. . . . . . "Behe Triasikoa (baita ere Triasiko Goiztiarra, Buntsandstein edo Scythian izenekin ezaguna) Triasiko garaiaren lehen aroa da. Duela 252 milioi urte ingurutik duela 247 milioi inguru arteraino hedatzen da. Behe Triasikoa Induar eta Olenekiar animali garaietan banatzen da. Paleozoiko aroaren azken aldian gertatu ziren iraungipen masiboek (Permo-Triasiar iraungipen masiboa) muturreko zailtasunak sortu zizkieten bizirautea lortu zuten espezieei. Koral, brakiopodo, ekinodermo, molusku eta beste ornogabe espezie asko erabat desagertu ziren. Garai honetako itsas ornogabe arruntenak bibalbioak, gastropodoak, ammonitesak, ekinoideoak eta brakiopodo gutxi batzuk izan ziren. Lurreko animalirik arruntena izeneko belarjale sinapsido txikia zen. Behe Triasikoko faunak ez du bioaniztasunik, hau, garai osoan zehar oso homogeneoa zelarik iraungipenaren eraginaren ondorioz. Klima Behe Triasikoan (bereziki Pangea superkontinentearen barnealdean) orokorrean idorra eta lehorra zen, basamortu zabalekin, poloek klima epel bat mantentzen zuten arren. Behe Triasikoko klima epela sumendi erupzio orokortuen eraginez izan daiteke, berotze globalaren erritmoa bizkortu zutenak eta, ziuraski, Permo-Triasiar iraungipen masiboak eragin zituztenak."@eu . . . "Nella scala dei tempi geologici, il Triassico inferiore rappresenta la prima delle tre epoche o serie stratigrafiche in cui \u00E8 suddiviso il Triassico, che a sua volta \u00E8 il primo dei tre periodi in cui \u00E8 suddivisa l'era del Mesozoico. Il Triassico inferiore \u00E8 compreso tra 251,0 \u00B1 0,4 e 245,9 milioni di anni fa (Ma), preceduto dal Lopingiano, l'ultima epoca del precedente periodo Permiano, e seguito dal Triassico medio."@it . . . "Trias Awal"@in . . . "Global"@en . . . . "247.2"^^ . . . . "Early/Lower Triassic"@en . . "\u00C4ldre trias"@sv . "The Early Triassic is the first of three epochs of the Triassic Period of the geologic timescale. It spans the time between 251.902 Ma and 247.2 Ma (million years ago). Rocks from this epoch are collectively known as the Lower Triassic Series, which is a unit in chronostratigraphy. The Early Triassic is the oldest epoch of the Mesozoic Era. It is preceded by the Lopingian Epoch (late Permian, Paleozoic Era) and followed by the Middle Triassic Epoch. The Early Triassic is divided into the Induan and Olenekian ages. The Induan is subdivided into the Griesbachian and Dienerian subages and the Olenekian is subdivided into the Smithian and Spathian subages. The Lower Triassic series is coeval with the Scythian Stage, which is today not included in the official timescales but can be found in older literature. In Europe, most of the Lower Triassic is composed of Buntsandstein, a lithostratigraphic unit of continental red beds. The Early Triassic and partly also the Middle Triassic span the interval of biotic recovery from the Permian-Triassic extinction event, the most severe mass extinction event in Earth's history. A second extinction event, the Smithian-Spathian boundary event, occurred during the Olenekian."@en . . . . . . . . . . "251.902"^^ . . . . . . . . . . . . . "Untertrias"@de . . . . . . "Triassico inferiore"@it . . . . "\u0641\u062A\u0631\u0629 \u0627\u0644\u062B\u0644\u0627\u062B\u064A \u0627\u0644\u0645\u0628\u0643\u0631 (\u0628\u0627\u0644\u0625\u0646\u062C\u0644\u064A\u0632\u064A\u0629: Early Triassic)\u200F (\u0627\u0644\u0627\u0633\u0645 \u0641\u064A \u0627\u0644\u062C\u064A\u0648\u0644\u0648\u062C\u064A\u0627 \u0627\u0644\u0632\u0645\u0646\u064A\u0629) \u0623\u0648 \u0627\u0644\u062B\u0644\u0627\u062B\u064A \u0627\u0644\u0633\u0641\u0644\u064A (\u0628\u0627\u0644\u0625\u0646\u062C\u0644\u064A\u0632\u064A\u0629: Lower Triassic)\u200F (\u0627\u0644\u0627\u0633\u0645 \u0641\u064A \u0627\u0644\u062C\u064A\u0648\u0644\u0648\u062C\u064A\u0627 \u0627\u0644\u0637\u0628\u0642\u064A\u0629) \u0647\u064A \u0627\u0644\u0641\u062A\u0631\u0629 \u0627\u0644\u0623\u0648\u0644\u0649 \u0644\u0644\u0639\u0635\u0631 \u0627\u0644\u062B\u0644\u0627\u062B\u064A\u060C \u062A\u0645\u062A\u062F \u0645\u0646 251.0\u00B10.4 \u0625\u0644\u0649 245.9 \u0645\u0644\u064A\u0648\u0646 \u0633\u0646\u0629 \u0645\u0636\u062A. \u0648\u062A\u0639\u062A\u0628\u0631 \u0641\u062A\u0631\u0629 \u0627\u0644\u062B\u0644\u0627\u062B\u064A \u0627\u0644\u0645\u0628\u0643\u0631 \u0623\u0642\u062F\u0645 \u0627\u0644\u0641\u062A\u0631\u0627\u062A \u0644\u062D\u0642\u0628\u0629 \u0627\u0644\u0645\u064A\u0633\u0648\u0632\u064A. \u0648\u0642\u062F \u0643\u0627\u0646 \u064A\u0637\u0644\u0642 \u0639\u0644\u064A\u0647\u0627 \u0641\u064A \u062F\u0631\u0627\u0633\u0629 \u0627\u0644\u0637\u0628\u0642\u0627\u062A \u0627\u0644\u0635\u062E\u0631\u064A\u0629 \u0627\u0644\u0623\u0648\u0631\u0648\u0628\u064A\u0629 \" \"."@ar . "FAD of the Conodont Hindeodus parvus"@en . "3029043"^^ . . "Triassic"@en . "Early Triassic"@en . . "Epoch"@en . . . "\u524D\u671F\u4E09\u7573\u7D00"@ja . . . . . "Behe Triasikoa (baita ere Triasiko Goiztiarra, Buntsandstein edo Scythian izenekin ezaguna) Triasiko garaiaren lehen aroa da. Duela 252 milioi urte ingurutik duela 247 milioi inguru arteraino hedatzen da. Behe Triasikoa Induar eta Olenekiar animali garaietan banatzen da."@eu . "Not formally defined"@en . . . . . "Nella scala dei tempi geologici, il Triassico inferiore rappresenta la prima delle tre epoche o serie stratigrafiche in cui \u00E8 suddiviso il Triassico, che a sua volta \u00E8 il primo dei tre periodi in cui \u00E8 suddivisa l'era del Mesozoico. Il Triassico inferiore \u00E8 compreso tra 251,0 \u00B1 0,4 e 245,9 milioni di anni fa (Ma), preceduto dal Lopingiano, l'ultima epoca del precedente periodo Permiano, e seguito dal Triassico medio."@it . . "31.07979965209961"^^ . . "Series"@en . . . . "ICS Time Scale"@en . . . "Behe Triasiko"@eu . . . . . . . . . . "Early Triassic"@en . . . "\u65E9\u4E09\u53E0\u4E16\u662F\u4E09\u53E0\u7EAA\u4E09\u4E2A\u4E16\u4E4B\u9996\uFF0C\u81EA251.902Ma\u6301\u7EED\u5230247.2Ma (\u767E\u4E07\u5E74\u524D)\u3002\u8FD9\u4E00\u4E16\u7684\u5CA9\u77F3\u7EDF\u79F0\u4E3A\u4E0B\u4E09\u53E0\u7EDF\u3002 \u65E9\u4E09\u53E0\u4E16\u662F\u4E2D\u751F\u4EE3\u7684\u7B2C\u4E00\u4E2A\u4E16\uFF0C\u5B83\u4E4B\u524D\u662F\u4E50\u5E73\u4E16(\u53E4\u751F\u4EE3\u665A\u4E8C\u53E0\u4E16)\uFF0C\u4E4B\u540E\u662F\u4E2D\u4E09\u53E0\u4E16\u3002\u65E9\u4E09\u53E0\u4E16\u53EF\u88AB\u5206\u4E3A\u5370\u5EA6\u671F\u548C\u5965\u4F26\u5C3C\u514B\u671F\u3002\u5370\u5EA6\u671F\u53C8\u53EF\u5206\u4E3A\u548C\uFF0C\u5965\u4F26\u5C3C\u514B\u671F\u4E5F\u53EF\u5206\u4E3A\u548C\u3002 \u4E0B\u4E09\u53E0\u7EDF\u5728\u4EE5\u524D\u4E5F\u88AB\u79F0\u4E3A\u65AF\u57FA\u6CF0\u9636\u3002\u5728\u6B27\u6D32\uFF0C\u4E0B\u4E09\u53E0\u7EDF\u7684\u5927\u90E8\u5206\u7531\u7EC4\u6210\uFF0C\u5B83\u662F\u4E00\u4E2A\u9646\u4E0A\u7684\u5CA9\u77F3\u5730\u5C42\u5B66\u5355\u4F4D\u3002 \u751F\u7269\u5708\u5386\u7ECF\u65E9\u4E09\u53E0\u4E16\u548C\u4E00\u90E8\u5206\u4E2D\u4E09\u53E0\u4E16\uFF0C\u624D\u4ECE\u5730\u7403\u53F2\u4E0A\u89C4\u6A21\u6700\u5927\u7684\u706D\u7EDD\u4E8B\u4EF6\u2014\u2014\u4E8C\u53E0\u7EAA\uFF0D\u4E09\u53E0\u7EAA\u706D\u7EDD\u4E8B\u4EF6\u4E2D\u6062\u590D\u8FC7\u6765\u3002\u7B2C\u4E8C\u6B21\u706D\u7EDD\u4E8B\u4EF6\u2014\u2014\u53F2\u5BC6\u65AF-\u65AF\u6D3E\u65AF\u671F\u8FB9\u754C\u4E8B\u4EF6\u53D1\u751F\u5728\u5965\u4F26\u5C3C\u514B\u671F\u3002"@zh . . . "119.7058029174805"^^ . "* FAD of the Conodont Chiosella timorensis\n* Base of magnetic zone MT1n"@en . . . . . . . "25343"^^ . "Wczesny trias (ang. Early Triassic) \u2013 najstarsza epoka triasu (era mezozoiczna), trwaj\u0105ca oko\u0142o 4,7 milion\u00F3w lat (od 251,902 \u00B1 0,024 do 247,2 mln lat temu). Jest to epoka m\u0142odsza od lopingu, a starsza od \u015Brodkowego triasu. Wczesny trias dzieli si\u0119 na dwa wieki: ind i olenek. Chronostratygraficznym odpowiednikiem epoki wczesnego triasu jest oddzia\u0142 trias dolny. Dolny trias dzieli si\u0119 na dwa pi\u0119tra: ind i olenek."@pl . "Na escala de tempo geol\u00F3gico, o Tri\u00E1ssico Inferior \u00E9 a \u00E9poca do per\u00EDodo Tri\u00E1ssico da era Mesozoica do \u00E9on Fanerozoico que est\u00E1 compreendida entre h\u00E1 252,17 milh\u00F5es de anos e 247,2 milh\u00F5es de anos, aproximadamente. A \u00E9poca Tri\u00E1ssica Inferior sucede a \u00E9poca Lopingiana do per\u00EDodo Permiano da era Paleozoica de seu \u00E9on e precede a \u00E9poca Tri\u00E1ssica M\u00E9dia de seu per\u00EDodo. Divide-se nas idades Indiana e Olenequiana, da mais antiga para a mais recente."@pt . "\u65E9\u4E09\u53E0\u4E16"@zh . . "Na escala de tempo geol\u00F3gico, o Tri\u00E1ssico Inferior \u00E9 a \u00E9poca do per\u00EDodo Tri\u00E1ssico da era Mesozoica do \u00E9on Fanerozoico que est\u00E1 compreendida entre h\u00E1 252,17 milh\u00F5es de anos e 247,2 milh\u00F5es de anos, aproximadamente. A \u00E9poca Tri\u00E1ssica Inferior sucede a \u00E9poca Lopingiana do per\u00EDodo Permiano da era Paleozoica de seu \u00E9on e precede a \u00E9poca Tri\u00E1ssica M\u00E9dia de seu per\u00EDodo. Divide-se nas idades Indiana e Olenequiana, da mais antiga para a mais recente."@pt . . . "\u0641\u062A\u0631\u0629 \u0627\u0644\u062B\u0644\u0627\u062B\u064A \u0627\u0644\u0645\u0628\u0643\u0631 (\u0628\u0627\u0644\u0625\u0646\u062C\u0644\u064A\u0632\u064A\u0629: Early Triassic)\u200F (\u0627\u0644\u0627\u0633\u0645 \u0641\u064A \u0627\u0644\u062C\u064A\u0648\u0644\u0648\u062C\u064A\u0627 \u0627\u0644\u0632\u0645\u0646\u064A\u0629) \u0623\u0648 \u0627\u0644\u062B\u0644\u0627\u062B\u064A \u0627\u0644\u0633\u0641\u0644\u064A (\u0628\u0627\u0644\u0625\u0646\u062C\u0644\u064A\u0632\u064A\u0629: Lower Triassic)\u200F (\u0627\u0644\u0627\u0633\u0645 \u0641\u064A \u0627\u0644\u062C\u064A\u0648\u0644\u0648\u062C\u064A\u0627 \u0627\u0644\u0637\u0628\u0642\u064A\u0629) \u0647\u064A \u0627\u0644\u0641\u062A\u0631\u0629 \u0627\u0644\u0623\u0648\u0644\u0649 \u0644\u0644\u0639\u0635\u0631 \u0627\u0644\u062B\u0644\u0627\u062B\u064A\u060C \u062A\u0645\u062A\u062F \u0645\u0646 251.0\u00B10.4 \u0625\u0644\u0649 245.9 \u0645\u0644\u064A\u0648\u0646 \u0633\u0646\u0629 \u0645\u0636\u062A. \u0648\u062A\u0639\u062A\u0628\u0631 \u0641\u062A\u0631\u0629 \u0627\u0644\u062B\u0644\u0627\u062B\u064A \u0627\u0644\u0645\u0628\u0643\u0631 \u0623\u0642\u062F\u0645 \u0627\u0644\u0641\u062A\u0631\u0627\u062A \u0644\u062D\u0642\u0628\u0629 \u0627\u0644\u0645\u064A\u0633\u0648\u0632\u064A. \u0648\u0642\u062F \u0643\u0627\u0646 \u064A\u0637\u0644\u0642 \u0639\u0644\u064A\u0647\u0627 \u0641\u064A \u062F\u0631\u0627\u0633\u0629 \u0627\u0644\u0637\u0628\u0642\u0627\u062A \u0627\u0644\u0635\u062E\u0631\u064A\u0629 \u0627\u0644\u0623\u0648\u0631\u0648\u0628\u064A\u0629 \" \"."@ar . . . . . "Tri\u00E1ssico Inferior"@pt . . . . . . "1124293186"^^ . "El Tri\u00E1sico Inferior o Tri\u00E1sico Temprano, una divisi\u00F3n de la escala temporal geol\u00F3gica, es la primera \u00E9poca y serie del per\u00EDodo y sistema Tri\u00E1sico. Se extiende desde 252,2 \u00B1 0,5 hasta 247,2 millones de a\u00F1os. El Tri\u00E1sico Inferior se divide en los pisos Induense y Olenekiense, aunque anteriormente ambos se correspond\u00EDan con el Scythiano o Escitiense, un piso ahora obsoleto. Las extinciones masivas que se dieron al final de la era Paleozoica (extinci\u00F3n masiva del P\u00E9rmico-Tri\u00E1sico) causaron dificultades extremas para las especies que sobrevivieron. Muchas especies de corales, braqui\u00F3podos, moluscos, equinodermos y otros invertebrados desaparecieron por completo. Los invertebrados marinos m\u00E1s comunes de la \u00E9poca fueron los bivalvos, gaster\u00F3podos, ammonites, equinoideos, y unos pocos braqui\u00F3podos. El animal terrestre m\u00E1s com\u00FAn era el peque\u00F1o herb\u00EDvoro sin\u00E1psido Lystrosaurus. La fauna del Tri\u00E1sico Inferior carece de biodiversidad siendo esta relativamente homog\u00E9nea a lo largo de la \u00E9poca por los efectos de la extinci\u00F3n. El clima durante el Tri\u00E1sico Inferior (especialmente en el interior del supercontinente Pangea) era en general \u00E1rido y seco, con extensos desiertos, aunque los polos manten\u00EDan un clima templado. El clima relativamente c\u00E1lido del Tri\u00E1sico Inferior puede haber sido causado por erupciones volc\u00E1nicas generalizadas, que aceleraron el ritmo del calentamiento global y posiblemente causaron las extinciones masivas del P\u00E9rmico-Tri\u00E1sico. Las facies Buntsandstein son caracter\u00EDsticas de esta \u00E9poca.\u200B"@es . . "0.024"^^ . . . . . . . . . "* Desli Caira, Northern Dobruja, Romania\n* Guandao, Guizhou, China"@en . . . . . . . . . . . . . "The Early Triassic is the first of three epochs of the Triassic Period of the geologic timescale. It spans the time between 251.902 Ma and 247.2 Ma (million years ago). Rocks from this epoch are collectively known as the Lower Triassic Series, which is a unit in chronostratigraphy. The Lower Triassic series is coeval with the Scythian Stage, which is today not included in the official timescales but can be found in older literature. In Europe, most of the Lower Triassic is composed of Buntsandstein, a lithostratigraphic unit of continental red beds."@en . "Lower Triassic"@en . . . "Trias Awal adalah kala pertama dari Periode Trias, yang dimulai pada 252.2 juta tahun lalu, hingga 247,2 juta tahun lalu. Kala ini adalah kala paling pertama di Era Mesozoikum. Batuan dari kala ini berada tepat dibawah batuan dari Peristiwa kepunahan Perm-Trias. Trias Awal juga disebut dengan tahap Scythian, yang dapat ditemukan dalam literatur yang lebih tua. Di Eropa, batuan dari kala ini biasanya merupakan batu pasir, karena batuan dari kala ini ditemukan di (strata batuan sedimen berwarna merah, yang terbentuk di kondisi teroksidasi) kontinental, yang terbentuk di darat di kondisi gurun,"@in . . . . . . . . "\u00C4ldre trias \u00E4r en geologisk epok som varade f\u00F6r 251\u2013245 miljoner \u00E5r sedan. Det \u00E4r den f\u00F6rsta av de tre som perioden trias indelas i. Undre trias \u00E4r namnet p\u00E5 motsvarande geologiska lagerserie inom stratigrafi. Epoken omfattar etagerna indus och . I \u00E4ldre vetenskaplig, framf\u00F6r allt europeisk litteratur kallas epoken ibland Buntsandstein efter som finns i Tyskland. Efter den revidering av den geologiska tidsskalan som skedde 2004 \u00E4ndrade man dock den globala referenspunkten (GSSP) f\u00F6r \u00E4ldre trias till en lokalitet i Kina. P\u00E5 n\u00E4rmare tv\u00E5 kilometers djup under Sk\u00E5ne finns lager i som h\u00E4rr\u00F6r fr\u00E5n \u00E4ldre trias. \u00C4ldre trias inleder den mesozoiska eran, och gr\u00E4nsdragningen mellan paleozoikum och mesozoikum \u00E4r i h\u00F6g grad kopplad till perm\u2013trias-utd\u00F6endet, d\u00E5 det uppskattas att runt 95% av alla havslevande och 70% av alla landlevande arter dog ut."@sv . . . . "Trias wczesny"@pl . . . . . . . . . . . . "Stadtroda Sandstein.jpg"@en . . . . . "2001"^^ . . . . . . "Formal"@en . . . . . . "Trias Awal adalah kala pertama dari Periode Trias, yang dimulai pada 252.2 juta tahun lalu, hingga 247,2 juta tahun lalu. Kala ini adalah kala paling pertama di Era Mesozoikum. Batuan dari kala ini berada tepat dibawah batuan dari Peristiwa kepunahan Perm-Trias. Trias Awal juga disebut dengan tahap Scythian, yang dapat ditemukan dalam literatur yang lebih tua. Di Eropa, batuan dari kala ini biasanya merupakan batu pasir, karena batuan dari kala ini ditemukan di (strata batuan sedimen berwarna merah, yang terbentuk di kondisi teroksidasi) kontinental, yang terbentuk di darat di kondisi gurun,"@in . . . "31.0798 119.7058" . . . "earth"@en . . . . . . . . . "\u524D\u671F\u4E09\u7573\u7D00\uFF08\u305C\u3093\u304D\u3055\u3093\u3058\u3087\u3046\u304D\u3001Early Triassic\uFF09\u306F\u3001\u4E2D\u751F\u4EE3\u306E\u4E09\u7573\u7D00\u3092\u4E09\u5206\u3057\u305F\u3046\u3061\u306E\u6700\u521D\u306E\u5730\u8CEA\u6642\u4EE3\u3002\u7D042\u51045190\u4E072000\u5E74\u524D\u00B12\u4E074000\u5E74\u304B\u30892\u51044720\u4E07\u5E74\u306B\u3042\u305F\u308A\u3001\u53E4\u3044\u9806\u306B\u30A4\u30F3\u30C9\u30A5\u30A2\u30F3\u671F\u30FB\u30AA\u30EC\u30CD\u30AD\u30A2\u30F3\u671F\u306B\u5206\u3051\u3089\u308C\u308B\u3002\u30DA\u30EB\u30E0\u7D00\u672B\u306E\u5927\u91CF\u7D76\u6EC5\u306E\u76F4\u5F8C\u306E\u6642\u4EE3\u3067\u3042\u308A\u3001\u9678\u4E0A\u6D77\u6D0B\u5171\u306B\u751F\u614B\u7CFB\u306F\u56DE\u5FA9\u306E\u9014\u4E2D\u3067\u3042\u3063\u305F\u3002"@ja . . . "\u00C4ldre trias \u00E4r en geologisk epok som varade f\u00F6r 251\u2013245 miljoner \u00E5r sedan. Det \u00E4r den f\u00F6rsta av de tre som perioden trias indelas i. Undre trias \u00E4r namnet p\u00E5 motsvarande geologiska lagerserie inom stratigrafi. Epoken omfattar etagerna indus och . I \u00E4ldre vetenskaplig, framf\u00F6r allt europeisk litteratur kallas epoken ibland Buntsandstein efter som finns i Tyskland. Efter den revidering av den geologiska tidsskalan som skedde 2004 \u00E4ndrade man dock den globala referenspunkten (GSSP) f\u00F6r \u00E4ldre trias till en lokalitet i Kina."@sv . . . "Wczesny trias (ang. Early Triassic) \u2013 najstarsza epoka triasu (era mezozoiczna), trwaj\u0105ca oko\u0142o 4,7 milion\u00F3w lat (od 251,902 \u00B1 0,024 do 247,2 mln lat temu). Jest to epoka m\u0142odsza od lopingu, a starsza od \u015Brodkowego triasu. Wczesny trias dzieli si\u0119 na dwa wieki: ind i olenek. Chronostratygraficznym odpowiednikiem epoki wczesnego triasu jest oddzia\u0142 trias dolny. Dolny trias dzieli si\u0119 na dwa pi\u0119tra: ind i olenek."@pl . . . . . . . "El Tri\u00E1sico Inferior o Tri\u00E1sico Temprano, una divisi\u00F3n de la escala temporal geol\u00F3gica, es la primera \u00E9poca y serie del per\u00EDodo y sistema Tri\u00E1sico. Se extiende desde 252,2 \u00B1 0,5 hasta 247,2 millones de a\u00F1os. El Tri\u00E1sico Inferior se divide en los pisos Induense y Olenekiense, aunque anteriormente ambos se correspond\u00EDan con el Scythiano o Escitiense, un piso ahora obsoleto. Las facies Buntsandstein son caracter\u00EDsticas de esta \u00E9poca.\u200B"@es . . . . . . . . "POINT(119.70580291748 31.0797996521)"^^ . . . "Sandstone from the Lower Triassic Series"@en . . "Early Triassic"@en . "\u524D\u671F\u4E09\u7573\u7D00\uFF08\u305C\u3093\u304D\u3055\u3093\u3058\u3087\u3046\u304D\u3001Early Triassic\uFF09\u306F\u3001\u4E2D\u751F\u4EE3\u306E\u4E09\u7573\u7D00\u3092\u4E09\u5206\u3057\u305F\u3046\u3061\u306E\u6700\u521D\u306E\u5730\u8CEA\u6642\u4EE3\u3002\u7D042\u51045190\u4E072000\u5E74\u524D\u00B12\u4E074000\u5E74\u304B\u30892\u51044720\u4E07\u5E74\u306B\u3042\u305F\u308A\u3001\u53E4\u3044\u9806\u306B\u30A4\u30F3\u30C9\u30A5\u30A2\u30F3\u671F\u30FB\u30AA\u30EC\u30CD\u30AD\u30A2\u30F3\u671F\u306B\u5206\u3051\u3089\u308C\u308B\u3002\u30DA\u30EB\u30E0\u7D00\u672B\u306E\u5927\u91CF\u7D76\u6EC5\u306E\u76F4\u5F8C\u306E\u6642\u4EE3\u3067\u3042\u308A\u3001\u9678\u4E0A\u6D77\u6D0B\u5171\u306B\u751F\u614B\u7CFB\u306F\u56DE\u5FA9\u306E\u9014\u4E2D\u3067\u3042\u3063\u305F\u3002"@ja . . . . . . "Tri\u00E1sico Inferior"@es . "\u65E9\u4E09\u53E0\u4E16\u662F\u4E09\u53E0\u7EAA\u4E09\u4E2A\u4E16\u4E4B\u9996\uFF0C\u81EA251.902Ma\u6301\u7EED\u5230247.2Ma (\u767E\u4E07\u5E74\u524D)\u3002\u8FD9\u4E00\u4E16\u7684\u5CA9\u77F3\u7EDF\u79F0\u4E3A\u4E0B\u4E09\u53E0\u7EDF\u3002 \u65E9\u4E09\u53E0\u4E16\u662F\u4E2D\u751F\u4EE3\u7684\u7B2C\u4E00\u4E2A\u4E16\uFF0C\u5B83\u4E4B\u524D\u662F\u4E50\u5E73\u4E16(\u53E4\u751F\u4EE3\u665A\u4E8C\u53E0\u4E16)\uFF0C\u4E4B\u540E\u662F\u4E2D\u4E09\u53E0\u4E16\u3002\u65E9\u4E09\u53E0\u4E16\u53EF\u88AB\u5206\u4E3A\u5370\u5EA6\u671F\u548C\u5965\u4F26\u5C3C\u514B\u671F\u3002\u5370\u5EA6\u671F\u53C8\u53EF\u5206\u4E3A\u548C\uFF0C\u5965\u4F26\u5C3C\u514B\u671F\u4E5F\u53EF\u5206\u4E3A\u548C\u3002 \u4E0B\u4E09\u53E0\u7EDF\u5728\u4EE5\u524D\u4E5F\u88AB\u79F0\u4E3A\u65AF\u57FA\u6CF0\u9636\u3002\u5728\u6B27\u6D32\uFF0C\u4E0B\u4E09\u53E0\u7EDF\u7684\u5927\u90E8\u5206\u7531\u7EC4\u6210\uFF0C\u5B83\u662F\u4E00\u4E2A\u9646\u4E0A\u7684\u5CA9\u77F3\u5730\u5C42\u5B66\u5355\u4F4D\u3002 \u751F\u7269\u5708\u5386\u7ECF\u65E9\u4E09\u53E0\u4E16\u548C\u4E00\u90E8\u5206\u4E2D\u4E09\u53E0\u4E16\uFF0C\u624D\u4ECE\u5730\u7403\u53F2\u4E0A\u89C4\u6A21\u6700\u5927\u7684\u706D\u7EDD\u4E8B\u4EF6\u2014\u2014\u4E8C\u53E0\u7EAA\uFF0D\u4E09\u53E0\u7EAA\u706D\u7EDD\u4E8B\u4EF6\u4E2D\u6062\u590D\u8FC7\u6765\u3002\u7B2C\u4E8C\u6B21\u706D\u7EDD\u4E8B\u4EF6\u2014\u2014\u53F2\u5BC6\u65AF-\u65AF\u6D3E\u65AF\u671F\u8FB9\u754C\u4E8B\u4EF6\u53D1\u751F\u5728\u5965\u4F26\u5C3C\u514B\u671F\u3002"@zh . . . "Formal"@en . "\u0627\u0644\u062B\u0644\u0627\u062B\u064A \u0627\u0644\u0645\u0628\u0643\u0631"@ar . . . . .