Hydrogen profiles and localization of methanogenic activities in the highly compartmentalized hindgut of soil-feeding higher termites (Cubitermes spp.)
D. Schmitt-wagner et A. Brune, Hydrogen profiles and localization of methanogenic activities in the highly compartmentalized hindgut of soil-feeding higher termites (Cubitermes spp.), APPL ENVIR, 65(10), 1999, pp. 4490-4496
It has been shown that the coexistence of methanogenesis and reductive acet
ogenesis in the hindgut of the wood-feeding termite Reticulitermes flavipes
is based largely on the radial distribution of the respective microbial po
pulations and relatively high hydrogen partial pressures in the gut lumen.
Using Clark-type microelectrodes, we showed that the situation in Cubiterme
s orthognathus and other soil-feeding members of the subfamily Termitinae i
s different and much more complex. All major compartments of agarose-embedd
ed hindguts were anoxic at the gut center, and high H-2 partial pressures (
1 to 10 kPa) in the alkaline anterior region rendered the mixed segment and
the third proctodeal segment (P3) significant sources of H-2. Posterior to
the P3 segment, however, H-2 concentrations were generally below the detec
tion limit (<100 Pa). All hindgut compartments turned into efficient hydrog
en sinks when external H-2 was supplied, but methane was formed mainly in t
he P3/4a and P4b compartments, and in the latter only when H-2 or formate w
as added. Addition of H-2 to the gas headspace stimulated CH4 emission of l
iving termites, indicating that endogenous H-2 production limits methanogen
esis also in vivo. At the low H-2 partial pressures in the posterior hindgu
t, methanogens would most likely outcompete homoacetogens for this electron
donor. This might explain the apparent predominance of methanogenesis over
reductive acetogenesis in the hindgut of soil-feeding termites, although t
he presence of homoacetogens in the anterior, highly alkaline region cannot
yet be excluded. In addition, the direct contact of anterior and posterior
hindgut compartments in situ permits a cross-epithelial transfer of H-2 or
formate, which would not only fuel methanogenesis in these compartments, b
ut would also create favorable microniches for reductive acetogenesis, In s
itu rates and spatial distribution of H-2-dependent acetogenic activities a
re addressed in a companion paper (A. Tholen and A. Brune, Appl. Environ. M
icrobiol. 65:4497-4505, 1999).