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
"1. That the whole mass of sarcode throughout the organism was
continuous; the apparently detached secondary chambers being, as
I had previously suspected, connected with the larger chambers by
canals filled with sarcode.
"2. That some of the irregular portions without lamination are not
fragmentary, but due to the acervuline growth of the animal; and that
this irregularity has been produced in part by the formation of
projecting patches of supplementary skeleton, penetrated by beautiful
systems of tubuli. These groups of tubuli are in some places very
regular, and have in their axes cylinders of compact calcareous
matter. Some parts of the specimens present arrangements of this kind
as symmetrical as in any modern Foraminiferal shell.
"3. That all except the very thinnest portions of the walls of
the chambers present traces, more or less distinct, of a tubular
structure.
"4. These facts place in more strong contrast the structure of
the regularly laminated species from Burgess, which do not show
tubuli, and that of the Grenville specimens, less regularly
laminated and tubulous throughout. I hesitated however to regard
these two as distinct species, in consequence of the intermediate
characters presented by specimens from the Calumet, which are
regularly laminated like those of Burgess, and tubulous like those
of Grenville. It is possible that in the Burgess specimens, tubuli,
originally present, have been obliterated, and in organisms of this
grade, more or less altered by the processes of fossilisation, large
series of specimens should be compared before attempting to establish
specific distinctions."
(B.) Original Description of the Specimens added by Dr. Carpenter to
the above--in a Letter to Sir W. E. Logan.
[_Journal of Geological Society_, February, 1865.]
Public-domain text, read in full here on John Shaqi.
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