The Cambridge natural history, Vol. 01 (of 10)Hickson, Sydney J. (Sydney John)
Science
The Cambridge natural history, Vol. 01 (of 10)
Hickson, Sydney J. (Sydney John)
Animals
The existence of the above points of resemblance between Spintharophora and
Tetractinellida suggests a relationship between the two groups as its
cause. In judging this possibility the following reflections occur to us. A
cortex exists in various independent branches of Tetractinellida. It has in
all probability had a different phylogenetic history in each—why not then
in these Monaxonida also? Within single genera of Tetractinellida some
species are corticate, others not, witness _Tetilla_. The value of a cortex
for purposes of classification may easily be overestimated. If we are to
uphold the relationship between these two groups, we must base our argument
on the conjunction of similar characters in each.
The genus _Proteleia_[248] is interesting for its slender grapnel-like
spicules, which project beyond the radially disposed cortical spicules, and
simulate true anatriaenes of minute proportions. That they are not
anatriaenes is shown by the absence of an axial thread in their cladi. It
is not surprising that a form of spicule of such obvious utility as the
anatriaene should arise more than once.
Of exceptional interest, on account of their boring habit, are the
Clionidae. How the process of boring is effected is not known; the presence
of an acid in the tissues was suspected, but has been searched for in vain.
The pieces of hard substance removed by the activity of the sponge take
their exit through the osculum and have a fixed shape[249] (Fig. 108).
As borers into oyster shells, Clionidae may be reckoned as pests of
practical importance, and in some coasts they even devastate the rocks,
penetrating to a depth of some feet, and causing them to crumble away.[250]
Sponges, however, as agents in altering the face of the earth do not figure
as destroyers merely. On the contrary, it has {219}been calculated[251]
that sponge skeletons may give rise with considerable rapidity to beds of
flint nodules; in fact, it appears that a period so short as fifty years is
sufficient for the formation of a bed of flints out of the skeletons of
sponges alone.
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