Abstract
We evaluated plankton trophic structure in a short-term temporal survey performed throughout a downwelling-up welling cycle at the SE Brazilian coast. Size-fractioned phytoplankton biomass (PB), microzooplankton (MiZA) and mesozooplankton (MeZA) abundances along with primary (PP) and bacterial production (BP) were estimated for 5 consecutive days at a fixed station in the Cabo Frio upwelling core area. During the downwelling period, the dominance of pico- and nanoplankton in PB, and higher BP (0.1 μg C l-1 h -1) and MiZA (170 ind. l-1), characterized a microbial food web structure. After the South Atlantic Central Water (SACW) upwelling, the decrease in BP (0.02 μg C l-1 h-1), MiZA (50 ind. l-1) and picoplankton contribution to PB, along with the appearance of microplankton in PB and the increase in opportunistic herbivorous copepods densities (Paracalanus parvus: 2.0 ind. l-1) indicated the establishment of a herbivorous food web structure. Particulate organic carbon (POC) production was mainly due to phytoplankton (98%) and did not differ between periods. However, the observed variability in plankton trophic interactions should affect the magnitude of POC export from this dynamic system. © Inter-Research 2008.
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Guenther, M., Gonzalez-Rodriguez, E., Carvalho, W. F., Rezende, C. E., Mugrabe, G., & Valentin, J. L. (2008). Plankton trophic structure and particulate organic carbon production during a coastal downwelling-upwelling cycle. Marine Ecology Progress Series, 363, 109–119. https://doi.org/10.3354/meps07458
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