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首页> 外文期刊>Marine ecology progress series >Temporal dynamics of carbon flow through the microbial plankton community in a coastal upwelling system off northern Baja California, Mexico
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Temporal dynamics of carbon flow through the microbial plankton community in a coastal upwelling system off northern Baja California, Mexico

机译:墨西哥北下加利福尼亚州沿海上升流系统中微生物浮游生物群落中碳流动的时间动态

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ABSTRACT: We investigated the temporal dynamics of carbon flow through the microbial food web of a coastal upwelling system (ENSENADA station) off northern Baja California during 6 cruises (September 2007 to November 2008). Carbon biomass assessments for major autotrophic size groups (pico- to micro-sized cells) and their microzooplankton grazers were based on analyses using flow cytometry, HPLC pigments and epifluorescence microscopy. Taxon-specific phytoplankton growth and microzooplankton grazing rates were determined from 24 h in situ incubations in the euphotic zone using an abbreviated 3-treatment dilution technique. Carbon biomass and instantaneous growth and grazing rate determinations were used to estimate daily rates of taxon-specific production and losses due to microzooplankton grazing. Overall, microbial biomass showed a close balance between autotrophic and heterotrophic components, except during a period of very strong upwelling (April 2008), which favored large phytoplankters and high primary production. Throughout a wide range of environmental conditions, the community primary production (PP) attributed both to small (mostly picophytoplankton and prasinophytes) and large (mostly diatoms and autotrophic dinoflagellates) autotrophs was significantly grazed (78 ± 9% of PP) by small (20 µm) and large (20 µm) ciliates and flagellates (including mixotrophic dinoflagellates), respectively, showing complementary temporal shifts in protistan grazer types that matched the dominant phytoplankton. While large diatoms were strongly consumed by large ciliates during the 2 most productive periods (September 2007 and April 2008), pico- and nano-sized phytoplankton were grazed most by nanoflagellates and small ciliates from November 2007 to January 2008. Consequently, biogenic carbon production in this ecosystem is transferred through a multivorous food web.
机译:摘要:我们研究了在6次航行中(2007年9月至2008年11月),北加利福尼亚北部沿海上升流系统(ENSENADA站)的微生物食物网中碳流动的时间动态。主要自养体大小组(皮细胞到微米大小的细胞)及其微浮游生物放牧者的碳生物量评估是基于使用流式细胞仪,HPLC颜料和落射荧光显微镜进行的分析。使用简化的3处理稀释技术,从在富营养区的24 h原位孵育中确定了分类单元特异性浮游植物的生长和微浮游动物的放牧率。碳生物量以及瞬时生长和放牧率测定用于估计分类群特定日产量和由于微浮游动物放牧而造成的损失的每日速率。总体而言,微生物生物量显示自养成分和异养成分之间的紧密平衡,除非在上升势头非常强劲的时期(2008年4月),这有利于大型浮游植物和高初级生产力。在广泛的环境条件下,小( PP纤毛和鞭毛(包括混合营养的鞭毛鞭毛)分别为20 µm和大(> 20 µm),显示出与优势浮游植物相匹配的原生动物放牧者类型的时间互补性。在两个生产力最高的时期(2007年9月和2008年4月),大型硅藻被大型纤毛虫大量消耗,而在2007年11月至2008年1月,皮鞭状和纳米级浮游植物主要被纳米鞭毛虫和小型纤毛虫吞噬。因此,生物碳的产生在这个生态系统中,食物是通过多种食物网传播的。

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