During 1992, the Joint Global Ocean Flux Study (JGOFS) investigated bi
ogeochemical fluxes in the central equatorial Pacific Ocean. The equat
orial Pacific is the largest natural source of atmospheric carbon diox
ide, but the magnitude of the flux varies interannually with the El Ni
no-Southern Oscillation cycle. Sediments beneath the equatorial upwell
ing are enriched in organic carbon indicating a strong export flux, bu
t contemporary new primary production is lower than expected given the
relative concentrations of new nutrients. The multidisciplinary JGOFS
research plan was designed to address apparent contradictions in this
system, and to assess the. roles of equatorial physical and biologica
l processes in regulating the ocean-atmosphere exchange of carbon.