Changes

==PAPER 60: URANTIA DURING THE EARLY LAND-LIFE ERA==   

==PAPER 60: URANTIA DURING THE EARLY LAND-LIFE ERA==   

60:0.1 The era of exclusive marine life has ended. Land elevation, cooling crust and cooling oceans, sea restriction and consequent deepening, together with a great increase of land in northern latitudes, all conspired greatly to change the world's climate in all regions far removed from the equatorial zone.

60:0.1 The era of exclusive [[marine]] life has ended. [[Land]] elevation, cooling [http://en.wikipedia.org/wiki/Earth%27s_crust crust] and cooling [[oceans]], sea restriction and consequent deepening, together with a great increase of [[land]] in northern latitudes, all conspired greatly to [[change]] the world's [[climate]] in all regions far removed from the [[equatorial]] zone.

60:0.2 The closing epochs of the preceding era were indeed the age of frogs, but these ancestors of the land vertebrates were no longer dominant, having survived in greatly reduced numbers. Very few types outlived the rigorous trials of the preceding period of biologic tribulation. Even the spore-bearing plants were nearly extinct.

60:0.2 The closing [[epochs]] of the preceding era were indeed the age of [http://en.wikipedia.org/wiki/Frog frogs], but these [[ancestors]] of the [[land]] [http://en.wikipedia.org/wiki/Vertebrates vertebrates] were no longer [[dominant]], having [[survived]] in greatly reduced numbers. Very few types outlived the rigorous trials of the preceding period of [[biologic]] [[tribulation]]. Even the [http://en.wikipedia.org/wiki/Spores spore]-bearing [[plants]] were nearly [[extinct]].

==60:1. THE EARLY REPTILIAN AGE==   

==60:1. THE EARLY REPTILIAN AGE==