Phyllograptus
fructicosus
Phylum
Hemichordata; Class Graptolithina
Geological
Time: Early Ordovician, Bendigonian Stage (475-473 million years ago)
Size: 20
mm
Fossil Site:
Spring Gully, Bendigo, Victoria, Australia
This
is a fine example of a graptolite that existed during a time that
saw a transgression of the seas over low-lying landforms. Graptolites
are colonial animals belonging to the hemichordates. The term originates
from the patronymic genus Graptolithus. The Graptoloidea were pelagic,
drifting with the currents, and were the most important members
of the plankton before dying out in the early Devonian. Many were
quite cosmopolitan in distribution, and the limited temporal duration
of individual species make them excellent index fossils for correlation
of strata and biota from widespread locations. In addition to the
second partial example at the edge of the matrix, there are several
examples of a very different morphology on the reverse side, making
for a most interesting specimen.
See
other Graptolites
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