with at least 250 species, are vermiform animals
which have calcareous spicules, scales, or plates em-
bedded in the mantle and which are separable into
two principal groups, sometimes considered as inde-
pendent classes. The more or less cylindrical, gono-
choristic Caudofoveata (Figure 1a), having the body
somewhat separated into anterior, medial, and pos-
terior sections and possessing an anteroventral pedal
shield, attain lengths of 140 mm and live mostly as
infaunal burrowers. Fewer than 100 species are
known, and they feed mainly on microorganisms
and detritus. The free-living, more or less uniformly
worm-like, elongate and laterally compressed Soleno-
gastres (Figure 1b, c), with over 200 recognized
species, are 1–300 mm in length. Hermaphroditic
and predacious, they have a distinct pedal groove,
posterior gill folds and live either epibiotically on
sediments or epizoically on cnidarians, which usually
constitute their principal food.
000 7 The Monoplacophora (Figure 1d, e), with fewer
than 20 living species, have a controversial fossil
history dating from the Early Cambrian; they are
benthic, mainly deep-sea animals having a single
cap-shaped or limpet-like shell and variously paired
organ systems such as the pedal retractor muscles,
gills or ctenidia, nephridia or kidneys and gonads,
reflecting a primitive metamerism. In monoplaco-
phorans, the foot is large with a flattened, creeping
sole, and the pallial mantle cavity is peripheral along
the sides of the animal.
0008 The chitons or so-called coat-of-mail shells, separ-
ated as the class Polyplacophora (Figure 1f, g), also
have a broadened, flat muscular foot and a mantle
cavity containing numerous pairs of ctenidia. Con-
sisting of about 600 species of marine benthic epi-
faunal animals with dorsoventrally depressed bodies,
they are unique in having eight calcareous shell plates
held together by a strong, peripheral girdle. The body
outline is elongate to ovate, and adult individuals
range in size from 3 to almost 400 mm in length.
Although some chitons are known to occur at depths
beyond 7000 m, most live in shallower waters and are
mainly grazing herbivores, with a radula having 17
teeth in transverse rows and cusps reinforced with
magnetite. The anterior portions of the alimentary
canal have pairs of glands for the digestion of carbo-
hydrates, and the broad, large foot is used to creep
over, or to attach by suction to, the substrate. Special
photosensory structures, the esthetes, are found on the
dorsal surface of the valves and may, along with the
iron-containing radula, facilitate homing behavior.
000 9 The Gastropoda or snails (Figure 2a–c), the largest
and most diverse class with as many as 40 000
species, have representatives in most of the world’s
biotopes and are known from the Early Cambrian.
Although most species live in the marine environ-
ment, many kinds occur both on land and in fresh
water; a few taxa have become specialized internal
parasites. Principally, gastropods are univalves,
usually with a coiled, apically closed calcareous
shell, which also exhibits a great many different shapes
and forms, being sometimes merely cap-shaped,
greatly reduced, or even altogether lost. The very
largest of living snails has a shell over 500 mm in
length, the smallest less than 1 mm.
0010Anatomically, snails and their relatives are basic-
ally divisible into head, foot, and visceral mass; they
are all characterized by a unique process called tor-
sion which occurs during ontogeny. Primitively, the
mantle cavity, into which the alimentary canal, excre-
tory structures, and gonads of the visceral mass
empty, contains a pair of laterally disposed respira-
tory ctenidia or gills and is located posteriorly in the
early larval gastropod (Figure 2a). During develop-
ment, the entire mantle cavity and its contents are
twisted or torted through an arc of 180
to the right,
bringing the cavity itself into an anterior position
above and behind the neck and head of the snail
(Figure 2b). Internally, torsion causes a peculiar cross-
ing (or streptoneury) of the laterally disposed, paired
nervous connections between the anteriorly placed
cerebral ganglia and the posteriorly located visceral
ganglia.
0011The head of a gastropod usually has at least one
pair of cephalic tentacles, and eyes are often associ-
ated with them; however, both structures can be lost.
The foot has a creeping sole, and primitively, there are
lateral grooves between it and the mantle, forming a
so-called epipodium with sensory tentaculate and
integumentary organs. The sole of the foot may be
subdivided and variously modified for swimming
and, in the case of internal parasites, it is entirely
lost. The distinctive visceral mass, a dorsal hump, is
covered by the mantle which secretes the shell, and
contains the internal organs or viscera, including the
heart, kidneys, gonads, and alimentary canal. Gener-
ally speaking, the jaws and radula assist the mouth in
bringing food into the digestive tract; one or more
pairs of salivary glands or specialized pouches may
contribute enzymes to the buccal cavity or esophagus;
the stomach leads through the intestine to the
terminal anus and may have a crystalline style, style
pouch, typhlosole, digestive diverticula, and a tritur-
ating gizzard associated with it. All these structures –
the head, foot, visceral mass, mantle and shell – are
different and variously altered in the major sub-
divisions of the Gastropoda.
0012Traditionally, the snails are subdivided into three
major subclasses: the Prosobranchia, Opisthobran-
chia, and Pulmonata. Recently, with the advent of
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