This means they existed for a very long time, spanning multiple geological periods:
* Silurian: Late Silurian
* Devonian: Entire period
* Carboniferous: Entire period
* Permian: Early Permian
While they were around for a significant portion of the Paleozoic, they went extinct at the end of the Early Permian, likely due to the Permian-Triassic extinction event.