To quantify the global distribution of free gas in shallow marine sediments
, we have identified and indexed over 100 documented cases in the scientifi
c and engineering literature. Our survey confirms previous assumptions, pri
marily that gas bubbles are ubiquitous in the organic-rich muds of coastal
waters and shallow adjacent seas. Acoustic turbidity, as recorded during se
ismo-acoustic surveys, is the most frequently cited evidence used to infer
the presence of seafloor gas. Biogenic methane predominates within these sh
allow subbottom deposits. Because of their global prevalence, growing inter
est in gassy marine sediments is understandable, as their presence can have
profound scientific, engineering and environmental significance.