A new tuboid graptolite, Camarotubus graptocamaraeformis gen. et sp.n., is
described from a calcareous erratic boulder of middle Ordovician (Caradoc?)
age from Poland. This encrusting form combines characters of both the tubo
id and the camaroid graptolites, and is regarded as a purely morphological
intermediate between them. This finding supports Kozlowski's (1949) concept
of a close phylogenetic relationship between the orders Tuboidea and Camar
oidea.