The hydrothermal vent tubeworm Riftia pachyptila lacks a mouth and gut and
lives in association with intracellular, sulfide-oxidizing chemoautotrophic
bacteria. Growth of this tubeworm requires an exogenous source of nitrogen
for biosynthesis, and, as determined in previous studies, environmental am
monia and free amino acids appear to be unlikely sources of nitrogen. Nitra
te, however, is present in situ (K, Johnson, J. Childress, R. Hessler, C. S
akamoto-Arnold, and C. Beehler, Deep-Sea Res. 35:1723-1744, 1988), is taken
up by the host, and can be chemically reduced by the symbionts (U. Hentsch
el and H. Felbeck, Nature 366:338-340, 1993), Here we report that at an in
situ concentration of 40 mu M, nitrate is acquired by R, pachyptila at a ra
te of 3.54 mu mol g(-1) h(-1), while elimination of nitrite and elimination
of ammonia occur at much lower rates (0.017 and 0.21 mu mol g(-1) h(-1), r
espectively), We also observed reduction of nitrite (and accordingly nitrat
e) to ammonia in the trophosome tissue. When R. pachyptila tubeworms are ex
posed to constant in situ conditions for 60 h, there is a difference betwee
n the amount of nitrogen acquired via nitrate uptake and the amount of nitr
ogen lost via nitrite and ammonia elimination, which indicates that there i
s a nitrogen "sink" Our results demonstrate that storage of nitrate does no
t account for the observed stoichiometric differences in the amounts of nit
rogen, Nitrate uptake was not correlated with sulfide or inorganic carbon f
lux, suggesting that nitrate is probably not an important oxidant in metabo
lism of the symbionts, Accordingly, we describe a nitrogen flux model for t
his association, in which the product of symbiont nitrate reduction, ammoni
a, is the primary source of nitrogen for the host and the symbionts and ful
fills the association's nitrogen needs via incorporation of ammonia into am
ino acids.