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See also:CAINOZOIC (from the Gr. icalvbs, See also:recent, See also:life) , also written Cenozoic (See also:American), Kainozoisch, Citnozoisch (See also:German), Cenozoaire (See also:Renevier), in See also:geology, the name given to the youngest of the three See also:great eras of See also:geological See also:time, the other two being the Mesozoic and Palaeozoic eras . Some authors have employed the See also:term " Neozoic " (Neozoisch) with the same significance, others have restricted its application to the See also:Tertiary See also:epoch (Neozoique, De See also:Lapparent) . The " Neogene " of Homes (1853) included the See also:Miocene and See also:Pliocene periods; Renevier subsequently modified its See also:form to Neogenique . The remaining Tertiary periods were classed as Paleogaen by See also:Naumann in 1866 . The word " Neocene " has been used in See also:place of Neozoic, but its employment is open to objection . Some confusion has been introduced by the use of the term See also:Cainozoic to include, on the one See also:hand, the Tertiary See also:period alone, and on the other hand, to make it include both the Tertiary and the See also:post-Tertiary or See also:Quaternary epochs; and in See also:order that it may See also:bear a relationship to the concepts of time and faunal development similar to those indicated by the terms Mesozoic and Palaeozoic it is advisable to restrict its use to the latter alternative . Thus the Cainozoic era would embrace all the geological periods from See also:Eocene to See also:Recent . (See TERTIARY and See also:PLEISTOCENE.) (J . A . |
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