Supergene chalcocite enrichment during weathering is an economically v
ital natural process that may lead to severalfold increases in the cop
per content of sulfide deposits. A scanning electron microscope study
of chalcocite (Cu2S) from major enriched copper deposits in northern C
hile revealed myriad bacterioform bodies in original growth positions
near replacement interfaces with remnant hypogene sulfide grains. Thes
e minute (0.03 to 0.2 micrometers) chalcocite bodies are interpreted a
s fossilized and metallized nannobacteria that promoted the fixation o
f mobilized copper ions. Bacterial activity may thus be a fundamental
factor in supergene enrichment of copper deposits.