The evolutionary lineage of
our post-protozoan ancestors can be followed through three phyla that left many
existing related groups. The related
groups diversified into forms, most of which are not in our ancestral line.
PORIFERA, THE SPONGES
The first post-protozoan phylum
is the sponges. They are so different
from other animals that many have thought they were an evolutionary dead end or
side-shoot that was not in the mainstream of evolution. The peculiar amphiblastula larva of some
sponges was so different that it seemed to preclude them being in the
mainstream. But Bergquist (1978), in her
book on sponges, illustrates a wide variety of sponge larvae, some of which
have great resemblance to the planula larvae of some cnidarians. The mainstream position of sponges was proposed by Tuzet (1963).
If we do not consider the
sponges as in the mainstream, it would be necessary to postulate a similar organism
as an intermediate form between protozoans and cnidarians. For more on the intermediate nature of
sponges you can find some discussion in the introduction to sponges in the
second (1968) and third (1981) editions of Invertebrate
Zoology which I edited. I later
found research describing spicules in nematocysts of some cnidarians and it
made sense in terms of a spicule, nematocyst, and rhabdite transition found in
sponges, cnidarians, and flatworms.
Spicules
Spicules, both calcareous and
siliceous ones, found in an early fossil anthozoan (Kazmierczak, 1984) show
cnidarians are most likely derived from a sponge most like the Sclerospongea
which also have both types of spicules. The
Calcarea, but not the Hexactinellida or Demospongea, may have had an earlier
ancestral role, but it is just as likely a primitive member of the Sclerospongia
was in that ancestral role.
Hexactinellida have only siliceous spicules, Demospongea have only siliceous
spicules if spicules are present (bath sponges in this group lack spicules).
As sessile (attached)
animals, sponges were dependent for survival on the selection of things that
made them unpalatable to new and mobile predators. A diversity of toxic substances are found in
today’s sponges. Spicules also may deter
predators. Spicules also served as
skeletal elements preventing collapse of the canal systems essential to sponge
growth to larger forms.
Protruding spicules increased
the sponge’s ability to passively deliver adhering toxins. Improvements in partially enclosing the
spicule in a tube of poison allowed selection for increasingly more effective
delivery as the evolution to cnidarians continued. The nematocysts of most cnidarians may have
lost the need for the spicule once the tubular delivery system for poison was
effective.
Nutrition
Sponge nutrition involves
trapping of small food particles by the collar of the flagellated cells lining
some of the chambers of the sponge. The
particles are taken into the cells for digestion. Water transporting the food particles passes
in through small openings (the ostia) on the surface and passes through the
chambers with the flagellated cells before exiting through a larger chamber and
a large opening, (the osculum). Sponges
may have symbiotic, photosynthetic microorganisms in their tissues. These were especially important for nutrition
during the early evolution into cnidarians before the capacity for feeding on
larger living organisms developed.
Other features
As indicted in a previous
post, sponge tissue structure is much like loose connective tissue of
vertebrates. Rudimentary muscular and
nervous cellular structure has been observed.
Sexual reproduction is present and eggs produce ciliated or flagellated
larvae. Asexual reproduction occurs in
several ways. Internal buds are produced
by some sponges, fragments can regenerate new sponges, and bath sponges can
regenerate from a portion left attached to the sea bottom.
The sponges of today are
mostly specialized in ways that do not indicate the ancestral position of an
unknown ancient member of the Sclerospongea, already specialized in its own
way. Living Sclerospongea were discovered
in the last half of the last century; they live hidden away in cavities in
coral reefs and are presumably quite different from the ones that evolved into
cnidarians.
After listing seven points supporting
the ancestral role of sponges, but before the 1984 report by Kazmierczak, I
made the following statement in the 1981 invertebrate text: “In view of the preceding it is reasonable to
anticipate further evidence of an important phylogenetic position for ancestral
sponges with hopes for clarification or resolution of this issue.” The discovery of a spicule at the apex of some
nematocysts is further new evidence. The
conclusions presented are based in part on hypothetical interpretations of the
role of spicules in the absence of any other reasonable hypothesis.
References
Bergquist, P. R. 1978.
Sponges. Univ. of California Press,
Berkeley. 268 pp.
Engemann, J. G., and R. W.
Hegner. 1981. Invertebrate
Zoology, 3rd ed.
Macmillan, N. Y. 746 pp.
Kazmierczak, Jozef.
1984. Favositid tabulates: evidence for
poriferan affinity. Science, 225:835-837.
Tuzet, O. 1963. The phylogeny of sponges according to embryological, histological, and serological data, and their affinities with the Protozoa and the Cnidaria. pp. 129-148. In E. Dougherty, The Lower Metazoa. Univ. of California Press, Berkeley. 478 pp.
Tuzet, O. 1963. The phylogeny of sponges according to embryological, histological, and serological data, and their affinities with the Protozoa and the Cnidaria. pp. 129-148. In E. Dougherty, The Lower Metazoa. Univ. of California Press, Berkeley. 478 pp.
Joseph G. Engemann July 18, 2013
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