The Botanic Garden, a Poem in Two Parts. Part 1: the Economy of VegetationDarwin, Erasmus
History
The Botanic Garden, a Poem in Two Parts. Part 1: the Economy of Vegetation
Darwin, Erasmus
Natural history; Plants -- Poetry; Portland Vase
These strata consist of the accumulated exuviae of shell-fish, the
animals perished age after age but their shells remained, and in
progression of time produced the amazing quantities of lime-stone which
almost cover the earth. Other marine animals called coralloids raised
walls and even mountains by the congeries of their calcareous
habitations, these perpendicular corralline rocks make some parts of the
Southern Ocean highly dangerous, as appears in the journals of Capt.
Cook. From contemplating the immense strata of lime-stone, both in
respect to their extent and thickness, formed from these shells of
animals, philosophers have been led to conclude that much of the water
of the sea has been converted into calcareous earth by passing through
their organs of digestion. The formation of calcareous earth seems more
particularly to be an animal process as the formation of clay belongs to
the vegetable economy; thus the shells of crabs and other testaceous
fish are annually reproduced from the mucous membrane beneath them; the
shells of eggs are first a mucous membrane, and the calculi of the
kidneys and those found in all other parts of our system which sometimes
contain calcareous earth, seem to originate from inflamed membranes; the
bones themselves consist of calcareous earth united with the phosphoric
or animal acid, which may be separated by dissolving the ashes of
calcined bones in the nitrous acid; the various secretions of animals,
as their saliva and urine, abound likewise with calcareous earth, as
appears by the incrustations about the teeth and the sediments of urine.
It is probable that animal mucus is a previous process towards the
formation of calcareous earth; and that all the calcareous earth in the
world which is seen in lime-stones, marbles, spars, alabasters, marls,
(which make up the greatest part of the earth's crust, as far as it has
yet been penetrated,) have been formed originally by animal and
vegetable bodies from the mass of water, and that by these means the
solid part of the terraqueous globe has perpetually been in an
increasing state and the water perpetually in a decreasing one.
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