Vom Urknall bis zum Weltuntergang
vom Urknall bis zum Weltuntergang
{"blocks":[{"key":"3h0eg","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"8v0lj","text":"-","type":"atomic","depth":0,"inlineStyleRanges":[],"entityRanges":[{"offset":0,"length":1,"key":0}],"data":{}},{"key":"9l1pt","text":"Der Urknall","type":"header-two","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"6croa","text":"Filter","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[{"offset":0,"length":6,"key":1}],"data":{}},{"key":"anick","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"dqe95","text":"-","type":"atomic","depth":0,"inlineStyleRanges":[],"entityRanges":[{"offset":0,"length":1,"key":2}],"data":{}},{"key":"b77g2","text":"Vor 13,8 Mrd. Jahren begann alles mit dem Urknall, dem Tag ohne gestern. Raum und Zeit waren plötzlich da.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[{"offset":42,"length":7,"key":3}],"data":{}},{"key":"ek1a2","text":"Der Urknall, auch Big Bang genannt, ist das Modell, das beschreibt, wie das Universum entstanden ist. Nach dem Urknall expandierte das Universum rasch und wurde immer kälter und dunkler. Etwa 300.000 Jahre später bildeten sich die ersten Atome, hauptsächlich Wasserstoff und Helium.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"em6hk","text":"Die ersten Sterne entstanden in kosmischen Maßstäben schon relativ kurz nach dem Urknall aus kollabierenden Gaswolken. Diese waren sehr massereich, und es konnten darin schwere Elemente wie Kohlenstoff, Sauerstoff und Eisen erbrütet werden.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[{"offset":4,"length":13,"key":4}],"data":{}},{"key":"6sc59","text":"Wegen ihrer großen Masse war die Lebensdauer dieser Sterne mit 3 -10 Millionen Jahren aber recht kurz und sie explodierten in einer Supernova.Supernova","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[{"offset":142,"length":9,"key":5}],"data":{}},{"key":"2uv5r","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"ah6m0","text":"Die Entstehung der Erde","type":"header-two","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"2uk0s","text":"Filter","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[{"offset":0,"length":6,"key":6}],"data":{}},{"key":"1lup4","text":"-","type":"atomic","depth":0,"inlineStyleRanges":[],"entityRanges":[{"offset":0,"length":1,"key":7}],"data":{}},{"key":"dh7l7","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"at8fb","text":"Neun Milliarden Jahre nach dem Urknall konnte dann endlich unser Sonnensystem entstehen und damit auch unsere Erde.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[{"offset":59,"length":18,"key":8}],"data":{}},{"key":"f9ar6","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"3c5sb","text":"Unser Sonnensystem entstand, als sich aus einer Wolke von Gasen und Staub, die sich im Weltraum befand, ein Stern bildete. Dieser Stern, die Sonne, zog das umgebende Material an und es bildete sich eine Scheibe aus Gasen und Staub um die Sonne. ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"cpqpi","text":"Im Laufe der Zeit kondensierten immer größere Klumpen aus diesem Material und bildeten schließlich die Planeten unseres Sonnensystems.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"efcdg","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"br9b2","text":"Die Erde entstand vor etwa 4,54 Milliarden Jahren. ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"fomit","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"4r2tm","text":"Die Entstehung des Lebens","type":"header-two","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"jqtb","text":"Filter","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[{"offset":0,"length":6,"key":9}],"data":{}},{"key":"fgbs2","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"9e5kg","text":"Es gibt viele Fragen, die noch immer unbeantwortet sind, wenn es um die Entstehung des Lebens auf der Erde geht. Zum Beispiel ist es noch immer unklar, wie das erste Lebewesen überhaupt entstanden ist. Einige Wissenschaftler glauben, dass das Leben auf der Erde durch Meteoriten oder Kometen, die organische Moleküle enthielten, auf die Erde gebracht wurde. Andere glauben, dass das Leben auf der Erde spontan entstanden ist, wenn bestimmte Bedingungen erfüllt waren.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"2vkps","text":"Es gibt einige Theorien darüber, wie das Leben auf der Erde entstanden sein könnte, aber keine von ihnen ist bisher vollständig bewiesen. Eines der bekanntesten Modelle ist das sogenannte \"RNA-Welt\"-Modell, das besagt, dass das Leben auf der Erde durch die Entstehung von RNA, einem biologischen Molekül, entstanden ist.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"4eh0f","text":"Eine Theorie besagt, dass es einen einzigen gemeinsamen Vorfahren aller Lebewesen gibt, Luca (Last Universal Common Ancestor) genannt, der vor 3,6 Mrd. Jahren entstanden ist. Luca war vermutlich ein einfaches, einzelliges Lebewesen, das in den Ozeanen der Erde existierte.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[{"offset":88,"length":37,"key":10}],"data":{}},{"key":"ek31t","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"ed0e6","text":"Die Entwicklung des Lebens","type":"unstyled","depth":0,"inlineStyleRanges":[{"offset":0,"length":26,"style":"BOLD"},{"offset":0,"length":26,"style":"ITALIC"}],"entityRanges":[],"data":{}},{"key":"40vj1","text":"Filter","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[{"offset":0,"length":6,"key":11}],"data":{}},{"key":"9pa4b","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"73mq5","text":"Nachdem das Leben erstmals vor etwa 3,5 Milliarden Jahren entstanden war, entwickelten sich im Laufe der Zeit immer komplexere Lebewesen.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"1nksj","text":"Eines der frühesten Ereignisse in der Entwicklung des Lebens auf der Erde war die sogenannte \"große Sauerstoffkatastrophe\", die vor etwa 2,4 Milliarden Jahren stattfand. Mikroorganismen hatten gelernt, aus einer einfachen Form der Photosynthese Energie zu gewinnen. Als Abfallstoff blieb Sauerstoff übrig.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[{"offset":93,"length":29,"key":12}],"data":{}},{"key":"7go3e","text":"Während dieser Zeit wurden plötzlich so große Sauerstoffmengen in der Atmosphäre frei, dass dies zu einer Veränderung der Lebensbedingungen auf der Erde führte. Einige Lebewesen starben aus, während andere sich an die veränderten Bedingungen anpassten und überlebten.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"5v4h6","text":"Im Laufe der Zeit entwickelten sich erste Lebewesen mit einem richtigen Zellkern.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[{"offset":72,"length":8,"key":13}],"data":{}},{"key":"7r9v8","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"3s0ip","text":"Das Leben kam aber erst mit der kambrischen Explosion knapp 2 Milliarden Jahre nach der großen Sauerstoffkatastrophe so richtig in Gang. In einem geologisch sehr kurzen Zeitraum vor etwa 541 Millionen Jahren entwickelte sich das Leben auf der Erde rapide weiter. Es kam zu einem explosionsartigen Anstieg der Vielfalt von Arten wie Schwämmen, Stachelhäutern, Gliederfüßlern, Nessel-, Weich- und Wirbeltieren. Fast gleichzeitige kamen Vertreter fast aller heutigen Tierstämme vor. Das Phanerozoikum, das Zeitalter des sichtbaren Lebens begann.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[{"offset":32,"length":21,"key":14},{"offset":484,"length":13,"key":15}],"data":{}},{"key":"aiofh","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"72htt","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"cb0ov","text":"-","type":"atomic","depth":0,"inlineStyleRanges":[],"entityRanges":[{"offset":0,"length":1,"key":16}],"data":{}},{"key":"c8q0v","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"69fej","text":"Eine der ersten Gruppen von Tieren, die sich auf der Erde entwickelten, waren die Trilobiten, die vor etwa 521 Millionen Jahren die Erde besiedelten. Diese Tiere hatten einen körpereigenen Schutzpanzer und konnten sich fortbewegen. Nahezu alle Meere war von diesen Tieren bevölkert.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[{"offset":82,"length":10,"key":17}],"data":{}},{"key":"d3rlv","text":"Wir befinden uns in einem Erdzeitalter, das sich Ordovizium nennt. Das Leben spielt sich hier noch hauptsächlich im Meer ab. Auf den Kontinenten war es durch die fehlende Ozonschicht und damit dem fehlenden Schutz vor UV-Strahlung für Lebewesen noch sehr unwirtlich. Dennoch beginnen im frühen Ordovizium die ersten Pflanzen und sogar die ersten Gliederfüßler sich auf das Land auszubreiten.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[{"offset":49,"length":10,"key":18}],"data":{}},{"key":"47t8h","text":"Am Ende des Ordoviziums stand dann aber das erste große Massenaussterben der Erde. ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[{"offset":56,"length":16,"key":19}],"data":{}},{"key":"dfolc","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"872r3","text":"Die Entwicklung des Lebens erfuhr immer wieder auch zuvor große Änderungen durch solche Massenaussterben.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"24meb","text":"Ein Beispiel war die bereits erwähnte große Sauerstoffkatastrophe. Allein im Kambrium sind drei Massenaussterben bekannt. Durch die schnelle Zunahme an verschiedenen Arten in dieser Zeit war jedoch das Hintergrundartensterben so derart hoch, dass eine genaue Abgrenzung von Artenaustausch und Massenaussterben schwierig ist.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[{"offset":77,"length":8,"key":20}],"data":{}},{"key":"c47h6","text":"Wir konzentrieren uns hier im Folgenden auf die fünf großen bekannten Massenaussterben (Big Five).","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"79luh","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"a7onk","text":"Massenaussterben am Ende des Ordoviziums","type":"unstyled","depth":0,"inlineStyleRanges":[{"offset":0,"length":40,"style":"BOLD"},{"offset":0,"length":40,"style":"ITALIC"}],"entityRanges":[{"offset":0,"length":40,"key":21}],"data":{}},{"key":"662g9","text":"Das erste große Massenaussterben war das eben genannte Ordovizische Massenaussterben, bei dem unter anderem viele Trilobitenarten verschwanden. Als Ursache wird die Anden-Sahara-Eiszeit vermutet, deren Grund man aber nicht kennt.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[{"offset":55,"length":29,"key":22},{"offset":165,"length":20,"key":23}],"data":{}},{"key":"1qpck","text":"Erst nach dieser Eiszeit traten auch die Wirbeltiere ihren Gang ans Land an.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[{"offset":41,"length":31,"key":24}],"data":{}},{"key":"bkk9g","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"9r5hk","text":"Kellwasser-Ereignis","type":"unstyled","depth":0,"inlineStyleRanges":[{"offset":0,"length":19,"style":"BOLD"},{"offset":0,"length":19,"style":"ITALIC"}],"entityRanges":[{"offset":0,"length":19,"key":25}],"data":{}},{"key":"688jd","text":"Die Gründe für das zweite große Massensterben, bei dem etwa 50-75% der Lebewesen ausstarben sind nur in Umrissen bekannt.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"djodr","text":"Man weiß, dass sich die chemische Beschaffenheit der Meere drastisch veränderte. Von den Pflanzen, die durch ihre Wurzeln den Boden veränderten und dadurch giftige Stoffe ins Meer gespült wurden, bis hin zu einer Supernova wird hier viel spekuliert.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"f2lj2","text":"Die Trilobiten trotzen aber diesen und vielen Katastrophen mehr, wenngleich ihre Population und ihr Artenreichtum immer sehr von den Ereignissen betroffen waren.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"bhia7","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"786oh","text":"Massenaussterben am Ende des Perm","type":"unstyled","depth":0,"inlineStyleRanges":[{"offset":0,"length":33,"style":"BOLD"},{"offset":0,"length":33,"style":"ITALIC"}],"entityRanges":[{"offset":0,"length":33,"key":26}],"data":{}},{"key":"7tgfq","text":"-","type":"atomic","depth":0,"inlineStyleRanges":[],"entityRanges":[{"offset":0,"length":1,"key":27}],"data":{}},{"key":"7kmjp","text":"Vor etwa 252 Millionen Jahren war mit dem \"Perm-Trias-Massenaussterben\", bei dem 98% der Pflanzen und Tieren ausstarben, dann aber auch die Zeit der Trilobiten vorbei. Es war das größte Sterbeereignis der bekannten Erdgeschichte.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[{"offset":42,"length":29,"key":28}],"data":{}},{"key":"d1fr8","text":"Vermutliche Ursache war ein riesiger Vulkanausbruch in Sibirien, dessen Auswirkungen sich noch heute im Sibirischen Trapp, einem Flutbasalt zeigen. Das Bild zeigt die immensen Ausdehnungen des sibirischen Trapp.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[{"offset":104,"length":17,"key":29}],"data":{}},{"key":"3222a","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"cgeqe","text":"Massenaussterben zwischen Trias und Jura","type":"unstyled","depth":0,"inlineStyleRanges":[{"offset":0,"length":40,"style":"BOLD"},{"offset":0,"length":40,"style":"ITALIC"}],"entityRanges":[{"offset":0,"length":40,"key":30}],"data":{}},{"key":"2tf6a","text":"201 Millionen Jahre vor unserer Zeit kam es zum fünftgrößten bekannten Massenaussterben. 80% der Lebewesen starben hierbei aus. Ursache vermutlich auch hier wieder riesige Vulkanausbrüche, die durch die Trennung der Kontinentalschollen von Europa und Nordamerika verursacht wurden. Die Entstehung der Zentralatlantischen Magmenprovinz fällt in diese Zeit.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[{"offset":301,"length":33,"key":31}],"data":{}},{"key":"epjb1","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"1qkbl","text":"Das Ende der Dinos","type":"unstyled","depth":0,"inlineStyleRanges":[{"offset":0,"length":18,"style":"BOLD"},{"offset":0,"length":18,"style":"ITALIC"}],"entityRanges":[{"offset":4,"length":14,"key":32}],"data":{}},{"key":"b486t","text":"-","type":"atomic","depth":0,"inlineStyleRanges":[],"entityRanges":[{"offset":0,"length":1,"key":33}],"data":{}},{"key":"6ehmq","text":"Im Trias konnten sich dann die Dinosaurier entwickeln, die über 160 Millionen Jahre die Welt beherrschten.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[{"offset":31,"length":11,"key":34}],"data":{}},{"key":"58f8m","text":"Lange nach den ersten Dinosauriern, in einem Zeitalter, das sich Kreide nennt, konnten dann die ersten Säugetiere ihren Platz auf der Erde finden.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[{"offset":96,"length":17,"key":35}],"data":{}},{"key":"cjnmg","text":"Das Ende der Epoche der Dinosaurier passt wieder sehr gut mit einem Vulkanausbruch zusammen. Dieser verursachte den Dekkan-Trapp im westlichen Indien.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"5tunc","text":"Auch ein Meteoriteneinschlag auf der Yuccatan-Halbinsel vor etwa 66 Millionen Jahren könnte ein Mitverursacher des großen Sterbens gewesen sein.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"6cug1","text":"Staub und Dreck blockierten das Sonnenlicht und führten zu einer Abkühlung der Erde.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"6qc69","text":"Das darauf folgende Massenaussterben markiert den Übergang von der Kreidezeit zum Paläogen (früher erster Teil des Tertiär). 76% aller Lebewesen starben dabei aus.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[{"offset":20,"length":16,"key":36}],"data":{}},{"key":"rplq","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"3ul45","text":"Nach dem Aussterben der Dinosaurier konnten sich die Säugetiere entfalten, die sich von Pflanzen ernährten. Sie waren kleiner als die Dinosaurier und konnten sich besser an die veränderten Lebensbedingungen anpassen.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"9stgk","text":"Übrigens begann ungefähr zur Ende der Dinozeit auch die Faltung der Alpen.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[{"offset":56,"length":17,"key":37}],"data":{}},{"key":"9c6ps","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"7kni5","text":"Der Mensch","type":"header-two","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"20i91","text":"Filter","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[{"offset":0,"length":6,"key":38}],"data":{}},{"key":"8pomu","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"bl6ne","text":"-","type":"atomic","depth":0,"inlineStyleRanges":[],"entityRanges":[{"offset":0,"length":1,"key":39}],"data":{}},{"key":"fent","text":"Im Laufe der Zeit entwickelten sich immer komplexere Säugetiere, unter anderem begann vor 6 Millionen Jahren die allmähliche Entwicklung des Menschen. Diese ersten Hominiden waren noch sehr affenähnlich und lebten in den Wäldern Afrikas.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"2vt0a","text":"Ein wichtiger Schritt im Entwicklungsprozess war die Aufrichtung des Körpers, was es den Hominiden ermöglichte, aufrecht zu gehen und die Hände frei zu haben.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"b599h","text":"Homo habilis war vor etwa 2,8 Millionen Jahren der erste Hominide, der Werkzeuge herstellen und benutzen konnte. Er war auch der erste, der Fleisch aß und damit begann, sich von Pflanzen zu ernähren.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"8j185","text":"In den folgenden Jahrmillionen entwickelten sich immer fortschrittlichere Hominiden, wie der Homo erectus und der Homo sapiens. ","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"9eng0","text":"Die ersten Menschen der Gattung Homo Sapiens, der auch wir angehören, lebten vor etwa 300.000 Jahren auf der Erde. Der Homo sapiens hatte ein größeres Gehirn als seine Vorfahren und war in der Lage, komplexe Sprache und Kultur zu entwickeln.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"9ucbb","text":"Heute leben wir, die Homo sapiens sapiens, als die einzige überlebende Art der Hominiden.","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"dl5g5","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"9oevv","text":"Das Ende","type":"header-two","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"8om85","text":"Filter","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[{"offset":0,"length":6,"key":40}],"data":{}},{"key":"9euhj","text":"","type":"unstyled","depth":0,"inlineStyleRanges":[],"entityRanges":[],"data":{}},{"key":"fdjbk","text":"Selbst wenn alles gut laufen sollte, ist in etwa einer Mrd. 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Urknall
Entstehung unseres Sonnensystems
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Spätestes Ende der Menschheit wegen Sonnenhitze
Sonne wird zum roten Riesen
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Entwicklung des Lebens auf der Erde
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Entwicklung des Menschen
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Dinosaurier
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Erste Sterne entstehen
Sonne wird zum Weißen Zwerg
Luca (Urvorfahr)
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Steinzeit
[Die Epochen der Erdgeschichte - Äontherm](165) [Äratherm](190) [System](191) [Serie](193) [Stufe](192)
erste kieferlose Fischartige
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Trilobiten
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Große Sauerstoffkatastrophe
Perm-Trias-Ereignis
Kreide-Paläogen-Grenze
Ordovizisches Massenaussterben
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Kellwasser-Ereignis
erste Säugetiere
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Homo Sapiens
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Maximum der letzen Eiszeit
Kambrische Explosion
Trias-Jura Grenze
Bildung Erdkruste und Urmeer
Erster Kontinent "Ur"
Erste Lebewesen mit Zellkern
Schneeball-Erde
Landgang der Pflanzen
Landgang der Wirbeltiere
Faltung der Alpen
Perm
Trias
Jura
Kreide
Siderium
Rhyacium
Orosirium
Statherium
Calymmium
Ectasium
Stenium
Tonium
Cryogenium
Ediacarium
Kambrium
Entfaltung der wirbellosen Tiere. Zeitepoche besonders der Arthropoden, z.B. der Trilobiten und der Stachelhäuter [Kambro-Ordovizisches Massenaussterben](-1050953)
Ordovizium
erste Wirbeltiere (kieferlose Panzerfische) [Kambro-Ordovizisches Massenaussterben](-1050953) [Ordovizisches Massenaussterben](-1065985)
Silur
Korallenriffe, erste Festlandpflanzen wie z.B. Schachtelhalme, Bärlappgewächse, Farne, ersten kiefertragende Fische aus. [Ordovizisches Massenaussterben](-1065985)
Devon
ersten baumgroße Pflanzen, erste Insekten, der Quastenflosser, erste Amphibien
Karbon
ersten großen Wälder (Basis heutiger Torflager und Steinkohlenvorkommen), erste Nacktsamer (z.B. die Tanne, Fichte, Kiefer), Riesenlibellen, erste Reptilien
Paläogen
[Kreide-Pläogen-Grenze](-55811)
Neogen
Quartär
___Das könnte dich auch interessieren:___ [Gesamtgeschichte](179) [Die Geschichte Deutschlands](251)
Phanerozoikum (Zeitalter des sichtbaren Lebens)
Anden-Sahara-Eiszeit
Sibirischer Trapp
Zentralatlantische Magmenprovinz
Dekkan-Trapp
Entstehung der Erde
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Entstehung des Mondes
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