A phylogeny of 54 Recent and fossil species of Soritacea (Foraminifera) was
used to test the hypothesis that endosymbiosis has driven the evolution of
the clade. Endosymbiosis with photosynthetic eukaryotes is the plesiomorph
ic condition for the entire clade Soritacea. Living species dwell in tropic
al-subtropical, shallow-water habitats and are characterized by the possess
ion of rhodophyte, chlorophyte, or dinophyte photosymbionts. Two distinct c
hanges in endosymbiont type are recognized when endosymbiont type is mapped
in the cladogram of Soritacea: (1) a change from rhodophyte to chlorophyte
endosymbionts occurred in the stem lineage of the least inclusive clade co
ntaining New clade B, Orbiculinida. and Soritida; and (2) a change from chl
orophyte to dinophyte endosymbionts occurred in the stem lineage of the lea
st inclusive clade containing New clade G. New clade H, New clade I, Sorite
s, Amphisorus, and Orbitolites. When habitat and ontogeny are optimized on
the cladogram of Soritida, the acquisition of dinophyte endosymbionts appea
rs as a key innovation that facilitated a switch in habitat from free-livin
g to attached living on non-phytal and phytal substrata. A subsequent chang
e in the attached habitat from nonphytal to predominantly phytal (seagrasse
s and macroalgae) substrata is accompanied by a peramorphic trend in the me
galospheric tests. The diversification (adaptive radiation) of the crown So
ritida subclade resulted from the interplay between the acquisition of a ke
y innovation (dinophyte endosymbionts) and the subsequent change in the eco
logy of the group (radiation to phytal substrates).