The Sea and Its Living Wonders: A Popular Account of the Marvels of the Deep and of the Progress of Martime Discovery from the Earliest Ages to the Present TimeHartwig, G. (Georg)
History
The Sea and Its Living Wonders: A Popular Account of the Marvels of the Deep and of the Progress of Martime Discovery from the Earliest Ages to the Present Time
Hartwig, G. (Georg)
Animal behavior; Discoveries in geography; Discoveries in geography -- History; Marine animals; Marine plants; Ocean
The dry land develops the most exuberant vegetation on the lowest
grounds, the plains and deep valleys, and the size and multiplicity of
plants gradually diminish as we ascend the higher mountain regions, until
at last merely naked or snow-covered rocks raise their barren pinnacles
to the skies: but the contrary takes place in the realms of ocean; for
here the greater depths are completely denuded of vegetation, and it
is only within 600 or 800 feet from the surface that the calcareous
nullipores begin to cover the sea-bottom, as mosses and lichens clothe
the lofty mountain-tops. Gradually corallines and a few algæ associate
with them, until finally about 80 or 100 feet from the surface begins the
rich vegetable zone which encircles the margin of the sea. The plants
of which it is composed do not indeed attain the same high degree of
development as those of the dry land, being deprived of the beauties of
flower and fruit: but as the earth at different heights and latitudes
constantly changes her verdant robe, and raises our highest admiration
by the endless diversity of her ornaments, thus also the forms of the
sea-plants change, whether we descend from the brink of ocean to a
greater depth, or wander along the coast from one sea to another; and
their delicate fronds are as remarkable for beauty of colour and elegance
of outline, as the leaves of terrestrial vegetation.
The difference of the mediums in which land- and sea-plants exist
naturally requires a different mode of nourishment, the former
principally using their roots to extract from a varying soil the
substances necessary for their perfect growth, while the latter absorb
nourishment through their entire surface from the surrounding waters, and
use their roots chiefly as holdfasts.
The constituent parts of the soil are of the greatest importance to
land-plants, to whose organisation they are made to contribute; while to
the sea-plant it is generally indifferent whether the ground to which it
is attached be granite, chalk, slate, or sandstone, provided only its
roots find a safe anchorage against the unruly waters.
Flat rocky coasts, not too much exposed to the swell of the waves, and
interspersed with deep pools in which the water is constantly retained,
are thus the favourite abode of most algæ, while a loose sandy sea-bottom
is generally as poor in vegetation as the Arabian desert.
Public-domain text, read in full here on John Shaqi.
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