Australasian Fossils: A Students' Manual of Palaeontology — John Shaqi
Australasian Fossils: A Students' Manual of PalaeontologyChapman, Frederick
Science
Australasian Fossils: A Students' Manual of Palaeontology
Chapman, Frederick
Paleontology -- Australia
The Sea-mats or Polyzoa, represented by _Retepora_ (the Lace-coral)
(Fig. 24) and _Flustra_ (the Sea-mat) of the present sea-shore, have a
calcareous skeleton, or zoarium, which is easily preserved as a fossil.
Polyzoa are very abundant in the Cainozoic beds of Australia, New Zealand,
and elsewhere (Fig. 25). In the Mesozoic series, on the other hand, they
are not so well represented; but in Europe and North America they play an
important part in forming the Cretaceous and some Jurassic strata by the
abundance of their remains.
WORMS (VERMES).--The hard, calcareous tubes of Sea-worms, the Polychaeta
("many bristles") are often found in fossiliferous deposits, and sometimes
form large masses, due to their gregarious habits of life; they also occur
attached to shells such as oysters (Fig. 26). The burrows of the wandering
worms are found in Silurian strata in Australia; and the sedentary forms
likewise occur from the Devonian upwards.
ECHINODERMATA.--Sea-urchins (Echinoidea) possess a hard, calcareous,
many-plated test or covering and, when living are covered with spines
(Fig. 27). Both the tests and spines are found fossil, the former
sometimes whole when the sediment has been quietly thrown down upon them;
but more frequently, as in the Shepherd's crown type (_Cidaris_), are
found in disjointed plates, owing to the fact that current action, going
on during entombment has caused the plates to separate. The spines are
very rarely found attached to the test, more frequently being scattered
through the marl or sandy clay in which the sea-urchins are buried. The
best conditions for the preservation of this group is a marly limestone
deposit, in which case the process of fossilisation would be tranquil
(Fig. 28).
[Illustration: =Fig. 26.--Fossil Worm Tubes (? Serpula.)=
Attached to a Pecten.
Slightly Enlarged. Cainozoic (Balcombian). Muddy Creek, Hamilton, Victoria.
(_F. C. Coll._)
]
[Illustration: =Fig. 27.=
=A Regular Sea-Urchin (Strongylocentrotus erythrogrammus, Val.)=
About 2/3 nat. size. Showing Spines attached. Living. Victoria.
(_F. C. Coll._)
]
[Illustration: =Fig. 28.--A Fossil Sea-Urchin (Linthia antiaustralis,
Tate).=
Test denuded of Spines.
About 2/3 nat. size. Cainozoic (Janjukian): Curlewis, Victoria.
(_Nat. Mus. Coll._)
]
[Illustration: =Fig. 29.--Ophioderma egertoni, Broderip, sp.=
About 1/2 nat. size. A Brittle Star from the Lias of Seaton, Devon,
England.
(_Nat. Mus. Coll._)
]
The true Starfishes (Asteroidea), are either covered with calcareous
plates, or the skin is hardened by rough tubercles; and these more lasting
portions are preserved in rocks of all ages. The shape of the animal is
also often preserved in an exquisite manner in beds of fine mud or clay.
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