The Chain of Life in Geological Time: A Sketch of the Origin and Succession of Animals and PlantsDawson, John William, Sir
Science
The Chain of Life in Geological Time: A Sketch of the Origin and Succession of Animals and Plants
Dawson, John William, Sir
Paleobotany; Paleontology
128 must
have been seven inches in expanse of wings. The habits of the modern
May-flies show us how animals of this group, living as larvæ in the
streams and lakes, must have afforded large supplies of food to fishes,
and when mature must have emerged from the waters in countless myriads,
filling the air for the brief term of their existence in the perfect
state. The May-flies represent another insect order.[50] The
Coal-measures of Saarbruck have afforded several species allied to the
white ants (_Termites_), insects which must have found abundant scope
for their activity in the dead trees of the carboniferous forests. The
occurrence of beetles,[51] especially of the weevil family, which have
as yet been found only in Europe, might have been expected, considering
the habits and modern distribution of this group. It has been asserted
that moths[52] have been found in the Carboniferous; but the proof of
this, so far as known to me, is the occurrence of leaves, noticed by
Sternberg, with markings similar to those made by the larvæ of minute
leaf-mining moths. This, however, is uncertain evidence. If we consider
the orders of insects not found in the Coal-formation, we can perceive
good reasons for the absence of some of them. Those containing the lice
and fleas, and other minute and parasitic insects, we can scarcely
expect to find. The bees and wasps, and the butterflies and moths, are
little likely to have been present where there were scarcely any
flowering plants; but such groups as those of the two-winged flies, the
plant-bugs and the ants, we might have expected, but for the fact of
their being highly specialised forms, and for that reason likely to have
appeared later.[53] There are, indeed, as yet no haustellate or
suctorial insects known in this early period. Plausible theories of the
phylogeny of insects are not wanting; but they do not well suit the
known facts as to their first appearance; and perhaps we may venture
without much blame to apply to the insects of the Coal-period the remark
made by Wollaston with reference to the rich insect fauna of the
isolated rock of St. Helena: “To a mind which, like my own, can accept
the doctrine of creative acts as not necessarily ‘unphilosophical,’ the
mysteries [of the existence of these species in an island so remote from
other lands], however great, become at least conceivable; but those
which are not able to do this may, perhaps, succeed in elaborating some
special theory of their own, which, even if it does not satisfy all the
requirements of the problem, may at least prove convincing to
themselves.”
[Illustration: FIG. 127.—Wings of Cockroaches. From the Coal-formation.
_a_, _Archimulacris Acadicus_ (Scudder). _b_, _Blattina Bretonensis_
(Scudder). _c_, _B. Hesri_ (Scudder).]
[Illustration: FIG. 128.—Wing of May-fly (_Haplophlebium Barnesii_,
Scudder). From the Coal-formation.]
[Illustration: FIG. 129.—A Jurassic Sphinx-moth (_Sphinx Snelleri_,
Weyenburgh).]
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