Desert and water gardens of the Red Sea : $b Being an account of the natives and the shore formations of the coastCrossland, Cyril
Science
Desert and water gardens of the Red Sea : $b Being an account of the natives and the shore formations of the coast
Crossland, Cyril
Coral reefs and islands; Red Sea; Sudan -- Social life and customs
It is obvious that colonies cannot live for ever, any more than do
individuals, and we need to know the fate of a dead colony and how
it is replaced by a living one which shall continue the building. So
great is the competition among the crowds of the floating young of
the fixed animals that any vacant spot is at once appropriated. When
a coral colony dies the coloured film of flesh speedily rots away
and the snow-white stony skeleton remains, washed clean by waves and
currents[46]. In a few days this is covered with a film of the finest
green seaweed, invisible among which are the embryos of several
orders of animals, e.g. shell-fish, or, there may be the larvae
of some other coral. There is a tense struggle for survival among
these young creatures, but on a growing reef conditions of course
generally favour the coral’s young (otherwise the reef would cease
to grow), some of which grow at the expense of nearly everything else
and cover the site. Many of the large hemispherical corals live on
the reef like loose stones, but on turning them over one may find
quite a small shell, or coral branch, attached to the centre of the
underside. This is the foundation of the whole, the resting place of
the tiny floating larva, the growth of which first covered the stone
on which it settled by a vigorous colony which when large enough
to be independent of support continued its growth until the mass
exceeded by hundreds of times the bulk of the original foundation.
The more delicate of coral skeletons, such as those of the porous
branched madrepores, rarely survive the death of the polyps that
formed them. On losing its coat of living flesh the coral is exposed
to the action of boring animals, as well as to the direct solvent
action of the sea-water, and many are thus destroyed. Partly they
go back into solution, but the greater portion is broken down to
mud and sand. In shallow water branched colonies are broken up into
pebbles and coarse sand by the waves, and these materials serve to
fill in the spaces between the larger colonies and pack the whole
together into a solid mass.
Public-domain text, read in full here on John Shaqi.
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