B. Thamdrup et De. Canfield, PATHWAYS OF CARBON OXIDATION IN CONTINENTAL-MARGIN SEDIMENTS OFF CENTRAL CHILE, Limnology and oceanography, 41(8), 1996, pp. 1629-1650
Rates and oxidative pathways of organic carbon mineralization were det
ermined in sediments at six stations on the shelf and slope off Concep
cion Bay at 36.5 degrees S. The depth distribution of C oxidation rate
s was determined to 10 cm from accumulation of dissolved inorganic C i
n 1-5-d incubations. Pathways of C oxidation were inferred from the de
pth distributions of the potential oxidants (O-2, NO3-, and oxides of
Mn and Fe) and from directly determined rates of SO42- reduction. The
study area is characterized by intense seasonal upwelling, and during
sampling in late summer the bottom water over the shelf was rich in NO
3- and depleted of O-2. Sediments at the four shelf stations were cove
red by mats of filamentous bacteria of the genera Thioploca and Beggia
toa. Carbon oxidation rates at these sites were extremely high near th
e sediment surface (> 3 mu mol cm(-3) d(-1)) and decreased exponential
ly with depth. The process was entirely coupled to SO42- reduction. At
the two slope stations where bottom-water O-2 was > 100 mu M, C oxida
tion rates were 10-fold lower and varied less with depth; C oxidation
coupled to the reduction of O-2, NO3-, and Mn oxides combined to yield
an estimated 15% of the total C oxidation between 0 and 10 cm. Carbon
oxidation through Fe reduction contributed a further 12-29% of the de
pth-integrated rate, while the remainder of C oxidation was through SO
42- reduction. The depth distribution of Fe reduction agreed well with
the distribution of poorly crystalline Fe oxides, and as this pool de
creased with depth, the importance of SO42- reduction increased. The r
esults point to a general importance of Fe reduction in C oxidation in
continental margin sediments. At the shelf stations, Fe reduction was
mainly coupled to oxidation of reduced S. These sediments were genera
lly H2S-free despite high SO42- reduction rates, and precipitation of
Fe sulfides dominated H2S scavenging during the incubations. A large N
O3- pool was associated with the Thioploca, and the shelf sediments we
re thus enriched in NO3- relative to the bottom water, with maximum co
ncentrations of 3 mu mol cm(-3). The NO3- was consumed during our sedi
ment incubations, but no effects on either C or S cycles could be disc
erned.