Biogeosciences, 15, 2325–2348, 2018 https://doi.org/10.5194/bg-15-2325-2018 © Author(s) 2018. This work is distributed under the Creative Commons Attribution 4.0 License. Physico-chemical and biological factors influencing dinoflagellate cyst production in the Cariaco Basin Manuel Bringué1,2,a, Robert C. Thunell1, Vera Pospelova2, James L. Pinckney1,3, Oscar E. Romero4, and Eric J. Tappa1 1School of the Earth, Ocean and Environment, University of South Carolina, 701 Sumter Street, EWS 617, Columbia, SC 29208, USA 2School of Earth and Ocean Sciences, University of Victoria, P.O. Box 1700, STN CSC, Victoria, BC, V8W 2Y2, Canada 3Belle W. Baruch Institute for Marine and Coastal Sciences, University of South Carolina, 700 Sumter Street, EWS 604, Columbia, SC 29208, USA 4MARUM, Center for Marine Environmental Sciences, University Bremen, Leobenerstraße, 28359 Bremen, Germany anow at: Geological Survey of Canada, 3303 33rd Street NW, Calgary, AB, T2L 2A7, Canada Correspondence: Manuel Bringué (
[email protected]) Received: 20 November 2017 – Discussion started: 22 November 2017 Revised: 19 March 2018 – Accepted: 25 March 2018 – Published: 19 April 2018 Abstract. We present a 2.5-year-long sediment trap record duction in the basin with a 1-year lag, and may have con- of dinoflagellate cyst production in the Cariaco Basin, off tributed to the unusually high fluxes of cysts type “Cp” Venezuela (southern Caribbean Sea). The site lies under (possibly the cysts of the toxic dinoflagellate Cochlodinium the influence of wind-driven, seasonal upwelling which pro- polykrikoides sensu Li et al., 2015), with cyst type Cp fluxes motes high levels of primary productivity during boreal win- up to 11.8 × 103 cysts m−2 day−1 observed during the weak ter and spring.