Fossils: A Story of the Rocks and Their Record of Prehistoric LifeMarkman, Harvey C.
Science
Fossils: A Story of the Rocks and Their Record of Prehistoric Life
Markman, Harvey C.
Fossils; Paleontology
If most of these conclusions are correct we have here another case of
over-specialization and a possible explanation of the extinction of two
species. Such evidence as we have is far from conclusive, for there is
no proof that Rancho La Brea was the last stand of either the
saber-tooth or the ground-sloth. Both races were widely distributed and
their living conditions could not have been exactly duplicated in other
localities. It has been suggested, however, that _Smilodon_ ate the last
of _Mylodon_, and starved soon afterward because it had become unable to
partake of other foods. The conjecture is offered for what it is worth,
together with the facts on which the story has been based.
The geological record for Pleistocene time is not as complete as one
might imagine. Numerous localities have produced representative fossils
but the yield is rarely large enough to solve many of the riddles which
are constantly arising as investigation proceeds. Aside from those areas
which bordered the retreating ice cap and where living conditions were
far from favorable, the sedimentary deposits of this period are not
continuous over large areas. Many Pleistocene fossils are found in
stream channel beds which are always subject to removal by subsequent
floods.
[Illustration: Early Man in North America
There is abundant evidence to indicate that the great elephants of
Pleistocene time were hunted by primitive Americans whose only
weapons were darts or spears tipped with points of stone. A skull
and the lower jaws of several mammoths are shown here.]
Isolated patches of fossil-bearing sediments frequently record the
migration of animals in unmistakable terms, but the details of the
wanderings and the conditions encountered in the newly established
habitats are often left in doubt. To correlate the facts revealed at one
locality with findings at other places and, if possible, to date all
prehistoric events with a greater degree of accuracy are among the major
tasks of current investigations.
THE AGE OF MAN
The Pleistocene or “Ice Age,” and the Recent period in which we are
living at the present moment are not sharply separated by any event
readily recognized or dated, and the two combined are of very short
duration as compared with other periods more clearly established by the
passing of centuries. Together they comprise the Age of Man as commonly
recognized, with about a million years representing the Pleistocene
period, some ten to twenty thousand years the Recent. When geologists of
the nineteenth century suggested that the coming of man should be
regarded as the beginning of a new era, the name Psychozoic was
proposed, and to some extent this term has been applied to the present
period. More in keeping with other period names is Holocene, meaning
_entirely recent_. Common usage, however, applies the simple term Recent
to this unfinished chapter which is also without a clear-cut beginning.
Public-domain text, read in full here on John Shaqi.
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