EES 227: Paleobiology
Spring 2004
return to
syllabus
Lecture 18: April 13
Reading:
- Chapter 15 textbook, pages
272-279
- Johnson, C. J., 2002. The rise and fall
of rudist reefs. American Scientist, Vol. 90, p. 148-153 (abstract
and some figures available
online)
- Vermeij,
G. J., 1999. Inequality and the Directionality of history. The
American Naturalist, vol. 153 (3), p. 243-253
Web resources for this
lecture:
Lecture Notes: Mollusca
Mollusca are a group that strongly
diversfied in the Mesozoic, and have been mentioned as one of the
main groups participating in the Mesozoic Marine
Revolution.
Mesozoic Revolutions:
- On Land: evolution of Angiosperms
(lecture
15)
- External causes: high CO2
levels (??)
- Internal causes: co-evolution
with insects and/or herbivorous dinosaurs
- In the Oceans: rapid evolution of more
active life styles, higher metabolic rates (e.g, snails, starfish.
sharks and rays, modern fish, crabs, marine reptiles)
- External causes: nutrients in sea
water (large igneous provinces; ????)
- Internal causes: arms
races
The Mollusca are the second most diverse phylum of animals (after
Arthropoda), with some 55,000 living and 35,000 fossil species
described. The total diversity is estimated to be much larger, maybe
up to 130,000 species. The most common group are the
Gastropoda (snails, ~40,000 species), followed by Bivalvia (about
13,000 species). Maybe it is because of their great diversity that
their cladistics are not yet clear (see below).
The name Mollusca indicates one of their
distinctive characteristics: a soft body. Molluscs are an incredibly
diverse group, containing forms that do not at all resemble each
other superficially: from intelligent, large-brained, fast-moving
predators with large eyes such as a squid, to non-moving animals
without eyes, a head or a clear brain that live on symbiont algae
such as the giant clam. One can derive all these diverse forms from
some kind of basic type, proto-mollusc, however. Mollusca possess at
least some or all of the following characteristics (see figure 15.3,
text book p. 277 1st edition, 285 2nd
edition):
- a muscular fleshy
foot, which gastropods (snails)
used to crawl, clams to burrow, and which in cephalopods is
modified into tentacles
- a visceral
mass containing the digestive,
excretory, and reproductive organs
- a mantle,
usually two folds that enclose the gills or lungs, and secretes
the shell
- a radula,
a tongue-like organ equipped with rows of microscopic teeth that
scrape food off hard surfaces or grind through shells of other
molluscs
- a respiratory gill
(the ctenidium) or lung
- a shell
made of calcium
carbonate.
Note that the shell is not really a
skeleton; it encloses the soft body (to greater or lesser extent) and
protects it.
I inserted a cladogram for the Mollusca (T. R.
Waller, 1998, Origin of the Molluscan Class Bivalvia and a Phylogeny
of Major Groups; In: An Eon of Evolution; Paleobiological Studies
Honoring Norman D. Newell, edited by P. A. Johnston and J. W.
Haggart, Univ. of Calgary Press, p. 1-45). Note the differences with
the subdivision in Classes as given in your text book.
For all molluscs, studies on functional
morphology have been conducted (see text book p. 108-109;
lecture
11). Different shapes of snail
shells are better at burrowing or sliding over sediment; the shape of
bivalve shells influences how deep and how rapid the animals burrows.
The scars of attachment of muscles and of the mantle in clams shows
whether the animals had one or two muscles, and whether the animal
had a sipho (see below). Similarly, the shape of ammonites (flat,
irregular, ornamented) determines whether the animal was a good
swimmer or crawler.M
ollusca are subdivided into the following
classes. The most common groups are marked in red, lesser groups in
blue.
- Class Aplacophora
(see cladogram), also called Caudofoveata or Chaetodermomorpha or
Solenogastres). Worm-like, no shell, spicules of calcite.
- Class Monoplacophora:
living fossil Neopilina (2 species, known only since the
1950s); fossils long known, early Paleozoic. Limpet-like shells,
internally very different structure
- Class Polyplacophora
(chitons): shell of 8 parts, greatly expanded foot
- Class Scaphopoda
(tosk shells): tusk-shaped, small shell with openings at both
ends
- Class
Gastropoda (snails). The
gastropods are by far the most numerous and diverse: about 40,000
living and 15,000 fossil species. The shell is always one piece,
coiled or uncoiled, and is not subdivided into chambers. In the
oceans, fresh water, and on land. Examples: snails, limpets,
slugs, whelks, sea slugs, abalone. Internally, snails have very
unsual, torqued structure,
- Class
Bivalvia (clams and such).
Bivalved molluscs (13,000 recent species) are mostly sedentary
filter feeders that depend on currents produced by the gills to
bring in food. They have no head and no radula. Deeply-buried
forms have a double tube (the sipho) through which they pump water
in and out the shell; the tube sticks out above the sediment.
Examples: mussels, clams, scallops, oysters, shipworms. Live in
salt, brackish and fresh waters.
- Class
Cephalopoda. The most complex
class of molluscs; all living forms are marine, active predators.
The foot is modified into tentacles and the mantle edge is grown
into a funnel, expelling water from the mantle cavity (jet
propulsion). Recent forms have no shells or an internal shell
(cuttlebone), with the exception of the chambered Nautilus.
Extinct Ammonites also had a spiral, chambered shell. Examples:
squids, octopi, nautiluses, cuttlefish, ammonites.
Many snails are fierce predators (there are
also many herbivores)
- Have grating mechanism mouth: radula;
faster than prey.
- Snails developed more and more
specialized radula to drill holes
- Poisonous snails
- Snails which use their muscular 'foot'
to suffocate prey
- Snails which use spines at front of
shell to hammer into barnacles and clams
- High, narrow snails: fast burrowers,
digging up clams.
Especially Geerat Vermeij argues that snails
are an important factor in the Mesozoic Marine Revolution, and in the
overall Arms Race:
- If predator (snails, crabs) invents more
ways to attack bivalves and other snails, prey invents way to
counter attack (Red Queen hypothesis: see lecture
12)
- Bivalves: develop muscles, spines,
crenulated edges

Mesozoic Revolution of Marine
Invertebrates:
- Many new methods of predation developed,
specifically as to breaking shells open (bivalves): snails,
crabs, lobsters
- Fossil record of more and more predation
upon shell-bearing organisms, and more and more response of prey
species
- Modern ways of living in ocean evolved
during Mesozoic
- No clear linkages between changes in
ways of living and environmental changes
- Competition/arms races
- Increased diversity ('cropping
principle')
If this is true:
- Paleozoic snails would not have a chance
in the present oceans
- Environmental influence on evolution may
be limited because organisms can not 'call up' a wished-for
mutation
- But replacement of major groups (e.g.,
dinosaurs/mammals) may happen only after a major ecosystem
disruption (mass extinction), because incumbents are hard to
dislodge (see lecture
12).