P693:4, 61:1.1
50,000,000 years ago the land areas of the world were very generally
above water or only slightly submerged. The formations and deposits of this
period are both land and marine, but chiefly land. For a considerable time
the land gradually rose but was simultaneously washed down to the lower levels
and toward the seas
P693:5, 61:1.2
Early in this period and in North America the placental type of mammals suddenly
appeared, and they constituted the most important evolutionary development
up to this time. Previous orders of nonplacental mammals had existed, but
this new type sprang directly and suddenly from the pre-existent reptilian
ancestor whose descendants had persisted on down through the times of dinosaur
decline. The father of the placental mammals was a small, highly active, carnivorous,
springing type of dinosaur.
P693:6, 61:1.3
Basic mammalian instincts began to be manifested in these primitive mammalian
types. Mammals possess an immense survival advantage over all other forms
of animal life in that they can:
P694:1, 61:1.4
45,000,000 years ago the continental
backbones were elevated in association
with a very general sinking of the coast lines. Mammalian life was evolving
rapidly. A small reptilian,
egg-laying type of mammal flourished, and the
ancestors of the later kangaroos roamed Australia. Soon there were small horses,
fleet-
footed rhinoceroses,
tapirs with
proboscises, primitive pigs, squirrels,
lemurs,
opossums, and several tribes of monkeylike animals. They were all
small, primitive, and best suited to living among the forests of the mountain
regions. A large
ostrichlike land bird developed to a height of ten feet and
laid an egg nine by thirteen inches. These were the ancestors of the later
gigantic passenger birds that were so highly intelligent, and that onetime
transported human beings through the air.
P694:2, 61:1.5
The mammals of the early Cenozoic lived on land, under the water, in the air,
and among the treetops. They had from one to eleven pairs of
mammary glands,
and all were covered with considerable hair. In common with the later appearing
orders, they developed two successive sets of teeth and possessed large brains
in comparison to body size. But among them all no modern forms existed.
P694:3, 61:1.6
40,000,000 years ago the land areas of the Northern Hemisphere began
to elevate, and this was followed by new extensive land deposits and other
terrestrial activities, including lava flows, warping, lake formation, and
erosion.
P694:4, 61:1.7
During the latter part of this epoch most of Europe was submerged. Following
a slight land rise the continent was covered by lakes and bays. The Arctic
Ocean, through the Ural depression, ran south to connect with the Mediterranean
Sea as it was then expanded northward, the highlands of the Alps,
Carpathians,
Apennines, and
Pyrenees being up above the water as islands of the sea. The
Isthmus of Panama was up; the Atlantic and Pacific Oceans were separated.
North America was connected with Asia by the Bering Strait land bridge and
with Europe by way of Greenland and Iceland. The earth circuit of land in
northern latitudes was broken only by the Ural Straits, which connected the
arctic seas with the enlarged Mediterranean.
P694:5, 61:1.8
Considerable
foraminiferal limestone was deposited in European waters. Today
this same stone is elevated to a height of 10,000 feet in the Alps, 16,000
feet in the Himalayas, and 20,000 feet in Tibet. The chalk deposits of this
period are found along the coasts of Africa and Australia, on the west coast
of South America, and about the West Indies.
P694:6, 61:1.9
Throughout this so-called
Eocene period the evolution of mammalian
and other related forms of life continued with little or no interruption.
North America was then connected by land with every continent except Australia,
and the world was gradually overrun by primitive mammalian fauna of various
types.