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- Eocene abstract "The Eocene /ˈiːəsiːn/ (symbol Eo ) epoch, lasting from 56 to 33.9 million years ago, is a major division of the geologic timescale and the second epoch of the Paleogene Period in the Cenozoic Era. The Eocene spans the time from the end of the Palaeocene Epoch to the beginning of the Oligocene Epoch. The start of the Eocene is marked by a brief period in which the concentration of the carbon isotope 13C in the atmosphere was exceptionally low in comparison with the more common isotope 12C. The end is set at a major extinction event called the Grande Coupure (the "Great Break" in continuity) or the Eocene–Oligocene extinction event, which may be related to the impact of one or more large bolides in Siberia and in what is now Chesapeake Bay. As with other geologic periods, the strata that define the start and end of the epoch are well identified, though their exact dates are slightly uncertain.The name Eocene comes from the Greek ἠώς (eos, dawn) and καινός (kainos, new) and refers to the "dawn" of modern ('new') fauna that appeared during the epoch.".
- Eocene wikiPageExternalLink terpaleo.html.
- Eocene wikiPageExternalLink Basilosaurus1.html.
- Eocene wikiPageExternalLink Eocene-Epoch.
- Eocene wikiPageExternalLink fossils.
- Eocene wikiPageExternalLink querydb.php?age=Eocene&aktion=suche.
- Eocene wikiPageExternalLink Harlan1834b.html.
- Eocene wikiPageExternalLink Eocene.htm.
- Eocene wikiPageExternalLink eocene.html.
- Eocene wikiPageExternalLink arctic.
- Eocene wikiPageExternalLink www.scotese.com.
- Eocene wikiPageExternalLink newpage9.htm.
- Eocene wikiPageExternalLink gssp.htm.
- Eocene wikiPageID "9419".
- Eocene wikiPageRevisionID "606021441".
- Eocene hasPhotoCollection Eocene.
- Eocene subject Category:Cenozoic.
- Eocene subject Category:Eocene.
- Eocene comment "The Eocene /ˈiːəsiːn/ (symbol Eo ) epoch, lasting from 56 to 33.9 million years ago, is a major division of the geologic timescale and the second epoch of the Paleogene Period in the Cenozoic Era. The Eocene spans the time from the end of the Palaeocene Epoch to the beginning of the Oligocene Epoch. The start of the Eocene is marked by a brief period in which the concentration of the carbon isotope 13C in the atmosphere was exceptionally low in comparison with the more common isotope 12C.".
- Eocene label "Eoceen".
- Eocene label "Eocen".
- Eocene label "Eocene".
- Eocene label "Eocene".
- Eocene label "Eoceno".
- Eocene label "Eoceno".
- Eocene label "Eozän".
- Eocene label "Éocène".
- Eocene label "Эоцен".
- Eocene label "الإيوسين".
- Eocene label "始新世".
- Eocene label "始新世".
- Eocene sameAs Eocén.
- Eocene sameAs Eozän.
- Eocene sameAs Eoceno.
- Eocene sameAs Eozeno.
- Eocene sameAs Éocène.
- Eocene sameAs Eosen.
- Eocene sameAs Eocene.
- Eocene sameAs 始新世.
- Eocene sameAs 에오세.
- Eocene sameAs Eoceen.
- Eocene sameAs Eocen.
- Eocene sameAs Eoceno.
- Eocene sameAs m.02kwm.
- Eocene sameAs Mx4rlytdrJ0rQdeZcNDtLoxupw.
- Eocene sameAs Q76274.
- Eocene sameAs Q76274.
- Eocene wasDerivedFrom Eocene?oldid=606021441.
- Eocene isPrimaryTopicOf Eocene.