Australasian Fossils: A Students' Manual of PalaeontologyChapman, Frederick
Science
Australasian Fossils: A Students' Manual of Palaeontology
Chapman, Frederick
Paleontology -- Australia
Polyzoa are divided into the Sub-classes Phylactolaemata, in which the
mouth of the zoöid has a lip, and the series of tentacles is horse-shoe
shaped; and the Gymnolaemata, in which there is no lip to the mouth, and
the tentacles form a complete circle. The first group forms its polypary
of soft or horny material, which is not preserved fossil. The latter
has a calcareous polypary, and is of much importance as a fossil group.
This latter sub-class is further subdivided into the following Orders,
viz.:--Trepostomata ("turned mouths"), Cryptostomata ("hidden mouths"),
Cyclostomata ("round mouths"), and Cheilostomata ("lip mouths" furnished
with a moveable operculum).
=Trepostomata (Palaeozoic).--=
The Order Trepostomata may include some genera as _Monticulipora_ and
_Fistulipora_, previously referred to under the corals. They become
extinct after Permian times. _Fistulipora_ occurs in certain Gippsland
limestones.
[Illustration: =Fig. 83--PALAEOZOIC POLYZOA.=
A--Fenestella margaritifera, Chapm. Silurian. Near Yering, Vict.
B--Polypora australis, Hinde. Carbopermian. Gascoyne River, Western
Australia
C--Rhombopora tenuis, Hinde. Carbopermian. Gascoyne River, Western
Australia
D--Protoretepora ampla, Lonsdale sp. Carbopermian. N.S.W.
]
=Cryptostomata (Palaeozoic).--=
In the order Cryptostomata we have the genus _Rhombopora_ with its long,
slender branches, which occurs in the Silurian of Victoria and the
Carbopermian of Queensland and W. Australia (Fig. 83 C). Of this order a
very important Australian genus is _Fenestella_, the funnel-shaped zoaria
of which are found in the Silurian of Victoria and New South Wales, and
also in the Carboniferous of the latter State. _Fenestella_ also occurs in
the Carbopermian of W. Australia and Tasmania (Fig. 83 A). Accompanying
the remains of _Fenestella_ in the Carbopermian rocks, and closely related
to it, are found the genera _Protoretepora_ and _Polypora_ (Fig. 83 B, D).
Polyzoa have been noticed in Jurassic rocks in W. Australia, but no
species have been described.
[Illustration: =Fig. 84--CAINOZOIC POLYZOA.=
A--Lichenopora australis, MacGillivray. Balcombian. Hamilton, Victoria
B--Heteropora pisiformis, MacGillivray. Janjukian. Moorabool, Victoria
C--Cellaria australis, MacGillivray. Balcombian. Hamilton, Vict.
D--Selenaria cupola, T. Woods sp. Balcombian. Hamilton, Vict.
E--Lepralia elongata, MacGill. Balcombian. Hamilton, Victoria
]
=Cheilostomata (Cretaceous).--=
Species of the genera (?) _Membranipora_ and (?) _Lepralia_, belonging to
the Cheilostomata, have been described from the Lower Cretaceous of the
Darling River, New South Wales, and Wollumbilla, Queensland, respectively.
=Cainozoic Polyzoa.--=
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