Most long distance calcium signals are believed to take the form of ac
tively propagated calcium waves. In 1991, when this proposal was first
advanced, all such waves were thought to belong to one class, for whi
ch fertilization waves were the prototype. Moreover, the speeds of suc
h waves were found to be conserved at about 10 mu m/s for primary fert
ilization waves and 30 mu m/s for waves through fully active systems a
t 20 degrees C. In 1993, preliminary evidence for a second class of su
ch waves was published and the prototype for these were ones which dri
ve cell cleavage. These move at only about 1 mu m/s at 20 degrees C an
d were, therefore, called slow calcium waves as opposed to the fast on
es first considered. Here we compile compelling evidence that slow wav
es comprise a second distinct class of actively propagated calcium wav
es. This is based on 30 papers which yield evidence of slow calcium wa
ves in organisms ranging from Dictyostelium to mammals and phenomena r
anging from the surface contraction waves seen long ago in axolotl egg
s to embryonic cleavage and mitotic waves and to ones recently seen to
accompany primary neural induction in axolotls. Ultraslow and ultrafa
st calcium waves are also considered.