʊ-, ˌpeɪ-/ pal-ee-ə-ZOH-ik, -⁠ee-oh-, pay-;) was coined by the British geologist Adam Sedgwick in 1838by combining the Greek words palaiós (παλαιός, "old") and zōḗ (ζωή), "life", meaning "ancient life"). It is the longest of the Phanerozoic eras, lasting from 538.8 to 251.902 million years ago, and is subdivided into six geologic periods (from oldest to youngest): 1. * Cambrian 2. * Ordovician 3. * Silurian 4. * Devonian 5. * Carboniferous 6. * Permian The Paleozoic comes after the Neoproterozoic Era of the Proterozoic Eon and is followed by the Mesozoic Era. The Paleozoic was a time of dramatic geological, climatic, and evolutionary change. The Cambrian witnessed the most rapid and widespread diversification of life in Earth's history, known as the Cambrian explosion, in which most modern phyla first appeared. Arthropods, molluscs, fish, amphibians, synapsids, and diapsids all evolved during the Paleozoic. Life began in the ocean but eventually transitioned onto land, and by the late Paleozoic, great forests of primitive plants covered the continents, many of which formed the coal beds of Europe and eastern North America. Towards the end of the era, large, sophisticated synapsids and diapsids were dominant and the first modern plants (conifers) appeared. The Paleozoic Era ended with the largest extinction event of the Phanerozoic Eon, the Permian–Triassic extinction event. The effects of this catastrophe were so devastating that it took life on land 30 million years into the Mesozoic Era to recover.Recovery of life in the sea may have been much faster. (en)</li> <li style="display:none;">Paleozoikum (atau Palaeozoikum) (/ˌ p eɪ l i ə z oʊ ɪ k, ˌ p æ - /; dari palaios Yunani (παλαιός), "tua" yang berarti "kehidupan purba" adalah awal dari tiga era geologi pada zaman Fanerozoikum, mulai dari 541 sampai 252,17 juta tahun yang lalu. Era ini merupakan yang terlama dari era Fanerozoikum, dan dibagi menjadi enam periode geologiKambrium, Ordovisium, Silur, Devon, Carbonivera, dan Permia. Paleozoikum datang setelah Era Neoproterozoikum dari zaman Proterozoikum, dan diikuti oleh Era Mesozoikum. Paleozoikum adalah masa dimana perubahan geologi, iklim, dan evolusi sangatlah dramatis. Periode Kambrium menyaksikan diversifikasi kehidupan paling cepat dan luas dalam sejarah bumi, yang dikenal sebagai ledakan Kambrium, di mana filum modern pertama kali muncul. Ikan, arthropoda, amfibi, reptil, dan synapsida semuanya berevolusi pada era Paleozoikum. Kehidupan dimulai dari laut tetapi akhirnya berpindah ke daratan, dan saat akhir Paleozoikum, bumi didominasi oleh berbagai bentuk organisme. Hutan tanaman primitif berukuran raksasa menutupi benua, banyak yang kemudian membentuk lapisan batubara membentang dari Eropa hingga timur Amerika. Menjelang akhir era, reptil besar dan maju menjadi yang dominan dan tanaman modern pertama (konifer) muncul. Era Paleozoikum berakhir dengan kepunahan massal terbesar dalam sejarah bumi, yakni peristiwa kepunahan Perm-Trias. Efek dari bencana ini begitu dahsyat sehingga kehidupan di darat butuh 30 juta tahun, hingga era Mesozoikum, untuk pulih. Pemulihan kehidupan di laut diduga jauh lebih cepat. (in)</li> <li style="display:none;">Il Paleozoico, in passato noto anche come Era Primaria, è una delle più importanti divisioni della scala dei tempi geologici, una delle quattro ere geologiche tradizionali. Si estende da 542,0 ± 1,0 a 252,17 ± 0,06 milioni di anni fa. (it)</li> <li style="display:none;">고생대(古生代, Paleozoic Era)는 5억 4100만년 전부터 2억 5천2백만년 전까지의 지질 시대를 말한다. 고생대 이전을 신원생대(선캄브리아시대)이후를 중생대라고 한다. (ko)</li> <li style="display:none;">古生代（こせいだい、仏: Paléozoïque、英: Paleozoic era）は、古生代・中生代・新生代と分かれる地質時代の大きな区分の一つである。約5億4100万 - 約2億5190万年前。先カンブリア時代（隠生代）の後に相当する。地質学的には、古生代以前の地質年代をはっきりと確定することはできない。無脊椎動物の繁栄から、恐竜が繁栄しはじめる中生代の手前までの期間に対応する。 (ja)</li> <li style="display:none;">Het geologisch tijdperk Paleozoïcum (Grieks voor oud leven) is een era in de geologische tijdschaal die het gedeelte van de geschiedenis van de Aarde tussen 541 en 251,902 miljoen jaar geleden omvat. Het Paleozoïcum beslaat een grote hoeveelheid tijd, die wordt onderverdeeld in zes periodes: Cambrium, Ordovicium, Siluur, Devoon, Carboon en Perm. Het eon voorafgaand aan het Paleozoïcum wordt het Proterozoïcum genoemd, de era erna heet het Mesozoïcum. Het Paleozoïcum was een tijd van dramatische geologische, klimatologische en evolutionaire veranderingen. Het Paleozoïsche tijdperk eindigde met de grootste massa-extinctie in de geschiedenis van de Aarde, de Perm-Trias-massa-extinctie. (nl)</li> <li style="display:none;">Paleozoikum är en geologisk era som sträcker sig från 542 till 251 miljoner år sedan. Paleozoikum delas in i perioderna kambrium, ordovicium, silur, devon, karbon och perm. Kambrosilur används ofta som samlande benämning på perioderna kambrium, ordovicium och silur. (sv)</li> <li style="display:none;">Paleozoik (z gr. πᾰλαιός – dawny i ζωή – życie) – termin ma dwa znaczenia: * w sensie geochronologicznym – najstarsza era fanerozoiku, trwająca około 291 milionów lat (od 541,0 ± 1,0 do 251,902 ± 0,024 mln lat temu). Paleozoik dzieli się na sześć okresów: kambr, ordowik, sylur, dewon, karbon i perm. Nieformalnie paleozoik czasami jest dzielony na starszy paleozoik (obejmujący kambr, ordowik i sylur) oraz młodszy paleozoik (obejmujący dewon, karbon i perm). * w sensie chronostratygraficznym – najniższy eratem fanerozoiku, wyższy od neoproterozoiku, niższy od mezozoiku. Dzieli się na sześć systemów: kambr, ordowik, sylur, dewon, karbon, perm. (pl)</li> <li style="display:none;">Палеозо́йская э́ра, палеозо́й, PZ (от греч. πᾰλαιός — древний, ζωή — жизнь) — геологическая эра в истории планеты Земля, известная как эра древней жизни. Первая эра фанерозойского эона. Следует за неопротерозойской эрой и предшествует мезозойской. Началась 538,8 ± 0,2 миллиона лет назад и закончилась 251,902 ± 0,024 млн лет назад. Таким образом, она продолжалась около 287 млн лет. Делится на 6 периодов: кембрий, ордовик, силур, девон, карбон и пермь. Палеозой — время колоссальных изменений в биосфере. В кембрии происходит диверсификация различных групп животных, известная как кембрийский взрыв. В течение палеозоя появились такие группы животных, как членистоногие, моллюски и хордовые (рыбы, амфибии, синапсиды и диапсиды). Если в кембрии вся жизнь была в океанах, то к концу эры жизнь вышла и на сушу: планету покрывали леса примитивных древовидных растений, появились полностью наземные группы позвоночных, членистоногих и моллюсков. В начале эры южные материки были объединены в единый суперконтинент Гондвану, а к её концу к нему присоединились другие континенты и образовался суперконтинент Пангея. Началась эра с кембрийского взрыва таксономического разнообразия живых организмов, а закончилась массовым пермским вымиранием. Породы, образовавшиеся в течение палеозойской эры, называются палеозойской группой. Эту группу впервые выделил в 1837 году английский геолог Адам Седжвик. ▲▲▲▲▲▲ (ru)</li> <li style="display:none;">Na escala de tempo geológico, o Paleozoico (pré-AO 1990: Paleozóico) é a era do éon Fanerozoico que está compreendida entre há 542 milhões e 251 milhões de anos, aproximadamente. A era Paleozoica sucede a era Neoproterozoico do éon Proterozoico e precede a era Mesozoica de seu éon. Divide-se nos períodos Cambriano, Ordoviciano, Siluriano, Devoniano, Carbonífero e Permiano, do mais antigo para o mais recente. O nome desta era tem origem no grego palaios (παλαιός), "velho" e zoe (ζωή), "vida", significando "vida antiga". O Paleozoico corresponde praticamente a metade do Fanerozoico, com aproximadamente 300 milhões de anos. Durante esta era havia seis massas continentais principais, que conheceram montanhas enormes ao longo de suas margens, e incursões e recuos dos mares rasos através de seus interiores, como mares continentais. Muitas rochas paleozoicas são economicamente importantes. Por exemplo, rochas calcárias para finalidades industriais de construção civil, assim como os depósitos de carvão, que foram formadas durante o paleozoico. O Paleozoico é conhecido por dois dos eventos mais importantes na história da vida animal. No seu começo houve uma grande diversificação evolutiva dos animais, a explosão cambriana, em que quase todos os filos animais atuais e vários outros extintos apareceram nos primeiros milhões dos anos. Já no extremo oposto do Paleozoico ocorreu a extinção maciça, a maior da história da vida na Terra, que extinguiu aproximadamente 90% de todas as espécies animais marinhas. As causas de ambos estes eventos ainda não são bem conhecidas. Também pode ao éon Proterozoico e a antecedente à Era Mesozoica. A sua duração foi de aproximadamente 380 milhões de anos. Embora a vida já se achasse presente na Era Proterozoica, é nos terrenos mais antigos da Era Paleozoica que os vestígios de organismos se mostram mais abundantes. De acordo com os dados paleontológicos, no Cambriano achavam-se presentes todos os grandes grupos de invertebrados. As formas ancestrais da fauna cambriana são desconhecidas ou porque o elevado metamorfismo e os dobramentos a que foram sujeitas as rochas da Era Proterozoica as destruíram, ou porque a erosão apagou grande parte dessa documentação antes da deposição dos sedimentos cambrianos. Os animais do início da Era Paleozoica viveram dominantemente em ambiente marinho: graptólitos, trilobites, moluscos, briozoários, braquiópodes, equinodermos, corais, etc. Os peixes surgiram no Ordoviciano, nas águas doces. As plantas terrestres mais antigas conhecidas datam do Siluriano (Austrália). No Carbonífero e também no Permiano constituíram grandes florestas das quais se originaram carvões em várias partes do mundo. Daí a designação de dada em esses dois períodos conjuntamente. Especialmente curiosas foram as Pteridospermae, vulgarmente conhecidas como "fetos com sementes". Os insetos mais antigos datam do Devoniano. Os anfíbios surgiram no Devoniano e os répteis no Carbonífero. Angiospermas, aves e mamíferos apareceram mais tarde, na Era Mesozoica. A paleogeografia da Era Paleozoica é a matéria de controvérsia. As similaridades demonstradas entre a geologia da parte meridional da América do Sul, África do Sul, Índia e Austrália- flora fóssil comum, designada flora de Glossópteris, vestígios de glaciação tipo inlândsis, aparentemente da mesma idade, levaria, segundo certos autores, à aceitação de um antigo continente, Continente de Gonduana, reunindo tais regiões, ou, segundo outros, à suposição de que elas estiveram diretamente unidas até o fim da Era Mesozoica (teoria de Wegener). Dois ciclos orogenéticos importantes ocorreram na Era Paleozoica: dobramentos caledonianos do Siluriano e dobramentos hercinianos do Carbonífero. Vários grupos de animais e de plantas foram privativos da Era Paleozoica: Psilotales, vegetais que desapareceram no Devoniano; trilobites, euripterídeos, graptólitos, corais dos grupos tetracorais e tabulados; briozoários dos grupos Trepostomados e Criptos tomados; foraminíferos da família dos ; equinodermos dos grupos cistoides, blastoise e heterosteleado; peixes dos grupos Ostracodermas e Placodermas. (pt)</li> <li style="display:none;">古生代（Paleozoic，符号PZ）是地质时代中的一个代，开始于同位素年龄542±0.3百万年（Ma），结束于251±0.4Ma。古生代是显生宙的第一个代，上一个代是元古宙的新元古代，下一个代是中生代。古生代包括寒武纪、奥陶纪、志留纪、泥盆纪、石炭纪、二叠纪。其中寒武纪、奥陶纪又合称早古生代，志留纪、泥盆纪又合称中古生代，石炭纪、二叠纪又合称晚古生代。古生代意為遠古的生物時代，持續约3亿年。對動物界來說，這是一個重要時期。它以一場至今不能完全解釋清楚的進化拉開了寒武紀的序幕。寒武紀動物的活動範圍只限於海洋，但在古生代的廷續下，有些動物的活動轉向乾燥的陸地。古生代後期，爬行動物和類似哺乳動物的動物出現，古生代以迄今所知最大的一次生物絕滅宣吿完結。 (zh)</li> <li style="display:none;">Палеозой або палеозойська ера (від дав.-гр. παλαιός, «старий» і ζωή, «життя», тобто ера «стародавнього життя») (рос. палеозой; англ. Palaeozoic (Era), нім. Paläozoikum n, Erdaltertum n) — геологічна ера, що тривала від 541,0 ± 1,0 до 251,902 ± 0,024 млн років тому. Підрозділяється на шість геологічних періодів; від найранішого до найпізнішого: кембрій, ордовик, силур, девон, карбон і перм. 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href="http://www.w3.org/2003/01/geo/wgs84_pos#SpatialThing">geo:SpatialThing</a></li> </ul></td></tr><tr class="odd"><td class="col-2"><a class="uri" href="http://www.w3.org/2000/01/rdf-schema#comment">rdfs:comment</a> </td><td class="col-10 text-break"><ul> <li style="display:none;">Paleozoikum (z řec. paleos, starý a zóé, život), česky prvohory, je nejstarší ze tří geologických ér fanerozoika, nejmladšího eonu (věku) Země. Podle současného datování tato éra zahrnuje období před 541 až 252 miliony let a trvala zhruba 289 milionů let. Dělí se na celkem šest period (od nejstarší): kambrium, ordovik, silur, devon, karbon a perm. Paleozoikum začíná kambrickou explozí, mohutným rozvojem vícebuněčných organismů, a končí vymíráním na konci permu, největším hromadným vymíráním druhů v historii Země, po kterém nastupuje éra mezozoika (druhohor), nazývaná také "érou plazů". (cs)</li> <li style="display:none;">Ο Παλαιοζωικός αιώνας είναι ο πρώτος από τους τρεις του Φανεροζωικού μεγααιώνα. Καλύπτει την περιόδο από περίπου 542 εώς 251 εκατομμύρια χρόνια προ παρόντος (π.π.) (ICS, 2004) και ακολουθείται από το Μεσοζωικό αιώνα. Περιλαμβάνει έξι περιόδους. Από την νεότερη ως τη αρχαιότερη είναι οι εξής: * Η Πέρμια (299–251 π.π.). * Η Λιθανθρακοφόρος (359,2–299 π.π.) * Η Δεβόνια (416–359,2 π.π.) * Η Σιλούρια (443,7–416 π.π.) * Η Ορδοβίκια (488,3–443,7 π.π.) * Η Κάμβρια (542–488,3 π.π.) (el)</li> <li style="display:none;">Paleozoiko estas la unua erao post la antaŭkambrio, dum kiu formiĝis la kambria, ordovicia, siluria, devonia, karbonia kaj permia formacioj. Ĉi tiu erao komenciĝis antaŭ 550 milionoj da jaroj kaj daŭris ĝis 355 milionoj da jaroj. 1 En milionoj da jaroj. (eo)</li> <li style="display:none;">Das Paläozoikum, auch Erdaltertum oder Erdaltzeit, ist die älteste der drei Ären, in die das Äon Phanerozoikum in der geologischen Zeitskala untergliedert wird. Es umfasst den Zeitraum von ca. 541 Millionen Jahre bis ca. 251,9 Millionen Jahre vor heute. Auf das Paläozoikum folgte das Mesozoikum (Erdmittelalter). (de)</li> <li style="display:none;">Paleozoikoa Lurraren Historiako garai geologiko bat da. Bere iraupena 291 milioi urtekoa izan zen. Hasiera orain dela 542 milioi urte kokatzen da eta bukaera orain dela 251 milioi urte.Paleontologikoki hasiera Kanbriarreko leherketarekin bat jartzen dugu eta bukaera lehenengo extintzio masiboarekin. Bere barnean honako periodoak daude: * Kanbriarra. Orain dela 570 milioi urte. * Ordoviziarra. Orain dela 510 milioi urte * Siluriarra. Orain dela 439 milioi urte. * Devoniarra. Orain dela 408 milioi urte. * Karboniferoa. Orain dela 360 milioi urte. * Permiarra. Orain dela 280 milioi urte. (eu)</li> <li style="display:none;">Le Paléozoïque est une ère géologique qui s'étend de −541 à −252,2 Ma (millions d'années). Anciennement appelée Ère Primaire ou Ère des Poissons, elle est la première ère du Phanérozoïque. Son début correspond classiquement à l'apparition de nombreux animaux à coquilles dures, bien que l'on sache maintenant qu'il en existe depuis l'Édiacarien, dernier système du Néoprotérozoïque (l'ère précédant le Paléozoïque). Il s'achève par l'extinction Permien-Trias au cours de laquelle près de 95% de la faune marine et de 70% des vertébrés terrestres auraient disparu. (fr)</li> <li style="display:none;">Il Paleozoico, in passato noto anche come Era Primaria, è una delle più importanti divisioni della scala dei tempi geologici, una delle quattro ere geologiche tradizionali. Si estende da 542,0 ± 1,0 a 252,17 ± 0,06 milioni di anni fa. (it)</li> <li style="display:none;">고생대(古生代, Paleozoic Era)는 5억 4100만년 전부터 2억 5천2백만년 전까지의 지질 시대를 말한다. 고생대 이전을 신원생대(선캄브리아시대)이후를 중생대라고 한다. (ko)</li> <li style="display:none;">古生代（こせいだい、仏: Paléozoïque、英: Paleozoic era）は、古生代・中生代・新生代と分かれる地質時代の大きな区分の一つである。約5億4100万 - 約2億5190万年前。先カンブリア時代（隠生代）の後に相当する。地質学的には、古生代以前の地質年代をはっきりと確定することはできない。無脊椎動物の繁栄から、恐竜が繁栄しはじめる中生代の手前までの期間に対応する。 (ja)</li> <li style="display:none;">Paleozoikum är en geologisk era som sträcker sig från 542 till 251 miljoner år sedan. Paleozoikum delas in i perioderna kambrium, ordovicium, silur, devon, karbon och perm. Kambrosilur används ofta som samlande benämning på perioderna kambrium, ordovicium och silur. (sv)</li> <li style="display:none;">Paleozoik (z gr. πᾰλαιός – dawny i ζωή – życie) – termin ma dwa znaczenia: * w sensie geochronologicznym – najstarsza era fanerozoiku, trwająca około 291 milionów lat (od 541,0 ± 1,0 do 251,902 ± 0,024 mln lat temu). Paleozoik dzieli się na sześć okresów: kambr, ordowik, sylur, dewon, karbon i perm. Nieformalnie paleozoik czasami jest dzielony na starszy paleozoik (obejmujący kambr, ordowik i sylur) oraz młodszy paleozoik (obejmujący dewon, karbon i perm). * w sensie chronostratygraficznym – najniższy eratem fanerozoiku, wyższy od neoproterozoiku, niższy od mezozoiku. Dzieli się na sześć systemów: kambr, ordowik, sylur, dewon, karbon, perm. (pl)</li> <li style="display:none;">古生代（Paleozoic，符号PZ）是地质时代中的一个代，开始于同位素年龄542±0.3百万年（Ma），结束于251±0.4Ma。古生代是显生宙的第一个代，上一个代是元古宙的新元古代，下一个代是中生代。古生代包括寒武纪、奥陶纪、志留纪、泥盆纪、石炭纪、二叠纪。其中寒武纪、奥陶纪又合称早古生代，志留纪、泥盆纪又合称中古生代，石炭纪、二叠纪又合称晚古生代。古生代意為遠古的生物時代，持續约3亿年。對動物界來說，這是一個重要時期。它以一場至今不能完全解釋清楚的進化拉開了寒武紀的序幕。寒武紀動物的活動範圍只限於海洋，但在古生代的廷續下，有些動物的活動轉向乾燥的陸地。古生代後期，爬行動物和類似哺乳動物的動物出現，古生代以迄今所知最大的一次生物絕滅宣吿完結。 (zh)</li> <li style="display:none;">Палеозой або палеозойська ера (від дав.-гр. παλαιός, «старий» і ζωή, «життя», тобто ера «стародавнього життя») (рос. палеозой; англ. Palaeozoic (Era), нім. Paläozoikum n, Erdaltertum n) — геологічна ера, що тривала від 541,0 ± 1,0 до 251,902 ± 0,024 млн років тому. Підрозділяється на шість геологічних періодів; від найранішого до найпізнішого: кембрій, ордовик, силур, девон, карбон і перм. (uk)</li> <li style="display:none;">حقبة الحياة القديمة أو الحياة المبكرة أو الحَفِيريّ (باللاتينية: Paleozoic)، بالاغريقية: (palaios = παλαιός = قديم + zoe = ζωή = حياة)، وهي أول وأطول حقبة من الحقب الجيولوجية الثلاثة لدهر البشائر، امتدت من 541 ± 1.0 إلى 251.902 ± 0.024 مليون سنة مضت، لمدة 289.098 مليون سنة تقريبا. انتهت حقبة الحياة القديمة بأكبر انقراض جماعي في تاريخ الأرض، حدث انقراض البرمي-الثلاثي. وكانت آثار هذه الكارثة المدمرة بأن أنهكت الحياة على الأرض مدة 30 مليون سنة حتى تعافت في حقبة الحياة الوسطى. وكان انتعاش الحياة في البحر أسرع بكثير. (ar)</li> <li style="display:none;">El Paleozoic és l'era geològica que començà fa 541 ± 1,0 milions d'anys i s'acabà fa 251,902 ± 0,024 milions d'anys. Es tracta de la primera època de l'eó Fanerozoic, que encara dura. El seu nom deriva de les paraules gregues antigues παλαιός (paleós), que significa 'antic', i ζωή (zoé), que significa 'vida', i en el seu conjunt vol dir 'vida antiga'. La divisió del temps en diferents eres, la divisió més gran del temps geològic, ve ja de Giovanni Arduino, del segle xviii, tot i que el seu nom original per l'era ara coneguda com el Paleozoic era «Primitiu». (ca)</li> <li style="display:none;">El Paleozoico o era paleozoica es una división de la escala temporal geológica que pertenece al eón Fanerozoico, con la categoría de era (como tiempo) y eratema (como conjunto de rocas). El Paleozoico sucede al supereón Precámbrico y precede al Mesozoico. De más de 290 millones de años (M.a.) de duración, se inició hace 541 millones de años y acabó hace unos 252 millones de años. Su nombre procede del griego «palaio/παλαιο» («viejo») y «zoe/ζωη» («vida»), que significa «vida antigua». Anteriormente era conocido por los términos, hoy obsoletos, de Primario o era primaria. (es)</li> <li style="display:none;">570-230 milliún bliain ó shin. Thosaigh orgánaigh ilcheallacha is éisc ag teacht chun cinn. Roinntear an ré seo ina tréimhsí mar seo: an tréimhse Chaimbriach (570-500 milliún bliain ó shin) inar thosaigh ainmhithe mara gan chnámh droma; an tréimhse Ordaivíseach (500-435 milliún bliain ó shin) inar thosaigh na chéad éisc, fungais is feamainn; an tréimhse Shiliúrach (435-400 milliún bliain ó shin) inar tharla na chéad phlandaí ar thalamh thirim; an tréimhse Dheavónach (400-345 milliún bliain ó shin) inar mhéadaigh na héisc is ar thosaigh na feithidí is na hainmhithe tire; an tréimhse Charbónmhar (345-280 milliún bliain ó shin) inar thosaigh na reiptílí is na débheathaigh; an tréimhse Pheirmeach (280-230 milliun bliain ó shin) inar díothaíodh an-chuid de na hainmhithe gan chnámh droma is ar t (ga)</li> <li>The Paleozoic (or Palaeozoic) Era is the earliest of three geologic eras of the Phanerozoic Eon.The name Paleozoic ( /ˌpæli.əˈzoʊ.ɪk, -i.oʊ-, ˌpeɪ-/ pal-ee-ə-ZOH-ik, -⁠ee-oh-, pay-;) was coined by the British geologist Adam Sedgwick in 1838by combining the Greek words palaiós (παλαιός, "old") and zōḗ (ζωή), "life", meaning "ancient life"). It is the longest of the Phanerozoic eras, lasting from 538.8 to 251.902 million years ago, and is subdivided into six geologic periods (from oldest to youngest): (en)</li> <li style="display:none;">Paleozoikum (atau Palaeozoikum) (/ˌ p eɪ l i ə z oʊ ɪ k, ˌ p æ - /; dari palaios Yunani (παλαιός), "tua" yang berarti "kehidupan purba" adalah awal dari tiga era geologi pada zaman Fanerozoikum, mulai dari 541 sampai 252,17 juta tahun yang lalu. Era ini merupakan yang terlama dari era Fanerozoikum, dan dibagi menjadi enam periode geologiKambrium, Ordovisium, Silur, Devon, Carbonivera, dan Permia. Paleozoikum datang setelah Era Neoproterozoikum dari zaman Proterozoikum, dan diikuti oleh Era Mesozoikum. (in)</li> <li style="display:none;">Het geologisch tijdperk Paleozoïcum (Grieks voor oud leven) is een era in de geologische tijdschaal die het gedeelte van de geschiedenis van de Aarde tussen 541 en 251,902 miljoen jaar geleden omvat. Het Paleozoïcum beslaat een grote hoeveelheid tijd, die wordt onderverdeeld in zes periodes: Cambrium, Ordovicium, Siluur, Devoon, Carboon en Perm. Het eon voorafgaand aan het Paleozoïcum wordt het Proterozoïcum genoemd, de era erna heet het Mesozoïcum. (nl)</li> <li style="display:none;">Na escala de tempo geológico, o Paleozoico (pré-AO 1990: Paleozóico) é a era do éon Fanerozoico que está compreendida entre há 542 milhões e 251 milhões de anos, aproximadamente. A era Paleozoica sucede a era Neoproterozoico do éon Proterozoico e precede a era Mesozoica de seu éon. Divide-se nos períodos Cambriano, Ordoviciano, Siluriano, Devoniano, Carbonífero e Permiano, do mais antigo para o mais recente. O nome desta era tem origem no grego palaios (παλαιός), "velho" e zoe (ζωή), "vida", significando "vida antiga". (pt)</li> <li style="display:none;">Палеозо́йская э́ра, палеозо́й, PZ (от греч. πᾰλαιός — древний, ζωή — жизнь) — геологическая эра в истории планеты Земля, известная как эра древней жизни. Первая эра фанерозойского эона. Следует за неопротерозойской эрой и предшествует мезозойской. Началась 538,8 ± 0,2 миллиона лет назад и закончилась 251,902 ± 0,024 млн лет назад. Таким образом, она продолжалась около 287 млн лет. Делится на 6 периодов: кембрий, ордовик, силур, девон, карбон и пермь. ▲▲▲▲▲▲ (ru)</li> </ul></td></tr><tr class="even"><td class="col-2"><a class="uri" href="http://www.w3.org/2000/01/rdf-schema#label">rdfs:label</a> </td><td class="col-10 text-break"><ul> <li>Paleozoic (en)</li> <li style="display:none;">حقبة الحياة القديمة (ar)</li> <li style="display:none;">Paleozoic (ca)</li> <li style="display:none;">Paleozoikum (cs)</li> <li style="display:none;">Paläozoikum (de)</li> <li style="display:none;">Παλαιοζωικός αιώνας (el)</li> <li style="display:none;">Paleozoiko (eo)</li> <li style="display:none;">Era paleozoica (es)</li> <li style="display:none;">Paleozoiko (eu)</li> <li style="display:none;">Paléozoïque (fr)</li> <li style="display:none;">Pailéasóch (ga)</li> <li style="display:none;">Paleozoikum (in)</li> <li style="display:none;">Paleozoico (it)</li> <li style="display:none;">고생대 (ko)</li> <li style="display:none;">古生代 (ja)</li> <li style="display:none;">Paleozoïcum (nl)</li> 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rev="dbp:period" resource="http://dbpedia.org/resource/Upper_Svratka_Highlands" href="http://dbpedia.org/resource/Upper_Svratka_Highlands">dbr:Upper_Svratka_Highlands</a></li> <li><a class="uri" rev="dbp:period" resource="http://dbpedia.org/resource/Chu-Ili_Range" href="http://dbpedia.org/resource/Chu-Ili_Range">dbr:Chu-Ili_Range</a></li> <li><a class="uri" rev="dbp:period" resource="http://dbpedia.org/resource/Angara_Range" href="http://dbpedia.org/resource/Angara_Range">dbr:Angara_Range</a></li> <li><a class="uri" rev="dbp:period" resource="http://dbpedia.org/resource/Anti-Atlas" href="http://dbpedia.org/resource/Anti-Atlas">dbr:Anti-Atlas</a></li> <li><a class="uri" rev="dbp:period" resource="http://dbpedia.org/resource/Main_Caucasian_Range" href="http://dbpedia.org/resource/Main_Caucasian_Range">dbr:Main_Caucasian_Range</a></li> <li><a class="uri" rev="dbp:period" resource="http://dbpedia.org/resource/Sierra_Madrona" href="http://dbpedia.org/resource/Sierra_Madrona">dbr:Sierra_Madrona</a></li> <li><a class="uri" rev="dbp:period" resource="http://dbpedia.org/resource/Sierra_Norte_de_Sevilla" href="http://dbpedia.org/resource/Sierra_Norte_de_Sevilla">dbr:Sierra_Norte_de_Sevilla</a></li> <li><a class="uri" rev="dbp:period" resource="http://dbpedia.org/resource/Sierra_de_Algairén" href="http://dbpedia.org/resource/Sierra_de_Algairén">dbr:Sierra_de_Algairén</a></li> <li><a class="uri" rev="dbp:period" resource="http://dbpedia.org/resource/Sierra_de_Aracena" href="http://dbpedia.org/resource/Sierra_de_Aracena">dbr:Sierra_de_Aracena</a></li> <li><a class="uri" rev="dbp:period" resource="http://dbpedia.org/resource/Sierra_de_San_Pedro" href="http://dbpedia.org/resource/Sierra_de_San_Pedro">dbr:Sierra_de_San_Pedro</a></li> <li><a class="uri" rev="dbp:period" resource="http://dbpedia.org/resource/Sierra_de_Vicort" href="http://dbpedia.org/resource/Sierra_de_Vicort">dbr:Sierra_de_Vicort</a></li> <li><a class="uri" rev="dbp:period" resource="http://dbpedia.org/resource/Tunka_Goltsy" href="http://dbpedia.org/resource/Tunka_Goltsy">dbr:Tunka_Goltsy</a></li> <li><a class="uri" rev="dbp:period" resource="http://dbpedia.org/resource/Chrysler_Formation" href="http://dbpedia.org/resource/Chrysler_Formation">dbr:Chrysler_Formation</a></li> <li><a class="uri" rev="dbp:period" resource="http://dbpedia.org/resource/Javořice_Highlands" href="http://dbpedia.org/resource/Javořice_Highlands">dbr:Javořice_Highlands</a></li> <li><a class="uri" rev="dbp:period" resource="http://dbpedia.org/resource/Kazakh_Uplands" href="http://dbpedia.org/resource/Kazakh_Uplands">dbr:Kazakh_Uplands</a></li> <li><a class="uri" rev="dbp:period" resource="http://dbpedia.org/resource/Křižanov_Highlands" href="http://dbpedia.org/resource/Křižanov_Highlands">dbr:Křižanov_Highlands</a></li> <li><a class="uri" rev="dbp:period" resource="http://dbpedia.org/resource/Lateral_Range" href="http://dbpedia.org/resource/Lateral_Range">dbr:Lateral_Range</a></li> <li><a class="uri" rev="dbp:period" resource="http://dbpedia.org/resource/Kuznetsk_Alatau" href="http://dbpedia.org/resource/Kuznetsk_Alatau">dbr:Kuznetsk_Alatau</a></li> </ul></td></tr><tr class="even"><td class="col-2">is <a class="uri" href="http://dbpedia.org/property/period12Text">dbp:period12Text</a> of</td><td class="col-10 text-break"><ul> <li><a class="uri" rev="dbp:period12Text" resource="http://dbpedia.org/resource/History_of_life" href="http://dbpedia.org/resource/History_of_life">dbr:History_of_life</a></li> </ul></td></tr><tr class="odd"><td class="col-2">is <a class="uri" href="http://xmlns.com/foaf/0.1/primaryTopic">foaf:primaryTopic</a> of</td><td class="col-10 text-break"><ul> <li><a class="uri" rev="foaf:primaryTopic" resource="http://en.wikipedia.org/wiki/Paleozoic" href="http://en.wikipedia.org/wiki/Paleozoic">wikipedia-en:Paleozoic</a></li> </ul></td></tr> </tbody> </table> </div> </div> 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