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Plankton trophic structure and particulate organic carbon production during a coastal downwelling-upwelling cycle

机译:沿海岸向下上升-上升周期的浮游生物营养结构和颗粒有机碳的产生

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We evaluated plankton trophic structure in a short-term temporal survey performed throughout a downwelling-upwelling 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 ugC l~(-1) h~(-1)) and MiZA (170 ind. l~(-1)), characterized a micro-bial 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.
机译:我们在巴西东南部沿上升-上升-上升周期进行的短期时间调查中评估了浮游生物的营养结构。在Cabo Frio上升流核心区的固定站点,连续5天估计了大小分级的浮游生物量(PB),微浮游动物(MiZA)和中游浮游动物(MeZA)的丰度以及主要(PP)和细菌产生(BP)。在下沉期间,皮克和浮游生物在PB以及较高的BP(0.1 ugC l〜(-1)h〜(-1))和MiZA(170 ind。l〜(-1))中占主导地位,微生物食物网结构。在南大西洋中央水(SACW)上升之后,BP(0.02μgC l〜(-1)h〜(-1)),MiZA(50 ind。l〜(-1))和浮游生物对PB的贡献降低,随着PB中浮游生物的出现以及机会性草食性co足类动物密度的增加(Paracalanus parvus:2.0 ind.l〜(-1)),表明草食性食物网结构的建立。颗粒有机碳(POC)的产生主要是由于浮游植物(98%)引起的,并且在不同时期之间没有差异。但是,在浮游生物营养相互作用中观察到的变异性应影响该动态系统中POC的出口量。

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