The Cambridge natural history, Vol. 02 (of 10)Beddard, Frank E. (Frank Evers)
Science
The Cambridge natural history, Vol. 02 (of 10)
Beddard, Frank E. (Frank Evers)
Animals
Amongst the Nereidiformia the remains are fewer, but the {302}acicula and
the hard jaws are preserved in certain rocks, and can be referred to
existing families. _Eunicites avitus_[363] is represented by a double
series of acicula, indicating the parapodia of the two sides; and by
remains of both upper and lower jaws (Fig. 159). Four different species of
the worm have been described from the lithographic slate of Bavaria, of
Jurassic age; and several upper jaws of other Eunicids have been discovered
in the Palaeozoic beds of Canada and Scotland, and have received the names
_Lumbriconereites_, _Oenonites_, and _Arabellites_, in reference to their
nearest allies amongst living genera.
There are, however, numerous remains, in the forms of tracks or casts, in
the earlier rocks, which have been referred to the Polychaeta. The names
_Crossopodia_, _Myrianites_, _Nereites_, _Phyllodocites_, have been given
to some of these traces, though they are open to numerous other
interpretations. Some of the "tracks" are similar to those made by living
Crustacea in walking over wet sand; others appear to be the casts of some
animals. Tubular burrows in rocks or fossils, some straight, others
U-shaped, have received such names as _Arenicolites_, _Scolithus_,
_Histioderma_; whilst under the name _Lumbricaria_ certain cylindrical,
coiled structures, resembling worm "castings," are met with in this same
lithographic stone of Solenhofen. Many of the tubes referred to Polychaetes
by the earlier palaeontologists have been transferred to other groups; thus
_Cornulites_ is now believed to be a Pteropod shell.
This very meagre geological record is quite insufficient to form any basis
for a phylogeny of the group. And this poor supply of remains is not
surprising, when we consider the soft nature of the tissues, the absence,
in the majority of families, of skeleton and of other parts which could
have been fossilised; yet we might have expected a greater abundance of
fossilised jaws than is represented at present. But it must be borne in
mind that the conditions of life of these soft-bodied animals are not
conducive to their leaving abundant fossilised remains.
{303}CHAPTER XII
CHARACTERS OF THE SUB-ORDERS OF POLYCHAETES—CHARACTERS OF THE
FAMILIES—DESCRIPTION OF BRITISH GENERA AND SPECIES—THE MYZOSTOMARIA.
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