DINOFLAGELLATE CYST PRODUCTION IN THE CARIACO BASIN: A 12.5 YEAR-LONG SEDIMENT TRAP STUDY
The time series consists of > 300 sediment trap samples, each representing ~ 14 days of sedimentation, collected at the CARIACO station between Nov. 8, 1996 and May 19, 2009. Mass fluxes of biogenic silica, calcium carbonate and organic carbon reflect dominantly the timing and strength of wind-driven, seasonal upwelling that brings colder, nutrient-rich waters to the surface, fostering primary productivity and the export of biogenous materials to the depths. On seasonal time scales, dinoflagellate cyst production is closely coupled with upwelling strength, with higher cyst fluxes consistently observed under active upwelling conditions (average of 50.5 × 103 cysts m-2 day-1) compared to non-active upwelling intervals (29.0 × 103 cysts m-2 day-1). Year-to-year variability is characterized by a large increase in cyst production observed over the last ~ 4 years of the time series (2006–2009) and minimum cyst fluxes recorded in the years 1998 and 1999, following the strong 1997/98 El Niño event.
The detailed response of each dinoflagellate cyst taxon to environmental variability is presented in the form of an atlas, providing photomicrographs and detailing overall monthly production, contribution to the total trap assemblage as well as cyst production over the 12.5 years of the time series.