Geology: The Science of the Earth's Crust — John Stuart Mill — John Shaqi
Geology: The Science of the Earth's Crust
John Stuart Mill · en
In fact this simple type, almost exactly like its early Paleozoic
ancestor, has been the only one out of this whole remarkable class of
animals to persist to the present time, being now barely represented by
the well-known pearly nautilus of the Indian Ocean.
During the Mesozoic era the highest type of cephalopod, represented by
modern squids and so-called "cuttlefishes," branched off and developed
in great profusion. These had slender internal shells, but no external
chambered shells. An inky black liquid secreted in a bag was forced
out to cloud the water when the animal was escaping its enemy, thus
antedating by millions of years the principle of smoke screen so
effectively used by ships during the World War. Some Jurassic species
got to be over two feet long, and a few specimens of that age have
been found in such perfect state of preservation that drawings of the
fossils have actually been made with the ink (after moistening) taken
from their own ink bags.
[Illustration: Fig. 54.--A fossil nonchambered cephalopod of Jurassic
age. It was closely related to the modern squid, and its ink bag is
well shown just to the left of the middle. (Modified after Mantell.)]
Before concluding this chapter we shall take up the salient points
in the geological history of Arthropods which constitute the highest
subkingdom of all animals except the Vertebrates. They are now very
abundant and varied, familiar examples being crabs and insects. A few
scant remains of simpler forms are known from the Proterozoic, but
since very early Paleozoic time they have been very common and have
undergone great evolutionary changes. A few striking examples only will
be dwelt upon. Among the most common and interesting of all Paleozoic
animals were the trilobites, distantly related to modern lobsters and
crabs.
[Illustration: Fig. 55.--Restorations of trilobites based upon actual
fossils characteristic of earlier Paleozoic time: a, Cambrian; b,
Ordovician; c, Devonian; b shows the appendages.]