The ultrastructure of Trimastix marina is documented for the first time. Th
is protist has four flagella which insert at the head of a longitudinal fee
ding groove. The basal bodies are elongate and arranged in a cruciate patte
rn. The anterior and posterior basal bodies lack cartwheels. The posterior
flagellum bears two vanes. The anterior flagellum is thickened. The cell ha
s a poorly organised Golgi-like region and small hydrogenosome-like organel
les. The flagellar apparatus includes left and right major microtubular roo
ts which support the margins of the groove, and a third, major anterior roo
t associated with a fan of microtubules which supports the dorsal side of t
he cell, There is also a singlet 'root' associated with the groove, a minor
anterior root and a suite of non-microtubular structures (including the A,
B, C and I fibres). Arrays of microtubules diverge from both left and righ
t roots to support the floor of the groove, Some microtubules from the righ
t array converge to form an inner right root, Halfway down the cell the lef
t root ends, while the right root reduces and associates with a sheet-like
striated/dense composite fibre, The groove ends as a cytopharynx, with a 't
ongue' structure associated with its opening. Trimastix marina is most simi
lar to T: pyriformis, the only previously studied member of Trimastix, Amon
g the other 'excavate taxa', Trimastix is most similar to 'core jakobids',
Malawimonas, Carpediemonas and retortamonads but also shares several unusua
l features with some heteroloboseids. The complexities and detail of struct
ural similarities amongst various excavate taxa support the 'excavate hypot
hesis' (i,e. that the excavate taxa have a common excavate ancestor) but su
ggest that understanding the relationships amongst the excavate taxa throug
h morphological data will be a complex task.