Sp. Pelegri et Th. Blackburn, BIOTURBATION EFFECTS OF THE AMPHIPOD COROPHIUM VOLUTATOR ON MICROBIALNITROGEN TRANSFORMATIONS IN MARINE-SEDIMENTS, Marine Biology, 121(2), 1994, pp. 253-258
Microcosms containing different densities of Corophium volutator, rang
ing from 0 to 6000 ind m(-2) were incubated in a flow-through system.
Benthic fluxes of CO2, O-2, NO3- and NH4+ were measured regularly. Thi
rteen days after setup the microcosms were sacrificed and sediment cha
racteristics, pore water NO3-, No-4(+) and exchangeable NH4+ concentra
tions, and potential nitrification activity were measured. The presenc
e of C. volutator increased overall mineralization processes due to bu
rrow construction and irrigation. The amphipods increased the ratio Si
gma CO2/O-2 fluxes from 0.73 to 0.86 in microcosms inhabited by 0 and
6000 ind m(-2), respectively. Burrow ventilation removed NH4+ from the
sediment, which was nitrified in the oxic layer and transported NO3-
to the burrow sediment, where denitrification potential was enhanced.
Nitrification and total denitrification rates (denitrification of NO3-
coming from the overlying water and of NO3- generated within the sedi
ment) were calculated and discussed. Bioturbation by C. volutator incr
eased both nitrification and denitrification, but denitrification was
stimulated more than nitrification. Denitrification of NO3- coming fro
m the overlying water was stimulated 1.2- and 1.7-fold in microcosms c
ontaining 3000 and 6000 ind m(-2) relative to control microcosms. The
presence of C. volutator (6000 ind m(-2)) stimulated nitrogen removal
from the system, as dinitrogen, 1.5-fold relative to non-bioturbated m
icrocosms. C. volutator individuals used in our study were collected f
rom Norsminde Fjord, Denmark, in 1990.