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Learn about the different types of graptolites, from colonial stipes to pelagic floating colonies. Discover how the number of stipes decreased and the structure of thecae became more complex over time. Explore the correlation between Monograptus fossils and Silurian rocks.
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GRAPTOLITES The first graptolites were colonies of animals attached to each other on branches (stipes) and attached to the sea-bed by a hold-fast. They extracted their food from sea-water. STIPES HOLD-FAST
Tetragraptus STIPE As time passed, it became more efficient for graptolite colonies to float freely in the oceans to find food (pelagic floating). The number of stipes reduced and the trilobite animals on each colony decreased in number. Their chambers (thecae) became larger and are clearly seen in this picture. THECAE
TWO STIPES Didymograptus murchisoni In the Ordovician period the number of stipes per colony reduced to two. Often the thecae became more complex in structure. THECA
Monograptus Later, in the Silurian period the two stipes of Didymograptus united and became one, but with thecae on both sides. Monograptus is only found in Silurian rocks and is therefore an excellent zone fossil to correlate rocks of this age. THECAE ON BOTH SIDES OF THE STIPE SINGLE STIPE
Climacograptus Dictyonema