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Graptolites are named after the marks they leave on bedding planes - an early, natural form of graffiti.
The delicate skeletons of these marine invertebrates formed an 'apartment block' for a colony of tiny, individual
animals, probably interconnected by some sort of nervous system.
Graptolites were planktonic, drifting wherever the currents would take them. Their widespread occurrence makes
them good fossils to use for correlating rocks in different parts of the world.
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Dendroid graptolites are found in rocks of Cambrian to Carboniferous age.
Graptoloid graptolites (see photograph) are restricted to the Ordovician and Silurian.
Geopix Study Guide "Graptolites"
- gives an illustrated description of graptolites;
- describes the main morphological features;
- explains how the mode of life can be determined;
- shows how graptolites can be used for correlation.
The Study Guide contains the following pages:
'Grapholites' is part of the Geopix Fossils Study Guide CD.
To order this CD go to the Geopix Online Store