Seismic profiling with 3.5-kHz and GeoPulse in the Amazon submarine de
lta indicates that gas-charged sediments cover an area greater than 31
,000 km(2). Gas appears on seismic profiles as gas-brightening reflect
ors near the river mouth, where mud and sand are well stratified. In f
ine sediments of the distal portion of the system, gas turbidity zones
predominate. Biogenic gas is generated during degradation of terrestr
ial and marine organic matter by bacteria. The depth of gas in sedimen
t below the seabed depends in part on anaerobic methane oxidation and
the base of the sulfate reduction zone and on stratigraphic traps.