The lowest stratum of the Cambrian formations has been regarded as the most ancient of the Palæozoic rocks; now, however, strata of crystallized limestone near the base of the Laurentian system, which is 50,000 feet thick in Canada, are discovered by Sir W. E. Logan to have been the work of the Eozoön Canadense, a gigantic Foraminifer, at a period so inconceivably remote that it may be regarded as the first appearance of animal life upon the earth. In a paper published by Dr. Carpenter, in May 1865, he expressed his opinion that the Eozoön would be found in the older rocks of central Europe; and in the December following he received specimens from the fundamental quartz rocks of Germany, in which he found undoubted traces of the Eozoön. Here the superincumbent strata are 90,000 feet thick; the transcendent antiquity of the Eozoön is therefore beyond all estimation. The fossil Eozoön consists of a succession of parallel rows or tiers of chambers, in which the sarcode of the living animal had been replaced by a siliceous infiltration, so that when the calcareous shell was destroyed by dilute acid, the cast was found to be precisely like that of a Nummulite; thin slices of it taken in different directions being examined with a microscope, it was found that the siliceous matter had not only filled that portion of the chambers which had been occupied by the sarcode-body of the animal and the canal-system, but had actually taken the place of the pseudopodial threads, the softest and most transitory of living substances, which were put forth through tubuli in the shell-walls of less than the 1/10000 part of an inch in diameter. ‘These are the very threads themselves turned into stone by the substitution which took place, particle by particle, between the sarcode body of the animal and certain constituents of the water of the ocean, before the destruction of the sarcode by ordinary decomposition.’[9] The shell had an intermediate skeleton, but the minute tubes in the walls of the chambers are so characteristic of the Nummulites, that they were sufficient alone to determine the relationship of the Eozoön to its modern representative.