|
MESOZOIC ERA , in geology, the name given to theSee also: period of See also: 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 See also: 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 See also: 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
.
|
|
|
[back] MESOZOA |
[next] MESQUITE, or HONEY LOCUST |
There are no comments yet for this article.
Do not copy, download, transfer, or otherwise replicate the site content in whole or in part.
Links to articles and home page are encouraged.