File:Estonian Museum of Natural History Specimen No 171200 photo (g1 g1-177 jpg).jpg

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Eesti: Palaeofavosites efalveolasis Goldfuss, Favosites asper dOrb. Fossiilne korall Eesti Ülem-Ordoviitsiumi settekivimitest kuulub väljasurnud korallirühma – tabulaatsed korallid. Tabulaadid on tüüpilised varapaleosoilise merelise fauna esindajad. Nende leviku kõrgperiood jääb Silurisse. Ordoviitsiumi lõpus toimunud tabulaatide fauna mitmekesistumine ja levimine Eesti aladel tähistab Baltika paleokontinendi jõudmisest lõunapoolkera troopilisse kliimavöötmesse. Rohkem teavet selle faili ja selle eksemplari kohta lehel geocollections.info
English: Palaeofavosites efalveolasis Goldfuss, Favosites asper dOrb. Fossil coral from upper Ordovician beds belongs to the extinct group of invertebrates – tabulate corals. Tabulate corals flourished in early Palaeozoic, being in their prime in Silurian. The group became extinct at the end of Permian. The spreading and diversification of tabulate fauna in Baltic Paleobasin at the end of Ordovician, reflects the movement of Baltica paleocontinent into tropical latitudes in southern hemisphere in those times. More info about this file and about this specimen at geocollections.info
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institution QS:P195,Q12361299
Author Tiit Hunt
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current20:22, 18 August 2019Thumbnail for version as of 20:22, 18 August 20191,600 × 1,200 (351 KB)LoodusmuuseumBot (talk | contribs){{Information |Description = {{et|1=Palaeofavosites efalveolasis Goldfuss, Favosites asper dOrb. Fossiilne korall Eesti Ülem-Ordoviitsiumi settekivimitest kuulub väljasurnud korallirühma – tabulaatsed korallid. Tabulaadid on tüüpilised varapaleosoilise merelise fauna esindajad. Nende leviku kõrgperiood jääb Silurisse. Ordoviitsiumi lõpus toimunud tabulaatide fauna mitmekesistumine ja levimine Eesti aladel tähistab Baltika paleokontinendi jõudmisest lõunapoolkera troopiliss...

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