the fossils of the Devonian and Caledonian types of old red in Britain we have a pretty full catalogue of invertebrate.
No. of Species. | ||
Polypiaria | 34 | Of these, 25 species are also found in the Silurian system; and 51 in the carboniferous limestone series, 57 occur in the Devonian strata of the Eifel, a limestone district wkich corresponds with the Plymouth group.[1] |
Crinoidea | 16 | |
Lamellibranchiata | 46 | |
Brachiopoda | 83 | |
Gasteropoda | 36 | |
Cephalopoda | 44 | |
Heteropoda | 7 | |
Crustacea | 9 | |
—— | ||
275 | ||
—— |
As characteristic Devonian forms we may mention—
- Cystiphyllum damnoniense.—a. Lamellæ,
- Strombodes vermicularis.—a. Lamellæ.
- Leptæna nodulosa.
- Calceola sandalina.
- Palaeopora pyriformis.
- Strigocephalus Burtini.
- Cyrtoceras tredecimale.—a. Aperture.
- Clymenia laevigata.—a. Aperture.
- Brontes flabellifer.
The fishes of the old red sandstone which have been systematized by Agassiz, and described with much effect by Miller[2], are very characteristic of this palæozoic period. The classification of Agassiz, presented to the British Association in 1843, includes 63 British species, viz.:
Placoid.—Ichthyodorulites 6; Cestraciontes 1.
Ganoid.—Lepidoid 33; Sauroid 13; Coelacanthoid 10.
Some of these, as well as a considerable number of the invertebrate, occur also in Russia, the only region which presents something like a fair example of the