Spirograptus
turriculatus
Phylum
Hemichordata, Graptolithina
Geological
Time: Early Silurian, Late Llandovery Stage (435-434 million years
ago)
Size: 10
mm
Fossil Site:
Cotton Formation, Cottons Hill Quarry, New South Wales, Australia
This
is a specimen of a graptolite whose genus name derives from its
spiral shape. 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.
See
other Graptolite
Fossils
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