The mighty deep : $b and what we know of itGiberne, Agnes
Science
The mighty deep : $b and what we know of it
Giberne, Agnes
Marine biology; Nature study
Immense supplies have been thus dredged and hauled up from the
bottom of the sea. Muds and oozes, sands and pebbles, stones and
rocks, shelly deposits, volcanic deposits, remains innumerable of
dead plants, remains still more abundant of animals, including
earbones of whales and teeth of sharks, and more rarely other parts
of animal-skeletons--large, small, microscopic, these all have been,
with infinite care, with infinite patience, sorted and examined and
classified.
Teeth and earbones! But where are the great shark-skeletons? Where are
the mighty bone frameworks of whales?
If a whale’s earbones lie here, surely here also must have sunk
the enormous carcase. Yet all the rest has vanished. All has been
dissolved--disintegrated--eaten up, as it were, by the black and silent
waste of water. Sea-water has an extraordinary dissolving power, much
intensified by added pressure at great depths, and few substances can
long withstand that power. Not even the massive skeletons of sharks
and whales, with the exception of the teeth and earbones, which are
formed of peculiarly hard material.
And never once, throughout the whole cruise, was any single bone of Man
brought up from the ocean-bed.
After all is this surprising? Where even whale-skeletons are mastered,
small chance can remain for a human skeleton to stand out long against
absorption.
The marvel is how tiny foraminifer shells can last as they do. The
majority no doubt disappear. Unless they reach the bottom quickly, and
are there covered up and protected, they must soon be dissolved.
Yet that vast numbers do thus escape we know by the masses of ooze
found over the sea-bottom; by the fifty millions or more of square
miles of the ocean-floor carpeted with coral muds and sands, and with
oozes of foraminifera and kindred shells.
Only down to a depth of about two miles. Beyond that, carbonate-of-lime
shells are seldom found. It is believed that these light shells take
as much as three or four days to sink one mile; and in about two miles
they all succumb to the power of sea-water. But the hard little diatom
cases are present in all depths, more especially in Earth’s colder
regions, where they abound most freely.
The ocean-bed has been described as one huge sepulchre, full of the
remains of once-living creatures. And this is true; yet by itself it
gives a very one-sided view. Not less is the ocean-bed to be described
as a world of abounding Life.
Everywhere, throughout the whole sea, in all parts, above and below
and between--near the surface, on the floor, in all intermediate
reaches--living creatures flourish in numbers past imagination.
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Elsewhere in the archive
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account