Pterobranchs are the closest living relatives of graptolites. Their sk
eleton is constructed from the same material, and in a homologous mann
er. Growth rates of the pterobranch Cephalodiscus gracilis are describ
ed for the first time and, along with rhabdopleuran growth rates, they
are used to estimate the amount of time invested by a graptolite colo
ny in growing its rhabdosome. This is a measure of minimum age. The si
gnificance of age calculations is shown for individuals and large comm
unities of graptoloids. Large individuals can be shown to be much olde
r than the time it would have taken them to settle through seawater an
d so it is shown that graptoloids moved up, as well as down, through t
he water column. Life tables constructed for biserial graptoloids from
the Utica shale in Quebec, Canada, suggest that these graptoloids die
d from constant environmental stress. Graptoloid length can thus be a
function of environment and should only cautiously be considered to be
of taxonomic significance.