The History of Creation, Vol. 2 (of 2): Or the Development of the Earth and its Inhabitants by the Action of Natural CausesHaeckel, Ernst
Science
The History of Creation, Vol. 2 (of 2): Or the Development of the Earth and its Inhabitants by the Action of Natural Causes
Haeckel, Ernst
Evolution; Heredity; Human beings -- Origin
We must next bear in mind that the dead bodies of the inhabitants of the
sea are much more likely to be preserved and petrified in the deposits
of mud than those of the inhabitants of fresh water and of the land.
Organisms living on land can, as a rule, become petrified only when
their corpses fall accidentally into the water and are buried at the
bottom in the hardening layers of mud. But this event depends upon very
many conditions. We cannot therefore be astonished that by far the
majority of petrifactions belong to organisms which have lived in the
sea, and that of the inhabitants of the land proportionately only very
few are preserved in a fossil state. How many contingencies come into
play here we may infer from the single fact that of many fossil mammals,
in fact of all the mammals of the secondary, or mesozoic epoch, nothing
is known except the lower jawbone. This bone is in the first place
comparatively solid, and in the second place very easily separates
itself from the dead body, which floats on the water. Whilst the body is
driven away and dissolved by the water, the lower jawbone falls down to
the bottom of the water and is there enclosed in the mud. This explains
the remarkable fact that in a stratum of limestone of the Jurassic
system near Oxford, in the slates of Stonesfield, as yet only the lower
jawbones of numerous pouched animals (Marsupials) have been found. They
are the most ancient mammals known, and of the whole of the rest of
their bodies not a single bone exists. The opponents of the theory of
development, according to their usual logic, would from this fact be
obliged to draw the conclusion that the lower jawbone was the only bone
in the body of those animals.
Footprints are very instructive when we attempt to estimate the many
accidents which so arbitrarily influence our knowledge of fossils; they
are found in great numbers in different extensive layers of sandstone;
for example, in the red sandstone of Connecticut, in North America.
These footprints were evidently made by vertebrate animals, probably by
reptiles, of whose bodies not the slightest trace has been preserved.[1]
The impressions which their feet have left on the mud alone betray the
former existence of these otherwise unknown animals.
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account