In doing that two operations are requisite. The first is to ascertain the depth: when that is known, the nature of the sea-bed must be determined, and on that account a sample of it is then sounded for; but owing to the difficulty of ascertaining the exact time at which the ground is struck, a quantity of rope in excess of the depth is given out, which lies on the bottom of the sea while the machine is being drawn up, which occupies a considerable time when the depth is great. About midway between Greenland and the north of Ireland, when the machine was hauled up from a depth of a mile and a half, several starfish were clinging with their long spiny arms to fifty fathoms of the rope that had been lying on the surface of the sea-bed while the machine was being drawn up, and to that part of the rope alone. They continued to move their limbs energetically for more than a quarter of an hour after they were out of the water. They certainly had not been entangled in the line while swimming, because star-fishes are invariably creeping animals. The deposit on which they had rested at the bottom of the ocean contained ninety-five per cent. of Globigerinæ. Abundance of these minute Foraminifera were found in the stomachs of the starfish; which seemed to prove not only that the starfish were caught on their natural feeding ground, but that their food was living organisms whose normal abode is the surface of the bed of the deep ocean.
Dr. Wallich also discovered in the ooze brought up from a depth of nearly two miles and a quarter a number of small bodies from 1⁄16 to 1⁄4 of an inch in length and about a line in breadth. They consisted of equal globes arranged in a straight line like the Nodosaria, or built up, each lying on part of the one below it, and increasing in size from the uppermost about 1⁄1250 to the undermost about 1⁄450 of an inch in diameter. Both of these forms, called coccospheres, consisted of sarcode enclosed in a calcareous deposit; and were studded at nearly regular distances by minute round or oval bodies concave below, and with an aperture on their convex surface sometimes single, sometimes double. These coccospheres were also found free in the ooze, and had been seen previously by Capt. Dayman. They have likewise been seen as free organisms living on the surface of the ocean.
The ooze in the bed of the Atlantic ocean, as well as of the Mediterranean and Adriatic contains fifty per cent. of Globigerinæ; they exist in the Red Sea, in the vicinity of the West Indian Islands, on both sides of South America and near the Isle of France, but not in the Coral Sea which is occupied by different genera. Though in utter darkness, at the bottom of a deep ocean, these little creatures can procure food by means of their pseudopodia, whose extreme sensibility makes up for the want of sight; and the very excess of pressure under which they live insures them a supply of oxygen at depths to which free air cannot penetrate, for it is believed that the quantity of dissolved air that water contains is in proportion to the pressure.
Fossil Foraminifera enter so abundantly into the sedimentary strata, that Buffon declared ‘the very dust had been alive.’ 58,000 of these fossil shells have been computed in a cubic inch of the stone of which Paris and Lyons are built. The remains of these Rhizopods are for the most part microscopic. M. D’Orbigny estimated that an ounce of sand from the Antilles contained 1,800,000 shells of Foraminifera. A handful of sand anywhere, dry sea-weeds, the dust shaken from a dry sponge, are full of them.
When the finer portions of chalk amounting to one half or less are washed away, the remaining sediment consists almost entirely of the shells of Foraminifera, some perfect, others in various stages of disintegration. In some of the hard limestones and marbles, the relics of Foraminifera can be detected in polished sections and in thin slices laid on glass. It is now universally admitted that some crystallized limestones which are destitute of fossil remains, had been originally formed by the agency of animal life, and subsequently altered by metamorphic action; the opinion is gradually gaining ground among geologists that such is the history of the oldest limestones.
At certain geological periods circumstances favoured the development of an enormous multitude of individual animals. In the earlier part of the Tertiary period the Nummulites acquired an extraordinary size. They were like very large coins two or more inches in diameter, and were accumulated in such quantities as to constitute the chief part of the nummulitic limestone; a formation in some places 1,500 feet thick, which extends through southern Europe, Libya, Egypt, Asia Minor, and is continued through the Himalayan mountains into various parts of the Indian peninsula, where it is extensively distributed. The Great Pyramid of Egypt is built of this limestone, which gave rise to singular speculations with regard to the Nummulites in very ancient and even in more recent times. Although this is incomparably the greatest, it is by no means the only instance of an accumulation of the fossil shells of individual animals. The ‘Lingula flags,’ a stratum in the upper Cambrian series of North Wales, was so named from the abundance of the Brachiopod Lingula that it contains.
Professor Ehrenberg discovered that the shells of the Foraminifera sometimes undergo an infiltration of silicate of iron, which fills not only the chambers, but also their canal-system even to its minutest ramifications, so that if the shell be destroyed by dilute acid, a perfect cast of the sarcode matter remains. The greensands in the different geological strata from the Silurian formation upwards, are chiefly composed of these casts; and Professor Baily of the United States more recently discovered that a process of infiltration is even now taking place in some parts of the ocean bed, and that beautiful casts of Foraminifera may be obtained by dissolving their shells with dilute acid.
A most extensive comparison of the Foraminiferous group of Rhizopods, recent and fossil, has been made by Messrs. Parker and Rupert Jones from almost every latitude on the globe, from the arctic and tropical seas, from the temperate zones in both hemispheres, and from shallow as well as deep-sea beds. They have also reviewed the fossil Foraminifera in their manifold aspects as presented by the ancient geological faunas throughout the whole series from the Tertiary down to the Carboniferous strata inclusive; and have come to the astonishing conclusion that scarcely any of the species of the Foraminifera met with in the secondary rocks have become extinct. All that they had seen have their counterparts in the recent Mediterranean deposits. Throughout that long series of geological epochs even to the present day, the Foraminifera show no tendency to rise to a higher type; but variety of form in the same species prevailed then as it does now.
Subsequently to this investigation, a gigantic Orbitulite twelve inches in diameter, and the third of an inch thick, has been found in the Silurian strata in Canada. The largest recent species Dr. Carpenter had seen was about the size and thickness of a shilling.
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.