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
FOSSIL CORALS.—A great number of the genera of corals found in the newer
Tertiary deposits, and a smaller number of those occurring in the older
Tertiary and Cretaceous strata clearly belong to families now represented
by recent corals. In the earlier strata, however, fossils are found which
cannot be placed in our system with any degree of certainty. Attempts have
been made from time to time to arrange these corals in their proper
positions by the careful study and comparison of their skeletal features,
but the reasons given are not convincing. The genus _Syringopora_, and the
families Favositidae, Heliolitidae, and Coccoseridae have been noticed in
the chapter on Alcyonaria (pp. 343-346). The family Zaphrentidae will be
noticed when dealing with the order Zoanthidea.
Among the families of fossil corals of uncertain position which may still
be included in the order Madreporaria, the more important are:—
{394}CYATHOPHYLLIDAE, a family of solitary and colonial corals with
numerous radially arranged septa, extending from the Silurian to the
Carboniferous limestone. It includes the genera _Cyathophyllum_, which was
very abundant in Devonian times, and _Lithostrotion_, which, in the times
of the formation of the Carboniferous limestone, occurred in continuous
masses extending over great areas of the sea-bottom. The Cyathophyllidae
may possibly be ancestral to the representatives of both Astraeidae and
Fungiidae, which appeared in the Triassic strata.
The CYATHAXONIIDAE form a family of solitary turbinate or horn-shaped
corals, with septa showing a regular, radial arrangement, and may have been
the ancestors of the modern family Turbinoliidae. They have the same
geological range as the Cyathophyllidae.
The CYSTIPHYLLIDAE.—This family consists of solitary corals with very thin
septa; the interseptal spaces are filled with an abundant vesicular
substance called the "stereoplasm." The systematic position of this family
is very doubtful, as the structure is evidently much destroyed, but by some
authors it is supposed to be ancestral to the family Eupsammiidae.
These three families, together with the Zaphrentidae (p. 406), were
formerly grouped together as the Tetracoralla or Rugosa.
SUB-ORDER 1. ENTOCNEMARIA.
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