Life's Dawn on Earth: Being the history of the oldest known fossil remains, and their relations to geological time and to the development of the animal kingdomDawson, John William, Sir
History
Life's Dawn on Earth: Being the history of the oldest known fossil remains, and their relations to geological time and to the development of the animal kingdom
Dawson, John William, Sir
Life -- Origin; Paleontology -- Precambrian
In the Silurian and Devonian ages, these Stromatoporæ evidently carried
out the same function as the Eozoon in the Laurentian. Winchell tells
us that in Michigan and Ohio single specimens can be found several feet
in diameter, and that they constitute the mass of considerable beds of
limestone. I have myself seen in Canada specimens a foot in diameter,
with a great number of laminæ. Lindberg[AK] has given a most vivid
account of their occurrence in the Isle of Gothland. He says that they
form beds of large irregular discs and balls, attaining a thickness of
five Swedish feet, and traceable for miles along the coast, and the
individual balls are sometimes a yard in diameter. In some of them the
structure is beautifully preserved. In others, or in parts of them,
it is reduced to a mass of crystalline limestone. This species is of
the Cœnostroma type, and is regarded by Lindberg as a coral, though
he admits its low type and resemblance to Protozoa. Its continuous
calcareous skeleton he rightly regards as fatal to its claim to be a
true sponge. Such a fossil, differing as it does in minute points of
structure from Eozoon, is nevertheless probably allied to it in no very
distant way, and a successor to its limestone-making function. Those
which most nearly approach to Foraminifera are those with thick and
solid calcareous laminæ, and with a radiating canal system; and one
of the most Eozoon-like I have seen, is a specimen of the undescribed
species already mentioned from the Guelph (Upper Silurian) limestone
of Ontario, collected by Mr. Weston, and now in the Museum of the
Geological Survey. I have attempted to represent its structures in fig.
44.
[Footnote AK: _Transactions of Swedish Academy_, 1870.]
[Illustration: Fig. 46. _Receptaculites, restored._ (_After Billings._)
(_a._) Aperture. (_b._) Inner wall. (_c._) Outer wall. (_n._) Nucleus,
or primary chamber. (_v._) Internal cavity.]
[Illustration: Fig. 47. _Diagram of Wall and Tubes of Receptaculites._
(_After Billings._)
(_b._) Inner wall. (_c._) Outer wall. (_d._) Section of plates. (_e._)
Pore of inner wall. (_f._) Canal of inner wall. (_g._) Radial stolon.
(_h._) Cyclical stolon. (_k._) Suture of plates of outer wall.]
[Illustration: Fig. 48. _Receptaculites, Inner Surface of Outer Wall
with the Stolons remaining on its Surface._ (_After Billings._)]
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.
Elsewhere in the archive
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account