DOWNWARD EXPORT OF CARBON BY DIEL MIGRANT MESOZOOPLANKTON IN THE CENTRAL EQUATORIAL PACIFIC

Using data collected during cruises of the JGOFS equatorial Pacific St udy in March/April and October of 1992 at the equator (140 degrees W), we examine the downward transport of carbon by three size classes of diel migrant mesozooplankton (200-500 mu m, 500-1000 mu m and 1000-200 0 mu m). In addition to respiratory carbon flux, we consider the flux due to mortality of migrators below the euphotic zone. Diel migrant me sozooplankton biomass was estimated from the difference between nightt ime and daytime biomass within the euphotic zone. Except for a four-da y period early in the March/April cruise, mesozooplankton nighttime bi omass was significantly larger than daytime biomass within the euphoti c zone during both cruises. We estimate that the downward flux of carb on from the euphotic zone due to mesozooplankton diel vertical migrato rs was an average of 0.6 mmol C m(-2) d(-1) and 1.1 mmol C m(-2) d(-1) during the March/April and October cruises, respectively. Addition of this flux to the gravitational particle sinking flux estimated from T h-234 measurements during the same period results in a 31% increase in the carbon export flux from the euphotic zone in the equatorial Pacif ic during the March/April cruise and a 44% increase in the October cru ise. The migratory flux is strongly dependent on whether feeding takes place below the euphotic zone, the length of time migrators spend in the deep waters, and the mortality rate of migrators. (C) 1998 Elsevie r Science Ltd.