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首页> 外文期刊>Deep-sea research, Part II. Topical studies in oceanography >Biomass, feeding and metabolism of mesozooplankton in the equatorial Pacific along 180°
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Biomass, feeding and metabolism of mesozooplankton in the equatorial Pacific along 180°

机译:mesozooplankton生物量、喂养和新陈代谢在赤道太平洋180°

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Mesozooplankton biomasses, grazing rates, and metabolism (respiration, ammonium and phosphate excretion) were measured in the central Pacific (180°; 8°S-8°N) during the EBENE cruise, in October-November 1996. In the HNLC zone, the highest mesozooplankton biomass occurred between 6°S and the equator. The decrease of biomass at the northern part of the HNLC zone was accounted to the passage of a tropical instability wave, carrying poorer zooplankton concentrations from the north. Within the HNLC zone, most of the biomass (60-96%) was found above 100 m in accordance with the upper distribution of phytoplankton and heterotrophic protists. No significant day-night differences were observed in mesozooplankton biomass. These results suggest a strong and permanent coupling between mesozooplankton and the first links of the food chain. Respiration and phosphate excretion rates were steady at the different latitudes, but at the equator, grazing rates were the lowest, and ammonium excretion the highest. These variations were accounted to latitudinal differences in microzooplankton density and in particles C/N ratios, suggesting that more nitrogen was available for food at the equator. Moreover, among the dominant copepod species, higher proportions of carnivorous were found at the equator. Higher particle grazing and ammonium excretion rates occurred at the equator during the day, while the chlorophyll gut content of copepods did not show any significant diel cycle. These results suggest a strong trophic link between mesozooplankton feeding activity, on the one hand, and cyclic variations of phytoplankton production and of of their main predators (microzooplankton protists), on the other hand. From biomass estimations of phytoplankton and protists in the euphotic layer and results of dilution experiments, the production and grazing mortality of the main autotrophic taxa (from picoplankton to microplankton) were computed at the equator. Mesozooplankton, which was mainly involved in the catch of the largest (> 8 μm) food particles, such as diatoms or dinoflagellates, accounted for only a minor part (22%) in total phytoplankton grazing, compared to microzooplankton. As the chlorophyll ration was insufficient to balance its metabolism expenditures, mesozooplankton had to to complete its diet with other sources of food such as microzooplankton. The low level of zooplankton metabolic O:N ratios, suggesting the use of a food with a large protein content, supports of this hypothesis.
机译:Mesozooplankton生物量中,放牧率新陈代谢(呼吸、铵和磷酸排泄)测量中太平洋(180°;1996年的10月。最高mesozooplankton生物量之间发生6°S和赤道。HNLC区北部的贡献热带的通道不稳定波,携带贫穷浮游动物浓度北方。生物质(60 - 96%)被发现超过100年根据上的分布浮游植物和异养原生生物。明显的昼夜差异观察在mesozooplankton生物量。一个强大和永久的之间的耦合mesozooplankton第一个链接的食物链。稳定在不同的纬度,但在哪里赤道,放牧率最低铵排泄最高。是占纬度的差异microzooplankton密度和颗粒C / N率,这表明更多的氮可用于食品在赤道。中占主导地位的桡足动物物种,更高肉食的比例被发现的赤道。排泄率发生在赤道天,而叶绿素肠道的内容桡足类没有任何明显的昼夜循环。这些结果表明强营养链接mesozooplankton喂养活动,之间一方面,和循环变化的浮游植物生产和他们的主要捕食者(microzooplankton原生生物),另一方面。从浮游植物生物量的估计原生生物的透光层和结果稀释试验,生产和放牧死亡率的主要自养类群(从picoplankton microplankton)计算赤道。参与捕捉最大的(> 8μm)食物残渣,如硅藻或甲藻、仅占一小部分总浮游植物(22%)放牧,而microzooplankton。不足以平衡其新陈代谢支出,mesozooplankton必须完成与其他来源的饮食的食物等microzooplankton。代谢O: N比率,建议使用食物蛋白质含量大,支持的这一假设。

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