Online Encyclopedia

MESOZOIC ERA

Online Encyclopedia
Originally appearing in Volume V18, Page 188 of the 1911 Encyclopedia Britannica.
Spread the word: del.icio.us del.icio.us it!

MESOZOIC ERA  , in

geology, the name given to the period of time between the Palaeozoic and Cainozoic eras; it is synonymous with the older and less satisfactory
See also:
term " Secondary " as applied to the major divisions of
See also:
geological time and with the " Flozgebirge " of the Wernerian school . This era is sub-divided into a
See also:
lower, Triassic, a
See also:
middle,
See also:
Jurassic, and an upper, Cretaceous period or epoch . The duration of the Mesozoic era was not more than one
See also:
fourth of that of the Palaeozoic era, measured by the thickness of strata formed during these periods . It was an era marked by peaceful conditions in the earth's crust and by a general freedom from volcanic activity . The sediments as a whole are characterized by the prevalence of limestones as compared with those of the preceding era; they are seldom much altered or disturbed except in the younger mountain regions . Mammals, represented by small marsupials, and
See also:
primitive forms of birds and bony fishes make their first appearance in rocks of Mesozoic age . Saurian reptiles played an extremely prominent
See also:
part;
See also:
ammonites and belemnites lived in extraordinary variety in the seas along with the echinoids and pelecypods, which had to a
See also:
great extent supplanted the crinoids and brachiopods of the preceding periods . The first clear indications of monocotyledonous and dicotyledonous
See also:
angiosperms made their appearance, while Cycads and Conifers constituted the bulk of the
See also:
land
See also:
flora .

End of Article: MESOZOIC ERA
[back]
MESOZOA
[next]
MESQUITE, or HONEY LOCUST

Additional information and Comments

There are no comments yet for this article.
» Add information or comments to this article.
Please link directly to this article:
Highlight the code below, right click and select "copy." Paste it into a website, email, or other HTML document.