The flints, _figs. 3, 7, 8, 9, Lign. 25_, were evidently formed

in the manner exemplified in _fig. 3, Lign. 26_; _figs._ 2, 4, 6,

are illustrated by _fig. 4, Lign. 26_; for the chalk specimens,

_Lign. 26_, shew that all these flints have been moulded around

_Ventriculites_, and that their diversity of figure has arisen from

the quantity of silex that happened to permeate the substance of the

zoophyte; if but a small portion, flint like _figs._ 2 and 4, were

the result; if the quantity were considerable, the larger fungiform

examples were produced.

Note IX. Page 50. _Minute Corals from Chalk._

Some layers of chalk are composed of an aggregation of many kinds of

delicate corals, the interstices being filled up with _Rotaliæ_ and

other foraminiferous shells. In the cliffs near Dover there are several

beds of this nature, well known to collectors for the profusion of

exquisite specimens they yield to the experienced investigator. _Lign.

17_, p. 50, represents several varieties from different localities;

the small figures shew the natural size, and the enlarged ones their

appearance when magnified. Attached to the surface of shells, and

sometimes standing erect in crannies of flint nodules, beautiful corals

may often be detected by the aid of a lens of moderate power. By

brushing chalk in water, and examining the deposit, delicate fossils of

this kind may also be obtained.[AR]

[AR] Refer to '_Medals of Creation_,' p. 284, and to '_Wonders of

Geology_,' _Lecture VI._ p. 588, for a comprehensive view of Recent and

Fossil Corals.

[Sidenote: NATURE OF CORALS.]

From the close analogy of the fossil corals to existing forms, it would

not be difficult to give restored figures of the originals. Every

little branch might be represented fraught with living polypes: in some

cells the agile inmates might be shown with the mouth expanded, and

the tentacula in rapid motion; in others withdrawn into their stony

recesses, and devouring the infinitesimal atoms that constitute their

food: even their varied hues might be introduced, and thus a vivid

picture be presented of the microscopic beings which peopled the waters

of the ancient chalk ocean.

That the Corals, which from their elegance and beauty are preserved in

almost every cabinet, have been fabricated--or, in other words, built

up--by polypes, in the same manner as the honey-comb of the bee and

wasp, is so prevalent yet erroneous an opinion, that I am induced to

point out its fallacy, by giving a brief account of the formation of

these substances. The three recent specimens represented in _Lign. 27_

will serve to illustrate my remarks.

[Illustration: Lign. 27:--Recent Corals.

1. _Oculina ramea._

2. _Madrepora muricata._

3. _Isis hippuris._

]

The coral, _fig. 1_, was an internal axis or skeleton, deposited by the

soft fleshy integument with which, when living, it was wholly invested;

in the same manner as are the bones of animals, by the special membrane

(_periosteum_) that secretes them. This integument lined every cell,

and the polypes were permanently united to it. When the live coral is

taken out of the water, the animalcules shrink up and quickly perish;

their soft parts and the external investing substance putrefy, and the

stony axis beset with the radiated cells alone remains.

[Sidenote: RECENT CORALS.]

In the example of _Oculina ramea_, or May-blossom Coral, _fig. 1_, from

the Mediterranean, the cells are large and distinct; in the _Madrepore_

from the West Indies, _fig. 2_, they are small and very closely

aggregated.

The specimen of _Isis_ (_fig. 3_) belongs to a group of coral-zoophytes

in which the polype-cells consist of a substance that is durable, but

not so hard as coral, and invests an axis composed of a tough flexible

material, which is exposed at the base of _fig 3_, by the removal of

the external or cortical part in which the polypes were situated. The

_Gorgonia_, or Venus's fan, has a similar structure and composition.[AS]

[AS] See '_Wonders of Geology_,' vol. ii. p. 616.

In the _Red Coral_, so largely employed in the manufacture of beads,

brooches, and other ornaments, not only the animalcules, but also

their receptacles, are composed of a soft perishable substance. When

alive, the polypes, as well as the investing fleshy integument, are of

a delicate bluish tint; the internal calcareous axis alone possesses

the peculiar red colour. Upon being taken out of the sea, vitality

quickly ceases, the soft parts decompose, and the beautiful crimson

stone commonly known as the _true coral_, is obtained free from all

traces of the soft mass by which it was secreted. Although an actual

investigation of the facts described can only be instituted near the

seas of warm climates, yet our coasts abound in certain coral-zoophytes

in which similar phenomena may readily be observed. Most persons in

their rambles by the sea-side must have noticed on the fuci, algæ,

shells, pebbles, &c., patches of a white earthy substance, which

when closely examined resemble delicate lace-work. These apparently

calcareous incrustations are clusters of the zoophytes termed

the _Flustra_, or sea-mat.[AT] When removed from the water, this

aggregation of polypes seems coated over with a glossy film or varnish;

and with a lens of moderate power the surface is seen to be full of

pores, disposed with much regularity. If viewed under the microscope

while immersed in sea-water, a very different appearance is presented.

Every pore is found to be the opening of a cell whence issues a tube

fringed with several long feelers or arms; these expand, then suddenly

contract and withdraw into the cell, and again issue forth; the whole

surface of the Flustra being covered with these hydra-like animalcules.

The Flustra, therefore, like the corals, constitutes an assemblage of

polypes, each individual being permanently fixed in a durable cell,

and the whole attached to a common integument by which the calcareous

frame-work was secreted and maintained.[AU]

[AT] See '_Wonders of Geology_,' Plate 5.

[AU] See Dr. Johnson's beautiful work on '_British Zoophytes_,' in

which are numerous figures of various species of Flustra.

Note X. Page 53. _Infusorial earth from Richmond in Virginia._

[Sidenote: INFUSORIAL EARTHS.]

The greatest natural operations are produced by the most simple

and apparently inadequate agents: for as the illustrious Galileo

emphatically remarked, "_La nature fait beaucoup avec peu, et ses

opérations sont toutes également merveilleuses._" The profound thinker

Hobbes, in the same spirit observes, "The majesty of God appeareth no

less in small things than in great, and as it exceedeth human sense in

the immensity of the universe, so also doth it in the smallness of the

parts thereof." This sublime truth is strongly impressed on the mind

of the geological inquirer, who perceives that whole countries and

mountain ranges of great elevation and extent, are wholly composed of

the aggregated remains of beings of such infinite minuteness that but

for the powerful optical instruments of modern times, their presence

would never have been suspected.

A few years only have elapsed since the sagacious Ehrenberg first

drew attention to this subject, and pointed out the proper method of

investigation;[AV] and so rapid has been the progress of discovery in

this department of science, that _infusorial deposits_, as these beds

of fossil animalcules are designated, have been detected in every

quarter of the globe. A fact equally unexpected and remarkable has also

been established, namely, that at the present moment similar minute

living agents are largely contributing to the increase of the solid

materials of the crust of our planet.

[AV] See '_Medals of Creation_,' p. 244, for instructions for the

microscopical examination of earths, chalk, &c.

[Sidenote: RICHMOND EARTH.]

The infusorial earth of Virginia, alluded to in the text, is a

yellowish siliceous clay, forming a deposit from twelve to fifteen

feet in thickness, upon which the towns of Richmond and Petersburgh

are built. The surface of the country over which it extends is

characterized by a scanty vegetation, owing to the siliceous nature of

the soil dependent on the minute organisms of which it almost entirely

consists. When a few grains of this earth are properly prepared for

microscopic examination, immense numbers of the shields or cases of

animalcules are visible under a magnifying power of 300 diameters; in

fact, the merest stain left by the evaporation of water in which some

of the marl has been mixed, teems with these fossil remains.[AW]

[AW] Specimens of Infusorial earths, prepared for the microscope, may

be obtained of Mr. Topping, 4, New Winchester Street, Pentonville Hill,

New Road, London.

These organisms are of exquisite structure, and comprise many

species and genera. The most beautiful and abundant are the circular

shields, termed _Coscinodisci_ (sieve-like disks), which are elegant

saucer-shaped cases, elaborately ornamented with hexagonal apertures

disposed in curves, somewhat resembling the engine-turned sculpturing

of a watch; these shells are from 1/1000 to 1/100 of an inch in

diameter. A segment of one of these disks, highly magnified, is

represented in _Lign. 18, fig. 2_. The body of the living animalcule

was protected and enclosed by a pair of these concave shells, the

perforations admitting of the exsertion of filaments or tentacula.

This species of _Coscinodiscus_ abounds in the present seas, and

constitutes no inconsiderable proportion of the food of Pectens and

other testaceous mollusca.[AX]

[AX] See '_Thoughts on Animalcules_,' p. 103.

All the animalcules found in the Richmond earth are marine, and most

of them belong to genera, and many to existing species; although the

position of the American strata proves that they are referable to a

period of immense antiquity.

In Germany, beds of a white infusorial earth, resembling magnesia

in appearance, and termed _Bergh-mehl_, or fossil farina, occur at

Bilin, and several other places: at San Fiora in Tuscany, near Egra

in Bohemia, in the Bermudas, Barbadoes, &c., similar deposits have

been discovered; all being composed of the shields of various kinds of

animalcules. But I must not extend these remarks, and will only add a

few observations on the infusorial earth of Barbadoes, which has but

recently been brought under the notice of geologists by Sir Robert

Schomburgk, and is especially interesting for the exquisite beauty and

variety of its organisms, and the circumstances under which the deposit

occurs.

[Sidenote: FOSSIL INFUSORIA OF BARBADOES.]

Barbadoes, an island of the West Indies, is about twelve miles in

length from north to south, and consists of coral reefs, capped in one

district by tertiary sandstones and limestones, which attain a height

of 1200 feet above the sea. Over the rest of the island, coral reefs

form the entire surface, which is divided by vertical walls of coral,

some of them nearly 200 feet high, into six terraces, indicating as

many periods of upheaval. In the lowest reef, Indian hatchets have

been found twenty feet above high water mark; shewing that the last

movement, at least, took place within the human period. The tertiary

strata are more or less inclined, and in many places vertical, and

contorted. Strata of marl, several hundred feet thick, predominate; and

there are beds of bituminous coal, sandstone, clays, and ferruginous

sands. Arenaceous limestone containing teeth of sharks, spines of

echini, and shells, forms the summit of a hill nearly 1,000 feet high.

The white marls abound in 300 species of the most beautiful siliceous

infusoria; many are peculiar, others the same as occur in the Richmond

earth, and some belong to recent species.[AY]

[AY] Sir R. H. Schomburgk: Brit. Assoc. 1847.

THE END.

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Thoughts on a Pebble, or, A First Lesson in Geology · 第 3 / 4 段