Australasian Fossils: A Students' Manual of PalaeontologyChapman, Frederick
Science
Australasian Fossils: A Students' Manual of Palaeontology
Chapman, Frederick
Paleontology -- Australia
The test of age by rock-structure has a more restricted use, but is of
value when taken in conjunction with the sequence of the strata and the
character of their included fossils.
To explain both the valuable and the uncertain elements of this last
method as a determinant of age, we may cite, for instance, the Upper
Ordovician slates of Victoria and New South Wales as an example of uniform
rock formation; whilst the yellow mudstones and the grey limestones of
the Upper Silurian (Yeringian series) of the same states, are instances
of diverse lithological structures in strata of similar age. A reference
in the latter case to the assemblages of fossils found therein, speedily
settles the question.
(3). Hence, the structure and composition of the rocks (lithology), gives
only partial evidence in regard to age.
=Strata Vertically Arranged.--=
The Stratigraphical Series of fossiliferous sediments comprises bedded
rocks from all parts of the world, which geologists arrange in a vertical
column according to age.
A general computation of such a column for the fossiliferous rocks of
Europe gives a thickness of about 14 miles. This is equivalent to a mass
of strata lying edgewise from Melbourne to Ringwood. The Australian
sediments form a much thicker pile of rocks, for they can hardly fall
short of 37 miles, or nearly the distance from Melbourne to Healesville.
This vertical column of strata was formed during three great eras of time.
The oldest is called the Primary or Palaeozoic ("ancient life"), in which
the animals and plants are of primitive types. This is followed by the
Secondary or Mesozoic ("middle life"), in which the animals and plants are
intermediate in character between the Palaeozoic and the later, Cainozoic.
The third era is the Tertiary or Cainozoic ("recent life"), in which the
animals and plants are most nearly allied to living forms. These great
periods are further subdivided into epochs, as the Silurian epoch; and
these again into stages, as the Yeringian stage.
Vertical Column of Fossiliferous Strata, Australia.
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