Australasian Fossils: A Students' Manual of PalaeontologyChapman, Frederick
Science
Australasian Fossils: A Students' Manual of Palaeontology
Chapman, Frederick
Paleontology -- Australia
The _PHYLLOPODA_, which belong to the Crustacea in the strict sense of
the term, comprise the Estheriidae and Cladocera (water-fleas). The
former group is represented by _Leaia mitchelli_, which is found in the
Upper Carboniferous or Carbopermian of the Newcastle District, New South
Wales. In the still later Hawkesbury series (Triassic) of New South Wales,
_Estheria coghlani_ (Fig. 111 D) occurs. This species is a minute form,
the carapace measuring from 1.25mm. to 2mm. in the longer diameter of
the shell. In the upper part of the Wairoa Series (Triassic) of Nelson,
New Zealand, there is found another species of _Estheria_, identified
with a European form _E. minuta_. _Estheria mangaliensis_ is another form
occurring in the Jurassic (Ipswich series) of Queensland. At the present
day these little _Estheriae_ sometimes swarm in countless numbers in
freshwater lakes or salt marshes.
=Ostracoda: Their Structure.--=
Passing on to the next group, the bivalved _OSTRACODA_, we note that these
have existed from the earliest geological periods to the present day. They
are usually of minute size, commonly about the sixteenth of an inch in
length, although some attained a length of nearly one inch (_Leperditia_).
Their bodies are indistinctly segmented, and are enclosed within a
horny or calcareous shell. This shell consists of two valves which are
joined along the back by a ligament or hinge, the ends and ventral edge
remaining quite free. The pairs of appendages present are the antennae
(2), mandibles (1), maxillae (2), and thoracic feet (2). The only portion
found in the fossil state is the bivalved carapace, the two valves being
frequently met with still united, especially when these tiny animals have
settled down quietly on the sea-bed and have been quickly covered with
sediment.
=Features of the Ostracod Carapace.--=
Since the body parts of the ostracod are wanting in the fossil examples,
the generic determination is attended with some difficulty, especially
in regard to the smooth or bean-shaped forms. The chief distinctive
characters to note are, the contour of the carapace seen in three
directions (top, side and end views), the structure of the hinge, and
the position and figure of the muscle-spots or points of adhesion of the
muscular bands which hold or relax the two valves. The valves in certain
genera fit closely upon one another. In others, one overlaps the other,
the larger being sometimes the right (as in _Leperditia_), sometimes
the left (as in _Leperditella_). The hinge-line is often simple or
flange-like, or it may consist of a groove and corresponding bar, or there
may be a series of teeth and sockets. Lateral eye-tubercles are sometimes
seen on the surface of the valve, whilst in the animal there was also a
small eye.
=Habits of Ostracoda.--=
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