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
A further stage of mineralization occurs when the substance of the
organism is altogether removed and replaced by foreign matter, either
little by little, or by being entirely dissolved or decomposed,
leaving a cavity to be filled by infiltration. In this state are some
silicified woods, and those corals which have been not filled with but
converted into silica, and can thus sometimes be obtained entire and
perfect by the solution in an acid of the containing limestone, or by
its removal in weathering. In this state are the beautiful silicified
corals obtained from the corniferous limestone of Lake Erie. It may be
well to present to the eye these different stages of fossilization. I
have attempted to do this in fig. 22, taking a tabulate coral of the
genus Favosites for an example, and supposing the materials employed to
be calcite and silica. Precisely the same illustration would apply to a
piece of wood, except that the cell-wall would be carbonaceous matter
instead of carbonate of lime. In this figure the dotted parts represent
carbonate of lime, the diagonally shaded parts silica or a silicate.
Thus we have, in the natural state, the walls of carbonate of lime
and the cavities empty. When fossilized the cavities may be merely
filled with carbonate of lime, or they may be filled with silica; or
the walls themselves may be replaced by silica and the cavities may
remain filled with carbonate of lime; or both the walls and cavities
may be represented by or filled with silica or silicates. The ordinary
specimens of Eozoon are in the third of these stages, though some exist
in the second, and I have reason to believe that some have reached to
the fifth. I have not met with any in the fourth stage, though this is
not uncommon in Silurian and Devonian fossils.
[Illustration: Fig. 22. _Diagram showing different States of
Fossilization of a Cell of a Tabulate Coral._
(_a._) Natural condition--walls calcite, cell empty. (_b._) Walls
calcite, cell filled with the same. (_c._) Walls calcite, cell filled
with silica or silicate. (_d._) Walls silicified, cell filled with
calcite. (_e._) Walls silicified, cell filled with silica or silicate.]
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