Some Salient Points in the Science of the EarthDawson, John William, Sir
Science
Some Salient Points in the Science of the Earth
Dawson, John William, Sir
Geology; Paleontology
But what are we to say of the cause of this new series of facts, so
wonderfully superimposed upon the merely vegetable and mineral? Must
it remain to us as an act of creation, or was it derived from some
pre-existing matter in which it had been potentially present? Science
fails to inform us, but conjectural "phylogeny" steps in and takes its
place. Haeckel, the prophet of this new philosophy, waves his magic
wand, and simple masses of sarcode spring from inorganic matter, and
form diffused sheets of sea slime, from which are in time separated
distinct amœboid and foraminiferal forms. Experience, however, gives us
no facts whereon to build this supposition, and it remains neither more
nor less scientific or certain than that old fancy of the Egyptians,
which derived animals from the fertile mud of the Nile.
If we fail to learn anything of the origin of Eozoon, and if its life
processes are just as inscrutable as those of higher creatures, we
can at least enquire as to its history in geological time. In this
respect we find, in the first place, that the Protozoa have not had a
monopoly in their profession of accumulators of calcareous rock.
Originated by Eozoon in the old Laurentian time, this process has
been proceeding throughout the geological ages; and while Protozoa,
equally simple with the great prototype of the race, have been and
are continuing its function, and producing new limestones in every
geological period, and so adding to the volume of the successive
formations, new workers of higher grades have been introduced, capable
of enjoying higher forms of animal activity, and equally of labouring
at the great task of continent building; of existing, too, in seas
less rich in mineral substances than those of the Eozoic time, and for
that very reason better suited to higher and more skilled artists. It
is to be observed in connection with this, that as the work of the
Foraminifers has thus been assumed by others, their size and importance
have diminished, and the larger forms of more recent times have some of
them been fain to build up their hard parts of cemented sand instead of
limestone.
Public-domain text, read in full here on John Shaqi.
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